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  • 1
    Monograph available for loan
    Monograph available for loan
    New York, NY : Cambridge Univ. Press
    Call number: AWI A11-15-89031
    Description / Table of Contents: Thermodynamics, Kinetics and Microphysics of Clouds presents a unified theoretical foundation that provides the basis for incorporating cloud microphysical processes in cloud and climate models. In particular, the book provides: • a theoretical basis for understanding the processes of cloud particle formation, evolution and precipitation, with emphasis on spectral cloud microphysics based on numerical and analytical solutions of the kinetic equations for the drop and crystal size spectra along with the supersaturation equation; • the latest detailed theories and parameterizations of drop and crystal nucleation suitable for cloud and climate models derived from the general principles of thermodynamics and kinetics; • a platform for advanced parameterization of clouds in weather prediction and climate models; • the scientific foundation for weather and climate modification by cloud seeding. This book will be invaluable for researchers and advanced students engaged in cloud and aerosol physics, and air pollution and climate research.
    Type of Medium: Monograph available for loan
    Pages: XVIII, 782 S. : graph. Darst., Kt.
    ISBN: 978-1-107-01603-3
    Language: English
    Note: Contents: Preface. - 1. Introduction. - 1.1. Relations among Thermodynamics, Kinetics, and Cloud Microphysics. - 1.2. The Correspondence Principle. - 1.3. Structure of the Book. - 2. Clouds and Their Properties. - 2.1. Cloud Classification. - 2.2. Cloud Regimes and Global Cloud Distribution. - 2.2.1. Large-Scale Condensation in Fronts and Cyclones. - 2.2.2. Sc-St Clouds and Types of Cloud-Topped Boundary Layer. - 2.2.3. Convective Cloudiness in the Intertropical Convergence Zone. - 2.2.4. Orographic Cloudiness. - 2.3. Cloud Microphysical Properties. - 2.4. Size Spectra and Moments. - 2.4.1. Inverse Power Laws. - 2.4.2. Lognormal Distributions. - 2.4.3. Algebraic Distributions. - 2.4.4. Gamma Distributions. - 2.5. Cloud Optical Properties. - Appendix A.2. Evaluation of the Integrals with Lognormal Distribution. - 3. Thermodynamic Relations. - 3.1. Thermodynamic Potentials. - 3.2. Statistical Energy Distributions. - 3.2.1. The Gibbs Distribution. - 3.2.2. The Maxwell Distribution. - 3.2.3. The Boltzmann Distribution. - 3.2.4. Bose–Einstein Statistics. - 3.2.5. Fermi–Dirac Statistics. - 3.3. Phase Rules. - 3.3.1. Bulk Phases. - 3.3.2. Systems with Curved Interfaces. - 3.4. Free Energy and Equations of State. - 3.4.1. An Ideal Gas. - 3.4.2. Free Energy and the van der Waals Equation of State for a Non-Ideal Gas. - 3.5. Thermodynamics of Solutions. - 3.6. General Phase Equilibrium Equation for Solutions. - 3.6.1. General Equilibrium Equation. - 3.6.2. The Gibbs–Duhem Relation. - 3.7. The Clausius–Clapeyron Equation. - 3.7.1. Equilibrium between Liquid and Ice Bulk Phases. - 3.7.2. Equilibrium of a Pure Water Drop with Saturated Vapor. - 3.7.3. Equilibrium of an Ice Crystal with Saturated Vapor. - 3.7.4. Humidity Variables. - 3.8. Phase Equilibrium for a Curved Interface - The Kelvin Equation. - 3.9. Solution Effects and the Köhler Equation. - 3.10. Thermodynamic Properties of Gas Mixtures and Solutions. - 3.10.1. Partial Gas Pressures in a Mixture of Gases. - 3.10.2. Equilibrium of Two Bulk Phases around a Phase Transition Point. - 3.10.3. Raoult’s Law for Solutions. - 3.10.4. Freezing Point Depression and Boiling Point Elevation. - 3.10.5. Relation of Water Activity and Freezing Point Depression. - 3.11. A diabatic Processes. - 3.11.1. Dry Adiabatic Processes. - 3.11.2. Wet Adiabatic Processes. - Appendix A.3. Calculation of Integrals with the Maxwell Distribution. - 4. Properties of Water and Aqueous Solutions. - 4.1. Properties of Water at Low Temperatures and High Pressures. - 4.1.1. Forms of Water at Low Temperatures. - 4.1.2. Forms of Water at High Pressures. - 4.2. Theories of Water. - 4.3. Temperature Ranges in Clouds and Equivalence of Pressure and Solution Effects. - 4.4. Parameterizations of Water and Ice Thermodynamic Properties. - 4.4.1. Saturated Vapor Pressures. - 4.4.2. Heat Capacity of Water and Ice. - 4.4.3. Latent Heats of Phase Transitions. - 4.4.4. Surface Tension between Water and Air or Vapor. - 4.4.5. Surface Tension between Ice and Water or Solutions. - 4.4.6. Surface Tension between Ice and Air or Vapor. - 4.4.7 Density of Water. - 4.4.8. Density of Ice. - 4.5. Heat Capacity and Einstein-Debye Thermodynamic Equations of State for Ice. - 4.6. Equations of State for Ice in Terms of Gibbs Free Energy. - 4.7. Generalized Equations of State for Fluid Water. - 4.7.1. Equations of the van der Waals Type and in Terms of Helmholtz Free Energy. - 4.7.2. Equations of State Based on the Concept of the Second Critical Point. - Appendix A.4. Relations among Various Pressure Units. - 5. Diffusion and Coagulation Growth of Drops and Crystals. - 5.1. Diffusional Growth of Individual Drops. - 5.1.1. Diffusional Growth Regime. - 5.1.2. The Kinetic Regime and Kinetic Corrections to the Growth Rate. - 5.1.3. Psychrometric Correction Due to Latent Heat Release. - 5.1.4. Radius Growth Rate. - 5.1.5. Ventilation Corrections. - 5.2. Diffusional Growth of Crystals. - 5.2.1. Mass Growth Rates. - 5.2.2. Axial Growth Rates. - 5.2.3. Ventilation Corrections. - 5.3. Equations for Water and Ice Supersaturations. - 5.3.1. General Form of Equations for Fractional Water Supersaturation. - 5.3.2. Supersaturation Relaxation Times and Their Limits. - 5.3.3. E quation for Water Supersaturation in Terms of Relaxation Times. - 5.3.4. Equivalence of Various Forms of Supersaturation Equations. - 5.3.5. Equation for Fractional Ice Supersaturation. - 5.3.6. Equilibrium Supersaturations over Water and Ice. - Liquid Clouds. - Ice Clouds. - Mixed Phase Clouds. - 5.3.7. A diabatic Lapse Rates with Non zero Supersaturations. - 5.4. The Wegener–Bergeron–Findeisen Process and Cloud Crystallization. - 5.5. Kinetic Equations of Condensation and Deposition in the Adiabatic Process. - 5.5.1. Derivation of the Kinetic Equations. - 5.5.2. Some Properties of Regular Condensation. - 5.5.3. Analytical Solution of the Kinetic Equations of Regular Condensation. - 5.5.4. Equation for the Integral Supersaturation. - 5.6. Kinetic Equations of Coagulation. - 5.6.1. Various Forms of the Coagulation Equation. - 5.6.2. Collection Kernels for Various Coagulation Processes. - Brownian Coagulation. - Gravitational Coagulation. - 5.7. Thermodynamic and Kinetic Equations for Multidimensional Models. - 5.8. Fast Algorithms for Microphysics Modules in Multidimensional Models. - 6. Wet Aerosol Processes. - 6.1. Introduction. - 6.1.1. Empirical Parameterizations of Hygroscopic Growth. - 6.1.2. Empirical Parameterizations of Droplet Activation. - 6.2. Equilibrium Radii. - 6.2.1. Equilibrium Radii at Subsaturation. - 6.2.2. Equilibrium Radii of Interstitial Aerosol in a Cloud. - 6.3. Critical Radius and Supersaturation. - 6.4. Aerosol Size Spectra. - 6.4.1. Lognormal and Inverse Power Law Size Spectra. - 6.4.2. Approximation of the Lognormal Size Spectra by the Inverse Power Law. - 6.4.3. Examples of the Lognormal Size Spectra, Inverse Power Law, and Power Indices. - 6.4.4. Algebraic Approximation of the Lognormal Distribution. - 6.5. Transformation of the Size Spectra of Wet Aerosol at Varying Humidity. - 6.5.1. Arbitrary Initial Spectrum of Dry Aerosol. - 6.5.2. Lognormal Initial Spectrum of Dry Aerosol. - 6.5.3. Inverse Power Law Spectrum. - 6.5.4. Algebraic Size Spectra. - 6.6. CCN Differential Supersaturation Activity Spectrum. - 6.6.1. A rbitrary Dry Aerosol Size Spectrum. - 6.6.2. Lognormal Activity Spectrum. - 6.6.3. Algebraic Activity Spectrum. - 6.7. Droplet Concentration and the Modified Power Law for Drops Activation. - 6.7.1. Lognormal and Algebraic CCN Spectra. - 6.7.2. Modified Power Law for the Drop Concentration. - 6.7.3. Supersaturation Dependence of Power Law Parameters. - Appendix A.6. Solutions of Cubic Equations for Equilibrium and Critical Radii. - 7. Activation of Cloud Condensation Nuclei into Cloud Drops. - 7.1. Introduction. - 7.2. Integral Supersaturation in Liquid Clouds with Drop Activation. - 7.3. Analytical Solutions to the Supersaturation Equation. - 7.4. Analytical Solutions for the Activation Time, Maximum Supersaturation, and Drop Concentration. - 7.5. Calculations of CCN Activation Kinetics. - 7.6. Four Analytical Limits of Solution. - 7.7. Limit #1: Small Vertical Velocity, Diffusional Growth Regime. - 7.7.1. Lower Bound. - 7.7.2. Upper Bound. - 7.7.3. Comparison with Twomey’s Power Law. - 7.8. Limit #2: Small Vertical Velocity, Kinetic Growth Regime. - 7.8.1. Lower Bound. - 7.8.2. Upper Bound. - 7.9. Limit #3: Large Vertical Velocity, Diffusional Growth Regime. - 7.9.1. Lower Bound. - 7.9.2. Upper Bound. - 7.10. Limit #4: Large Vertical Velocity, Kinetic Growth Regime. - 7.10.1. Lower Bound. - 7.10.2. Upper Bound. - 7.11. Interpolation Equations and Comparison with Exact Solutions. - Appendix A.7. Evaluation of the Integrals J2 and J3 for Four Limiting Cases. - 8. Homogeneous Nucleation. - 8.1. Metastable States and Nucleation of a New Phase. - 8.2. Nucleation Rates for Condensation and Deposition. - 8.2.1. Application of Boltzmann Statistics. - 8.2.2. The Fokker–Planck
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  • 2
    Call number: AWI G3-16-90176
    Type of Medium: Dissertations
    Pages: XXIV, 168 S.
    Series Statement: Schriftenreihe Physische Geographie 57
    Language: English
    Note: Zugl.: Zürich, Univ., Diss., 2007 , Contents: Abstract. - Zusammenfassung. - Acknowledgements. - Contents. - List of figures. - List of tables. - List of abbreviations. - List of symbols. - Latin symbols. - Greek symbols. - 1 Introduction. - 1.1 State of research. - 1.1.1 Hydrothermal regime of the active layer in debris slopes. - 1.1.2 Slope stability of the active layer in debris slopes. - 1.2 Motivation. - 1.3 Hypothesis. - 1.4 Objectives. - 2 Field investigations. - 2.1 Study site. - 2.2 Field methods. - 2.2.1 Field research infrastructure. - 2.2.2 Field measuring array. - 2.2.3 Measurements in detail. - 2.3 Field results and interpretation. - 2.3.1 Meteorological conditions. - 2.3.2 Hydrological ground parameters. - 2.3.3 Thermal ground parameters. - 2.3.4 Geotechnical parameters. - 2.4 Discussion of field investigations. - 2.4.1 Water balance. - 2.4.2 Heat balance. - 2.4.3 Relation between water and heat balance. - 2.4.4. Suitability of measuring equipment and reliability of data. - 2.4.5 Relevance of results in context of climate change. - 2.5 Summary of field investigations. - 3 Laboratory experiments. - 3.1 Analysis of granular materials. - 3.2 Development of inclinable shear apparatus. - 3.2.1 Requirements. - 3.2.2 Solution. - 3.2.3 Construction. - 3.3 Systematic 4-factorial screening shear test series. - 3.3.1 Methods of systematic shear test series. - 3.3.2 Results and analysis of systematic shear test series. - 3.3.3 Discussion of systematic shear test series. - 3.3.4 Summary of systematic shear test series. - 3.4 Physical simulation of thaw-induced failure of the active layer. - 3.4.1 Methods for simulation of thaw-induced active layer failure. - 3.4.2 Results of simulation of thaw-induced active layer failure. - 3.4.3 Discussion of simulation of thaw-induced active layer failure. - 3.4.4 Summary of simulation of thaw-induced active layer failure. - 3.5 Comparison of systematic shear tests and failure simulation. - 4 Integral discussion of field and laboratory investigations. - 4.1 Implications of the laboratory simulation for the field study site. - 4.2 Implications of the shear test series for the field in general. - 5 Conclusions. - 6 Outlook. - References. - Curriculum Vitae. , Zsfassung in dt. Sprache
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  • 3
    Monograph available for loan
    Monograph available for loan
    Novosibirsk : Izd. Nauka
    Call number: AWI G3-16-90240
    Type of Medium: Monograph available for loan
    Pages: 135 S. , Ill., graph. Darst.
    Language: Russian
    Note: In kyrill. Schr.
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  • 4
    Call number: AWI NBM-17-90885
    Description / Table of Contents: While researching for another film, filmmakers Tom Radford and Peter Raymont came across the story of Nugliak, an Inuvialuit man born just before the end of the 19th century who observed and wrote of the changes that occurred in the north during his lifetime on Herschel Island. Radford's film loosely follows the book, touching on much the same subjects, but using Nugliak's descendents as a link to the present.
    Description / Table of Contents: It is easy to overlook Herschel Island - a tiny speck of land just off the Yukon coast - where the Inuvialuit hunter Nuligak once followed the great journeys of caribou, polar bears, and whales. The island lays silently on the margins of geography, entrapped in the footnotes of history, a forgotten place frozen in time. And yet just over a century ago Herschel Island was a frontier boomtown, branded "the Sodom of the Arctic" by some visitors at the time. A place cohabited by whalers, Inuit, missionaries, and police; a place of contact and conflict; a place where worlds collided and lives were changed forever. It was on Herschel Island that a young Inucialuit boy, Nuligak (later named Bob Cockney by the missionaries) came of age - fascinated by Herschel, but equally repelled by the excess of so-called civilization. Through Nuligak's touching yet tragic life-story expressed through his writings and echoed by his grandchildren's poignant return to the Island - we are offered a unique view into an often troubling past and a potentially hopeful future.
    Type of Medium: Non-book medium
    Pages: 1 videodisc , round, color and black and white ; 4 3/4 in , 116 min. (70 min. + 46 min.)
    Language: English
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  • 5
    Monograph available for loan
    Monograph available for loan
    Fairbanks, Alas. : Institute of Northern Engineering, University of Alaska
    Associated volumes
    Call number: AWI G3-16-90316-1
    In: Ninth International Conference on Permafrost, extended abstracts
    Type of Medium: Monograph available for loan
    Pages: 372 Seiten , Illustrationen
    Series Statement: Ninth International Conference on Permafrost extended abstracts
    Language: English
    Note: Contents: Preface. - NICOP Sponsors. - Deep Permafrost Studies at the Lupin Mine: Hydrogeological and Geochemical Information for Nuclear Waste Disposal / L. Ahonen, T. Ruskeeniemi, R. Stotler, S. Frape, K. Lehto, I. Puigdomenech, M. Hobbs, and P. Degnan. - Effect of Fire on Pond Dynamics in Regions of Discontinuous Permafrost: A State of Change Following the Fires of 2004 and 2005? / G. Altmann, D. Verbyla, K. Yoshikawa, and J. Fox. - Cryological Status of Russian Soils: Cartographic Assessment / T.V. Ananko, D.E. Konyushkov, and E.M. Naumov. - Acoustical Surveys of Methane Plumes Using the Quantitative Echo Sounder in the Japan Sea / C. Aoyama, R. Matsumoto, M. Hiromatsu, and G. Snyder. - Permafrost Delineation Near Fairbanks, Alaska, Using Geophysical Techniques / B.N. Astley and A.J. Delaney. - Preparatory Work for a Permanent Geoelectrical Measurement Station for Permafrost Monitoring at the Hoher Sonnblick, Austria / M. Avian, A. Kellerer-Pirklbauer, A. Römer, and R. Supper. - A Provisional Soil Map of the Transantarctic Mountains, Antarctica / M.R. Balks, M. McLeod, and J.G. Bockheim. - Martian Permafrost Depths from Orbital Neutron and Temperature Measurements / J.L. Bandfield and W.C. Feldman. - Time Series Analyses of Active Microwave Satellite Data for Monitoring of Hydrology at High Latitudes / A. Bartsch. - Impact of Permafrost Degradation on Carbon and Nitrogen Stocks Related to Pedogenesis and Ecosystem Functioning / F. Baumann, J-S. He, P. Kühn, and T. Scholten. - DC Resistivity Soundings Across a Pebbly Rock Glacier, Kapp Linné, Svalbard / I. Berthling and H. Juliussen. - Modeling Thermal and Moisture Regimes of Permafrost with New Deep Soil Configuration in CLASS / J-P. Blanchette, L. Sushama, and R. Laprise. - A Provisional Permafrost Map of the Transantarctic Mountains / J.G. Bockheim, M. McLeod, and M.R. Balks. - Alpine Permafrost Distribution at Massif Scale: Assessment of Mean Surface Temperatures During the Winter Equilibrium Period Thanks to Topoclimatic and Geomorphological Data (Combeynot Massif, French Alps) / X. Bodin, P. Schoeneich, and M. Fort. - Cryogenic Formations of the Caucasus and the Significance of Their Impact on the Natural Phenomena of the Region / I.V. Bondyrev. - Modeling Potential Climatic Change Impacts on Mountain Permafrost Distribution, Wolf Creek, Yukon, Canada / P.P. Bonnaventure and A.G. Lewkowicz. - A Hypothesis: A Condition of Growth of Thick Ice Wedges / A. Brouchkov. - Modeled Continual Surface Water Storage Change of the Yukon River Basin / R. Bryan, L.D. Hinzman, and R.C. Busey. - Freeze/Thaw Properties of Tundra Soils, with Applications to Trafficability on the North Slope, Alaska / C.F. Bryant, R.F. Paetzold, and M.R. Lilly. - Discontinuous Permafrost Distribution and Groundwater Flow at a Contaminated Site in Fairbanks, Alaska / A.E. Carlson and D.L. Barnes. - Thermal Regime Within an Arctic Waste Rock Pile: Observations and Implications / J.W. Cassie and L.U. Arenson. - Seasonal and Interannual Variability of Active Layer Development in Permafrost Wetland Systems / C.M. Chiu and L.C. Bowling. - Twelve-Year Thaw Progression Data from Zackenberg, Northeast Greenland / H.H. Christiansen and C. Sigsgård. - Continued Permafrost Warming in Northwest Alaska as Detected by the DOI/GTN-P Borehole Array / G.D. Clow. - Landsliding Following Forest Fire on Permafrost Slopes, Klondike Area, Yukon, Canada / J. Coates and A.G. Lewkowicz. - A Permafrost Model Incorporating Dynamic Variable Soil Depth and Properties / R. Coppell and S. Venevsky. - Seasonal Sources of Soil Respiration from High Arctic Landscapes Dominated by Polar Stripes / C.I. Czimczik, S.E. Trumbore, and J. Welker. - Greenland Permafrost Temperature Simulations / R.P. Daanen, V.E. Romanovsky, S.S. Marchenko, J.H. Christensen, M. Stendel, and T. Ingeman-Nielsen. - The Importance of Snow Cover Evolution in Rock Glacier Temperature Modeling / M. DallAmico, S. Endrizzi, R. Rigon, and S. Gruber. - The Account of Long-Term Air Temperature Changes for Building Design in Permafrost / I.V. Davidova and L.N. Khroustalev. - The Combined Isotopic Analysis of Late Quaternary Ice Wedges and Texture Ice at the Lena-Anabar Lowland, Northern Siberia / A. Dereviagin, H. Meyer, A. Chizhov, and D. Magens. - Adaptating and Managing Nunavik’s Transportation Infrastructure / G. Doré, A. Guimond, and G. Grondin. - Human Experience of Cryospheric Change in Nunavut, Canada: Preliminary Findings / N. Doubleday, S. Donaldson, T. Vlasova, A. Kushwaha, and M. Ip. - HiRISE Observations of Fractured Mounds in the Martian Mid-Latitudes / C.M. Dundas and A.S. McEwen. - A Soil Freeze-Thaw Model Through the Soil Water Characteristic Curve / S. Endrizzi, R. Rigon, and M. DallAmico. - Mapping and Modeling the Distribution of Permafrost in the Nordic Countries / B. Etzelmüller, H. Farbrot, O. Humlum, H. Christiansen, H. Juliussen, K. Isaksen, T.V. Schuler, R.S. Ødegård, and H. Ridefelt. - First Results of Ground Surface Temperature Modeling in Finnmark, Northern Norway / H. Farbrot, B. Etzelmüller, K. Isaksen, T.V. Schuler, O.E. Tveito, and H.H. Christiansen. - Historical Changes in the Seasonally Frozen Ground Regions of the Russian Arctic / O.W. Frauenfeld, T. Zhang, A.J. Etringer, R.G. Barry, and D. Gilichinsky. - Rock Glaciers in the Kåfjord Area, Troms, Northern Norway / R. Frauenfelder, J. Tolgensbakk, H. Farbrot, and T.R. Lauknes. - Snowpack Evolution on Permafrost, Non-Permafrost Soils, and Glaciers in the Monte Rosa Massif (Northwest Alps, Italy) / M. Freppaz, M. Maggioni, S. Gandino, and E. Zanini. - Climate Change in Permafrost Regions in North America / M.K.Gavrilova. - Maximizing Construction Season in a Subarctic Environment, Fort Wainwright, Alaska / Q. Gehring and F.J. Wuttig. - Pleistocene Sand-Wedge, Composite-Wedge, and Complex-Wedge Growth in Flanders, Belgium / G. Ghysels, I. Heyse, J.-P. Buylaert, A.S. Murray, D. Vandenberghe, F. De Corte, and P. Van den haute. - Response of Arctic and Subarctic Soils in a Changing Earth (RASCHER) – Project of IPY: Methodology, Activity, Results / S.V. Goryachkin, J.M. Kimble, N.B. Badmaev, M. Drewnik, D.G. Fedorov-Davydov, S.A. Iglovski, E.M. Lapteva, G.M., Mazhitova, N.S. Mergelov, V.E. Ostroumov, and E-M. Pfeiffer. - Monitoring of the Floodplain Talik Downstream from the Ust’-Srednekan Reservoir / S.A. Guly and V.M. Mikhailov. - Retrogressive Thaw Slump Impacts on Inconnu Spawning Habitat in the Selawik River, Alaska / R. Hander, K. Yoshikawa, and N. OlsonClimatic Change and Permafrost Stability in the Eastern Canadian Cordillera / S.A. Harris. - Idealized Modeling of the Impact of Atmospheric Forcing Variables on Mountain Permafrost Degradation / C. Hauck and N. Salzmann. - A Method for the Analysis of the Thermal Permafrost Dynamics / M.A. Hidalgo, J.J. Blanco, M. Ramos, D. Tomé, and G. Vieira. - Ground Truth Observations of the Interior of a Rock Glacier as Validation for Geophysical Monitoring Datasets / C. Hilbich, I. Roer, and C. Hauck. - Internal Structure of Rock Glacier Murtèl Delineated by Electrical Resistivity Tomography and Forward/Inverse Modeling / C. Hilbich. - Permafrost Degradation Beneath a Heat-Producing Coal Waste Rock Pile, Svalbard (78°N) / J. Hollesen and B. Elberling. - Patterns in Soil Carbon Distribution in the Usa Basin (Russia): Linking Soil Properties to Environmental Variables in Constrained Gradient Analysis / G. Hugelius and P. Kuhry. - Total Storage and Landscape Distribution of Soil Carbon in the Central Canadian Arctic Using Different Upscaling Tools / G. Hugelius, P. Kuhry, C. Tarnocai, and T. Virtanen. - Liquid Water Destabilizes Frozen Debris Slope at the Melting Point: A Case Study of a Rock Glacier in the Swiss Alps / A. Ikeda and N. Matsuoka. - TSP NORWAY – Thermal Monitoring of Mountain Permafrost in Northern Norway / K. Isaksen, H. Farbrot, B. Etzelmüller, H.H. Christiansen, L.H. Blikra, K. Midttømme, and J.S. Rønning. - Mapping the Mountain Permafrost in Areas Surrounding
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  • 6
    Call number: AWI G3-17-90703-1
    In: Materialy četvertoj konferencii geokriologov Rossii, Tom 1, Časti 1-4
    Type of Medium: Monograph available for loan
    Pages: 375 S. , Ill., graph. Darst., Kt.
    ISBN: 978-5-91304-182-1
    Language: Russian
    Note: Table of Contents - Čast' 1.: Research by the pulsing method of a NRM of the metastable water formed at dissociation freonhydrate-12 in the field of negative temperatures / V. A. Vlasov, A. G. Zavodovsky, M. S. Madygulov, A. N. Nesterov, A. M. Reshetnikov. - Kinetics crystallization subcooling of the water contacting to surface gas hydrate / V. A. Vlasov, A. G. Zavodovsky, M. S. Madygulov, A. N. Nesterov, A. M. Reshetnikov. - Transformation of cryogenic structure of frozen clay soils at plain stamp test / S. S. Volokhov. - About influence of contact zone structure of frozen soils with materials on adfreezing strength / S. S. Volokhov, N. V. Solovyeva. - Possibilities of calculating the effective diffusion coefficient of water vapour in snow due to field observations data / R. I. Gavriliev. - Features of water's crystallization in dispersed rocks / V. N. Golubev, G. A. Rzhanitsyn. - Mass exchange in the system of atmosphere-snow cover-ground / V. N. Golubev, D. M. Frolov. - Physical and mechanical aspects of phase transition processes in frozen and freezing ground / J. B. Gorelik. - The experimental stadies of cryogenic preassure into water-saturated saline soils / S. E. Grechishchev, A. V. Brousehkov, Ark. V. Pavlov, O. V. Grechisheheva. - Phase composition of frozen saline ground with petroleum pollution / E. S. Grechishcheva, R. G. Motenko. - About plastic deformation of frozen rocks / M. M. Iudin. - Studies of Soil Moisture Transfer and ice extraction in clay loam Patterns Under External Pressure / O. A. Kazansky. - Isotopic content of interfacial water and ice frozen ground / V. N. Konischev, V. V. Rogov, V. N. Golubev, S. A. Sokratov. - On longevity and structured physical system organizations (on example of frozen soils and ice) / A. A. Konovalov. - On toughness and deforming the frozen ground / A. A. Konovalov. - The study of deformation characteristics of thawing soils / P. I. Kotov. - Thermal properties of volcanic ashes (Kamchatka) / E. P. Kuznetsova, R. G. Motenko. - About temperature extension coeffision of frozen soils / V. P. Merzlyakov. - Classification indicators of frost-susceptible soils / A. L. Nevzorov. - Separation of the pore solution compounds during mass transfer in disperse ice / V. Ye. Ostroumov, N. V. Ostroumova. - Achievements and problems of frozen soils mechanics / L. T. Roman. - Classification of frozen soils / L. T. Roman, V. I. Aksenov, A. V. Iospa. - Modification of frozen soils and ice by adding polyvinyl alcohol in order to facilitate construction / E. V. Safronov, V. V. Vialdin, V. G. Cheverev, V. E. Gagarin, D. V. Hvostikov. - Method of mass crystallization calculation for multiphased rheological mediums / N. I. Sidnyaev, D. A. Krylov. - The deflected mode of the freezing soils layer taking into account the creep and compliance of the boundary conditions / Z. G. Ter-Martirosyan, P. A. Gorbachev. - Study of deformation characteristics of thawing soils of Vankor oilfield / M. N. Tsarapov. - Influence of outer loading on frost heaving of freezing soils, according to theoretical and experimental researches / V. G. Cheverev, M. A. Minkin, E. V. Safronov, V. E. Gagarin, R. S. Bumaev. , Table of Contents - Čast' 2.: Investigation of glaciers and fumarolic activity of Mt Elbrus / V. A. Alekseev, N. G. Alekseeva, M. G. Daniyalov, P. A. Morozov, C. M. Pershin, P. V. Hlebopashev. - The study of impact craters near the Tunguska meteorite epicenter / V. A. Alekseev, V. V. Kopeykin, N. G. Alekseeva, V. V. Krivulin, L. G. Pelehan', V. A. Rukavishnikov, V. A. Chechin. - Engineering geophysical investigations to substantiate the investments for Nizhne-Timptonsk HPP construction / O. K. Voronkov, N. N. Sigatcheva, O. A. Semenov, Yu. Yu. Punin. - Essentials of technique for seismic hazard zoning of extended linear structures in cryolithic zone / V. I. Dzhurik, S. P. Serebrennikov, L. A. Usynin, E. V. Bryzhak. - Temperature dependence of seasonal changes of electrical resistance of frozen ground / V. N. Efremov. - Role and place geophysical methods at studying criolitozone / Y. D. Zykov, A. V. Koshurnikov, N. V. Paramonov, A. A. Pogorelov, R. D. Ostrovsky, A. Y. Gunar. - EM sounding technology's capability in long-term engineering-geological studies in transition zones (case study: transition of a pipeline Bovanenkovo-Ukhta through Baidaratskaya Bay) / Y. D. Zykov, Y. V. Kuleshov, S. V. Kulakov, A. V. Koshurnikov, E. I. Gorshkov, A. A. Pogorelov, E. M. Sizykh. - Experience using of aerospace infrared thermal data for characteristics of the permafrost / S. G. Kornienko. - Wave characteristics of permafrost in Western Yakutia / L. G. Neradovsky. - Geological-geophysical analysis of seismic events in the cryolithic zone of Mongolia / S. P. Serebrennikov, Ts. Batsaikhan, V. I. Dzhurik, A. Yu. Eskin, A. F. Drennov. - Seismic geocryological study of shallow waters in permafrost / A. G. Skvortsov, M. R. Sadurtdinov, A. M. Tsarev. - Features of seismic methods in engineering geocryological studies / A. G. Skvortsov, A. M. Tsarev, M. R. Sadurtdinov. - Descriptiveness of geophysical methods in the assessment of oil pollution / A. D. Skobelev, Y. D. Zykov, A. V. Koshurnikov, A. A. Pogorelov, P. D. Ostrovsky, A. Y. Gunnar. - Radiolocation of the upper frozen ground in Anadyr city: structure, interpretation, forecast / O. D. Tregubov. - Estimating of rock state and properties in long-tem physical weathering by an ultrasonic method / L. F. Ushakova, O. K. Voronkov. - The efficiency of geophysical methods in studies of cryolithic zone in the process of placer accumulation by dredge acquisition / I. M. Khasanov, N. L. Alevskaya, A. V. Koshumikov. - Impact assessment of cryolithic zone in geophysical explorations of gold minefields on a prospecting step, that arc disposed in background medium, consisted of finest sedimentary rock / I. M. Khasanov, V. M. Sharaphytdinov, A. V. Koshurnikov. - Engineering-geocryological research in offshore area of Kruzenshternsky field in Kara sea / V. A. Kholodilov, M. L. Tsemkalo, M. F. Savitskiy, N. V. Paramonov, A. V. Koshumikov, A. A. Pogorelov. - Using electrical resistivity tomography to investigate near-shore permafrost dynamics / P. Overduin, M. Grigoriev, T. Haberlau, S. Wetterich, S. Westermann, K. Yoshikawa. , Table of Contents - Čast' 3.: Cryogenic and seismogenic deormations in the Late Cenozoic deposits of Tunkinskaya depression in Baikal rift zone / S. V. Alexeev, L. P. Alexeeva, A. C. Gladkov, O. V. Lunina, A. M. Kononov, A. V. Andreev. - Coastal Permafrost evolution of Western Yamal in context of climate change / A. A. Vasiliev, I. D. Streletskaya, R. S. Shirokov, G. E. Oblogov. - Classification of massive ice /Yu. K. Vasil'chuk. - δ18O variation of Late Holocene ice-wedge of Aventdalen, Svalbard / Yu. K. Vasil'chuk, N. A. Budantseva, A. M. Zemskova. - Pollen spectra of massive ice of Yerkutayakha River valley, Southern Yamal Peninsula / A. C. Vasil'chuk, Yu. K. Vasi l'chuk, N. A. Budantscva. - Complex assessment of crioecolological and bioresource state of northern geosystems / L. I. Zotova, S. J. Dedjusova. - Study of Quaternary sediments and ground ice with detailed grane-size composition analysis at Yenisey North / M. S. Pavlov, I. D. Streletskaya, A. G. Matyukhin, G. E. Oblogov, A. V. Surkov. - On rock weathering in Cryolithozone / D. M. Shesternev. - Fossil organic matter in permafrost deposits of northern East Siberia - contents and characteristics / L. Schirrmeister, S. Wetterich, G. Grosse, J. Strauss, C. Siegert, P. P. Overduin, H.-W. Hubberten. , Table of Contents - Čast' 4.: The influence of reservoir parameters on hydrate formation in gas wells in permafrost / E. A. Bondarev, K. K. Argunova, I. I. Rozhin. - Research features of deposits wells with abnormal low field temperature / Z. A. Vasil'eva, D. S. Djafarov. - Technogenic indicators of natural gas hydrates presence in deposits of the western part of the Siberian Platform and Yenisei-Khatanga Depression / Z. A. Vasil'eva, D. S. Dzhafarov. - The commercially viable unconventional gas sources (gas hydrates, coalbed methane and shale gas) - experience of development and prospects in Russia / E. V. Perlova. - Gas hydrate of Yamal region (Yamal Peninsular, Kara Sea's shelf) - occurance, types, resources, technogenic challenges / E. V. Perlova, S. A. Leonov, E. S. Miklyaeva, S. D. Perlov. - Variation of thermal conductivity in gas-saturated sediments during hydrate accumulation and freezing / E. M. Chuvilin, B. A. Buhanov. - Sources of natural gas in cryolithozone of Yamal Pemnsula / V. S. Yakushev. , In kyrill. Schr.
