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  • 1
    Monograph available for loan
    Monograph available for loan
    Cambridge [u.a.] : Cambridge Univ. Press
    Call number: AWI A3-09-0026 ; M 14.0117
    Type of Medium: Monograph available for loan
    Pages: X, 270, [4] S. : Ill., graph. Darst., Kt.
    ISBN: 9780521847995
    Classification:
    Meteorology and Climatology
    Language: English
    Note: Contents: Preface. - Acknowledgements. - 1 The meteorology of monsoons. - 1.1 Introduction. - 1.2 Meteorology of the tropics. - 1.3 The Indian Ocean monsoon system. - 1.4 Theory of monsoons. - 2 Controls on the Asian monsoon over tectonic timescales. - 2.1 Introduction. - 2.2 The influence of Tibet. - 2.3 Oceanic controls on monsoon intensity. - 2.4 Summary. - 3 Monsoon evolution on tectonic timescales. - 3.1 Proxies for monsoon intensity. - 3.2 Monsoon reconstruction by oceanic upwelling. - 3.3 Continental climate records. - 3.4 Eolian dust records. - 3.5 Evolving flora of East Asia. - 3.6 History of Western Pacific Warm Pool and the Monsoon. - 3.7 Summary. - 4 Monsoon evolution on orbital timescales. - 4.1 Introduction. - 4.2 Orbital controls on monsoon strength. - 4.3 Eolian records in North-east Asia. - 4.4 Monsoon records from cave deposits. - 4.5 Monsoon variability recorded in ice caps. - 4.6 Monsoon variability recorded in lacustrine sediments. - 4.7 Salinity records in marine sediments. - 4.8 Pollen records in marine sediments. - 4.9 Paleoproductivity as an indicator of monsoon strength. - 4.10 The Early Holocene monsoon. - 4.11 Mid–Late Holocene monsoon. - 4.12 Summary. - 5 Erosional impact of the Asian monsoon. - 5.1 Monsoon and oceanic strontium. - 5.2 Reconstructing erosion records. - 5.3 Reconstructing exhumation. - 5.4 Estimating marine sediment budgets. - 5.5 Erosion in Indochina. - 5.6 Erosion in other regions. - 5.7 Monsoon rains in Oman. - 5.8 Changes in monsoon-driven erosion on orbital timescales. - 5.9 Tectonic impact of monsoon strengthening. - 5.10 Climatic control over Himalaya exhumation. - 5.11 Summary. - 6 The Late Holocene monsoon and human society. - 6.1 Introduction. - 6.2 Holocene climate change and the Fertile Crescent. - 6.3 Holocene climate change and the Indus Valley. - 6.4 Holocene climate change and early Chinese cultures. - 6.5 Monsoon developments since 1000 AD. - 6.6 Monsoon and religion. - 6.7 Impacts of future monsoon evolution. - 6.8 Summary. - References. - Further reading. - Index.
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  • 2
    Call number: M 05.0523 ; AWI G4-06-0009
    Type of Medium: Monograph available for loan
    Pages: XV, 381 Seiten , Illustrationen
    ISBN: 140203010X , 1-4020-3010-X
    Classification:
    Meteorology and Climatology
    Language: English
    Note: Contents Introduction 1. Isotope hydrology: a historical perspective / P.K. Aggarwal, K. Froehlich, R. Gonfiantini, J.R. Gat ISOTOPIC AND NUCLEAR METHODOLOGIES 2. Isotopic tracers for obtaining hydrologic parameters / H. Moser, W. Rauert 3. Hydrologic process studies using radionuclides produced by cosmic rays / D.Lal 4. Stable oxygen and hydrogen isotopes / L.L. Gourcy, M. Groening, P.K. Aggarwal 5. Tritium in the hydrologic cycle / R.L. Michel 6. Assessing sources and transformations of sulphate and nitrate in the hydrosphere using isotope techniques / B. Mayer 7. Rare gases / H.H. Loosli, R. Purtschert 8. U and Th series nuclides in natural waters / A. Kaufman 9. Optical isotope ratio measurements in hydrology / E.R.Th. Kerstel, H.A.J. Meijer HYDROLOGIC PROCESSES AND SYSTEMS 10. Some classical concepts of isotope hydrology / J.R. Gat 11. Istotopes in lake studies: a historical perspective / K.Froehlich, R. Gonfiantini, K. Rozanski 12. A review of isotope applications in catchment hydrology / T. Vitvar, P.K. Aggarwal, J.J. McDonnell 13. Contribution of isotopic and nuclear tracers to study of groundwaters / W.M. Edmunds 14. Dating of young groundwater / LN. Plummer 15. Dating of old groundwater - history, potential, limits and future / M.A. Geyh 16. Geotermal systems / Y.K. Kharaka, R.H. Mariner 17. Saline waters / J. Horita HYDROLOGIC PROCESSES AND SYSTEMS 18. Isotopes in atmospheric moisture / K. Rozanski 19. How much climatic information do water isotopes contain? / G. Hoffmann, M. Cuntz, J. Jouzel, M. Werner 20. Stable isotopes through the holocene as recorded in low-latitude, high-altitude ice cores / L.G. Thompson, M.E. Davis 21. Groundwater as an archive of climatic and environmental change / W.M. Edmunds 22. Isotopic palaeolimnology / F. Gasse Appendices A. List of seminal papers on isotope hydrology (the isotopes of hydrogen and oxygen) B. List of papers presented at the 1st IAEA Symposium on Isotope Hydrology (Tokyo, 1963) C. Excerpts from report of 1st IAEA Panel on the Application of Isotope Techniques in Hydrology
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  • 3
    Call number: AWI SCAR-AR-19-92813
    In: National report to SCAR on Antarctic scientific activities for the years ... and planned program for ... : progress report, 41
    Type of Medium: Series available for loan
    Pages: 25 Seiten
    Series Statement: National report to SCAR on Antarctic scientific activities for the years ... and planned program for ... : progress report 41
    Language: English
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  • 4
    Call number: AWI SCAR-IT-19-92821
    In: Italy antarctic research report to SCAR, June-1999
    Type of Medium: Series available for loan
    Pages: 15, V Seiten
    Language: English
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  • 5
    Call number: M 99.0204 ; AWI Bio-99-0155
    Description / Table of Contents: Diatoms are microscopic algae which are found in virtually every habitat where water is present. This volume is an up-to-date summary of the expanding field of their uses in environmental and earth sciences. Their abundance and wide distribution , and their well-preserved, glass-like walls make them ideal tools for a wide range of applications as both fossils and living organisms. Examples of their wide range of applications include use as environmental indicators, for oil exploration, and for forensic examination. The major emphasis is on their use in analyzing ecological problems such as climate change, acidification and eutrophication. The contributors to the volume are leading researchers in their fields and are brought together for the first time to give a timely synopsis of a dynamic and important area. This book should be read by environmental scientists, phycologists, limnologists, ecologists and paleoecologists, oceanographers, archeologists and forensic scientists.
