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  • English  (4,545)
  • Russian  (146)
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  • 1975-1979  (2,048)
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  • 1
    Monograph available for loan
    Monograph available for loan
    Santa Fe, NM : School for Advanced Research Press
    Call number: IASS 18.91705
    Type of Medium: Monograph available for loan
    Pages: XIII, 290 S., [8] Bl , Ill., graph. Darst., Kt , 26 cm
    Edition: 1. ed
    ISBN: 1930618875 (pa) , 9781930618879 (pa)
    Series Statement: A School Of Advanced Research Resident Scholar Book
    Language: English
    Branch Library: RIFS Library
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  • 2
    Call number: 9/M 07.0421(467)
    In: Geological Society Special Publication
    Description / Table of Contents: Gullies on Mars resemble terrestrial gullies involved in the transport of abundant material down steep slopes by liquid water. However, liquid water should not be stable at the Martian surface. The articles in this volume present the two main opposing theories for Martian gully formation: climate-driven melting of surficial water-ice deposits and seasonal dry-ice sublimation. The evidence presented ranges from remote-sensing observations, to experimental simulations, to comparison with Earth analogues. The opposing hypotheses imply either that Mars has been unusually wet in the last few million years or that it has remained a cold dry desert – both with profound implications for understanding the water budget of Mars and its habitability. The debate questions the limits of remote-sensing data and how we interpret active processes on extra-terrestrial planetary surfaces, even beyond those on Mars, as summarized by the review paper at the beginning of the book.
    Type of Medium: Monograph available for loan
    Pages: vi, 434 Seiten , Illustrationen
    ISBN: 978-1-78620-360-1
    Series Statement: Geological Society Special Publication 467
    Language: English
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  • 3
    Monograph available for loan
    Monograph available for loan
    Princeton [u.a.] : Princeton Univ. Press
    Call number: IASS 18.91773
    Type of Medium: Monograph available for loan
    Pages: XIV, 321 S. , Ill
    ISBN: 0691120641 (alk. paper) , 9780691120645 (alk. paper) , 069112065X (pbk.) , 9780691120652 (pbk.)
    Language: English
    Branch Library: RIFS Library
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  • 4
    Call number: PIK T 060-18-91853
    Type of Medium: Monograph available for loan
    Pages: XXIII, 287 Seiten , Illustrationen, Diagramme, Karten
    Edition: Reprinted
    ISBN: 0470843497 , 9780470843499
    Language: English
    Note: Contents: 1. Introduction to urban Geosimulation ; 2. Formalizing Geosimulation with Geographic Automata Systems (GAS) ; 3. System Theory, Geography, and Urban Modelling ; 4. Modelling urban land usage with cellular automata ; 5. Modelling Urban Dynamics with Multi-Agent Systems ; 6. Finale: Epistemology of Geosimulation
    Location: A 18 - must be ordered
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  • 5
    Monograph available for loan
    Monograph available for loan
    Cambridge, Massachusetts : The MIT Press
    Call number: IASS 19.91995
    Description / Table of Contents: Winner of the 2006 Giovanni Sartori Book Award, given by the American Political Science Association's Qualitative Methods Section. The use of case studies to build and test theories in political science and the other social sciences has increased in recent years. Many scholars have argued that the social sciences rely too heavily on quantitative research and formal models and thus have attempted to develop and refine rigorous methods for using case studies. This text presents a comprehensive analysis of research methods using case studies and examines the place of case studies in social science methodology. It argues that case studies, statistical methods, and formal models are complementary rather than competitive. The book explains how to design case study research that will produce results useful to policymakers and it emphasizes the importance of developing policy-relevant theories. It offers three major contributions to case study methodology: an emphasis on the importance of within-case analysis, a detailed discussion of process tracing, and development of the concept of typological theories. Case Studies and Theory Development in the Social Sciences will be particularly useful to graduate students and scholars in social science methodology and the philosophy of science, as well as to those designing new research projects, and will contribute greatly to the broader debate about scientific methods.
    Type of Medium: Monograph available for loan
    Pages: xv, 331 Seiten , 24cm
    ISBN: 0262072572 , 9780262072571 , 0262572222 , 9780262572224
    Series Statement: BCSIA studies in international security
    Language: English
    Branch Library: RIFS Library
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  • 6
    Series available for loan
    Series available for loan
    Stuttgart : Schweizerbart
    Associated volumes
    Call number: SR 90.0066(33)
    In: Geologisches Jahrbuch . Reihe A, Allgemeine und regionale Geologie Bundesrepublik Deutschland und Nachbargebiete, Tektonik, Stratigraphie, Paläontologie, 33
    Type of Medium: Series available for loan
    Pages: 159 S. , Ill., graph. Darst., Kt. , 2 Beil.
    Series Statement: Geologisches Jahrbuch / A Heft 33
    Language: German , English , French , Russian
    Note: Mit engl., franz. und russ. Zsfassungen
    Location: Lower compact magazine
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  • 7
    Call number: ZSP-SCAR-570-1
    In: Report to SCAR on Antarctic research activities of Germany (FRG), 1
    Type of Medium: Series available for loan
    Pages: 21 Seiten
    ISSN: 0179-0072
    Series Statement: Report to SCAR on Antarctic research activities of Germany (FRG) 1
    Language: English
    Note: Contents: Membership of the National Committee on Antarctic Research of the Federal Republic of Germany. - Introduction. - Station. - Field Activities 1974-1979. - Planned Activities 1979/80. - References.
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  • 8
    Monograph available for loan
    Monograph available for loan
    Moskva : Izdatel'stvo "Nauka"
    Call number: MOP 40046 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 113 Seiten , Illustrationen
    Language: Russian
    Note: In kyrillischer Schrift
    Location: MOP - must be ordered
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  • 9
    Call number: ZSP-201-76/33
    In: CRREL Report, 76-33
    In: Detecting structural heat losses with mobile infrared thermography / R.H. Munis, S.J. Marshall and M.A. Bush, Part IV
    Description / Table of Contents: During the winter of 1973-74 a mobile infrared thermography system was used to survey campus buildings at Dartmouth College, Hanover, New Hampshire. Both qualitative and quantitative data are presented regarding heat flow through a small area of a wall of one brick dormitory building before and after installation of aluminum reflectors between radiators and the wall. These data were used to estimate annual cost savings for 22 buildings of similar construction having aluminum reflectors installed behind 1100 radiators. The data were then compared with the actual savings which were calculated from condensate meter data. The discrepancy between estimated and actual annual cost savings is explained in detail along with all assumptions required for these calculations.
    Type of Medium: Series available for loan
    Pages: iii, 14 Seiten , Illustrationen
    Series Statement: CRREL Report 76-33
    Language: English
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  • 10
    Call number: MOP 41424 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 31 Seiten , Illustrationen
    Language: Russian
    Note: In kyrillischer Schrift
    Location: MOP - must be ordered
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  • 11
    Call number: M 19.92455
    Type of Medium: Monograph available for loan
    Pages: 178 Seiten , Illustrationen
    ISBN: 9789090240619
    Language: English
    Location: Upper compact magazine
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  • 12
    Monograph available for loan
    Monograph available for loan
    Zürich : World Glacier Monitoring Service
    Call number: AWI G7-19-92411
    Type of Medium: Monograph available for loan
    Pages: 88 Seiten , Illustrationen
    ISBN: 9789280728989
    Language: English
    Note: Contents Foreword by UNEP Foreword by WGMS Summary 1 Introduction 2 Glaciers and climate 3 Global distribution of glaciers and ice caps 4 Glacier fluctuation series 5 Global glacier changes 6 Regional glacier changes 6.1 New Guinea 6.2 Africa 6.3 New Zealand 6.4 Scandinavia 6.5 Central Europe 6.6 South America 6.7 Northern Asia 6.8 Antarctica 6.9 Central Asia 6.10 North America 6.11 Arctic Islands 7 Conclusions References Appendix 1 - National Correspondents of the WGMS Appendix 2 - Meta-data on available fluctuation data
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  • 13
    Monograph available for loan
    Monograph available for loan
    Stroudsburg : Dowden, Hutchinson & Ross
    Associated volumes
    Call number: G 8115
    In: Benchmark papers in geology
    Type of Medium: Monograph available for loan
    Pages: XV, 468 Seiten , Illustrationen
    ISBN: 0-471-13540-2
    Series Statement: Benchmark papers in geology 15
    Language: English
    Location: Upper compact magazine
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  • 14
    Monograph available for loan
    Monograph available for loan
    Sofija
    Call number: MOP 44702 / Mitte
    Type of Medium: Monograph available for loan
    Language: Russian
    Location: MOP - must be ordered
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  • 15
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-79/13
    In: CRREL Report, 79-13
    Description / Table of Contents: Heat transfer in turbulent flow was measured in a rectangular channel with a width of 0.254 m and a flow depth of 0.0254 m. Correlations between the Nusselt and Reynolds numbers are given for a range of 3020 Re 22360. A Prandtl number range of 9.90 or = Pr or = 12.28 for water was used in the tests. The results are compared with those of other investigations and show that some well-known correlations underpredict the heat transfer by about 35%.
    Type of Medium: Series available for loan
    Pages: ii, 5 Seiten , Illustrationen
    Series Statement: CRREL Report 79-13
    Language: English
    Location: AWI Archive
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  • 16
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-79/10
    In: CRREL Report, 79-10
    Description / Table of Contents: Ice cores from Byrd Station and Little America V have been used to test an ultrasonic technique for evaluating crystal anisotropy in the Antarctic Ice Sheet. P-wave velocities measured parallel and perpendicular to the vertical axes of cores from the 2164-m-thick ice sheet at Byrd Station have yielded results in excellent agreement with the observed c-axis fabric profile and with the in-situ P-wave velocity profile measured parallel to the bore hole axis. Velocity differences in excess of 140 m/s for core samples from deeper than 1300 m attest to the strong single pole clustering of crystallographic c-axes about the vertical, especially in the zone from 1300-1800 m. Such oriented structure is compatible only with strong horizontal shearing in this zone. The existence in an ice sheet of widespread shearing several hundred meters above its bed raises serious questions as to the validity of current concepts of the flow of large ice masses that tend to gloss over or ignore crystal alignments of this magnitude.
    Type of Medium: Series available for loan
    Pages: IV, 16 Seiten , Illustrationen
    Series Statement: CRREL Report 79-10
    Language: English
    Note: CONTENTS Abstract Preface Introduction Laboratory measurements Sample sources Ultrasonic velocity measurements Effects of inclined drilling at Byrd Station Results Byrd Station Little America V Summary and conclusions Literature cited
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  • 17
    Call number: 8/M 19.92771 ; S 02.0465(32)
    In: Cahiers du Centre Européen de Géodynamique et de Séismologie
    Type of Medium: Series available for loan
    Pages: 97 Seiten , Illustrationen
    ISBN: 9789995904630
    Series Statement: Cahiers du Centre Européen de Géodynamique et de Séismologie 32
    Uniform Title: European Macroseismic Scale 1998
    Classification:
    Seismology
    Language: Spanish
    Location: Reading room
    Location: Lower compact magazine
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  • 18
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-78/11
    In: CRREL Report, 78-11
    In: Mechanics of cutting and boring, Part VIII
    Description / Table of Contents: The report deals with forces and power requirements for cutting machines of the belt type, as exemplified by large chain saws and ladder trenchers. The forces of single cutting tools are considered, and related to the overall forces on a cutter bar. Forces are related to power, and sources of loss are identified. Tractive thrust and normal reaction are analyzed and used to assess the traction, weight and balance.
    Type of Medium: Series available for loan
    Pages: vi, 24 Seiten , Illustrationen
    Series Statement: CRREL Report 78-11
    Language: English
    Note: CONTENTS Abstract Preface Foreword Introduction Terminology Tool forces Number of active cutting teeth Tool force and chain force Chain power Tool turce and belt power Tractive thrust and normal reaction Traction of carrier vehicles Power/weight ratio Cutter bar moments Specific energy Performance index Power density Apparent belt pressure Acceleratin and transport of cuttings Examples
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  • 19
    Call number: ZSP-201-76/24
    In: CRREL Report, 76-24
    Description / Table of Contents: Chemical analysis of surface snows and deeper ice core samples from Milcent, Greenland, indicates a marine origin for Na and Cl and a terrestrial origin for Al, Mn and V. Pre-1900 enrichment factors, based on average crustal composition, are high for Zn and Hg and appear to be related to their volatility. A comparison of pre-1900 and 1971-1973 concentrations of V and Hg shows no decided increase from industrial production; however, the abundance of Zn (relative to Al) increased three-fold during this time period. The chemical composition of ancient ice is extremely useful in interpreting modern aerosols.
    Type of Medium: Series available for loan
    Pages: ii, 6 Seiten , Illustrationen
    Series Statement: CRREL Report 76-24
    Language: English
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  • 20
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-76/25
    In: CRREL Report, 76-25
    Description / Table of Contents: The primary objective of this investigation was to compile baseline information pertaining to the ocean circulation, especially the extent and patterns of tidal currents and tidal flushing, in Cook Inlet, Alaska, utilizing aircraft and satellite imagery with corroborative ground truth data. LANDSAT-1 and NOAA-2 and -3 imagery provided repetitive, synoptic views of surface currents, water mass migration and sediment distribution during different seasons and tides. Color, color infrared and thermal infrared imagery acquired on 22 July 1972 with the NASA NP-3A aircraft were used to analyze currents, mixing patterns and sediment dispersion in selected areas. Temperature(C), salinity (0/00) and suspended sediment concentration (mg/l) data and hand-held photography were utilized as ground truth information in the interpretation of the aircraft and satellite imagery. Coriolis effect, semidiurnal tides and the Alaska current govern the estuary circulation. Clear, oceanic water enters the inlet on the southeast during flood tide, progresses northward along the east shore with minor lateral mixing, and remains a distinct water mass to the latitude of Kasilof-Ninilchik. South of the forelands, mixing with turbid inlet water becomes extensive. Turbid water moves south primarily along the north shore during ebb tide and a shear zone between the two water masses forms in mid-inlet south of Kalgin Island. Currents adjacent to and north of the forelands are complicated by tidal action, coastal configuration and bottom effects. Turbulence is greatest throughout the water column along the south shore and stratification is more pronounced in Kamishak and Kachemak Bays, especially when fresh water runoff is high.
    Type of Medium: Series available for loan
    Pages: ix, 92 Seiten , Illustrationen
    Series Statement: CRREL Report 76-25
    Language: English
    Note: CONTENTS Abstract Preface Summary Conversion factors: U.S. customary to metric (SI) units of measurement. Introduction Background Objectives Project history Approach Aircraft imagery LANDSAT-1 imagery NOAA-2 and -3 satellite imagery Ground truth data Imagery and ground truth data analysis Physical and cultural setting Geography Geology Climate Hydrology Local industry and population density Sources of estuarine pollution Results and discussion Coastal configuration Bathymetry Tides Asymmetry of tidal flow/duration across inlet Suspended sediment distribution and circulation Sea ice Tidal flushing characteristics Summary and conclusions Applications Recommendations Literature cited Appendix A. RS-14 infrared scanner imagery
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  • 21
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-76/28
    In: CRREL Report, 76-28
    Description / Table of Contents: Fourier transforms of selected ground-motion time histories from five underground high-explosive and nuclear detonations are used to define the transmission properties (Transfer functions) of three rock types. Absorption, a measure of a rock's energy dissipating characteristics, is expressed for each of the tests as a function of the frequency of transmission. Dispersion results from a variation in transmission velocity with frequency and is described for each test by a phase velocity spectrum. The transmission properties from one of the sites are used to predict a ground-motion time history at that site from another nuclear event. The potential use of Fourier techniques to make ground-motion predictions and to measure in-situ material properties is discussed.