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  • 7
    Monograph available for loan
    Monograph available for loan
    Leningrad : Gidrometeoizdat
    Call number: AWI A10-17-90636
    Description / Table of Contents: The book "Radiation in cloudy atmosphere" is devoted to description of the radiative peculiarities of the cloudy atmosphere which depends on the large-scale and microphysical properties of clouds. The data of micro- and macrophysical and optical characteristics of clouds are widely presented. The various methods for calculations of shortwave and longwave radiative fluxes in cloudy and clear atmosphere are described. There are shown some regularities of variations of albedo, absorbability and heat fluxes of clouds and cloudy atmosphere in dependence on their properties. The empirical radiation models of atmosphere in dependence on their properties. The empirical radiation models of atmosphere are presented. The results of measurements and calculations are compared. The book may be of interest for specialists in atmospheric physics, oceanology and some adjacent sciences. It has a reference character and so may be useful to scientists who take interest in radiation and cloudiness structure of the atmosphere. It may be used also by students, post-graduate students and lectureres of corresponding specialities.
    Type of Medium: Monograph available for loan
    Pages: 279 S.
    Language: Russian
    Note: In kyrill. Schr. , Zsfassung in engl. Sprache
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  • 8
    Monograph available for loan
    Monograph available for loan
    New York, NY [u.a.] : Elsevier
    Call number: AWI G2-17-90655
    Type of Medium: Monograph available for loan
    Pages: S. 123-477 , Ill., graph. Darst., Kt
    ISSN: 0079-6611
    Series Statement: Progress in oceanography Vol. 71, No. 2-4
    Language: English
    Note: Contents: Structure and function of contemporary food webs on Arctic shelves: an introduction / P. Wassmann. - Past glacial and interglacial conditions in the Arctic Ocean and marginal seas - a review / D. A. Darby, L. Polyak and H. A. Bauch. - Climate variability and physical forcing of the food webs and the carbon budget on panarctic shelves / E. Carmack, D. Barber, J. Christensen, R. Macdonald, B. Rudels and E. Sakshaug. - Physical and biological characteristics of the pelagic system across Fram Strait to Kongsfjorden / H. Hop, S. Falk-Petersen, H. Svendsen, S. Kwasniewski, V. Pavlov, O. Pavlova and J. E. Søreide. - Food webs and carbon flux in the Barents Sea / P. Wassmann, M. Reigstad, T. Haug, B. Rudels, M. L. Carroll, H. Hop, G. W. Gabrielsen, S. Falk-Petersen, S. G. Denisenko, E. Arashkevich, D. Slagstad and O. Pavlova.
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  • 9
  • 10
    Monograph available for loan
    Monograph available for loan
    [Fairbanks] : State of Alaska, Department of Natural Resources, Division of Geological & Geophysical Surveys
    Call number: AWI G3-17-91271
    Type of Medium: Monograph available for loan
    Pages: 115 S. , Ill., graph. Darst., Kt.
    Edition: Preliminary Draft
    Series Statement: Guidebook 11
    Language: English
    Note: Conents: PART I FIELD GUIDE TO PERMAFROST, PERIGlACIAL, AND QUATERNARY HISTORY SITES NEAR FAIRBANKS, ALASKA. - Site 1 Thompson Drive / Doug Goering. - Site 2 The Fairbanks Permafrost Experiment Station, Alaska - Historical highlights / Karen S. Henry, Kevin Bjella and Thomas A. Douglas. - Site 3 Trans Alaska Pipeline and Permafrost / Elden Johnson. - Site 4 Studying the effectiveness of an underground adjustable Foundation on alleviating the problems associated with building on permafrost / Danielle L. Jamieson and Michael R. Lilly. - Site 5 Sunnyside House - Building on Permafrost: failures and solutions / Michael R. Lilly and Dennis Filler. - Site 6 O'Connor Creek Pingos / Kenji Yoshikawa. - Site 7 Murphy Dome / De Anne S. P. Stevens. - Site 8 Gold Hill / James E. Beget, David Stone, Paul Layer, Jeffrey Benowitz, and Jason Addison. - Site 9 Thermokarst pits and fens in Goldstream Valley / Torre Jorgenson. - Site 10 Great Northwest Peat Mine / Kenji Yoshikawa and Vladimir Romonovsky. - Site 11 GeoData Center - Map Office - Alaska Satellite Facility User Services Office / Patricia Burns. - Site 12 Thermokarst and drunken forest / Katey Walters. - Site 13 Late-Pleistocene Syngenetic Permafrost in the CRREL Permafrost Tunnel, Fox, Alaska / M. Z. Kanevskiy, H. M. French, and Y. L. Shur (eds.). - Site 14 Thermokarst lakes and methane emissions / Katey Walter. - PART II PERMAFROST FEATURES IN CARIBOU-POKER CREEKS RESEARCH WATERSHED (CPCRW) AND ENVIRONS OF FAIRBANKS, ALASKA / KENJI YOSHIKAWA, VLADIMIR ROMANOVSKY, LES VIERECK, AND LARRY HINZMAN. - Stop 1 Pearl Creek Elementary School Permafrost / Active Layer Monitoring Site (active layer, permafrost temperature). - Stop 2 Goldstream Creek tussock tundra (permafrost condition and Holocene ice wedge). - Stop 3 O'Connor Creek pingo site (open system pingo). - Stop 4 Fox gold mining site permafrost outcrop (Pleistocene ice wedge). - Stop 5 Chatanika (gold mine and convection heat transfer). - Stop 6 Caribou Poker Creeks Research Watershed oil spill experiments: oil spill and frost fire experiments. - Stop 7 Aufeis (icing) and permafrost hydrology. - Stop 8 Caribou Poker Creeks Research Watershed fire impact / thermokarst developments. - Stop 9 Isabella Creek bog lake. - Stop 10 Grenac Creek (Farmer's loop) pingo.
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  • 11
    Call number: AWI Bio-19-92359
    In: Special publications : ESA SP / European Space Agency, 1299
    Type of Medium: Series available for loan
    Pages: VII, 200 Seiten , Illustrationen
    ISBN: 92-9092-393-8
    ISSN: 0379-6566
    Series Statement: Special publications : ESA SP / European Space Agency 1299
    Language: English
    Note: Contents Foreword Introduction / Charles Cockell, Gerda Horneck 1. Mars Simulations - Past Studies on the Biological Response to Simulated Martian Conditions / Aviaja Anna Hansen 2. Possible Atmospheric and UV Conditions on Mars in the Past - Biological Implications / H. Lammer, Yu. N. Kulikov 3. The Microbial Case for Mars and its Implication for Human Expeditions to Mars / Gerda Horneck 4. Response of Organics to Simulated Martian Conditions / J.R.C. Garry, I.L. ten Kate, P. Ehrenfreund, B.H. Foing 5. Mars Simulation Experiments with Complex Microbial Soil Communities / Kai Finster, Aviaja A. Hansen, Lars Liengaard, Karina Mikkelsen, Tommy Kristoffersen, Jonathan Merrison, Per Nornberg, Bente Aa.Lomstein 6. Fungi From Antarctic Desert Rocks as Analogues for Martian Life / S. Onofri, L. Zucconi, L. Selbmann, G. S. de Hoog, D. Barreca, S. Ruisi, M. Grube 7. The Response of Bacillus Subtilis to Simulated Martian Conditions and to the Space Environment / Petra Rettberg 8. Photosynthetic Organisms on Mars - Prospects and Limitations / Charles S. Cockell, Andrew C. Schuerger, Daniela Billi, E. Imre Friedmann, Corinna Panitz 9. Viable Haloarchaea from Ancient Salt Sediments and their Response to Simulated Mars Conditions / Helga Stan-Lotter, Sergiu Fendrihan 10. Response of Methanogenic Archaea from Siberian Permafrost to Martian Thermophysical Conditions / Daria Morozova, Diedrich Mohlmann, Dirk Wagner 11. Adaptation of the Lichen Rhizocarpon Geographicum to Harsh High-Altitude Conditions: Relevance to a Habitable Mars / Rosa de la Torre, Leopoldo Garcia-Sancho, Gerda Horneck 12. Photosynthetic Life Support Systems in the Martian Conditions / Kirsi Lehto, Eira Kanervo, Kurt Stahle, Harry Lehto, Milja Tammi, Joni Virtanen 13. Photo-Catalytic Redox-Processes and Adsorption Water on Mars / Chr. Jung, D. Mohlmann, Chr. Sattler, R. Staudt, M. Weeks 14. Design, Building and Applications of a Portable Martian UV Simulator / C. Kolb, R. Abart, A. Berces, J.R.C. Garry, A. A. Hansen, W. Hohenau, G. Kargl, H. Lammer, MR. Patel, P. Rettberg, H. Stan-Lotter 15. Raman Spectroscopic Analysis of Extremophilic Organisms Under Martian Conditions / Howell G. M. Edwards
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  • 12
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-82/23
    In: CRREL Report, 82-23
    Description / Table of Contents: A direct filtration, water treatment pilot plant was operated on the Kenai River at Soldotna, Alaska, during the summer of 1980. The purpose of the pilot plant operations was to determine the feasibility of the direct filtration process for removal of glacial silt. The major criterion used to determine feasibility was production of water containing less than 1.0 NTU of turbidity. For the range of raw water turbidities encountered (22-34 NTU), the pilot plant testing indicated that direct filtration was feasible and could be considered as an alternative to conventional waiter treatment plants containing sedimentation tanks.
    Type of Medium: Series available for loan
    Pages: 26 Seiten , Illustrationen
    Series Statement: CRREL Report 82-23
    Language: English
    Note: CONTENTS Abstract Preface Conversion factors: U.S. customary to metric Introduction Glacial characteristics Water treatment Materials and methods Experimental design Pilot plant intake Hydrocyclone Chemical addition system Flocculation system Filtration system Pilot plant operations Coagulant chemical preparations Flow measurement Sampling Results and discussion Kenai River w ater quality Evaluation of pilot plant testing Performance of pilot plant elements Physical and chem ical variables Conclusions Recommendations Literature cited
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  • 13
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-82/24
    In: CRREL Report, 82-24
    Description / Table of Contents: Velocity data derived from petroleum industry seismic records from Harrison Bay show that high-velocity material ( or = 2 km/s) interpreted to be ice-bonded permafrost is common. In the eastern part of the bay, the depth to high velocity material increases and velocity decreases in an orderly manner with increasing distance from shore until the layer is no longer apparent. The western part of the bay is less orderly, possibly reflecting a different geological and thermal history. This western part may be an inundated section of the low coastal plain characterized by the region north of Teshekpuk Lake, and could have contained deep thaw lakes, creating low velocity zones. Along some seismic lines, the high-velocity material extends approximately 25 km offshore. Two anomalies have been found which could be associated with rapidly degrading permafrost. One is strong attenuation, which was interpreted as an indication of gas in the shallow deposits. The other is the presence of considerable seismic noise, including identifiable small seismic events. The origin of this noise has not been positively established, and it is proposed that it may indicate that some movement is occurring in the sediments due to thaw.
    Type of Medium: Series available for loan
    Pages: 65 Seiten , Illustrationen
    Series Statement: CRREL Report 82-24
    Language: English
    Note: CONTENTS Abstract Preface Introduction Methods Reading records Refractions Reflections Rayleigh waves Spatial resolution Anomalies Results and discussion Seismic velocity distribution Attenuation Low-level natural seismicity Summary Literature cited Appendix A: Error estimates Appendix B: Velocity profiles Appendix C: Seismic cross sections
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  • 14
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-82/27
    In: CRREL Report, 82-27
    Description / Table of Contents: Recommendations for economical thicknesses for building insulation result from a study of fuel and construction costs of 12 military installations in Alaska. A comparison between the insulation thickness that a building owner might choose today and what he might choose in 20 years indicates a trend for much thicker insulation in the future. An analysis of how much more expensive a building built today with the thickness that would be appropriate 20 years hence indicates only a small penalty in life-cycle costs for the additional insulation. Therefore, a minimum of R-32 walls and R-62 attics is recommended for most of Alaska.
    Type of Medium: Series available for loan
    Pages: 54 Seiten , Illustrationen
    Series Statement: CRREL Report 82-27
    Language: English
    Note: CONTENTS Abstract Preface Conversion factors Summary Introduction Determining economic thicknesses for insulation Background Analysis method for new construction Analysis method for reinsulating existing construction Sensitivity and longevity of the results Sensitivity Longevity Recommendations Saving money vs. saving energy Energy economics conservation Building energy performance standards Conclusion Literature cited Appendix A: Heating system costs Appendix B: Present worth factors Appendix C: Base case and incremental thermal properties Appendix D: LCC comparison graphs for wall and roof systems Appendix E: Cost penalties for energy conservatism Appendix F: Graphic aid for figuring energy savings thermal improvements
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  • 15
    Call number: ZSP-201-82/26
    In: CRREL Report, 82-26
    Description / Table of Contents: The Caribou-Poker Creeks Research Watershed is a small (101.5-sq km) drainage basin located 48 km northwest of Fairbanks, Alaska. Elevations within the watershed range from 210 to 826 m, and approximately 28% of its area is underlain by permafrost. Climatic differences between the watershed and Fairbanks are primarily due to the higher elevation of the watershed. Generally the watershed climatic sites are warmer in winter and cooler in summer than Fairbanks. Within the watershed the greatest temperature contrasts exist in winter, when the valley-bottom sites are beneath the regional air temperature inversion, and the higher sites are above it. From May through September the total precipitation averages 270 mm, 1.47 times that received at Fairbanks. The annual precipitation is about 1.7 times that of Fairbanks. The historical precipitation record at Fairbanks indicates that summer precipitation was below the long-term normal in eight of the eleven years of watershed measurements (1969-1980); no climatic extremes occurred during this period. An analysis of annual streamflow data showed an inconsistency of baseflow recessions from year to year. The runoff-rainfall ratio for individual summer storms averaged 0.35 for Caribou Creek. Comparisons of spot discharge measurements of predominantly permafrost and non-permafrost subwatersheds showed that permafrost-dominated watersheds have a much flashier response to precipitation than non-permafrost watersheds. A comparison of the annual flow distribution of the watershed indicated that Caribou Creek has lower summer and higher winter discharges per unit area than the Chena or Salcha Rivers.
    Type of Medium: Series available for loan
    Pages: 42 Seiten , Illustrationen
    Series Statement: CRREL Report 82-26
    Language: English
    Note: CONTENTS Abstract Preface Introduction Setting Geology and soils Vegetation Climate Air temperature Precipitation Hydrology Annual and monthly runoff Individual storms Baseflow recessions Spatial flow variability Temporal flow variability Summary and conclusions Literature cited Appendix A: Station histories
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  • 16
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-82/29
    In: CRREL Report, 82-29
    Description / Table of Contents: Ice grains in a snow cover with a low temperature gradient assume a well-rounded equilibrium form. However, at temperature gradients of 0.1 to 0.2 C/cm (depending somewhat on temperature and snow density), the rounded grains recrystallize into a faceted kinetic growth form. The large temperature gradient must play a decisive role in moving the vapor fast enough to sustain the rapid growth rate associated with the kinetic growth form. Once the large temperature gradient is removed, the grains recrystallize back to the equilibrium form. the recrystallization occurs in either direction without a change in bulk density. The growth of faceted crystals begins at the warmer base of the snow cover where the excess vapor pressure is largest. A transition between the overlying rounded grains moves upward in time. Faceted crystals also grow just below crusts of reduced permeability, where the increased vapor accumulation can sustain the excess vapor pressure neded for kinetic growth. The heat and vapor flows are described using a model based on thermodynamic equilibrium. The temperature distribution is shown to be quasi-linear at steady state in homogeneous snow. The recrystallization of the snow is modeled using the rounded grains as sources and the faceted grains as sinks. In the future this model should be extended to account for different temperatures among the sources and sinks.
    Type of Medium: Series available for loan
    Pages: 27 Seiten , Illustrationen
    Series Statement: CRREL Report 82-29
    Language: English
    Note: Contents: Abstract Preface Introduction Vapor flow Temperature profile Crystal growth rates Equilibirum versus kinetic growth forms of snow crystals Discussion Summary Literature cited
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  • 17
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-82/30
    In: CRREL Report, 82-30
    Description / Table of Contents: Equations are developed that can be used to determine the amount of gas present in sea ice from measurements of the bulk ice density, salinity and temperature in the temperature range o f-2 to -30°C. Conversely these relationships can be used to give the density of sea ice as a function of its temperature and salinity, considering both the presence of gas and of solid salts in the ice. Equations are also given that allow the calculation of the gas and brine volumes in the ice at temperatures other than that at which the bulk density was determined.
    Type of Medium: Series available for loan
    Pages: 13 Seiten , Illustrationen
    Series Statement: CRREL Report 82-30
    Language: English
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  • 18
    Monograph available for loan
    Monograph available for loan
    Oslo : Arctic Monitoring and Assessment Programme (AMAP)
    Call number: AWI G3-19-92396
    Type of Medium: Monograph available for loan
    Pages: 97 Seiten , Illustrationen
    ISBN: 978-82-7971-073-8
    Language: English
    Note: Contents: What has changed since the Arctic Climate Impact Assessment in 2005? Part 1. How the Arctic cryosphere is changing 1.1. The Arctic cryosphere 1.2. Monitoring change in the Arctic cryosphere 1.3. Snow cover is decreasing 1.4. Permafrost is thawing 1.5. Lakes and rivers are losing ice cover 1.6. Mountain glaciers, ice caps and the Greenland Ice Sheet are all diminishing 1.7. Summer sea-ice cover has declined dramatically Part 2. Why the Arctic cryosphere is changing 2.1. The Arctic climate is changing 2.2. The cryosphere interacts with other aspects of climate Part 3. More change is expected. Where in the Arctic? 3.1. Modelling the future 3.2. Future changes in temperature, rain and snowfall 3.3. Future changes in snow, permafrost, lake and river ice 3.4. Future changes in mountain glaciers, ice caps and the Greenland Ice Sheet 3.5. Future changes in sea ice Part 4. How these changes affect people and nature. Where in the Arctic? 4.1. Changing Arctic ecosystems 4.2. Changing supplies of natural resources 4.3. Changing access 4.4. Changing risks to buildings and land 4.5. Changing movement of contaminants 4.6. Changing Arctic living conditions Part 5. Why changes in the Arctic matter globally 5.1. Changes in the Arctic cryosphere affect the global climate 5.2. Melting Arctic land ice contributes to sea-level rise 5.3. Consequences for global society Part 6. What should be done? 6.1. Adapting to change 6.2. The big unknowns Glossary.
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  • 19
    Monograph available for loan
    Monograph available for loan
    Leningrad : Gidrometeoizdat
    Call number: AWI A4-19-92407
    Type of Medium: Monograph available for loan
    Pages: 127 Seiten , Illustrationen
    Language: Russian
    Note: In kyrillischer Schrift
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  • 20
    Call number: AWI A13-19-92401
    Description / Table of Contents: The book "Mathematical modelling of general circulation of the atmosphere and ocean" (G. I. Marchuk, V. P. Dymnikov, V. N. Lykossov, V. B. Zalesny, V. Ya. Galin) contains the sistematic description of the mathematical and physical aspects of the problem of general circulation atmosphere and ocean modelling, beginning from the governing equations to the analysis of numerical experiments and programme realization on the different generation computers. The problems of sub-grid processes parametrization methods and the sensitivity of the models to the parametrization of the cloud-radiation interaction, large-scale condensation processes parametrization of the boundary layer are also considered in the book. The book is intended for the experts in numerical and applied mathematics, geophysical hydrodynamics as well as students of universities, concerned with numerical methods of the ocean and the atmosphere simulation.
    Type of Medium: Monograph available for loan
    Pages: 320 Seiten , Illustrationen
    Language: Russian
    Note: In kyrillischer Schrift
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  • 21
    Call number: AWI G3-19-92416
    Description / Table of Contents: The book contains proceedings of the Second International School on paleopedology for young scholars «Paleosoils as a source of information about past environments». Abstracts of main lectures, description of region where the School was carried out and papers of young scientists are published in the book. Proceedings of the School are of interest for researchers of soil science, paleogeography, Quaternary geology and ecology.
    Type of Medium: Monograph available for loan
    Pages: 145 Seiten , Illustrationen
    ISBN: 978-5-8406-0430-4
    Language: Russian , English
    Note: CONTENT Preface / M. Dergacheva, A. Makeev Description of study area and paleosol / M. Dergacheva, N. Mironycheva-Tokareva, S. Ponomarev, D. Gavrilov LECTURES Essentials of the paleopedology and a review of Quaternary paleosols of the Northern Hemisphere: main items, presented in the lectures / A. Makeev Paleosols in geologic history of the Earth / A. Makeev Possibilites and limits of pedohumus method used at investigations types and environment of ancient pedogenesis / M. Dergacheva Classification system of paleosols / I. Fedeneva Indicating function of pedogenic carbonates in paleoclimatic reconstruction of Holocene and Pleistocene / O. Khokhlova Miromorphological capacities for reseaching of palaeosoils / M. Lebedeva (Verba) Three-dimensional morphology of soil / A. V. Zakharchenko Paleomagnetic method for studing Pliocene and Quaternary deposits of Siberia (current status, problems, prospects) / Z. N. Gnibidenko Specific chemical state anthropogenic transformed soil of the ancient settlements / O. Yakimenko Geochemical peculiarities of soils as an indicator of specific of their formation and anthropogenic transformation / L. Rikhvanov REPORTS Problem of paleosols weed / A. Blagodatnova Spatial distribution of mobile phosphates in Kamennyi Ambar settlement (Chelyabinsk region) / K. Bojtsova Review of literature data for the study of humus horizon chernozem rate formation / E. Burnatova Pedogenic features in paleosols of Samara Volga region archaeological sites / D. Vassilieva Paleosols of Early Iron Age double kurgan of burial ground Kuigenzhar (Northern Kazakhstan) / D. Gavrilov, R. Ishmuratov, A. Toguzbaev Salt soils of Central-Tuva depression / Ch. Danchai-ool Humus composition of Zaural' e forest-steppe and steppe zones on example of archaeological sites / T. Zhdanova Properties variation of the upper part of the modern soils and surface paleosols of key site Volodarka (Barnaul Priobye) / H. Zhaharova Chernozems morphological properties of key area «Volodarka» / O. Kazachenok Comparative characteristics of the modern turf-podzolic soil and the soil buried under centenary dump (Sysert' District, Middle Urals) / L. Kirilyuk Paleopedology: objects and article of researches (review of publications in a «Soil Science» magazine for 2008-2010) / M. Komarova Soils with a buried humus horizon / B. Mongush Paleogeography formation conditions of Tuva sandy landscapes / Ch. Mongush, S. Kurbatskaya The comparative characteristic of 700-year-old and background soil near Sovetskiy city (middle taiga) / O. Nekrasova Humus soil memory: the conditions and time limits for the conservation of steppe / A. Nikiforov Study Holocene evolution of Central Tuva soil and soil formation / K. Ochur Estimation of restoration rate of damaged soils (on materials of studying archaeological objects of the foreststeppe zone) / E. Politova, V. Valdayskih Some polygenetic chernozem characteristics of the Ob Plateau Eastern edge (for example, the key area "Volodarka") / S. Ponomarev Vertical zonality soils in the Sayan mountains in Tuva / V. Sanchaiban Soil physical properties as a soil memory flash / E. Surkova Peculiarities of soddy-alluvial soil of the river Sysert' water-meadow (The Middle Urals) / A. Uchaev Aqueous extract composition of anthropogenically disturbed soils of Kamennyi Am bar settlement / D. Filimonova Environmental conditions of steppe soils for example near the village of Volodarka / H. Cherepanova New investigations at Tokaj-Csorgukut II. Loess section, Northeast Hungary / D. G. Páll, G. Persaits, P. Sümegi P Preliminary results on the phytoliths of the dutch neolithic site Swifterbant as seen from samples retrieved from soils, pig droppings and molars / G. Persaits, D. C. M. Raemaekers , In kyrillischer Schrift , Beiträge teilweise in englischer, teilweise in russischer Sprache
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  • 22
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-82/42
    In: CRREL Report, 82-42
    Description / Table of Contents: A high-resolution impulse radar profiling system was evaluated for 1) detecting the existence of sea ice which coring has revealed to exist on the bottom of the Ross Ice Shelf at Site J-9, 2) detecting the preferred horizontal c-axis azi-muthal direction of the sea ice crystals, using the voltage amplitude of the radar reflection from the sea ice bottom, and 3) determining the direction of the currents under an Antarctic ice shelf. A field program was conducted consisting of a surface radar survey on the Ross Ice Shelf at Site J-9 and surface and airborne radar profiling on the McMurdo Ice Shelf. The CRREL impulse radar system, operating at a center frequency of either 80 MHz or 20 MHz, was unable to detect the shelf bottom at Site J-9, which drilling revealed to be 416 m below the snow surface. The radar system was used to profile the McMurdo Ice Shelf both from the snow surface and from the air; a shelf thickness of about 275 m was easily detected. Theoretical considerations indicate that the bulk conductivity of the ice shelf at Site J1-9 was higher than originally anticipated, and this limited the radar sounding depth to about 405 m when operating at a frequency of 20 MHz.
    Type of Medium: Series available for loan
    Pages: iv, 19 Seiten , Illustrationen
    Series Statement: CRREL Report 82-42
    Language: English
    Note: CONTENTS Abstract Introduction Profiling system Theoretical considerations Field program Discussion Literature cited
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  • 23
    Non-book medium
    Non-book medium
    [Herstellungsort nicht ermittelbar] : AMBERNET Ltd.
    Call number: AWI NBM-19-92576
    Type of Medium: Non-book medium
    Pages: 1 CD-ROM (circa 25 min) , farbig , 002500 , 12 cm
    Language: English
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  • 24
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-83/30
    In: CRREL Report, 83-30
    Description / Table of Contents: Ice sheets are formed and retained in several ways in nature, and an understanding of these factors is needed before most structures can be successfully applied. Many ice sheet retention structures float and are somewhat flexible; others are fixed and rigid or semirigid. An example of the former is the Lake Erie ice boom and of the latter, the Montreal ice control structure. Ice sheet retention technology is changing. The use of timber cribs is gradually but not totally giving way to sheet steel pilings and concrete cells. New structures and applications are being tried but with caution. Ice-hydraulic analyses are helpful in predicting the effects of structures and channel modifications on ice cover formation and retention. Often, varying the flow rate in a particular system at the proper time will make the difference between whether a structure will or will not retain ice. The structure, however, invariably adds reliability to the sheet ice retention process.
    Type of Medium: Series available for loan
    Pages: iv, 39 Seiten , Illustrationen , 1 Beilage
    Series Statement: CRREL Report 83-30
    Language: English
    Note: Contents Abstract Preface Introduction Natural ice sheets Choosing an ice control structure Flexible structures Ice booms Frazil collector lines Fence booms Rigid or semirigid structures Pier-mounted booms Stone groins Artificial islands Removable gravity structures Timber cribs Weirs Pilings and dolphins Structures built for other purposes Hydroelectric dams Wicket dams Light piers and towers Bridge piers Breakwaters Ice control not using Structures Channel improvements Ice sheet tying Ice sheet bridges Conclusions Literature cited Appendix A: Ice control structure
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  • 25
    Call number: ZSP-201-83/32
    In: CRREL Report, 83-32
    Description / Table of Contents: Ice forces on a bridge pier in the Ottauquechee River, in Quechee, Vermont, were measured by installing fourpanels-each capable of measuring forces in the normal and tangential direction - on both sides of a vertical V-shaped pier nose. The measured forces are presented for a short period during an ice run. After the ice run, the thickness and sizes of the ice floes were measured and the compressive strength of the ice was determined in the laboratory from the ice samples collected along the river banks. The water level measurements made at several locations along theriver are also presented for the period of the ice run.
    Type of Medium: Series available for loan
    Pages: ii, 8 Seiten , Illustrationen
    Series Statement: CRREL Report 83-32
    Language: English
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  • 26
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-83/31
    In: CRREL Report, 83-31
    Description / Table of Contents: A mathematical model is described that is used to determine the maximum ice conveyance capacity of a river channel. Based upon this model, computer programs were developed that enable the ice discharge to be calculated for steady-state flow conditions. For rivers that have uniform flow, the maximum ice-conveying capacity can be described with a simple function expressed in terms of the size of the ice fragments, channel geometry, and the flow of water in the river. For nonuniform flows, the computer program determines the elevation profile of the surface layer in addition to other flow characteristics, such as the velocity and surface concentration of the ice fragments. The location along this surface profile where the ice conveyance capacity becomes less than the upstream supply is determined and is considered to be the position where a surface ice jam or ice bridge will be formed.
    Type of Medium: Series available for loan
    Pages: iv, 21 Seiten , Illustrationen
    Series Statement: CRREL Report 83-31
    Language: English
    Note: CONTENTS Abstract Preface Nomenclature Introduction Constitutive relationships Equations of motion Uniform flow Nonuniform flow Ice transport: Uniform flow Symmetric channel Asymmetric channel Ice transport: Nonuniform flow Further considerations Basis for model improvement Conclusions Literature cited
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  • 27
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-83/29
    In: CRREL Report, 83-29
    Description / Table of Contents: A literature review indicated that the effects or permafrost on streambank erodibility and stability are not yet understood because systematic and quantitative measurements are seriously lacking. Consequently, general controversy exists as to whether perennially frozen ground inhibits lateral erosion and bankline recession, or whether it increases bank recession rates. Perennially frozen streambanks erode because of modification of the bank's thermal regime by exposure to air and water, and because of various erosional processes. Factors that determine rates and locations of erosion include physical, thermal and structural properties of bank sediments, stream hydraulics and climate. Thermal and physical modification of streambanks may also induce accelerated erosion within permafrost terrain removed from the immediate river environment. Bankline or bluffline recession rates are highly variable, ranging from less than 1 m/year to over 30 m/year and, exceptionally, to over 60 m/year. Long-term observations of the physical and thermal erosion processes and systematic ground surveys and measurements of bankline-bluffline recession rates are needed.
