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  • 1
    Monograph available for loan
    Monograph available for loan
    Berlin : Springer
    Call number: AWI G3-13-0054
    Description / Table of Contents: Permafrost hydrology systematically elucidates the roles of seasonally and perennially frozen ground on the distribution, storage and flow of water. Cold regions of the world are subject to mounting development which significantly affects the physical environment. Climate change, natural or human-induced, reinforces the impacts. Knowledge of surface and ground water processes operating in permafrost terrain is fundamental to planning, management and conservation. This book is an indispensable reference for libraries and researchers, an information source for practitioners, and a valuable text for training the next generations of cold region scientists and engineers.
    Type of Medium: Monograph available for loan
    Pages: XII, 563 Seiten , Illustrationen, Diagramme, Karten (teilweise farbig)
    ISBN: 9783642234613
    Language: English
    Note: Contents: 1 Introduction. - 1.1 The world cold regions. - 1.2 Water in frozen soils. - 1.3 Permafrost. - 1.3.1 Definitions. - 1.3.2. Distribution. - 1.3.3. Factors influencing permafrost occurence. - 1.4 Permafrost and hydrology. - 1.4.1 Permafrost hydrology. - 1.4.2 Hydrologic behavior of seasonal frost and permafrost. - 1.5 Environments of permafrost regions. - 1.5.1 Hydroclimatology. - 1.5.2 Geology. - 1.5.3 Glaciation. - 1.5.4 Physiography. - 1.5.5 Vegetation. - 1.5.6 Peat cover. - 1.6 Presentation of the book. - 2 Moisture and heat. - 2.1 Precipitation. - 2.1.1 General pattern. - 2.1.2 Cyclones. - 2.1.3 Recycling. - 2.1.4 Trace precipitation. - 2.2 Surface energy balance. - 2.3 Evaporation. - 2.3.1 Eddy Fluctuation Method. - 2.3.2 Aerodynamic method. - 2.3.3 Bowen Ratio Method. - 2.3.4 Priestley and Taylor Method. - 2.4 Energy balance of the active layer. - 2.4.1 Energy Balance. - 2.4.2 Thermal conductivity and heat capacity. - 2.5 Ground temperature. - 2.5.1 Penetration of temperature waves. - 2.5.2 Frost table development. - 2.6 Heat and moisture flows in frozen soils. - 2.6.1 Stefan's Algorithm. - 2.6.2 Near-Surface ground temperature. - 2.6.3 Moisture migration and ice lens formation. - 2.7 Ground ice. - 2.7.1 Types of ground ice. - 2.7.2 Excess ice. - 3 Groundwater. - 3.1 Groundwater occurence in permafrost. - 3.1.1 Suprapermafrost groundwater. - 3.1.2 Intrapermafrost groundwater. - 3.1.3 Subpermafrost groundwater. - 3.2 Groundwater recharge and circulation. - 3.2.1 Recharge. - 3.2.2 Groundwater movement. - 3.3 Groundwater discharge. - 3.3.1 Seeps. - 3.3.2 Springs. - 3.3.3 Baseflow. - 3.3.4 Ponds and lakes. - 3.4 Icings. - 3.4.1 Ground and spring icings. - 3.4.2 River icings. - 3.4.3 Icing dimension. - 3.4.4 Icing problems. - 3.5 Domed ice features. - 3.5.1 Frost mounds and icing mounds. - 3.5.2 Pingos. - References. - 4 Snow cover. - 4.1 Snow accumulation. - 4.1.1 Winter precipitation. - 4.1.2 Blowing snow. - 4.1.3 Terrain heterogeneity. - 4.1.4 Vegetation cover. - 4.2 Characteristics of the snow cover. - 4.2.1 Snow temperature and insulation. - 4.2.2 Snow metamorphism. - 4.2.3 Snow stratigraphy. - 4.3 Snowmelt processes. - 4.3.1 Radiation melt. - 4.3.2 Turbulent fluxes melt. - 4.3.3 Other melt terms. - 4.4 Snowmelt in permafrost areas. - 4.4.1 Tundra and Barren areas. - 4.4.2 Dirty snow. - 4.4.3 Shrub fields. - 4.4.4 Forests. - 4.5 Meltwater movement in snow. - 4.5.1 Dry snow. - 4.5.2 Wet snow. - References. - 5 Active layer dynamics. - 5.1 Freeze-back and winter periods. - 5.1.1 Snow cover and ground freezing. - 5.1.2 Moisture flux and ice formation. - 5.1.3 Vapor flux from soil to snow. - 5.2 Snowmelt period. - 5.2.1 Snowmelt and basal ice. - 5.2.2 Infiltration into frozen soil. - 5.2.3 Soil warming. - 5.2.4 Surface saturation, evaporation and runoff. - 5.3 Summer. - 5.3.1 Active layer thaw. - 5.3.2 Summer precipitation. - 5.3.3 Evaporation. - 5.3.4 Rainwater infiltration. - 5.3.5 Soil moisture. - 5.3.6 Groundwater. - References. - 6 Slope processes. - 6.1 Flow paths. - 6.1.1 Flow paths in snow. - 6.1.2 Surface and subsurface flows. - 6.1.3 Flow in bedrock areas. - 6.1.4 Flow in unconsolidated materials. - 6.2 Water sources. - 6.3 Factors influencing slope runoff generation. - 6.3.1 Microclimatic control. - 6.3.2 Topographic influence. - 6.3.3 Importance of the Frost table. - 6.3.4 Roles of organic materials. - 6.3.5 Bedrock control. - 6.4 Basin slopes in permafrost regions. - 6.4.1 High Arctic slopes. - 6.4.2 Low Arctic slopes. - 6.4.3 Subarctic slopes. - 6.4.4 Alpine permafrost zones. - 6.4.5 Precambrian bedrock terrain. - 6.5 Concepts for basin flow generation. - 6.5.1 Variable source area and fill-and-spill concepts. - 6.5.2 Heterogenous slopes. - References. - 7 Cold lakes. - 7.1 Types of lake. - 7.2 Lake ice. - 7.2.1 Lake ice regime. - 7.2.2 Ice formation and growth. - 7.2.3 Ice decay. - 7.3 Lake circulation. - 7.4 Hydrologic inputs. - 7.5 Lake evaporation. - 7.6 Lake outflow. - 7.6.1 Outflow conditions. - 7.6.2 Fill-and-Spill concept and lake outflow. - 7.7 Lake level. - 7.8 Large lakes. - 7.9 Permafrost and lakes. - References. - 8 Northern wetlands. - 8.1 Wetlands in permafrost regions. - 8.2 Factors favoring wetland occurence. - 8.2.1 Climate. - 8.2.2 Topography. - 8.2.3 Stratigraphy. - 8.2.4 Other factors. - 8.3 Hydrogeomorphic features in wetlands. - 8.3.1 Bog-related features. - 8.3.2 Fen-related features. - 8.3.3 Marshes and swamps. - 8.3.4 Shallow water bodies. - 8.4 Hydrologic behavior of wetlands. - 8.4.1 Seasonality of hydrologic activities. - 8.4.2 Wetland storage. - 8.4.3 Flow paths. - 8.4.4 Application of Fill-and-Spill concept. - 8.5 Patchy arctic wetlands. - 8.5.1 Wetlands maintained by snowmelt. - 8.5.2 Groundwater-fed wetlands. - 8.5.3 Valley bottom fens. - 8.5.4 Wetlands due to lateral inundation. - 8.5.5 Tundra ponds. - 8.5.6 Lake-fed and lake-bed wetlands. - 8.6 Extensive wetlands. - 8.6.1 Wet terrain. - 8.6.2 Ice-wedge polygon fields. - 8.6.3 Coastal plains. - 8.6.4 Deltas. - 8.6.5 Subarctic continental wetlands. - 8.7 Wetlands, permafrost and disturbances. - References. - 9 Rivers in cold regions. - 9.1 Drainage patterns. - 9.2 In-valley conditions. - 9.2.1 Geological setting for channels. - 9.2.2 River ice. - 9.2.3 River icing. - 9.2.4 In-channel snow. - 9.2.5 Permafrost. - 9.2.6 Alluvial environment. - 9.3 In-channel hydrology. - 9.3.1 Lateral inflow. - 9.3.2 Channel inflow. - 9.3.3 Vertical water exchanges. - 9.3.4 Storage in channels. - 9.4 Flow connectivity and delivery. - 9.4.1 Flow network integration. - 9.4.2 Decoupling of flow network. - 9.4.3 Flow delivery. - References. - 10 Basin hydrology. - 10.1 Basin outflow generation. - 10.1.1 The roles of snow. - 10.1.2 Meltwater from glaciers. - 10.1.3 Rainfall contribution. - 10.1.4 Groundwater supply. - 10.1.5 Evaporation losses. - 10.1.6 Permafrost effects. - 10.1.7 Consequences of basin storage. - 10.2 Streamflow hydrograph. - 10.3 Streamflow regimes. - 10.3.1 Nival regime. - 10.3.2 Proglacial regime. - 10.3.3 Pluvial regime. - 10.3.4 Spring-fed Regime. - 10.3.5 Prolacustrine regime. - 10.3.6 Wetland regime. - 10.4 Streamflow in large basins. - 10.4.1 Scaling up to large rivers. - 10.4.2 Flow generation in a large basin: the Liard river. - 10.4.3 Regulated discharge of large rivers. - 10.4.4 Flow in a sub-continental scale basin: Mackenzie basin. - 10.5 Basin water balance. - 10.5.1 Considerations in water balance investigation. - 10.5.2 Regional tendencies. - 10.5.3 Examples from permafrost environments. - 10.6 Permafrost basin hydrology: general remarks. - References. - Appendices. - Index.
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  • 2
    Monograph available for loan
    Monograph available for loan
    Leipzig : Teubner
    Associated volumes
    Call number: MOP 4059
    In: Wissenschaft und Hypothese
    Type of Medium: Monograph available for loan
    Pages: XVI, 346 S.
    Edition: 2., verb. Aufl.
    Series Statement: Wissenschaft und Hypothese 1
    Uniform Title: La science et l'hypothèse
    Language: German
    Location: MOP - must be ordered
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  • 3
    Call number: M 98.0150
    Type of Medium: Monograph available for loan
    Pages: Losebl.-Ausg.
    Language: German
    Location: Upper compact magazine
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  • 4
    Monograph available for loan
    Monograph available for loan
    Cambridge : Cambridge University Press
    Call number: M 14.0133 ; M 14.0159
    Description / Table of Contents: This book presents an innovative new approach to studying source mechanisms of earthquakes, combining theory and observation in a unified methodology, with a key focus on the mechanics governing fault failures. It explains source mechanisms by building from fundamental concepts such as the equations of elasticity theory to more advanced problems including dislocation theory, kinematic models and fracture dynamics. The theory is presented first in student-friendly form using consistent notation throughout, and with full, detailed mathematical derivations that enable students to follow each step. Later chapters explain the widely-used practical modelling methods for source mechanism determination, linking clearly to the theoretical foundations, and highlighting the processing of digital seismological data. Providing a unique balance between application techniques and theory, this is an ideal guide for graduate students and researchers in seismology, tectonophysics, geodynamics and geomechanics, and a valuable practical resource for professionals working in seismic hazard assessment and seismic engineering.
    Type of Medium: Monograph available for loan
    Pages: x, 302 S. : Ill., graph. Darst.