    Type of Medium: Monograph available for loan
    Pages: xii, 469 Seiten , Illustrationen
    ISBN: 0521582814
    Classification:
    Paleontology
    Language: English
    Note: Contents Preface Part I Introduction 1 Applications and uses of diatoms: prologue / EUGENE F. STOERMER AND JOHN P. SMOL Part II Diatoms as indicators of environmental change in flowing waters and lakes 2 Assessing environmental conditions in rivers and streams with diatoms / R. JAN STEVENSON AND YANGDONG PAN 3 Diatoms as indicators of hydrologic and climatic change in saline lakes / SHERILYN C. FRITZ, BRIAN F. CUMMING, FRANQOISE GASSE, AND KATHLEEN R. LAIRD 4 Diatoms as mediators of biogeochemical silica depletion in the Laurentian Great Lakes / CLAIRE L. SCHELSKE 5 Diatoms as indicators of surface water acidity / RICHARD W. BATTARBEE, DONALD F. CHARLES, SUSHIL S. DIXIT, AND INGEMAR RENBERG 6 Diatoms as indicators of lake eutrophication / ROLAND I. HALL AND JOHN P. SMOL 7 Continental diatoms as indicators of long-term environmental change / J. PLATT BRADBURY 8 Diatoms as indicators of water level change in freshwater lakes / JULIE A. WOLIN AND HAMISH C. DUTHIE Part III Diatoms as indicators in extreme environments 9 Diatoms as indicators of environmental change near arctic and alpine treeline / ANDRE F. LOTTER, REINHARD PIENITZ, AND ROLAND SCHMIDT 10 Freshwater diatoms as indicators of environmental change in the High Arctic / MARIANNE S. V. DOUGLAS AND JOHN P. SMOL 11 Diatoms as indicators of enviromental change in antarctic freshwaters / SARAH A. SPAULDING AND DIANE M. MCKNIGHT 12 Diatoms of aerial habitats / JEFFREY R. JOHANSEN Part IV Diatoms as indicators in marine and estuarine environments 13 Diatoms as indicators of coastal paleoenvironments and relative sea-level change / LUC DENYS AND HEIN DE WOLF 14 Diatoms and environmental change in brackish waters / PAULI SNOEIJS 15 Applied diatom studies in estuaries and shallow coastal environments / MICHAEL J. SULLIVAN 16 Estuarine paleoenyironmental reconstructions using diatoms / SHERRI R. COOPER 17 Diatoms and marine paleoceanography / CONSTANCE SANCETTA PartV Other applications 18 Diatoms and archeology / STEVEN JUGGINS AND NIGEL CAMERON 19 Diatoms in oil and gas exploration / WILLIAM N. KREBS 20 Forensic science and diatoms / ANTHONY J. PEABODY 21 Toxic and harmful marine diatoms / GRETA A. FRYXELL AND MARIA C. VILLAC 22 Diatoms as markers of atmospheric transport / MARGARET A. HARPER 23 Diatomite / DAVID M. HARWOOD Part VI Conclusions 24 Epilogue: a view to the future / EUGENE F. STOERMER AND JOHN P. SMOL Glossary, and acronyms Index
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  • 6
    Call number: M 00.0109 ; PIK L 820-00-0099 ; AWI G1-00-0066
    Type of Medium: Monograph available for loan
    Pages: S. 113-404 , Ill.