    Type of Medium: Series available for loan
    Pages: iv, 26 Seiten , Illustrationen
    Series Statement: CRREL Report 83-29
    Language: English
    Note: CONTENTS Abstract Preface Introduction Stream bank erosional processes Permafrost and related factors Permafrost and erosion General Erosional processes Bank zone processes Bluff zone processes Factors affecting perm afrost erodibility Exposure to currents and wind waves Texture and stratigraphy Ice content, distribution and type Slope aspect Coriolis force Timing and depth of thaw Water level and temperature Vegetation Ice and snow cover Groundwater Rates and timing of erosion and recession Overall effects of permafrost Recommendations for research Literature cited Appendix A : Processes of stream bank modifications
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  • 28
    Call number: ZSP-980-70
    In: 2nd Working Meeting "Radioisotope Application and Radiation Processing in Industry", Part 2, 50 to 97
    In: ZfI-Mitteilungen, Nr. 70
    Type of Medium: Series available for loan
    Pages: 355 Seiten , Illustrationen
    ISSN: 0323-8776
    Series Statement: ZfI-Mitteilungen 70
    Language: English
    Note: Contents of Part 2 Hecht, K. Gerber, R. Otto: Studies on the drying of paints by means of 14C-labelled compounds K. Wagner, F. Brutschin, I. Ritter, T. Gritsch, H. Zimmermann, H. Borchert: Investigations by the aid of radioisotope methods on the technology of the production of carbon and silicon carbide materials K. Gloe, P. Mühl: Determination of metal extraction process parameters using tracer technique W. Migdał, W. Łada, K. Malec-Czechowska: Studies on liquid-liquid extraction of noble metals using radiotracers L. Petryka, K. Przewłocki: Radiotracer investigations of benefication copper ore in the industrial flotation process Z. Bazaniak, J. Palige: Determination of Cu recovery degree from slags in shaft process by means of radiotracers R. Burek, J .K. Zurawicz: On the optimization of concentration measurements in heterogeneous materials based on β-backscatter measurements B. Heinrich: Analysis of carbon content in crude brown coal by inelastic scattering of neutrons and the method of time correlated associated particles P. Urbańaki, D. Wagner, M. Jankowska, E. Kowalska: Determination of calcium and iron and measurements of ash content in the brown coal H.-W. Thümmel: Some considerations relating to the prediction of the efficiency of radiometric methods for the continuous ash content determination of coal L. Wawrzonek: Monitor of ash content of coal with X-ray source I. Pavlicsek, V. Stenger, A. Veres: Apparatus for gamma activation analysis I. Végvári, I. Juhász: Determination of PbO content of lead-glass samples on the ground of gamma-absorption E. Schöntube, H.-J. Große: Aerosol ionization gas analysis as a monitoring for waste halothane in the atmosphere of operating theatre S. Mothes, P. Popp, G. Oppermann, W.-D. Herberg: Measurement of fluorocarbons with the ECD P. Popp, E. Schöntube, G. Oppermann: The usability of radiation ionization detectors for the determination of N2O concentrations in the air of operating theatres P. Popp, G. Arnold, G. Oppermann: A hydrocarbon-sensitized argon ionization detector for the detection of inorganic compounds R. Szepke, W. Lisieski, J. Harasimczuk: Automatic dust monitor AMIZ G. Vormum: Sealed sources - problems of design, measurement and quality control L. Gąsiorowski: New trends in developments of ratioisotope gauges in Poland G. Brunner: Direct chemical information from special radio tracers as well as from outer X-ray excitation J. Hirling: Experience and future trend in industrial application of nuclear methods in Hungary I. N. Ivanov, O. K. Nikolaenko, Yu. V. Phecktistov, V. L. Chulkin: Use of short-lived nuclides in activation analysis Kl.-P. Rudolph, J. Flachowsky, A. Lange: Trace element determination in semiconducter selenium by neutron activation analysis (NAA) W. Lisieski, J. Mirowicz: Some industrial applications of instruments with neutron sources R. Dybczyński, H. Maleszewaka, S. Sterliński, Z. Szopa, M. Wasek: Some problems in neutron activation determination of gold and silver in ores and concentrates of copper industry L. Jankowski: Cost-benefit aspects of radioisotope application in industry B. Manouchev, T. Boschkova, L. Tsankov, V. Gurev, I. Kojucharov, G. Grozev: On the possibilities of the direct gamma-spectremetry in natural waters P. Morgenstern, D. Müller, W. Riedel: A parallel grid proportional scintillation counter for the X-ray region from 3 to 20 keV with regard to high count rates N. A. Anders, V. S. Isaev, V. I. Filatov, B. E. Kolesnikov, D. Müller, P. Morgenstern, W. Riedel, V. P. Varvaritsa: X-ray fluroescence analyzer of light elements with proportional scintillation counter D. Müller, P. Morgenstern, W. Riedel, W. Warwariza, B. E. Kolesnikow, N. A. Anders, W. J. Filatov: General considerations concerning the use of the X-ray analyzer "RALE" in industry
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  • 29
    Call number: ZSP-980-71
    In: 2nd Working Meeting "Radioisotope Application and Radiation Processing in Industry", Part 3, 98 to 155
    In: ZfI-Mitteilungen, Nr. 71
    Type of Medium: Series available for loan
    Pages: 368 Seiten , Illustrationen
    ISSN: 0323-8776
    Series Statement: ZfI-Mitteilungen 71
    Language: English
    Note: Contents of Part 3 P. Popp, J. Leonhardt: Characterization of coulometric and hypercoulometric ECD mode of operation D. Hinneburg, H.-J. Grosse, J. Leonhardt, P. Popp: Calculation of current-voltage characteristics of electron-capture detectors A.G. Rozno, V.V. Gromov: Study of volume electric charge in radioactive dielectrics by the method of "acoustic sounding" Iv. N. Pandev, M.G. Christova, St.D. Stefanov, N.V. Gentchev, St.T. Bakardjiev, D.T. Genov, Ch.D. Christov: Portable gamma-irradiator - modified model P. Hargittai, V. Stenger: Planning of dose-rate distribution of radiation fields by computer M. Remer: DOSKMF2 - A contribution to the computer-aided design of dose rate distributions A. Heger, H. Dorschner, W. Schumann, D. Pleul: Characterization of the radiation field and control of the optimal electron beam accelerator operation for industrial processes V. Prenerov, K. Shivarov, P. Ivanov: Programme for radiation protection by using portable defectoscopes in industrial building T. Geßner, K. Irmer: Nuclear radiation detectors using high resistivity neutron transmutation doped silicon H.-G. Könnecke, D. Luther: The influence of airing systems on the residence time in biological clarification plants J. Dermietzel, C. Wienhold, H. Grundmann, A. Staschok, J. Koch, E. Bordes: Tracer studies on carbon monoxide and carbon dioxide formation in liquid phase oxidation of p-xylene W. Smułek: Use of technical mixtures of carboxylic acids to the extraction of silver H. Förster: Determination of oxide film thickness on aluminium using 14-MeV neutron activation and BET method H. Jaskólska, L. Waliś, C. Janusz: Investigations of the monocrystallization process of neodymium doped YAG using radiotracers H. Wagler: Substoichiometric determination of Pd-II-traces with dithizone and problems of determination P. Tábor, L. Molnár, D. Nagymihá!yi: Radioisotope gauge for automatic control of cottonwool package H.-W. Thummel, G. Körner, D. Fritzsche: Compensation for thickness variations in determining the bulk material composition on conveyor belts using combined scatter-transmission and thickness measuring methods D. Fritzsche, W. Dolak: Radiometric determination of ash content of raw lignites M. Braune: A simplified mathematical model for scattered transmission of X-rays in raw brown coal P. S. Kamenov, E. I. Vapirev, S. I. Ormandjiev: A new type of nuclear weighing device for transporter belts W. Smulek, M. Borkowski: Separation of reduced molybdenum from fission products. The Mo - HN03 - HDEHP system J. Komosiński, M. Radwan: Selected problems of radioisotope technique for wear investigation of precise elements Dr. A. Várkonyi: The thin layer activation for industry G. Hartmann, P. Kulicke: Wear testing in power stations J. Kraś, Z. Banasik: The radioisotopes in wear investigation of combustion engines H.-D. Grohmann: Short-time measurements of wear on surface activated rails G.M. Ter-Akopian, E.A. Sokol, Fam Ngok Chyong, M.P. Ivanov, L.P. Chelnokov, V.I. Smirnov, V.A. Gorshkov: Neutron multiplicity detector for the study of rare nuclear decay events L. Gąsiorowski, P. Mroziński, K. Sobkowicz, F. Zrudelny: Implementation of Intel 8080 - based microcomputer system in the radioisotope measurements control instrumentation W. Birkholz, M. Steinert: Evaluation of autoradiograms using a microcomputer F. Myšák, M. Krejči, J. Hakl, E. Smrkovský: Study of boron diffusion in high temperature Ni-base alloys by means of solid state track detectors W. Birkholz, H.-Ch. Treutler, K. Freyer, M. Geisler, J. Dubnack: Autoradiography of gallium in silicon H.C. Treutler, K. Freyer: On quantitative autoradiography of semiconductor basic material A.S. Shtan': Radiation evaluation techniques and facilities used for quality assurance of fuel elements and fuel assemblies for nuclear power plants D. Babić, A. Šafranj, V. Marković: Radiation degradation of poly-propylene-molecular weight and melt viscosity change A. Ciszek: Modern irradiation processes equipment-accelerators and their applications G. Kummer: Identification of signals by means of the decision theory N.S. Batchvarov, I.D. Vankov, L.P. Dimitrov, Ch.D. Shukov, P.A. Pavlov: Betareflektometer SR-77
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  • 30
    Monograph available for loan
    Monograph available for loan
    Bremerhaven : Alfred-Wegener-Institut für Polar- und Meeresforschung
    Call number: AWI Bio-19-20533
    Type of Medium: Monograph available for loan
    Pages: 48 Seiten , Illustrationen
    Language: English
    Note: Content: Preface. - Polar ecosystems in a changing climate. - Ice edge blooms - Migrating oases in polar seas. - Antarctic: Krill has evolved adaptation strategies to its extreme environment. - Living at -20 degrees: why sea Ice algae don't freeze up. - ocean acidification and Iron deficiency affect Antarctic phytoplankton communities. - The oceans are acidifying: spIder crabs and Ice fIsh are feeling the repercussions of climate change. - melting glaciers - Changing coastal ecosystems in the West Antarctic. - In the service of science: elephant seals explore the Southern Ocean. - Ocean Acoustics - palaoa broadcasts live from the Southern Ocean. - When ice shelves disintegrate - diversity of life on the Antarctic seabed. - RV 'Polarstern' in Antarctica - observations in the ice. - deep-sea observatory in the Arctic: Climate change affects life on the ocean floor. - plankton rain in the vicinity of the Arctic HAUSGARTEN: What do sinking particles tell us?. - pelagic research in the Arctic faces new challenges. - fram observatory - live conference with the Arctic deep sea in preparation. - dom - the oceans' molecular memory. - siberian forests moving north - impact on the climate and biodiversity. - promoting young talent: High school pupils learn together with AWI scientists. - dream job- polar scientist - How a student achieved her goal over an icy path. - marIne biosciences in the scientific-societal context of the 21st. century. - Contact persons at the AWI. - Imprint. - geographic locatIons of the research reports of this brochure
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  • 31
    Call number: AWI Bio-20-93530
    Description / Table of Contents: The Arctic tundra, covering approx. 5.5 % of the Earth’s land surface, is one of the last ecosystems remaining closest to its untouched condition. Remote sensing is able to provide information at regular time intervals and large spatial scales on the structure and function of Arctic ecosystems. But almost all natural surfaces reveal individual anisotropic reflectance behaviors, which can be described by the bidirectional reflectance distribution function (BRDF). This effect can cause significant changes in the measured surface reflectance depending on solar illumination and sensor viewing geometries. The aim of this thesis is the hyperspectral and spectro-directional reflectance characterization of important Arctic tundra vegetation communities at representative Siberian and Alaskan tundra sites as basis for the extraction of vegetation parameters, and the normalization of BRDF effects in off-nadir and multi-temporal remote sensing data. Moreover, in preparation for the upcoming German EnMAP (Environmental Mapping and Analysis Program…
    Type of Medium: Dissertations
    Pages: circa 330 Seiten , Illustrationen, Diagramme
    Language: English
    Note: TABLE OF CONTENTS Abstract Kurzfassung Table of Contents List of Figures List of Tables List of Abbreviations List of Symbols 1 INTRODUCTION 1.1 Background and Scientific Setting 1.2 Motivation and Research Questions 1.3 Structure of Thesis 2 FUNDAMENTALS OF HYPERSPECTRAL AND SPECTRO-DIRECTIONAL REMOTE SENSING 2.1 Hyperspectral Remote Sensing of Vegetation 2.2 Spectro-Directional Remote Sensing of Vegetation 2.3 The EnMAP Satellite System 2.4 Spectro-Goniometer Systems for the Ground-Based Measurement of BRDF Effects 3 THE TUNDRA PERMAFROST STUDY LOCATIONS AND THEIR ENVIRONMENT 3.1 The Eurasia Arctic Transect (EAT) 3.1.1 Geological and Climatic Setting 3.1.2 Vegetation 3.2 The North American Arctic Transect (NAAT) 3.2.1 Geological and Climatic Setting 3.2.2 Vegetation 4 OBSERVATIONS AND METHODOLOGY 4.1 Observations Used for this Study 4.1.1 The ECI-GOA-Yamal 2011 Expedition 4.1.2 The EyeSight- NAAT-Alaska 2012 Expedition 4.1.3 Data Used for Hyperspectral Characterization of Arctic Tundra 4.1.4 Data Used for Spectro-Directional Characterization of Arctic Tundra 4.2 Methodology Used for Field Work and Data Analysis 4.2.1 Field Spectroscopy and Hyperspectral Data Analysis 4.2.2 Considerations for the Field Spectro-Goniometer Measurements and the Spectro-Directional Data Analysis 5 DEVELOPMENT AND PRECOMMISSIONING INSPECTION OF THE MANTIS FIELD SPECTRO-GONIOMETER 5.1 Introduction 5.2 Theoretical Background 5.3 Description of the Field Spectro-Goniometer System 5.3.1 Construction Schedule 5.3.2 Description of the Field Spectro-Goniometer Platform (ManTIS) 5.3.3 Sensor Configuration of the AWI ManTIS Field Spectro-Goniometer 5.3.4 Measurement Strategy 5.3.5 Software for Semi-Automatic Control 5.4 Error Assessment 5.4.1 Radiometrical Accuracy 5.4.2 Pointing Accuracy 5.4.3 Ground Instantaneous Field of View and Sensor Self-Shadowing 5.4.4 Temporal Illumination Changes and Environmental Influences 5.5 Data Analysis 5.5.1 Data Processing 5.5.2 Data Visualization 5.6 Performance of ManTIS Field Spectro-Goniometer in the Field 5.6.1 Test Site and Experiment Setup 5.6.2 Results and Discussion 5.7 Conclusions and Outlook 6 HYPERSPECTRAL REFLECTANCE CHARACTERIZATION OF LOW ARCTIC TUNDRA VEGETATION 6.1 Introduction 6.2 Material & Methods 6.2.1 Study Area 6.2.2 Environmental Gradients/Zones and Vegetation Description 6.2.3 Data Acquisition and Pre-Processing 6.2.4 Data Analysis 6.3 Results 6.3.1 The Zonal Climate Gradient 6.3.2 Acidic Versus Non-Acidic Tundra (Soil pH Zones) 6.3.3 The Toposequence at Happy Valley (Subzone E) 6.3.4 The Soil Moisture Gradient at Franklin Bluffs (Subzone D) 6.4 Discussion 6.4.1 Overview of Field Characterization and Spectral Properties along the Gradients 6.4.2 Performance of Spectral Metrics and Vegetation Indices 6.5 Conclusions 7 RESULTS OF THE SPECTRO-DIRECTIONAL REFLECTANCE INVESTIGATIONS 7.1 Overview of the Spectro-Directional Reflectance Characteristics of Low Arctic Tundra Vegetation 7.1.1 Representativeness of the Study Plots Representing Tundra Vegetation 7.1.2 Vaskiny Dachi – Bioclimate Subzone D 7.1.3 Happy Valley – Bioclimate Subzone E 7.1.4 Franklin Bluffs – Bioclimate Subzone D 7.2 Influence of High Sun Zenith Angles on the Reflectance Anisotropy 7.2.1 MAT (Happy Valley) 7.2.2 MNT (Franklin Bluffs) 7.3 Variability in Multi-Angular Remote Sensing Products of Low Arctic Tundra Environments 7.3.1 Spectro-Directional Variability of Different Low Arctic Plant Communities 7.3.2 Spectro-Directional Variability under Varying Sun Zenith Angles 8 DISCUSSION 8.1 The Hyperspectral Reflectance Characteristics of Tundra Vegetation in Context of the Spectro-Goniometer Measurements 8.2 Applicability of the ManTIS Field Spectro-Goniometer System 8.3 The Spectro-Directional Reflectance Characteristics of Tundra Vegetation 8.4 Variability in Reflectance Anisotropy at High Sun Zenith Angles 8.5 Applicability of Multi- Angular Remote Sensing Products for Arctic Tundra Environments 9 CONCLUSIONS & OUTLOOK Acknowledgments References Appendix Table of Contents of the Appendix References of the Appendix Statutory Declaration / Eidesstattliche Erklärung
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  • 32
    Call number: AWI Bio-20-93529
    Description / Table of Contents: The Arctic is considered as a focal region in the ongoing climate change debate. The currently observed and predicted climate warming is particularly pronounced in the high northern latitudes. Rising temperatures in the Arctic cause progressive deepening and duration of permafrost thawing during the arctic summer, creating an ‘active layer’ with high bioavailability of nutrients and labile carbon for microbial consumption. The microbial mineralization of permafrost carbon creates large amounts of greenhouse gases, including carbon dioxide and methane, which can be released to the atmosphere, creating a positive feedback to global warming. However, to date, the microbial communities that drive the overall carbon cycle and specifically methane production in the Arctic are poorly constrained. To assess how these microbial communities will respond to the predicted climate changes, such as an increase in atmospheric and soil temperatures causing increased bioavailability of organic carbon, it is necessary to investigate the current status …
    Type of Medium: Dissertations
    Pages: 146 Blätter , Illustrationen
    Language: English
    Note: Table of content Abstract Zusammenfassung 1. Introduction 1.1. Motivation 1.2. Scientific Background 1.2.1. Permafrost in arctic environments 1.2.2. Carbon storage and emission in arctic environments 1.2.3. Methane cycling in arctic environments 1.3. Study Sites 1.3.1. Lena-Delta, Siberia 1.3.2. El’gygytgyn Crater Lake, Chukotka 1.4. Objectives and approach 1.5. Thesis organization 1.6. Summary of the included manuscripts and contribution of the co-authors 1.6.1. Response of methanogenic archaea to Late Pleistocene and Holocene climate changes in the Siberian Arctic 1.6.2. Response of microbial communities to landscape and climatic changes in a terrestrial permafrost sequence of the El’gygytgyn crater, Far East Russian Arctic 1.6.3. Glacial-interglacial microbial community dynamics in Middle Pleistocene sediments in the Lake El’gygytgyn, Far East Russian Arctic 2. Response of methanogenic archaea to Late Pleistocene and Holocene climate changes in the Siberian Arctic 2.1. Abstract 2.2. Introduction 2.3. Materials and Methods 2.3.1. Study site 2.3.2. Permafrost drilling and sample preparation 2.3.3. Sediment properties 2.3.4. Potential methane production rates 2.3.5. Lipid biomarker analysis 2.3.6. Detection of archaeol and isoprenoid GDGTs 2.3.7. Detection of PLFAs and PLELs 2.3.8. DNA extraction and polymerase chain reaction (PCR) amplification 2.3.9. Phylogenetic analysis 2.4. Results and Discussion 2.4.1. Methane profile of the Kurungnakh permafrost sequence 2.4.2. Signals of living microbial communities in the Kurungnakh permafrost sequence 2.4.3. Reconstruction of past microbial communities in the Kurungnakh permafrost sequence 2.4.4. Climate impact on the distribution of microbial communities in the Kurungnakh permafrost sequence 2.4.5. Climatic impact on the composition of methanogenic communities in the Kurungnakh permafrost sequence 2.5. Conclusion 2.6. Acknowledgement 3. Response of microbial communities to landscape and climatic changes in a terrestrial permafrost sequence of the El’gygytgyn crater, Far East Russian Arctic 3.1. Abstract 3.2. Introduction 3.3. Materials and Methods 3.3.1.Study site 3.3.2. Drilling and sample material 3.3.3. Sediment properties 3.3.4. Lipid biomarker analysis 3.3.5. Detection of glycerol dialkyl glycerol tetraethers (GDGTs) and archaeol 3.3.6. Detection of phospholipid fatty acids (PLFA) 3.3.7. Deoxyribonucleic acid (DNA) extraction and amplification 3.3.8. Quantitative PCR analysis of archaeal and bacterial small sub unit (SSU) rRNA genes 3.3.9. Phylogenetic analysis 3.4. Results 3.4.1. TOC-contents 3.4.2. Distribution of glycerol dialkyl glycerol tetraethers (GDGTs) and archaeol 3.4.3. Distribution of phospholipid fatty acids (PLFA) 3.4.4. Composition of archaeol and isoprenoid GDGTs 3.4.5. Quantification of bacterial and archaeal genes 3.4.6. Analysis of methanogenic community fingerprints 3.5. Discussion 3.5.1. Microbial communities in subaquatic deposits 3.5.2. Microbial communities in subaerial deposits 3.5.3. Microbial succession in the Holocene sequence of Lake El’gygytgyn permafrost 3.6.Conclusion 3.7. Acknowledgements 4. Glacial-interglacial microbial community dynamics in Middle Pleistocene sediments in the Lake El’gygytgyn, Far East Russian Arctic 4.1. Abstract 4.2. Introduction 4.3. Materials and Methods 4.3.1. Study site 4.3.2. Drilling and sample preparation 4.3.3. Sediment properties 4.3.4. Lipid biomarker analyses 4.3.5. Deoxyribonucleic acid (DNA) extraction and quantitative polymerase chain reaction (qPCR) 4.3.6. PCR amplification of methanogenic SSU rRNA genes 4.4. Results 4.4.1. Sedimentary TOC and biogenic silica concentration 4.4.2. Quantification of bacterial and archaeal genes 4.4.3. Quantification and composition of lipid biomarkers 4.4.4. Potential methane production 4.4.5. Methanogenic community composition 4.5. Discussion 4.6. Acknowledgements 5. Synthesis 5.1. The reaction of microbial communities to past climatic change in the Arctic 5.2.The response of microbial communities to carbon composition and availability 5.3. Implications from this study for future research 6. Data collection 6.1. Manuscript I: Response of methanogenic archaea to Late Pleistocene and Holocene climate changes in the Siberian Arctic 6.1.1. Sediment properties 6.1.2. Isoprenoid glycerol dialkyl glycerol tetraethers and archaeol 6.1.3. Branched glycerol dialkyl glycerol tetraethers 6.1.4. Phospholipid ester and ether lipids (summary) 6.2. Manuscript II: Response of microbial communities to landscape and climatic changes in a terrestrial permafrost sequence of the El’gygytgyn crater, Far East Russian Arctic 6.2.1. Sediment properties and gene quantifications 6.2.2. Phospholipid fatty acids composition 6.2.3. Isoprenoid glycerol dialkyl glycerol tetraethers and archaeol 6.2.4. Branched glycerol dialkyl glycerol tetraethers 6.3. Manuscript III: Glacial-interglacial microbial community dynamics in Middle Pleistocene sediments in the Lake El’gygytgyn, Far East Russian Arctic 6.3.1. Sediment properties and gene quantifications 6.3.2. Isoprenoid glycerol dialkyl glycerol tetraethers and archaeol 6.3.3. Branched glycerol dialkylglycerol tetraethers 7. References 8. Final thoughts and acknowledgements 9. Curriculum vitae 10.Erklärung
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  • 33
    Call number: AWI Bio-20-93993
    Type of Medium: Dissertations
    Pages: III, 127 Seiten , Illustrationen
    Language: English
    Note: Dissertation, Universität Potsdam, 2014 , Table of contents I - Abstract II - Zusammenfassung Chapter 1 - Introduction 1.1. Introduction 1.1.1 Motivation 1.1.2 Organisation of thesis 1.1 Scientific background 1.2.1 Arctic and wetland bryophytes 1.2.2 Bryophyte remains as palaeo-environmental indicators 1.2.3 Regional setting 1.3 Objectives ofthe thesis 1.4 Overview of the manuscripts 1.5 Contribution of the authors Chapter 2 - Manuscript #1 Abstract 2.1 Introduction 2.2 Geographic setting 2.3 Materials and methods 2.3.1 Fieldwork 2.3.2 Radiocarbon dating 2.3.3 Geochemical, stable carbon isotope, and granulometric analyses 2.3.4 Analyses of moss remains and vascular plant macrofossils 2.3.5 Pollen analysis 2.3.6 Diatom analysis 2.3.7 Statistical analysis 2.4 Results 2.4.1 High-resolution spatial characteristics oft the investigated polygon and vegetation pattern 2.4.2 Geochronology and age-depth relationships 2.4.3 General properties of the sedimentary fill 2.4.4 Bioindicators 2.4.5 Characterization oftwo different types of polygon pond sediment 2.5. Discussion 2.5.1 Small-scale spatial structure of polygons 2.5.2 Age-depth relationships 2.5.3 Proxy value of the analysed parameters 2.5.4 The general polygon development 2.5.5 Polygon development as a function of external controls and internal adjustment mechanisms 2.6 Conclusions Chapter 3 - Manuscript #11 Abstract 3.1 Introduction 3.2 Material und methods 3.2.1 Regional setting 3.2.3 Field methods and environmental data collection 3.2.4 Data analysis 3.3 Results 3.3.1 Major characteristics of the investigated polygons 3.3.2 Vegetation cover and its relationships with micro-relief and vegetation type 3.3.3 Vegetation alpha-diversity and its relationship with micro-relief and vegetation type 3.3.4 Vegetation composition and its relationship with micro-relief and vegetation type 3.4 Discussion 3.4.1 Patterns of cover, alpha-diversity and compositional turnover of vascular plants and bryophytes along the rim-pond transect (local-scale) 3.4.2 Patterns of cover, alpha-diversity and compositional turnover of vascular plants and bryophytes along the regional-scale forest-tundra transect 3.4.3 Indicator potential ofvascular plant and bryophyte remains from polygonal peats for the reconstruction of local hydrological and regional vegetation changes 3.4.4. Implications of the performed vegetation transect studies for future Arctic warming 3.5 Acknowledgements 2.4.4 Bioindicators 2.4.5 Characterization of two different types of polygon pond sediment 2.5. Discussion 2.5.1 Small-scale spatial structure of polygons 2.5.2 Age-depth relationships 2.5.3 Proxy value of the analysed parameters 2.5.4 The general polygon development 2.5.5 Polygon development as a function of external controls and internal adjustment mechanisms 2.6 Conclusions Chapter 3 - Manuscript #II Abstract 3.1 Introduction 3.2 Material und methods 3.2.1 Regional setting 3.2.3 Field methods and environmental data collection 3.2.4 Data analysis 3.3 Results 3.3.1 Major characteristics of the investigated polygons 3.3.2 Vegetation cover and its relationships with micro-relief and vegetation type 3.3.3 Vegetation alpha-diversity and its relationship with micro-relief and vegetation type 3.3.4 Vegetation composition and its relationship with micro-relief and vegetation type 3.4 Discussion 3.4.1 Patterns of cover, alpha-diversity and compositional turnover of vascular plants and bryophytes along the rim-pond transect (local-scale) 3.4.2 Patterns of cover, alpha-diversity and compositional turnover of vascular plants and bryophytes along the regional-scale forest-tundra transect 3.4.3 Indicator potential of vascular plant and bryophyte remains from polygonal peats for the reconstruction of local hydrological and regional vegetation changes 3.4.4. Implications of the performed vegetation transect studies for future Arctic warming 3.5 Acknowledgements Chapter 4 - Manuscript #3 Abstract 4.1 Introduction 4.2 Material and methods 4.2.1 Sites 4.2.2 Sampling 4.2.3 Investigated moss species 4.2.4 Measurements 4.2.5 Statistical Tests 4.3 Results 4.4 Discussion Chapter 5 - Discussion 5.1 Bryophytes of polygonal landscapes in Siberia 5.1.1 Modern bryophytes in the Siberian Arctic 5.1.2 Biochemical and isotopic characteristics of mosses 5.1.3 Reliability and potential of fossil bryophyte remains as palaeoproxies 5.2 Dynamics of low-centred polygons during the late Holocene 5.3 Outlook Appendix I - Preliminary Report Motivation Material and methods Results and first interpretation Appendix II Additional tables and figures of manuscript #1 Appendix III Additional figures of manuscript #2 Appendix IV - Quantitative approach of Standard Moss Stem (SMS3) Bibliography Acknowledgements Eidesstattliche Erklärung
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  • 34
    Call number: ZSP-201-80/10
    In: CRREL Report, 80-10
    Description / Table of Contents: A mathematical model of coupled heat and moisture flow in soils has been developed. The model includes algorithms for phase change of soil moisture and frost heave and permits several types of boundary and initial conditions. The finite element method of weighted residual (Galerkin procedure) was chosen to simulate the spatial regime and the Crank-Nicholson method was used for the time domain portion of the model. To facilitate evaluation of the model, the heat and moisture fluxes were essentially decoupled; moisture flux was then simulated accurately, as were heat flux and frost heave in a laboratory test. Comparison of the simulated and experimental data illustrates the importance of unsaturated hydraulic conductivity. It is one parameter which is difficult to measure and for which only a few laboratory test results are available. Therefore, unsaturated hydraulic conductivities calculated in the computer model may be a significant source of error in calculations of frost heave. The algorithm incorporating effects of surcharge and overburden was inconclusively evaluated. Time-dependent frost penetration and frost heave in laboratory specimens were closely simulated with the model. After 10 days of simulation, the computed frost heave was about 2.3 cm vs 2.0 cm and 2.8 cm in two tests. Frost penetration was computed as 15 cm and was measured at 12.0 cm and 12.2 cm in the two laboratory samples after 10 days.
    Type of Medium: Series available for loan
    Pages: v, 49 Seiten , Illustrationen
    Series Statement: CRREL Report 80-10
    Language: English
    Note: CONTENTS Abstract Preface Introduction One-dimensional equations of simultaneous heat and moisture flux Moisture transport Heat transport Phase change Coupling effects Frost heave algorithm Development of computer model Finite difference vs finite element method Finite element formulation Time domain solution Evaluation of the mathematical model Heat flux Moisture flux Numerical dispersion Frost heave of homogeneous laboratory samples Conclusions Recommended studies to refine the model Literature cited Appendix A. Work plan, staffing and instrumentation requirements for correlating results oflaboratory frost susceptibility tests with field performance Appendix B. Proposed investigation of thaw weakening of subgrade soil and granular unboundbase course Appendix C. Derivation of finite element system matrices
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  • 35
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-80/9
    In: CRREL Report, 80-9
    Description / Table of Contents: Explosive cratering tests were conducted in seasonally frozen and thawed gravel at Ft. Richardson near Anchorage, Alaska, and in seasonallly frozen and thawed silt overlying permafrost and in silt permafrost at Ft. Wainwright near Fairbanks, Alaska. Explosive charge weights ranged from 26 to 3120 lb and charge burial depths ranged from about 3 to 40 ft. The cube root of the charge weight scaling was used to determine maximum scaled crater dimensions and optimum scaled depth of burial of the charge. Test results for frozen and thawed gravel were essentially the same because of the low moisture content and the relatively shallow depth of freezing (5 to 6 ft). The optimum depth of burial of the charge for maximizing the apparent radius and depth and the true radius was about 1.8 times the cube root of the charge weight for both the frozen and thawed conditions. In seasonally frozen silt overlying a talik and silt permafrost the maximum scaled crater dimensions and optimum scaled burial depths of the charge were smaller than for the thawed condition except for the true crater dimensions. The channeling of energy in the talik produces maximum crater dimensions and an optimum burial depth for the true crater that is larger than for the thawed condition. The results for the homogeneous silt permafrost were very similar to the frozen gravel results with much smaller maximum crater dimensions and smaller optimum charge burial depths than for the thawed silt overlying permafrost.
    Type of Medium: Series available for loan
    Pages: v, 21 Seiten , Illustrationen
    Series Statement: CRREL Report 80-9
    Language: English
    Note: CONTENTS Abstract Preface Metric conversion table Introduction Test sites Test procedures and materials Analysis of test data Mobility tests Conclusions Literature cited
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  • 36
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-80/8
    In: CRREL Report, 80-8
    Description / Table of Contents: This report presents the results of the tests on the new U.S. Coast Guard 140-ft icebreaker Katmai Bay (WTGB-101) in the level plate ice and brash ice in Whitefish Bay and the St. Marys River. The results indicate that the vessel can penetrate 22 in. of level freshwater ice with 2-3 in. of snow cover. It can also penetrate up to 48 in. of brash ice in a continuous mode and at least 30 in. of plate ice by backing and ramming. The installed bubbler system decreased the required power of the vessel from 10 to 30% in brash ice and 25 to 35% in level ice. The low friction coating appears to be effective in decreasing the friction factor when it remains intact; when it peels off it appears to make conditions worse than plain paint. An average dynamic friction factor of 0.15 could be used over the entire hull for these tests.
    Type of Medium: Series available for loan
    Pages: iv, 28 Seiten , Illustrationen
    Series Statement: CRREL Report 80-8
    Language: English
    Note: CONTENTS Abstract Preface Metric conversion table Introduction Roughness and friction measurements Level plate ice performance Brash ice performance Ramming icebreaking performance Analysis of the data Propulsion efficiency in ice Regression analysis Conclusions and recommendations Literature cited
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  • 37
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    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-80/24
    In: CRREL Report, 80-24
    Description / Table of Contents: The fluid shear stress applied to the underside of a simulated floating ice cover was measured in a laboratory flume. The measured values were compared with values of the shear stress computed from the von Karman-Prandtl velocity distribution fitted to the velocity profiles measured beneath the cover. For the lower velocity runs (approx 0.079 m/s) the measured and computed values of the shear stress were in close agreement. At the high velocity flows (approx 0.137 m/s) the measured values were roughly one-half those calculated from the velocity distribution. As the underside of the cover became increasingly rougher, the position of maximum velocity moved closer to the bottom of the channel. It was shown that the Darcy friction coefficient is exponentially related to a normalized ice cover thickness, which suggests that it is measure of the roughness of a fragmented ice cover.
    Type of Medium: Series available for loan
    Pages: iv, 11 Seiten , Illustrationen
    Series Statement: CRREL Report 80-24
    Language: English
    Note: CONTENTS Abstract Preface List of symbols Introduction Experimental apparatus Experimental procedures Analysis of forces Experimental results Analysis of data Conclusions Literature cited
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  • 38
    Monograph available for loan
    Monograph available for loan
    Amsterdam : Elsevier
    Call number: AWI G2-21-94484
    Description / Table of Contents: Although it is generally accepted that the Arctic Ocean is a very sensitive and important region for changes in the global climate, this region is the last major physiographic province of the earth whose short-and long-term geological history is much less known in comparison to other ocean regions. This lack of knowledge is mainly caused by the major technological/logistic problems in reaching this harsh, ice-covered region with normal research vessels and in retrieving long and undisturbed sediment cores. During the the last about 20 years, however, several international and multidisciplinary ship expeditions, including the first scientific drilling on Lomonosov Ridge in 2004, a break-through in Arctic research, were carried out into the central Artic and its surrounding shelf seas. Results from these expeditions have greatly advanced our knowledge on Arctic Ocean paleoenvironments. Published syntheses about the knowledge on Arctic Ocean geology, on the other hand, are based on data available prior to 1990. A comprehensive compilation of data on Arctic Ocean paleoenvironment and its short-and long-term variability based on the huge amount of new data including the ACEX drilling data, has not been available yet. With this book, presenting (1) detailed information on glacio-marine sedimentary processes and geological proxies used for paleoenvironmental reconstructions, and (2) detailed geological data on modern environments, Quaternary variability on different time scales as well as the long-term climate history during Mesozoic-Tertiary times, this gap in knowledge will be filled.
    Type of Medium: Monograph available for loan
    Pages: XIV, 592 Seiten , Illustrationen
    Edition: First edition
    ISBN: 9780444520180
    Series Statement: Developments in marine geology 2
    Language: English
    Note: Contents Preface Acknowledgements List of Abbreviations Part 1: Introduction and Background Chapter 1. Introduction to the Arctic: Significance and History 1.1 The Arctic Ocean and Its Significance for the Earth's Climate System 1.2 History of Arctic Ocean Research 1.3 Plate Tectonic Evolution and Palaeogeography 1.4 Glaciations in Earth's History Chapter 2. Modern Physiography, Hydrology, Climate, and Sediment Input 2.1 Bathymetry and Physiography 2.2 Oceanic Circulation Pattern and Water-Mass Characteristics 2.3 Sea-Ice Cover: Extent, Thickness, and Variability 2.4 Primary Production and Vertical Carbon Fluxes in the Arctic Ocean 2.5 River Discharge 2.6 Permafrost 2.7 Coastal Erosion 2.8 Aeolian Input 2.9 Modern Sediment Input: A Summary Part 2: Processes and Proxies Chapter 3. Glacio-Marine Sedimentary Processes 3.1 Sea-Ice Processes: Sediment Entrainment and Transport 3.2 Ice Sheet- and Iceberg-Related Processes 3.3 Sediment Mass-Wasting Processes 3.4 Turbidite Sedimentation in the Central Arctic Ocean Chapter 4. Proxies Used for Palaeoenvironmental Reconstructions in the Arctic Ocean 4.1 Lithofacies Concept 4.2 Grain-Size Distribution 4.3 Proxies for Sources and Transport Processes of Terrigenous Sediments 4.4 Trace Elements Used for Palaeoenvironmental Reconstruction 4.5 Micropalaeontological Proxies and Their (Palaeo-) Environmental and Stratigraphical Significance 4.6 Stable Isotopes of Foraminifers 4.7 Organic-Geochemical Proxies for Organic-Carbon Source and Palaeoenvironment Part 3: The Marine-Geological Record 5 Modern Environment and its record in surface sediments 5.1 Terrigenous (non-biogenic) components in Arctic Ocean surface sediments: Implications for provenance and modern transport processes 5.2 Organic-Carbon Content: Terrigenous Supply versus Primary Production Chapter 6. Quaternary Variability of Palaeoenvironment and Its Sedimentary Record 6.1 The Stratigraphic Framework of Arctic Ocean Sediment Cores: Background, Problems, and Perspectives 6.2 Variability of Quaternary Ice Sheets and Palaeoceanographic Characteristics: Terrestrial, Model, and Eurasian Continental Margin Records 6.3 Circum-Arctic Glacial History, Sea-Ice Cover, and Surface-Water Characteristics: Quaternary Records from the Central Arctic Ocean 6.4 Accumulation of Particulate Organic Carbon at the Arctic Continental Margin and Deep-Sea Areas During Late Quaternary Times Chapter 7. Mesozoic to Cenozoic Palaeoenvironmental Records of High Northern Latitudes 7.1 Mesozoic High-Latitude Palaeoclimate and Arctic Ocean Palaeoenvironment 7.2 Cenozoic High-Latitude Palaeoclimate and Arctic Ocean Palaeoenvironment Chapter 8. Open Questions and Future Geoscientific Arctic Ocean Research 8.1 Quaternary and Neogene Climate Variability on Sub-Millennial to Milankovich Time Scales 8.2 The Mesozoic-Cenozoic History of the Arctic Ocean References Index
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  • 39
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-81/16
    In: CRREL Report, 81-16
    Description / Table of Contents: An air-transportable shelter designed and built at CRREL for use in cold regions underwent testing in Hanover, New Hampshire, and Ft. Greely, Alaska. The shelter demonstrated some of its capabilities for mobility by being towed for more than 60 miles behind various vehicles and by being transported on a C-130 cargo airplane, a CH-47 helicopter, and a trailer truck. The shelter proved to be very easy for a crew of two to four to set up in all weather conditions including -40 F cold. However, the gasoline-powered generator, which was a source for space heat as well as electricity, functioned very poorly. Overall, the prototype successfully demonstrated qualities of self-reliance, ease of operation and thermal efficiency.