    ISBN: 9781107040274
    Classification:
    Seismology
    Language: English
    Note: Earthquakes and fault motion. pp. 1-21. doi:10.1017/CBO9781139628792.002 --- Processing and analysis of recorded seismic signals. pp. 22-40. doi:10.1017/CBO9781139628792.003 --- Mathematical representation of the source. pp. 41-62. doi:10.1017/CBO9781139628792.004 --- Point source models. pp. 63-89. doi:10.1017/CBO9781139628792.005 --- The seismic moment tensor. pp. 90-107. doi:10.1017/CBO9781139628792.006 --- Determination of point source mechanisms. pp. 108-134. doi:10.1017/CBO9781139628792.007 --- Kinematics of extended sources. pp. 135-162. doi:10.1017/CBO9781139628792.008 --- Determination of source dimensions. pp. 163-188. doi:10.1017/CBO9781139628792.009 --- Simple dynamic models. pp. 189-204. doi:10.1017/CBO9781139628792.010 --- Dynamics of fracture. Homogeneous models. pp. 205-231. doi:10.1017/CBO9781139628792.011 --- Fracture dynamics. Heterogeneous models. pp. 232-258. doi:10.1017/CBO9781139628792.012 --- Modeling earthquakes using fracture dynamics. pp. 259-283. doi:10.1017/CBO9781139628792.013
    Location: Upper compact magazine
    Location: Upper compact magazine
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  • 5
    Monograph available for loan
    Monograph available for loan
    Jena : Zeiss-Aerotopograph
    Associated volumes
    Call number: AWI E3-14-0024
    In: Deutsche antarktische Expedition 1938/39 mit dem Flugzeugstützpunkt der Deutschen Lufthansa A. G. M. S. "Schwabenland", Kapitän A. Kottas, ausgeführt unter der Leitung von Kapitän A. Ritscher
    Type of Medium: Monograph available for loan
    Pages: Seite 157-230 , Illustrationen , 3 Kartenbeilagen, 2 Stereobrillen, 1 Beilage ([26] S.)
    Series Statement: Deutsche Antarktische Expedition 1938/39 Band 1: Wissenschaftliche und fliegerische Ergebnisse
    Language: German
    Note: In Fraktur
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  • 6
    Monograph available for loan
    Monograph available for loan
    Associated volumes
    Call number: 3/S 01.0446(2012)
    In: Jahresbericht
    Type of Medium: Monograph available for loan
    Pages: 81 S. : farb. Ill., graph. Darst.
    Edition: Stand: Juli 2013
    Language: German
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  • 7
    Monograph available for loan
    Monograph available for loan
    Sankt-Peterburg : Sankt-Peterburgskij Gosudarstvennyj Universitet
    Call number: AWI Bio-13-0030
    Description / Table of Contents: Atlas contains photographic images of 91 plant species and pollen which are found in Lena River Delta as well as information about current conditions of their growth. This is a major advantage of this atlas as compared to other publications of this kind. All information is presented in Russian and English. All materials were collected in framework of the Russian-German expeditions "Lena-2009", "Lena-2010", "Lena-2011" and "Lena-2012". Photographs illustrate the general view of the plant, inflorescence and pollen grains in different positions and from high to low focus. Plants are grouped into families, where each family has its own color. Atlas is addressed not only to specialists in palynology, but to all who are interested in the flora and vegetation of the Arctic region, including students of geographical, biological and environmental fields.
    Type of Medium: Monograph available for loan
    Pages: 111 Seiten , Illustrationen
    ISBN: 9785439100361
    Language: Russian , English
    Note: Contents: Introduction. - Apiaceae. - Asteraceae. - Betulaceae. - Boraginaceae. - Brassicaceae. - Campanulaceae. - Caryophyllaceae. - Crassulaceae. - Cyperaceae. - Diapensiaceae. - Ericaceae. - Fabaceae. - Gentianaceae. - Hippuriadaceae. - Juncaceae. - Lentibulariaceae. - Liliaceae. - Onagraceae. - Papaveraceae. - Parnassiaceae. - Pinaceae. - Plumbaginaceae. - Poaceae. - Polemoniaceae. - Polygonaceae. - Portulacaceae. - Primulaceae. - Pyrolaceae. - Ranunculaceae. - Rosaceae. - Salicaceae. - Saxifragaceae. - Scrophulariaceae. - Valerianaceae. - Index of plants by family. - Alphabetical index of plants. , In englischer und russischer Sprache. , Teilw. in kyrillischer Schrift
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  • 8
    Call number: 2013/17
    Pages: 400 S.
    ISBN: 9783492302784
    Series Statement: Piper 30278
    Uniform Title: Powering the future
    Language: German
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  • 9
    Call number: 9/M 07.0421(375) ; https://doi.org/10.1144/SP375
    In: Geological Society special publication
    Description / Table of Contents: The historical links between geology and medicine are surprisingly numerous and diverse. This, the first ever volume dedicated to the subject, contains contributions from an international authorship of geologists, historians and medical professionals.Rocks, minerals, fossils and earths have been used therapeutically since earliest times and details recorded on ancient papyri, clay tablets, medieval manuscripts and early published sources. Pumice was used to clean teeth, antimony to heal wounds, clays as antidotes to poison, gold to cure haemorrhoids and warts, and gem pastes to treat syphilis and the plague, while mineral springs preserved health. Geology was crucial in the development of public health. Medical men who made important contributions to geology include Steno, Worm, Parkinson, Bigsby, William Hunter, Jenner, John Hulke, Conan Doyle, Gorini and various Antarctic explorers.
    Type of Medium: Monograph available for loan
    Pages: vi, 490 Seiten , Illustrationen, Diagramme, Karten
    ISBN: 9781862393561
    Series Statement: Geological Society special publication 375
    Classification:
    Geology
    Language: English
    Note: TABLE OF CONTENTS Geology as medicine and medics as geologists / Christopher J. Duffin / Geological Society, London, Special Publications, 375, 1-6, 23 August 2013, https://doi.org/10.1144/SP375.29 Lithotherapeutical research sources from antiquity to the mid-eighteenth century / Christopher J. Duffin / Geological Society, London, Special Publications, 375, 7-43, 4 September 2013, https://doi.org/10.1144/SP375.25 Cryptopalaeontology / Eladio Liñán, María Liñán and Joaquín Carrasco / Geological Society, London, Special Publications, 375, 45-64, 10 May 2013, https://doi.org/10.1144/SP375.14 The stomatological use of stones cited in the Kitab al-tasrif treatise (Abulcasis, 1000 CE) / Joaquín Carrasco and María Liñán / Geological Society, London, Special Publications, 375, 65-80, 11 December 2012, https://doi.org/10.1144/SP375.7 The gem electuary / Christopher J. Duffin / Geological Society, London, Special Publications, 375, 81-111, 17 December 2012, https://doi.org/10.1144/SP375.9 Medicinal terra sigillata: a historical, geographical and typological review / Arthur Macgregor / Geological Society, London, Special Publications, 375, 113-136, 15 November 2012, https://doi.org/10.1144/SP375.1 Materia medica in the seventeenth-century Paper Museum of Cassiano dal Pozzo / W. D. Ian Rolfe / Geological Society, London, Special Publications, 375, 137-156, 15 November 2012, https://doi.org/10.1144/SP375.3 History of the pharmaceutical use of pumice / Christopher J. Duffin / Geological Society, London, Special Publications, 375, 157-169, 17 December 2012, https://doi.org/10.1144/SP375.8 Pharmaceutical use of gold from antiquity to the seventeenth century / Renzo Console / Geological Society, London, Special Publications, 375, 171-191, 2 April 2013, https://doi.org/10.1144/SP375.12 Bezoar stones, magic, science and art / Maria Do Sameiro Barroso / Geological Society, London, Special Publications, 375, 193-207, 26 February 2013, https://doi.org/10.1144/SP375.11 Some early eighteenth century geological Materia Medica / Christopher J. Duffin / Geological Society, London, Special Publications, 375, 209-233, 2 April 2013, https://doi.org/10.1144/SP375.13 Religiosity and magic in some lithoiatric practices of European folk medicine / Massimo Aliverti / Geological Society, London, Special Publications, 375, 235-242, 23 August 2013, https://doi.org/10.1144/SP375.27 Britain’s spa heritage: a hydrogeological appraisal / John D. Mather / Geological Society, London, Special Publications, 375, 243-260, 2 April 2013, https://doi.org/10.1144/SP375.16 Groundwater – Medicine by the Glassful? / N. S. Robins and P. L. Smedley / Geological Society, London, Special Publications, 375, 261-267, 2 April 2013, https://doi.org/10.1144/SP375.17 Sunday Stone: an enduring metaphor of mining diseases and underground mining conditions / John H. Pearn and Christopher Gardner-Thorpe / Geological Society, London, Special Publications, 375, 269-278, 11 July 2013, https://doi.org/10.1144/SP375.22 The influence of geology in the development of public health / Beverly P. Bergman / Geological Society, London, Special Publications, 375, 279-287, 15 November 2012, https://doi.org/10.1144/SP375.6 From flesh to fossils – Nicolaus Steno’s anatomy of the Earth / Jakob Bek-Thomsen / Geological Society, London, Special Publications, 375, 289-305, 2 April 2013, https://doi.org/10.1144/SP375.15 Diagnosing fossilization in the Nordic Renaissance: an investigation into the correspondence of Ole Worm (1588–1654) / Ella Hoch / Geological Society, London, Special Publications, 375, 307-327, 17 September 2013, https://doi.org/10.1144/SP375.26 Education forms the tender mind / Christopher Gardner-Thorpe / Geological Society, London, Special Publications, 375, 329-337, 23 August 2013, https://doi.org/10.1144/SP375.28 James Parkinson’s ‘system of successive creations’ / Cherry Lewis / Geological Society, London, Special Publications, 375, 339-348, 15 May 2013, https://doi.org/10.1144/SP375.18 From obstetrics to oryctology: inside the mind of William Hunter (1718–1783) / J. J. Liston / Geological Society, London, Special Publications, 375, 349-373, 15 May 2013, https://doi.org/10.1144/SP375.21 John Jeremiah Bigsby, MD: British Army physician and pioneer North American geologist / Leonard G. Wilson / Geological Society, London, Special Publications, 375, 375-394, 15 May 2013, https://doi.org/10.1144/SP375.20 Five eighteenth-century medical polymaths / Gillian C. Hull / Geological Society, London, Special Publications, 375, 395-407, 15 November 2012, https://doi.org/10.1144/SP375.5 John Whitaker Hulke, surgeon and palaeontologist / Simon Wills / Geological Society, London, Special Publications, 375, 409-427, 22 February 2013, https://doi.org/10.1144/SP375.10 Dr Arthur Conan Doyle’s contribution to the popularity of pterodactyls / David M. Martill and Tony Pointon / Geological Society, London, Special Publications, 375, 429-443, 15 May 2013, https://doi.org/10.1144/SP375.19 Physicians and their contribution to the early history of earth sciences in Austria / Daniela Claudia Angetter, Bernhard Hubmann and Johannes Seidl / Geological Society, London, Special Publications, 375, 445-454, 15 November 2012, https://doi.org/10.1144/SP375.4 Medical geologists during the Heroic Age of Antarctic exploration / Henry Guly / Geological Society, London, Special Publications, 375, 455-462, 15 November 2012, https://doi.org/10.1144/SP375.2 Vomiting stones: mental illness and forensic medicine in 18th century Italy / Alessandro Porro, Carlo Cristini, Bruno Falconi, Antonia Francesca Franchini and Lorenzo Lorusso / Geological Society, London, Special Publications, 375, 463-468, 4 July 2013, https://doi.org/10.1144/SP375.23 Geology, conservation and dissolution of corpses by Paolo Gorini (1813–1881) / Lorenzo Lorusso, Bruno Falconi, Francesca Antonia Franchini and Alessandro Porro / Geological Society, London, Special Publications, 375, 469-474, 9 July 2013, https://doi.org/10.1144/SP375.24
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  • 10
    Call number: PIK N 531-13-0220
    Description / Table of Contents: Contents: Prolog ; EINLEITUNG - Im Homogenozän ; 1 Zwei Monumente ; TEIL EINS - Atlantikreisen ; 2. Die Tabakküste ; 3. Schlechte Luft ; TEIL ZWEI - Pazifikreisen ; 4. Schiffe voller Geld (Seide für Silber, Teil eins) ; 5. Liebeskrank-Gras, fremde Knollen und Jadereis (Seide für Silber,Teil zwei) ; TEIL DREI - Europa in der Welt ; 6. Der agroindustrielle Komplex ; 7. Schwarzes Gold ; TEIL VIER - Afrika in der Welt ; 8. Verrückte Suppe ; 9. Wald der Entlaufenen SCHLUSS - Lebensströme ; 10. In Bulalacao ; Anhang
    Type of Medium: Monograph available for loan
    Pages: 807 S. : Ill., graph. Darst., Kt.