    ISSN: 0800-0395
    Series Statement: Polar research 18,2
    Classification:
    Oceanology
    Language: English
    Location: Upper compact magazine
    Location: A 18 - must be ordered
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  • 7
    Monograph available for loan
    Monograph available for loan
    Oxford : Blackwell Science
    Call number: M 99.0434 ; AWI G1-00-0103
    Type of Medium: Monograph available for loan
    Pages: xvi, 592 Seiten
    ISBN: 0632049766
    Classification:
    Sedimentology
    Language: English
    Note: Contents Preface Acknowledgements Part 1: Introduction 1 Sedimentology in the earth sciences 1.1 Introduction: sedimentology and earth cycling 1.2 Erosional drainage basins and depositional sedimentary basins 1.3 Global sediment discharge and earth recycling: the rock cycle 1.4 Comparative interplanetary sedimentology 1.5 Practical sedimentology 1.6 A brief history of sedimentology Part 2: Origin and Types of Sediment Grains 2 Water-rock interactions: chemical and physical breakdown of catchment bedrock to soil and elastic sediment grains 2.1 Introduction 2.2 Natural waters as proton donors: pH, acid hydrolysis and limestone weathering 2.3 Metallic ions, electron transfer and Eh-pH diagrams 2.4 Behaviour of silicate minerals during chemical weathering: breakdown products and newly formed minerals 2.5 Acid rain and whole-catchment studies of chemical weathering 2.6 The rates and mechanisms of chemical weathering 2.7 A simple index of chemical alteration (CIA) 2.8 Vegetation, chemical weathering and the Precambrian controversy 2.9 Physical weathering 2.10 Soils as valves and filters for the natural landscape 3 The inorganic and organic precipitation of sediment: chemical, biochemical and biological 3.1 Marine and freshwater chemical composition: chemical fluxes to and from the oceans 3.2 The carbonate system in the oceans 3.3 Advances in understanding carbonate reaction kinetics and their significance 3.4 Pre-Recent and future CaCO3 reactions 3.5 Ooids 3.6 Carbonate grains from plants and animals 3.7 Carbonate muds, oozes and chalks 3.8 Other carbonate grains of biological origins 3.9 Organic productivity, sea-level and atmospheric controls of biogenic CaCO3 deposition rates 3.10 CaCO3 dissolution in the deep ocean and the oceanic CaCO3 compensation mechanism 3.11 Evaporite salts and their inorganic precipitation 3.12 Silica and pelagic plankton 3.13 Iron minerals and biomineralizers 3.14 Phosphates Part 3: User's Guide to Sedimentological Fluid Dynamics 4 Back to basics: fluid flow in general 4.1 Introduction 4.2 Material properties of fluids 4.3 Plastic behaviour 4.4 Dimensionless numbers 4.5 Reference frames for flows 4.6 The concepts of flow steadiness and uniformity 4. 7 Visualization of flow patterns 4.8 Ideal (potential) flow 4.9 Dynamics of fluid motion 4.10 Strategies for coping with the dynamic equations 5 Flow in the real world: laminar and turbulent behaviour 5.1 Osborne Reynolds and types of flow 5.2 The distribution of velocity in viscous flows: the boundary layer 5.3 Turbulent flow 5.4 The distribution of velocity in turbulent flows 5.5 Shear velocity, bed roughness, bed shear stress and flow power 5.6 The periodic coherent structures of turbulent shear flows 5.7 Shear flow instabilities, flow separation and secondary currents 6 Sediment grains in fluids: settling, transport and feedback 6.1 Introduction 6.2 Fall of grains through stationary fluids 6.3 Natural flows carrying particulate material are complex 6.4 Fluids as transporting machines 6.5 Initiation of particle motion 6.6 Initiation of motion by air flow 6.7 Paths of grain motion 6.8 Solid transmitted stresses 6.9 A dynamic sediment suspension theory 6.10 A warning: nonequilibrium effects may dominate natural sediment transport systems 6.11 Steady state, deposition or erosion: the sediment continuity equation Part 4: Sediment Transport and Sedimentary Structures 7 Bedforms and structures formed by unidirectional water flows over granular sediment 7.1 The 'trinity' of flow, transport and bedform 7.2 Current ripples 7.3 Lower-stage plane beds and cluster bedforms 7.4 Dunoids (bars, 2D dunes) 7.5 Dunes 7.6 Upper-stage plane beds 7.7 Antidunes, transverse ribs, chutes and pools, and related forms 7.8 Bedforms and sediment transport in poorly sorted sediment 7.9 Bedform phase diagrams 7.10 Bedform 'lag' effects 7.11 Bedform theory 7.12 Measurement of palaeocurrents and problems arising from trough-shaped sets of cross- stratification 8 Bedforms and structures formed by atmospheric flows 8.1 Introduction: some contrasts between air and water flows 8.2 Aeolian bedforms in general 8.3 Ballistic ripples and ridges 8.4 Dunes in general 8.5 Flow-transverse dunes 8.6 Flow-parallel dunes 8.7 Complex flow dunes 8.8 Vegetated parabolic dunes 9 Oscillatory water waves, combined flows and tides: their bedforms and structures 9.1 Introduction 9.2 Simple wave theory 9.3 Near-bed flow and bedforms 9.4 Combined flows, wave-current ripples and hummocky cross-stratification 9.5 Tidal flows 10 Bedforms and cohesive sediment transport and erosion 10.1 The 'special' case of clays and cohesive beds 10.2 Flow erosion of cohesive beds 10.3 Erosion by 'tools' 11 Sediment gravity flows and their deposits 11.1 Introduction and static grain aggregates 11.2 Static friction and stability of granular masses 11.3 Grain flow avalanches: from cross-bedding to megabreccias 11.4 Debris flows 11.5 Turbidity flows 12 Liquefaction, liquefaction structures and other 'soft' sediment deformation structures 12.1 Liquefaction 12.2 Sedimentary structures formed by and during liquefaction 12.3 Submarine landslides, growth faults and slumps 12.4 Desiccation and synaeresis shrinkage structures Part 5: External Controls on Sediment Derivation, Transport and Deposition 13 Climate and sedimentary processes 13.1 Introduction: climate as a fundamental variable in sedimentology 13.2 Solar radiation: ultimate fuel for the climate machine 13.3 Earth's reradiation and the 'greenhouse' concept 13.4 Radiation balance, heat transfer and simple climatic models 13.5 Climate and the water cycle, 13.6 General atmospheric circulations 13.7 Global climates: a summary 13.8 Climate, mountains and plateaux 13.9 Climate change 13.10 Sedimentological evidence for palaeoclimate 14 Changing sea level and sedimentary sequences 14.1 Introduction: sea level as datum 14.2 Sea-level changes 14.3 Rates and magnitude of sea-level change 14.4 Origins of global sea-level change: slow vs. fast eustasy 14.5 Sequence stratigraphy: layers, cheesewires and bandwagons 15 Tectonics, denudation rates and sediment yields 15.1 Basic geodynamics of uplift 15.2 Elevation and gradients 15.3 Catchment processes 15.4 Erosion and denudation 15.5 Large-scale studies of denudation rates 15.6 Basinal studies of denudation and sediment flux: the inverse approach 15.7 Sediment supply, vegetation and climate change: implications for basin stratigraphy 15.8 Marine strontium isotope ratio and continental erosion rates Part 6: Sediment Deposition, Environments and Facies in Continental Environments 16 Aeolian sediments in low-latitude deserts 16.1 Introduction 16.2 Physical processes and erg formation 16.3 Modern desert bedform associations and facies 16.4 Aeolian architecture 16.5 Climate change, erg abandonment and desert-lake-river sedimentary cycles 16.6 Ancient desert facies 17 Rivers 17.1 Introduction 17.2 Channel magnitude and gradient 17.3 Channel form 17.4 Channel sediment transport processes, bedforms and internal structures 17.5 The floodplain 17.6 Channel belts, alluvial ridges, combing and avulsion 17.7 River channel changes, adjustable variables and equilibrium 17.8 The many causes of channel incision-aggradation cycles 17.9 Fluvial architecture: scale, controls and time 17.10 Fluvial deposits in the geological record 18 Alluvial fans and fan deltas 18.1 Introduction 18.2 Controls on the size (area) of fans 18.3 Physical processes on alluvial fans 18.4 Debris-flow-dominated alluvial fans 18.5 Stream-flow-dominated alluvial fans 18.6 Recognition of ancient alluvial fans 18.7 Fan deltas 19 Lakes 19.1 Introduction 19.2 Lake stratification 19.3 Clastic input by rivers and the effect of turbidity currents 19.4 Wind-forced physical processes 19.5 Chemical processes and cycles 19.6 Biological processes and cycles 19.7 Modern temperate lakes and their continental sedimentary facies 19.8 Lakes in the East African rifts 19.9 Lake Baikal 19.10 Shallow saline lakes 19.11 The succes
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  • 8
    Call number: M 98.0275 ; ZSP-387-11
    In: International project on paleolimnology and late cenozoic climate
    Type of Medium: Monograph available for loan
    Pages: 160 S.