    Type of Medium: Series available for loan
    Pages: vi, 91 Seiten , Illustrationen
    Series Statement: CRREL Report 76-28
    Language: English
    Note: Contents Section I: Introduction Section II: Analytical procedures 1. Fourier transforms 2. Basic transform properties 3. Transform techniques 4. The transfer function Section II: Parameter studies and program evaluations 1. Analytical parameter study 2. I-TRAIN evaluation 3. S-TRAIN evaluation Section IV: Data 1. DATEX I 2. DATEX II 3. STARMET 4. MINERAL LODE 5. HARD HAT and PILEDRIVER Section V: Analysis of transformed data 1. Absorption 2. Dispersion 3. Transfer function Section VI: Fourier synthesis Section VII: Discussion Literature cited Appendix A: The Fourier integral and series Appendix B: Subroutine FOURT used in analysis Appendix C: I-TRAIN and S-TRAIN programs
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  • 22
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-76/32
    In: CRREL Report, 76-31
    Description / Table of Contents: Four large grounded multi-year shear ridge formations were found in the grounded ice subzone of the fast ice zone near the Harrison Bay/Prudhoe Bay area of Alaska. A 166-m-long cross section of one of these formations was obtained by leveling and sonar measurements. These measurements revealed that the maximum ridge height was 12.6 m and that the formation was grounded in 17-18 m of water. The salinity, temperature, brine volume and density of the ice were determined on samples obtained by coring. The physical characteristics of the formations as observed in satellite, SLAR and aerial imagery indicate that these formations have not moved between the time of their formation in the fall of 1974 and August of 1976. Evidence of significant aeolian debris discoloring the ice is discussed.
    Type of Medium: Series available for loan
    Pages: iv, 27 Seiten , Illustrationen
    Series Statement: CRREL Report 76-32
    Language: English
    Note: Contents Abstract Preface Introduction Background Fast ice study area Results and discussion Literature cited
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  • 23
    Call number: ZSP-201-76/31
    In: CRREL Report, 76-31
    Description / Table of Contents: Sections in the Connecticut River where ice jam potential is high were identified through the use of low-altitude black and white photographs taken during low-flow, ice-free conditions. The hydraulics and mechanics of ice jam initiation were investigated in the river reach where these sections were identified. Certain areas were found in the river that had a high susceptibility to ice clogging, but this high potential decreased with increasing discharge because of the improved surface conveyance of the ice through the reach. The stability of ice floes was established along the channel, but the floes generally became unstable as the flow increased. This was calculated by using a Froude number criterion. Grounding locations for ice became evident when the critical Froude number was zero for a given thickness and water depth. No single factor was determined to be responsible for initiating the ice jams in the Connecticut River at Windsor. Apparently there existed a multitude of interacting conditions: surface constrictions, possible high backwater conditions from the Brattleboro Dam, a solid ice cover in the backwater of the Brattleboro Dam that prevented ice transport from the Windsor area, deep pools followed by shallow depth sections upstream of bridge piers, a greater ice thickness accumulation of fragmented floes than would result if a uniform cover could be established in the same reach, and the diurnal fluctuation of river stage casued by the release of water at Wilder Dam.
    Type of Medium: Series available for loan
    Pages: vi, 39 Seiten , Illustrationen
    Series Statement: CRREL Report 76-31
    Language: English
    Note: CONTENTS Abstract Preface Summary Conversion factors: U.S. customary to metric units of measurement Introduction Testsite Aerial photography Channel morphology — Interpretation of aerial photographs Ground surveys Hydraulic analysis Analysis of ice jam locations Winter field observations Conclusions Literature cited Appendix: Locations and plots of cross sections from Sumner Falls to Chase Island, Connecticut River
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  • 24
    Call number: MOP 44631 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 80 Seiten , 21 cm
    Language: Russian
    Note: In kyrillischer Schrift
    Location: MOP - must be ordered
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  • 25
    Call number: MOP 44652 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 61 Seiten , Illustrationen , 20 cm
    Series Statement: Serija Meteorologija / VNII Gidrometeorologičeskoj Informacii - Mirovoj Centr dannych
    Language: Russian
    Note: In kyrillischer Schrift
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  • 26
    Call number: MOP 44808 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 152 Seiten , Illustrationen , 21 cm
    Language: Russian
    Note: In kyrillischer Schrift
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  • 27
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-76/41
    In: CRREL Report, 76-41
    Description / Table of Contents: Eight Geoceiver stations were established and suitably marked along or near the crestiline of the Greenland ice sheet during GISP field operations from 1971 to 1975. At one of these stations, DYE-3, repeated Geoceiver positions indicate an ice velocity of 12.7 m.yr on an azimuth of approximately 60 degrees. Data from the International Greenland Glaciological Expedition (EGIG) surveys show that ice flow in the vicinity of Crete is radiating outward from a dome to the south. Two independent calculations of the state of equilibrium at Crete indicate ice sheet thinning rates of 0.25 to 0.37 m/yr, while direct measurement of elevation change by EGIG indicates an ice sheet thickening rate of difference of 0.06 m/yr. Resolution of these differences must await further geophysical work and deep drilling in the ice sheet.
    Type of Medium: Series available for loan
    Pages: iii, 13 Seiten , Illustrationen
    Series Statement: CRREL Report 76-41
    Language: English
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  • 28
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-76/43
    In: CRREL Report, 76-43
    Description / Table of Contents: Ice fog generated at the Eielson AFB power plant cooling pond contributes heavily to the total ice fog problem on the base. Several methods for ice fog suppression were studied and two techniques were tested experimentally. Experiments were also conducted to determine the magnitude of the various modes of heat transfer within the pond's microclimate. Values of evaporative and radiative heat loss during ice fog are presented. Ice cover is shown to be an effective ice fog suppression technique. Monomolecular films are also shown to be effective and offer some unique advantages, such as ease of application and low overall cost. The heat normally lost to evaporation must be dissipated by other means during suppression. With the ice cover technique this is accomplished by melting the ice cover. During suppression with monomolecular films, the heat must be dissipated by increasing radiative and convective losses. The simplicity of application of monomolecular films, along with their lower cost, combine to make this technique attractive; however, the lower pond temperatures and increased suppression effectiveness weigh heavily in favor of the ice-cover technique.
    Type of Medium: Series available for loan
    Pages: viii, 86 Seiten , Illustrationen
    Series Statement: CRREL Report 76-43
    Language: English
    Note: CONTENTS Abstract Preface List of symbols Conversion factors: U.S. customary to metric units of measurement Introduction Section I. Ice fog Section II. Evaporation Bowen's equation Evaporation equation Evaporation measurements during ice fog conditions Evaporation measurements at Eielson Power Plant cooling pond Data analysis Section Ill. Radiation during ice fog Brunt's equation Ångström equation Elsasser's equation Cloud cover Reflection Field experimental results Analysis of experimental results Radiation equations for ice fog Transmissivity of ice fog Radiation model Wind effect Summary Section IV. Convection Convective heat transfer theory Rotem and Claassen equation Kay's approach Russian approach Analysis Heat budget at the surface Conclusions Section V. Ice fog suppression techniques Fans Injection wells Latent heat storage Monomolecular films Use of heated water from the cooling pond Section VI. Latent heat storage experiments Freezing rates Cooling pond Ice building Ice growth rate -maximum system limitation Evaporation heat loss -maximum Realistic growth rate Ice building techniques Ice volume measurements Melting experiments Ice fog suppression considerations Experimental results Section VII. Recommendations and conclusions Hexadecanol studies Injection well suppression Latent heat storage suppression Comparison of approaches Measurements of evaporation Measurements of radiation loss Convective heat losses Ice fog suppression Selected bibliography Appendix A. Convective heat transfer coefficient from water to ice and from ice to air
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  • 29
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-77/3
    In: CRREL Report, 77-3
    Description / Table of Contents: Tests were conducted in uniaxial compression and tension to determine the effect of temperature on the strength of frozen Fairbanks silt. Test temperatures ranged from 0 C to -56.7 C. Two machine speeds, 4.23 cm/sec and 0.0423 cm/sec, were used for the constant displacement rate tests. From the highest to the lowest temperature, the compressive strength increased up to about one order of magnitude and the tensile strength increased one-half an order of magnitude. Equations are presented which correlate strength with temperature at the strain rates obtained. The initial tangent and 50% strength moduli and the specific energy are given for each test. The mode of fracture and the effects of unfrozen water content and ice matrix strengthening are discussed, and the test results are compared with the data of other investigations.
    Type of Medium: Series available for loan
    Pages: iv, 27 Seiten , Illustrationen
    Series Statement: CRREL Report 77-3
    Language: English
    Note: CONTENTS Abstract Preface Introduction Sample preparation Apparatus and testing procedure Test results Discussion Compressive strength Tensile strength Initial tangent and 50% stress moduli Specific energy Mode of failure Strength as a function of unfrozen water Thermal activation Conclusions and recommendations Literature cited
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  • 30
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-77/6
    In: CRREL Report, 77-6
    Description / Table of Contents: It has been reported that small arms projectiles are inherently unstable in snow and that snow has an unexpectedly high ability to stop them and other fast-moving projectiles. Field tests showed that the typical subarctic snow of interior Alaska can be used effectively to provide protection from both rifle and machine gun fire. The undisturbed snow had an average density of 0.18 g/cu. cm., but simple processing, such as shoveling, increased the density to around 0.34 g/cu. cm. Further processing increased the density to above o.40 g/cm3 but densities much above that value were difficult to obtain with simple hand equipment. Tests of the M16 rifle and M60 and M2HB machine guns showed that bullet penetration was inversely related to density - the higher the density the lower the bullet penetration. Design values for the three weapons were determined. A number of types of snow trenches and structures were designed and tested. They were found to provide good protection, in part since bullets showed a strong tendency to ricochet from the snow surface when striking it at a low angle. Burlap bags were filled with snow to revet structures and worked very well. Several types of Russian defensive works of snow were tested but proved unsuitable in the light, weak subarctic snow. The times required for troops to build several types of structures using only shovels and scoops were recorded.
    Type of Medium: Series available for loan
    Pages: vi, 23 Seiten , Illustrationen
    Series Statement: CRREL Report 77-6
    Language: English
    Note: CONTENTS Abstract Preface Summary Background Objectives Subarctic snow General Snow processing Construction productivity Shovel capacity Snow piles Bullet behavior and penetration in snow Test procedure M16 M60 ball M60 tracers .50 caliber Tumbling Bullet deformation and breakage Design penetration values Defensive works of snow Revetments Snow bags The snow trench The hardened snow trench Breastworks and bunkers Evaluation of foreign technology Russian expedient snow trenches Snow blocks and block structures The snow arch An expedient shelter Conclusions Recommendations Literature cited
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  • 31
    Monograph available for loan
    Monograph available for loan
    New York [u.a.] : McGraw-Hill Book Company
    Call number: MOP 44210 / Mitte
    Type of Medium: Monograph available for loan
    Pages: XV, 523 Seiten , graphische Darstellungen
    ISBN: 978-0-070-56042-0
    Language: English
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  • 32
    Monograph available for loan
    Monograph available for loan
    Heidelberg : Physica-Verlag
    Call number: IASS 20.93369
    Type of Medium: Monograph available for loan
    Pages: XVI, 243 Seiten , graphische Darstellungen , 235 mm x 155 mm
    ISBN: 9783790823356 , 9783790823363 (electronic; eISBN)
    Language: German , English
    Note: Beitr. teilw. dt., teilw. engl.
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  • 33
    Call number: MOP 45557 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 221 Seiten , Illustrationen , 21 cm
    Language: Russian
    Note: In kyrillischer Schrift
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  • 34
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-76/34
    In: CRREL Report, 76-34
    Description / Table of Contents: Some physical characteristics of two grounded floebergs (fragments of multi-year pressure ridges) near Prudhoe Bay, Alaska, are described. Cross-sectional profiles of the sails and keels of both floebergs were obtained. A sail to keel ratio of 1 to 3.38 obtained with one floeberg was found to be in good agreement with previous investigations. A survey of the sea floor for evidence of scoring induced during grounding yielded a maximum depth of gouging of 1.1m. Additional studies included investigations of the internal structure of the floebergs, and a brief examination of the organic and sedimentary debris found entrained within the floebergs. The grounding of ice on the continental shelves of the Arctic is of considerable interest to those concerned with the development and impact of development of these continental shelves. The field study reported here provides information useful in assessing the nature and characteristics of interactions between floebergs and the sea bed on which they are grounded.
    Type of Medium: Series available for loan
    Pages: iii, 13 Seiten , Illustrationen
    Series Statement: CRREL Report 76-34
    Language: English
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  • 35
    Call number: ZSP-201-76/35
    In: CRREL Report, 76-35
    Description / Table of Contents: Crystalline textures and fabrics of ice cores from the 2164-m-thick ice sheet at Byrd Station, Antarctica, reveal the existence of an anisotropic ice sheet. A gradual but persistent increase in the c-axis preferred orientation of the ice crystals was observed between the surface and 1200m. This progressive growth of an oriented crystal fabric is accompanied by a 20-fold increase in crystal sized between 56 and 600m, followed by virtually no change in crystal size between 6000 and 1200m. A broad vertical clustering of c-axes develops by 1200m. Between 1200 and 1300 m the structure transforms into a fine-grained mosaic of crystals with their basal glide planes now oriented substantially within the horizontal. This highly oriented fine-grained structure, which persists to 1800m, is compatible only with a strong horizontal shear deformation in this part of the ice sheet. Rapid transformation from single- to multiple-maximum fabrics occurs below 1800m. This transformation, accompanied by the growth of very large crystals, is attributed to the overriding effect of relatively high temperatures in the bottom layers of old ice at Byrd Station rather than to a significant decrease in stress. The zone of single-maximum fabrics between 1200 and 1800 m also contains numerous layers of volcanic dust. Fabrics of the very fine-grained ice associated with these dust bands indicate the bands are actively associated with shearing in the ice sheet. Some slipping of ice along the bedrock seems likely at Byrd Station, since the basal ice is at the pressure melting point and liquid water is known to exist at the ice/rock interface.