    Type of Medium: Series available for loan
    Pages: v, 20 Seiten , Illustrationen
    Series Statement: CRREL Report 81-16
    Language: English
    Note: CONTENTS Abstract Preface Metric conversion factors Summary Introduction Description of shelter Test procedures and results Mobility Ease of erecting and striking Therinal efficiency and performance Heat output Electrical system Habitation Safety features Water system Shelter reliability Structure Performance of other shelters Conclusions Future studies Literature cited
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  • 40
    Call number: ZSP-201-81/15
    In: CRREL Report, 81-15
    Description / Table of Contents: This report analyzes the results of a field study previously reported by Scrivner et al. (1969) for the National Cooperative Highway Research Program. These authors studied the seasonal pavement deflection characteristics of 24 test sites on roads in service in regions with freezing indexes ranging from 100 F-days to 2100 F-days. They used the Dynaflect cyclic pavement loading device to determine the pavement system response. Of specific interest to my analysis was the increased pavement deflection after freezing and thawing and the time to recovery of normal deflection characteristics. These characteristics were related to soil and climatic factors using statistical techniques. The most significant observations of this statistical analysis are: (1) that the freezing index is not a significant parameter in determining the percent increase in pavement deflection during thawing, and (2) that the recovery time is inversely proportional to the depth of freezing. As was expected, the most significant variable affecting the increase in pavement deflection was the frost susceptibility classification. This observation reinforces the necessity for careful selection of soil materials used in pavement systems.
    Type of Medium: Series available for loan
    Pages: v, 10 Seiten , Ilustrationen
    Series Statement: CRREL Report 81-15
    Language: English
    Note: CONTENTS Abstract Preface Nomenclature Introduction Description of test site Test results Method of analysis Results of analysis Change in resilient deflection due to thawing, A Recovery time after onset of thawing, t20 Discussion of results Change in resilient deflection due to thawing, A. Recovery time after thawing, t20 Conclusions Literature cited ILLUSTRATIONS Figure Pavement deflection and frost penetration vs time Data points and regression line for A and t2 0 versus F Data points and regression line for A and t2 0 versus W Data points and regression line for A and t2 0 versus I Data points and regression line for A and t20 versus N Data points and regression line for A and t20 versus D Data points and regression line for t20 versus A Permeability vs void ratio for the Toledo Penn 7 material TABLES Properties of test sections Test results from Scrivner et al Results of regression analysis
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  • 41
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-81/11
    In: CRREL Report, 81-11
    Description / Table of Contents: Abstract: Relative displacement data from high explosive, shallow-buried bursts in rock are combined with relative displacement data from the contained nuclear explosion MIGHTY EPIC. Analysis of these data yields a preliminary, semi-empirical technique for predicting the location, direction and magnitude of relative displacements in rock from contained explosions. This technique is used to make relative displacement predictions for the DIABLO HAWK nuclear blast.
    Type of Medium: Series available for loan
    Pages: iv, 23 Seiten , Illustrationen
    Series Statement: CRREL Report 81-11
    Language: English
    Note: CONTENTS Abstract Preface Introduction DIHEST analysis MIGHTY EPIC analysis Geological setting and relative displacement documentation Shear stress analysis 8 Displacement analysis DIABLO HAWK predictions Literature cited
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  • 42
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    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-81/9
    In: CRREL Report, 81-9
    Description / Table of Contents: Abstract: The calculation of the largest horizontal force a relatively thin floating ice plate may exert on a structure requires the knowledge of the buckling load for this floating plate. In the published literature on the stability of continuously supported beams and plates, it is usually assumed that this buckling force corresponds to the lowest bifurcation force Pcr. However, recent studies indicate that, generally, this is not the case, and this report clarifies the situation for floating ice plates. This problem is first studied on a simple model that exhibits the buckling mechanism of a floating ice plate but is amenable to an exact nonlinear analysis. This study shows that, depending on the ratio of the rigidities of the "liquid" and "plate," the post-buckling branch may rise or drop away from the bifurcation point. Thus, Pcr may or may not be the actual buckling load. It is also shown that when lift-off of "plate" from the "liquid" takes place the actual buckling load may drop substantially. This study is followed by an analysis of a floating compressed semi-infinite plate with a straight free edge, assuming that there is no lift-off. It is found that for this case there always exists a buckling load that is lower than Pcr. According to the obtained results, the value Pcr should be used with caution as a buckling load for floating ice plates. It is suggested that the buckling load be determined using the postbuckling equilibrium branch of the plate, taking into consideration the possibility of lift-off of the ice cover from the liquid base.
    Type of Medium: Series available for loan
    Pages: 7 Seiten , Illustrationen
    Series Statement: CRREL Report 81-9
    Language: English
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  • 43
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    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-81/20
    In: CRREL Report, 81-20
    Description / Table of Contents: A historical review of research is presented to establish the state- of-the-art for analyzing the behavior of vehicles in shallow snow. From this review, the most comprehensive and promising model is put together to establish a first-cut performance prediction model for vehicles operating in shallow snow, slush, ice and thawing soils.
    Type of Medium: Series available for loan
    Pages: iv, 21 Seiten , Illustrationen
    Series Statement: CRREL Report 81-20
    Language: English
    Note: CONTENTS Abstract Preface List of symbols Introduction Historical review Model selection Traction Resistance Slush and thawing soils Ice, hard-packed snow, packed snow River and lake ice Model use Conclusions Literature cited
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  • 44
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-81/21
    In: CRREL Report, 81-21
    Description / Table of Contents: The reflection of solar radiation by a snow cover in situ and the apparent influence of selected substrates were examined in wavelength bands centered at 0.81, 1.04, 1.10, 1.30, 1.50 and 1.80 micrometers. Substrates included winter wheat, timothy, corn, alfalfa, grass, concrete and subsurface layers of 'crusty' snow and ice. Reasonable qualitative agreement between measurements and theoretical predictions was demonstrated, with indications of quantitative agreement in the definition of a 'semi-infinite depth' of snow cover. It was concluded that ultimate quantitative agreement between theory and measurement will require that an 'optically effective grain size' be defined in terms of physically measuarable dimensions or meteorologically predictable characteristics of the ice crystals composing the snowpack.
    Type of Medium: Series available for loan
    Pages: iii, 17 Seiten , Illustrationen
    Series Statement: CRREL Report 81-21
    Language: English
    Note: CONTENTS Abstract Preface Introduction Experimental method Substrate preparation Experimental configuration Radiometric measurements Snow characterization Reflectance standards Data analysis Reflectance measurements Snow replica analysis Discussion of results Comparative reflectance of various substrates under snow Ablation of a snow cover Reflectance from a very light, fresh snow cover Measurements at angles other than vertical Reflectance from substrates Concluding observations Literature cited
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  • 45
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-81/25
    In: CRREL Report, 81-25
    Description / Table of Contents: The problem of heat conduction with phase changeAoften called the Stefan problemrincludes some of the mostintractable mathematical areas of heat transfer. Exact solutions are extremely limited and approximate methodsare widely used. This report discusses the collocation method for the heat balj ce integral approximation. The methodis applied to some standard problems of phase change-Neumann's problem-and a new solution is presented for thecase of surface convection for a semi-infinite body. Numerical results are given for soil systems and also for materialsof interest in latent heat thermal storage.
    Type of Medium: Series available for loan
    Pages: v, 14 Seiten , Illustrationen
    Series Statement: CRREL Report 81-25
    Language: English
    Note: CONTENTS Abstract Preface Nomenclature Conversion factors Introduction Collocation method Neumann problem Specified surface heat flux Convective surface heat flux Insulated semi-infinite body Conclusion Literature cited Appendix A: Program listing for numerical quadrature of equation 28
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  • 46
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-82/3
    In: CRREL Report, 82-3
    Description / Table of Contents: The conditions that lead to initial breakup of a solid ice on a river due to rapid water level variations are analyzed. The analysis is based on the theory of beams on an elastic foundation. First cracking is assumed to occur when the bending moment induced in the ice cover by the wave exceeds the flexural strength of the ice cover.
    Type of Medium: Series available for loan
    Pages: iv, 17 Seiten , Illustrationen
    Series Statement: CRREL Report 82-3
    Language: English
    Note: CONTENTS Abstract Preface Symbols Introduction Purpose of the study Stating the problem Fracturing of the ice cover due to the passage of surge waves Basic assumptions Derivation of the bending moments Determination of the wave characteristics Deflection of the ice Discussion and field observations Summary Literature cited
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  • 47
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-82/5
    In: CRREL Report, 82-5
    Description / Table of Contents: The problem of simultaneous heat and mass transfer in a homogeneous snow layer, with one side kept at its initial temperature and the other side with a step temperature increase, was solved for the case of constant through-flow conditions. An experimentally determined effective thermal conductivity function, i.e. Ke = 0.0014 + 0.58 G (where G is dry mass flow rate of air in g/sq cm-s), was employed in the solution. The computed nondimensional temperature distribution agreed quite well with experimental data taken under pseudo-steady state conditions with the exception of the temperature for the lowest flow rate used in the experiment. The pronounced nonlinearity of the temperature distribution was found to be a strong function of the flow rate. For sinusoidal variation of atmospheric pressure, the responding flow in the snow medium was also found to be sinusoidal. In conjunction with the diurnal temperature change, this variation facilitated the process of repeated sublimation and condensation in alternate directions and thereby produced a surface layer of approximately constant snow density.
    Type of Medium: Series available for loan
    Pages: v, 10 Seiten , Illustrationen
    Series Statement: CRREL Report 82-5
    Language: English
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  • 48
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-82/4
    In: CRREL Report, 82-4
    Description / Table of Contents: Several proposed methods for treating the momentum flux between drifting sea ice and the underlying ocean are interpreted in terms of simple planetary-boundary-layer (PBL) turbulence theory. The classical two-layer approach, in which the solution for a thin surface layer is matched to an Ekman solution for the outer layer, is used to derive several forms of the drag law. These forms range from linear (where stress is proportional to relative speed), through quadratic (where stress is proportional to relative speed squared), to a Rossby-similarity law like that used to express frictional drag on geostrophic wind in the atmosphere. Only formulations which conform with Rossby-similarity scaling are consistent with free-drift data from the 1975 AIDJEX drift station experiment.
    Type of Medium: Series available for loan
    Pages: iv, 17 Seiten , Illustrationen
    Series Statement: CRREL Report 82-4
    Language: English
    Note: CONTENTS Abstract Preface Background Hierarchy of drag laws and simple models The momentum equation for the planetary boundary layer Linear eddy viscosity - the constant stress layer Two-layer eddy viscosity PBL scaling A dimensionless two-layer system A dimensionless two-layer system with modified stress Evaluating the drag laws Rossby similarity parameters and buoyancy effects Discussion Literature cited
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  • 49
    Call number: 9781629487991 (e-book)
    Description / Table of Contents: This book described the current status and possible future changes of the thermokarst (thaw) lakes of western Siberia as dominant forms of landscape and regulators of greenhouse gas exchange within the atmosphere. Thawing permafrost and resulting microbial decomposition of previously frozen organic carbon is one of the most significant terrestrial ecosystem positive feedbacks to a warming climate. Ongoing processes of the permafrost thawing in Western Siberia are likely to increase the surface of water bodies via forming so-called thermokarst lakes, mobilizing the organic carbon (OC) from the soil pool to the rivers and, finally, to the ocean, and thus modifying the fluxes of methane (CH4) and CO2 to the atmosphere. Despite their tremendous importance for green house gazes regulation and hydrological regime control, very little is known about hydrochemistry of western Siberia thaw lakes. This book assesses the variation of major and trace elements (TE) and organic carbon (OC) concentration along the chronosequence of lake development and the latitude profile of variable permafrost abundance; characterizes the colloidal status of TE and distinguishes between the relative proportion of organic and organo-mineral colloids; describes the particularity of microbiological composition of thermokarst lake waters and production/mineralization processes in the water column; and presents the perspective of water chemical composition evolution under the climate change scenario. Each of these aforementioned objectives present a scientific challenge given mainly the paucity of existing information on these important but still very poorly studied ecosystems. Taken together, understanding of these issues and identification and quantification of controlling environmental parameters should produce conceptually new knowledge of biogeochemical processes operating within the Western Siberia Plain with the possibility of extrapolation of generated knowledge to much larger territories of arctic and subarctic permafrost-affected areas. (Imprint: Nova)
    Type of Medium: 12
    Pages: 1 Online-Ressource (179 Seiten) , Illustrationen
    ISBN: 9781629487991 (e-book)
    Series Statement: Biochemistry research trends
    Language: English
    Note: Table of Contents Introduction: Thermokarst Lakes of Western Siberia as Dominant Forms of Landscape and Regulators of Greenhouse Gas Exchange with the Atmosphere Chapter 1. Thermokarst Lakes: Distribution, Cycle of Development, Surface Coverage and Evolution Chapter 2. Sources of Dissolved Components in Thermokarst Lakes Chapter 3. Temperature and Gas Regime Chapter 4. Dissolved Organic Carbon Chapter 5. Microbiology of Thermokarst Lake Systems Chapter 6. Trace Elements in Thermokarst Lakes Chapter 7. Colloids in Thermokarst Lakes Chapter 8. Latitude Profile Gradients of Lakes: Substituting Space for Time Chapter 9. Possible Impact of Climate Warming on Stocks and Fluxes of Carbon and Related Elements in Western Siberian Lakes Conclusions: Thaw Lakes as Indicators of Climate Change References Index
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  • 50
    Monograph available for loan
    Monograph available for loan
    Viévy : Éditions de l'Escargot Savant
    Call number: AWI A4-22-94545
    Description / Table of Contents: Sea ice covers 20 million km² of our planet’s surface. It plays an important role in the Earth’s climate and is home to a variety of fascinating fauna, from the polar bear to the emperor penguin. Sailors and meteorologists use a wide range of terms such as frazil, pancake ice, floe or hummock to describe the different features of sea ice. This book includes an illustrated guide to sea ice so that polar travellers can discover this environment and understand ice charts. The story of sea ice is also a story of human endeavour. For the Inuit, fast ice is an ideal terrain for hunting, fishing and travelling. But for European explorers the drifting ice was an insurmountable barrier for centuries, crushing ships and forcing crews to spend long and difficult winters on the ice. It has also been the scene of incredible adventures involving planes, submarines, icebreakers and sometimes even rafts of drifting ice. But our planet is warming and the oldest polar sea ice is disappearing. The declining sea ice encourages the economic and industrial development of the Arctic, but also disrupts the climate, societies and fauna of the Far North. The author is a meteorologist who has wintered in Antarctica, lived in Greenland and guides several polar expedition cruises each year.
    Type of Medium: Monograph available for loan
    Pages: 112 Seiten , Illustrationen , 15 x 21 cm
    ISBN: 978-2-918299-26-4
    Series Statement: Maxi-Guides Collection : Polar Regions
    Language: English
    Note: Contents ILLUSTRATED GUIDE TO SEA ICE Presentation Ice development Fast ice Occurrence and concentration of floating ice Forms of floating ice Distribution of ice Openings in the ice Ice surface features Melt stages Break-up Charting sea ice Egg code SEA ICE Extent and area Thickness and salinity Currents Climatic role Life in the ice FAUNA The Arctic Antarctica MAN AND THE SEA ICE The Inuit Explorers from the 15th to the 19th century Shipwrecked on a raft of ice The Fram and the drifting ice stations Polar aircraft Polar submarines Icebreakers Tourism Sports , Übersetzung aus dem Französischen
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  • 51
    Call number: AWI G3-22-94801
    Type of Medium: Monograph available for loan
    Pages: 95 Seiten , Illustrationen
    ISBN: 978-5-89658-049-2
    Language: English
    Note: Contents INTRODUCTION / P.V.Krasilnikov PART I GENERAL CHARACTERIZATION OF ENVIRONMENTAL CONDITIONS Geological settings / D.E.Konyushkov, R.V.Desyatkin Climate and soil temperature dynamics / D.E.Konyushkov, R.V.Desyatkin, A.R.Desyatkin Geocryological conditions / D.E.Konyushkov, A.N.Fedorov Vegetation / D.E.Konyushkov, R.V.Desyatkin SOILS AND SOIL COVER PATTERNS – GENERAL SCOPE / D.E.Konyushkov, R.V.Desyatkin, S.F.Khokhlov ALAS PHENOMEN: SPECIFIC FEATURES, GENESIS AND DYNAMICS / R.V.Desyatkin, A.R.Desyatkin AGRICULTURE AND OTHER ANTHROPOGENIC ACTIVITY IN CENTRAL YAKUTIA / R.V.Desyatkin, M.V.Okoneshnikova PART II SOILS OF CENTRAL SAKHA (YAKUTIA) / S.V.Goryachkin, R.V.Desyatkin, E.M.Lapteva, M.N.Lebedeva, N.S.Mergelov, P.V.Krasilnikov, V.A.Shishkov, I.V.Turova E.P.Zazovskaya METHODS OF STUDY DAY 1 Vilyui road. Cambic Turbic Cryosol. Profile 11 Vilyui road. Turbic Cryosol Reductaquic. Profile 12 Sand hills near Tabaga. Haplic Stagnosol Arenic Turbic. Profile 15 DAY 2 Abalakh alas vicinities. Haplic Cryosol Albic Luvic Sodic. Profile 14 Abalakh alas. Salic Fluvisol. Profile 13-1 Abalakh alas. Stagnic Solonetz Turbic. Profile 13-2 DAY 3 Desyatkin Alas. Cryic Limnic Histosol. Profile 9-1 Desyatkin Alas. Thapto-Histic Limnic Fluvisol. Profile 9-2 Desyatkin Alas. Endogleyic Stagnosols Albic Arenic Turbic. Profile 9-3 Observation point. Khonorosh alas. Bulgunyakh (pingo) 4 DAY 4 Tabaga post-agrogenic soil. Stagnic Cambisol Calcaric. Profile 2-1 Tabaga post-agrogenic soil. Luvic Phaeozem Albic Turbic. Profile 2-2 Tabaga post-agrogenic soil. Calcic Mollic Solonetz Albic. Profile 2-3 Observation point. Badland on icy permafrost Lena terrace. Stagnic Chernozem Molliglossic Turbic. Profile 5 Lena terrace. Mollic Endogleyic Solonetz Turbic. Profile 6 Lena terrace. Hyposalic Solonetz. Profile 7 SOME GENERAL CHARACTERISTICS OF SOILS Cryogenic microfeatures Soluble salts in investigated soils DAY 5. Lena pillars CONCLUSION / (S.V.Goryachkin) ACKNOWLEDGEMENTS REFERENCES
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  • 52
    Monograph available for loan
    Monograph available for loan
    Novosibirsk : Akademičeskoe Izdatel'stvo "GEO"
    Call number: AWI G2-22-94741
    Type of Medium: Monograph available for loan
    Pages: 289, 3 Seiten , Illustrationen , 25 cm
    ISBN: 978-5-904682-70-5
    Language: Russian
    Note: In kyrillischer Schrift
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  • 53
    Monograph available for loan
    Monograph available for loan
    Fairbanks, Alas. : Institute of Northern Engineering, University of Alaska
    Associated volumes
    Call number: AWI G3-16-90316-4
    In: Ninth International Conference on Permafrost, Volume 1
    Type of Medium: Monograph available for loan
    Pages: xxx, 1054, xxxvi, xl Seiten , Illustrationen
    ISBN: 978-0-9800179-2-2
    Series Statement: Ninth International Conference on Permafrost Volume 1
    Language: English
    Note: Contents Preface Acknowledgments NICOP Organizing Team Members NICOP Sponsors Associate Editors and Reviewers Volume 1 Initial Disturbance and Recovery Measurements from Military Vehicle Traffic on Seasonal and Permafrost Terrain / R.T. Affleck, S.A. Shoop, C.M. Collins, and E. Clark Erosion of the Barrow Environmental Observatory Coastline 2003–2007, Northern Alaska / A. Aguirre, C.E. Tweedie, J. Brown, and A. Gaylord Pore Water and Effective Pressure in the Frozen Fringe During Soil Freezing / S. Akagawa, S. Hiasa, S. Kanie, and S.L. Huang Coastal Processes and Their Influence Upon Discharge Characteristics of the Strokdammane Plain, West Spitsbergen, Svalbard / H.J. Akerman Forecasting Chemical Thawing of Frozen Soil as a Result of Interaction with Cryopegs / V.I. Aksenov, N.G. Bubnov, G.I. Klinova, A.V. Iospa, and S.G. Gevorkyan Permafrost and Cryopegs of the Anabar Shield / S.V. Alexeev, L.P. Alexeeva, and A.M. Kononov A First Estimate of Mountain Permafrost Distribution in the Mount Cook Region of New Zealand’s Southern Alps / S. Allen, I. Owens, and C. Huggel The Perennial Springs of Axel Heiberg Island as an Analogue for Groundwater Discharge on Mars / D.T. Andersen, W.H. Pollard, and C.P. McKay Geotechnical Considerations for Cut-Off Wall in Warm Permafrost / S.L. Anderson, T.G. Krzewinski, and J. Swendseid Water Chemistry of Hydrogenous Taliks in the Middle Lena / N.P. Anisimova and N.A. Pavlova A New Hypothesis on Ice Lens Formation in Frost-Susceptible Soils / L.U. Arenson, T.F. Azmatch, and D.C. Sego Impact of the August 2000 Storm on the Soil Thermal Regime, Alaska North Slope / D.E. Atkinson and L. Hinzman Global Simulation of Permafrost Distribution in the Past, Present, and Future Using the Frost Number Method / T. Aus der Beek and E. Teichert Remote Sensing Data for Monitoring Periglacial Processes in Permafrost Areas: Terrestrial Laser Scanning at the Hinteres Langtalkar Rock Glacier, Austria / M. Avian, A. Kellerer-Pirklbauer, and A. Bauer Permafrost Temperatures and Erosion Protection at Shishmaref, Alaska / M.T. Azelton and J.E. Zufelt Measuring Ice Lens Growth and Development of Soil Strains during Frost Penetration Using Particle Image Velocimetry (GeoPIV) / T.F. Azmatch, L.U. Arenson, D.C. Sego, and K.W. Biggar Evidence of Permafrost Formation Two Million Years Ago in Central Alaska / J.E. Beget, P. Layer, D. Stone, J. Benowitz, and J. Addison Recent Advances in Mapping Deep Permafrost and Gas Hydrate Occurrences Using Industry Seismic Data, Richards Island Area, Northwest Territories, Canada / G. Bellefleur, K. Ramachandran, M. Riedel, T. Brent, and S. Dallimore Massive Ground Ice on the Ural Coast of Baydaratskaya Bay, Kara Sea, Russia / N.G. Belova, V.I. Solomatin, and F.A. Romanenko A Direct Method for Obtaining Thermal Conductivity of Gravel Using TP02 Probes / H. Bing, P. He, N.I. Koemle, and W. Feng The Effect of Near-Freezing Temperatures on the Stability of an Underground Excavation in Permafrost / K.L. Bjella Distribution of Permafrost Types and Buried Ice in Ice-Free Areas of Antarctica / J.G. Bockheim, I.B. Campbell, M. Guglielmin, and J. López-Martínez Estimation of Ice Wedge Volume in the Big Lake Area, Mackenzie Delta, NWT, Canada / J.A. Bode, B.J. Moorman, C.W. Stevens, and S.M. Solomon High Resolution DEM Extraction from Terrestrial LIDAR Topometry and Surface Kinematics of the Creeping Alpine Permafrost: the Laurichard Rock Glacier Case Study (Southern French Alps) / X. Bodin, P. Schoeneich, and S. Jaillet Comparison of Exposure Ages and Spectral Properties of Rock Surfaces in Steep, High Alpine Rock Walls of Aiguille du Midi, France / R. Böhlert, S. Gruber, M. Egli, M. Maisch, D. Brandová, W. Haeberli, S. Ivy-Ochs, M. Christl, P.W. Kubik, and P. Deline Heat and Water Transfer Processes in Permafrost-Affected Soils: A Review of Field- and Modeling-Based Studies for the Arctic and Antarctic (Plenary Paper) / J. Boike, B. Hagedorn, and K. Roth Estimation of Hydraulic Properties in Permafrost-Affected Soils Using a Two-Directional Freeze-Thaw Algorithm / W.R. Bolton, J. Boike, and P.P. Overduin Engineering Solutions for Foundations and Anchors in Mountain Permafrost / C. Bommer, H.R. Keusen, and M. Phillips Carbon, Nitrogen, and Phosphorus Interactions in the Hyporheic Zones of Arctic Streams that Drain Areas of Continuous Permafrost / W.B. Bowden, M.J. Greenwald, BM.N. Gooseff, BJ.P. Zarnetske, BJ.P. McNamara, J. Bradford, and T. Brosten Geomorphology and Gas Release from Pockmark Features in the Mackenzie Delta, Northwest Territories, Canada / R.G. Bowen, S.R. Dallimore, M.M. Côté, J.F. Wright, and T.D. Lorenson Current Capabilities in Soil Thermal Representations Within a Large-Scale Hydrology Model for Regions of Continuous Permafrost / L.C. Bowling, K.A. Cherkauer, and J.C. Adam Effects of Soil Cryostructure on the Long-Term Strength of Ice-Rich Permafrost Near Melting Temperatures /M.T. Bray Warming of Cold Permafrost in Northern Alaska During the Last Half-Century / M.C. Brewer and H. Jin Characterization and Classification of Topsoils as a Tool to Monitor Carbon Pools in Frost-Affected Soils / G. Broll and C. Tarnocai The International Permafrost Association: 1983–2008 / J. Brown, H. French, and C. Guodong Experimental Study of the Thermal Conductivity of Frozen Sediments Containing Gas Hydrates / B.A. Buhanov, E.M. Chuvilin, O.M. Guryeva, and P.I. Kotov Permafrost Dynamics Within an Upper Lena River Tributary: Modeled Impact of Infiltration on the Temperature Field Under a Plateau / S. Buldovich, N. Romanovskiy, G. Tipenko, D. Sergeev, and V. Romanovsky Permafrost Distributions on the Seward Peninsula: Past, Present, and Future / R.C. Busey, L.D. Hinzman, J.J. Cassano, and E. Cassano Soil and Permafrost Properties in the Vicinity of Scott Base, Antarctica / I.B. Campbell and G.G.G.Claridge Patterned Ground Features and Vegetation: Examples from Continental and Maritime Antarctica / N. Cannone and M. Guglielmin Rainfall-Runoff Hydrograph Characteristics in A Discontinuous Permafrost Watershed and Their Relation to Ground Thaw / S.K. Carey and C.M. DeBeer Innovative Designs of the Permafrost Roadbed for the Qinghai-Tibet Railway (Plenary Paper) / G. Cheng, Q. Wu, and W. Ma Does Permafrost Deserve Attention in Comprehensive Climate Models? / J.H. Christensen, M. Stendel, P. Kuhry, V. Romanovsky, and J. Walsh Trace Gas Budgets of High Arctic Permafrost Regions (Plenary Paper) / T.R. Christensen, T. Friborg, and M. Johansson Interannual Variations in Active Layer Thickness in Svalbard / H.H. Christiansen and O. Humlum Experimental Study of the Self-Preservation Effect of Gas Hydrates in Frozen Sediments / E.M. Chuvilin and O.M. Guryeva Effects of Recent Climate Change on High Mountains of Western North America / J.J. Clague A Model of Permafrost Distribution and Disturbance Sensitivity for Denali National Park, Using Soil-Ecological Site Inventory Information / M.H. Clark A Multi-Disciplinary Approach to Assess the Impact of Global Climate Change on Infrastructure in Cold Regions / J. Clarke, C. Fenton, A. Gens, R. Jardine, C. Martin, D. Nethercot, S. Nishimura, S. Olivella, C. Reifen, P. Rutter, F. Strasser, and R. Toumi Freezeback of an Anthropogenic Talik Within Tailings at Nanisivik Mine, Canada / G. Claypool, J.W. Cassie, and R. Carreau Geologic Controls on the Occurrence of Permafrost-Associated Natural Gas Hydrates / T.S. Collett Laboratory Simulations of Martian Debris Flows / F. Costard, E. Védie, M. Font, and J.L. Lagarde Modeling the Erosion of Ice-Rich Deposits Along the Yukon Coastal Plain / N.J. Couture, M.A. Hoque, and W.H. Pollard Dynamics of Patterned Ground Evolution / J.G.A. Croll Legacy and Accomplishments of Frozen Ground Engineering Studies in Alaska 60 Years Ago / M. Cysewski and Y. Shur High-Resolution Surface and Subsurface Survey of a Non-Sorted Circle System / R. Daanen, V. Romanovsky, D. Walker, and M. LaDouceur Effect of Adsorbed Cations on Unfrozen Water in Silty Soil as Det
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  • 54
    Call number: AWI G4-22-94837
    Description / Table of Contents: This monograph summarizes many years of theoretical, laboratory and field studies on the chemistry of groundwater, including cryopegs, and frozen sediments in the permafrost zone of Central Yakutia. Based on analysis of the research findings, it offers solutions to a number of scientific and applied problems; it also presents water, ice and icy-sediment sampling methods for chemical analyses. Several case studies are provided to show how these findings can be used in engineering site investigations, as well as in geocryological and hydrogeological studies in permafrost regions. The book is intended for hydrogeologists, geocryologists, hydrologists, reclamation experts, ecologists and other specialists working in permafrost regions, as well as a textbook for students studying geology and geography.
    Description / Table of Contents: Монография является обобщением многолетних теоретических, лабораторных и полевых исследований химического состава подземных вод, включая криопэги, и мерзлых отложений в специфических условиях криолитозоны Центральной Якутии. На основе анализа материалов исследований решен ряд научных и практических задач, разработана методика отбора проб воды, льда и ледяных отложений дл.я химических анализов. На конкре'l'НЫХ примерах рассматриваете. я возможность использования полученных результатов при проведении инженерно-геологических изысканий, геокрилогических и гидрогеологических исследований в области распространения многолетнемерзлых пород. Книга предназначена дл.я гидрогеологов, геокриологов, гидрологов, мелиораторов, экологов и других специалистов, работающих в области распространения многолетнемерзлых пород, а также может быть рекомендована в качестве учебного пособия для студентов геолого-географического профиля.