    Edition: 2. Aufl.
    ISBN: 9783498045241
    Uniform Title: 1493. Uncovering the new world Columbus created
    Language: German
    Location: A 18 - must be ordered
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  • 11
    Series available for loan
    Series available for loan
    Hanover, NH : Corps of Engineers, U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-342
    In: Research report / Cold Regions Research and Engineering Laboratory
    Description / Table of Contents: CONTENTS: Abstract. - Preface. - Introduction. - Experimental procedure. - Results. - Work-hardening effect. - Strain rate sensitivity of flow stress. - Discussion. - Conclusions. - Literature cited.
    Description / Table of Contents: Single crystals of high purity ice deformed by uniaxial compression on an Instron machine showed remarkable work-hardening after about 8% strain. By changing the strain rate during compression tests in the plastic region of the stress-strain curve, an apparent activation volume V* and a dislocation mobility exponent m were calculated from the strain rate sensitivity of flow stress. The large work-hardening and the rapid increase in the value of m beyond about 10% strain indicate that the plastic flow in this region is controlled by dislocation intersections and nonconservative motion of jogs.
    Type of Medium: Series available for loan
    Pages: iii, 11 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 342
    Language: English
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  • 12
    Monograph available for loan
    Monograph available for loan
    Berlin : Links
    Call number: PIK N 454-14-0177
    Description / Table of Contents: Contents: Prolog: Eine Reise in die Welt des Wassers ; Die neue Wasserunsicherheit ; Das Zeitalter der Wasserfürsten ; Ein neues Wasserzeitalter ; Epilog: Die Macht des Wassers
    Type of Medium: Monograph available for loan
    Pages: 256 S.
    Edition: 1. Aufl.
    ISBN: 9783861537328
    Uniform Title: En reise i vannets fremtid
    Language: German
    Location: A 18 - must be ordered
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  • 13
    Monograph available for loan
    Monograph available for loan
    London [u.a.] : Academic Press
    Call number: M 98.0230
    Type of Medium: Monograph available for loan
    Pages: 890 S.
    Edition: 9th print.
    ISBN: 0125649223
    Series Statement: Probability and mathematical statistics : a series of monographs and textbooks
    Classification:
    Geodynamics
    Language: English
    Location: Upper compact magazine
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  • 14
    Call number: IASS 14.0061
    Type of Medium: Monograph available for loan
    Pages: 99 S.
    Edition: 7. Aufl. 2012
    ISBN: 9783932109126
    Series Statement: Wolffs Broschuren
    Uniform Title: Discours sur le bonheur
    Language: German
    Branch Library: IASS Library
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  • 15
    Monograph available for loan
    Monograph available for loan
    Berlin : Suhrkamp
    Call number: PIK D 024-14-0128
    Type of Medium: Monograph available for loan
    Pages: 204 S. : Ill., graph. Darst.
    Edition: 2. Aufl.
    ISBN: 9783518423851
    Uniform Title: 10 Billion
    Language: German
    Location: A 18 - must be ordered
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  • 16
    Call number: 4/M 14.0107
    Description / Table of Contents: THE FACE OF THE EARTH - The Legacy of Eduard Suess ist ein posthumes Buch vom "Vater der modernen Geologie" Eduard Suess. Viele seiner bahnbrechenden, wissenschaftlichen Thesen haben heute noch Gültigkeit, er prägte Begriffe wie Atmosphäre, Hydro-, Litho- und Biosphäre oder Tethys und Gondwana-Land. Eduard Suess war nicht nur ein Pionier der Geowissenschaften sondern auch ein Vorreiter innovativer Ideen als Politiker. Er initiierte eine weltweit beispielhafte Wasserversorgung einer Großstadt, die 1. Wiener Hochquellenwasserleitung, oder die Donauregulierung in Wien, geplant und ausgeführt als eine natürliche Schutzvorrichtung vor Überschwemmungen. Zum 100. Todestag des Kosmopoliten - er wurde in England geboren, lebte in Prag und Wien und forschte auf der ganzen Welt - am 26. April 2014 setzt "The Face of the Earth" ein Zeichen. Zitate aus der Feder des exzellenten Schreibers Eduard Suess , wissenschaftliche reflektierende Texte von einigen der besten Geologen der Gegenwart und faszinierende Bilder von einem der renommiertesten Fotografen machen das Buch zu einer würdigen Hommage.
    Type of Medium: Monograph available for loan
    Pages: 104 S. : 60 farb. Ill. ; 302 mm x 245 mm
    ISBN: 9783901753695
    Classification:
    Geology
    Language: English
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  • 17
    Series available for loan
    Series available for loan
    Hanover, NH : CRREL
    Associated volumes
    Call number: ZSP-202-296
    In: Research report
    Description / Table of Contents: A theory is developed to describe the percolation of water through isothermal snow with a vertical porosity gradient. While the necessary laboratory experiments have not been done for snow, concepts from the general theory of two phase flow through porous media are used in the development. The general solution for the one-dimensional problem is given, which, when combined with any periodic boundary condition, can be used to make quantitative predictions. The theory is applied to water percolation through firn on the upper Seward Glacier (Sharp, 1951a). Using appropriate values for the parameters, theory shows a wave of volume flux which travels down into the firn and develops features similar to those observed by Sharp. These include an initially symmetric wave which distorts with depth, continuous (rather than intermittent) downward flow beneath the surface, and a decreasing value for the wave crest with depth. The rate at which the waves propagate is calculated using the method of characteristics and is in fair agreement with the observed rate where the permeability of the bulk firn with ice layers is reduced by a factor of two over homogeneous snow samples studied in the laboratory (Kuroiwa, 1963). The theory predicts that the waves advance with a shock front which grows with depth. The shock front is thought to be only an approximation to the actual physical process
    Description / Table of Contents: CONTENTS: Preface. - Symbols. - Introduction. - Theory. - Darcy's Law. - Functional permeability. - Equations. - Characteristics. - Seward Glacier firn. - Discussion. - Summary. - Literature cited. - Abstract.
    Type of Medium: Series available for loan
    Pages: iv, 17 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 296
    Language: English
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  • 18
    Series available for loan
    Series available for loan
    Hanover, NH : Corps of Engineers, U.S. Army, Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-295
    In: Research report
    Description / Table of Contents: CONTENTS: Introduction. - Physical basis of microwave moisture sensing. - Physics of transmission and reflection. - General behavior of reflection and transmission of electromagnetic waves through media of finite thicknesses. - Water-content determination by reflection or transmission measurements on micro-waves. - Outlook for microwave moisture sensors. - Future studies. - Bibliography. - Appendix A. Computer program. - Abstract.
    Description / Table of Contents: Microwave instrumentation is used for nondestructive measurement of the water content of materials. The basis of all microwave moisture sensors is that the dielectric constants of material that contains water are a strong function of water content. The microwave moisture sensors based on a reflection or transmission principle are shown to have the disadvantage of requiring that a calibration be made for each sample thickness. Several alternative routes for developing reliable microwave moisture sensors are discussed.
    Type of Medium: Series available for loan
    Pages: iii, 17 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 295
    Language: English
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  • 19
    Call number: 9/M 07.0421(378)
    In: Geological Society special publication
    Description / Table of Contents: Decoding the complete history of Earth and our solar system requires the placing of the scattered pages of Earth history in a precise chronological order, and the 40Ar/39Ar dating technique is one of the most trusteddating techniques to do that. The 40Ar/39Ar method has been in use for more than 40 years, and has constantlyevolved since then. The steady improvement of the technique is largely due to a better understandingof the K/Ar system, an appreciation of the subtleties of geological material and a continuous refinement ofthe analytical tools used for isotope extraction and counting. The 40Ar/39Ar method is also one of the mostversatile techniques with countless applications in archaeology, tectonics, structural geology, orogenic processesand provenance studies, ore and petroleum genesis, volcanology, weathering processes and climate,and planetary geology. This volume is the first of its kind and covers methodological developments, modelling,data handling, and direct applications of the 40Ar/39Ar technique.