    Type of Medium: Series available for loan
    Pages: v, 30 Seiten , Illustrationen
    Series Statement: CRREL Report 76-35
    Language: English
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  • 36
    Call number: MOP 44439 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 68 Seiten
    Language: English
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  • 37
    Monograph available for loan
    Monograph available for loan
    [Erscheinungsort nicht ermittelbar] : [Verlag nicht ermittelbar]
    Call number: MOP 44941 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 24 Seiten
    Language: English
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  • 38
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-79/29
    In: CRREL Report, 79-29
    Description / Table of Contents: An analytical study of the propagation of shock waves in snow was carried out to evaluate the response of medium density snow to high rates of loading. One solution was developed for steady shock waves; this resulted in calculation of pressure jump, density jump and stress wave speed. Correlation with available experimental data was found to be good. Nonsteady shock waves were also considered in order to evaluate wave attenuation rates in snow. Very few data were available to compare with the analytical results, so no definite conclusions on the part of the study could be made. The results show, however, that shock waves that produce plastic deformation attenuate at extremely high rates and that differences in pressure between two waves are quickly eliminated within a short distance. Calculations were also made to evaluate the effect of wave frequency on attenuation rates. The results show that, for plastic waves, frequency is not a predominant factor for determining attenuation rates.
    Type of Medium: Series available for loan
    Pages: v, 14 Seiten , Illustrationen
    Series Statement: CRREL Report 79-29
    Language: English
    Note: CONTENTS Abstract Preface Nomenclature I. Introduction II. A constitutive law for snow and balance principles III. Compatibility laws and jump equations for stress waves IV. Steady shock waves in snow V. Comparison of steady-wave theory with experimental results VI. A numerical solution to the nonsteady wave problem VII. Jump equations for nonsteady shock waves VIII. Reduced jump equations Discussion and conclusions Literature cited
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  • 39
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-79/28
    In: CRREL Report, 79-28
    Description / Table of Contents: Transmission and scanning electron micrographs of Umiat bentonite revealed thin, mica-like grains with irregular shapes. Most of the bentonite showed electron diffraction ring patterns, but some showed hexagonal net patterns as well as ring patterns. The lengths of the unit cells were calculated to be 5.18 A along the a-axis and 8.97 A along the b-axis. Semiquantitative analyses were made using an energy dispersive spectrometer. Common elements such as Si, Ti, Al, Fe, Mg, Na and K were determined. The molecular ratio of SiO2:Al2O3 was calculated to be 492:100 for the bulk sample, indicating that Umiat bentonite is similar in most respects to Wyoming bentonite, and is classified as a mont-morillonite. The microstructure of frozen Umiat bentonite was observed at a specimen temperature of -100 C using a scanning electron microscope equipped with a cold stage. Frozen bentonite and segregated ice patterns formed from wet bentonite were examined using an X-ray map and Si X-ray line scan. Sublimation processes of ice in the frozen bentonite were observed at specimen temperatures of -60 and -80 C. After sublimation of the ice the bentonite displayed a honeycomb structure. It was concluded that the freezing-sublimation cycle in frozen soil increases the permeability of water vapor due to the three-dimensional structure of the coagulated clay formed by freezing.
    Type of Medium: Series available for loan
    Pages: iii, 14 Seiten , Illustrationen
    Series Statement: CRREL Report 79-28
    Language: English
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  • 40
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-79/25
    In: CRREL Report, 79-25
    In: Charged dislocation in ice, I.
    Description / Table of Contents: The motion of dislocations in single crystal ice under an electric field was observed by using X-ray topographic methods. Electric charge density on these dislocations was deduced from the amplitude and length of the dislocation segment under the known AC electrical field. The most likely linear charge density was about +5x10^-11 c/m, although considerable variation is possible depending on the effective field acting on the dislocation lines.
    Type of Medium: Series available for loan
    Pages: iii, 12 Seiten , Illustrationen
    Series Statement: CRREL Report 79-25
    Language: English
    Note: CONTENTS Abstract Preface Introduction Theory Experimental apparatus and procedure Results Discussion Concluding remarks Selected bibliography Appendix A. Mosotti type field on core of cylindrical cavity
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  • 41
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-79/24
    In: CRREL Report, 79-24
    Description / Table of Contents: By using a new thermocoring technique, a hole was successfully drilled through the 416-m thickness of the Ross Ice Shelf at J-9 Camp. This report provides a description of the drill and an account of this drilling project. A provisional examination of the core shows the ice shelf to consist of 410 m of snow and glacial ice underlain by 6 m of sea ice formed by direct freezing of sea water to the bottom of the Ross Ice Shelf.
    Type of Medium: Series available for loan
    Pages: ii, 12 Seiten , Illustrationen
    Series Statement: CRREL Report 79-24
    Language: English
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  • 42
    Call number: ZSP-201-79/23
    In: CRREL Report, 79-23
    Description / Table of Contents: The performance of surface impedance and magnetic induction electromagnetic subsurface exploration techniques was studied seasonally at various sites in Alaska where permafrost and massive ground ice occurred. The surface impedance method, which uses radiowaves in the LF and VLF bands, and the magnetic induction method, which uses low-frequency magnetic induction fields, distinguish subsurface materials by the electrical resistivity of the materials. The methods used have greatest sensitivity within about 20 m of the surface and are, therefore, most applicable for shallow subsurface investigations. The selection of study sites was based on anticipated contrasts in electrical resistivity between ground ice and adjacent earth materials. A magnetic induction instrument, using a separation of 3.66-m between the transmitter and receiver antennas, in general was able to detect near-surface zones of massive ice and to provide data regarding permafrost distribution in both the Fairbanks and Prudhoe Bay areas. At this antenna separation, the depth of magnetic field penetration was sufficient to include mainly the zone containing maximum contrasts in resistivity between ground ice and other earth materials. In the Fairbanks area, contrasts, in this zone were greatest in late winter when the seasonally thawed surface layer was completely frozen. When thawed, this layer usually becomes more conductive and often masks the deeper resistivity contrasts. In the Prudhoe Bay area, maximum ground resistivity contrasts were detected in late summer when shallow subsurface temperatures had risen sufficiently to permit resistivity contrasts between the massive ice and the ice-rich ground to appear.
    Type of Medium: Series available for loan
    Pages: v, 24 Seiten , Illustrationen
    Series Statement: CRREL Report 79-23
    Language: English
    Note: CONTENTS Abstract Preface Introduction Background Obiectives and procedures Ground electrical resistivity in permafrost regions Electromagnetic techniques General Magnetic induction method Surface impedance fradiowave method Direct current method General description of field sites Results Site 1 CRREL permafrost station, Fairbanks, Alaska Site 2 Planned road cut for Steese Highway near Fox, Alaska Site 3 Relic floodplain near Fairbanks, Alaska Site 4 Pingos, Prudhoe Bay, Alaska Site 5 Ice wedges, Prudhoe Bay, Alaska Comparisons between the surface impedance and magnetic induction methods Conclusions and recommendations Literature cited Appendix A. Discussion of the depth of sensitivity of the magnetic induction method using two- and three-layer apparent resistivity curves
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  • 43
    Call number: MOP 46654 / Mitte
    In: World weather program : plan for fiscal year, 1980 and 1981
    Type of Medium: Series available for loan
    Language: English
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  • 44
    Monograph available for loan
    Monograph available for loan
    Durham : Duke University Press
    Call number: IASS 20.95309
    Type of Medium: Monograph available for loan
    Pages: 620 Seiten , 25 cm
    ISBN: 0822335182 , 9780822335184 , 0822335069 , 9780822335061
    Series Statement: Politics, history, and culture
    Language: English
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  • 45
    Monograph available for loan
    Monograph available for loan
    New York : Oxford Univ. Press
    Call number: IASS 20.94162
    Type of Medium: Monograph available for loan
    Pages: XII, 278 S , Ill , 24 cm
    ISBN: 9780195187434 , 0195187431 , 019518744X , 9780195187441
    Series Statement: Studies in feminist philosophy
    Language: English
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  • 46
    Call number: MOP 42980 / Mitte
    Type of Medium: Monograph available for loan
    Language: English
    Location: MOP - must be ordered
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  • 47
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-79/27
    In: CRREL Report, 79-27
    Description / Table of Contents: Some Bessel function identities found by solving problems of the deflection of a floating ice plate by two different methods are rigorously proved. The master formulas from which all the identities are derived are in a Fourier reciprocal relationship, connecting a Hankel function to an exponential function. Many new formulas can be derived from the master formulas. The analytical method presented here now opens the way to study a hitherto impossible type of problem--the deflection of floating elastic plates of various shapes and boundary conditions.
    Type of Medium: Series available for loan
    Pages: ii, 13 Seiten , Illustrationen
    Series Statement: CRREL Report 79-27
    Language: English
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  • 48
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-79/26
    In: CRREL Report, 79-26
    Description / Table of Contents: A 19-year record of the annual closing and opening dates of operation of the Lake Champlain ferry at Grand Isle, Vermont, which are controlled by the lake's ice cover, was made available to CRREL. These navigation records accurately approximated the freeze-over and breakup dates for the ferry crossing area between Gordon Landing, Vermont, and Cumberland Head, New York. When compared statistically with water temperature and climatological data for the same years at nearby Lake Champlain locations, the dates allowed accurate predictions of ice formation. From nearby air temperature records, cumulative freezing degree-day (deg C) curves were plotted for each year of record, and ice formation dates and standard deviations were predicted with considerable accuracy. Several methods of predicting ice formation on Lake Champlain were attempted. The most accurate approach used a combination of water temperatures and freezing degree-days. The influence of wind speed on ice cover formation and prediction are also discussed in the report.
    Type of Medium: Series available for loan
    Pages: v, 21 Seiten , Illustrationen
    Series Statement: CRREL Report 79-26
    Language: English
    Note: CONTENTS Abstract Preface Introduction Data tabulation and collection Air temperatures 11-reezing degree-days Water temperatures Closing and opening dates Results Air temperature Freezing degree-days Water temperatures Analysis: Attempted methods of predicting ice formation Predicting air temperatures 8Summer water temperatures Fall water temperatures and freezing degree-days Wind speed influence on closing of the lake Water temperature vs surface air temperature analysis Prediction of ice-out dates Conclusions Literature cited Appendix A. Freezing degree-day curves with ice notations and watertemperature notations Appendix B. Summary
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  • 49
    Monograph available for loan
    Monograph available for loan
    New York [u.a.] : Plenum Press
    Call number: 9790
    Type of Medium: Monograph available for loan
    Pages: XV, 508 Seiten , Illustrationen
    ISBN: 0306307391
    Language: English
    Location: Upper compact magazine
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  • 50
    Monograph available for loan
    Monograph available for loan
    London : Thames & Hudson
    Call number: IASS 21.94677
    Type of Medium: Monograph available for loan
    Pages: 528 S , zahlr. Ill., graph. Darst , 29cm
    Edition: 1. publ.
    ISBN: 0500513759 (hbk.) , 9780500513750 (hbk.)
    Language: English
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  • 51
    Call number: IASS 20.94318
    Type of Medium: Monograph available for loan
    Pages: 207 Seiten , 24cm
    ISBN: 9781138882331 , 9780415466202
    Series Statement: Environmental politics
    Language: English
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  • 52
    Call number: MOP 44044 / Mitte
    Type of Medium: Monograph available for loan
    Pages: vi, 126 Seiten , Illustrationen , 28 cm