    Classification:
    Historical Geology
    Language: English
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  • 9
    Monograph available for loan
    Monograph available for loan
    Chichester : Wiley
    Call number: M 99.0142 ; AWI G5-00-0220
    Type of Medium: Monograph available for loan
    Pages: xii, 211 Seiten , Illustrationen
    Edition: Reprinted
    ISBN: 0471969133
    Series Statement: Coastal morphology and research
    Language: English
    Note: Contents Preface Acknowledgements Introduction Chapter One: Causes of sea-level change 1.1 Introduction 1.2 Changes in the quantity of oceanic water 1.3 Deformation of the shape of the oceanic basin 1.4 Variations of water density and dynamic changes affecting the water masses Chapter Two: Evidence of former sea levels 2.1 Rocky shores 2.2 Sedimentary shores 2.3 Archaeological and historical sea-level indicators 2.4 Dating a sea-level indicator 2.5 How sea-level curves are constructed Chapter Three: The ice age Earth 3.1 How the last glaciation developed 3.2 The sea-level positions during the last Ice age 3.3 Low-sea-level land bridges and landscapes 3.4 Last glaciation climate and hydrology 3.5 Last glaciation biomass and CO2 exchanges Chapter Four: Deglacial sea-level changes 4.1 Introduction 4.2 Modelling results 4.3 Regional case studies 4.4 A gradually rising or a fluctuating sea level? 4.5 The Younger Dryas sea-level change 4.6 Impacts of past sea-level rise on coastal systems 4.7 Palaeomonsoons Chapter Five: Relative sea-level changes in the late Holocene 5.1 Delta and coral reef development 5.2 Continuance of isostatic emergence / submergence processes 5.3 Seismo-tectonic displacements 5.4 Relative sea-level changes produced by aseismic tectonics 5.5 Transgression-regression sequences and sea-level changes 6 Present-day sea-level trends 6.1 Introduction 6.2 Instrumental measurements . 6.3 Explanation of current estimations of global sea-level rise 6.4 Coastal areas at risk from sea-level rise Conclusions References Author Index Geographical Index Subject Index
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  • 10
    Monograph available for loan
    Monograph available for loan
    Cambridge : Cambridge Univ. Press
    Call number: M 00.0005 ; AWI G4-98-0233
    Type of Medium: Monograph available for loan
    Pages: XXI, 341 S. : Ill, graph. Darst., Kt.
    Edition: 1. publ.
    ISBN: 0521664004
    Language: English
    Note: Contents: Preface. - List of Symbols. - 1 Groundwater flow. - 1.1 Darcy's law. - 1.1.1 The limits of Darcy's law. - 1.1.2 Driving forces for groundwater flow. - 1.2 Crustal permeability. - 1.2.1 Permeability versus porosity. - 1.2.2 Heterogeneity and anisotropy. - 1.2.3 Scale dependence. - 1.2.4 Depth dependence. - 1.2.5 Time dependence. - 1.2.6 Some limiting values. - 1.3 Conceptualizing groundwater systems. - 1.4 The continuum approach. - 1.5 The groundwater flow equation. - 1.5.1 Conservation of mass. - 1.5.2 The storage term. - 1.5.3 Various forms of the groundwater flow equation Problems. - 2 Solute transport. - 2.1 Governing equations. - 2.1.1 Molecular diffusion. - 2.1.2 Advection. - 2.1.3 Mechanical dispersion. - 2.1.4 Mass balance equation. - 2.1.5 Chemical reactions. - 2.1.6 Initial and boundary conditions. - 2.2 Numerical solution techniques. - 2.3 Density-driven flow. - 2.4 Multicomponent diffusion. - 2.5 Multicomponent reactive transport. - 2.5.1 Rate-based reactions. - 2.5.2 Surface reactions. - 2.5.3 Homogeneous reactions. - 2.5.4 Heterogeneous reactions. - 2.5.5 Solution algorithms Problems. - 3 Heat transport. - 3.1 Governing equations. - 3.1.1 Choice of dependent variables. - 3.1.2 Statements of mass and energy conservation. - 3.1.3 A form of Darcy's law for two-phase flow of compressible fluids. - 3.1.4 Conductive heat flux. - 3.1.5 One-dimensional forms of the governing equations. - 3.1.6 Extending the governing equations to three dimensions. - 3.1.7 Assumptions. - 3.1.8 Fluid properties. - 3.1.9 Numerical solution. - 3.2 Initial and boundary conditions. - 3.3 Temperature-based formulations. - 3.4 One-dimensional groundwater flow. - 3.4.1 Steady vertical flow. - 3.4.2 Flow in a confined aquifer or fault zone. - 3.5 Dimensionless numbers. - 3.5.1 Nusselt number. - 3.5.2 Peclet number. - 3.5.3 Rayleigh number. - 3.6 Buoyancy-driven flow. - 3.7 Heatpipes Problems. - 