    Type of Medium: Monograph available for loan
    Pages: VI, 378 Seiten , Illustrationen, Diagramme, Karten
    ISBN: 978-1-86239-360-8
    Series Statement: Geological Society special publication 378
    Classification:
    Historical Geology
    Language: English
    Note: TABLE OF CONTENTS Introduction Advances in 40Ar/39Ar dating: from archaeology to planetary sciences – introduction / Fred Jourdan, Darren F. Mark and Chrystele Verati / Geological Society, London, Special Publications, 378, 1-8, 16 January 2014, https://doi.org/10.1144/SP378.24 Perspectives on 40Ar/39Ar dating / Ian McDougall / Geological Society, London, Special Publications, 378, 9-20, 30 September 2013, https://doi.org/10.1144/SP378.20 Methodological developments Some footnotes to the optimization-based calibration of the 40Ar/39Ar system / Paul R. Renne / Geological Society, London, Special Publications, 378, 21-31, 25 July 2013, https://doi.org/10.1144/SP378.17 Neutron-induced 37Ar recoil ejection in Ca-rich minerals and implications for 40Ar/39Ar dating / F. Jourdan and P. R. Renne / Geological Society, London, Special Publications, 378, 33-52, 25 July 2013, https://doi.org/10.1144/SP378.15 Direct measurement of recoil effects on 40Ar/39Ar standards / Chris M. Hall / Geological Society, London, Special Publications, 378, 53-62, 13 March 2013, https://doi.org/10.1144/SP378.7 FCs-EK: a new sampling of the Fish Canyon Tuff 40Ar/39Ar neutron flux monitor / L. E. Morgan, D. F. Mark, J. Imlach, D. Barfod and R. Dymock / Geological Society, London, Special Publications, 378, 63-67, 30 September 2013, https://doi.org/10.1144/SP378.21 Petrology and geochronology of ‘muscovite age standard’ B4M / Alexandra R. Heri, Martin Robyr and Igor M. Villa / Geological Society, London, Special Publications, 378, 69-78, 24 January 2013, https://doi.org/10.1144/SP378.2 Argon extraction from geological samples by CO2 scanning laser step-heating / D. N. Barfod, D. F. Mark, A. Tait, R. C. Dymock and J. Imlach / Geological Society, London, Special Publications, 378, 79-90, 24 October 2013, https://doi.org/10.1144/SP378.23 The multi-diffusion domain model: past, present and future / T. Mark Harrison and Oscar M. Lovera / Geological Society, London, Special Publications, 378, 91-106, 13 March 2013, https://doi.org/10.1144/SP378.9 Diffusion of Ar in K-feldspar: Present and absent / Igor M. Villa / Geological Society, London, Special Publications, 378, 107-116, 24 January 2013, https://doi.org/10.1144/SP378.4 40Ar/39Ar geochronology and the diffusion of 39Ar in phengite–muscovite intergrowths during step-heating experiments in vacuo / Marnie A. Forster and Gordon S. Lister / Geological Society, London, Special Publications, 378, 117-135, 25 July 2013, https://doi.org/10.1144/SP378.16 Ar diffusion and solubility measurements in plagioclases using the ultra-violet laser depth-profiling technique / Jo-Anne Wartho, Simon P. Kelley and Stephen C. Elphick / Geological Society, London, Special Publications, 378, 137-154, 25 July 2013, https://doi.org/10.1144/SP378.13 Modelling effect of sericitization of plagioclase on the 40K/40Ar and 40Ar/39Ar chronometers: implication for dating basaltic rocks and mineral deposits / Chrystèle Verati and Fred Jourdan / Geological Society, London, Special Publications, 378, 155-174, 25 July 2013, https://doi.org/10.1144/SP378.14 The other isotopes: research avenues based on 36Ar, 37Ar and 38Ar / Grenville Turner and Ray Burgess / Geological Society, London, Special Publications, 378, 175-188, 13 March 2013, https://doi.org/10.1144/SP378.8 Applications: Tectonics 40Ar/39Ar Thermochronology on Central China Orogen: Cooling, uplift and implications for orogeny dynamics / Fei Wang, Rixiang Zhu, Quanlin Hou, Dewen Zheng, Liekun Yang, Lin Wu, Wenbei Shi, Huile Feng, Haiqing Sang, Hongyuan Zhang and Qing Liu / Geological Society, London, Special Publications, 378, 189-206, 24 January 2013, https://doi.org/10.1144/SP378.3 40Ar/39Ar ages of crystallization and recrystallization of rock-forming polyhalite in Alpine rocksalt deposits / C. Leitner, F. Neubauer, J. Genser, S. Borojević-Šoštarić and G. Rantitsch / Geological Society, London, Special Publications, 378, 207-224, 24 January 2013, https://doi.org/10.1144/SP378.5 Persistent long-term (c. 24 Ma) exhumation in the Eastern Alaska Range constrained by stacked thermochronology / Jeff A. Benowitz, Paul W. Layer and Sam Vanlaningham / Geological Society, London, Special Publications, 378, 225-243, 20 June 2013, https://doi.org/10.1144/SP378.12 40Ar/39Ar hornblende provenance clues about Heinrich event 3 (H3) / Greg E. Downing, Sidney R. Hemming, Anne Jost and Martin Roy / Geological Society, London, Special Publications, 378, 245-263, 30 September 2013, https://doi.org/10.1144/SP378.18 Observation of centimetre-scale argon diffusion in alkali feldspars: implications for 40Ar/39Ar thermochronology / Stephanie Flude, Alison M. Halton, Simon P. Kelley, Sarah C. Sherlock, James Schwanethal and Camilla M. Wilkinson / Geological Society, London, Special Publications, 378, 265-275, 10 January 2013, https://doi.org/10.1144/SP378.25 Applications: Volcanology 40Ar/39Ar age constraints on the Haifanggou and Lanqi formations: When did the first flowers bloom? / Su-Chin Chang, Haichun Zhang, Sidney R. Hemming, Gary T. Mesko and Yan Fang / Geological Society, London, Special Publications, 378, 277-284, 24 January 2013, https://doi.org/10.1144/SP378.1 Timing of geothermal activity in an active island-arc volcanic setting: First 40Ar/39Ar dating from Bouillante geothermal field (Guadeloupe, French West Indies) / C. Verati, P. Patrier-Mas, J. M. Lardeaux and V. Bouchot / Geological Society, London, Special Publications, 378, 285-295, 30 September 2013, https://doi.org/10.1144/SP378.19 Applications: Planetary sciences Issues in dating young rocks from another planet: Martian shergottites / Jisun Park, Donald D. Bogard, Laurence E. Nyquist and G. F. Herzog / Geological Society, London, Special Publications, 378, 297-316, 20 June 2013, https://doi.org/10.1144/SP378.10 A laser probe 40Ar/39Ar investigation of poikilitic shergottite NWA 4797: implications for the timing of shock metamorphism / Erin L. Walton, Simon Kelley, Christopher D. K. Herd and Anthony J. Irving / Geological Society, London, Special Publications, 378, 317-332, 20 June 2013, https://doi.org/10.1144/SP378.11 40Ar/39Ar ages of impacts involving ordinary chondrite meteorites / Timothy D. Swindle, D. A. Kring and J. R. Weirich / Geological Society, London, Special Publications, 378, 333-347, 24 January 2013, https://doi.org/10.1144/SP378.6 A high-precision 40Ar/39Ar age for hydrated impact glass from the Dellen impact, Sweden / D. F. Mark, P. Lindgren and A. E. Fallick / Geological Society, London, Special Publications, 378, 349-366, 30 September 2013, https://doi.org/10.1144/SP378.22
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  • 20
    Call number: AWI P1-14-0015 ; PIK N 454-14-0080
    Description / Table of Contents: Contents: - 1 Land, Leute und Bodenschätze. - 1.1 Die Arktis und ihre Grenzen: eine physisch-geographische Einführung. - 1.2 Geologische Entwicklung und tektonischer Bau der Antarktis. - 1.3 Geschichte der antarktischen Entdeckungen. - 1.4 Abriss der Geschichte der Entdeckung der Arktis. - 1.5 Die indigenen Völker im Norden: frühere und gegenwärtige Entwicklungen. - 1.6 Die mittelalterliche Besiedlung Westgrönlands durch die Wikinger - ein fehlgeschlagenes Experiment?. - 1.7 Permafrost - ein weit verbreitetes Klimaphänomen der Arktis und Subarktis. - 1.8 Die Geologie der Arktis, ihre Bodenschätze und ihr rechtlicher Status. - 2 Meeresströmung, Stürme und Eis. - 2.1 Struktur, Dynamik und Bedeutung des antarktischen Wasserringes. - 2.2 Wassermassenänderungen im Arktischen Ozean. - 2.3 Änderungen in der Nordatlantischen Tiefenwasserbildung und ihre Auswirkungen auf das Europäische Klima. - 2.4 Roaring Forties und Riesenwellen - Gefahren im Südpolarmeer. - 2.5 Polare Mesozyklonen: Die Hurrikane der Polargebiete. - 2.6 Die Wechselwirkung zwischen antarktischen Schelfeisgebieten und dem Ozean und der Beitrag zur ozeanischen Wassermassenbildung. - 2.7 Die Massenbilanzen des antarktischen und grönländischen Inlandeises und der Charakter ihrer Veränderungen. - 2.8 Veränderung der Dicke und Ausdehnung des Polarmeereises. - 3 Flora, Fauna und Ökosysteme. - 3.1 Flora und Vegetation des terrestrischen Bereichs. - 3.2 Ökophysiologie und Wachstum arktischer Pflanzen im Klimawandel. - 3.3 Das Meereis als Lebensraum. - 3.4 Einfluss von Fischerei und Klima auf die Bestände des antarktischen Krill. - 3.5 Klimabedingte ökologische Veränderungen in den Bodenfaunen polarer Schelfmeere. - 3.6 Die Fische des Nord- und Südpolarmeeres. - 3.7 Vogelwelt der Polarregionen und ihre Gefährdung. - 3.8 Robben und Robbenschlag in der Antarktis. - 3.9 Arktische Robben und Eisbären - Auswirkungen von Klimaerwärmung und Ressourcennutzung. - 3.10 Warnsignale Walfang. - 3.11 Marine Biodiversität in den Polarregionen nach der Volkszählung der Meere. - 4 Das Weltklima und die Polarregionen. - 4.1 Wechselwirkungen zwischen arktischem Meereis und der atmosphärischen Zirkulation. - 4.2 Niederschläge in den Polarregionen und ihre Erfassung. - 4.3 Atmosphärische Messungen an der AWIPEV Station Spitzbergen. - 4.4 Das Polarlicht. - 4.5 Erwärmung der Polarregionen in den letzten 50 Jahren: Ursachen und Folgen. - 4.6 Verhalltes Warnsignal: Die Erwärmung ds Nordpolargebietes während der ersten Hälfte des 20. Jahrhunderts. - 4.7 Die Rolle ozeanischer Wärmetransporte für das Klima der Arktis im letzten Jahrtausend. - 4.8 Polareiskerne - Archive globaler Klima- und Umweltveränderungen. - 4.9 Die polaren Meeressedimente als Archiv des Weltklimas. - 4.10 Der katabatische Wind über den polaren Eisschilden. - 4.11 Meeresspiegelanstieg - Eisschilde, Gletscher und thermische Ausdehnung: eine kurze Übersicht. - 4.12 Anmerkungen über Veränderungen in den Eisströmen der Eisschilde. - 4.13 Permafrostbeeinflusste Böden (Kryosole) im Klimawandel. - 4.14 Methanhydrate in arktischen Sedimenten - Einfluss auf Klima und Stabilität der Kontinentalränder. - 5 Forschung, Gefährdung und Schutz. - 5.1 Über die deutschen Forschungsaktivitäten in den Polarregionen. - 5.2 Rückgang des Ozons in der Stratosphäre der Polarregionen. - 5.3 Ausbreitung von Schadstoffen in die Polarregionen. - 5.4 Anreicherung und Effekte von organischen Schadstoffen in der polaren Umwelt. - 5.5 Tourismus und seine Auswirkungen. - 5.6 Globale Gefahren durch intensive Nutzung der Taiga-Wälder. - 5.7 Die Nutzung von Öl- und Gasvorkommen in einer nahezu eisfreien Arktis. - 5.8 Antarktis im Spannungsfeld zwischen Forschung, Tourismus und Umweltschutz. - 5.9 Meeresschutzgebiete in der Antarktis: Lassen sich Schutz- und Fischerei-Interessen verbinden?. - 5.10 Gebietsstreitigkeiten in der Arktis - Ist eine friedliche Beilegung mittels Abgrenzung erreichbar?. - 5.11 Umweltschutz in einer Arktis im Wandel. - 6 Sachregister.
    Description / Table of Contents: Die Polarregionen üben trotz ihrer abgelegenen Lage einen erheblichen Einfluss auf das Weltklima aus. Dies hängt besonders mit den bedeutenden Kopplungsprozessen zwischen dem Eis (Eisschilde, Meereis, Schnee und Permafrost) und der atmosphärischen sowie ozeanischen Zirkulation zusammen. Das Abschmelzen aller polaren Eisschilde würde beispielsweise einen globalen Anstieg des Meeresspiegels um etwa 70 m bewirken. Aber auch schon geringe Schwankungen im polaren Eisvolumen führen zu merklichen Veränderungen des Meeresspiegels. Die Klima-Prognosen der letzen Jahre haben sich weitgehend bestätigt. Die heutigen Messungen zeigen sogar, dass sich das Klima eher schneller ändert als erwartet. Die beobachtete Erderwärmung während des 20. Jahrhunderts hat sich in diesem Jahrhundert fortgesetzt; zurzeit beträgt die mittlere globale Erwärmung über den Kontinenten bereit 0,9°C. Diese Entwicklung wird sich fortsetzen, wenn die Anreicherung der Atmosphäre mit Treibhausgasen (vor allem CO2) anhält. Besorgniserregend ist die Tatsache, dass die heute emittierten CO2-Mengen Jahrhunderte in der Atmosphäre verbleiben. Die Folgen des Klimawandels sind vielfältig. Der Meeresspiegelanstieg stieg von 1,7 mm/Jahr in den 1970/80er Jahren auf jetzt 3 mm/Jahr. Der 5. Sachstandsbericht des IPCC (2013) gibt für den Zeitraum 1993 - 2010 einen globalen mittleren Meeresspiegelanstieg von 3,2 mm/Jahr an. Viele Inselstaaten und tief gelegene Küstenländer, die am wenigsten zur Erderwärmung beitragen, werden am härtesten von den Folgen betroffen sein. Sie sind nicht in der Lage, sich mit Dämmen zu schützen. Die Erwärmung ist am stärksten in der nördlichen Polarregion. Die eisbedeckte Fläche hat sich dort fast halbiert. Auch der Westantarktische Eisschild schrumpft; dort gehen 180 km3 Eis jährlich verlären. Zahlreiche polare Arten, zum Beispiel der Eisbär, drohen ihre Lebensräume zu verlieren. Wir befinden uns bereits jetzt in einem Klimawandel, der bei ungenügendem Klimaschutz zu Temperaturen führen kann, die die Erde seit mindestens einer Million Jahre nicht mehr erlebt hat. Studien zeigen, dass der Mensch maßgeblich für den jetzigen Klimawandel verantwortlich ist. Mit diesen und anderen Themen befassen sich rund 100 Experten im vorliegenden Buch. Die Beiträge sind leicht verständlich geschrieben.