    Language: English
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  • 53
    Call number: AWI Bio-21-94355
    Type of Medium: Monograph available for loan
    Pages: 168 Seiten , Illustrationen
    ISBN: 9783906166568
    Series Statement: Diatom monographs 9
    Language: English
    Note: CONTENTS ABSTRACT 1. INTRODUCTION 2. AIMS AND SCOPE 3. NATURAL AND ANTHROPOGENIC ACIDIFICATION AND ITS ECOLOGICAL CONSEQUENCES 3.1. The role of water pH 3.2. Description of natural and anthropogenic acid sources 3.3. Anthropogenic acidification and its ecological consequences 3.4. Diatoms as indicators of water acidity and related factors 4. MATERIAL AND METHODS 4.1. Field samples 4.2. Laboratory methods 4.3. Data analysis 5. DESCRIPTION OF THE STUDY AREAS 6. RESULTS 6.1. Diatom community patterns vs. water chemistry in relation to different water types 6.2. Diatom community patterns in relation to altitude 6.3. Diatom community patterns in relation to dijf'erent geographical regions in Poland and Finland 6.4. Diatoms as indicators of pH, alkalinity and TOC 6.5. Restoration and recovery of acidified aquatic ecosystems 6.5.1. Diatoms as indicators of restoration: effect of water neutralization 6.5.2. Diatoms as indicators of lake recovery 7. DISCUSSION 8. NOTES ON AUTECOLOGY OF SELECTED DIATOM TAXA 9. SUMMARY AND CONCLUSIONS ACKNOWLEDGEMENTS REFERENCES APPENDIX (Codes of diatom taxa used in the graphs and tables) PLATES
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  • 54
    Monograph available for loan
    Monograph available for loan
    New Dehli : New Age International Publishers
    Call number: AWI Bio-22-94883
    Type of Medium: Monograph available for loan
    Pages: XI, 349 Seiten , Illustrationen
    Edition: Reprint 2005
    ISBN: 0470213590 , 085226240X , 81-224-1343-9
    Language: English
    Note: Contents Foreword, by Professor Dr. Martin Bopp Preface Acknowledgements 1. EXPERIMENTS ON SPORES AND GEMMAE Spore Germination in Liverwort - Jungermanniales, Marchantiales, Anthocerotales, Sphaerocarpales; Types of Spore Germination in Mosses - Sphagnales, Andreaeales, Tetraphidales, Bryales Factors Affecting Spore Germination - Light, Temperature, Sugars, Minerals, Growth Regulators, Hydrogen-ion concentration (pH), OtheT Factors Mechanism of Spore Germination Experiments on Gemmae - light, Temperature, Humidity and other Physical Factors, Growth Regulators, Nitrogenous Substances, Hydrogen-ion concentration (pH), Other Chemical Factors References 2. PROTONEMAL DIFFERENTIATION AND BUD FORMATION IN MOSSES Protonemal Differentiation Bud Formation Factors Affecting Bud Formation - Light, Temperature, Auxins, Cytokinins, Gibberellins, Adenosine 3', 5'-cyclic monophosphate, Adenine and Amino Acids, Minerals and Chelates Vitamins, Abscisic Acid, Sugars, pH, Influence of Other Organisms References. 3. REGENERATION Potentialities of Various Organs for Regeneration - Regeneration from Leaves, Regeneration from Setae Morphology of Régénérants Factors Affecting Regeneration - Light. Radiation, pH, Season, Humidity. Wounding, Temperature, Size of the Fragment Reserve Food Material. Location in the Plant, Age, Correlative Inhibition. Polarity and Apical Dominance Changes Occurring in Regenerating Cells References 4. REPRODUCTIVE BIOLOGY Factors Affecting Gametangial Induction - Light Duration, Light Level, Light Quality. Temperature, Temperature-Photoperiod Interaction. Humidity. Hydration. Carbohydrates. Nitrogenous Substances, Growth Regulators, Chelating Agents, pH and Other Factors References 5. ALTERNATIVE PATHWAYS IN LIFE CYCLE Apogamy - Occurrence of Apogamy in Diplophase and Haplophase, Spore Production in Apogamous Sporophytes, Differentiation of Apogamous Sporophytes from Callus, Factors Controlling Differentiation of Apogamous Sporophytes: Exogenous Factors, Endogenous Factors, Differentiation of Sporophyte and Gametophyte, Role of Calyptra in Sporogon Development Apospory Callus Formation and its Differentiation - Formation of Callus. Differentiation in Callus Controls in Differentiation Alternation of Generations References 6. PHOTOMORPHOGENESIS Spore Germination - Liverworts, Mosses Growth - Liverworts, Mosses Vegetative Propagation - Liverworts, Mosses Metabolism - Liverworts. Mosses; Senescence Bud Induction in Mosses Tropic Responses - Liverworts, Mosses References. 7. ULTRASTRUCTURAL STUDIES Spore Protonema Stem Leaf Gametangia - Antheridium Gametogenesis - Spermatogenesis, Oogenesis Sporogenesis - Spore Sac or Tapetum. Fluctuation in Plastid Number, Structural Changes in Plastids, Cytoplasm, and Other Organelles. Meiosis. Spore Wall Formation Sporophyte-Ganietophyte Junction Seta Histoenzymological Studies - Localization of Enzymes in the Haustorial Foot References 8. CHEMICAL CONSTITUENTS OF BRYOPHYTES Antibiotics Growth Substances - Specified Growth Substances, Non-specified Growth Substances Lipids - Alkanes, Fatty Acids, Cuticular Components Terpenoids - Monoterpenoids, Sesquiterpenoids, Ditetpenoids, Triterpenoids and Sterols Flavonoids - Flavones, Isoflavones, Flavonols, Dihydrofiavonoids and Biflavonyls, Aurones and Chalcones, Acylated Flavonoids, Anthocyanins and Proanthocyanidins, Sphagnorubins Lignins; Other Constitutents - Carotenoids, Carbohydrates, Organic Acids, Dihydrostilbenes, Enzymes, Amino Acids and Quinones, Inorganic Compounds, Miscellaneous, Antitumour Activities, Allergenic Activities References 9. BRYOPHYTES AS INDICATORS OF POLLUTION Heavy Metals - Lead, Cadmium, Zinc, Mercury, Arsenates, Chromium, Nickel. Vanadium Stability Pattern of Metal Ions Metal Tolerance - Copper Mosses, Peat Mosses Gaseous Pollutants - Sulphur dioxide. Fluorides, Ozone Radionuclides (Radio Isotopes) - Cesium. Strontium, Uranium; Radiations References. 10. PROTOPLAST CULTURE Isolation of Protoplasts - Mechanical Method, Enzymatic Method, Source Material for Protoplasts, Factors Affecting Protoplast Isolation: Culture of Protoplasts—Liquid Culture Agar Plating of Protoplasts: Regeneration of Protoplasts - Factors Affecting Regeneration Protoplast Fusion and Somatic Hybrids Induction and Isolation of Mutants References. 11. CONDUCTION IN BRYOPHYTES External Conduction - Gametophyte. Sporophyte, Significance of External Conduction Internal Conduction - Cells Involved in Conduction, Anatomy of the Horizontal Axis, Midribs and Leaf Traces. Conducting Strand in Seta and Capsule, Development and Structure of Mature Conducting Tissues. The Interphase, Internal Conduction of Water, Conduction of Organic Compounds; Evolutionary Trends in the Conducting Strands References. 12. WATER RELATIONS Absorption and Conduction of Water - Endohydric.' Ectohydric, Myxohydric Water Holding Capacity and Growth Rate Desiccation and Rehydration Mechanism of Damage Growth-Forms References SUBJECT INDEX PLANT INDEX AUTHOR INDEX
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  • 55
    Call number: MR 22.94991
    Type of Medium: Monograph available for loan
    Pages: 186, XVI, 187 - 410 Seiten , Illustrationen [zum Teil farbig], graphische Darstellungen, Karten
    ISBN: 978-1893912-00-7
    Series Statement: SI/MAB Series 11
    Language: English
    Note: Sprache der Zusammenfassung: Französisch
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  • 56
    Call number: AWI G3-23-94993
    Type of Medium: Monograph available for loan
    Pages: 24 Seiten , Illustrationen
    Language: English
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  • 57
    Monograph available for loan
    Monograph available for loan
    Malden, Mass. [u.a.] : Blackwell
    Call number: AWI G3-23-95310
    Type of Medium: Monograph available for loan
    Pages: XVIII, 261 Seiten , Illustrationen, Diagramme, Karten
    ISBN: 140512976X , 1-4051-2976-X , 978-1-4051-2976-3
    Series Statement: Environmental systems and global change series 1
    Language: English
    Note: Contents Preface 1 The evidence for cryospheric change 1.1 Introduction 1.2 The geomorphic and hydrologic effects of cryospheric change 1.3 Sub-arctic and alpine hydrology 1.4 Glacier loss and mountain permafrost 1.5 Permafrost 1.6 The carbon balance of the cryosphere 1.7 River and lake ice break-up and freeze-up 1.8 Ocean circulation 1.9 The mass balance of the polar ice sheets 1.10 Sea level 1.11 Importance of sea ice. 1.12 Ecological impacts 1.13 Socio-economic effects 1.14 Conclusions (Text word count-including figure captions and tables but excluding references- 9,015) 2 The monitoring of cryospheric change 2.1 Introduction 2.2 In situ measurements 2.2.1 Land surface air temperature 2.2.2 Terrestrial snow and snow on sea ice 2.2.3 Sea ice 2.2.4 Ice sheets and alpine glaciers 2.2.5 Permafrost and seasonally frozen ground 2.2.6 River runoff 2.2.7 River and lake ice freeze-up and break-up 2.3 Conclusions 3 Processes of cryospheric change 3.1 Introduction 3.2 Snow and ice as energy regulators 3.2.1 The energetics of the snow surface 3.2.2 The energetics of the snowpack 3.2.3 The energetics of glaciers 3.2.4 The energetics of sea ice and various terrain types 3.2.5 Permafrost 3.3 Snow and ice reservoir functions 3.3.1 Mass budget for snow 3.3.2 Mass balance for glacier ice 3.3.3 The mass balance of an ice sheet 3.3.4 Mass balance of sea ice 3.4 Snowfall 3.4.1 Interception by vegetation 3.4.2 Snow accumulation 3.4.3 Snow cover structure 3.5 Snow avalanches 3.6 Snow melt, runoff and streamflow generation 3.7 Snow chemistry 3.8 Snow ecology 3.9 Glacier melt 3.10 Formation of an ice cover 3.11 River and lake ice 3.12 Sediment budgets 4 Patterns of the contemporary cryosphere at local to global scales 4.1 Introduction 4.2 Remote sensing observations 4.3 Land and sea surface temperature 4.3.1 Terrestrial snow and snow on sea ice 4.3.2 Sea ice 4.3.3 Ice sheets & glaciers: estimation of volume 4.3.4 Ice sheets & glaciers: mass balance components 4.3.5 Permafrost 4.3.6 River runoff 4.3.7 River and lake ice freeze-up/break-up 4.4 Numerical Models 4.5 Conclusions: validation, coordinated projects and climate data records 5 The evidence for past cryospheric changes 5.1 Introduction 5.2 The uniqueness of the Quaternary Period 5.3. Initiation of glacial ages 5.4 Reconstructing extent of glacial environments 5.5 Extreme events 5.6 Ice sheet modelling 5.6.1 The Antarctic Ice Sheet 5.6.2 Greenland 5.6.3 North America: Innuitian, Laurentide and Cordilleran ice sheets 5.6.4 British Isles, Scandinavian and Barents ice sheets 5.6.5 The Patagonian and New Zealand ice caps 5.7 Non-glacial Quaternary environments 5.7.1 Late Quaternary permafrost in North America and Europe 5.7.2 Treeline variations 5.7.3 Climatic snowline 5.7.4 Glacier fluctuations 5.7.5 Paraglaciation 6 The transience of the cryosphere and transitional landscapes 6.1 Introduction 6.1.1 The landscape as palimpsest 6.2 Glacial landscapes: macro scale 6.2.1 Cirque landscapes 6.2.2 Fjord and strandflat landscapes 6.3 Periglacial landscapes: macro-scale 6.4 Paraglacial landscapes: macro-scale 6.5 Glacial landscapes: medium-scale 6.5.1 The transition from glacial to fluvial dominance 6.6 Proglacial landscapes: medium-scale 6.6.1 Glacifluvial landforms 6.6.2 The Channeled Scablands 6.6.3 Sub-glacial channels 6.6.4 Sub-glacial, ice-marginal and supraglacial sediment-landform associations 6.7 Periglacial landscapes: medium scale 6.7.1 The transition from periglacial to fluvial dominance 6.8 Paraglacial landscapes: medium-scale 6.9 Glacial landscapes: local-scale 6.9.1 Primary glacigenic deposits 6.9.2 Small scale erosional forms 6.10 Proglacial landscapes: local-scale 6.11 Periglacial landscapes: local scale 6.13 Paraglacial landscapes: local-scale 6.13 Landscape resistance, collapse and recovery 6.14 Transitional landscapes at Quaternary, Holocene and Anthropocene timescales 7 Cryospheric change and vulnerability at Quaternary, Holocene and Anthropocene time scales 7.1 Introduction 7.2 Panarchy 7.2.1 Panarchy, sustainability and transformability 7.2.2 Collapse and the vulnerability of socio-economic systems 7.3 Changing ice cover and biomes since the Last Glacial Maximum 7.3.1 The Last Glacial Maximum 7.3.2 The Holocene Optimum 7.4 The first explorers in North America 7.5 Implications of cryospheric change/collapse 7.5.1 Snow quantity 7.5.2 Snow quality 7.5.3 River and lake ice 7.5.4 Permafrost 7.5.5 Glaciers 7.5.6 River basins 7.5.7 Sea ice 7.5.8 Ice sheets 7.5.9 Sea level change 7.5.10 Carbon sequestration 7.5.11 Vegetation 7.5.12 Polar bears 7.5.13 Human health 7.5.14 Persistent organic pollutants 7.5.15 Socio-cultural conditions and health status 7.5.16 Livelihoods and socio-economic conditions 7.5.17 Governance 7.6 Concluding thoughts References Index
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  • 58
    Call number: AWI G3-23-95315
    Description / Table of Contents: In the monograph results of long-term ground and remote sensing experimental and theoretical investigations of heat-water exchange of typical permafrost landscapes and small river basins of Eastern Siberia and its factors situated in subarctic tundra, plain taiga and southern mountain taiga are generalized. Detailed maps of landscape structure of range grounds as well as results of analysis of wide range of parameters and variables of permafrost landscapes characterizing spatial and temporal variability of their state in daily, seasonal and long-term scales are presented. Zonal-landscape features of heat and water exchange as well as water regime of small river basins have been revealed. Spatial distribution of vertical turbulent heat and moisture flows in the boundary layer of the atmosphere above heterogeneous surface by measurements from board a plane has been investigated. Spatial and temporal analysis of thermo- and water-physical properties of perennially frozen grounds, which are applied as parameters in hydro-climatic models, has been fulfilled. Processes of interaction of surface and underground waters on plain and in the mountains have been considered, as well as cryogenic phenomena, which have considerable impact upon water regime of rivers and permafrost landscapes.