4Regional-scale flow and transport. - 4.1Sources and sinks of fluid. - 4.1.1 Geologic forcing. - 4.1.2 Anomalous fluid pressures. - 4.1.3 Hydraulic fracturing. - 4.1.4 The Gulf Coast. - 4.1.5 Accretionary prisms. - 4.2 Regional-scale solute transport. - 4.2.1 Groundwater age. - 4.2.2 Large-scale dispersion. - 4.2.3 Evolution of regional groundwater chemistry. - 4.3 Regional-scale heat transfer. - 4.3.1 The conductive regime in sedimentary basins. - 4.3.2 Thermal effects of groundwater flow in sedimentary basins. - 4.3.3 Some case studies of sedimentary basins. - 4.3.4 An example from volcanic terrane. - 4.3.5 The stress-heat flow paradox of the San Andreas fault Problems. - 5 Ore deposits. - 5.1Mississippi Valley-type deposits. - 5.1.1 Evidence for regional-scale brine migration. - 5.1.2 The salt problem. - 5.1.3 Controls on ore deposition. - 5.1.4 Driving forces for fluid flow. - 5.1.5 The Irish MVTs. - 5.2 Sediment-hosted uranium. - 5.2.1 Redox control of uranium solubility. - 5.2.2 Tabular uranium deposits. - 5.2.3 Unconformity-type uranium deposits. - 5.3 Supergene enrichment of porphyry copper. - 5.4 Colombian emeralds. - Problems. - 6 Hydrocarbons. - 6.1 Maturation. - 6.1.1 The oil window. - 6.1.2 Groundwater flow and the thermal regime. - 6.2 Migration. - 6.2.1 Capillary effects. - 6.2.2 Primary migration. - 6.2.3 Secondary migration. - 6.3 Entrapment. - 6.4 Governing equations for immiscible multiphase flow. - 6.5 Case studies. - 6.5.1 The Uinta basin. - 6.5.2 The Los Angeles basin. - Problems. - 7 Geothermal processes. - 7.1 Crustal heat flow. - 7.1.1 Measurement. - 7.1.2 Lateral and vertical variations. - 7.1.3 Perturbations due to groundwater flow. - 7.2 Magmatic-hydrothermal systems. - 7.2.1 Magmatic heat sources. - 7.2.2 Heat transfer from magma to groundwater. - 7.2.3 Fluid circulation near magma bodies. - 7.2.4 Permeabilities in near-magma environments. - 7.3 Fluid flow and heat transport near the critical point. - 7.3.1 One-dimensional pressure-enthalpy paths. - 7.3.2 Two-dimensional convection. - 7.4 Multiphase processes. - 7.4.1 Phase separation. - 7.4.2 Vapor-dominated zones. - 7.4.3 Pressure transmission. - 7.4.4 Boiling point-depth curves. - 7.5 Hotsprings. - 7.6 Geysers. - 7.7 Geothermal resources. - 7.8 Ore deposits. - 7.9 Subsea hydrothermal systems. - 7.9.1 Importance to the Earth's thermal budget. - 7.9.2 Influence on ocean chemistry. - 7.9.3 Quantitative description. - Problems. - 8 Earthquakes. - 8.1 Effective stress. - 8.2 Coulomb's law of failure. - 8.3 Induced seismicity. - 8.3.1 The Rocky Mountain arsenal. - 8.3.2 Rangely,Colorado. - 8.4 Fluid pressures at seismogenic depths. - 8.4.1 Hubbert and Rubey. - 8.4.2 Irwin and Barnes model for the San Andreas. - 8.4.3 Byerlee and Rice models for the San Andreas. - 8.5 Earthquake-induced hydrologic phenomena. - 8.5.1 Stream flow and springs. - 8.5.2 Well behavior. - 8.5.3 Geysering. - 8.6 Effect of earthquakes on crustal permeability. - 8.6.1 Analysis of the Loma Prietacase. - 8.6.2 State-of-stress and the orientation of conductive fractures. - Problems. - 9 Evaporites. - 9.1 Evaporite formation. - 9.1.1 The marine evaporite problem. - 9.1.2 Groundwater inflow. - 9.1.3 CaCl2 brines. - 9.1.4 Magnesium depletion. - 9.1.5 Continental evaporites. - 9.1.6 Groundwater outflow. - 9.2 Bedded evaporites. - 9.3 Saltdomes. - 9.3.1 Variable-density convection. - 9.3.2 Caprock formation. - Problems. - 10 Diagenesis and metamorphism. - 10.1 Reaction-Flow coupling. - 10.2 Diagenesis of siliciclastic sequences. - 10.2.1 Diagenesis in sedimentary basins. - 10.2.2 Silica cementation by thermal convection. - 10.3 Diagenesis of carbonate platforms. - 10.3.1 Dolomitization. - 10.3.2 Mixing-zone dissolution. - 10.4Local-scale diagenetic features. - 10.4.1 Mechanochemical coupling. - 10.4.2 Geochemical banding. - 10.5 Metamorphism. - 10.5.1 The evidence for voluminous fluid fluxes. - 10.5.2 The nature of permeability in metamorphic environments. - 10.5.3 Contact metamorphism at Skaergaard. - 10.5.4 Low-pressure metamorphic belts. - Problems. - References. - Index.
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  • 11
    Monograph available for loan
    Monograph available for loan
    Cambridge [u.a.] : Cambridge Univ. Press
    Call number: M 98.0486 ; AWI G6-98-0144
    Type of Medium: Monograph available for loan
    Pages: XII, 368 S.