    Type of Medium: Monograph available for loan
    Pages: 375 Seiten , Illustrationen
    ISBN: 9783980966863
    Language: German
    Location: AWI Reading room
    Location: A 18 - must be ordered
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  • 21
    Series available for loan
    Series available for loan
    Hanover, NH : Corps of Engineers, U.S. Army, Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-334
    In: Research report
    Description / Table of Contents: CONTENTS: Abstract. - Preface. - List of symbols and associated dimensions. - Introduction and purpose. - Site characteristics. - Outline of study scheme. - Analysis. - Heat conduction to the drill hole. - Heat transfer between conduit wall and coolant. - Heat transfer between surface pipe and air. - Total heat extraction process. - Example calculations. - Estimate of basal water thickness and flow rates. - Summary of investigations of multiple-hole. - Literature cited.
    Description / Table of Contents: A scheme for cooling the lower portion of the edge of the Greenland ice sheet, which abuts a potential mining operation, is examined. The magnitude of cooling which may be accomplished by drilling a series of holes about the periphery of the mine site is determined as a function of hole size, spacing and time. Refrigeration is accomplished by pumping a coolant downhole in a central pipe, then uphole in an annulus between the pipe and hole wall, and then through a thin-walled pipe exposed to the surface climate above the ice sheet. It was found possible to achieve a temperature change in the ice of the order of -1°C with hole spacings and pumping requirements which are considered reasonable. Other effects are briefly examined and include an estimate of the basal water thickness and flow rates.
    Type of Medium: Series available for loan
    Pages: vii, 19 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 334
    Language: English
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  • 22
    Call number: AWI P5-15-0006
    Type of Medium: Monograph available for loan
    Pages: XIII, 495 Seiten
    Edition: printed original edition 1967
    ISBN: 0-8047-0272-1
    Language: English
    Note: Contents: 1 Introduction. - 2 Geology of the Floor of Bering and Chukchi Seas - American Studies. - 3 Late Quaternary Sediments of Bering Sea and the Gulf of Alaska. - 4 Quaternary Marine Transgressions in Alaska. - 5 Quaternary Geology of the Alaskan Shore of Chukchi Sea. - 6 Quaternary Geology of Western Seward Peninsula, Alaska. - 7 Paleogeography of Chukotka During Late Neogene and Quaternary Time. - 8 Radiocarbon Chronology in Siberia. - 9 Neogene and Early Quaternary Vegetation of Northwestern North America and Northeastern Asia. - 10 Quaternary Vegetational History of Arctic Alaska. - 11 Vegetation of Eastern Siberia During the Anthropogene Period. - 12 Distribution, Ecology, and Cytology of the Ogotoruk Creek Flora and the History of Beringia. - 13 Mammal Remains of Pre-Wisconsin Age in Alaska. - 14 On the Origin of the Mammalian Fauna of Canada. - 15 The Effect of the Bering Land Bridge on the Quaternary Mammalian Faunas of Siberia and North America. - 16 Palearctic-Nearctic Mammalian Dispersal in the Late Cenozoic. - 17 The Stratigraphy of Tjbrnes, Northern Iceland, and the History of the Bering Land Bridge. - 18 Cenozoic Migrations of Marine Invertebrates Through the Bering Strait Region. - 19 Marine Mammals and the History of Bering Strai. - 20 Depth Changes in Bering Sea During the Upper Quaternary, as Indicated by Benthonic Foraminifera. - 21 Diatom Floras and the History of Okhotskand Bering Seas. - 22 On Migrations of Hunters across the Bering Land Bridge in the Upper Pleistocene. - 23 Human Migration and Permanent Occupation in the Bering Sea Area. - 24 The Cenozoic History of Beringia - A Synthesis. - General Index. - Index to Faunal and Floral Taxa.
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  • 23
    Call number: IASS 15.0023
    Type of Medium: Monograph available for loan
    Pages: 437 S.
    ISBN: 9783593391694
    Uniform Title: Commonwealth
    Language: German
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  • 24
    Call number: AWI A4-15-0009
    Type of Medium: Monograph available for loan
    Pages: 174 S. : Ill., graph. Darst., Kt.
    ISBN: 9788389743060
    Language: English
    Note: Contents: Preface. - 1. Introduction. - 1.1. Research purpose. - 1.2. Research area and methodology. - 2. Atmospheric circulation and dynamic conditions. - 2.1. Atmospheric circulation. - 2.2. Atmospheric pressure. - 2.3. Wind. - 3. Radiation conditions. - 3.1. Cloud cover. - 3.2. Sunshine duration. - 3.3. Solar radiation. - 4. Thermal conditions. - 4.1. Ground temperature. - 4.2. Air temperature. - 5. Higric conditions. - 5.1. Relative air humidity. - 5.2. Precipitation. - 6. The influence of atmospheric circulation on temperature and humidity conditions. - 6.1. The influence of atmospheric circulation on temperature conditions. - 6.2. The influence of atmospheric circulation on humidity conditions. - 7. Comparison of meteorological conditions in the area of Forlandsundet in the summer seasons of 2010-2011 with meteorological conditions in the years of 1975-2011. - 7.1. Introduction. - 7.2. Kaffiøyra. - 7.3. Waldemar Glacier. - Appendixes.
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  • 25
    Call number: ZSP-202-346
    In: Research report / Cold Regions Research and Engineering Laboratory, 346
    Description / Table of Contents: CONTENTS: Abstract. - Preface. - USA CRREL project and personnel involvement. - Part I. Introduction. - Background. - Literature review. - Part II. CRREL investigations from 1970 - 1974. - Initial literature survey (1970). - Oil detection kit development. - Survey of Cape Simpson, Alaska, natural crude oil seepages (1970). - Haines-Fairbanks military pipeline investigations (1971-1973). - Barrow investigations (1970-1974). - Fairbanks and Fox investigations. - Germination studies. - Physiological studies. - Dispersant studies. - Microbiological investigations. - Field investigations of accidental petroleum losses. - Part III. Recent related literature. - Part IV. Conclusions and recommendations. - USA CRREL reports, publications and presentations on Alaska oil spill research. - Literature cited.
    Description / Table of Contents: Knowledge concerning the biological effects of oil pollution on arctic and subarctic terrestrial ecosystems is limited. USA CRREL research personnel conducted investigations from 1970 through 1974 to expand information in this field. Objectives were to: 1) define the ecosystems most sensitive to the presence of crude oil or its refined products, 2) quantify and understand the injury response, and 3) establish time frames for manifestation of damage and natural restorative processes in arctic and subarctic regions. This was accomplished through: 1) surveys of natural oil seepages and past accidential spills in the Arctic and Subarctic, 2) initiation of controlled oil spills and 3) detailed laboratory investigations. Results demonstrated that terrestrial oil spills will to some degree be detrimental to both arctic and subarctic plant communities. Degree and longevity of damage will be influenced primarily by the magnitude of the spill, season of occurrence and existing soil moisture content. Rapid recovery of plant communities subjected to spills will occur only if root systems remain relatively unaffected. Damage will be more extensive and long-term when root systems are saturated with oil. Effects of damage will be manifested gradually over several seasons being influenced by winter stresses. Variation does exist in plant species susceptibility. Carex aquatilis, a predominant sedge of the arctic, is markedly resistant to crude oil damage. In the taiga Picea mariana is very susceptible. Plant recovery can be enhanced through the application of fertilizer. Fertilization, in addition to its direct effect on plant nutrition, will stimulate microbial decomposition of crude oil.
    Type of Medium: Series available for loan
    Pages: vii, 66 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 346
    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-202-345
    In: Research report / Cold Regions Research and Engineering Laboratory, 345
    Description / Table of Contents: CONTENTS: Abstract. - Preface. - List of symbols. - Introduction. - Previous work. - Experimental design. - The radioisotope 22Na. - Description of apparatus. - Experimental procedure. - Correction of profiles. - Assumptions. - Decay correction. - Boundary correction. - Error analysis. - Results. - Salinity data. - Temperature data. - Growth velocity. - Discussion. - Brine and ice properties. - Brine salinity. - Brine density. - Brine volume. - Brine latent heat of freezing. - Brine viscosity, specific heat, and thermal conductivity. - Ice properties. - Theoretical brine expulsion model. - Continuity equations. - Thermal energy equation. - Simplified brine expulsion equations. - Brine expulsion in NaCl ice. - Results. - Discussion. - Gravity drainage in NaCl ice. - Application of results to natural sea ice. - Effective distribution coefficient. - Previous work. - Experimental procedure and results. - Conclusions. - Literature cited. - Appendix A: Profile correction data. - Appendix B: Program "correct" and sample output. - Appendix C: Tabulation of salinity data. - Appendix D: Tabulation of profile data. - Appendix E: Time-ice thickness equations (Runs 2 and 3). - Appendix F: Tabulation of distribution coefficient data.
    Description / Table of Contents: To obtain a better understanding of the desalination of natural sea ice, an experimental technique was developed to measure sequential salinity profiles of a growing sodium chloride ice sheet. Using radioactive 22Na as a tracer, it was possible to determine both the concentration and movement of the brine within the ice without destroying the sample. A detailed temperature and growth history of the ice was also maintained so that the variation of the salinity profiles could be properly interpreted. Since the experimental salinity profile represented a smoothed, rather than a true salinity distribution, a deconvolution method was devised to restore the true salinity profile. This was achieved without any significant loss of end points. In all respects, the salinity profiles are similar to those of natural sea ice. They have a characteristic C-shape, and clearly exhibit the effects of brine drainage. Not knowing the rates of brine expulsion or gravity drainage, the variation of the salinity profiles during the period of ice growth could be explained by either process. To determine the relative importance of the desalination mechanisms, a theoretical brine expulsion model was derived and compared to the experimental data. As input for the model, equations describing the variation of some properties of NaCl brine with temperature were derived. These included the brine salinity, viscosity, specific heat, thermal conductivity, and latent heat of freezing. The theoretical brine expulsion model was derived by performing mass and energy balances over a control volume of NaCl ice. A simplified form of the model, when compared to the experimental results, indicated that brine expulsion was only important during the first several hours of ice growth, and later became a minor desalination process relative to gravity drainage which continued to be the dominant mechanism for the remainder of the study period (up to 6 weeks). The rate of gravity drainage was found to be dependent on the brine volume and the temperature gradient of the ice. As either the brine volume or temperature gradient was increased, the rate of change of salinity due to gravity drainage increased. The equation commonly used to calculate the effective distribution coefficient (Weeks and Lofgren 1967) was modified and improved by taking brine drainage into account. An expression was also derived to give the distribution coefficient at very low growth velocities.