    Type of Medium: Monograph available for loan
    Pages: 575 Seiten , Illustrationen
    ISBN: 978-5-89658-033-1 , 978-5-94789-232-1
    Language: Russian
    Note: Contents Introduction / A.G. Georgiadi, A.N. Zolotokrylin CHAPTER 1. SUBARCTIC TUNDRA 1.1. Characteristics of subarctic polygon and a complex of field experimental investigations / A.G. Georgiadi 1.2. Landscapes and their characteristics 1.2.1. Types and distribution over territory / R.V. Desyatkin, L.D. Hinzman 1.2.2. Seasonal changes of spectral characteristics of landscapes by data of remote sensing measurements / V.B. Malyshev, N. S. Ozerov 1.3. The active layer of subarctic landscapes: typology and geography 1.3.1. Spatial variabi!ity of the active layer thickness / A.G. Georgiadi, V.G. Onischenko 1.3.2. Hydrophysical characteristics of the seasonal-melting layer / A.G. Georgiadi,V.G. Onischenko 1.4. Radiation and thermal characteristics of landscapes in the summer period 1.4.1. Systematization of experimental information on albedo and surface temperature / A.N. Zolotokrylin 1.4.2. Analysis of experimental information on the surface temperature / A.N. Zolotokrylin, V.V. Vinogradova 1.5. Heat exchange in tundra landscapes 1.5.1. Structure of heat exchange and its seasonal features / A.N. Zolotokrylin 1.5.2. Theoretical analysis of the process of heat transfer in the surface thawed layer of soil grounds / A.B. Kazansky, A.N. Zolotokrylin 1.6. Features of water regime and water exchange in tundra 1.6.1. Water regime and water balance of river basins by results of experimental measurements / A.G. Georgiadi 1.6.2. Interrelationship of underground and surface waters and underground alimentation of rivers in different year seasons / V.V. Shepelev CHAPTER 2. CENTRAL PLAIN TAIGA 2.1. Geographical characteristics of Spasskaya Pad polygon / A.N. Fedorov 2.2. Types of landscapes, their distribution over territory and seasonal dynamics / A.N. Fedorov, Ya. I. Torgovkin, S.P. Varlamov 2.3. Characteristics of the active layer and its physical properties 2.3.1. Spatial and seasonal variability of the active layer thickness 2.3.1.1. Inter-landscape variability of the seasonal-thawing layer thickness / I.S. Vasiliev 2.3.1.2. Variability of the active layer thickness at experimental sites / E.Yu. Gerasimov 2.3.1.3. Freezing of the active layer / P.Ya. Konstantinov 2.3.2. Physical properties of soils of the seasonal-thawing layer under larch forest / A.G. Georgiadi, V.G. Onischenko 2.3.3. Inter-landscape differences of physical properties of the active layer / P.Ya. Konstantinov, I.S. Ugarov, R.N. Argunov 2.3.4. Features of thermal conductivity of soil grounds / V.G. Onischenko, I.S. Lisker, A.G. Georgiadi 2.4. Radiation balance and thermal regime of landscapes 2.4.1. Radiation balance and its components / I.S. Ugarov 2.4.2. Temperature regime of the active layer / P.P. Gavriliev, I.S. Ugarov, P.V. Efremov 2.4.3. Temperature regime of the upper layers of perennially frozen grounds / P.Ya. Konstantinov 2.5.Heat exchange in permafrost landscapes of plain taiga / P.P. Gavriliev 2.6. Features of heat and moisture balance in taiga-alas landscapes / R.V. Desyatkin, I. Ishii, Kh. Yabuki, A.R. Desyatkin, P.P. Fedorov, T.N. Semenova 2.7. Turbulent energy- and moisture exchange in the atmospheric boundary layer (ABL) over thermally heterogeneous surface (over the Lena River lowland in the Yakutsk area) / M.A. Strunin 2.7.1. Some aspects of the atmospheric boundary layer (ABL) observations using the aircraft laboratory 2.7.2. Aircraft experiment of the atmospheric boundary layer (ABL) observations in the Yakutsk area 2.7.2.1. Aicraft laboratory IL-18d and its instruments for investigations of ABL 2.7.2.2. Scheme and conditions of the aircraft experiment 2.7.2.3. Radiosounding, surface measurements and satellite observations 2.7.2.4. Turbulence and turbulent fluxes data processing and analyzing 2.7.3. Some features of the convective boundary layer (CBL) development over thermally heterogeneous surface 2.7.3.1. Seasonal variability of turbulent fluxes 2.7.3.2. Fine spatial ABL structure 2.7.3.3. Conditions of appearance and development of the mesoscale thermal internal boundary layer (MTIBL) inside the CBL 2.7.3.4. Appearance of the local circulation over thermal mesoscale patch on the underlying surface 2.7.3.5. The local circulation and the problem of energy balance in the atmospheric boundary layer 2.7.3.6. Conditions of applying the scaling models for the CBL developing over heterogeneous underlying surface 2.7.3.7. The spectral structure of fluxes 2.7.3.8. Flux separating into turbulent and mesoscale portions 2.7.3.9. Separating approach models for mesoscale and turbulent fluxes in the CBL 2.7.3.10. Some f eatures of mesoscale and turbulent fluxes seasonal variations 2.7.4. The main results of observations of the CBL, developing over the thermally heterogeneous surface 2.8 Moisture exchange in plain taiga landscape 2.8.1. Moisture regime of the active layer 2.8.1.1. Landscape features of moisture dynamics of the active layer / P.P. Gavriliev, I.S. Ugarov, P.V. Efremov, R.N. Argunov 2.8.1.2. Spatial and temporal distribution of moisture reserves in the active layer / A.N. Fedorov, Ya.I.Torgovkin, R.N. Arguniov, P.P. Gavriliev, I.S. Vasiliev, J.S. Ugarov, P.V. Efremov 2.8.2. Interrelationship of underground and surface waters and underground alimentation of rivers in different seasons / V.V. Shepelev CHAPTER 3. SOUTHERN MOUNTAIN TAIGA 3.1. Natural conditions of the region / V.S. Vuglinsky, M.L. Markov 3.1.1. Climate 3.1.2. Relief and geological structure 3.1.3. Permafrost and hydrogeological conditions 3.1.4. Hydrography and hydrological conditions 3.1.5. Interrelationship of surface and underground waters, underground alimentation of rivers 3.1.5.1. lntraannual dynamics of water exchange of rivers with drained aquifers 3.1.5.2. Seasonal glaciation and its impact upon formation of river runoff 3.2. Results of study of regularities of heat- and moisture exchange at an experimental SHI Mogot polygon / N.G. Vasilenko, S.A. Zhuravin 3.2.1. General characteristics of the Mogot polygon and program of investigations 3.2.2. Landscape and soil characteristics of catchments of the Mogot polygon 3.2.2.1. Landscapes of the Mogot polygon 3.2.2.2. Landscape-hydrology complexes 3.2.2.3. Types of soils and their water physical characteristics 3.2.3. Features of climate in the region of the Mogot polygon 3.2.4. Radiation and heat balances 3.2.4.1. Radiation balance 3.2.4.2. Heat balance 3.2.5. Water balance 3.2.5.1. Methods of identification of the main components of water balance 3.2.5.2. Features of fo rmation of water balance elements 3.2.5.3. Results of calculation of water balances List of literature SUPPLEMENT TO PART 2.7. INSTRUMENTS AND METHODS FOR INVESTIGATION OF THE ATMOSPHERE USING THE AIRCRAFT LABORATORY / M.A. Strunin S.2.7.1. Methods of wind speed and direction, air temperature and humidity and turbulence measurements based on aircraft data S.2.7.2. Aircraft laboratory IL-18d and its instruments for investigation of the atmosphere S.2.7.3. Database of aircraft observations and preliminary data processing S.2.7.4. Errors of turbulent fluxes calculations based on aircraft data S.2.7.5. Methods of spectral analysis of turbulence data S.2.7.6. Calculations of spectral characteristics of fluctuations based on Fourier analysis S.2.7.7. Using the wavelet-transformations for the spectral analysis List of literature to Supplement 2.7 , In kyrillischer Schrift , Einführung und Inhaltsverzeichnis in englischer Sprache
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  • 59
    Monograph available for loan
    Monograph available for loan
    Tsukuba : National Research Institute for Earth Science and Disaster Prevention
    Associated volumes
    Call number: M 19.95290
    In: Technical note of the National Research Institute for Earth Science and Disaster Prevention
    Type of Medium: Monograph available for loan
    Pages: 1 v. (various pagings) , ill., maps (some col.) , 1 CD-ROM (digital ; 4 3/4 in.) , 30 cm.
    Series Statement: Technical note of the National Research Institute for Earth Science and Disaster Prevention 234
    Language: English
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  • 60
    Monograph available for loan
    Monograph available for loan
    Cambridge : Cambridge University Press
    Call number: PIK 24-95567
    Type of Medium: Monograph available for loan
    Pages: XVI, 558 S , graph. Darst
    Edition: Repr.
    ISBN: 0521588707 , 9780521588706 , 9780521380430
    Language: English
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  • 61
    Monograph available for loan
    Monograph available for loan
    Hanover, NH : US Army Cold Regions Research and Engineering Laboratory
    Call number: AWI G7-19-92301
    Description / Table of Contents: The pulse radiosounding technique was used in studying Antarctic land and sea ice, their internal structures, volumes, movements, and physical properties. Electromagnetic properties of different ice types and their measurement are discussed.
    Type of Medium: Monograph available for loan
    Pages: 83 Seiten , Illustrationen
    Series Statement: Draft translation / Cold Regions Research and Engineering Laboratory, Corps of Engineers, U.S. Army 614
    Uniform Title: Radiozondirovanie lʺda 〈rus.〉
    Language: English
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  • 62
    Monograph available for loan
    Monograph available for loan
    Berlin : Springer
    Associated volumes
    Call number: AWI S4-19-91819
    In: Texts in computational science and engineering, 3
    Type of Medium: Monograph available for loan
    Pages: XXIV, 750 Seiten , Illustrationen
    Edition: third edition, corrected 2nd printing 2009
    ISBN: 3540739157 , 9783540739159 , 9783540739166 (electronic)
    Series Statement: Texts in computational science and engineering 3
    Language: English
    Note: Table of Contents 1 Introduction 1.1 Scripting versus Traditional Programming 1.1.1 Why Scripting is Useful in Computational Science 1.1.2 Classification of Programming Languages 1.1.3 Productive Pairs of Programming Languages 1.1.4 Gluing Existing Applications 1.1.5 Scripting Yields Shorter Code 1.1.6 Efficiency 1.1.7 Type-Specification (Declaration) of Variables 1.1.8 Flexible Function Interfaces 1.1.9 Interactive Computing 1.1.10 Creating Code at Run Time 1.1.11 Nested Heterogeneous Data Structures 1.1.12 GUI Programming 1.1.13 Mixed Language Programming 1.1.14 When to Choose a Dynamically Typed Language 1.1.15 Why Python? 1.1.16 Script or Program? 1.2 Preparations for Working with This Book 2 Getting Started with Python Scripting 2.1 A Scientific Hello World Script 2.1.1 Executing Python Scripts 2.1.2 Dissection of the Scientific Hello World Script 2.2 Working with Files and Data 2.2.1 Problem Specification 2.2.2 The Complete Code 2.2.3 Dissection 2.2.4 Working with Files in Memory 2.2.5 Array Computing 2.2.6 Interactive Computing and Debugging 2. 2.7 Efficiency Measurements 2.2.8 Exercises 2.3 Gluing Stand-Alone Applications 2.3.1 The Simulation Code 2.3.2 Using Gnuplot to Visualize Curves 2.3.3 Functionality of the Script 2.3.4 The Complete Code 2.3.5 Dissection 2.3.6 Exercises 2.4 Conducting Numerical Experiments 2.4.1 Wrapping a Loop Around Another Script 2.4.2 Generating an HTML Report 2.4.3 Making Animations 2.4.4 Varying Any Parameter 2.5 File Format Conversion 2.5.1 A Simple Read/Write Script 2.5.2 Storing Data in Dictionaries and Lists 2.5.3 Making a Module with Functions 2.5.4 Exercises 3 Basic Python 3.1 Introductory Topics 3.1.1 Recommended Python Documentation 3.1.2 Control Statements 3.1.3 Running Applications 3.1.4 File Reading and Writing 3.1.5 Output Formatting 3.2 Variables of Different Types 3.2.1 Boolean Types 3.2.2 The None Variable 3.2.3 Numbers and Numerical Expressions 3.2.4 Lists and Tuples 3.2.5 Dictionaries 3.2.6 Splitting and Joining Text 3.2.7 String Operations 3.2.8 Text Processing 3.2.9 The Basics of a Python Class 3.2.10 Copy and Assignment 3.2.11 Determining a Variable's Type 3.2.12 Exercises 3.3 Functions 3.3.1 Keyword Arguments 3.3.2 Doc Strings 3.3.3 Variable Number of Arguments 3.3.4 Call by Reference 3.3.5 Treatment of Input and Output Arguments 3.3.6 Function Objects 3.4 Working with Files and Directories 3.4.1 Listing Files in a Directory 3.4.2 Testing File Types 3.4.3 Removing Files and Directories 3.4.4 Copying and Renaming Files 3.4.5 Splitting Pathnames 3.4.6 Creating and Moving to Directories 3.4.7 Traversing Directory Trees 3.4.8 Exercises 4 Numerical Computing in Python 4.1 A Quick NumPy Primer 4.1.1 Creating Arrays 4.1.2 Array Indexing 4.1.3 Loops over Arrays 4.1.4 Array Computations 4.1.5 More Array Functionality 4.1.6 Type Testing 4.1.7 Matrix Objects 4.1.8 Exercises 4.2 Vectorized Algorithms 4.2.1 From Scalar to Array in Function Arguments 4.2.2 Slicing 4.2.3 Exercises 4.3 More Advanced Array Computing 4.3.1 Random Numbers 4.3.2 Linear Algebra 4.3.3 Plotting 4.3.4 Example: Curve Fitting 4.3.5 Arrays on Structured Grids 4.3.6 File I/O with NumPy Arrays 4.3.7 Functionality in the Numpyutils Module 4.3.8 Exercises 4.4 Other Tools for Numerical Computations 4.4.1 The ScientificPython Package 4.4.2 The SciPy Package 4.4.3 The Python- Matlab Interface 3 4.4.4 Symbolic Computing in Python 4.4.5 Some Useful Python Modules 5 Combining Python with Fortran, C, and C++ 5.1 About Mixed Language Programming 5.1.1 Applications of Mixed Language Programming 5.1.2 Calling C from Python 5.1.3 Automatic Generation of Wrapper Code 5.2 Scientific Hello World Examples 5.2.1 Combining Python and Fortran 5.2.2 Combining Python and C 5.2.3 Combining Python and C++ Functions 5.2.4 Combining Python and C++ Classes 5.2.5 Exercises 5.3 A Simple Computational Steering Example 5.3.1 Modified Time Loop for Repeated Simulations 5.3.2 Creating a P ython Interface 5.3.3 The Steering Python Script 5.3.4 Equipping the Steering Script with a GUI 5.4 Scripting Interfaces to Large Libraries 6 Introduction to GUI Programming 6.1 Scientific Hello World GUI 6.1.1 Introductory Topics 6.1.2 The First Python/Tkinter Encounter 6.1.3 Binding Events 6.1.4 Changing the Layout 6.1.5 The Final Scientific Hello World GUI 6.1.6 An Alternative to Tkinter Variables 6.1.7 About the Pack Command 6.1.8 An Introduction to the Grid Geometry Manager 6.1.9 Implementing a GUI as a Class 6.1.10 A Simple Graphical Function Evaluator 6.1.11 Exercises 6.2 Adding GUis to Scripts 6.2.1 A Simulation and Visualization Script with a GUI 6.2.2 Improving the Layout 6.2.3 Exercises 6.3 A List of Common Widget Operations 6.3.1 Frame 6.3.2 Label 6.3.3 Button 6.3.4 Text Entry 6.3.5 Balloon Help 6.3.6 Option Menu 6.3.7 Slider 6.3.8 Check Button 6.3.9 Making a Simple Megawidget 6.3.10 Menu Bar 6.3.11 List Data 6.3.12 Listbox 6.3.13 Radio Button 6.3.14 Combo Box 6.3.15 Message Box 6.3.16 User-Defined Dialogs 6.3.17 Color-Picker Dialogs 6.3.18 File Selection Dialogs 6.3.19 Toplevel 6.3.20 Some Other Types of Widgets 6.3.21 Adapting Widgets to the User's Resize Actions 6.3.22 Customizing Fonts and Colors 6.3.23 Widget Overview 6.3.24 Exercises 7 Web Interfaces and CGI Programming 7.1 Introductory CGI Scripts 7.1.1 Web Forms and CGI Scripts 7.1.2 Generating Forms in CGI Scripts 7.1.3 Debugging CGI Scripts 7.1.4 A General Shell Script Wrapper for CGI Scripts 7.1.5 Security Issues 7.2 Adding Web Interfaces to Scripts 7.2.1 A Class for Form Parameters 7.2.2 Calling Other Programs 7.2.3 Running Simulations 7.2.4 Getting a CGI Script to Work 7.2.5 Using Web Applications from Scripts 7.2.6 Exercises 8 Advanced Python 8.1 Miscellaneous Topics 8.1.1 Parsing Command-Line Arguments 8.1.2 Platform-Dependent Operations 8.1.3 Run-Time Generation of Code 8.1.4 Exercises 8.2 Regular Expressions and Text Processing 8.2.1 Motivation 8.2.2 Special Characters 8.2.3 Regular Expressions for Real Numbers 8.2.4 Using Groups to Extract Parts of a Text 8.2.5 Extracting Interval Limits 8.2.6 Extracting Multiple Matches 8.2.7 Splitting Text 8.2.8 Pattern-Matching Modifiers 8.2.9 Substitution and Backreferences 8.2.10 Example: Swapping Arguments in Function Calls 8.2.11 A General Substitution Script 8.2.12 Debugging Regular Expressions 8.2.13 Exercises 8.3 Tools for Handling Data in Files 8.3.1 Writing and Reading Python Data Structures 8.3.2 Pickling Objects 8.3.3 Shelving Objects 8.3.4 Writing and Reading Zip and Tar Archive Files 8.3.5 Downloading Internet Files 8.3.6 Binary Input/Output 8.3.7 Exercises 8.4 A Database for NumPy Arrays 8.4.1 The Structure of the Database 8.4.2 Pickling 8.4.3 Formatted ASCII Storage 8.4.4 Shelving 8.4.5 Comparing the Various Techniques 8.5 Scripts Involving Local and Remote Hosts 8.5.1 Secure Shell Commands 8.5.2 Distributed Simulation and Visualization 8.5.3 Client/Server Programming 8.5.4 Threads 8.6 Classes 8.6.1 Class Programming 8.6.2 Checking the Class Type 8.6.3 Private Data 8.6.4 Static Data 8.6.5 Special Attributes 8.6.6 Special Methods 8.6.7 Multiple Inheritance 8.6.8 Using a Class as a C-like Structure 8.6.9 Attribute Access via String Names 8.6.10 New-Style Classes 8.6.11 Implementing Get/Set Functions via Properties 8.6.12 Subclassing Built-in Types 8.6.13 Building Class Interfaces at Run Time 8.6.14 Building Flexible Class Interfaces 8.6.15 Exercises 8.7 Scope of Variables 8.7.1 Global, Local, and Class Variables 8.7.2 Nested Functions 8.7.3 Dictionaries of Variables in Namespaces 8.8 Exceptions 8.8.1 Handling Exceptions 8.8.2 Raising Exceptions 8.9 Iterators 8.9.1 Constructing an Iterator 8.9.2 A Pointwise Grid Iterator 8.9.3 A Vectorized Grid Iterator 8.9.4 Generators 8.