    Type of Medium: Monograph available for loan
    Pages: 185 Seiten , Illustrationen
    ISBN: 978-5-906284-56-3
    Language: Russian
    Note: CONTENTS Introduction Chapter 1. CRYOGENIC FACTORS CONTROLLING GROUNDWATER CHEMISTRY IN PERMAFROST ZONE DURING FREEZING OF WATER-BEARING MATERIALS 1.1. Physicochemical processes in freezing water-saturated rocks 1.2. Silica, fluorine, and biogenic- and organic-matter contents of groundwater in permafrost zone Chapter 2. CONTROLS ON CHEMISTRY OF LAKE WATER, TALIKS, AND BOTOOM SEDIMENTS 2.1. Chemical investigations of lake water and sediments in Central Yakutia 2.2. Chemical composition of mud solutions in lake sediments as a paleohydrologic indicator Chapter 3. CONTROLS ON CHEMISTRY OF ACTIVE-LA YER SUPRAPERMAFROST WATER AND TALIK WATER 3.1. Cryogenic factors con trolling the chemistry of active-layer suprapermafrost water 3.2. Controls on chemistry of intrapermafrost water in subaerial discharge areas 3.3. Chemical composition of groundwater in river, lake, and other types of taliks in the middle Lena valley Chapter 4. FORMATION OF CRYOPEGS 4.1. Natural conditions and anthropogenic factors for cryopeg formation 4.2. Investigations of the regime and dynamics of anthropogenic cryopegs in the Yakutsk area 4.3. Ground temperature regime in cryopegs areas 4.4. Changes in permafrost hydrogeochemistry in buit-up areas Chapter 5. CONTROLS ON CHEMISTRY OF FROZEN LOOSE DEPOSITS 5.1. Effect of the freezing process on salinity of frozen alluvial deposits 5.2. Changes in solute concentrations in permafrost deposits Chapter 6. PRACTICAL APPLICATIONS OF CRYOHYDROGEOCHEMICAL RELATIONSHIPS 6.1. The potential use of the icing process for improving water quality 6.2. Reconstruction of the water composition and mineralization of an icing-forming spring from hydrochemical analysis of ice samples 6.3. Improvement of the drinking quality of lake water Chapter 7. METHODOLOGICAL ISSUES IN CRYOHYDROGEOCHEMICAL RESEARCH 7.1. Potential sources of error in groundwater sampling in permafrost zone 7.2. Hydrochemical investigation of ground ice 7.3. Frozen soil sampling for chemical analysis 7.4. Hydrogeochemical monitoring in cryopeg areas 7.5. Application of the hydrogeochemical method for predicting cryopeg development 7.6. Chemical classification of natural water and presentation of analysis data Conclusions References. , ОГЛАВЛЕНИЕ Введение Глава 1. РОЛЬ КРИОГЕННЫХ ФАКТОРОВ В ФОРМИРОВАНИИ ХИМИЧЕСКОГО СОСТАВА ПОДЗЕМНЫХ ВОД КРИОЛИТОЗОНЫ В ПРОЦЕССЕ ПРОМЕРЗАНИЯ ВОДОНОСНЫХ ПОРОД 1.1. Физико-химические процессы в промерзающих водонасы-щенных породах 1.2. Содержание кремнекислоты, фтора, биогенных и органических веществ в подземных водах криолитозоны Глава 2. ОСОБЕННОСТИ ФОРМИРОВАНИЯ ХИМИЧЕСКОГО СОСТАВА ВОДЫ ОЗЕР, ПОДОЗЕРНЫХ ТАЛИКОВ И ДОННЫХ ОТЛОЖЕНИЙ 2.1. Исследования химического состава воды озер и донных отложений Центральной Якутии 2.2. Химический состав иловых растворов озерных осадков как палеогидрологический показатель Глава 3. ФОРМИРОВАНИЕ ХИМИЧЕСКОГО СОСТАВА НАДМЕРЗЛОТНЫХ ВОД СЕЗОННОТАЛОГО СЛОЯ И ТАЛИКОВЫХ ВОД 3.1. Криогенные факторы формирования химического состава надмерзлотных вод сезонноталого слоя 3.2. Особенности формирования химического состава подземных межмерзлотных вод на участках их субаэральной разгрузки 3.3. Химический состав подземных вод подрусловых, подозерных и других видов таликов в долине среднего течения р. Лены Глава 4. ОСОБЕННОСТИ ФОРМИРОВАНИЯ КРИОПЭГОВ 4.1. Естественные условия и техногенные факторы формирования криопэгов 4. 2. Изучение режима и динамики техногенных криопэгов на территории г. Якутска 4.3. Температурный режим пород на участках распространения криопэгов 4.4. Изменения мерзлотно-гидрогеохимических условий на освоенных площадях Глава 5. ФОРМИРОВАНИЕ ХИМИЧЕСКОГО СОСТАВА МЕРЗЛЫХ РЫХЛЫХ ОТЛОЖЕНИЙ 5 .1. Влияние условий промерзания на формирование засоленности мерзлых аллювиальных отложений 5.2. Изменение содержания водорастворимых веществ в многолетнемерзлых рыхлых отложениях Глава 6. ИСПОЛЬЗОВАНИЕ КРИОГИДРОГЕОХИМИЧЕСКИХ ЗАКОНОМЕРНОСТЕЙ В ПРИКЛАДНЫХ ЦЕЛЯХ 6.1. О возможности использования процесса наледеобразования для улучшения качества воды 6.2. Воссоздание состава и минерализации воды наледеобразующего источника по данным гидрохимического опробования льда 6.3. Улучшение питьевых качеств озерных вод Глава 7. МЕТОДИЧЕСКИЕ ВОПРОСЫ КРИОГИДРОГЕОХИМИЧЕСКИХ ИССЛЕДОВАНИЙ 7.1. Ошибки, возможные при гидрохимическом опробовании подземных вод криолитозоны 7. 2. Особенности гидрохимических исследований подземных льдов 7 .3. Специфика отбора проб мерзлых пород для химического анализа 7.4. Особенности проведения режимных гидрогеохимических наблюдений на площадях развития криопэгов 7.5. Применение гидрогеохимического метода для прогноза мест формирования криопэгов 7.6. Классификация природных вод по химическому составу и оформление данных анализа Заключение Литература , In kyrillischer Schrift
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  • 55
    Call number: AWI G6-22-94848
    Description / Table of Contents: Появившиеся в последние десятилетия новые данные (множественные радиометрические определения возраста памятников, в том числе их ряды, для памятников голоценового каменного века Северо-Восточной Азии), а также новые геоархеологические объекты (например, палеолитическая Янская стоянка - самый северный памятник раннего верхнего палеолита мира), позволяют обратиться к рассмотрению проблем хронометрии последовательностей культурноисторического развития Северо-Востока Азии в позднем неоплейстоцене и голоцене, в эпохи, предшествовавшие формированию современной этнической карты этих территорий. Наибольшее внимание в предлагаемой работе уделено проблемам радиоуглеродной хронологии и хроностратиграфии памятников верхнего палеолита, документирующих на настоящий момент древнейшие достоверные этапы расселения человека на Северо-Востоке Азии. Для археологов, специалистов в области четвертичной геологии, геоморфологов, палеогеографов.
    Type of Medium: Monograph available for loan
    Pages: 263 Seiten , Illustrationen , 25 cm
    ISBN: 9785020255203
    Language: Russian
    Note: CONTENTS Preface lnroduction Chapter I. Radiocarbon chronology and chronostratigraphy of the Paleolith of NE Asia: Statement of a Question Chapter II. Paleolithic sites of the Aidan River Valley Features of geology and geomorphology of Aldan valley Age and validity of archaeological sites in Aldan valley "Tectonic hypothesis" Chronostratigraphy of the Late Pleistocene and Holocene sites in Aldan valley Chapter III. Archaeological sites of the Yana-Indighirka Lowland The Yana site It's discovery and history of research General description of the site area Deposits of the second terrace of Yana River and position of the cultural layer of the Yana site Radiocarbon age of the cultura layer Archaeological finds Fauna remains The Berelekh site History of research Geological profile and radiocarbon chronology of Berelekh geocomplex Archaeological component of Berelekh geocomplex Fauna remains Chapter IV. Radiocarbon dated Paleolithic site of NE Asia beyond the Aidan valley and Coastal (Yana-Kolyma) lowland Geoarchaeological objects of Upper and Middle Lena River Archaeological sites of Kolyma River basin and Sea of Okhotsk and Kolyma River watershed Ushki sites in Kamchatka Peninsula Concluding remarks for the Fourth Chapter Chapter V. Basic elements of radiocarbon chronology of the Holocene Stone Age of NE Asia Chapter VI. Radiocarbon chronology, archaeological periodization and peculiarities of cultural development of the Late Pleistocene and Holocene of NE Asia Conclusions Summary References List of abbreviations Radiocarbon laboratory's codes List of illustrations List of tables Appendices Table 1. Radiocarbon dates of archaeological site of NE Asia Table 8. A synopsis for geomorphology of 14C dated Late Pleistocene and Early Holocene archaeological sites of NE Asia , СОДЕРЖАНИЕ Предисловие Введение Глава I. Радиоуглеродная хронология и хроностратиrрафия палеолита Северо- Востока Азии: постановка проблемы Глава II. Памятники палеолита в долине р. Алдан Особенности строения долины р. Алдан Возраст и валидность археологических памятников Алдана «Тектоническая гипотеза» Хроностратиграфия памятников позднего неоплейстоцена и голоцена Алдана Глава III. Памятники Яно-Индиrирской низменности Янская стоянка История открытия и изучения Общая характеристика района стоянки Отложения разреза второй надпойменной террасы р. Яны и положение культурного слоя Янской стоянки Радиоуглеродный возраст культурного слоя Археологическая составляющая Фаунистическая характеристика Стоянка Берелёх История изучения Характеристика разреза и хронология Берелёхского комплекса Археологическая составляющая Берелёхского комплекса Комплекс фаунистических находок Глава IV. Датированные памятники палеолита Северо-Восточной Азии вне пределов долины Алдана и Приморской (Я но-Колымской) низменности Геоархеологические объекты Верхней и Средней Лены Памятники Колымской системы и Охотска-Колымского водораздела Комплекс Ушковских стоянок (Камчатский полуостров) Заключительные замечания к разделу Глава V. Основные черты радиоуглеродной хронологии rолоценовых памятников каменноrо века Северо-Восточной Азии Глава VI. Радиоуглеродная хронология, археологическая периодизация и особенности культурно-исторических процессов позднего неоплейстоцена и rолоцена Северо-Восточной Азии Заключение Summary Литература Список сокращений Список иллюстраций Список табличного материала Список индексов лабораторий, проводящих радиоуглеродное датирование Приложения Таблица 1. Список радиоуглеродных дат археологических объектов Северо-Востока Азии Таблица 8. Краткий конспект геоморфологического положения датированных поздненеоплейстоценовых и раннеrолоценовых археологических памятников Северо-Востока Азии , Zusammenfassung in englischer Sprache , In kyrillischer Schrift
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  • 56
    Monograph available for loan
    Monograph available for loan
    New Dehli : New Age International Publishers
    Call number: AWI Bio-22-94883
    Type of Medium: Monograph available for loan
    Pages: XI, 349 Seiten , Illustrationen
    Edition: Reprint 2005
    ISBN: 0470213590 , 085226240X , 81-224-1343-9
    Language: English
    Note: Contents Foreword, by Professor Dr. Martin Bopp Preface Acknowledgements 1. EXPERIMENTS ON SPORES AND GEMMAE Spore Germination in Liverwort - Jungermanniales, Marchantiales, Anthocerotales, Sphaerocarpales; Types of Spore Germination in Mosses - Sphagnales, Andreaeales, Tetraphidales, Bryales Factors Affecting Spore Germination - Light, Temperature, Sugars, Minerals, Growth Regulators, Hydrogen-ion concentration (pH), OtheT Factors Mechanism of Spore Germination Experiments on Gemmae - light, Temperature, Humidity and other Physical Factors, Growth Regulators, Nitrogenous Substances, Hydrogen-ion concentration (pH), Other Chemical Factors References 2. PROTONEMAL DIFFERENTIATION AND BUD FORMATION IN MOSSES Protonemal Differentiation Bud Formation Factors Affecting Bud Formation - Light, Temperature, Auxins, Cytokinins, Gibberellins, Adenosine 3', 5'-cyclic monophosphate, Adenine and Amino Acids, Minerals and Chelates Vitamins, Abscisic Acid, Sugars, pH, Influence of Other Organisms References. 3. REGENERATION Potentialities of Various Organs for Regeneration - Regeneration from Leaves, Regeneration from Setae Morphology of Régénérants Factors Affecting Regeneration - Light. Radiation, pH, Season, Humidity. Wounding, Temperature, Size of the Fragment Reserve Food Material. Location in the Plant, Age, Correlative Inhibition. Polarity and Apical Dominance Changes Occurring in Regenerating Cells References 4. REPRODUCTIVE BIOLOGY Factors Affecting Gametangial Induction - Light Duration, Light Level, Light Quality. Temperature, Temperature-Photoperiod Interaction. Humidity. Hydration. Carbohydrates. Nitrogenous Substances, Growth Regulators, Chelating Agents, pH and Other Factors References 5. ALTERNATIVE PATHWAYS IN LIFE CYCLE Apogamy - Occurrence of Apogamy in Diplophase and Haplophase, Spore Production in Apogamous Sporophytes, Differentiation of Apogamous Sporophytes from Callus, Factors Controlling Differentiation of Apogamous Sporophytes: Exogenous Factors, Endogenous Factors, Differentiation of Sporophyte and Gametophyte, Role of Calyptra in Sporogon Development Apospory Callus Formation and its Differentiation - Formation of Callus. Differentiation in Callus Controls in Differentiation Alternation of Generations References 6. PHOTOMORPHOGENESIS Spore Germination - Liverworts, Mosses Growth - Liverworts, Mosses Vegetative Propagation - Liverworts, Mosses Metabolism - Liverworts. Mosses; Senescence Bud Induction in Mosses Tropic Responses - Liverworts, Mosses References. 7. ULTRASTRUCTURAL STUDIES Spore Protonema Stem Leaf Gametangia - Antheridium Gametogenesis - Spermatogenesis, Oogenesis Sporogenesis - Spore Sac or Tapetum. Fluctuation in Plastid Number, Structural Changes in Plastids, Cytoplasm, and Other Organelles. Meiosis. Spore Wall Formation Sporophyte-Ganietophyte Junction Seta Histoenzymological Studies - Localization of Enzymes in the Haustorial Foot References 8. CHEMICAL CONSTITUENTS OF BRYOPHYTES Antibiotics Growth Substances - Specified Growth Substances, Non-specified Growth Substances Lipids - Alkanes, Fatty Acids, Cuticular Components Terpenoids - Monoterpenoids, Sesquiterpenoids, Ditetpenoids, Triterpenoids and Sterols Flavonoids - Flavones, Isoflavones, Flavonols, Dihydrofiavonoids and Biflavonyls, Aurones and Chalcones, Acylated Flavonoids, Anthocyanins and Proanthocyanidins, Sphagnorubins Lignins; Other Constitutents - Carotenoids, Carbohydrates, Organic Acids, Dihydrostilbenes, Enzymes, Amino Acids and Quinones, Inorganic Compounds, Miscellaneous, Antitumour Activities, Allergenic Activities References 9. BRYOPHYTES AS INDICATORS OF POLLUTION Heavy Metals - Lead, Cadmium, Zinc, Mercury, Arsenates, Chromium, Nickel. Vanadium Stability Pattern of Metal Ions Metal Tolerance - Copper Mosses, Peat Mosses Gaseous Pollutants - Sulphur dioxide. Fluorides, Ozone Radionuclides (Radio Isotopes) - Cesium. Strontium, Uranium; Radiations References. 10. PROTOPLAST CULTURE Isolation of Protoplasts - Mechanical Method, Enzymatic Method, Source Material for Protoplasts, Factors Affecting Protoplast Isolation: Culture of Protoplasts—Liquid Culture Agar Plating of Protoplasts: Regeneration of Protoplasts - Factors Affecting Regeneration Protoplast Fusion and Somatic Hybrids Induction and Isolation of Mutants References. 11. CONDUCTION IN BRYOPHYTES External Conduction - Gametophyte. Sporophyte, Significance of External Conduction Internal Conduction - Cells Involved in Conduction, Anatomy of the Horizontal Axis, Midribs and Leaf Traces. Conducting Strand in Seta and Capsule, Development and Structure of Mature Conducting Tissues. The Interphase, Internal Conduction of Water, Conduction of Organic Compounds; Evolutionary Trends in the Conducting Strands References. 12. WATER RELATIONS Absorption and Conduction of Water - Endohydric.' Ectohydric, Myxohydric Water Holding Capacity and Growth Rate Desiccation and Rehydration Mechanism of Damage Growth-Forms References SUBJECT INDEX PLANT INDEX AUTHOR INDEX
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  • 57
    Monograph available for loan
    Monograph available for loan
    Jakutsk : Jakutskij Filial SO AN SSSR
    Call number: AWI G3-22-94893
    Description / Table of Contents: В книге приводится обстоятельная и разносторонняя характеристика основных генетических типов почв аласов. Выявлено влияние термокарстового аласообразования на почвообразовательный процесс. Полученные результаты позволяют рассматривать почвы аласов как самостоятельные типы, возникновение которых связано со своеобразным аласным процессом, присущим, только термокарстовым ландшафтам. Впервые охарактеризованы особенности структуры почвенного покрова аласов и раскрыты причины ее дифференциации . Книга предназначена для почвоведов, мелиораторов, агрохимиков, а также для других специалистов сельского хозяйства и проектных организаций, связанных с использованием и освоением земель в области широкого распространения многалетнемерзлых пород.
    Description / Table of Contents: Translation of the abstract: The book provides a detailed and versatile description of the main genetic types of Alas soils. The influence of thermokarst alas formation on the soil-forming process was revealed. The results obtained allow us to consider alas soils as independent types, the occurrence of which is associated with a peculiar alas process, inherent only in thermokarst landscapes. For the first time the features of the structure of the soil cover of the alas were characterized and the reasons for its differentiation were revealed. The book is intended for soil scientists, land reclamators, agrochemists, as well as for other agricultural specialists and design organizations involved in the use and development of land in the area of ​​widespread permafrost.
    Type of Medium: Monograph available for loan
    Pages: 168 Seiten , Illustrationen
    Language: Russian
    Note: ОГЛАВЛЕНИЕ Введение 3 Глава 1. Природно-климатические условия 1.1. Геология и геоморфология 1.2. Многолетняя мерзлота 1.3. Почвообразующие породы 1.4. Климат 1.5. Поверхностные воды 1.6. Растительность Глава 2. Особенности почвообразования в аласах 2.1. Краткая история исследования почв аласов 2.2. Аласный термокарстовый рельеф 2.3. Влияние аласов на почвообразование 2.4. Аласный тип почвообразования Глава 3. Почвы 3.1. Зональные почвы 3.1.1. Мерзлотные палевые почвы 3.1.2. Мерзлотные палевые осолоделые почвы 3.1 .3. Мерзлотные таежные оподз аленные почвы 3.2. Почвы аласов 3.2.1. Аласные болотные и заболоченные почвы 3.2.2. Аласные луговые почвы 3.2.3. Аласные остепненные почвы Глава 4. Структура почвенного покрова аласов 4.1. Условия дифференциации почвенного покрова аласов 4.2. Структура почвенного покрова различных по рельефу аласов 4.3. Неоднородность почвенного покрова разновозрастных термокарстовых котловин Заключение Список литературы
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  • 58
    Call number: AWI G3-23-95351
    In: Trudy Instituta Geologii i Geofiziki, vypusk 508
    Description / Table of Contents: Это четвертая книга авторского колпектива по силуру Сибирской платформы. в первой части работы даются общая характеристика методологии экостратиграфических исследований, проводимых на Сибирской платформе комnлекснои литолого-палеонтолоrической группой, и сопоставление региональнои шкалы с общей стратиграфической. Затем приводится описание новых свит силура и нижнего девона Норильского и Игарскоrо районов. Во второй части работы дается стратиграфический анализ и описание фауны и флоры. Книга представляет интерес для геологов, стратиграфов и палеонтологов.
    Description / Table of Contents: Translation of the abstract: This is the fourth book of the author’s team on the Silurian of the Siberian Platform. The first part of the work provides a general description of the methodology of ecostratigraphic studies carried out on the Siberian platform by an integrated lithological and paleontological group, and a comparison of the regional scale with the general stratigraphic scale. Then a description of the new formations of the Silurian and Lower Devonian of the Norilsk and Igarsk regions is given. The second part of the work provides a stratigraphic analysis and description of the fauna and flora. The book is of interest to geologists, stratigraphers and paleontologists.
    Type of Medium: Series available for loan
    Pages: 187 Seiten , Illustrationen
    Series Statement: Trudy Instituta Geologii i Geofiziki vypusk 508
    Language: Russian
    Note: In kyrillischer Schrift
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  • 59
    Call number: AWI G6-23-95368
    Type of Medium: Monograph available for loan
    Pages: XIX, 1004 Seiten , Illustrationen
    ISBN: 9780891189602 , 978-0-891-18960-2 , 0891189602
    ISSN: 2163-5804 , 1047-4986
    Series Statement: Soil Science Society of America book series 10
    Language: English
    Note: Contents Foreword Preface Contributors Chapter 1 Issues of Sampling Design in Wetlands / Monica Rivas Casado, Ron Corstanje, Pat Bellamy, and Ben Marchant DESIGN-BASED SAMPLING APPROACHES MODEL-BASED SAMPLING APPROACHES Chapter 2 Soil and Sediment Sampling of Inundated Environments / Todd Z. Osborne and R.D. DeLaune SAMPLING IN INUNDATED ENVIRONMENTS: SAMPLING PLAN AND GENERAL CONSIDERATIONS SAMPLING METHODS FOR INUNDATION DEPTHS LESS THAN 1.5 METERS SAMPLING METHODS FOR INUNDATION DEPTHS GREATER THAN 1.5 METERS SPECIAL CONDITIONS OR CONSIDERATIONS Chapter 3 Physicochemical Characterization of Wetland Soils / K.R. Reddy, M.W. Clark, R.D. DeLaune, and M. Kongchum SOIL SAMPLING PHYSICOCHEMICAL PROPERTIES CONCLUSIONS Chapter 4 Soil Pore Water Sampling Methods / M.M. Fisher and K.R. Reddy TECHNIQUES FOR SAMPLING SOIL PORE WATER SAMPLE HANDLING CONSIDERATIONS SAMPLING PORE WATER GASES SUMMARY Chapter 5 Reduction–Oxidation Potential and Oxygen / J. Patrick Megonigal and Martin Rabenhorst REDOX POTENTIAL THEORY OXYGEN MEASUREMENT WITH DIFFUSION CHAMBERS REDOX MEASUREMENT Chapter 6 Determination of Dissolved Oxygen, Hydrogen Sulfide, Iron(II), and Manganese(II) in Wetland Pore Waters / George W. Luther III and Andrew S. Madison EXPERIMENTAL PRINCIPLES OF ELECTRODE FABRICATION EXPERIMENTAL PRINCIPLES OF WORKING ELECTRODE CALIBRATIONS PROCEDURES FOR MICROPROFILING SUMMARY Chapter 7 Soil Redox Potential and pH Controllers / Kewei Yu and Jörg Rinklebe REDOX POTENTIAL AND pH CONTROL MODIFICATIONS AN AUTOMATED BIOGEOCHEMICAL MICROCOSM SYSTEM APPLICATIONS Chapter 8 Morphological Methods to Characterize Hydric Soils / M.J. Vepraskas EQUIPMENT METHODS AND TECHNIQUES FOR DESCRIBING HYDRIC SOILS FIELD TEST TO ASSESS SOIL MATERIAL TYPE IDENTIFYING HYDRIC SOIL FIELD INDICATORS Chapter 9 Emergent Macrophyte Biomass Production / Christopher Craft SAMPLING CONSIDERATIONS INDIRECT METHODS DIRECT METHODS EMERGING METHODS Chapter 10 Photosynthetic Measurements in Wetlands / S.R. Pezeshki OXYGEN EXCHANGE MEASUREMENT TECHNIQUE CARBON ISOTOPE TECHNIQUE MICROMETEOROLOGICAL TECHNIQUE CHLOROPHYLL FLUORESCENCE METHOD PHOTOSYNTHETIC MEASUREMENTS USING CHAMBERS SUMMARY Chapter 11 Gas Transport and Exchange through Wetland Plant Aerenchyma / Brian K. Sorrell and Hans Brix GENERAL PRINCIPLES EXPERIMENTAL PRINCIPLES LABORATORY AND GLASSHOUSE CHAMBERS MODELING APPROACHES Chapter 12 A Primer on Sampling Plant Communities in Wetlands / Curtis J. Richardson and Ryan S. King OVERVIEW OF SAMPLING PLANT POPULATIONS AND COMMUNITIES SAMPLE SIZE PLANT SAMPLING APPROACHES RAPID ASSESSMENT APPROACHES TO ESTIMATE PLANT ABUNDANCE AND COVER PERCENTAGE PLANT SAMPLING METHODS AND CALCULATION PROCEDURES ANALYSIS OF DATA COMPARISON OF PLANT COMMUNITIES SUGGESTIONS FOR DEVELOPING A PLANT SAMPLING PROGRAM APPENDIX Chapter 13 Plant Productivity—Bottomland Hardwood Forests / William H. Conner and Julia A. Cherry ABOVEGROUND PRODUCTIVITY BELOWGROUND PRODUCTIVITY Chapter 14 Current Methods to Evaluate Net Primary Production and Carbon Budgets in Mangrove Forests / Victor H. Rivera-Monroy, Edward Castañeda-Moya, Jordan G. Barr, Vic Engel, Jose D. Fuentes, Tiffany G. Troxler, Robert R. Twilley, Steven Bouillon, Thomas J. Smith III, and Thomas L. O’Halloran CURRENT METHODS TO ESTIMATE NET PRIMARY PRODUCTIVITY COMPARING MANGROVE NET PRIMARY PRODUCTION ESTIMATES TO WHOLE-FOREST CARBON FLUX MEASUREMENTS SUMMARY AND FUTURE RESEARCH DIRECTIONS APPENDIX Chapter 15 Characterization of Wetland Soil Organic Matter / Robert L. Cook and Thomas S. Bianchi SAMPLE TREATMENT AND PROCESSING SPECTROSCOPIC CHARACTERIZATION BULK ELEMENTAL AND CHEMICAL BIOMARKER ANALYSES SUMMARY Chapter 16 Dissolved Organic Matter / Robert G. Qualls EQUIPMENT AND INSTRUMENTATION MATERIALS AND REAGENTS SAMPLE PREPARATION PROCEDURES CONCLUSIONS Chapter 17 Soil Microbial Biomass and Phospholipid Fatty Acids / Jörg Rinklebe and Uwe Langer THE SUBSTRATE-INDUCED RESPIRATION METHOD PHOSPHOLIPID FATTY ACIDS ESTIMATES OF MICROBIAL BIOMASS SUMMARY Chapter 18 Molecular Genetic Analysis of Wetland Soils / Hee-Sung Bae and Andrew V. Ogram DNA EXTRACTION QUANTITATIVE POLYMERASE CHAIN REACTION POLYMERASE CHAIN REACTION BASED MOLECULAR CLONING Chapter 19 Enzyme Activities / Hojeong Kang, Seon-Young Kim, and Chris Freeman EQUIPMENT AND INSTRUMENTATION MATERIALS AND REAGENTS SAMPLE PREPARATION PROCEDURE CALCULATION SUMMARY Chapter 20 Organic Matter Mineralization and Decomposition / Scott D. Bridgham and Rongzhong Ye LITTER DECOMPOSITION DECOMPOSITION OF STANDARD SUBSTRATES SOIL HETEROTROPHIC RESPIRATION PHOTODEGRADATION Chapter 21 Methanogenesis and Methane Oxidation in Wetland Soils / Kanika S. Inglett, Jeffery P. Chanton, and Patrick W. Inglett EXPERIMENTAL METHANE MEASUREMENTS ISOTOPIC MEASUREMENTS OF METHANE Chapter 22 Greenhouse Gas Emission by Static Chamber and Eddy Flux Methods / Kewei Yu, April Hiscox, and R.D. DeLaune STATIC CHAMBER MEASUREMENT EDDY COVARIANCE MEASUREMENT SUMMARY Chapter 23 Characterization of Organic Nitrogen in Wetlands / C.M. VanZomeren, H. Knicker, W.T. Cooper, and K.R. Reddy CHEMICAL FRACTIONATION OF SOIL ORGANIC NITROGEN CHLOROFORM FUMIGATION METHOD NUCLEAR RESONANCE SPECTROSCOPY MASS SPECTROMETRY OF ORGANIC NITROGEN CONCLUSIONS Chapter 24 Measurements of Nitrogen Mineralization Potential in Wetland Soils / Eric D. Roy and John R. White POTENTIALLY MINERALIZABLE NITROGEN SUBSTRATE-INDUCED NITROGEN MINERALIZATION LIMITATIONS SUMMARY Chapter 25 Wind Tunnel Method for Measurement of Ammonia Volatilization / M.E. Poach, K.S. Ro, and P.G. Hunt EQUIPMENT AND INSTRUMENTATION MATERIALS AND REAGENTS SAMPLE PREPARATION PROCEDURE SAMPLE ANALYSIS CALCULATION STATISTICAL ANALYSIS QUALITY ASSURANCE SUMMARY Chapter 26 Ammonium Oxidation in Wetland Soils / K.S. Inglett, A.V. Ogram, and K.R. Reddy AEROBIC AMMONIUM OXIDATION (NITRIFICATION) ANAEROBIC AMMONIUM OXIDATION (ANAMMOX) METHODS FOR ASSESSING AEROBIC AMMONIUM OXIDATION (NITRIFICATION) METHODS FOR ASSESSING ANAEROBIC AMMONIUM OXIDATION (ANAMMOX) POTENTIAL MOLECULAR METHODS FOR ASSESSING AMMONIUM OXDIATION IN WETLAND SOILS SUMMARY Chapter 27 Denitrification Measurement Using Membrane Inlet Mass Spectrometry / Patrick W. Inglett, Todd M. Kana, and Soonmo An GENERAL PRINCIPLES EXPERIMENTAL PRINCIPLES ISOTOPE PAIRING BY THE MIMS METHOD SUMMARY Chapter 28 Nitrate Reduction, Denitrification, and Dissimilatory Nitrate Reduction to Ammonium in Wetland Sediments / Amy J. Burgin, Stephen K. Hamilton, Wayne S. Gardner, and Mark J. McCarthy EQUIPMENT AND INSTRUMENTATION MATERIALS AND REAGENTS PROCEDURES SAMPLE PREPARATION CALCULATIONS Chapter 29 System-Level Denitrification Measurement Based on Dissolved Gas Equilibration Theory and Membrane Inlet Mass Spectrometry / Andrew Laursen and Patrick W. Inglett GENERAL THEORY EXPERIMENTAL PRINCIPLES CALCULATIONS DISCUSSION AND LIMITATIONS SUMMARY Chapter 30 Biogeochemical Nitrogen Cycling in Wetland Ecosystems: Nitrogen-15 Isotope Techniques / Dries Huygens, Mark Trimmer, Tobias Rütting, Christoph Müller, Catherine M. Heppell, Katrina Lansdown, and Pascal Boeckx EXPERIMENTAL STUDY SETUPS ISOTOPE PAIRING AND REVISED ISOTOPE PAIRING TECHNIQUES ISOTOPE DILUTION AND TRACING TECHNIQUES Chapter 31 Biological Dinitrogen Fixation / Patrick W. Inglett ACETYLENE REDUCTION DINITROGEN-15 INCORPORATION SUMMARY Chapter 32 Methods for Soil Phosphorus Characterization and Analysis of Wetland Soils / Curtis J. Richardson and K.R. Reddy TERMINOLOGY, OPERATIONAL DEFINITIONS, AND COMPARISON OF PHOSPHORUS FORMS SAMPLE PREPARATION AND STORAGE SOIL PHOSPHORUS ANALYSIS PHOSPHORUS AVAILABILITY INDICES ANION EXCHANGE RESIN AND IRON OXIDE PAPER SOIL INORGANIC PHOSPHORUS FORMS GENERAL COMMENTS Chapter 33 Phosphorus Characterization in Wetland Soils by Solution Phosphorus-31 Nuclear Magnetic Resonance Spectroscopy / Alexander W. Cheesman, James Rocca, and Benjamin L. Turner BRIEF OVERVIEW OF THE PRINCIPLES APPLICATION TO WETLAND SOILS Chapter 34 Phosphorus Sorption and Desorption
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  • 60
    Call number: AWI G3-23-95315
    Description / Table of Contents: In the monograph results of long-term ground and remote sensing experimental and theoretical investigations of heat-water exchange of typical permafrost landscapes and small river basins of Eastern Siberia and its factors situated in subarctic tundra, plain taiga and southern mountain taiga are generalized. Detailed maps of landscape structure of range grounds as well as results of analysis of wide range of parameters and variables of permafrost landscapes characterizing spatial and temporal variability of their state in daily, seasonal and long-term scales are presented. Zonal-landscape features of heat and water exchange as well as water regime of small river basins have been revealed. Spatial distribution of vertical turbulent heat and moisture flows in the boundary layer of the atmosphere above heterogeneous surface by measurements from board a plane has been investigated. Spatial and temporal analysis of thermo- and water-physical properties of perennially frozen grounds, which are applied as parameters in hydro-climatic models, has been fulfilled. Processes of interaction of surface and underground waters on plain and in the mountains have been considered, as well as cryogenic phenomena, which have considerable impact upon water regime of rivers and permafrost landscapes.