    Type of Medium: Series available for loan
    Pages: vii, 85 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 345
    Language: English
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    Call number: 18/M 14.0226
    Description / Table of Contents: Das mobile Web stellt Webdesigner vor völlig neue Herausforderungen: Mit was für einem Device greift ein Nutzer auf eine Website zu? Welche Hardware bringt ein Gerät mit? Welche Bildschirmgröße und -auflösung hat es? All diese Faktoren beeinflussen die Darstellung der Website und machen ein flexibles Design immer wichtiger. Responsive Webdesign setzt genau hier an: Es sorgt dafür, dass sich eine Website an das Gerät anpasst, mit dem sie aufgerufen wird.Dieses hoch gelobte Buch richtet sich an Webdesigner und -entwickler, die Grundkenntnisse in HTML und CSS mitbringen und sich nun mit Responsive Webdesign vertraut machen möchten. Behandelt werden sowohl technische Aspekte als auch konzeptionelle Fragen, die dieser Designansatz mit sich bringt.Was ist Responsive Webdesign?Mit dieser Frage beschäftigen Sie sich zu Beginn des Buchs. Sie erfahren, wie Sie ein Design entwickeln, das Ihre Inhalte auf allen Geräten so übersichtlich und benutzerfreundlich wie möglich darstellt. Zum Einsatz kommt dabei eine Kombination aus Fluid Layouts, Media Queries und Responsive Media.Feilen Sie an der User ExperienceWas ist zu bedenken, wenn eine Website sowohl auf Smartphones als auch auf Desktoprechnern angenehm zu nutzen sein soll? Wie sollten die Bedienelemente der Website beschaffen sein? Welche Interaktionsmöglichkeiten wollen Sie bieten? Und ganz wichtig: Was bedeutet das für die Inhalte Ihrer Website? Fragen wie diese werden eingehend diskutiert und mit Praxisbeispielen illustriert. So entwickeln Sie ein gutes Gespür, worauf Sie bei eigenen Projekten achten sollten.Verbessern Sie die PerformanceBenutzer erwarten heutzutage nicht nur, dass eine Website angenehm zu bedienen ist, sondern auch, dass sie schnell lädt. Sorgen Sie deshalb unbedingt für eine gute Performance Ihrer Website! Lernen Sie verschiedene Möglichkeiten kennen, das Download-Volumen Ihrer Website zu reduzieren und sie so vor allem für mobile Surfer attraktiver zu machen.
    Type of Medium: Monograph available for loan
    Pages: xvi, 287 S. , Ill., graph. Darst.
    Edition: 1. Aufl.
    ISBN: 9783955614331
    Series Statement: O'Reillys basics
    Uniform Title: Implementing responsive design
    Classification:
    Informatics
    Language: German
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    Journal available for loan
    Journal available for loan
    Albany, California : Seismological Society of America
    Call number: Z 92.0057 ; Z 92.0057 ; Z 92.0057 ; Z 92.0057 ; Z 92.0057 ; Z 92.0057 ; Z 92.0057 ; Z 92.0057 ; Z 92.0057
    Type of Medium: Journal available for loan
    ISSN: 0037-1106 , 1943-3573
    Language: English
    Location: Lower compact magazine
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    Call number: Z 93.0723
    ISSN: 0016-7746
    Former Title: Geologie en Mijnbouw
    Language: English
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    Washington : American Geophysical Union
    Call number: Z 93.0563
    ISSN: 0016-8521
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    Freiberg : Sächsisches Landesamt für Umwelt und Geologie / Bereich Boden und Geologie
    Call number: Z 92.0224
    ISSN: 0863-2200
    Language: German
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    Call number: Z 93.0312
    ISSN: 0195-928X
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    Tulsa : Society for Sedimentary Geology
    Call number: Z 94.0319
    ISSN: 1527-1404
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    Tucson : University of Arizona
    Call number: ZN-94.0329
    ISSN: 0033-8222
    Language: English
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    Call number: Z 94.0289
    ISSN: 1023-5809
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    Helsinki [u.a.] ; 326.1984 -
    Call number: Z 92.0098
    ISSN: 0367-522X
    Former Title: Bulletin / Geologinen Tutkimuslaitos
    Language: English
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    Triest : Osservatorio Geofisico Sperimentale
    Call number: Z 92.0525
    ISSN: 0006-6729
    Language: English
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    Call number: Z 91.0224
    ISSN: 0098-8847
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    Journal available for loan
    Journal available for loan
    Prague : Univerzita Karlova
    Call number: Z 91.0119
    Type of Medium: Journal available for loan
    ISSN: 0001-7132
    Language: English
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    Kopenhagen : Munksgaard
    Call number: Z 93.0491
    ISSN: 0021-8898
    Language: English
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    Call number: Z 91.0884
    ISSN: 0012-0308
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    Bratislava : Slovak Academic Press
    Call number: Z 91.0686
    ISSN: 1335-0552
    Language: English
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  • 44
    Call number: ZSP-202-315
    In: Research report
    Description / Table of Contents: CONTENTS: Preface. - Introduction. - Part 1:Mesoscale strain measurements on the Beaufort Sea pack ice. - Abstract. - Introduction. - Previous work. - Site location. - Results. - Correlation of synoptic aerial photography with measured strains. - Correlation of estimated wind stress and strain. - Conclusions. - Literature cited. - Part II: Structure of a multiyear pressure ridge. - Abstract. - Introduction. - Profiles. - Internal properties. - Largest ridge sail. - Conclusions. - Literature cited. - Part III: Top and bottom roughness of a multiyear ice floe. - Abstract. - Introduction. - Results. - Literature cited. - Part IV:Airphoto analysis of ice deformation in the Beaufort Sea Abstract. - Introduction. - Study area. - Method of analysis. - Ice deformations. - Net deformational changes. - Pressure ridge distribution. - Summary and conclusions. - Literature cited. - Part V: Data on morphological and physical characteristics of sea ice in the Beaufort Sea.
    Description / Table of Contents: Mesoscale strain measurements on the Beaufort Sea pack ice; Structure of a multiyear pressure ridge; Top and bottom roughness of a multiyear ice floe; Airphoto analysis of ice deformation in the Beaufort Sea; Data on morphological and physical characteristics of sea ice in the Beaufort Sea.
    Type of Medium: Series available for loan
    Pages: iii, 66 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 315
    Language: English
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    Call number: S 90.0086
    ISSN: 0085-6932
    Language: English
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  • 46
    Journal available for loan
    Journal available for loan
    Richmond, California : Earthquake Engineering Research Center, University of California
    Call number: Z 93.0334
    Type of Medium: Journal available for loan
    ISSN: 0363-5732
    Language: English
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  • 47
    Monograph available for loan
    Monograph available for loan
    San Diego [u.a.] : Acad. Press
    Call number: MOP 33002
    Type of Medium: Monograph available for loan
    Language: English
    Location: MOP - must be ordered
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    Monograph available for loan
    Monograph available for loan
    Berlin
    Call number: MOP Per 581
    Type of Medium: Monograph available for loan
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    Oxford [u.a.] : Pergamon Press
    Call number: ZSP-214
    Language: English
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  • 50
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-310
    In: Research report
    Description / Table of Contents: CONTENTS: Introduction. - Field sites and procedures. - Results. - Discussion. - Conclusions. - Literature cited. - Appendix A: Tabulation of AIDJEX core data. - Appendix B: Tabulation of average salinity/ice thickness data. - Abstract.
    Description / Table of Contents: The salinity distribution in multiyear sea ice is dependent on the ice topography and cannot be adequately represented by a single average profile. The cores collected from areas beneath surface hummocks generally showed a systematic increase in salinity with depth from 0 0/00 at tne surface to about 4 0/00 at the base. The cores collected from areas beneath surface depressions were much more saline and displayed large salinity fluctuations. Salinity observations from sea ice of varying thicknesses and ages collected at various arctic and subarctic locations revealed a strong correlation between the average salinity of the ice, S, and the ice thickness, h. For salinity samples collected from cold sea ice at the end of the growth season, this relationship can be represented by two linear equations: S = 14.24 - 19.39h (h? 0.4 m) ; S = 7.88 - 1.59h (h 〉 0.4 m) . It is suggested that the pronounced break in slope at 0.4 m is due to a change in the dominant brine drainage mechanism from brine expulsion to gravity drainage. A linear regression for the data collected during the melt season gives S = 1.58 + 0.18h. An annual cyclic variation of the mean salinity probably exists for multiyear sea ice. The mean salinity should reach a maximum at the end of the growth season and a minimum at the end of the melt season.
    Type of Medium: Series available for loan
    Pages: iii, 23 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 310
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    Beijing : Geological Publishing House
    Call number: K 97.0343/1-2
    Pages: 2 Spezialkt. auf 6 Bl. + Erl. (522 S.)
    ISBN: 711600615X
    Series Statement: Geological memoirs : series 1, regional geology / People's Republic of China, Ministry of Geology and Mineral Resources no. 22
    Language: English
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  • 52
    Series available for loan
    Series available for loan
    Hanover, NH : Corps of Engineers, U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-274
    In: Research report
    Description / Table of Contents: CONTENTS: Introduction. - The ice/ice interface. - The ice/air interface. - The silicate/water/silicate interface. - The silicate/water/ice interface. - Summary. - Literature cited. - Abstract.
    Description / Table of Contents: Interfacial regions in frozen soils are of the following types: ice/ice (grain boundary) ice/water/air, silicate/water/silicate (interlamellar) and silicate/water /ice (extralamellar). For the last, the mid-portion of the interfacial region should be regarded as a liquid-like solution of the ionic and undissociated substances sorbed by the interface and expelled from the ice during freezing. The interfacial forces operative in these regions result in distinct differences in the properties and behavior of the interfacial water, compared with water in bulk; but, in spite of strong interfacial forces, the interfacial water exhibits liquid-like mobility in its response to many kinds of driving forces. From the evidence and arguments considered, it is concluded that distinctly different zones of orientational order can be distinguished within the interfacial regions. For an advancing silicate/water/ice interface it is proposed that there is a zone of strong perturbation and disorder immediately proximate to silicate surfaces in which the protons of water molecules are partially delocalized; this makes them more easily dissociated. Two or three molecular diameters removed from the silicate surface the interfacial forces operative there combine to create a zone of enhanced order in the molecular configurations. At some farther distance, depending upon the temperature below freezing, it is suggested that there exists a disordered transition zone proximate to the ice surface as portrayed in Drost-Hansen's model. It is suggested that future investigations will contribute refinements in the model and will uncover still further complexities in the various interfaces mentioned.
    Type of Medium: Series available for loan
    Pages: iii, 19 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 274
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    Series available for loan
    Series available for loan
    Hanover, NH : Corps of Engineers, U.S. Army Cold Regions Research & Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-269
    In: Research report
    Description / Table of Contents: CONTENTS: Preface. - List of symbols. - Introduction. - Structure of ice and ice sheets. - Ice as a mineral. - Lake and sea ice. - Chemistry and phase relations. - Dislocations,cracks,and stress concentrators. - Direct observation of dislocations. - Crackformation. - Stress concentration. - Theoretical considerations. - Experimental results. - Compressive strength. - Indentation failure. - Tensile strength. - Flexural strength. - Shear strength. - Impact strength. - Scale effects. - Strength deterioration in the spring. - Recommended research. - Summary. - Selected bibliography. - Abstract.
    Description / Table of Contents: The increased activity in cold regions has made a thorough understanding of fracture in lake and sea ice quite desirable, inasmuch as this information has application to a number of problems of geophysical as well as engineering importance. This survey starts with a discussion of the structure of ice I and the macro- and microstructure of sea and lake ice as well as their chemistry and phase relations. Recent work on the direct observation of dislocations as well as the formation of cracks in ice is summarized. Formal ice-brine-air models for analyzing variations in ice strength are also reviewed. The results of the different types of tests are discussed and cornpared (compressive, indentation, direct and ring-tension, small beam flexure and in situ cantilevers and simple beams, shear, and impact). Scale effects are considered as well as the rapid strength deterioration experienced by ice sheets in the spring. Finally, a number of recommendations are made concerning future research in this field.