    Edition: repr.
    ISBN: 0521364728
    Classification:
    Petrology, Petrography
    Language: English
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  • 12
    Monograph available for loan
    Monograph available for loan
    Berlin : Springer
    Call number: M 98.0363 ; AWI G8-96-0626
    Type of Medium: Monograph available for loan
    Pages: XV, 433 Seiten , Illustrationen
    ISBN: 3540593489
    Classification:
    Historical Geology
    Language: English
    Note: Contents I Review of Current Concepts 1 Introduction 1.1 Sequence Stratigraphy: A New Paradigm? 1.2 From Sloss to Vail 1.3 Problems and Research Trends: The Current Status 1.4 Stratigraphic Terminology 2 Methods for Studying Sequence Stratigraphy 2.1 Introduction 2.2 Erecting a Sequence Framework 2.2.1 The Importance of Unconformities 2.2.2 Facies Cycles 2.2.3 Stratigraphic Architecture: The Seismic Method 2.3 Methods for Assessing Regional and Global Changes in Sea Level, Other Than Seismic Stratigraphy 2.3.1 Areas and Volumes of Stratigraphic Units 2.3.2 Hypsometric Curves 2.3.3 Backstripping 2.3.4 Sea-Level Estimation from Paleoshorelines and Other Fixed Points 2.3.5 Documentation of Meter-Scale Cycles 2.4 Integrated Tectonic-Stratigraphic Analysis 3 The Four Basic Types of Stratigraphic Cycle 3.1 Introduction 3.2 The Supercontinent Cycle 3.3 Cycles with Episodicities of Tens of Millions of Years 3.4 Cycles with Million-Year Episodicities 3.5 Cycles with Episodicities of Less Than One Million Years 4 The Basic Sequence Model 4.1 Introduction 4.2 Terminology 4.3 Depositional Systems and Systems Tracts 4.4 Sequence Boundaries 4.5 Other Sequence Concepts 5 The Global Cycle Chart II The Stratigraphic Framework 6 Cycles with Episodicities of Tens to Hundreds of Millions of Years 6.1 Climate, Sedimentation, and Biogenesis 6.2 The Supercontinent Cycle 6.2.1 The Tectonic-Stratigraphic Model 6.2.2 The Phanerozoic Record 6.3 Cycles with Episodicities of Tens of Millions of Years 6.3.1 Intercontinental Correlations 6.3.2 Tectonostratigraphic Sequences 6.4 Main Conclusions 7 Cycles with Million-Year Episodicities 7.1 Extensional and Rifted Clastic Continental Margins 7.2 Foreland Basin of the North American Western Interior 7.3 Other Foreland Basins 7.4 Forearc Basins 7.5 Backarc Basins 7.6 Cyclothems and Mesothems 7;7 Carbonate Cycles of Platforms and Craton Margins 7.8 Evidence of Cyclicity in the Deep Oceans 7.9 Main Conclusions 8 Cycles with Episodicities of Less Than One Million Years 8.1 Introduction 8.2 Neogene Clastic Cycles of Continental Margins 8.3 Pre-Neogene Marine Carbonate and Clastic Cycles 8.4 Late Paleozoic Cyclothems 8.5 Lacustrine elastic and Chemical Rhythms 8.6 Clastic Cycles of Foreland Basins 8.7 Main Conclusions III Mechanisms 9 Long-Term Eustasy and Epeirogeny 9.1 Mantle Processes and Dynamic Topography 9.2 Supercontinent Cycles 9.3 Cycles with Episodicities of Tens of Millions of Years 9.3.1 Eustasy 9.3.2 Dynamic Topography and Epeirogeny 9.4 Main Conclusions 10 Milankovitch Processes 10.1 Introduction 10.2 The Nature of Milankovitch Processes 10.2.1 Components of Orbital Forcing 10.2.2 Basic Climatology 10.2.3 Variations with Time in Orbital Periodicities 10.2.4 Isostasy and Geoid Changes 10.2.5 The Nature of the Cyclostratigraphic Data Base 10.2.6 The Sensitivity of the Earth to Glaciation 10.2.7 Glacioeustasy in the Mesozoic? 10.2.8 Nonglacial Milankovitch Cyclicity 10.3 The Cenozoic Record 10.4 Late Paleozoic Cyclothems 10.5 The End-Ordovician Glaciation 10.6 Main Conclusions 11 Tectonic Mechanisms 11.1 Introduction 11.2 Rifting and Thermal Evolution of Divergent Plate Margins 11.2.1 Basic Geophysical Models and Their Implications for Sea-Level Change 11.2.2 Some Results from the Analysis of Modern Data Sets 11.3 Tectonism on Convergent Plate Margins and in Collision Zones 11.3.1 Magmatic Arcs and Subduction 11.3.2 Tectonism Versus Eustasy in Foreland Basins 11.3.2.1 The North American Western Interior Basin 11.3.2.2 The Appalachian Foreland Basin 11.3.2.3 Pyrenean and Himalayan Basins 11.3.3 Rates of Uplift and Subsidence 11.3.4 Discussion 11.4 Intraplate Stress 11.4.1 The Pattern of Global Stress 11.4.2 In-Plane Stress as a Control of Sequence Architecture 11.4.3 In-Plane Stress and Regional Histories of Sea-Level Change 11.5 Basement Control 11.6 Other Speculative Tectonic Hypotheses 11.7 Sediment Supply and the Importance of Big Rivers 11.8 Environmental Change 11.9 Main Conclusions IV Chronostratigraphy and Correlation: Why the Global Cycle Chart Should Be Abandoned 12 Time in Sequence Stratigraphy 12.1 Introduction 12.2 Hierarchies of Time and the Completeness of the Stratigraphic Record 12.3 Main Conclusions 13 Correlation, and the Potential for Error 13.1 Introduction 13.2 The New Paradigm of Geological Time? 13.3 The Dating and Correlation of Stratigraphic Events: Potential Sources of Uncertainty 13.3.1 Identification of Sequence Boundaries 13.3.2 Chronostratigraphic Meaning of Unconformities 13.3.3 Determination of the Biostratigraphic Framework 13.3.3.1 The