    Type of Medium: Monograph available for loan
    Pages: 575 Seiten , Illustrationen
    ISBN: 978-5-89658-033-1 , 978-5-94789-232-1
    Language: Russian
    Note: Contents Introduction / A.G. Georgiadi, A.N. Zolotokrylin CHAPTER 1. SUBARCTIC TUNDRA 1.1. Characteristics of subarctic polygon and a complex of field experimental investigations / A.G. Georgiadi 1.2. Landscapes and their characteristics 1.2.1. Types and distribution over territory / R.V. Desyatkin, L.D. Hinzman 1.2.2. Seasonal changes of spectral characteristics of landscapes by data of remote sensing measurements / V.B. Malyshev, N. S. Ozerov 1.3. The active layer of subarctic landscapes: typology and geography 1.3.1. Spatial variabi!ity of the active layer thickness / A.G. Georgiadi, V.G. Onischenko 1.3.2. Hydrophysical characteristics of the seasonal-melting layer / A.G. Georgiadi,V.G. Onischenko 1.4. Radiation and thermal characteristics of landscapes in the summer period 1.4.1. Systematization of experimental information on albedo and surface temperature / A.N. Zolotokrylin 1.4.2. Analysis of experimental information on the surface temperature / A.N. Zolotokrylin, V.V. Vinogradova 1.5. Heat exchange in tundra landscapes 1.5.1. Structure of heat exchange and its seasonal features / A.N. Zolotokrylin 1.5.2. Theoretical analysis of the process of heat transfer in the surface thawed layer of soil grounds / A.B. Kazansky, A.N. Zolotokrylin 1.6. Features of water regime and water exchange in tundra 1.6.1. Water regime and water balance of river basins by results of experimental measurements / A.G. Georgiadi 1.6.2. Interrelationship of underground and surface waters and underground alimentation of rivers in different year seasons / V.V. Shepelev CHAPTER 2. CENTRAL PLAIN TAIGA 2.1. Geographical characteristics of Spasskaya Pad polygon / A.N. Fedorov 2.2. Types of landscapes, their distribution over territory and seasonal dynamics / A.N. Fedorov, Ya. I. Torgovkin, S.P. Varlamov 2.3. Characteristics of the active layer and its physical properties 2.3.1. Spatial and seasonal variability of the active layer thickness 2.3.1.1. Inter-landscape variability of the seasonal-thawing layer thickness / I.S. Vasiliev 2.3.1.2. Variability of the active layer thickness at experimental sites / E.Yu. Gerasimov 2.3.1.3. Freezing of the active layer / P.Ya. Konstantinov 2.3.2. Physical properties of soils of the seasonal-thawing layer under larch forest / A.G. Georgiadi, V.G. Onischenko 2.3.3. Inter-landscape differences of physical properties of the active layer / P.Ya. Konstantinov, I.S. Ugarov, R.N. Argunov 2.3.4. Features of thermal conductivity of soil grounds / V.G. Onischenko, I.S. Lisker, A.G. Georgiadi 2.4. Radiation balance and thermal regime of landscapes 2.4.1. Radiation balance and its components / I.S. Ugarov 2.4.2. Temperature regime of the active layer / P.P. Gavriliev, I.S. Ugarov, P.V. Efremov 2.4.3. Temperature regime of the upper layers of perennially frozen grounds / P.Ya. Konstantinov 2.5.Heat exchange in permafrost landscapes of plain taiga / P.P. Gavriliev 2.6. Features of heat and moisture balance in taiga-alas landscapes / R.V. Desyatkin, I. Ishii, Kh. Yabuki, A.R. Desyatkin, P.P. Fedorov, T.N. Semenova 2.7. Turbulent energy- and moisture exchange in the atmospheric boundary layer (ABL) over thermally heterogeneous surface (over the Lena River lowland in the Yakutsk area) / M.A. Strunin 2.7.1. Some aspects of the atmospheric boundary layer (ABL) observations using the aircraft laboratory 2.7.2. Aircraft experiment of the atmospheric boundary layer (ABL) observations in the Yakutsk area 2.7.2.1. Aicraft laboratory IL-18d and its instruments for investigations of ABL 2.7.2.2. Scheme and conditions of the aircraft experiment 2.7.2.3. Radiosounding, surface measurements and satellite observations 2.7.2.4. Turbulence and turbulent fluxes data processing and analyzing 2.7.3. Some features of the convective boundary layer (CBL) development over thermally heterogeneous surface 2.7.3.1. Seasonal variability of turbulent fluxes 2.7.3.2. Fine spatial ABL structure 2.7.3.3. Conditions of appearance and development of the mesoscale thermal internal boundary layer (MTIBL) inside the CBL 2.7.3.4. Appearance of the local circulation over thermal mesoscale patch on the underlying surface 2.7.3.5. The local circulation and the problem of energy balance in the atmospheric boundary layer 2.7.3.6. Conditions of applying the scaling models for the CBL developing over heterogeneous underlying surface 2.7.3.7. The spectral structure of fluxes 2.7.3.8. Flux separating into turbulent and mesoscale portions 2.7.3.9. Separating approach models for mesoscale and turbulent fluxes in the CBL 2.7.3.10. Some f eatures of mesoscale and turbulent fluxes seasonal variations 2.7.4. The main results of observations of the CBL, developing over the thermally heterogeneous surface 2.8 Moisture exchange in plain taiga landscape 2.8.1. Moisture regime of the active layer 2.8.1.1. Landscape features of moisture dynamics of the active layer / P.P. Gavriliev, I.S. Ugarov, P.V. Efremov, R.N. Argunov 2.8.1.2. Spatial and temporal distribution of moisture reserves in the active layer / A.N. Fedorov, Ya.I.Torgovkin, R.N. Arguniov, P.P. Gavriliev, I.S. Vasiliev, J.S. Ugarov, P.V. Efremov 2.8.2. Interrelationship of underground and surface waters and underground alimentation of rivers in different seasons / V.V. Shepelev CHAPTER 3. SOUTHERN MOUNTAIN TAIGA 3.1. Natural conditions of the region / V.S. Vuglinsky, M.L. Markov 3.1.1. Climate 3.1.2. Relief and geological structure 3.1.3. Permafrost and hydrogeological conditions 3.1.4. Hydrography and hydrological conditions 3.1.5. Interrelationship of surface and underground waters, underground alimentation of rivers 3.1.5.1. lntraannual dynamics of water exchange of rivers with drained aquifers 3.1.5.2. Seasonal glaciation and its impact upon formation of river runoff 3.2. Results of study of regularities of heat- and moisture exchange at an experimental SHI Mogot polygon / N.G. Vasilenko, S.A. Zhuravin 3.2.1. General characteristics of the Mogot polygon and program of investigations 3.2.2. Landscape and soil characteristics of catchments of the Mogot polygon 3.2.2.1. Landscapes of the Mogot polygon 3.2.2.2. Landscape-hydrology complexes 3.2.2.3. Types of soils and their water physical characteristics 3.2.3. Features of climate in the region of the Mogot polygon 3.2.4. Radiation and heat balances 3.2.4.1. Radiation balance 3.2.4.2. Heat balance 3.2.5. Water balance 3.2.5.1. Methods of identification of the main components of water balance 3.2.5.2. Features of fo rmation of water balance elements 3.2.5.3. Results of calculation of water balances List of literature SUPPLEMENT TO PART 2.7. INSTRUMENTS AND METHODS FOR INVESTIGATION OF THE ATMOSPHERE USING THE AIRCRAFT LABORATORY / M.A. Strunin S.2.7.1. Methods of wind speed and direction, air temperature and humidity and turbulence measurements based on aircraft data S.2.7.2. Aircraft laboratory IL-18d and its instruments for investigation of the atmosphere S.2.7.3. Database of aircraft observations and preliminary data processing S.2.7.4. Errors of turbulent fluxes calculations based on aircraft data S.2.7.5. Methods of spectral analysis of turbulence data S.2.7.6. Calculations of spectral characteristics of fluctuations based on Fourier analysis S.2.7.7. Using the wavelet-transformations for the spectral analysis List of literature to Supplement 2.7 , In kyrillischer Schrift , Einführung und Inhaltsverzeichnis in englischer Sprache
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  • 61
    Call number: AWI A2-24-95687
    Type of Medium: Monograph available for loan
    Pages: 97 Seiten , Illustrationen
    Edition: 2nd edition
    ISBN: 9782880853051 , 978-2-940443-00-0
    Language: English
    Note: Contents Executive summary Overview Arctic climate change Key findings of this assessment 1. Atmospheric circulation feedbacks 2. Ocean circulation feedbacks 3. Ice sheets and sea-level rise feedbacks 4. Marine carbon cycle feedbacks 5. Land carbon cycle feedbacks 6. Methane hydrate feedbacks Author team
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  • 62
    Call number: AWI G3-24-95571-11
    In: Tektonika Sibiri, Tom 11
    Description / Table of Contents: Представлены материалы XIII сессии Научного совета по тектонике Сибири и Дальнего Востока (Якутск, 1980 г.). Подробно рассмотрены вопросы современного состояния теоретической геотектоники и закономерности формирования земной коры в докембрии и фанерозое. Приведены новые материалы по региональной тектонике платформенных и подвижных областей Сибири и Дальнего Востока СССР. Приведенные модели строения и эволюции земной коры с достаточной полнотой отражают современное состояние теоретической геотектоники. Сборник рассчитан на широкий круг геологов.
    Description / Table of Contents: Translation of the abstract: The materials of the XIII session of the Scientific Council on Tectonics of Siberia and the Far East (Yakutsk, 1980) are presented. The issues of the current state of theoretical geotectonics and the patterns of formation of the earth's crust in the Precambrian and Phanerozoic are considered in detail. New materials on the regional tectonics of platform and mobile regions of Siberia and the Far East of the USSR are presented. The presented models of the structure and evolution of the earth's crust sufficiently reflect the current state of theoretical geotectonics. The collection is intended for a wide range of geologists.
    Type of Medium: Monograph available for loan
    Pages: Seiten , Illustrationen
    Series Statement: Tektonika Sibiri / Akademija Nauk SSSR, Sibirskoe Otdelenie, Naučnyj Sovet po Tektonike Sibiri i Dalʹnego Vostoka Tom 11
    Language: Russian
    Note: СОДЕРЖАНИЕ Предисловие Теоретические вопросы геотектоники Некоторые методологические вопросы геологии / Ю. А. Косыгин Краткий методологический анализ современных глобальных тектонических гипотез / В. Ю. Забродин Главные этапы эволюции процесса рифтогенеза в истории Земли / Е. E. Милановский Закономерности формирования континентальной земной коры / М. С. Марков, Ю. М. Пущаровский Структурно-формационные парагенезы как индикаторы стадийности формирования континентальной коры / Б. М. Чиков Сдвиги и трансформные разломы литосферы / С. И. Шерман Структурная эволюция геосинклинальных складчатых систем / В. С. Буртмаи Механизм образования складчатости и ее морфология / А. В. Вихерт О формировании и локализации концентрических комплексов в связи с развитием разломов / Ю. А. Косыгин, В. В. Юшманов, Л. А. Маслов О тектонике и минерагении Восточной Сибири и Дальнего Востока / Л. И. Красный Становление земной коры в докембрии О процессах, образующих и преобразующих земную кору континентального типа / Ч. Б. Борукаев Закономерности формирования земной коры континентов в нижнем докембрии / М. А. Гилярова Особенности тектонического развития подвижных зон Гондваны и Евразии в позднем докембрии / Н. А. Божко Главные этапы становления континентальиой земной коры / В. И. Шульдинер Тентоника и этапы становления земной коры территории Янутии / Г. С. Гусев, Г. А. Гринберг, В. В. Ковальский, Б. В. Олейников, А. Ф. Петров, Г. С. Фрадкии, Н. В. Черский Модели строения и глубинной эволюции коры юго-востока Сибирской платформы / Л. П. Карсаков, Ю. Ф. Малышев Эволюция слоев земной коры в геологической истории архея Алданского щита / И. М. Фрумкин К проблеме пангеосинклинали / Р. Ф. Черкасов Этапы формирования земной коры Алданского щита в докембрии / Л. М. Реутов, А. Ф. Петров Этапы формирования земной коры и докембрийский рифтогенез на северо-востоке Сибирской платформы / Б. Р. Шпунт, Д. В. Аброскин, Ю. Х. Протопопов Этапы и факторы становления континентальной коры на территории Восточной Сибири / А. А. Бухаров К проблеме происхождения среднепротерозойских грабенов юго-востока Сибирской платформы и ее складчатого обрамления / А. А. Константиновский Тектоника платформенных областей Геоблоки Сибири и этапы их формирования / Е. П. Миронюк, И. А. Загрузииа Соотношение структурных этажей - критерий тектонического районироnания платформенных областей / К. И. Микуленко, В. С. Старосельцев, Г. С. Фрадкин Общая корреляция эндогенных процессов на Сибирской платформе / С. М. Замараев О мантийных абиссолитах и природе сводовых поднятий на древних платформах / П. Ф. Иванкин, А. А. Фельдман Становление земной коры молодых плит и ранние этапы их развития (на примере Западно-Сибирского сеrмента) / В. С. Бочкарев Тектоника подвижных областей Офиолитовые зоны палеозоид Казахстана и геодинамические реконструкции / Е. И. Паталаха Современная тектоника Байкальской рифтовой системы и концепция тектоники плит / В. П. Солоненко Современные представления о глубинном строении северо-восточноrо фланга Байкальской рифтовой зоны / М. М. Мандельбаум, И. П. Шпак Пространственно-временные связи и геодинамические соотношения мезозойских структур на Алданском щите и в Джугджуро-Становой области / В. Г. Ветлужских Офиолиты и олистостромы Верхояно-Колымской складчатой системы / Ю. В. Архипов, И. Г. Волкодав Литосферные плиты в Верхояно-Чукотской складчатой области / В. Б Спектор Структура и геодинамика Курило-Камчатскоrо желоба / Г. С. Гнибиденко, Т. Г. Быкова, О. В. Веселов, В. М. Воробьев, А. С. Сваричевский Литература , Translation of Contents Preface Theoretical issues of geotectonics Some methodological issues of geology / Yu. A. Kosygin Brief methodological analysis of modern global tectonic hypotheses / V. Yu. Zabrodin The main stages of the evolution of the rifting process in the history of the Earth / E. E. Milanovsky Patterns of formation of the continental crust / M. S. Markov, Yu. M. Pushcharovsky Structural-formational parageneses as indicators of the stages of formation of the continental crust / B. M. Chikov Shifts and transform faults of the lithosphere / S. I. Sherman Structural evolution of geosynclinal folded systems / V. S. Burtmai The mechanism of formation of folding and its morphology / A. V. Wikhert On the formation and localization of concentric complexes in connection with the development of faults / Yu. A. Kosygin, V. V. Yushmanov, L. A. Maslov On tectonics and minerageny of Eastern Siberia and the Far East / L. I. Krasny Formation of the earth's crust in the Precambrian On the processes that form and transform the earth's crust of continental type / Ch. B. Borukaev Patterns of formation of the continental crust in the Lower Precambrian / M. A. Gilyarova Features of the tectonic development of mobile zones of Gondwana and Eurasia in the Late Precambrian / N. A. Bozhko The main stages of the formation of the continental crust / V. I. Shuldiner Tentonics and stages of formation of the earth's crust in the territory of Janutia / G. S. Gusev, G. A. Grinberg, V. V. Kovalsky, B. V. Oleinikov, A. F. Petrov, G. S. Fradkii, N. V. Chersky Models of the structure and deep evolution of the crust of the southeast of the Siberian Platform / L. P. Karsakov, Yu. F. Malyshev Evolution of layers of the earth’s crust in the geological history of the Archean of the Aldan Shield / I. M. Frumkin On the problem of pangeosyncline / R. F. Cherkasov Stages of formation of the earth's crust of the Aldan shield in the Precambrian / L. M. Reutov, A. F. Petrov Stages of crust formation and Precambrian rifting in the northeast of the Siberian Platform / B. R. Shpunt, D. V. Abroskin, Yu. Kh. Protopopov Stages and factors of formation of the continental crust in Eastern Siberia / A. A. Bukharov On the problem of the origin of Middle Proterozoic grabens in the southeast of the Siberian Platform and its folded framing / A. A. Konstantinovsky Tectonics of platform areas Geoblocks of Siberia and stages of their formation / E. P. Mironyuk, I. A. Zagruzia The ratio of structural floors is a criterion for tectonic zoning of platform areas / K. I. Mikulenko, V. S. Staroseltsev, G. S. Fradkin General correlation of endogenous processes on the Siberian platform / S. M. Zamaraev On mantle abysolites and the nature of arched uplifts on ancient platforms / P. F. Ivankin, A. A. Feldman Formation of the earth's crust of young plates and early stages of their development (using the example of West Siberian cement) / V. S. Bochkarev Tectonics of mobile regions Ophiolite zones of the paleozoids of Kazakhstan and geodynamic reconstructions / E. I. Patalakha Modern tectonics of the Baikal rift system and the concept of plate tectonics / V. P. Solonenko Modern ideas about the deep structure of the northeast flank of the Baikal rift zone / M. M. Mandelbaum, I. P. Shpak Spatio-temporal connections and geodynamic relationships of Mesozoic structures on the Aldan shield and in the Dzhugdzhur-Stanovoy region / V. G. Vetluzhskikh Ophiolites and olistostromes of the Verkhoyansk-Kolyma fold system / Yu. V. Arkhipov, I. G. Volkodav Lithospheric plates in the Verkhoyansk-Chukotka folded region / V. B Spektor Structure and geodynamics of the Kuril-Kamchatka trench / G. S. Gnibidenko, T. G. Bykova, O. V. Veselov, V. M. Vorobyov, A. S. Svarichevsky Literature , In kyrillischer Schrift
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  • 63
    Call number: 9783034803960 (e-book)
    Type of Medium: 12
    Pages: 1 Online-Ressource (XI, 220 Seiten) , Illustrationen
    ISBN: 9783034803960 (e-book) , 978-3-0348-0396-0
    Language: English
    Note: Contents 1 High elevation treelines 1.1 The task 1.2 Previous works 2 Definitions and conventions 2.1 The life form ‘tree’ 2.2 Lines and transitions 2.3 Limitation, stress and disturbance 2.4 Altitude-related and other environmental drivers 2.5 Treeline nomenclature 3 Treeline patterns 3.1 Treeline taxa 3.2 The summit syndrome and other treeline depressions 3.3 Mass elevation effect 3.4 Treeline elevation 3.5 Time matters 3.6 Forest structure near treeline 4 Treeline climate 4.1 Specific aspects of treeline climatology 4.2 Criteria to define temperature regimes at treeline 4.3 Treeline temperatures in different bioclimatic regions 4.3.1 Subarctic and boreal zone (45–68° N) 4.3.2 Cool temperate zone (45–47° N, 44° S) 4.3.3 Warm temperate zone (28–42° N, 36° S) 4.3.4 Subtropical zone (19° S, 19° N) 4.3.5 Equatorial tropics (6° N to 3° S) 4.3.6 Mediterranean ‘treelines’ (38–42° N) 4.3.7 The Nothofagus and Metrosideros case 4.3.8 Treeline temperatures across bioclimatic zones 4.4 Seedbed and branch temperatures 4.5 Whole forest temperatures 5 Global mountain statistics based on treeline elevation 5.1 Mountain geostatistics 5.2 Elevational belts 5.3 Global treeline ecotones 6 Structure and stature of treeline trees 6.1 Foliage properties 6.2 Wood properties 6.3 Bark properties 6.4 Root traits 6.5 Tree stature 6.6 Dry matter allocation in treeline trees 7 Growth and development 7.1 Tree growth near the treeline 7.1.1 In situ growth of seedlings 7.1.2 In situ growth of saplings and adult trees 7.2 Xylogenesis at the treeline 7.2.1 In situ cambial activity 7.2.2 Apical growth dynamics 7.3 Root growth 7.4 Phenology at the treeline 8 Evolutionary adjustments to life at the treeline 8.1 Phylogenetic selection 8.2 Genotypic responses of growth and development 8.3 Genotypic responses of physiological traits 9 Reproduction, early life stages and tree demography 9.1 Amount and quality of seeds at high elevation 9.2 Germination, seedling and sapling stage 9.3 Tree demography at the treeline 10 Freezing and other forms of stress 10.1 Stress at the treeline in a fitness context 10.2 Mechanisms and principles of freezing resistance 10.3 Freezing resistance in treeline trees 10.4 Other forms of stress at the treeline 10.4.1 Freeze-thaw cycles and hydraulic failure 10.4.2 Winter desiccation 11 Water, nutrient and carbon relations 11.1 Tree water relations during the growing season 11.2 Nutrient relations 11.3 Carbon relations 12 Treeline formation - currently, in the past and in the future 12.1 Causes of current treelines 12.2 Treelines in the recent past 12.3 Treelines in the distant past (Holocene) 12.4 Treelines in the future References Subject Index Taxonomic Index
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  • 64
    Call number: AWI G3-23-95566
    In: Trudy Instituta Geologii i Geofiziki, Vypusk 511
    Description / Table of Contents: Монография является первой полной петрохимической характеристикои осадочно-метаморфических пород среднего и верхнего докембрия западной окраины Сибирской платформы (Игарского и Туруханского поднятий Енисейского кряжа и центральной части Восточного Саяна). На основе единой методики литолого-rеохимического изучения и опробования осадочно-метаморфических пород и большого количества новых аналитических данных (более 2000 полных химических анализов пород) рассмотрены стратиграфия, фациальные условия накопления, литологические, петрохимические, геохимические особенности и металлогеническая специализация средне- и верхнедокембрийских отложений а также влияние на них регионального и контактового метаморфизма. Книга представляет большой интерес для широкого круга геологов и геохимиков занимающихся изучением докембрия.
    Description / Table of Contents: Translation of the abstract: The monograph is the first complete petrochemical description of sedimentary-metamorphic rocks of the Middle and Upper Precambrian of the western margin of the Siberian Platform (Igarsky and Turukhansky uplifts of the Yenisei Ridge and the central part of the Eastern Sayan). Based on a unified methodology for lithological-reochemical study and sampling of sedimentary-metamorphic rocks and a large amount of new analytical data (more than 2000 complete chemical analyzes of rocks), stratigraphy, facies conditions of accumulation, lithological, petrochemical, geochemical features and metallogenic specialization of Middle and Upper Precambrian deposits are considered. also the influence of regional and contact metamorphism on them. The book is of great interest to a wide range of geologists and geochemists involved in the study of the Precambrian.
    Type of Medium: Series available for loan
    Pages: 205 Seiten , Illustrationen
    Series Statement: Trudy Instituta Geologii i Geofiziki 511
    Language: Russian
    Note: ОГЛАВЛЕНИЕ От редактора Прелисловие Распределение и краткая характеристика докембрийских отложений западного обрамления Сибирскои платформы Основные черты стратиграфии и nетрохимии покембрия западпого обрамления Сибирской платформы Докембрий Енисейского кряжа Докембрий Туруханского поднятия Докембрий Игарского поднятия Докембрий Бирюсинского района Центральвои части Восточного Саяна Литолого-фациальные комплексы осадочно метаморфических толщ докембрия западного обрамления Сибирскои платормы Приложения Литература , Translation of Table of Contents TABLE OF CONTENTS From the editor Preface Distribution and brief characteristics of Precambrian deposits of the western framing of the Siberian Platform Main features of stratigraphy and petrochemistry of the Pokembrian western frame of the Siberian Platform Precambrian of the Yenisei Ridge Precambrian of the Turukhansk uplift Precambrian of the Igara uplift Precambrian of the Biryusinsky district of the Central part of the Eastern Sayan Lithological-facies complexes of Precambrian sedimentary-metamorphic strata of the western framing of the Siberian plateau Applications Literature , In kyrillischer Schrift
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  • 65
    facet.materialart.12
    Boca Raton, FL : CRC Press
    Call number: 9781420073072 (e-book)
    Description / Table of Contents: As we discover more about the role of the ocean in global changes and identify the effects of global change on the ocean, understanding its chemical composition and processes becomes increasingly paramount. However, understanding these processes requires a wide range of measurements in the vast ocean, from the sea surface to deep-ocean trenches, from the tropics to the poles. Practical Guidelines for the Analysis of Seawater provides a common analytical basis for generating quality-assured and reliable data on chemical parameters in the ocean. A source of practical know-how, the book covers sampling and storage, analytical methodology, and guidelines and procedures for quality assurance. It presents analytical methods with the step-by-step procedures that help practitioners implement these methods successfully into the laboratory, making them instantly applicable without consulting further literature. The book also contains essential information for developing or improving quality control and quality assurance programs in the laboratory. It includes the availability and measurement of standard reference materials, blank estimation and correction, control of recoveries, and statistical evaluation of quality assurance data. Analytical chemistry is a very active and fast moving area. Despite the development of innovative new analytical techniques for chemical trace element research, obtaining reliable data at ultra-trace levels remains a formidable challenge. A complete and practical guide, this book delineates proven methods that consistently yield reproducible data in routine work.
    Type of Medium: 12
    Pages: 1 Online-Ressource (xii, 401 Seiten) , Illustrationen, Diagramme
    ISBN: 978-1-4200-7307-2 , 9781420073072
    Series Statement: Environmental science and technology
    Language: English
    Note: Contents Preface Editor Contributors Chapter 1 Sampling and Sample Treatments / Oliver Wurl Chapter 2 Analysis of Dissolved and Particulate Organic Carbon with the HTCO Technique / Oliver Wurl and Tsai Min Sin Chapter 3 Spectrophotometric and Chromatographic Analysis of Carbohydrates in Marine Samples / Christos Panagiotopoulos and Oliver Wurl Chapter 4 The Analysis of Amino Acids in Seawater / Thorsten Dittmar, Jennifer Cherrier, and Kai-Uwe Ludwichowski Chapter 5 Optical Analysis of Chromophoric Dissolved Organic Matter / Norman B. Nelson and Paula G. Coble Chapter 6 Isotope Composition of Organic Matter in Seawater / Laodong Guo and Ming-Yi Sun Chapter 7 Determination of Marine Gel Particles / Anja Engel Chapter 8 Nutrients in Seawater Using Segmented Flow Analysis / Alain Aminot, Roger Kérouel, and Stephen C. Coverly Chapter 9 Dissolved Organic and Particulate Nitrogen and Phosphorous / Gerhard Kattner Chapter 10 Pigment Applications in Aquatic Systems / Karen Helen Wiltshire Chapter 11 Determination of DMS, DMSP, and DMSO in Seawater / Jacqueline Stefels Chapter 12 Determination of Iron in Seawater / Andrew R. Bowie and Maeve C. Lohan Chapter 13 Radionuclide Analysis in Seawater / Mark Baskaran, Gi-Hoon Hong, and Peter H. Santschi Chapter 14 Sampling and Measurements of Trace Metals in Seawater / Sylvia G. Sander, Keith Hunter, and Russell Frew Chapter 15 Trace Analysis of Selected Persistent Organic Pollutants in Seawater / Oliver Wurl Chapter 16 Pharmaceutical Compounds in Estuarine and Coastal Waters / John L. Zhou and Zulin Zhang Appendix A: First Aid for Common Problems with Typical Analytical Instruments Appendix B: Chemical Compatibilities and Physical Properties of Various Materials Appendix C: Water Purification Technologies
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  • 66
    facet.materialart.12
    Chichester, [England] : Wiley
    Call number: 9781444328479 (e-book)
    Type of Medium: 12
    Pages: 1 Online-Ressource (XIII, 768 Seiten) , Illustrationen
    Edition: Second edition
    ISBN: 9781444328479 (e-book) , 978-1-4443-2847-9
    Language: English
    Note: Contents Contents Preface Acknowledgements Part 1: Making Sediment Introduction Clastic sediment as a chemical and physical breakdown product 1.1 Introduction: clastic sediments—'accidents' of weathering 1.2 Silicate minerals and chemical weathering 1.3 Solute flux: rates and mechanisms of silicate chemical weathering 1.4 Physical weathering 1.5 Soils as valves and filters for the natural landscape 1.6 Links between soil age, chemical weathering and weathered-rock removal 1.7 Provenance: siliciclastic sediment-sourcing Further reading 2 Carbonate, siliceous, iron-rich and evaporite sediments 2.1 Marine vs. freshwater chemical composition and fluxes 2.2 The calcium carbonate system in the oceans 2.3 Ooid carbonate grains 2.4 Carbonate grains from marine plants and animals 2.5 Carbonate muds, oozes and chalks 2.6 Other carbonate grains of biological origins 2.7 Organic productivity, sea-level and atmospheric controls of biogenic CaCO3 deposition rates 2.8 CaCO3 dissolution in the deep ocean and the oceanic CaCO3 compensation mechanism 2.9 The carbonate system on land 2.10 Evaporite salts and their inorganic precipitation as sediment 2.11 Silica and pelagic plankton 2.12 Iron minerals and biomineralizers 2.13 Desert varnish 2.14 Phosphates 2.15 Primary microbial-induced sediments: algal mats and stromatolites Further reading 3 Sediment grain properties 3.1 General 3.2 Grain size 3.3 Grain-size distributions 3.4 Grain shape and form 3.5 Bulk properties of grain aggregates Further reading Part 2: Moving Fluid Introduction 4 Fluid basics 4.1 Material properties of fluids 4.2 Fluid kinematics 4.3 Fluid continuity with constant density 4.4 Fluid dynamics 4.5 Energy, mechanical work and power Further reading 5 Types of fluid motion 5.1 Osborne Reynolds and flow types 5.2 The distribution of velocity in viscous flows: the boundary layer 5.3 Turbulent flows 5.4 The structure of turbulent shear flows 5.5 Shear flow instabilities, flow separation and secondary currents 5.6 Subcritical and supercritical flows: the Froude number and hydraulic jumps 5.7 Stratified flow generally 5.8 Water waves 5.9 Tidal flow—long-period waves Further reading Part 3: Transporting Sediment Introduction 6 Sediment in fluid and fluid flow—general 6.1 Fall of grains through stationary fluids 6.2 Natural flows carrying particulate material are complex 6.3 Fluids as transporting machines 6.4 Initiation of grain motion 6.5 Paths of grain motion 6.6 Categories of transported sediment 6.7 Some contrasts between wind and water flows 6.8 Cohesive sediment transport and erosion 6.9 A warning: nonequilibrium effects dominate natural sediment transport systems 6.10 Steady state, deposition or erosion: the sediment continuity equation and competence vs. capacity Further reading 7 Bedforms and sedimentary structures in flows and under waves 7.1 Trinity of interaction: turbulent flow, sediment transport and bedform development 7.2 Water-flow bedforms 7.3 Bedform phase diagrams for water flows 7.4 Water flow erosional bedforms on cohesive beds 7.5 Water wave bedforms 7.6 Combined flows: wave-current ripples and hummocky cross-stratification 7.7 Bedforms and structures formed by atmospheric flows Further reading 8 Sediment gravity flows and their deposits 8.1 Introduction 8.2 Granular flows 8.3 Debris flows 8.4 Turbidity flows 8.5 Turbidite evidence for downslope transformation from turbidity to debris flows Further reading 9 Liquefaction, fluidization and sliding sediment deformation 9.1 Liquefaction 9.2 Sedimentary structures formed by and during liquefaction 9.3 Submarine landslides, growth faults and slumps 9.4 Desiccation and synaeresis shrinkage structures Further reading Part 4: Major External Controls on Sedimentation and Sedimentary Environments Introduction 10 Major external controls on sedimentation 10.1 Climate 10.2 Global climates: a summary 10.3 Sea-level changes 10.4 Tectonics 10.5 Sediment yield, denudation rate and the sedimentary record Further reading Part 5: Continental Sedimentary Environments Introduction 11 Rivers 11.1 Introduction 11.2 River networks, hydrographs,patterns and long profiles 11.3 Channel form 11.4 Channel sediment transport processes, bedforms and internal structures 11.5 The floodplain 11.6 Channel belts, alluvial ridges and avulsion 11.7 River channel changes, adjustable variables and equilibrium 11.8 Alluvial architecture: product of complex responses 11.9 Alluvial architecture: scale, controls and time Further reading 12 Subaerial Fans: Alluvial and Colluvial 12.1 Introduction 12.2 Controls on the size (area) and gradient of fans 12.3 Physical processes on alluvial fans 12.4 Debris-flow-dominated alluvial fans 12.5 Stream-flow-dominated alluvial fans 12.6 Recognition of ancient alluvial fans and talus cones Further reading 13 Aeolian Sediments in Low-Latitude Deserts 13.1 Introduction 13.2 Aeolian system state 13.3 Physical processes and erg formation 13.4 Erg margins and interbedform areas 13.5 Erg and draa evolution and sedimentary architecture 13.6 Erg construction, stasis and destruction: climate and sea-level controls 13.7 Ancient desert facies Further reading 14 Lakes 14.1 Introduction 14.2 Lake stratification 14.3 Clastic input by rivers and the effect of turbidity currents 14.4 Wind-forced physical processes 14.5 Temperate lake chemical processes and cycles 14.6 Saline lake chemical processes and cycles 14.7 Biological processes and cycles 14.8 Modern temperate lakes and their sedimentary facies 14.9 Lakes in the East African rifts 14.10 Lake Baikal 14.11 The succession of facies as lakes evolve 14.12 Ancient lake facies Further reading 15 Ice 15.1 Introduction 15.2 Physical processes of ice flow 15.3 Glacier flow, basal lubrication and surges 15.4 Sediment transport, erosion and deposition by flowing ice 15.5 Glacigenic sediment: nomenclature and classification 15.6 Quaternary and modern glacial environments and facies 15.7 Ice-produced glacigenic erosion and depositional facies on land and in the periglacial realm 15.8 Glaciofluvial processes on land at and within the ice-front 15.9 Glacimarine environments 15.10 Glacilacustrine environments 15.11 Glacial facies in the pre-Quaternary geological record: case of Cenozoic Antarctica Further reading Part 6: Marine Sedimentary Environments Introduction 16. Estuaries 16.1 Introduction 16.2 Estuarine dynamics 16.3 Modern estuarine morphology and sedimentary environments 16.4 Estuaries and sequence stratigraphy Further reading 17. River and Fan Deltas 17.1 Introduction to river deltas 17.2 Basic physical processes and sedimentation at the river delta front 17.3 Mass movements and slope failure on the subaqueous delta 17.4 Organic deposition in river deltas 17.5 River delta case histories 17.6 River deltas and sea-level change 17.7 Ancient river delta deposits 17.8 Fan deltas Further reading 18. Linear Siliciclastic Shorelines 18.1 Introduction 18.2 Beach processes and sedimentation 18.3 Barrier-inlet-spit systems and their deposits 18.4 Tidal flats, salt marsh and chenier ridges 18.5 Ancient clastic shoreline facies Further reading 19 Siliciclastic Shelves 19.1 Introduction: shelf sinks and lowstand bypass 19.2 Shelf water dynamics 19.3 Holocene highstand shelf sediments: general 19.4 Tide-dominated, low river input, highstand shelves 19.5 Tide-dominated, high river input, highstand shelves 19.6 Weather-dominated highstand shelves Further reading 20 Calcium-carbonate-evaporite Shorelines, Shelves and Basins 20.1 Introduction: calcium carbonate 'nurseries' and their consequences 20.2 Arid carbonate tidal flats, lagoons and evaporite sabkhas 20.3 Humid carbonate tidal flats and marshes 20.4 Lagoons and bays 20.5 Tidal delta and margin-spillover carbonate tidal sands 20.6 Open-shelf carbonate ramps 20.7 Platform margin reefs and carbonate build-ups 20.8 Platform margin slopes and basins 20.9 Carbonate sediments, cycles and sea-level change 20.10 Displacement and destruction of carbonate environments: silicicl
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    Call number: AWI G3-24-95721
    Description / Table of Contents: Included in this book are papers on a wide range of problems of geology of the Cenozoic of Yacutia - stratigraphy, paleogeography, structural geomorphology, neotectonics, glaciations, as well as on main stages of man population of Yakutia. The collection of papers is published for the Xlth INQUA Congress. The book is of interest to those dealing with the Cenozoic history of Yakutia and the North-East USSR.
    Description / Table of Contents: В сборнике помещены статьи по широкому кругу вопросов геологии кайнозоя Якутии - стратиграфии, палеогеографии, структурной геоморфологии, неотектонике, оледенениям, а также основным этапам заселения человеком территории Якутии. Сборник издается к XI Конгрессу Международного союза по изучению четвертичного периода. Книга представляет интерес для специалистов, занимающихся кайнозойской историей Якутии и Северо-Востока СССР.