    Type of Medium: Series available for loan
    Pages: viii, 79 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 269
    Language: English
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    Series available for loan
    Series available for loan
    Hanover, NH : Corps of Engineers, U.S. Army Cold Regions Research & Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-261
    In: Research report
    Description / Table of Contents: This paper considers a load moving with a constant velocity across an ice sheet that is floating on water. The ice sheet is assumed to be an isotropic, elastic, thin plate extending to infinity. The water is assumed to be inviscous, incompressible, and of a constant depth. The dynamic equations describing this ice-water system are solved for the steady state solution. Both a concentrated load and a uniform load distributed over a circular area are considered. The velocity which causes resonance is determined. The deflection and stress directly under the load are numerically evaluated.
    Type of Medium: Series available for loan
    Pages: ii, 13 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 261
    Language: English
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    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Materiel Command, Terrestrial Sciences Center, Cold Regions Research & Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-256
    In: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command, 256
    Description / Table of Contents: The flow of a compressible fluid through a deep layer of a porous medium with non-uniform permeability was analyzed. The volumetric behavior of the fluid was described first by the perfect gas law, then by the van der Waal's equation of state. Darcy's law was assumed to be valid. For illustration, the model of air flowing through a deep bed of naturally compacted snow was used to carry out numerical computation. The permeability of snow was considered as a function of depth. The nonlinear partial differential equation obtained by combining the continuity equation with Darcy's law was solved by finite difference technique. A time dependent exponential decay boundary condition was used which included the step-rise constant boundary condition as a limiting case. Pressure distributions in the porous medium calculated from the assumption of ideal gas and van der Waal's gas were compared. The data were presented in dimensionless variables.
    Type of Medium: Series available for loan
    Pages: iv, 13 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 256
    Language: English
    Note: CONTENTS: Preface. - Abstract. - Introduction. - Theory. - Computation and results. - Conclusions. - Literature cited.
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    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Corps of Engineers, Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-250
    In: Research report
    Description / Table of Contents: CONTENTS: Introduction. - Methods. - Results. - Ground and aerial photography. - Hemispherical photography. - Light quality. - Discussion. - Literature cited. - Abstract.
    Description / Table of Contents: Aerial and ground photographs were taken over a 2-year period of sites in the El Verde rain forest to record the consistency of the vegetational patterns in untreated sites and the changes that occurred following gamma irradiation. Four emulsions were used: panchromatic infrared, false color transparency and color transparency. Densitometry was used to evaluate color film and the vegetation response to 3 months of radiation. The color emulsions provided the sharpest indication of damage to vegetation and the succession following treatment. Hemispherical photography of the canopy was evaluated in terms of a canopy cover index defined as percent of light passing through the negative in a 90-degree cone area. Control stations were remarkably constant in all photography, establishing the stability and slow natural changes in rain forest structure. Spectral light measurements within the forest confirmed the predominance of far red shade light. Compared to similar studies on the chronic irradiated forest at Brookhaven National Laboratory the El Verde results were less distinct.
    Type of Medium: Series available for loan
    Pages: iii, 21 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 250
    Language: English
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    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Materiel Command, Cold Regions Research & Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-246
    In: Research report
    Description / Table of Contents: CONTENTS: Preface. - Summary. - Introduction. - Theory. - Discussion. - Literature cited.
    Description / Table of Contents: Steady-state temperature profiles are calculated for the borehole drilled through the Greenland ice sheet at Camp Century. The profiles are found by modifying Robin's theory through the addition of several correction terms. One of these terms is the internal heating arising from creep deformation. The importance of this term was emphasized by Lliboutry. The new theoretical profiles do not differ appreciably from the profile derived from Robin's theory. The theoretical profiles do differ substantially from the Camp Century profile measured by Hansen. It is concluded that Hansen's observations are evidence that factors such as accumulation rate and the upper surface temperature are not in a long-term steady-state condition. Better agreement between theoretical and measured curves is obtained if it is assumed that the accumulation rate was about 40% smaller in the past and that the mean annual surface temperature varied by about 0.5°C over the past 1000 years.
    Type of Medium: Series available for loan
    Pages: iv, 13 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 246
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  • 58
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    East Melbourne : Department of Energy and Minerals Government of Victoria
    Call number: K 96.0075
    Pages: 1 Kt. + Erl.-H. (68 S.)
    Series Statement: Geological Survey of Victoria report 92
    Language: English
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    Call number: K 96.0078/1-2
    In: Deep lead gold deposits in Victoria
    Pages: 1 Kt., 1 Spezialbl. + Erl.-H. (38 S.)
    Series Statement: Geological Survey of Victoria bulletin no. 62
    Language: English
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  • 60
    Monograph available for loan
    Monograph available for loan
    Hamburg : Wissenschaftliche Auswertungen
    Call number: IASS 15.0031
    Type of Medium: Monograph available for loan
    Pages: 448 S. : Ill., graph Darst., Kt.
    Edition: 2. ed., completed and updated
    ISBN: 3000029257
    Uniform Title: Warnsignal Klima
    Language: English
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  • 61
    Call number: S 90.0066
    ISSN: 0341-6399
    Language: English
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    Krefeld : Geolog. Landesamt Nordrhein-Westfalen
    Call number: SR 90.0924
    ISSN: 0071-8009
    Language: German
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  • 63
    Call number: ZSP-292-288
    In: Research report
    Description / Table of Contents: Contents: Preface. - List of symbols. - Introduction. - Adsorption of volatile chemicals by soil. - Introduction. - Experimental procedure. - Results and discussion. - Diffusion of volatile chemicals in soil. - Introduction. - Experimental procedure. - Calculations. - Results and discussion. - Prediction of vapor diffusion in soil. - Introduction. - Construction of model. - Computations. - Results and discussion. - A statistical method for analysis of diffusion through soil. - Introduction. - Theory. - Application. - Literature cited. - Abstract.
    Description / Table of Contents: Detection of mines, explosives, and tunnels may be accomplished by sensing associated volatile effluvia. This investigation was undertaken to provide a basis for predicting the diffusion of volatile compounds from underground sources into the atmosphere. Diffusion of a volatile compound was studied for a range of soil conditions utilizing soils from the mine detection sites in Puerto Rico. A new mathematical analysis based on the Monte Carlo method was developed for predicting vapor diffusion through soil into the atmosphere. It was determined that diffusion in soil can be reliably predicted if soil porosity, moisture content, and affinity for the compound are known. Appearance in the atmosphere is also dependent on accumulation of the compound in air at the soil/atmosphere interface. Diffusion of volatile compounds through soil into the atmosphere is not likely to be an important factor in tunnel detection due to depth of overburden. However, adsorption of compounds at tunnel walls is likely to significantly reduce the amount of vapor appearing in the atmosphere through entrances and vents. Detection in the atmosphere of TNT vapor from mines and explosives buried in moist, porous soil should be possible under ideal sample collection conditions.
    Type of Medium: Series available for loan
    Pages: v, 43 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 288
    Language: English
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  • 64
    Monograph available for loan
    Monograph available for loan
    München [u.a.] : Oldenbourg
    Call number: M 93.0609
    Type of Medium: Monograph available for loan
    Pages: 315 S.
    Edition: 5., verb. u. erw. Aufl.
    ISBN: 3486217089
    Series Statement: Einführung in die Nachrichtentechnik
    Classification:
    C.5.1.
    Language: German
    Location: Upper compact magazine
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  • 65
    Monograph available for loan
    Monograph available for loan
    Englewood Cliffs, N.J. : Prentice-Hall
    Associated volumes
    Call number: PIK M 039-92-0688/a
    In: Internetworking with TCP/IP
    Type of Medium: Monograph available for loan
    Edition: 2nd ed
    ISBN: 0134743210
    Classification:
    C.2.7.
    Language: English
    Location: A 18 - must be ordered
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  • 66
    Series available for loan
    Series available for loan
    Hanover, NH : Corps of Engineers, U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-243
    In: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command, 243
    Description / Table of Contents: The internal friction of single-crystal ice has been attributed to reorientation of the water molecule under periodic stress. However, the theory for damped dislocations, which offers another mechanism for the internal friction of ice, has not been investigated. The effects of scratching the surface of 41 ice samples and X-irradiating and plastically deforming them were evaluated. The effects observed on the internal friction of pure, single-crystal ice, in the flexure mode of oscillation between 400 and 1400 Hz, supported the existence of a dislocation-controlled mechanism, with the drag produced by the interaction of the dislocation with the protons in the crystal. In addition, analysis of the detailed shape of the data curve showed two peaks of tan delta as a function of temperature. The second peak, which had not been previously reported, had an activation energy of 0.16 eV and a relaxation time of 1.7 x 10^8 sec at infinite temperature. These experiments indicated that both peaks vrere controlled by the dislocation mechanism described above.
    Type of Medium: Series available for loan
    Pages: iv, 41 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 243
    Language: English
    Note: CONTENTS: Introduction. - Previous work. - Previous theory. - Internal friction of a crystal. - Granato-Lücke theory of dislocation damping. - Double kink mechanism. - Mechanisms not involving dislocations. - Experimental work. - Experimental approach. - Experimental apparatus. - Mode of oscillation. - Automated system. - Support, acoustic isolation, and temperature control. - Sample preparation. - X-ray apparatus. - Data analysis. - Stage I. - Stage II. - Stage III. - Experimental results and discussion. - The second peak. - Interpretation of scratching, X-irradiation, and plastic deformation. - Scratching. - X-irradiation. - Plastic deformation. - Supporting research. - Interpretation of the two peaks. - Conclusions. - Literature cited. - Appendix A: Computer programs. - Abstract.
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  • 67
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Materiel Command, Terrestrial Sciences Center, Cold Regions Research & Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-242
    In: Research report, 242
    Description / Table of Contents: The attenuation of visible light by falling snow was studied by making simultaneous attenuation measurements and snow concentration measurements. The attenuation coefficient was calculated from photometric measurements and from visual observations. Snow concentration in the air was evaluated by two methods: from Formvar replicas collected during the snowfall, and by mass accumulation of snow in collecting pans. The snowflakes were arbitrarily classified by crystal types according to their estimated fall velocity. It was found that the correlation between extinction coefficient (attenuation) and snow concentration was generally much higher by types than when all snowflakes were considered together regardless of crystal components and degree of riming. Two types, apparently improperly classified, displayed lower correlations than the overall group. When no fog is present during the snowfall, the experimental results coincide well with attenuation theory if a reasonable correction is applied to the values obtained in the measurement of snowflake diameters. Measurements of mass flux indicate that for a given intensity the attenuation caused by snow is an order of magnitude greater than that caused by the same mass flux of rain.
    Type of Medium: Series available for loan
    Pages: iv, 27 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 242
    Language: English
    Note: CONTENTS: Preface. - Abstract. - Introduction. - Initial theoretical considerations. - Light attenuation by particles. - Basis of attenuation meter measurements. - Contrast reduction and visual range. - Transmissometer theory, Pritchard photometric method. - Terminal velocity of snowflakes. - Methods of measurement: Light attenuation. - Duntley (Scripps Institution) attenuation meter. - "Meteorological range" observations. - Pritchard photometric method. - Methods of measurement: Atmospheric concentration of snowflakes. - Replication method. - Mass accumulation method. - Analysis of snow samples. - Terminal velocity of snowflakes. - Flux density and atmospheric concentration. - Mass accumulation rate. - Concurrent attenuation due to fog. - Discussion of results. - Computational methods. - Correlations: Attenuation coefficient vs area concentration. - Correlations: Attenuation coefficient vs are a flux. - Correlations: Attenuation coefficient vs mass concentration and mass flux. - Comparison of sampling methods for mass flux. - Attenuation of visible light by snow compared to rain. - Literature cited. - Appendix A.