Problem of Incomplete Biostratigraphic Recovery 13.3.3.2 Diachroneity of the Biostratigraphic Record 13.3.4 The Value of Quantitative Biostratigraphic Methods 13.3.5 Assessment of Relative Biostratigraphic Precision 13.3.6 Correlation of Biozones with the Global Stage Framework 13.3.7 Assignment of Absolute Ages 13.3.8 Implications for the Exxon Global Cycle Chart 13.4 Correlating Regional Sequence Frameworks with the Global Cycle Chart 13.4.1 Circular Reasoning from Regional Data 13.4.2 A Rigorous Test of the Global Cycle Chart 13.4.3 A Correlation Experiment 13.4.4 Discussion 13.5 Main Conclusions 14 Sea-Level Curves Compared 14.1 Introduction 14.2 The Exxon Curves: Revisions, Errors, and Uncertainties 14.3 Other Sea-Level Curves 14.3.1 Cretaceous Sea-Level Curves 14.3.2 Jurassic Sea-Level Curves 14.3.3 Why Does the Exxon Global Cycle Chart Contain So Many More Events Than Other Sea-Level Curves? 14.4 Main Conclusions V Approaches to a Modern Sequence-Stratigraphic Framework 15 Elaboration of the Basic Sequence Model 15.1 Introduction 15.2 Definitions 15.2.1 The Hierarchy of Units and Bounding Surfaces 15.2.2 Systems Tracts and Sequence Boundaries 15.3 The Sequence Stratigraphy of Clastic Depositional Systems 15.3.1 Pluvial Deposits and Their Relationship to Sea-Level Change 15.3.2 The Concept of the Bayline 15.3.3 Deltas, Beach-Barrier Systems, and Estuaries 15.3.4 Shelf Systems: Sand Shoals and Condensed Sections 15.3.5 Slope and Rise Systems 15.4 The Sequence Stratigraphy of Carbonate Depositional Systems 15.4.1 Platform Carbonates: Catch-Up Versus Keep-Up 15.4.2 Carbonate Slopes 15.4.3 Pelagic Carbonate Environments 15.5 Main Conclusions 16 Numerical and Graphical Modeling of Sequences 16.1 Introduction 16.2 Model Design 16.3 Selected Examples of Model Results 16.4 Main Conclusions VI Discussion and Conclusions 17 Implications for Petroleum Geology 17.1 Introduction 17.2 Integrated Tectonic-Stratigraphic Analysis 17.2.1 The Basis of the Methodology 17.2.2 The Development of an Allostratigraphic Framework 17.2.3 Choice of Sequence-Stratigraphic Models 17.2.4 The Search for Mechanisms 17.2.5 Reservoir Characterization 17.3 Controversies in Practical Sequence Analysis 17.3.1 The Case of the Tocito Sandstone, New Mexico 17.3.2 The Case of Gippsland Basin, Australia 17.3.3 Conclusions: A Modified Approach to Sequence Analysis for Practicing Petroleum Geologists and Geophysicists 17.4 Main Conclusions 18 Conclusions and Recommendations 18.1 Sequences in the Stratigraphic Record 18.1.1 Long-Term Stratigraphic Cycles 18.1.2 Cycles with Million-Year Episodicities 18.1.3 Cycles with Episodicities of Less Than One Million Years 18.2 Mechanisms 18.2.1 Long-Term Eustasy and Epeirogeny 18.2.2 Milankovitch Processes 18.2.3 Tectonic Mechanisms 18.3 Chronostratigraphy and Correlation 18.3.1 Concepts of Time 18.3.2 Correlation Problems, and the Basis of the Global Cycle Chart 18.3.3 Comparison of Sea-Level Curves 18.4 Modern Sequence Analysis 18.4.1 Elaboration of the Basic Sequence Model 18.4.2 Numerical and Graphical Modeling of Stratigraphic Sequences 18.5 Implications for Petroleum Geology 18.6 The Global-Eustasy Paradigm: Working Backwards from the Answer? 18.6.1 The Exxon Factor 18.6.2 Conclusions . 18.7 Recommendations References Author Index Subject Index
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  • 13
    Call number: M 04.0382 ; AWI G6-03-0011
    Type of Medium: Monograph available for loan
    Pages: XVIII, 378 Seiten , Illustrationen
    Edition: 2. Auflage
    ISBN: 0195087135
    Language: English
    Note: Contents: Preface to the Second Edition. - Preface to the First Edition. - 1. INTRODUCTION AND HISTORICAL BACKGROUND. - History. - The Discovery of X-Rays. - The Discovery of X-Ray Diffraction. - History of Clay Mineralogy. - The Importance of Clay Mineralogy. - Box 1.1 Clay Minerals as Catalysts. - The Literature of Clay Mineralogy. - Summary. - References. - 2. NATURE AND PRODUCTION OF X-RAYS. - Box 2.1 Other Methods. - Safety and Protection. - Box 2.2 Defining a Dose of Radiation. - The Nature or X-Rays. - Continuous or White Radiation. - Characteristic Radiation. - General Absorption of X-Rays. - Characteristic Absorption. - Equipment for Producing and Recording X-Rays. - Stabilizing the Voltage. - Generating X-Rays. - The Diffractometer. - Step-Scanning with Automated Diffractometers. - The Single-Crystal Monochromator. - The Detector. - Signal Processing Circuitry. - The Strip-Chart Recorder. - An Example of a Checklist for Operating XRD Equipment. - Summary. - References. - 3. X-RAY DIFFRACTION. - Scattering. - Interference. - Scattering from a Row of Atoms. - Scattering from a Three-Dimensional Array of Atoms. - Bragg's Law. - Box 3.1 Diffraction and Reflection. - The Arithmetic of Scattering. - The Summation of Scattering Amplitudes. - The Structure Factor F. - Information from Intensity. - The Reciprocal Lattice. - Real versus Idealized Peaks on XRD Tracings. - The Interference Function F: Diffraction from a Crystal. - Whose Unit Cell Has a