    Type of Medium: Monograph available for loan
    Pages: 173 Seiten , Illustrationen, Karten
    Language: Russian
    Note: CONTENTS Preface Problems of stratigraphy and paleogeography of the Quaternary of Yakutia / M. N. AIekseyev Regional stratigraphic scheme of the Paleogene and Neogene sediments of the Lower-Aldan depression / A. F. Fradkina, O. V. Grinenko, V. A. Kamaletdinov, A. I. Tomskaya Paleomagnetic studies of the upper section of the Mamontova Gora on the Aldan-river / P. S. Minyuk New data on stratigraphy of the Cencizoic of the eastern part of the Primorsk lowland / L. P. Zharikova, A. S. Kazantsev, P. S. Minyuk, A. G. Savchenko Cenozoik sediments of the Ulakhan-Tas range / A. I. Sergeyenko, A. S. Kazantsev, Yu. V. Lykov, A. I. Tomskaya Small mammals in the key section of the Pliocene-Quaternary sediments on the Krestovka-river (Kolyma lowland) / G. G. FroIova Recent tectonics of Eastern Yakutia / V. B. Spector, V. A. BaIandin Structural-geomorphological character of the Kolyma lowland / N. G. Patyk-Kara, O. I. Gapon, O. V. Grinenko Modern tectonic stress field of North-East Asia / B. M. Koz'min Quantitative evalution of recent vertical tectonic movements in North-Eastern Yakutia / L. P. Imayeva, V. S. Imayev Basement relief and Quaternary cover structure in the Lena-Amga interfluve / V. A. KamaIetdinov Paleomorphological conditions during the formation of Cenozoik conglomerates on the right bank of the Selennyakh river (Indigirka basin) / L. A. Fatkhullin "Alas" sediments and taber formations of Yakutia / Ye. M. Katasonov Slope sediments in river valleys of Central Yakutia / Ye. G. Katasonova, H. G. Ziegert On differentiating the Neogene-Quaternary perennially frozen rocks by mineral composition and cryogenic microstructures / H. G. Ziegert, Ye. A. Slagoda On estimation of the amount of glaciations using different criteria (in the light of' the near-Indigirka zone) / E. D. Izbekov Glacial isostasy in Priverkhoyanie / V. V. KoIpakov, I. L. Shofman Main stages of man population in Yakutia / Yu. A. Mochanov, S. A. Fedoseyeva , СОДЕРЖАНИЕ Предисловие Проблемы стратиграфии и палеогеографии четвертичного периода Якутии / М. Н. Алексеев Региональная стратиграфическая схема палеогеновых и неогеновых отложений Нижнеалданской впадины / А. Ф. Фрадкина, О. В. Гриненко, В. А. Камалетдинов, А. И. Томская Палеомагнитные исследования верхней части разреза Мамонтова Гора на реке Алдан / П. С. Минюк Новые сведения по стратиграфии кайнозоя восточнои части Приморской низменности / Л . П. Жарикова, А. С. Казанцев, П. С. Минюк, А. Г. Савченко Кайнозойские отложения хребта Улахан-Тас / А . И. Сергеенко, А. С. Казанцев, Ю. В. Лыков, А. И. Томская Мелкие млекопитающие опорного разреза плиоцен-четвертичных отложении на реке Крестовке (Колымская низменность) / Г. Г. Фролова Новейшая тектоника Восточной Якутии / В. Б. Спектор, В. А. Баландин Структурно-геоморфологическое строение Колымском низменности / Н. Г. Патык-Кара, О. И. Гапон, О. В. Гриненко Современное поле тектонических напряжении Северо-Восточной Азии / Б. М. Козьмин Количественная оценка новеиших вертикальных тектонических движений Северо-Востока Якутии / Л. П. Имаева, В. С. Имаев Рельеф цоколя и строение четвертичного покрова Лено-Амгинского междуречья / В. А. Камалетдинов Палеогеоморфологические условия формирования кайнозойских конгломератов правобережья реки Селениях (бассейн реки Индигирки) / И. А. Фатхуллин Аласные отложения и таберальные образования Якутии / Е. М. Катасонов Склоновые отложения в долинах малых рек Центральной Якутии / Е. Г. Катасонова, Х . Г. 3игерт О расчленении многолетнемерзлых неоrен-четвертцчных отложений по минералогическому составу и криогенным микротекстурам / Х . Г. 3игерт, Е . А. Слагода К вопросу оценки количества оледенений по различным критериям (на примере Прииндиrирской зоны) / Э. Д. Избеков Гляциоизостазия в Приверхоянье / В. В. Колпаков, И. Л. Шофман Основные этапы заселения человеком Якутии / Ю. А. Мочанов, С. А. Федосеева , In kyrillischer Schrift
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  • 68
    Call number: AWI Bio-24-95729
    Type of Medium: Monograph available for loan
    Pages: XIV, 354 Seiten , Illustrationen
    ISBN: 0195154312 , 9780195154313 , 978-0-19-515431-3
    Series Statement: Long-Term Ecological Research Network Series
    Language: English
    Note: Contents Contributors Part I. Alaska's Past and Present Environment 1. The Conceptual Basis of LTER Studies in the Alaskan Boreal Forest / F. Stuart Chapin III, john Yarie, Keith Van Cleve, and Leslie A. Viereck 2. Regional Overview of Interior Alaska / James E. Beget, David Stone, and David L Verbyla 3. State Factor Control of Soil Formation in Interior Alaska / Chien-Lu Ping, Richard D. Boone, Marcus H. Clark, Edmond C. Packee, and David K. Swanson 4. Climate and Permafrost Dynamics of the Alaskan Boreal Forest / Larry D. Hinzman, Leslie A. Viereck, Phyllis C. Adams, Vladimir E. Romanovsky, and Kenji Yoshikawa 5. Holocene Development of the Alaskan Boreal Forest / Andrea H. Lloyd, Mary E. Edwards, Bruce P. Finney, Jason A. Lynch, Valerie Barber, and Nancy H. Bigelow Part II. Forest Dynamics 6. Floristic Diversity and Vegetation Distribution in the Alaskan Boreal Forest / F. Stuart Chapin III, Teresa Hollingsworth, David F. Murray, Leslie A. Viereck, and Marilyn D. Walker 7. Successional Processes in the Alaskan Boreal Forest / F. Stuart Chapin III, Leslie A. Viereck, Phyllis C. Adams, Keith Van Cleve, Christopher L. Fastie, Robert A. Ott, Daniel Mann, and Jill F. Johnstone 8. Mammalian Herbivore Population Dynamics in the Alaskan Boreal Forest / Eric Rexstad and Knut Kielland 9. Dynamics of Phytophagous Insects and Their Pathogens in Alaskan Boreal Forests / Richard A. Werner, Kenneth F. Raffa, and Barbara L. Illman 10. Running Waters of the Alaskan Boreal Forest / Mark W. Oswood, Nicholas F. Hughes, and Alexander M. Milner Part III. Ecosystem Dynamics 11. Controls over Forest Production in Interior Alaska / John Yarie and Keith Van Cleve 12. The Role of Fine Roots in the Functioning of Alaskan Boreal Forests / Roger W. Ruess, Ronald L. Hendrick, Jason C. Vogel, and Bjartmar Sveinbjornsson 13. Mammalian Herbivory, Ecosystem Engineering, and Ecological Cascades in Alaskan Boreal Forests / Knut Kielland, John P. Bryant, and Roger W. Ruess 14. Microbial Processes in the Alaskan Boreal Forest / Joshua P. Schimel and F. Stuart Chapin III 15. Patterns of Biogeochemistry in Alaskan Boreal Forests / David W. Valentine, Knut Kielland, F. Stuart Chapin III, A. David McCuire, and Keith Van Cleve Part IV. Changing Regional Processes 16. Watershed Hydrology and Chemistry in the Alaskan Boreal Forest: The Central Role of Permafrost / Larry D. Hinzman, W. Robert Bolton, Kevin C. Petrone, Jeremy B. Jones, and Phyllis C. Adams 17. Fire Trends in the Alaskan Boreal Forest / Eric S. Kasischke, T. Scott Rupp, and David L. Verbyla 18. Timber Harvest in Interior Alaska / Tricia L. Wurtz, Robert A. Ott, and John C. Maisch 19. Climate Feedbacks in the Alaskan Boreal Forest / A. David McCuire and F. Stuart Chapin III 20. Communication of Alaskan Boreal Science with Broader Communities / Elena B. Sparrow, Janice C. Dawe, and F. Stuart Chapin III 21. Summary and Synthesis: Past and Future Changes in the Alaskan Boreal Forest / F. Stuart Chapin III, A. David McCuire, Roger W. Ruess, Marilyn W. Walker, Richard D. Boone, Mary E. Edwards, Bruce P. Finney, Larry D. Hinzman, Jeremy B. Jones, Clenn P. Juday, Eric S. Kasischke, Knut Kielland, Andrea H. Lloyd, Mark W. Oswood, Chien-Lu Ping, Eric Rexstad, Vladimir E. Romanovsky, Joshua P. Schimel, Elena B. Sparrow, Bjartmar Sveinbjornsson, David W. Valentine, Keith Van Cleve, David L. Verbyla, Leslie A. Viereck, Richard A. Werner, Tricia L. Wurtz, and John Yarie Index
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  • 69
    Monograph available for loan
    Monograph available for loan
    Jakutsk : Inst. Merzlotovedenija
    Call number: AWI G3-16-90233
    Type of Medium: Monograph available for loan
    Pages: 164 S.
    Language: Russian
    Note: In kyrill. Schr.
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  • 70
    Call number: ZSP-980-89 ; ZSP-980-89(2. Ex.)
    In: ZfI-Mitteilungen ; 89, Nr. 89
    Type of Medium: Series available for loan
    Pages: 132 S. , Ill., graph. Darst., Kt.
    ISSN: 0323-8776
    Series Statement: ZfI-Mitteilungen 89
    Language: English
    Note: Contents: Preface. - Tritium in Antarctic precipitation - information on global distribution / D. Hebert. - On the physical geography of the Schirmacher Oasis (East Antarctica, Dronning Maud Land) / W. Richter. - Investigation of Deuterium concentration relations between atmospheric water vapour and precipitations in the Schirmacher Oasis, East Antarctica / P. Kowski. - Isotope-hydrological and hydrochemical characterization of lakes in the Schirmacher Oasis (East Antarctica) / W. Richter, U. Wand, G. Strauch, P. Kowski, W. Kurze. - Isotope-hydrological and hydrochemical studies of the interior Antarctic lake "Untersee" in the Wohlthat Massif, Dronning Maud Land, East Antarctica / W.-D. Hermichen, M. Crelle, P. Kowski, W. Kurze, U. Wand. - The isotope-glaciological situation in the surroundings of the Schirmacher Oasis/Dronning Maud Land - a first overview / W.-D. Hermichen, P. Kowski, G. Strauch. - Radiocarbon dating of breeding places of petrels in the Antarctic / A. Hiller, U. Wand. - K - Ar dating of basalt dykes in the Schirmacher Oasis, Dronning Maud Land, East Antarctica / G. Kaiser, U. Wand.
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  • 71
    Call number: AWI A12-17-90537
    Type of Medium: Monograph available for loan
    Pages: 267 S. , Ill., graph. Darst.
    Language: Russian
    Note: Contents: Preface. - I. INSTRUMENT AND TECHNIQUES OF MEASUREMENTS OF OZONE, SOLAR ULTRAVIOLET AND CONSTITUENTS OF THE ATMOSPHERE INFLUENCING THE OZONE. MEASUREMENT RESULTS. - The set of measurements for optical observations of ozone and other constituents of the atmosphere influcencing the ozone / G. I. Kuznetzov. - Investigation of time variations of ozone / G. I. Kuznetzov. - Analytical aspects of atmospheric ozone and oxidants studies / L. N. Tchernyh, V. A. Popov, E. V. Pechennikova. - Results of the airborne measurements of total ozone and nitrogen dioxide / A. Ya. Arabov, N. F. Elansky, Yu. L. Truttse. - Rocket head design of meteorological rockets MR-12 and M-100B for measuring of optical characteristics of the upper atmosphere / N. I. Brezgin, E. A. Krohina, S. G. Linnik, A. F. Chijov, O. V. Shtirkov. - Simultaneous measurements of the vertical ozone distribution by rocket and goundbased spectrometric methods / P. F. Boychenko, N. I. Brezgin, G. I. Kuznetzov, A. F. Chijov, O. V. Shtirkov. - The apparatus and method for investigation of ozone-sensitive chemiluminescent detectors at low pressures / S. P. Perov, V. I. Konkov, V. A. Kononkov, L. A. Udonova. - On the application of the chemiluminescent method of the investigation of atmospheric ozone with the help of meteorological rocket M100-B / V. I. Konkov, S. P. Perov. - Water vapour distribution in the ozonosphere / A. V. Fedinsky, V. A. Yuskov. - Sounding rocket measurements of aerosol concentration in the atmosphere up to 90 km / T. I. Orishich. - Basic problems of automation of total ozone measurements and the results of development of automatic ozonometer / V. A. Bajenov, T. D. Jukovskaya, A. N. Otto. - Automatic calculation of the common maintance of atmospheric ozone by filter ozonometers by means of methods of analogue transformation of functions / V. A. Bajenov. - II. OZONOSPHERE CHEMISTRY. - Systems modelling of stratospheric ozone transport and photochemistry / I. L. Karol. - Numerical methods of global transport of freons in the atmosphere and assessment of their effect on ozone / I. L. Karol, V. V. Babanova, A. A. Kiselev, L. A. Romanovskaya. - The stratosphere photo-chemical model / I. G. Dyominov. - The impact of galactic cosmic rays and solar proton events upon the ozone layer / I. G. Dyominov. - Mechanism of cosmic rays effect on earth ozonosphere / P. S. Vinogradov, I. K. Larin, A. I. Poroykova, V. L. Talrose. - Qualitative estimation of some stratospheric reactions rates based on orbital symmetry conservation rules / P. S. Vinogradov, I. K. Larin, V. L. Talrose, O. A. Travina. - On starting prerequisites of mesospheric ozone photochemical theory / G. M. Martynkevich. - Studies of ozone in urban atmosphere as an indicator of photochemical processes / V. A. Popov, L. N. Tchernyh, E. V. Pechennikova. - On the use of silver thin films for measuring of atomic oxygen concentration in the upper atmosphere / S. J. Toktomishev. - On the photochemistry of ozone in the laser sounding of the stratosphere / A. P. Sukhorukov, I. M. Sizova. - Aerosols and ozone in the lower stratosphere / A. P. Bobrovsky, V. N. Ivanov, L. S. Ivlev, V. G. Sirota. - III. THE INTERELAXION OF PROCESSES IN OZONOSPHERE WITH HYDROMETEOROLOGICAL PHENOMENA. - Spatial distribution of atmospheric ozone concentration over the USSR in the upper troposphere and lower stratosphere as derived from aircraft measurements / S. V. Solonin, V. V. Osetchkin. - Variations of the total ozone content of ozone depending on the type of jet streams and their comlexes / V. G. Bakhtiyarov, L. I. Bordovskaya, B. D. Belan. - The stratospheric circulation change in spring and preceeding to it the change of total ozone field in autumn / L. A. Uranova. - Some results of the investigation of ozone vertical distribution in the atmosphere in connection with meteorological phenomena / D. V. Harchilava. - Ozone vertical profiles and the solar activity / P. F. Bojchenko, Yu. N. Rybin. - The effect of solar activity on the general circulation and thermal regime of the atmosphere / L. R. Rakipova. - Seasonal variations of total ozone in the stratospheric circumpolar vortex / V. J. Bekoryukov. - On the relation of the total amount of atmospheric ozone and the near-ground concentrations of radioactive isotopes / V. J. Lujanas, V. K. Jocius, P. K. Zinkevichus. - A certain low-governed nature of ozone, radioactive and nonradioactive aerosols and electric field intensity distribution in the lower troposphere / A. G. Amiranashvily, A. A. Aphaidze, A. Sh. Balavadze, A. G. Nodia, D. V. Harchilava. - On a certain relation between ozone content in the atmosphere and thunderstorm hail phenomena under the conditions of East Georgia / D. V. Harchilava, A. I. Kartsivadze, T. G. Gzirishvily. - On the changeobility of ozone content during the thunderstorm situation / A. I. Kartsivadze, D. V. Harchilava. - Variation of atmospheric ozone and some parameters of jet streams / N. N. Vinogradova. , In kyrill. Schr. , Zsfassungen in engl. Sprache
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  • 72
    Call number: AWI P4-17-91082
    Type of Medium: Monograph available for loan
    Pages: 296 S. , Ill., graph. Darst. , 25 cm
    Edition: 1. ed
    ISBN: 9780988462601
    Language: English
    Note: Contents: 1. Introduction. - 2. Current Practices. - 3. Drivers of Change. - 4. The Fuel Penalty. - 5. Underwater Hull Related Environmental Concerns. - 6. Regulatory Aspects. - 7. Hull Coating Systems Compared. - 8. A Better, Viable Alternative. - 9. In-water Ship Hull Cleaning. - 10. Propeller Cleaning. - 11. Rudder Protection. - 12. Case Studies. - 13. Conclusion. - Resources. - Glossary. - Index.
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  • 73
    Monograph available for loan
    Monograph available for loan
    Berlin : Nordeuropa-Inst. der Humboldt-Univ.
    Call number: AWI P5-17-91081
    Description / Table of Contents: Iceland, Greenland and the Faroe Islands have in common their history as Danish dependencies within a historically and geographically coherent region. The complex aftermaths of Denmark's sovereignty over its North Atlantic territories and their ongoing nation building processes lie at the core of this book. Today, we are witnessing region building processes beyond bilateral links to Denmark. How do the countries position themselves, individually and collectively, vis-à-vis the European metropolitan centres, a larger transcontinental North Atlantic region, the "hot" Arctic, and global histories of colonialism and decolonisation? By examining the region from cultural, literary, historical, political, anthropological and linguistic perspectives, the articles in this book shed light on Nordic colonialism and its understanding as "exceptional", and challenge and modify established notions of postcolonialism. Iceland, Greenland and the Faroe Islands are shown to be both the (former) subjects as well as the producers of cultural hierarchisations in an entangled world.
    Type of Medium: Monograph available for loan
    Pages: 422 S.
    Edition: 1. Aufl.
    ISBN: 9783932406355
    Series Statement: Berliner Beiträge zur Skandinavistik 20
    Language: English
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  • 74
    Call number: AWI G3-17-91084-2
    In: Kvarter vo vsem ego mnogoobrazii, Tom 2
    Type of Medium: Monograph available for loan
    Pages: 350 S. , Ill., graph. Darst., Kt.
    ISBN: 978-5-91918-124-8
    Language: Russian , English
    Note: TABLE OF CONTENTS: Contemporary hydrographic network of the North-East of the Russian Plain: chronology of development / A. S. Lavrov, L. M. Potapenko. - Some distinctions of big and smoll interglacials (by way of example of Western Siberia during Late Pleistocene) / S. A. Laukhin, A. M. Firsov. - Pollen spectra in the lithological facies of lake bottom sediment on the White Sea Coast / N. B. Lavrova, V. V. Kolka, O. P. Korsakova. - Barsova Gora is the unical object of glacial geology and Taiga vegetation in the middle Priobie / N. B. Levina, V. A. Tkachenko, V. N. Turin, N. N. Lavrovich, E. V. Shepetova. - Geological role of ice in formation of the Arctic Ocean recent and quaternary sediments composition / M. A. Levitan, K. V. Syromyatnikov. - Granite protrusions as a relief-forming factor of the activated sections of platforms and mobile belts / M. G. Leonov, E. S. Przhiyalgovsky. - Glacial tectonics and the granulated substance mechanics / M. G. Leonov, O. G. Epshtein. - Late Pliocene-Early Pleistocene lake sediments in hollow D'Issyk-kul / O. N. Leflat, T. N. Voskresenskaya. - Complexity and diversity of genetic indication of loose formations and new things in the methods of their identification (according to the results of research of small rivers' valleys of the North of Amur-Zeya Plain, Lower Amur Region and Western Priokhotye / E. Yu. Likutov. - Landscape-geological characteristic of travertine cascade of the ancient thermal source of tract pymvashor / A. A. Ljubas, J. N. Bolotov, M. Y. Gofarov, S. A. lglovskiy. - Lake's lithogenesis: new formations are on the bottom of the drying up Udinsky Streach / L. A. Magaeva, M. T. Ustinov. - Genetic classification of peat deposits based on trophicity degree / G. L. Makarenko. - On the issue of classification of mires based on trophicity degree / G. L. Makarenko. - Some burning issues of a structural interpretation of the plain areas relief / V. I. Makarov, N. V. Makarova, T. V. Sukhanova. - The first experience of the 230Th/U dating of buried wood remains / R. E. Maksimov, V. Yu. Kuznetsov, S. A. Laukhin, I. E. Zherebtsov, S. B. Levchenko, N. G. Baranova. - Variations of the relative intensity of geomagnetic field in bottom sediments of the Bering Sea and North-Western Pacific during the last 380 kyr / M. I. Malakhov, S. A. Gorbarenko, D. Nurnberg, R. Tiedemann, G. Yu. Malakhova, J. Riethdorf. - Using high-resolution records petromagnetic and lithophysic characteristics of the sediments Bering Sea and high-latitude Western Pacific for reconstruction of climate and environment in the Late Pleistocene-Holocene / M. I. Malakhov, S. A. Gorbarenko, D. Nurnberg, R. Tiedemann, G. Yu. Malakhova, J. Riethdorf. - Some information about genetic classification of lakes of the Vepsovsky Hill East of the Leningrad Region / O. V. Malozemova, L. A. Nesterova, D. A. Subetto. - Middle Pleistocene small mammal faunas of Eastern and Central Europe: Chronology, correlation / A. K. Markova, T. van Kolfschoten. - Astronomical and meteorological criteria of defining human activity traces in ancient megalith rock complexes in the North-West Russia / L. S. Marsadolov, G. N. Paranina. - Palynological characteristics of the middle Pleistocene deposits in the Vychegda River Basin, the Komi Republic (preliminary data) / T. I. Marchenko-Vagapova. - Isotope specialization (δ18O, δ13C) of quaternary carbonates from Belarus and potential of palaeoenvironments indication / N. A. Makhnach. - The complex survey of quaternary deposits / A. V. Mashukov, A. E. Mashukova. - Quaternary deposits and construction materials' deposits in the Kaluga Region / S. G. Medvedeva. - Vegetation and climate of Sakhalin in the early Holocene / Yu. A. Mikishin, L. G. Gvozdeva. - Inorganic geochemistry record of stages 6-11 from Elgygytgyn lake sediments (deep drilling data) / P. S. Minyuk, V. Ya. Borkhodoev and Elgygytgyn Scientific Party. - Palaeoshorelines on the Murmansk coast / M. V. Mityaev. - Vertical matter flow in Gulfs on Murmansk and Karelian coasts / M. V. Mityaev, M. V. Gerasimova. - Channel and basin components of sediment yield in the formation of quaternary alluvial suites of rivers of the middle Volga Region / V. V. Mozzherin. - Late Pleistocene interglacial-glacial climatic transition (MIS 5/MIS 4) as derived from palynological analysis and IR-OSL dating of deposits from the Voka Reference Section, Southeastern coast of the Gulf of Finland / A. N. Molodkov, N. S. Bolikhovskaya. - Quaternary sediments in the Central Part of Northern West Siberia / D. V. Nazarov. - Palynological evidences of the postglacial warm event of the Laptev Sea Region / O. D. Naidina. - Some problems of using luminescent methods for absolute dating of glacial deposits (by the example of Chagan Section, SE Altai) / R. K. Nepop, A. R. Agatova, H. Rodnight. - Freshwater travertine-like carbonates of the Izhora Plateau as the natural markers of the structural dislocations / M. U. Nikitin, A. A. Medvedeva. - Fold deformations in late Pleistocene deposits of the Central Part Kola Region and their genesis / S. B. Nikolaeva. - Mammoths and man of stone age in Northern Europe - insight of a question on migrations to European Subarctic by Western paths / A. A. Nikonov. - Formation of present-day deposits in the conditions of technogenic litogenesis / E. N. Ogorodnikova, S. K. Nikolaeva. - Traces cryogenesis of Neopleistocene sediments the lower Irtysh / O. L. Opokina, E. A. Slagoda. - Stratigraphical subdivision of the Eopleistocene deposits of the Simbugino Site and new mollusc finds (Southern Foreurals) / E. M. Osipova, G. A. Danukalova. - Late Pleistocene to Holocene environment and climate in the Upper Ponoy Depression (Kola Peninsula) reconstracted from pollen record of Churozero lake bottom deposits / E. Yu. Pavlova, M. V. Dorozhkina, E. I. Devyatova. - Absolute chronology and climatic conditions of Valdai (Vistulian) terraces formation in the middle Seim River Valley / A. Panin, J.-P. Buylaert, E. Matlakhova, A. Murray, O. Pakholova. - Possibility of reconstruction of climate change in the Mongolian Altai based on analysis of annual records in glaciers and lacustrine sediment / T. S. Papma, E. Yu. Mitrofanova, N. S. Malygina. - Northern labyrinth - thee Gnomon: compass, clock, calendar / G. N. Paranina. - Late Pleistocene and Holocene paleogeography of the coastal lowlands of Is. Paramushir (Kuril Islands) / A. Ju. Pakhomov. - Upper-Kama (Verhnekama) Upland - the newest lifting of the middle Last Pleistocene / M. M. Pakhomov, I. L. Borodatyi. - Dating mass accumulations of Mammoth across Arctic Eurasia / V. V. Pitulko, P. A. Nikolskiy, A. E. Basilyan, E. Y. Pavlova. - Features of vertical distribution of the materials within the marginal zones of permafrost polygonal structures and its importance for dating of quaternary deposits in cryolitozone / V. V. Pitulko, E. Y. Pavlova, A. E. Basilyan, S. G. Kritsuk. - Morfogenesis of the tectonics active area of the Mongolian Altay / S. G. Platonova. - Reference section of the Lichvin interglacial in the North-Western Part of European Russia's Region / E. S. Pleshivtseva, V. L. Garkusha, M. A. Travina. - New radiocarbon dates of Late Quaternary Mammals in the Arkhangelsk Region in connection with reconstructions of the last glaciation in the Eastern Europe / D. V. Ponomarev, T. van Kolfschoten, A. K. Markova, J. van der Plicht. - Geological illustrations of Aral-Caspian Region's latest seismodynamic high activity / V. I. Popkov. - About Karagiinsk closed depression (Mangishlak)'s genesis / V. I. Popkov. - On the issue of formation of the Caucasian mineral waters' modern structural geomorphologic aspect / V. I. Popkov, I. G. Sazonov, D. A. Kolleganova. - Natural climate changes on the border of Late Pleistocene and Holocene / A. N. Popova, D. A. Subetto. - Some problems paleogeomorfologi Volga Region / I. V. Proletkin. - New perspectives on modern geomorphological studies / I. V. Proletkin. - Dynamics of small mammals local assem , In kyrill. Schr. , In engl. und rus. Sprache
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  • 75
    Monograph available for loan
    Monograph available for loan
    Amsterdam [u.a.] : Elsevier Scientific Publ.
    Associated volumes
    Call number: AWI Bio-99-0079-2
    In: The Northwest European Pollen Flora, II
    Type of Medium: Monograph available for loan
    Pages: V, 265 S. , zahlr. Ill.
    ISBN: 0444418806
    Language: English
    Note: CONTENTS: Preface / G. C. S. Clarke and W. Punt. - 8. Solanaceae / W. Punt and M. Monna-Brands. - 9. Saxifragaceae / A. A. M. L. Verbeek-Reuvers. - 10. Boraginaceae / G. C. S. Clarke. - 11. Escalloniaceae / A. A. M. L. Verbeek-Reuvers. - 12. Grossulariaceae / A.A.M.L. Verbeek-Reuvers. - 13. Hydrangeaceae / A. A. M. L. Verbeek-Reuvers. - 14. Parnassiaceae / A. A. M. L. Verbeek-Reuvers. - 15. Plantaginaceae / G. C. S. Clarke and M. R.Jones. - 16. Valerianaceae / G. C. S. Clarke and M. R. Jones. - 17. Aceraceae / G. C. S. Clarke and M. R. Jones. - 18. Hippuridaceae / M. S. Engel. - 19. Haloragaceae / M. S. Engel. - 20. Papaveraceae / A. J. Kalis. - Index. - Errata.
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  • 76
    Monograph available for loan
    Monograph available for loan
    Moskva : Izdat. Feorija
    Call number: AWI Atl-18-91583
    Type of Medium: Monograph available for loan
    Pages: 869 S. , zahlr. Ill., Kt. , 25,0 x 34,0
    ISBN: 5287005318 , 9785287005313
    Language: Russian
    Note: In kyrill. Schr.
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  • 77
    Monograph available for loan
    Monograph available for loan
    Kyoto : International Research Center for Japanese Studies
    Associated volumes
    Call number: AWI Bio-18-91448
    In: The pollen flora of Yunnan, China, Vol. 1
    Description / Table of Contents: The Pollen Flora of Yunnan, China is the first book of the series of pollen morphological studies of tree plants growing in the wild in the Yunnan Province and in the surrounding area of China: Asian Environmental History. The series will present the first detailed work on the pollen flora of China. This book includes electron microscope photographs and light micrographs of 67 species of Gymnosperm, Myricaceae and Juglandaceae and can be used for research on many areas including pollen analysis and plant taxonomy.
    Type of Medium: Monograph available for loan
    Pages: 144 S.
    ISBN: 8174363416
    Series Statement: Asian Environmental History 1
    Language: English
    Note: Contents: Preface. - Introduction. - Gymnosperm. - Pinaceae. - Taxodiaceae. - Cupressaceae. - Podocarpaceae. - Ephedraceae. - Angiosperm. - Juglandaceae. - Myricaceae. - Bibliography. - Plates. - Gymnosperm. - Pinaceae: Plates 1-23. - Taxodiaceae: Plates 24-26. - Cupressaceae: Plates 27-39. - Podocarpaceae: Plates 40-46. - Ephedraceae: Plates 47-52. - Angiosperm. - Juglandaceae: Plates 53-64. - Myricaceae: Plates 64-68. - Pollen Sample List. - Index.
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  • 78
    Call number: AWI G2-18-91973
    Type of Medium: Monograph available for loan
    Pages: 49 Seiten , Illustrationen
    Language: English
    Note: Table of Contents: Introduction. - Contact information. - List of participants. - Guidelines for presenters. - Registration. - Workshop program. - Hotel and workshop venues. - Travel information. - Abstracts. - Public lecture.
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  • 79
    Monograph available for loan
    Monograph available for loan
    New Delhi : Amerind Publishing
    Call number: AWI G2-18-91897
    Description / Table of Contents: This publication is concerned with problems of the origin, evolution and paleogeography of the Arctic Ocean and its coast during the Tertiary and Quaternary periods. Much emphasis is placed on the evolution of modern Arctic flora and fauna, both terrestrial and aquatic. All these problems are discussed on the basis of hydrological, paleontological, biogeographical, climatological and archaeological data presented at the AII-Union symposium held in Leningrad during April 1-6, 1968. This is a unique encyclopedia on the Arctic. lt will be of interest to many research workers - geographers, geologists, biologists, hydrologists and all who deal with problems of the geological history and paleogeography of the Northern Hemisphere.