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  • 63
    Monograph available for loan
    Monograph available for loan
    Novato, Calif. : New World Library
    Call number: IASS 18.91967
    Type of Medium: Monograph available for loan
    Pages: XIII, 417 S. , Ill.
    Edition: 3. ed.
    ISBN: 9781577315933 (hardcover)
    Series Statement: Bollingen series 17
    Language: English
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  • 64
    Monograph available for loan
    Monograph available for loan
    Berkeley, Calif. [u.a.] : Univ. of California Press
    Call number: IASS 19.91968
    Type of Medium: Monograph available for loan
    Pages: XV, 340 Seiten
    Edition: California ed., [Nachdr.]
    ISBN: 9780520015463
    Language: English
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  • 65
    Call number: AWI G6-19-92215
    Type of Medium: Monograph available for loan
    Pages: 182 Seiten , Illustrationen
    Edition: Izd. 2., pererabot. i dop.
    Language: Russian
    Note: In kyrillischer Schrift
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  • 66
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-76/29
    In: CRREL Report, 76-29
    Description / Table of Contents: In order to verify current theoretical equations on ice bearing capacity, a heavily loaded truck was used to make successive passes over two ice bridges. Equipment, weather and the normal problems associated with field work resulted in only one complete breakthrough test. Breakthrough occurred on one bridge with a vehicle weight of 53,630 lb (24,327 kg) and an ice thickness of 17.5 in. (44.5 cm). Since only one test was completed, the conclusions drawn cannot be unequivocal. However, the results do indicate that Nevel's equation for ultimate failure of a floating ice sheet is a good working tool.
    Type of Medium: Series available for loan
    Pages: iv, 19 Seiten , Illustrationen
    Series Statement: CRREL Report 76-29
    Language: English
    Note: Contents Abstract Preface Summary Introduction Location Test procedure Loading Site preparation and bridge construction Deflection measurements Conclusions Literature cited Appendix, Test data
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  • 67
    Call number: M 19.92942
    Type of Medium: Dissertations
    Pages: XVI, 190 Seiten , Illustrationen
    ISBN: 88-902361-0-8
    Language: English
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  • 68
    Call number: M 19.92944
    Type of Medium: Dissertations
    Pages: xxi, 134 Seiten , Illustrationen
    ISBN: 978-90-9022201-1
    Language: English
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  • 69
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-76/44
    In: CRREL Report, 76-44
    Description / Table of Contents: The deformation of wet snow is explained in terms of the thermodynamics of the three phases of water. When deformation by particle rearrangement is fully developed, deformation can occur most rapidly by melting at the particle contacts. The rate of deformation is highly sensitive to the liquid water content, ionic impurity content, particle contact area, and stress level. A model of the hydrostatic deformation of wet snow is constructed, and examples of the deformation of wet snow are given for a variety of conditions. These results are in agreement with existing experimental evidence. The model accurately simulates the transient nature of the deformation and the effect of water content on the quasi-stable density of wet snow subjected to a constant stress.
    Type of Medium: Series available for loan
    Pages: iv, 9 Seiten , Illustrationen
    Series Statement: CRREL Report 76-44
    Language: English
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  • 70
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-76/47
    In: CRREL Report, 76-47
    Description / Table of Contents: This report describes two mechanical ice-cutting systems for the removal of ice collars at the high pool level on the Poe Lock of the St. Marys Falls Canal at Sault Ste. Marie, Michigan. One system was a narrow-kerf (3.25-in.-wide) coal-cutting chain saw mounted on a bar, driven by a 65-hp wheeled trencher. The other system was a lumber-cutting chain saw mounted on a bar, driven by a 30-hp wheeled soil trencher which cut a 0.56-in.-wide kerf. The lumber-cutting saw's bar was too flexible and the desired cutting traverse speed was not met. The coal-cutting saw cut 6-ft-deep ice collars at traverse speeds of up to 10 ft/min and is acceptable. With a few modifications, the coal-cutting saw would be operational.
    Type of Medium: Series available for loan
    Pages: iii, 20 Seiten , Illustrationen
    Series Statement: CRREL Report 76-47
    Language: English
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  • 71
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-77/1
    In: CRREL Report, 77-1
    Description / Table of Contents: Studies of the growth history and structural characteristics of winter ice covers on two New Hampshire lakes are described. These investigations included measurements of ice cover thickness, characterization of the stratigraphic and crystalline structure of the ice, identification and classification of major ice types and measurements of electrolytic conductivity. The formation of cracks and flaws in the ice and their effects on the mechanical properties of the ice were also investigated. A method of correlating ice growth with surface wind and temperature measurement is described and the interrelationships of the various physical and mechanical properties of temperate lake ice covers are discussed.
    Type of Medium: Series available for loan
    Pages: v, 29 Seiten , Illustrationen
    Series Statement: CRREL Report 77-1
    Language: English
    Note: CONTENTS Abstract Preface Summary Introduction Study areas Study methods Winter freeze-up Composition of ice cover Freezing degree day records and applications Evaluation of ice growth coefficient α Growth history and entrapped bubble stratigraphy Mechanical properties Electrolytic conductivity Literature cited
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  • 72
    Call number: AWI G6-19-92329
    In: UFZ-Bericht, 02/2005
    Type of Medium: Series available for loan
    Pages: 173 Seiten , Illustrationen
    ISSN: 0948-9452
    Series Statement: UFZ-Report 02/2005
    Language: English
    Note: Contents: Conference Programme. - Session 1: Contamination / Chairman: D. Hunkeler. - Compound-specific isotope methods in contaminant hydrogeology: State-of-the-art and challenges / D. Hunkeler, Y. Abe. - Stable isotope study of a volatile hydrocarbons contaminated landfill site, Bortfol, Switzerland / Thierry R. Oppikofer, Torsten W. Vennemann, Jorge E. Spangenberg, Markus Bill. - Application of compound-specific stable carbon and hydrogen isotope analysis to characterize organic contamination of groundwater / Jeroen Verhack, Jan Bronders, Ilse Van Keer, Rudy Swennen, Jan Schwarzbauer, Tom N.P. Bosma. - Evidences for in situ natural attenuation of Monochlorobenzene in an anaerobic contaminated aquifer / Ivonne Nijenhuis, Sylvia Uhlig, Arno Kaschl, Marcell Nikolausz, Matthias Kastner, Hans-Hermann Richnow. - Stable isotopes as expert witness in traffic accidents: assessing the likelihood between forensic samples of motor oils / Jorge E. Spangenberg, Georges Pierrini, Christophe Champod, Franco Taroni. - Isotopic investigation of dissolved and sedimentary sulfur compounds for assessing in-situ biodegradation of petroleum hydrocarbons in a sulfate rich urban aquifer / Kay Knoeller, Michael Schubert. - Tracing the impact of river bank filtration on the transport of xenobiotica in urban groundwater by stable isotopes / Karsten Osenbrück, Rolf Trettin, Kay Knoller, Gerhard Strauch, Hans-Reinhard Glaser, Monika Möder. - Effects of covering spoil piles on its water budget determined by environmental isotopes / Stephan M. Weise, Jutta Parnieske-Pasterkamp, Rene Vogt, Franziska Rudolph. - Session 2: Geochemistry & Water / Chairman: J. Hoefs. - Isotope fingerprints in the earth sciences: a critical discussion / Jochen Hoefs. - Stable isotope ratio measurements using the Finnigan NEPTUNE multi collector ICPMS using high mass resolution / Johannes Schwieters, Claudia Bouman. - The mineral isotope composition of two Precambrian carbotiatitc complexes from the Karelian - Kola region / Marion Tichomirowa, Gerhard Grosche, Boris Belyatski, Elena Savva, Jörg Keller, Jens Gotze, Wolfgang Todi. - Development of methods for recovery of water from fluid inclusions for stable isotope analysis / Yuri Dublyansky. - Determination of δD and δ18O in brackish and saline natural waters. Part I: The question of distillation of water samples prior to isotopic analysis / Adam Porowski, Peter Kowski. - Isotopic evidences for a new type of groundwater in the Kinnerct basin, Israel / C. Siebert, S. Geyer, P. Möller. - Geochemical and isotopic investigations of a fractured rock aquifer including embedded lakes / Elke Bozau, Gerhard Strauch. - High spatial resolution sulfur isotope analysis of sulfide minerals from the Kupferschiefer deposits of Lubin area, SW Poland / H. Roy Krouse, Jan Parafiniuk, Jaroslaw Nowak, Stan Halas. - Stable isotope composition of daily and monthly precipitation in Zagreb / Jadranka Barešic, Nada Horvatincic, Ines Krajcar Bronic, Bogomil Obelic. - Geochemical investigations of the dissolved gases in the Boom Clay pore water / Sándor Kele, Hugo Moors, Maarten Van Geet, Mieke De Craen, Staf Valkiers, Mihai Variant. - The water isotopes use for determination of water origin in karstic areas: case study / Victor Feurdean, Lucia Feurdean, Ion Stefanescu, Carmen Varlam, Mihai Gligan. - Concentration and separation of uranium and thorium from sediment in north Algerian Sahara using organophosphorus extractant and ions exchange resin / A. W. Badreddine, H. Brahimi, F. Boucheneb. - Session 3: Ecology / Chairman: L. Waasenaar. - Global application of stable hydrogen isotopes to wildlife forensics / Leonard l. Wassenaar, Keith A. Hobson, Gabriel J. Bowen. - Nitrogen isotope ratios as indicator of organic production / Hilmar Forstel, Angelika Basu, Markus Boner. - Effects of clear cutting and soil preparation on natural 15N abundance and N concentration in the needle and soil of two boreal conifer tree species / S. P. Sah, H. llvesniemi. - Carbon isotopes distribution along pine needles (Pinus nigra) / Lidia Barszczowska, Mariusz-Orion Jedrysek. - Potential of natural fouling communities for assimilation offish farm derived particulate nitrogen: a case study in Gulf of Aqaba (Red Sea) / Sonja Lojen, Timor Katz, Anat Tsemel, Ehud Spanier, Dror L. Angel. - CO2 concentration and δ13C through time in sets of monthly air samples from downtown Parma and from the Parma and Taro river valleys, Italy / Antonio Longinelli. - Carbon isotope discrimination affected by atmospheric pollutants / Ralf Wagner. - Turnover of soil organic carbon - The microbial perspective / Christiane Kramer & Gerd Gleixner. - C and O isotope working standards from C3 and C4 photosynthates / Jorge E. Spangenberg. - Use of 15N tracer technique to understand chronic responses of Daphnia magna after shortterm expose to the pyrethroid insecticide fenvalerate / Sebastian Reynaldi, Matthias Liess, Klaus Jung. - Anthropogenic lakes - negligible sources for climate relevant gases? / Horst-Michael Nitzsche, Frank W. Junge. - Effects of environmental factors on δ13C of lichens / Stela Maria Cuna, Gabriela Balas, Elza Hauer. - Online measurement of N2-fluxes from soil cores by using the zeolite KÖSTROLITH SX6® coupled to a GC-ConFlow-IRMS / O. Spott, B. Apelt, R. Russow, C. F. Stange. - Deuterium content in plants with short lifetime: preliminary results / Victor Feurdean, Lucia Feurdean, Silviu Apahidean, Maria Apahidean, Augusta Lujerdean, Mihai Gligan. - Session 4: Sedimentology / Chairman: M. E. Böttcher. - Authigenic sulfur phases as recorders for black shale-triggered anaerobic oxidation of methane: Results from ODP Leg 207 / M.E. Böttcher, H.-J. Brumsack, A. Hetzel, A. Schipper. - Microbially-derived methane in coalbed gases: compound-specific carbon-isotopic study of coalbed gases from the Illinois Basin, USA / D. Strapoc, A. Schimmelmann, M. Mastalerz. - Early diagenesis of sulphur in recent estuarine sediments (Authie Bay, N France) / Sonja Lojen, Nevenka Mikac, Cedric Gabelle, Michel Wartel. - Sulfur and oxygen isotopes of Lower Miocene nonmarine evaporites in the Upper Silesian Coal Basin / S. Halas, T.M. Peryt, I. Pluta. - Ordovician and Silurian carbon isotope trend: a state of art report based on the East Baltic data / Tonu Martma, Dimitri Kaljo. - Variations of δ13 CTOC values of clastic sediments from Thuringia related to biogeochemical carbon cycle / Karin Bräuer, Knut Hahne, Birgit Mingram, Ulrich Wand. - Basin-Scale changes in Upper Cretaceous paleosols: paleoenvironmentai implication for the Maastricht deposits, South Carpathians / Ana-Voica Bojar, Dan Grigorescu, Franz Ottner, Zoltan Csiki. - Carbon, oxygen, and hydrogen isotope fractionation during experimental formation of pirssonite / M. E. Böttcher, S.M. Bernasconi, K. Simon. - Carbon isotope fractionation of methane and CO2 during coalbed gas desorption from coal, Illinois Basin, USA / D. Strapoc, A. Schimmelmann, M Mastahrz. - Carbon istopic preliminary studies on paleoenvironmentai variations recorded in the Lower Carboniferous deposits from the Bardzkie Mountains (Sudetes, SW Poland) / Monika Majewska-Bill, Mariusz Orion Jedrysek. - Session 5: Paleoclimatology / Chairman: G. H. Schleser. - Stable isotopes as proxies for the reconstruction of past climates / G.H. Schleser. - A stable isotope record of an ice core from Akadumii Nauk ice cap, Severnaya Zemlya, Russian Arctic / Diedrich Fritzsche, Rainer Schütt, Hanno Meyer, Heinrich Miller, Frank Wilhelms, Lev M. Savatyugin. - Stable isotope investigations on tree-ring cellulose of Late Glacial pine chronology of Reichwakie (Lusatia). Effects caused by destruction of fossil woods / M. Haupt, R. Wagner, T. Boettger. - Effect of river regulation on the isotopic characteristics of river water and molluscs / István Fórizs. - Stable isotope study on the carbonate phases of the Basahare toess-paleosol profile (Hungary) / Bernadett Bajnó
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  • 73
    Call number: 9/M 07.0421(473)
    In: Geological Society Special Publication
    Description / Table of Contents: This book complements the Geological Society's Special Publication 362: Military Aspects of Hydrogeology. Generated under the auspices of the Society's History of Geology and Engineering Groups, it contains papers from authors in the UK, USA, Germany and Austria. Substantial papers describe some innovative engineering activities, influenced by geology, undertaken by the armed forces of the opposing nations in World War I. These activities were reactivated and developed in World War II. Examples include trenching from World War I, tunnelling and quarrying from both wars, and the use of geologists to aid German coastal fortification and Allied aerial photographic interpretation in World War II. The extensive introduction and other chapters reveal that ‘military geology’ has a longer history. These chapters relate to pre-twentieth century coastal fortification in the UK and the USA; conflict in the American Civil War; long-term ‘going’ assessments for German forces; tunnel repair after wartime route denial in Hong Kong; and tunnel detection after recent insurgent improvisation in Iraq.