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  • 68
    Monograph available for loan
    Monograph available for loan
    Boston [u.a.] : Artech House
    Associated volumes
    Call number: M 92.1079/2
    In: Optical fiber sensors
    Type of Medium: Monograph available for loan
    Pages: XXII S., S. 329-799
    ISBN: 0890063761
    Classification:
    C.5.1.
    Language: English
    Location: Upper compact magazine
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  • 69
    Call number: 5/M 92.1329/40
    In: Geophysical monograph
    Type of Medium: Monograph available for loan
    Pages: XII, 323 S. : graph. Darst.
    ISBN: 087590064X
    Series Statement: Geophysical monograph 40
    Classification:
    Tectonics
    Language: English
    Location: Reading room
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  • 70
    Monograph available for loan
    Monograph available for loan
    Washington : American Geophysical Union [u.a.]
    Associated volumes
    Call number: 5/M 92.1329/39
    In: Geophysical monograph
    Type of Medium: Monograph available for loan
    Pages: VII, 486 S.
    ISBN: 0875900666
    Series Statement: Geophysical monograph 39
    Language: English
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  • 71
    Series available for loan
    Series available for loan
    Hanover, NH : Corps of Engineers, U.S. Army Cold Regions Research & Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-271
    In: Research report
    Description / Table of Contents: CONTENTS: Introduction. - Previous work. - Conduct of the research. - Fundamental properties of snow. - Derived properties of snow. - Environmental effects. - Conclusions. - Literature cited. - Abstract.
    Description / Table of Contents: One of the great deficiencies in snow science is the lack of an analytical framework for much of the snow cycle. Snow research to date has largely consisted of measuring index properties of snow, such as bulk density and snow strength, and correlating them. This is useful, particularly for engineering purposes, but it does not grapple with the basic problem of what fundamental properties of snow determine the magnitude of the index properties and how these properties respond to environmental conditions. This study was an attempt to measure, quantitatively, the fundamental properties of grain size, shape, and fabric (relationship between grains) and relate these to the index or derived properties of bulk density, shear and tensile strength, permeability for air, and the dielectric static permittivity and loss tangent. Despite numerous difficulties in defining fabric and quantifying it, it was possible to show that: 1) snow strength is a function of bond area with a relationship in the low density range that is described by: [Sigma]f = [Sigma]i exp - (0.14nf) where [Sigma]f is failure strength, [Sigma]i is the final strength of ice, and nf is the porosity on the failure surface; and 2) the rate of densification of low density snow can be explained in part by high stress concentrations (on the order of 10^7 dynes /cm^2) at intergranular contacts and by such factors as riming on crystals. The effect of the environmental factors of time, temperature, and gravitational stress is difficult to study in situ because they are not independent variables. However, it appears that their study is simplified when we study the fundamental properties of snow as opposed to index properties.
    Type of Medium: Series available for loan
    Pages: v, 70 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 271
    Language: English
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  • 72
    Call number: S 99.0015(433)
    In: Freiberger Forschungshefte
    Type of Medium: Series available for loan
    Pages: 137 S.
    ISBN: 3342009470
    Series Statement: Freiberger Forschungshefte : C 433 : Geowissenschaften, Geophysik
    Language: German
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  • 73
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Materiel Command, Terrestrial Sciences Center, Cold Regions Research & Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-254
    In: Research report
    Description / Table of Contents: CONTENTS: Preface. - Abstract. - Introduction. - Description of the anemometer. - Temperature effects and their compensation. - Input-output relations. - Vibration isolation and compensation. - Wind tunnel tests. - Conclusions.
    Description / Table of Contents: A triaxial semiconductor strain-gage anemometer measuring wind velocities in three directions and thereby also determining the direction of the wind was designed and subjected to many crucial tests under various conditions. It was found that the measurements were affected by temperature and vibrations. Temperature compensation in two directions was made and wind tunnel tests on an almost vibration-free platform were performed. The results show that this type of instrument can be successfully used to measure large-scale turbulences. Throughout this report, emphasis is placed on the compensation necessary for temperature and vibration effects and the determination of input-output relationships. It is concluded that it is possible to design a practical triaxial strain-gage anemometer with high-frequency response and high sensitivity and to measure wind velocities accurately with this type of instrument when temperature and vibration compensations are properly made.
    Type of Medium: Series available for loan
    Pages: iv, 15 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 254
    Language: English
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  • 74
    Series available for loan
    Series available for loan
    Washington, DC : United States Gov. Print. Off.
    Associated volumes
    Call number: SR 90.0001(905)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: VII, 80 S. + 1 pl.
    Series Statement: U.S. Geological Survey bulletin 905
    Language: English
    Location: Lower compact magazine
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  • 75
    Series available for loan
    Series available for loan
    Washington, DC : United States Gov. Print. Off.
    Associated volumes
    Call number: SR 90.0001(972)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: V, 97 S. + 2 pl.
    Series Statement: U.S. Geological Survey bulletin 972
    Language: English
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  • 76
    Series available for loan
    Series available for loan
    Washington, DC : United States Gov. Print. Off.
    Associated volumes
    Call number: SR 90.0001(964-E)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: IV S., S. 361-400, V S. + 11 pl.
    Series Statement: U.S. Geological Survey bulletin 964-E
    Language: English
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  • 77
    Series available for loan
    Series available for loan
    Washington, DC : United States Gov. Print. Off.
    Associated volumes
    Call number: SR 90.0001(965-A)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: VII, 164 S. + 7 pl.
    Series Statement: U.S. Geological Survey bulletin 965-A
    Language: English
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  • 78
    Call number: 9/M 92.1323(6)
    In: Global geoscience transect
    Type of Medium: Monograph available for loan
    Pages: 30 S. + 2Kt.-Beil.
    ISBN: 0875907830
    Series Statement: Publication of the International Lithosphere Program 192
    Classification:
    A.3.1.
    Language: English
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  • 79
    Series available for loan
    Series available for loan
    Washington, DC : United States Gov. Print. Off.
    Associated volumes
    Call number: SR 90.0001(974-B)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: III S., S. 35-49 + 2 pl.
    Series Statement: U.S. Geological Survey bulletin 974-B
    Language: English
    Location: Lower compact magazine
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  • 80
    Call number: SR 90.0001(1839-E,F)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: Getr. Zählung + 2 pl.
    Series Statement: U.S. Geological Survey bulletin 1839-E,F
    Language: English
    Location: Lower compact magazine
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  • 81
    Call number: SR 90.0001(1839-G,H)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: Getr. Zählung + 1 pl.
    Series Statement: U.S. Geological Survey bulletin 1839-G,H
    Language: English
    Location: Lower compact magazine
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  • 82
    Call number: SR 90.0001(1839-A-D)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: Getr. Zählung
    Series Statement: U.S. Geological Survey bulletin 1839-A-D
    Language: English
    Location: Lower compact magazine
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  • 83
    Call number: SR 90.0001(1787-A-C)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: VI, 36 S. + 1 pl.
    Series Statement: U.S. Geological Survey bulletin 1787-A-C
    Language: English
    Location: Lower compact magazine
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  • 84
    Call number: SR 90.0001(1787-H,I)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: VI, H10, I11 S. + 1 pl.
    Series Statement: U.S. Geological Survey bulletin 1787-H,I
    Language: English
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  • 85
    Series available for loan
    Series available for loan
    [Washington, DC] : United States Gov. Print. Off.
    Associated volumes
    Call number: SR 90.0001(1808-E,F)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: Getr. Zählungn
    Series Statement: U.S. Geological Survey bulletin 1808-E,F
    Language: English
    Location: Lower compact magazine
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  • 86
    Monograph available for loan
    Monograph available for loan
    Washington : American Geophysical Union
    Associated volumes
    Call number: 9/M 92.1323(1) ; M 92.1322(1)
    In: Global geoscience transect
    Type of Medium: Monograph available for loan
    Pages: 5 S. + 1 Kt.-Beil.
    ISBN: 0875907784
    Series Statement: Publication of the International Lithosphere program 187
    Classification:
    A.3.1.
    Language: English
    Location: Reading room
    Location: Upper compact magazine
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  • 87
    Series available for loan
    Series available for loan
    Washington, DC : United States Gov. Print. Off.
    Associated volumes
    Call number: SR 90.0001(976)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: S. 267-301, III S.
    Series Statement: U.S. Geological Survey bulletin 976
    Language: English
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  • 88
    Series available for loan
    Series available for loan
    Washington, DC : United States Gov. Print. Off.
    Associated volumes
    Call number: SR 90.0001(978-B)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: V S., S. 27-67 + 2 pl.
    Series Statement: U.S. Geological Survey bulletin 978-B
    Language: English
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  • 89
    Series available for loan
    Series available for loan
    Washington, DC : United States Gov. Print. Off.
    Associated volumes
    Call number: SR 90.0001(986)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: IV, 133 S. + 6 pl.
    Series Statement: U.S. Geological Survey bulletin 986
    Language: English
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  • 90
    Series available for loan
    Series available for loan
    Washington, DC : United States Gov. Print. Off.
    Associated volumes
    Call number: SR 90.0001(982-B)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: III S., S. 53-73 + 3 pl.
    Series Statement: U:S. Geological Survey bulletin 982-B
    Language: English
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  • 91
    Series available for loan
    Series available for loan
    Washington, DC : United States Gov. Print. Off.
    Associated volumes
    Call number: SR 90.0001(982-D)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: III S., S. 95-119
    Series Statement: U.S. Geological Survey bulletin 982-D
    Language: English
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  • 92
    Series available for loan
    Series available for loan
    Washington, DC : United States Gov. Print. Off. ; 976-C
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    Call number: SR 90.0001(976-C)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Series Statement: U.S. Geological Survey bulletin 976-C
    Language: English
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  • 93
    Series available for loan
    Series available for loan
    Washington, DC : United States Gov. Print. Off.
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    Call number: SR 90.0001(982-E)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: III S., S. 121-151 + 6 pl.
    Series Statement: U.S. Geological Survey bulletin 982-E
    Language: English
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  • 94
    Series available for loan
    Series available for loan
    Washington, DC : United States Gov. Print. Off.
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    Call number: SR 90.0001(982-F)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: VI S., S. 153-244 + 5 pl.
    Series Statement: U.S. Geological Survey bulletin 982-F
    Language: English
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  • 95
    Series available for loan
    Series available for loan
    Washington, DC : United States Gov. Print. Off.
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    Call number: SR 90.0001(976-D)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: III S., S. 211-266
    Series Statement: U.S. Geological Survey bulletin 976-D
    Language: English
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  • 96
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    Series available for loan
    Washington, DC : United States Gov. Print. Off.
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    Call number: SR 90.0001(991-C)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: III S., S. 145-194
    Series Statement: U.S. Geological Survey bulletin 991-C
    Language: English
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  • 97
    Series available for loan
    Series available for loan
    Washington, DC : United States Gov. Print. Off.
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    Call number: SR 90.0001(992)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: V, 94 S.
    Series Statement: U.S. Geological Survey bulletin 992
    Language: English
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  • 98
    Series available for loan
    Series available for loan
    Washington, DC : United States Gov. Print. Off.
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    Call number: SR 90.0001(981-A)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: III, 54 S.
    Series Statement: U.S. Geological Survey bulletin 981-A
    Language: English
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  • 99
    Series available for loan
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    Washington, DC : United States Gov. Print. Off.
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    Call number: SR 90.0001(994)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: V, 98 S.
    Series Statement: U.S. Geological Survey bulletin 994
    Language: English
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  • 100
    Series available for loan
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    Washington, DC : United States Gov. Print. Off.
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    Call number: SR 90.0001(978-A)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: IV, 25 S. + 8 pl.
    Series Statement: U.S. Geological Survey bulletin 978-A
    Language: English
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