    Type of Medium: Monograph available for loan
    Pages: XIV, 564 Seiten , Illustrationen
    Uniform Title: Severnyi Ledovityi Okean i Ego Poberezh'e v Kainozoe
    Language: English
    Note: Contents: PREFACE. - SECTION I. HISTORY OF THE ARCTIC OCEAN IN THE CENOZOIC ERA. - Linear and Areal Morphostructures of the Arctic Ocean Floor / V. D. Dibner. - Fluctuations in Arctic Climate as Revealed by Floor Sediment Analysis / N. A. Belov, N. N. Lapina. - Stratification and Rate of Accumulation of Floor Sediments of the Soviet Arctic Seas / N. N. Kulikov, N. N. Lapina, Yu. P. Semenov, N. A. Belov, M. A. Spiridonov. - Palynologic Study of Kara Sea Floor Sediment Cores / N. N. Kulikov, R. M. Khitrova. - Geologic Structure of the Glacial Shelves of the Atlantic Province of the Arctic Basin / M. A. Spiridonov. - Stratigraphy and Paleogeography of Spitsbergen in the Pleistocene / Yu. A. Lavrushin. - Role of Glaciers in Franz Josef Land Relief Formation / V. L. Sukhodrovskii. - Reconstruction of the Late- and Post-Pleistocene Arctic Basin Ice Sheet / P. M. Borisov. - Changes in the Arctic Basin since the Last Glaciation Maximum / D. P. Chizhov. - SECTION II. ARCTIC FLORA AND FAUNA AND THE HISTORY OF THEIR FORMATION. - Some Problems of Study of the Early Cenophytic Arctic Flora / L. Yu. Budantsev. - Arctic Flora and Its Historical Link with the Arctic Ocean / A. I. Tolmachev, B. A. Yurtsev. - Wide Fluctuations in Ocean Level in the Quaternary period and Their Influence on the Arctic Ocean Basin and its biological community / G. U. Lindberg. - Fresh Data on the Food of the Siberian Woolly Rhinoceros / V. E. Garutt, E. P. Meteltseva, B. A. Tikhomirov. - Characteristics of the Arctic Ocean Fauna and their significance for understanding the History of its formation / E. F. Guryanova. - Formation of macroscopic marine algal flora of the Arctic Basin / A. D. Zinova, Yu. E. Petrov. - The Concept of the Arctic origin of Pinnipeds and other solutions of this problem / K. K. Chapskii. - Ecological Adaptations of Pinnipeds in the Atlantic Province of the Polar Basin / V. A. Potelov, Yu. K. Timoshenko. - A General Review of th PIeistocene Marine Faunas of the Northern Coast of Eurasia / S. L. Troitskii. - History of the Evolution of Marine Mollusk Fauna of the Late Cenozoic Atlantic Arctic / V. S. Zarkhidze. - Late Cenozoic History of Foraminifera of the Pechora Lowland and Northern West Siberia / O. F. Baranovskaya, V. Ya. Slobodin. - Species composition of Modern Foraminifera as an Indication of the Arctic Sea's hydrological regime / S. V. Tamanova. - SECTION Ill. PALEOGEOGRAPHY OF THE NORTHERN TERRITORIES IN THE LATE CENOZOIC ERA. - Paleogeography of Northern USSR and contiguous areas of the Arctic Basin / G. S. Ganeshin. - North Eurasia in the Late Cenozoic Era / Yu. P. Degtyarenko, V. V. Zhukov, N. G. Zagorskaya, O. A. Ivanov, V. I. Kaiyalainen, Yu. N. Kulakov, A. P. Puminov, V. Ya. Slobodin, O. V. Suzdalskii. - On the History of the Migration of the Arctic Basin Shoreline in the Cenozoic Era / S. A. Strelkov. - Causes of Fluctuations in the Arctic Basin Level in the Neogene-Quaternary Period / J. L. Kuzin. - Spore-Pollen Analysis of Late Cenozoic Marine Sediments in the Reconstruction of the Paleogeography of the Arctic Coasts / N. G. Zagorskaya, F. M. Levina. - Forest Line Migration in North Asia in the Upper Pleistocene and Holocene (Based on Spore-Pollen Analysis) / R. E. Giterman, L. V. Golubeva, E. V. Koreneva, L. A. Skiba. - Holocene Transgressions and Variations in the Northern Coastline of the Kola Peninsula / B. I. Koshechkin, A. L. Kudlaeva. - Interpretation of Radiocarbon Datings of the Absolute Age of Organic Residues from the Upper Anthropogene Deposits of Fennoscandia / V. G. Chuvardinskii. - Structure and Stratigraphic Division of White Sea Bottom Deposits / V. S. Medvedev, E. N. Nevesskii, L. I. Govberg, E. S. Malyasova, R. N. Dzhinoridze, E. A. Kirienko. - Principal Stages in the History of the Vegetation of the Dvina Bay Coast of the White Sea during the Late- and Postglacial Transgression / E. S. Pleshivtseva. - Quaternary Transgressions in the Northern Russian Plain and Their Relationship with Continental Glaciations / E. N. Bylinskii. - Anthropogene Deposit-Forming Environments on Kolguev Island / O. F. Baranovskaya, T. A. Matveeva. - Cenozoic History of the Northern Coast of Europe / V. S. Zarkhidze. - Stages of Formation of the Southern Part of the Arctic Basin in Timan-Pechora Province in the Late Cenozoic Era / O. F. Baranovskaya, P. N. Safronov, G. N. Berdovskaya. - Pliocene-Pleistocene History of the Pechora Basin / V. L. Yakhimovich. - Paleogeography and Origin of Cenozoic Rocks in Soviet Europe as Revealed by Hydrochemical Data / V. D. Bezrodnov. - Study of Paleogeography and Neotectonics of Some Regions of the European Northeast by Coal Petrography / Yu. V. Stepanov. - History of the Formation of Arctic Shelf Foraminifer Fauna (Based on Data on the Timan-Ural Region) / I. N. Semenov. - Evolution of Pleistocene Marine Diatom Flora in the Northeast of Soviet Europe / E. I. Loseva. - Quaternary Deposits of the Middle Pechora and Vychegda River Basins / A. S. Lavrov. - Late Pleistocene Terraces in the Northeast of Soviet Europe and the Environments in which They were Formed / L. M. Potapenko, A. S. Lavrov. - Key Sections of the Lower Pechora and Their Importance for an Understanding of the Last Stages of the Geological Evolution of Northeastern Soviet Europe / V. S. Zarkhidze, I. I. Krasnov, M. A. Spiridonov, Yu. A. Lavrushin, I. I. Ryumina. - Siberian Elements in the Flora of the Far Northeast of Europe and Their Origin / O. V. Rebristaya. - Some Geographical Relationships of Ural Floras and Their Importance for Paleogeography / K. N. lgoshina. - Ostracod Complexes from the Late Cenozoic Marine Deposits of Northern Soviet Europe and West Siberia and Their Importance for Paleogeography / O. M. Lev. - Paleogeography of the Northern West Siberian Lowland and Russian Plain in the Late Pleistocene and Holocene / M. G. Kipiani, A. D. Kolbutov. - Mammals and Landscapes of the Northern Urals in the Late Anthropogene / I. E. Kuzmina. - Pleistocene Transgressions in Northern West Siberia and the Pechora Lowland / I. D. Danilov. - Salient Paleogeographic Features of the Pechora Lowland and Lower Ob Basin in the Neogene Epoch / P. P. Generalov, I. L. Kuzin, I. L. Zaionts, R. B. Krapivner. - Some Problems of the Quaternary Geology of Northern Soviet Europe and West Siberia / A. G. Kostyaev. - Northern West Siberia in the Pliocene and Pleistocene / O. V. Suzdalskii. - Boreal Transgressions and the Origin of Subsurface Sheet Ice Deposits / B. I. Vtyurin. - Dependence of Certain Types of Subsurface Glaciation in West Siberia on the Peculiarities of the Polar Sea / A .I. Popov. - History of Subsurface Freezing in West Siberia in the Light of Transgression of the Arctic Basin / V. V. Baulin. - New Data on the History of the Evolution of the Pre-Kazantseva and Kazantseva Vegetation in the Muzhi Urals and Southern Yamal (Based on Palynological Data) / E. E. Gurtovaya. - New Data on the Distribution of Recent Marine Deposits in West Siberia / I. L. Zaionts, Z. I. Kholodova. - Pleistocene Diatom Floras of the Yenisei North / Z. V. Aleshinskaya. - Some Upper Cenozoic Stratotypes of the Ust-Yenisei Depression / V. Ya. Slobodin. - Transgressions of the Arctic Basin and Evolution of the Yenisei North in the Pleistocene (Absolute Chronology of Events by 14C Dating) / N. V. Kind, L. D. Sulerzhitskii. - Kargin Diatoms from the Key Section of the Lower Yenisei / N. A. Khalfina. - Spread of Late Cenozoic Transgressions of the Arctic Basin in the Northwestern Central Siberian Tableland / V. D. Kryukov, V. V. Rogozhin. - Paleogeography of Northeastern Taimyr in the Quaternary Period (Based on Geological and Palynological Data) / G. N. Berdovskaya, N. A. Gei, V. M. Makeev. - Emergence and Development of Pleistocene Landscapes in the Eastern North Siberian Lowland / V. V. Zhukov, N. A. Pervuninskaya, L. Ya. Pinchuk. - History of Relief Formation in the Eastern North Siberian Lowland and the Adjoi
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  • 80
    Monograph available for loan
    Monograph available for loan
    [Erscheinungsort nicht ermittelbar] : Department of Science and Technology, Antarctic Division Australia
    Associated volumes
    Call number: AWI P2-86-0256
    In: Antarctic Telecommunications Guidance Manual, Volume 1
    Type of Medium: Monograph available for loan
    Pages: Diverse Seitenangaben (ca. 50 Seiten)
    Language: English
    Note: TABLE OF CONTENTS: Distribution List. - List of acronyms and abbreviations used. - Record of Amendments. - Foreword to 1st Edition. - Foreword to 2nd Edition. - HISTORY AND DEVELOPMENTS OF ANTARCTIC COMMUNICATIONS. - CONSIDERATION OF TELECOMMUNICATIONS BY SCAR AND ANTARCTIC TREATY CONSULTATIVE PARTIES. - OPERATION OF INDIVIDUAL NATIONS' NETWORKS. - Australia's Antarctic Communications. - Japan's Antarctic communications. - UK Antarctic communications. - US Antarctic communications. - ANTARCTIC TREATY RESOLUTIONS ON ANTARCTIC COMMUNICATIONS. - WMO RESOLUTIONS AND PRINCIPLES ON ANTARCTIC COMMUNICATIONS. - Introduction. - Engineering principles of the GTS. - Functions and responsibilities of Meteorological Telecommunications Centres. - Characteristics of the networks of the GTS. - Operational principles of the GTS. - The transmission of meteorological data an the GTS. - Collection and transmission of meteorological data. - Data processing. - Telecommunications system. - Weather reporting by traverse parties. - Automatic weather station in the Antarctic. - AIREP reports. - Mobile ship stations. - OTHER RELEVANT RECOMMENDATIONS AND RESOLUTIONS. - APPENDIXES. - APPENDIX I. - Manual an the Global Data Processing System, Regional Aspects, the Antarctic. - APPENDIX II. - Network of CLIMAT and CLIMAT TEMP reporting stations in the Antarctic. - APPENDIX III. - Results of the monitoring of Antarctic data reception carried out during the period 12-15 March 1982. - APPENDIX IV. - Existing links for the daily international exchange of meteorological data within the Antarctic. - APPENDIX V. - Principal routes by which Antarctic meteorological data enters the GTS. - APPENDIX VI. - List of Antarctic stations and the routing of their meteorological data to the GTS.
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  • 81
    Call number: ZSP-994
    Type of Medium: Series available for loan
    Pages: 21 x 21 cm
    ISSN: 1618-3703
    Former Title: Vorgänger: Zweijahresbericht / Stiftung Alfred-Wegener-Institut für Polar- und Meeresforschung
    Subsequent Title: Fortsetzung Zweijahresbericht ... / AWI, Alfred-Wegener-Institut für Polar- und Meeresforschung in der Helmholtz-Gemeinschaft
    Language: German , English
    Note: Erscheint alle 2 Jahre , Text in deutscher und englischer Sprache
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  • 82
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-82/31
    In: CRREL Report, 82-31
    Description / Table of Contents: Information on sea ice conditions in the Bering Strait and the icefoot formation around Fairway Rock, located in the strait, is presented. Cross-sectional profiles of Fairway Rock and the relief of the icefoot are given along with theoretical analyses of the possible forces active during icefoot formation. It is shown that the ice cover most likely fails in flexure as opposed to crushing or buckling, as the former requires less force. Field observations reveal that the Fairway Rock icefoot is massive, with ridges up to 15 m high, a seaward face only 20 degrees from vertical, and interior ridge slopes averaging 33 degrees. The icefoot is believed to be grounded and its width ranges from less than 10 to over 100 m.
    Type of Medium: Series available for loan
    Pages: 44 Seiten , Illustrationen
    Series Statement: CRREL Report 82-31
    Language: English
    Note: CONTENTS Abstract Preface Introduction Bering Strait Field reconnaissance Estimation of ice forces on Fairway Rock 1. Creep deformation 2. Crushing failure 3. Flexural failure 4. Forces required to form floating or grounded pressure ridges along therock or to pile ice on the beaches 5. Buckling failure Driving forces Angle of internal friction of sea ice Summary Literature cited Appendix A: April 1982 field observations at Fairway Rock
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  • 83
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-82/32
    In: CRREL Report, 82-32
    Description / Table of Contents: Low-frequency (10 Hz) volcanic earthquakes originate at a wide range of depths and occur before, during, and after magmatic eruptions. The characteristics of these earthquakes suggest that they are not typical tectonic events. Physically analogous processes occur in hydraulic fracturing of rock formations, low-frequency icequakes in temperate glaciers, and autoresonance in hydroelectric power stations. We propose that unsteady fluid flow in volcanic conduits is the common source mechanism of low-frequency volcanic earthquakes (tremor). The fluid dynamic source mechanism explains low-frequency earthquakes of arbitrary duration, magnitude, and depth of origin, as unsteady flow is independent of physical properties of the fluid and conduit. Fluid transients occur in both low-viscosity gases and high-viscosity liquids. A fluid transient analysis can be formulated as generally as is warranted by knowledge of the composition and physical properties of the fluid, material properties, geometry and roughness of the conduit, and boundary conditions. To demonstrate the analytical potential of the fluid dynamic theory, we consider a single-phase fluid, a melt of Mount Hood andeside at 1250 deg C, in which significant pressure and velocity variations occur only in the longitudinal direction.
    Type of Medium: Series available for loan
    Pages: 15 Seiten , Illustrationen
    Series Statement: CRREL Report 82-32
    Language: English
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  • 84
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-83/8
    In: CRREL Report, 83-8
    Description / Table of Contents: In the course of model tests with urea-doped ice in the CRREL Ice Engineering Facility test basin, the growth process and the physical and mechanical properties of the model ice were investigated. The parameters which were varied were: urea concentration in the tank water, air temperature during growth, growth duration, and tempering time. Uniformity of ice thickness and ice mechanical properties over the whole tank area were found to be satisfactory. The structure of the urea-doped ice was found to be similar to that of the ice except for a relatively thick incubation layer over a dendritic bottom layer. Empirical relationships were established between: ice thickness and negative degree-hours; mechanical properties and growth temperature, urea concentration, and ice thickness; and reduction in mechanical properties and tempting time. The results of the study are presented in charts which permit reliable scheduling of model tests with required ice thickness and ice flexural strength.
    Type of Medium: Series available for loan
    Pages: vii, 53 Seiten , Illustrationen
    Series Statement: CRREL Report 83-8
    Language: English
    Note: CONTENTS Abstract Preface Nomenclature Introduction Experimental facility and procedures Ice test basin Ice growth procedure Measurements Ice growth and structure Ice thickness distribution Ice growth during freeze-up Ice growth during warm-up Structure of urea-doped ice Mechanical properties of urea-doped ice Introductory remarks Model of a two-layer elastic material Properties of urea-doped ice during freeze-up Properties of urea-doped ice during warm-up Applications to test program scheduling Summary and conclusions Literature cited Appendix A: Results of ice thickness measurements for various growth conditions Appendix B: Properties of untempered ice Appendix C: Properties of tempered ice
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  • 85
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-82/41
    In: CRREL Report, 82-41
    Description / Table of Contents: Many of the important factors influencing the choice of appropriate aquifer test procedures are presented. The concepts of bias, accuracy and spatial variabil­ity are explained. The definitions of a number of aquifer parameters are devel­oped from basic principles demonstrating the underlying assumptions and limita­tions. The parameters considered are: piezometric head, hydraulic conductiv­ity/intrinsic permeability, flow direction, specific discharge magnitude, transmissivity, volumetric flow rate, total porosity, effective porosity, aver­age linear velocity, storage coefficient, specific yield, dispersion coefficient-aquifer dispersivity. For each parameter several techniques are described, evaluated and ranked in terms of perceived potential accuracy, simplicity and value to contaminant transport studies. It must be stressed, however, that the evaluations are based principally upon theoretical grounds, and not upon actual conduct of the described procedures.
    Type of Medium: Series available for loan
    Pages: iv, 111 Seiten , Illustrationen
    Series Statement: CRREL Report 82-41
    Language: English
    Note: CONTENTS Abstrac Preface Introduction Purpose Scope Concept of accuracy Test selection Definition of parameters Piezometric head Use of piezometers Hydraulic conductivity Flow direction Specific discharge magnitude Transmissivity Volumetric flow rate Porosity Average linear velocity Storage coefficient-specific yield Aquifer dispersivity Parameter estimation techniques Piezometric head Hydraulic conductivity Direction and magnitude of specific discharge vector Transmissivity Volumetric flow rate Total porosity Average linear velocity Storage coefficient Specific yield Effective porosity Aquifer dispersivity-dispersion coefficients Conclusions Literature cited
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  • 86
    Call number: ZSP-201-83/7
    In: CRREL Report, 83-7
    Description / Table of Contents: Peak power generation with hydropower creates tailwater flow conditions characterized by high and low flows with abrupt transitions between these states. Flows occurring in tailwaters typically form sharp-fronted, large-amplitude waves of relatively short period. An understanding of the mechanics of downstream propagation of these waves is important both for direct application in studies of the tailwater and because of the similarity of these waves to those following a dam break. An analysis of the dynamic equations of open channel flow is used to quantify the relative importance of flow wave convection, diffusion and dispersion in rivers. The relative importance of each process is re­lated to the relative magnitude of terms in the dynamic equations, providing a physical basis for model formulation. A one-dimensional diffusion wave flow routing model, modified for tailwaters, simulates the important physical pro­cesses affecting the flow and is straightforward to apply. The model is based upon a numerical solution of the kine­matic wave equation. The “modified equation,” Hirt, and von Neumann analyses are used to gain insight into the stability and dissipative and dispersive behavior of the numerical solution, and results of these analyses are compared. A set of linear routings is used to demonstrate the dissipative and dispersive behavior predicted by the analyses and to verify the accuracy of an expression that quantifies the numerical diffusion of the model. The analyses provide a basis for selection of numerical parameters for model applications. The capability and accuracy of the model are enhanced when physical wave diffusion is balanced by numerical diffusion in the model. Maintaining the diffusion balance re­quires that the time derivative weighting parameter 0 be variable and in some instances negative. Though some amount of phase error is introduced, negative 0 values have no adverse effect upon model stability. Field studies were con­ducted to demonstrate the benefits of careful model development and analysis, and to verify the diffusion wave model for rapidly varying tailwater flow. The bed slope and roughness characteristics of the field study reaches (below Apalachia and Norris Dams) differ greatly, spanning those of a large number of rivers of practical interest. The accurate simulation of flow in both of these tailwaters attests to the soundness of both the physical basis of the model and the numerical solution technique. The field studies confirm, for the extreme case of rapidly varying flow in a mildly sloped river, that inertia has a negligible effect upon unsteady flow waves at low Froude numbers. Additionally, these studies verify that diffusion of short-period waves in rivers is generally significant.
    Type of Medium: Series available for loan
    Pages: vi, 41 Seiten , Illustrationen
    Series Statement: CRREL Report 83-7
    Language: English
    Note: CONTENTS Abstract Preface Nomenclature Introduction Physical diffusion and dispersion in open channel flow Modeling approach Description of the diffusion wave flow routing model Analysis of the numerical model Modified equation and Hirt analyses of diffusion wave model von Neumann analysis of the diffusion wave model Linear case studies Accuracy considerations of the numerical solution Field studies Apalachia Dam tailwater Norris Dam tailwater Conclusions Literature cited
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  • 87
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-83/5
    In: CRREL Report, 83-5
    Description / Table of Contents: This report presents the results of dynamic ice-structure interaction model tests conducted at the CRREL Ice Engineering Facility. A flexible, single-pile, bottom-founded offshore structure was simulated by a test pile with about a one-to-ten scale ratio. Urea (instead of sodium chloride) was used as dopant to scale down the ice properties, resulting in good model ice properties. Six ice fields were frozen and 18 tests carried out. In all cases distinctive dynamic ice structure interaction vibrations appeared, from which abundant data were collected. In tests with linear ice velocity sweep, sawtooth-shaped ice force fluctuations occurred first. With increasing velocity the natural modes of the test pile were excited, and shifts from one mode to another occurred. The maximum ice force values appeared mostly with low loading rates, but high forces appeared random'y at high ice velocities. As a general trend, ice force maximums, averages and standard deviations decreased with increasing ice velocities. The aspect ratio effect of the ice force in continuous crushing follows the same dependence as in static loadings. The frequency of observed ice forces is strongly dominated by the natural modes of the structure. Dynamically unstable natural modes tend to make the developing ice force frequencies the same as the natural frequencies. Otherwise the resulting frequency depends directly on structural stiffness and ice velocity and inversely on the ice force range. During vibrations the displacement rates of the structure overcome the velocity of ice, making low loading rates and hence high ice forces possible. During crushing, ice induces both positive and negative damping.
    Type of Medium: Series available for loan
    Pages: iv, 53 Seiten , Illustrationen
    Series Statement: CRREL Report 83-5
    Language: English
    Note: CONTENTS Abstract Preface Introduction Test arrangements Ice properties Crushing patterns Maximum ice force vs velocity Dynamic aspect ratio effect and crushing strength Measured ice force frequencies Calculated ice force frequencies Accelerations, velocities and displacements Damping Ice-induced negative damping Limit cycles Buckling load Conclusions Literature cited
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  • 88
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    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-82/38
    In: CRREL Report, 82-38
    Description / Table of Contents: Extreme cold causes heavy buildup of frost, ice and condensation on many windows. It also increases the incentive for improving the airtightness of windows against heat loss. Our study shows that tightening specifications for Alaskan windows to permit only 30% of the air leakage allowed by current American airtightness standards is economically attractive. We also recommend triple glazing in much of Alaska to avoid window icing in homes and barracks. We base our conclusions on a two-year field study of Alaskan military bases that included recording humidity and temperature data, observing moisture accumulation on windows and measuring airtightness with a fan pressurization device.
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    Pages: v, 26 Seiten , Illustrationen
    Series Statement: CRREL Report 82-38
    Language: English
    Note: Contents Abstract Preface Nomenclature Introduction Previous work in cold weather window performance Investigation Data acquisition and analysis Modeling the window thermal regime Moisture and ice observations Airtightness testing and analysis Annual heat loss from air leakage Results and conclusions Moisture on windows Airtightness Airtightness economics Recommendations for windows in extreme cold Airtightness Multiple glazing Literature cited Appendix A: Moisture levels and airtightness Appendix B: Dewpoint data Appendix C: Sample observations of icing
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  • 89
    Call number: ZSP-201-82/37
    In: CRREL Report, 82-37
    Description / Table of Contents: This report presents a Landsat-derived land cover map of the northwest portion of the Arctic National Wildlife Refuge, Alaska. The report is divided into two parts. The first is devoted to the land cover map with detailed descriptions of the mapping methods and legend. The second part is a description of the study area. The classification system used for the maps is an improvement over existing methods of describing tundra vegetation. It is a comprehensive method of nomenclature that consistently applies the same criteria for all vegetation units. It is applicable for large- and small-scale mapping and is suitable for describing vegetation complexes, which are common in the patterned-ground terrain of the Alaskan Arctic. The system is applicable to Landsat-derived land cover classifications. The description of the study area focuses on five primary terrain types: flat thaw-lake plains, hilly coastal plains, foothills, mountainous terrain, and river flood plains. Topography, landforms, soils and vegetation are described for each terrain type. The report also contains area summaries for the Landsat-derived map categories. The area summaries are generated for the five terrain types and for the 89 townships within the study areas. Two land cover maps at 1:250,000 are included.
    Type of Medium: Series available for loan
    Pages: 68 Seiten , Illustrationen, 2 Karten
    Series Statement: CRREL Report 82-37
    Language: English
    Note: CONTENTS Abstract Preface Foreword Introduction A land cover map of the ANWR study area Legend development Mapping method Results Discussion Description of the ANWR study area General description Description of specific terrain types Conclusions Literature cited Appendix A: Descriptions of Landsat land cover categories for ANWR Appendix B: Area summaries Appendix C: Aproximate equivalent units in several systems of land cover, wetland and vegetation classifications used in northern Alaska Appendix D: Soil taxonomy Appendix E: Summary of principal Landsat land cover categories within the terrain types of the ANWR study area
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  • 90
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    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-82/36
    In: CRREL Report, 82-36
    Description / Table of Contents: Camp construction and drilling activities in 1950 at the East Oumalik drill site in northern Alaska caused extensive degradation of ice-rich, perennially frozen silt and irreversible modification of the upland terrain. In a study of the long-term degradational effects at this site, the near-surface geology was defined by drilling and coring 76 holes (maximum depth of 34 m) in disturbed and undisturbed areas and by laboratory analyses of these cores. Terrain disturbances, including bulldozed roads and excavations, camp structures and off-road vehicle trails, were found to have severely disrupted the site's thermal regime. This led to a thickening of the active layer, melting of the ground ice, thaw subsidence and thaw consolidation of the sediments. Slumps, sediment gravity flows and collapse of materials on slopes bounding thaw depressions expanded the degradation laterally, with thermal and hydraulic erosion removing materials as the depressions widened and deepened with time. Degradational processes became less active after thawed sediments thickened sufficiently to slow the increase in the depth of thaw and permit slope stabilization. The site's terrain is now irregular and hummocky with numerous depressions. Seasonal thaw depths are deeper in disturbed areas than in undisturbed areas and reflect the new moisture conditions and morphology. The severity of disturbance is much greater at East Oumalik than at another old drill site, Fish Creek. The difference results primarily from differences in the physical properties of the sediments, including the quantity and distribution of ground ice.
    Type of Medium: Series available for loan
    Pages: 42 Seiten , Illustrationen
    Series Statement: CRREL Report 82-36
    Language: English
    Note: CONTENTS Abstract Preface Summary Introduction Methodology Geologic setting Camp construction and occupation Types of disturbance Degradational processes and the effective area of impact Areal effects of disturbance Topography Groundwater, surface water and drainage Sediment properties and near-surface stratigraphy Surficial processes Depth of thaw Comparison to Fish Creek Discussion and conclusions Literature cited
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  • 91
    Call number: ZSP-201-83/21
    In: CRREL Report, 83-21
    Description / Table of Contents: The probability density function of the gouge depths into the sediment is represented by a simple negative exponential over four decades of gouge frequency. The exceedance probability function is, therefore, e to the -lambda d, where d is the gouge depth in meters and lambda is a constant. The value of lambda shows a general decrease with increasing water depth, from 9/m in shallow water to less than 3/m in water 30 to 35 m deep. The deepest gouge observed was 3.6 m, from a sample of 20,354 gouges that have depths greater than or equal to 0.2 m. The dominant gouge orientations are usually unimodal and reasonably clustered, with the most frequent alignments roughly parallel to the general trend to the coastline. The value of N(bar) sub 1, the mean number of gouges (deeper than 0.2 m) per kilometer measured normal to the trend of the gouges, varies from 0.2 for protected lagoons to 80 in water between 20 and 38 m deep in unprotected offshore regions. The distribution of the spacings between gouges as measured along a sampling track is a negative exponential. The form of the frequency distribution of N sub 1 varies with water depth and is exponential for lagoons and shallow offshore areas, previously skewed for 10 to 20 m depths off the barrier islands, and near-normal for deeper water. As a Poisson distribution gives a reasonable fit to the N sub 1 distributions for all water depths, it is suggested that gouging can be taken as approximating a Poisson process in both space and time. The distributions of the largest values per kilometer of gouge depths, gouge widths, and the heights of the lateral embankment of sediments plowed from the gouges are also investigated.
    Type of Medium: Series available for loan
    Pages: 40 Seiten , Illustrationen, 1 Karte
    Series Statement: CRREL Report 83-21
    Language: English
    Note: CONTENTS Abstract Preface Introduction Background and environmental setting Data collection and terminology Data analysis Gouge depths Gouge orientation Gouge frequency Extreme value analysis Applications to offshore design Gouge depth Extreme value statistics Burial depths Conclusion Literature cited Appendix A: Detailed bathymetric map of the Alaskan portion of the Beaufort Sea
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  • 92
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    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-83/19
    In: CRREL Report, 83-19
    Description / Table of Contents: Small-scale laboratory experiments were conducted on model bridge piers in the CRREL test basin. The experiments were performed by pushing model ice sheets against structures and monitoring the ice forces during the ice/structure interaction. The parameters, varied during the test program, were the geometry of the bridge piers and the velocity, thickness, and flexural strength of the ice. The results are presented in the form of ice forces on sloping and vertical structures with different geometries. During ice action on sloping structures, a phenomenon of transition of failure mode from bending to crushing was observed as the ice velocity was steadily increased.
    Type of Medium: Series available for loan
    Pages: 17 Seiten , Illustrationen
    Series Statement: CRREL Report 83-19
    Language: English
    Note: CONTENTS Abstract Preface Introduction Tests Results Ice forces on inclined structures Transition of ice action due to velocity increase Aspect ratio Bridge pier nose geometry Conclusions Literature cited
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  • 93
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    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-83/18
    In: CRREL Report, 83-18
    Description / Table of Contents: An evaluation of an impulse radar system for detecting cavities under concrete pavement is discussed, and field results are presented. It was found that a dual antenna mode of surveying was ideal for void detection. In this mode one antenna operated in a transceive mode and a second, offset from the first, operated in a receive-only mode. This arrangement allowed a refraction-type profile survey to be performed, which enabled subpavement voids to be easily detected. Field trails were held at Plattsburgh Air Force Base, where 28 cavities were detected and mapped. Drilling of holes verified that a cavity existed and allowed cavity depth to be measured. The cavities varied from 1.5 in. to 23 in, depth and were up to 20 ft. long.
    Type of Medium: Series available for loan
    Pages: 49 Seiten , Illustrationen
    Series Statement: CRREL Report 83-18
    Language: English
    Note: CONTENTS Abstract Preface Introduction Plattsburgh Air Force Base Radar sounding system Survey procedure Cavity inspection Radar cavity detection test Radar profile results Falling-weight deflectometer tests Discussion and conclusions Literature cited
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  • 94
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    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-83/12
    In: CRREL Report, 83-12
    Description / Table of Contents: This paper documents the development and verification of two finite difference models that solve the general two-dimensional form of the heat conduction equation, using the alternative-direction implicit method. Both can handle convective, constant flux, specified temperature and semi-infinite boundaries. The conducting medium may be composed of many materials. The first program, ADI, solves for the case where no change of state occurs. ADIPC solves for case where a freeze/thaw change of phase may occur, using the apparent heat capacity method. Both models are verified by comparison to analytical results.
    Type of Medium: Series available for loan
    Pages: 74 Seiten , Illustrationen
    Series Statement: CRREL Report 83-12
    Language: English
    Note: CONTENTS Abstract Preface Introduction Finite differences applied to heat transfer Heat conduction equation Boundary conditions Phase change Computer program ADDATA, the data subroutine TRIDIG, the matrix solver ISOTHM, the isotherm finider ADI, main program ADEPC, main program Verification of ADI Comparison of ADI with analytical results Comparison of ADI with experimental results Verification of ADIPC Comparison of ADIPC with analytical results-the Neumann solution Comparison of ADIPC with analytical results-two-dimensional phase change verification User instruction for ADI User instruction for ADIPC Conclusions Literature cited Appendix A. Program INFSUM and sample input and output for program ADI Appendix B. Program ADIPC and sample input and output
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  • 95
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    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-83/13
    In: CRREL Report, 83-13
    Description / Table of Contents: A review on past experimental and theoretical work indicates a need for additional experimentation to characterize the response of snow to inelastic pressure waves. Pressure data from previously conducted explosion tests are analyzed to estimate the elastic limit of snow of 400 -kg/cu m density to be about 36 kPa. This pressure corresponds to a scaled distance of 1.6 m/cu.rt.kg for charges fired beneath the surface of the snow, and to a scaled distance of 1.2 m/cu.rt.kg for charges fired in the air. The effects of a snow cover on the method of clearing a minefield by using an explosive charge fired in the air above the snow surface are also discussed and recommendations are given for further work in this area. Explosive pressure data are used to estimate the maximum effective scaled radius for detonating buried mines at shallow depth to be 0.8 m/cu.rt.kg. Fuel-air explosive will increase this effective radius significantly because of the increase in the size of the source region.
    Type of Medium: Series available for loan
    Pages: 33 Seiten , Illustrationen
    Series Statement: CRREL Report 83-13
    Language: English
    Note: CONTENTS Abstract Preface List of symbols Introduction Objectives Background Problems in describing the response of snow to an applied stress Methods of determining the dynamic behavior of materials Review of previous studies on snow Experimental measurements on snow Summary of snow experiments Theoretical studies Confirmation of the theory Discussion Applications Recommendations Summary Literature cited Appendix A. Selected data from Wisotski and Snyder (1966) Appendix B. Pressure data from Livingston (1964)
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  • 96
    Call number: ZSP-201-83/14
    In: CRREL Report, 83-14
    Description / Table of Contents: An analysis of ice fracture that incorporates dislocation mechanics and linear elastic fracture mechanics is discussed. The derived relationships predict a brittle to ductile transition in polycrystalline ice under tension with a Hall-Petch type dependence of brittle fracture strength on grain size. A uniaxial tensile testing technique, including specimen preparation and loading system design was developed and employed to verify the model. The tensile strength of ice in purely brittle fracture was found to vary with the square root of the reciprocal of grain size, supporting the relationship that the theory suggests. The inherent strength of the ice lattice and the Hall-Petch slope are evaluated and findings discussed in relation to previous results. Monitoring of acoustic emissions was incorporated in the tests, providing insights into the process of microfracture during ice deformation.
    Type of Medium: Series available for loan
    Pages: 43 Seiten , Illustrationen
    Series Statement: CRREL Report 83-14
    Language: English
    Note: CONTENTS Abstract Preface Introduction Background Development of testing technique Test specimens Tensile testing Compression testing Experimental results Tensile tests Compression tests Discussion Conclusions Suggestions for further work Literature cited Appendix A: Additional information on seed grains Appendix B: Thin-sectioning procedure Appendix C: Displacement transducer calibration
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  • 97
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    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-83/16
    In: CRREL Report, 83-16
    Description / Table of Contents: The presence of snow on the ground can impose limitations on the mobility of wheeled and tracked vehicles. Snow depth and density are the two most easily measured snow properties that can be related to mobility over snow. Existing models of snowpack accumulation and ablation processes and models of internal snowpack structure were examined to determine if a model of the snowpack can be developed for use in predicting the snow parameters that affect mobility. Simple models, such as temperature index models, do not provide sufficient snowpack details, and the more detailed models require too many measured inputs. Components of the various models were selected from a basis of a snowpack model for predicting snow properties related to mobility over snow. Methods of obtaining the input data from some components are suggested, and areas where more development is needed are described.
    Type of Medium: Series available for loan
    Pages: 34 Seiten , Illustrationen
    Series Statement: CRREL Report 83-16
    Language: English
    Note: CONTENTS Abstract Preface Nomenclature Conversion of metric units Introduction Review of existing models Accumulation models Ablation models Using existing models for studying mobility Proposed snowpack model for mobility studies Model components Implementation of the model Developing input data Conclusions Literature cited
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  • 98
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    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-83/17
    In: CRREL Report, 83-17
    Description / Table of Contents: A sea ice model was applied to the East Greenland Sea to examine a 60-day ice advance period beginning 1 October 1979. This investigation compares model results using driving geostrophic wind fields derived from three sources. Winds calculated from sea-level pressures obtained from the National Weather Service's operational analysis system resulted in strong velocities concentrated in a narrow band adjacent to the Greenland coast, with moderate velocities elsewhere. The model showed excessive ice transport and thickness build-ups in the coastal region. The extreme pressure gradient parallel to the coast resulted partially from a pressure reduction procedure that was applied to the terrain-following sigma coordinate system to obtain sea-level pressures. Additional sea-level pressure fields were obtained from an independent optimal interpolation analysis that merged FGGE buoys drifting in the Arctic basin with high latitude land stations and from manual digitization of the NWS hand-analyzed Northern Hemisphere Surface Charts. Modeling results using winds from both of these fields agreed favorably.
    Type of Medium: Series available for loan
    Pages: 19 Seiten , Illustrationen
    Series Statement: CRREL Report 83-17
    Language: English
    Note: CONTENTS Abstract Preface Introduction Description of study Model results The problem Conclusions Literature cited
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  • 99
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    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-83/11
    In: CRREL Report, 83-11
    Description / Table of Contents: Investigations of ground radar performance over thawed and seasonally frozen silts, and sands and gravels containing artificial and natural reflectors were carried out in Alaska. The radar emitted 5-10 ns pulses, the center frequency of which was approximately 150 MHz. The artificial reflectors were metal sheets and discs and the natural reflectors were the groundwater table and interfaces between frozen and thawed material. The water table was profiled at three sites where the subsurface material was coarse-grained alluvium. Dielectric constants of 16 to 18 were measured for the thawed silts, 6 to 7 for the frozen silts and 3 to 9 for the sands and gravels. Signal penetration in the thawed high moisture content silts may be achieved only by use of a lower frequency radar, whereas in the sands and gravels greater depths may be detected with more sophisticated signal processing.
    Type of Medium: Series available for loan
    Pages: 16 Seiten , Illustrationen
    Series Statement: CRREL Report 83-11
    Language: English
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  • 100
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    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-83/23
    In: CRREL Report, 83-23
    Description / Table of Contents: The problems associated with measuring stresses in ice are reviewed. Theory and laboratory test results are then presented for a stiff cylindrical sensor made of steel that is designed to measure ice stresses in a biaxial stress field. Loading tests on freshwater and saline ice blocks containing the biaxial ice stress sensor indicate that the sensor has a resolution of 20 kPa and an accuracy of better than 15% under a variety of uniaxial and biaxial loading conditions. Principal stress directions can also be determined within 5 degrees. The biaxial ice stress sensor is not significantly affected by variations in the ice elastic modulus, ice creep or differential thermal expansion between the ice and gauge. The sensor also has a low temperature sensitivity (5 kPa/deg C).
    Type of Medium: Series available for loan
    Pages: 38 Seiten , Illustrationen
    Series Statement: CRREL Report 83-23
    Language: English
    Note: CONTENTS Abstract Preface Introduction Previous work Stress measurements Design considerations Stress sensors Biaxial ice stress sensor Biaxial stress sensor theory Gauge deformation Stresses associated with cylindrical sensors Determination of ice stresses Gauge calibration Evaluation of the biaxial ice stress sensor Temperature sensitivity Biaxial loading test equipment Biaxial loading test results Differential thermal expansion Long-term drift Discussion of test results Conclusions Literature cited
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