    Type of Medium: Monograph available for loan
    Pages: vi, 314 Seiten , Illustrationen
    ISBN: 978-1-78620-394-6
    Series Statement: Geological Society Special Publication 473
    Language: English
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  • 74
    Call number: AWI Bio-19-92359
    In: Special publications : ESA SP / European Space Agency, 1299
    Type of Medium: Series available for loan
    Pages: VII, 200 Seiten , Illustrationen
    ISBN: 92-9092-393-8
    ISSN: 0379-6566
    Series Statement: Special publications : ESA SP / European Space Agency 1299
    Language: English
    Note: Contents Foreword Introduction / Charles Cockell, Gerda Horneck 1. Mars Simulations - Past Studies on the Biological Response to Simulated Martian Conditions / Aviaja Anna Hansen 2. Possible Atmospheric and UV Conditions on Mars in the Past - Biological Implications / H. Lammer, Yu. N. Kulikov 3. The Microbial Case for Mars and its Implication for Human Expeditions to Mars / Gerda Horneck 4. Response of Organics to Simulated Martian Conditions / J.R.C. Garry, I.L. ten Kate, P. Ehrenfreund, B.H. Foing 5. Mars Simulation Experiments with Complex Microbial Soil Communities / Kai Finster, Aviaja A. Hansen, Lars Liengaard, Karina Mikkelsen, Tommy Kristoffersen, Jonathan Merrison, Per Nornberg, Bente Aa.Lomstein 6. Fungi From Antarctic Desert Rocks as Analogues for Martian Life / S. Onofri, L. Zucconi, L. Selbmann, G. S. de Hoog, D. Barreca, S. Ruisi, M. Grube 7. The Response of Bacillus Subtilis to Simulated Martian Conditions and to the Space Environment / Petra Rettberg 8. Photosynthetic Organisms on Mars - Prospects and Limitations / Charles S. Cockell, Andrew C. Schuerger, Daniela Billi, E. Imre Friedmann, Corinna Panitz 9. Viable Haloarchaea from Ancient Salt Sediments and their Response to Simulated Mars Conditions / Helga Stan-Lotter, Sergiu Fendrihan 10. Response of Methanogenic Archaea from Siberian Permafrost to Martian Thermophysical Conditions / Daria Morozova, Diedrich Mohlmann, Dirk Wagner 11. Adaptation of the Lichen Rhizocarpon Geographicum to Harsh High-Altitude Conditions: Relevance to a Habitable Mars / Rosa de la Torre, Leopoldo Garcia-Sancho, Gerda Horneck 12. Photosynthetic Life Support Systems in the Martian Conditions / Kirsi Lehto, Eira Kanervo, Kurt Stahle, Harry Lehto, Milja Tammi, Joni Virtanen 13. Photo-Catalytic Redox-Processes and Adsorption Water on Mars / Chr. Jung, D. Mohlmann, Chr. Sattler, R. Staudt, M. Weeks 14. Design, Building and Applications of a Portable Martian UV Simulator / C. Kolb, R. Abart, A. Berces, J.R.C. Garry, A. A. Hansen, W. Hohenau, G. Kargl, H. Lammer, MR. Patel, P. Rettberg, H. Stan-Lotter 15. Raman Spectroscopic Analysis of Extremophilic Organisms Under Martian Conditions / Howell G. M. Edwards
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  • 75
    Call number: MOP 44818 / Mitte
    Type of Medium: Monograph available for loan
    Pages: vii, 50 Seiten , 28 cm
    Language: English
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  • 76
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-79/9
    In: CRREL Report, 79-9
    Description / Table of Contents: Sedimentation at the terminus of the Matanuska Glacier has been found to be primarily subaerial in a 100- to 300-m wide, ice-cored zone paralleling the edge of the active ice. Certain physical and chemical characteristics of the ice and debris of the superglacial, englacial and basal zones of the glacier indicate the debris of the basal zone, the primary source of sediment, is entrained during freeze-on of meltwater, probably surficially derived, to the glacier sole. Till formation results from the melting of buried ice of the basal zone. Melt-out till inherits the texture and particle orientations of basal ice debris; other properties are not as well preserved. Most deposits result from resedimentation of till and debris by sediment gravity flows, meltwater sheet and rill flow, slump, spall, and ice ablation. Depositional processes are interrelated in the process of backwasting of ice-cored slopes. Sediment flows are the primary process of resedimentation. Their physical characteristics, multiple mechanisms of flow and deposition, and characteristics of their deposits vary with the water content of the flow mass. Deposits of each process are distinguished from one another by detailed analysis of their internal organization, geometry and dimensions, and the presence of other internal and related external features. Genetic facies are defined by these characteristics. The interrelationship of processes develops a composite depositional sequence defined in terms of genetic facies associations; an upper, resedimented facies association, a middile, till facies association, and a lower, subglacial-resedimental facies association. The lateral and vertical distribution of genetic facies within the associations is mainly nonrepetitive.
    Type of Medium: Series available for loan
    Pages: X, 112 Seiten , Illustrationen , 1 Beilage
    Series Statement: CRREL Report 79-9
    Language: English
    Note: CONTENTS Abstract Preface Summary Chapter 1. Introduction Field site Historical background Chapter 2. Characteristics of the debris and ice Characteristics of the facies and subfacies Basal zone Characteristics of the debris Discussion Chapter 3. Oxygen isotope analysis Sampling and analysis Results Discussion Chapter 4. Depositional processes—till formation Methods of analysis Environmental setting Till formation Chapter 5. Depositional processes—resedimentation Sediment flows Other resedimentation processes Resedimentation process relationships Chapter 6. Process distribution, sediment dispersal and depositional patterns Physical characteristics Sediment dispersal Sedimentary facies Patterns of terminus sedimentation Chapter 7. Conclusions Literature cited
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  • 77
    Call number: MOP 45476 / Mitte
    Type of Medium: Monograph available for loan
    Pages: [400] Seiten , Illustrationen , 28 cm
    Language: English
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  • 78
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-79/21
    In: CRREL Report, 79-21
    Description / Table of Contents: The report studies the question of whether Great Lakes freighters could move effectively through ice-clogged channels with the aid of tows provided by warping or kedging systems. Ten operational concepts are outlined, and their advantages and disadvantages are noted. The crushing resistance of floating brash ice is then analyzed. The neutral, active and passive states of stress for laterally confined brash ice are considered, and the resistance to horizontal thrusting by a smooth vertical wall is calculated for cohesionless brash ice, and for ice in which there is finite cohesion between the ice fragments. The thickening of the ice cover in the vicinity of a "pusher", and the formation of pressure ridges, are analyzed in order to estimate the amount of pile-up that can occur against a ship hull. The analysis then moves on to consideration of ship resistance by brash ice, taking into account crushing resistance at the bow, tangential friction at the bow, and hull friction aft of the bow section. Comparisons are made between thrust from the ship’s screws and the calculated ice resistance. The next section of the report estimates the force requirements for a warping or kedging system in terms of thrust augmentation for existing vessels. Tow cable requirements are given, and estimates are made for cable anchors and for anchorage of underwater structures. The force and power requirements for winches and windlasses are given, the practical problems involved in the pickup or transfer of cables are mentioned, and the report concludes with a brief appraisal. The conclusion is that a simple warping tug system is appropriate for a full scale experiment, a chain ferry with auxiliary barge seems attractive for an operational system, and a chain ferry plow may be an efficient way to clear ice from channels.
    Type of Medium: Series available for loan
    Pages: iv, 21 Seiten , Illustrationen
    Series Statement: CRREL Report 79-21
    Language: English
    Note: CONTENTS Abstract Preface Introduction Operational concepts A. Warping tug system B. Chain ferry system C. Chain ferry with auxiliary barge D. Ski tow system E. Dual winch warping system F. Simple kedging G. Trailing-line system H. Above-surface dual winch system I. Pulley systems J. Chain ferry plow Crushing resistance of fragmented ice covers Resistance to ship passage by broken ice Crushing resistance at the bow Tangential friction at the bow Hull friction aft of the bow section Total ship resistance from brash ice Comparison of ship thrust and ice resistance Force requirements for a warping or kedging system Tow cable requirements Anchors and anchorages Force and power requirements for winches and windlasses Pickup or transfer of cable General appraisal Literature cited
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  • 79
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-76/26
    In: CRREL Report, 76-26
    Description / Table of Contents: Debris over a 44-mile stretch of the Chena River was studied. The study area extended from the first bridge on the Chena Hot Springs Road to the Chena River Flood Control damsite. The purpose of the study was to assess the potential danger to the Chena River Flood Control Dam outlet structure. Debris was catalogued, log jams were measured, and sources of debris were studied. The average size of logs was determined, as well as the number of logs present on the river. The authors concluded that a serious debris problem existed and would remain serious for the foreseeable future. Recommendations for debris handling were made.
    Type of Medium: Series available for loan
    Pages: iv, 17 Seiten , Illustrationen
    Series Statement: CRREL Report 76-26
    Language: English
    Note: Contents Abstract Preface Summary Introduction Origin of debris Volume, magnitude Types of debris Hazards of the debris Recommended measures to counteract log jamming Conclusions and recommendations Future work Epilogue Selected bibliography Appendix: Additional photographs of Chena River debris
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  • 80
    Call number: M 19.92947
    Type of Medium: Dissertations
    Pages: xiv, 182 Seiten , Illustrationen
    ISBN: 978-90-9022454-1
    Language: English
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  • 81
    Call number: MOP 40847 / Mitte
    Type of Medium: Monograph available for loan
    Pages: x, 424 Seiten
    Language: English
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  • 82
    Monograph available for loan
    Monograph available for loan
    Leningrad : Gidrometeoizdat
    Call number: MOP 40419 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 302 Seiten , Illustrationen
    Language: Russian
    Note: Zsfassung in englischer Sprache , In kyrillischer Schrift
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  • 83
    Monograph available for loan
    Monograph available for loan
    Leningrad : Gidrometeoizdat
    Call number: MOP 45175 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 181 Seiten
    Language: Russian
    Note: In kyrillischer Schrift
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  • 84
    Call number: MOP 44237 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 93 Seiten , Illustrationen , 20 cm
    Series Statement: Serija Meteorologija / VNII Gidrometeorologičeskoj Informacii - Mirovoj Centr dannych
    Language: Russian
    Note: In kyrillischer Schrift
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  • 85
    Monograph available for loan
    Monograph available for loan
    Leningrad : Gidrometeoizdat
    Call number: MOP 45690 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 263 Seiten , Illustrationen
    Language: Russian
    Note: In kyrillischer Schrift
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  • 86
    Monograph available for loan
    Monograph available for loan
    Leningrad : Gidrometeoizdat
    Call number: MOP 45688 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 119 Seiten
    Language: Russian
    Note: In kyrillischer Schrift
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  • 87
    Call number: AWI G7-19-92931
    In: Glacier mass balance bulletin, No. 8
    Type of Medium: Series available for loan
    Pages: 100 Seiten , Illustrationen
    Series Statement: Glacier mass balance bulletin 8
    Language: English
    Note: CONTENTS 1 INTRODUCTION 2 BASIC INFORMATION 2.1 SUMMARY TABLE (NET BALANCE, ELA, ELA0, AAR, AAR0) 2.2 CUMULATIVE SPECIFIC NET BALANCE GRAPHS 3 DETAILED INFORMATION 3.1 GLACIAR BAHIA DEL DIABLO (ANTARCTICA) 3.1.1 Topography and observational network 3.1.2 Net balance maps 2001/02 and 2002/03 3.1.3 Net balance versus altitude (2001/02 and 2002/03) 3.1.4 Accumulation area ratio (AAR) and equilibrium line altitude (ELA) versus specific net balance for the whole observation period 3.2 MARTIAL ESTE (ARGENTINA) 3.2.1 Topography and observational network 3.2.2 Net balance maps 2001/02 and 2002/03 3.2.3 Net balance versus altitude (2001/02 and 2002/03) 3.2.4 Accumulation area ratio (AAR) and equilibrium line altitude (ELA) versus specific net balance for the whole observation period 3.3 VERNAGTFERNER (AUSTRIA) 3.3.1 Topography and observational network 3.3.2 Net balance maps (2001/02 and 2002/03) 3.3.3 Net balance versus altitude (2001/02 and 2002/03) 3.3.4 Accumulation area ratio (AAR) and equilibrium line altitude (ELA) versus specific net balance for the whole observation period 3.4 ZONGO (BOLIVIA) 3.4.1 Topography and observational network 3.4.2 Net balance maps (2001/02 and 2002/03) 3.4.3 Net balance versus altitude (2001/02 and 2002/03) 3.4.4 Accumulation area ratio (AAR) and equilibrium line altitude (ELA) versus specific net balance for the whole observation period 3.5 WHITE (CANADA) 3.5.1 Topography and observational network 3.5.2 Net balance maps (2001/02 and 2002/03) 3.5.3 Net balance versus altitude (2001/02 and 2002/03) 3.5.4 Accumulation area ratio (AAR) and equilibrium line altitude (ELA) versus specific net balance for the whole observation period 3.6 URUMQIHE S. NO. 1 (CHINA) 3.6.1 Topography and observational network 3.6.2 Net balance maps (2001/02 and 2002/03) 3.6.3 Net balance versus altitude (2001/02 and 2002/03) 3.6.4 Accumulation area ratio (AAR) and equilibrium line altitude (ELA) versus specific net balance for the whole observation period 3.7 FONTANA BIANCA (ITALY) 3.7.1 Topography and observational network 3.7.2 Net balance maps (2001/02 and 2002/03) 3.7.3 Net balance versus altitude (2001/02 and 2002/03) 3.7.4 Accumulation area ratio (AAR) and equilibrium line altitude (ELA) versus specific net balance for the whole observation period 3.8 TSENTRALNIY TUYUKSUYSKIY (KAZAKHSTAN) 3.8.1 Topography and observational network 3.8.2 Net balance map (2001/02 and 2002/03) 3.8.3 Net balance versus altitude (2001/02 and 2002/03) 3.8.4 Accumulation area ratio (AAR) and equilibrium line altitude (ELA) versus specific net balance for the whole observation period 3.9 NIGARDSBREEN (NORWAY) 3.9.1 Topography and observational network 3.9.2 Net balance maps (2001/02 and 2002/03) 3.9.3 Net balance versus altitude (2001/02 and 2002/03) 3.9.4 Accumulation area ratio (AAR) and equilibrium line altitude (ELA) versus specific net balance for the whole observation period 3.10 WALDEMARBREEN (NORWAY) 3.10.1 Topography and observational network 3.10.2 Net balance maps (2001/02 and 2002/03) 3.10.3 Net balance versus altitude (2001/02 and 2002/03) 3.10.4 Accumulation area ratio (AAR) and equilibrium line altitude (ELA) versus specific net balance for the whole observation period 3.11 DJANKUAT (RUSSIA) 3.11.1 Topography and observational network 3.11.2 Net balance maps (2001/02 and 2002/03) 3.11.3 Net balance versus altitude (2001/02 and 2002/03) 3.11.4 Accumulation area ratio (AAR) and equilibrium line altitude (ELA) versus specific net balance for the whole observation period 3.12 MALIY AKTRU (RUSSIA) 3.12.1 Topography and observational network 3.12.2 Net balance maps (2001/02 and 2002/03) 3.12.3 Net balance versus altitude (2001/02 and 2002/03) 3.12.4 Accumulation area ratio (AAR) and equilibrium line altitude (ELA) versus specific net balance for the whole observation period 3.13 STORGLACIÄREN (SWEDEN) 3.13.1 Topography and observational network 3.13.2 Net balance maps (2001/02 and 2002/03) 3.13.3 Net balance versus altitude (2001/02 and 2002/03) 3.13.4 Accumulation area ratio (AAR) and equilibrium line altitude (ELA) versus specific net balance for the whole observation period 4 FINAL REMARKS AND ACKNOWLEDGEMENTS 5 PRINCIPAL INVESTIGATORS AND NATIONAL CORRESPONDENTS 5.1 PRINCIPAL INVESTIGATORS 5.2 NATIONAL CORRESPONDENTS OF WGMS
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  • 88
    Monograph available for loan
    Monograph available for loan
    Cambridge : Cambridge University Press
    Call number: PIK C 111-20-93514
    Type of Medium: Monograph available for loan
    Pages: XIX, 768 Seiten , Diagramme
    Edition: 15th printing
    ISBN: 9780521894753 (pbk) , 9780521815468 (hbk)
    Language: English
    Branch Library: PIK Library
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  • 89
    Call number: MOP 45353 / MItte
    In: Developments in atmospheric science, 9
    Type of Medium: Monograph available for loan
    Pages: 327 Seiten , Illustrationen
    ISBN: 0444417486
    Series Statement: Developments in atmospheric science 9
    Language: English
    Note: CONTENTS Preface CONFERENCE SUMMARY / A. L. Fymat TEMPERATURE SOUNDING INVERSION METHODS AND THE OBSOLESCENCE OF DIFFERENTIAL EQUATIONS FOR SPECIFYING PHYSICAL OBSERVABLES / J. I. F. King SOME EXPERIMENTS ON THE EFFECT OF REMOTE SOUNDING TEMPERATURES UPON WEATHER FORECASTING / M. Halem, M. Ghil and R. Atlas NONLINEAR INVERSION: THEORY AND PRAXIS / J. I. F. King A NEW TREATMENT OF THE BOUNDARY TERM IN THE INVERSION OF THE RADIATIVE TRANSFER EQUATION / H. E. Fleming and D. S. Crosby EVALUATION OF ERRORS IN DERIVED CLEAR COLUMN RADIANCES / L. McMillin RECURSIVE FILTERING OF RADIANCE DATA FROM NIMBUS-E SATELLITE / I. A. Ismail DEPENDENCE OF THE TEMPERATURE DEVIATION OF THE OCEAN SURFACE AS MEASURED BY SATELLITE ON THE SIZE DISTRIBUTION OF AEROSOLS / T. Takashima THE DETERMINATION OF ATMOSPHERIC TEMPERATURE PROFILES FROM INFRARED INTERFEROMETER MEASUREMENTS ON BOARD OF METEOR-25 / V. A. Golovko and D. Spänkuch COMPOSITION SOUNDING GLOBAL TOTAL OZONE DETERMINATION FROM NIMBUS 4 BUV SPACECRAFT DATA / A. J. Fleig, R. S. Fraser, B. W. Guenther, D. F. Heath, E. Hilsenrath, L. V. Novak, V. G. Kaveeshwar, R. D. McPeters, C. L. Mateer and A. G. Miller INFORMATION CONTENT AND RESULTS OF NON-LINEAR INVERSION OF NIMBUS 6 LIMB RADIANCE INVERSION RADIOMETER DATA / J. C. Gille and P. L. Bailey AN APPROXIMATE METHOD FOR NONLINEAR INVERSION OF LIMB RADIANCE OBSERVATIONS / P. L. Bailey and J. C. Gille A NONLINEAR TECHNIQUE FOR INVERTING LIMB ABSORPTION PROFILES / J. D. Mill and S. R. Drayson SENSITIVITY OF THE INVERSION OF LIMB RADIANCE MEASUREMENTS IN THE 6.3μm WATER VAPOR BAND / H. Fischer AN ANALYSIS OF NIMBUS-V THIR 6-7 μm OBSERVATIONS OVER THE MEDITERRANEAN SEA / M. Roulleau MICROWAVE GROUND-BASED DETERMINATION OF ATMOSPHERIC TOTAL WATER CONTENT / G. G. Shchukin and L. P. Bobylev A SOLAR HETERODYNE RADIOMETER FOR THE DETERMINATION OF THE ALTITUDINAL PROFILES OF ATMOSPHERIC GASES / V. I. Astakhov, N. V. Vanin, V. V. Galaktionov, V. M. Dorokhov, V. M. Zakharovand V. U. Khattatov PASSIVE REMOTE SENSING IN THE PRESENCE OF MULTIPLE SCATTERING: A NUMERICAL INVERSION METHOD / B. R. Barkstrom PARTICULATE SOUNDING RECONSTRUCTING THE SIZE DISTRIBUTION OF SPHERICAL PARTICLES FROM ANGULAR FORWARD SCATTERING DATA / A. L. Fymat and K. D. Mease COMPLEX REFRACTIVE INDEX OF ATMOSPHERIC AEROSOLS: A SIZE DISTRIBUTION INDEPENDENT RETRIEVAL APPROACH USING MULTISPECTRAL TRANSMISSION RATIOS / A. L. Fymat and K. D. Mease THE METHOD OF MULTIFREQUENCY LASER SOUNDING OF ATMOSPHERIC AEROSOL MICROSTRUCTURE / V. E. Zuev and I. E. Naats LASER SOUNDING OF THE ATMOSPHERE USING AEROSOL SCATTERING / V. E. Zuev STRATOSPHERIC AEROSOL LAYERS MONITORED BY LIDAR / R. Reiter, H. Jaeger, W. Carnuth and M. Littfass LIDAR DETECTION OF ATMOSPHERIC CONTAMINANTS BY RAMAN SCATTERING AND FLUORESCENCE SPECTRA / V. M. Zakharov and V. A. Torgovichev REMOTE SENSING OF CLOUD PROPERTIES FROM NIMBUS 5 / D. J. McCleese THE ATMOSPHERIC BLURRING EFFECT OF REMOTELY SENSED EARTH IMAGERY / S. Ueno, Y. Haba, Y. Kawata, T. Kusaka and Y. Terashita Author Index Subject Index
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  • 90
    Monograph available for loan
    Monograph available for loan
    Garmisch-Partenkirchen : Physikalisch-Bioklimatische Forschungsstelle der Fraunhofer-Gesellschaft zur Förderung der angewandten Forschung
    Call number: MOP 40082 / Mitte
    Type of Medium: Monograph available for loan
    Pages: ca. 100 Seiten
    Series Statement: AEC Document Number NYO - 3425 - 10
    Language: English
    Location: MOP - must be ordered
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  • 91
    Monograph available for loan
    Monograph available for loan
    Wellington : New Zealand Meteorological Service
    Call number: MOP 44877 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 127 Seiten
    Language: English
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  • 92
    Call number: MOP 40801 / Mitte
    Type of Medium: Monograph available for loan
    Pages: II, 170 Seiten , Illustrationen
    Language: English
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  • 93
    Call number: MOP 44705 / Mitte
    Type of Medium: Monograph available for loan
    Pages: iii, 78 Seiten , 24 cm
    Language: English
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  • 94
    Monograph available for loan
    Monograph available for loan
    Oak Ridge, Tenn. : U.S. Department of Energy
    Call number: MOP 44436 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 15, 3, 5 Seiten
    Language: English
    Note: The field experiments were continued to estimate convective storm particulate scavenging efficiency in proximity to the St. Louis, Missouri urban-industrial complex. Complementary studies of the urban aerosol characterization, source strength, and removal processes were also studied. The 1975 field effort shifted emphasis from the immediate St. Louis area to the Alton-Wood River industrial complex. Along with the change in size and configuration of the network, there were increases in the numbers of most types of samplers. The new network yielded the following types of samples for analysis and interpretation: 1065 total rain samples from 85 sites; 68 sequential rainwater samples from 2 locations; 272 wet/dry samples from 7 locations; 216 air filter samples from 7 locations; 36 air filter samples from aircraft; and raindrop spectrometer data from 11 sites for the period 17 June-18 August. The analysis procedures require that all water samples undergo filtering for separate analyses of soluble and insoluble fractions of the elemental concentrations. This data collection effort provided a record number of samples for chemical analysis. Approximately 4000 pibals and over 370 radiosondes were released in the operational period, providing wind and thermodynamic data on 33 days. Aircraft missions were flown on 24 days, with one air tracer release of cesium on 19 July 1975. The status of the analysis of all types of data is described.
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  • 95
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-79/14
    In: CRREL Report, 79-14
    Description / Table of Contents: Solid ice growth rates due to the presence of frazil slush beneath the ice cover have been shown to be greater than the so-called static growth. The frazil slush reduces the effective heat of ice solidification and the frazil particles freeze into the interstitial water. Numerical schemes are presented which clearly show the effect of frazil ice porosity on ice cover growth rates and the numerical model using air temperature as the major input is compared with field data on ice thickness in a small river laden with frazil ice beneath its cover.
    Type of Medium: Series available for loan
    Pages: ii, 4 Seiten , Illustrationen
    Series Statement: CRREL Report 79-14
    Language: English
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  • 96
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-79/22
    In: CRREL Report, 79-22
    Description / Table of Contents: Field observations at 60 Sites located in the fast or near-fast ice along a 1200-km stretch of the north coast of Alaska between Bering Strait and Barter Island have shown that the great majority of the ice samples (95%) exhibit striking c-axis alignments within the horizontal plane. Such alignments were usually well developed by the time the ice was 50 cm thick and in some cases when the ice was 20 cm thick. In all cases the degree of preferred orientation increased with depth in the ice. Representative standard deviations around a mean direction in the horizontal plane are commonly less than ± 10° for samples collected near the bottom of the ice. The general patterns of the alignments support a correlation between the preferred c-axis direction and the current direction at the ice/water interface. A comparison between c-axis alignments and spot current measurements made at 42 locations shows that the most frequent current direction coincides with the mean c-axis direction. Such alignments are believed to be the result of geometric selection with the most favored orientation being that in which the current flows normal to the (0001) plates of ice that compose the dendritic sea ice/sea water interface.
    Type of Medium: Series available for loan
    Pages: v, 21 Seiten , Illustrationen
    Series Statement: CRREL Report 79-22
    Language: English
    Note: CONTENTS Abstract Preface Summary Introduction Techniques and sampling Observations Crystal alignments “Odd” sites Causes Conclusions Literature cited Appendix A: Current observations
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  • 97
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-79/19
    In: CRREL Report, 79-19
    Description / Table of Contents: The critical velocities of loads moving over floating ice plates have been determined by several authors. In all these analyses it was assumed that the in-plane force field in the ice cover is zero. However, due to constrained thermal strains, in-plane forces do occur in the field. The purpose of the present paper is to determine their effect upon the critical velocities of the moving loads. It is shown that a uniform compression force field reduces the critical velocity, whereas a tension force field has the opposite effect.
    Type of Medium: Series available for loan
    Pages: ii, 12 Seiten , Illustrationen
    Series Statement: CRREL Report 79-19
    Language: English
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  • 98
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-79/17
    In: CRREL Report, 79-17
    Description / Table of Contents: Six test roofs of two different slopes — 16.3° and 39.8°, and three different roof coverings — asphalt shingles, cedar shingles, and corrugated aluminum sheeting, were constructed at USACRREL, Hanover, New Hampshire, and were instrumented with thermocouples, heat flow meters, and calibrated gutters. Measurements were recorded for the winters of 1971-72 and 1972-73. The degree of icing and the chronological changes in the snow cover were recorded on 35-mm Kodachrome slides. It was found that eave icing is a sensitive function of the slope, roof covering composi­tion, and solar radiation. The effects of wind were not investigated; the data were screened to remove all informa­tion corresponding to windspeeds over 8 km/h. In order of increasing tendency to form ice dams on the eaves, the roofs were high-slope asphalt, high-slope cedar, high-slope aluminum, low-slope asphalt, low-slope cedar, and low- slope aluminum.
    Type of Medium: Series available for loan
    Pages: vi, 40 Seiten , Illustrationen
    Series Statement: CRREL Report 79-17
    Language: English
    Note: CONTENTS Abstract Preface Summary Introduction Experimental procedure Description of roofs Meteorological data Procedure Analysis General Temperature profiles Temperature rankings Heat flow Snow depths and meltwater volumes Degree of icing Results and conclusions General Temperature profiles of the roofs Comparative temperatures of roofs by section — rankings Heat flow and accumulation Snow depth, coverage, and meltwater Degree of icing Discussion of the icing problem Literature cited
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  • 99
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-79/16
    In: CRREL Report, 79-16
    Description / Table of Contents: In 1973 two membrane encapsulated soil layer (MESL) test sections were constructed into existing gravel surfaced roads at Elmendorf A FB and at Ft. Wainwright in Anchorage and Fairbanks, Alaska, respectively. The Elmendorf AFB MESL contains a silty clay soil and the Ft. Wainwright MESL contains a nonplastic silt. Both sections were constructed at soil moisture contents of approximately 2% to 3% below optimum for the CE-12 compactive effort. There were no indica­tions of soil moisture migration during freezing in either test section and after-thaw field California Bearing Ratio values were nearly equal to values measured before freezing. There is growing evidence of a slight increase in the overall soil moisture content in the Elmendorf AFB MESL possibly from moisture entering through the single layer polyethylene sidewalls which were not treated with asphalt emulsion. There is good evidence that the membrane of the same section might have received damage during a soil sampling operation which allowed localized moisture infiltration. A two-layer polyethylene membrane used in the Ft. Wainwright MESL is considered a more positive moisture barrier than the single sheet and a justifiable added cost for permanent construction.
    Type of Medium: Series available for loan
    Pages: v, 27 Seiten , Illustrationen
    Series Statement: CRREL Report 79-16
    Language: English
    Note: CONTENTS Preface Introduction Laboratory studies General Elmendorf AFB silty clay Fairbanks silt Field studies Elmendorf AFB MESL Ft. Wainwright MESL Traffic use Elmendorf AFB MESL Ft. Wainwright MESL Performance observations Elmendorf AFB MESL Ft. Wainwright MESL Conclusions Elmendorf AFB MESL Ft. Wainwright MESL General Literature cited Appendix A. The MESL concept Appendix B. Classification, compaction, freezing and CBR test results for Fairbanks silt
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  • 100
    Call number: MOP 44440 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 105 Seiten , Illustrationen , 27 cm
    Language: English
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