Unitary Scattering Factor. - The Lorentz-Polarization Factors. - Putting It All Together—Building an 001 Diffraction Pattern. - Exercise: Calculation of the Intensity from d(001) for Illite. - Points to Remember. - References. - 4. STRUCTURE AND PROPERTIES: GENERAL TREATMENT. - General Structural Features. - Tetrahedral Sheets. - Octahedral Sheets. - Dioctahedral and Trioctahedral. - Joining the Sheets. - Stacking the Layers. - Properties. - Total Charge, Layer or Permanent Charge, and Variable Charge. - Electric Double Layer. - Exchangeable Ions or Cation-Exchange Capacity. - Interaction of Water with Clay Mineral Surfaces. - Interaction with Organic Compounds. - Classification. - Box 4.1 Nomenclature. - References. - 5. STRUCTURE, NOMENCLATURE, AND OCCURRENCES OF CLAY MINERALS. - The Individual Clay Minerals. - The 1:1 Layer Type. - Serpentine minerals. - Berthierine. - Odinite. - Kaolin minerals. - Box 5.1 Uses of Kaolinite. - Allophane and imogolite. - The 2:1 Layer Type, x = 0. - The 2:1 Layer Type, x ~ 1. - The trioctahedral subgroup. - The dioctahedral subgroup. - The 2:1 Layer Types with x 〈 1. - Illite. - Glauconite. - Smectite. - Box 5.2 Alteration of Ash-Fall Layers. - Vermiculite. - Chlorite. - Mixed-Layered Clay Minerals. - Mixed-layering, interlayering, and interstratification. - Illite/smectite (I/S). - Box 5.3 Reichweite or Ordering. - Models for smectite-to-illite transition. - MacEwan crystallite model. - Fundamental particle model. - Two-solid-solution model. - Chlorite/smectite (C/S). - Serpentine/chlorite. - Kaolinite/expandables (K/E). - Sepiolite and Palygorskite. - The Origin of Clay Minerals. - Summary. - Exercise: Calculating Structural Formulas. - Exercise: Making Structural Models of Layer Silicates. - References. - 6. SAMPLE PREPARATION TECHNIQUES FOR CLAY MINERALS. - Evaluating the Sample. - Disaggregating the Rock. - Separating Clay Minerals from Clastic Rocks. - Separating Clay Minerals from Carbonate Rocks. - Separating Clay Minerals from Sulfate Rocks. - Separating Clay Minerals from Unconsolidated Materials. - Box 6.1 Glacial Deposits, North American Interior. - Chemical Pretreatments. - Removal of Iron Oxides. - Removal of Organic Materials. - Saturating the Clay Minerals with Different Cations. - Particle-Size Separation. - Preparing the Oriented Clay Mineral Aggregates. - The Glass Slide Method. - The Smear Mount Method. - The Millipore® Filter Transfer Method. - The Centrifuged Porous Plate Method. - Dealing with Curlers or Peelers. - Making the Random Powder Mount. - Everyday random powder packs. - Freeze-dried random powder packs. - Ethylene Glycol Solvation. - Final Note. - References. - IDENTIFICATION OF CLAY MINERALS AND ASSOCIATED MINERALS. - Clay Mineral Identification—General Principles. - Illite and Glauconite. - Chlorite and Kaolinite. - Vermiculite. - Smectite. - Sepiolite, Palygorskite, and Halloysite. - 060 Reflections. - The Use of hkl Reflections for the Determination of Polytypes. - Chlorite Polytypes. - The Kaolin Polytypes. - The Micas, Illite, and Glauconite. - Nonclay Minerals. - Silica Minerals. - Feldspar. - Zeolites. - Carbonates. - Apatite, Pyrite, and Jarosite. - Gypsum, Anhydrite, Celestite, and Barite. - Lepidocrocite, Goethite, Gibbsite, and Anatase. - Summary. - References. - 8. IDENTIFICATION OF MIXED-LAYERED CLAY MINERALS. - Méring's Principles and Mixed-Layered Nomenclature. - The Q Rule, a Broadening Descriptor. - Mixed-Layered Clay Minerals. - Illite/Smectite. - Chlorite/Smectite and Chlorite/Vermiculite. - Kaolinite/Smectite. - Serpentine/Chlorite. - Mica/Vermiculite. - Summary. - References. - 9. QUANTITATIVE ANALYSIS. - Required Sample Characteristics. - Sample Length. - Sample Thickness. - Sample Position. - Homogeneity of the Sample. - Equations for Quantitative Analysis. - Basic Quantitative Diffraction Equation. - Derivation of a Working Form of the Equation for Analysis. - The Method of the Orienting Internal Standard. - Mineral Reference Intensities. - General Comments. - Calculated Mineral Reference Intensities. - Practical Examples of the Application of Reference. - Intensities. - Measurement of Peak Intensity. - Comments and Summary. - References. - 10. DISORDER IN SMECTITE, ILLITE/SMECTITE, AND ILLITE. - Small Crystals in Reciprocal Space. - Turbostratic Disorder. - Theory. - Smectite. - Illite/Smectite. - Rotational Disorder in Illite and Illite/Smectite. - Cis-Vacant Elite and Interstratified Cis- and Trans-Vacant. - Illite/Smectite. - Conclusions. - References. - APPENDIX: MODELING ONE-DIMENSIONAL X-RAY PATTERNS. - The Input Variables. - Simulating the Instrument. - Describing the Clay Mineral. - Theory. - Structures of the Component Layers. - Advanced Techniques. - Pure Minerals. - Compositional Superstructures. - Layer Types Not Specifically Included. - Atom Types Not Incorporated in the Model. - Defect Broadening. - References. - INDEX.
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  • 14
    Monograph available for loan
    Monograph available for loan
    Oxford [u.a.] : Blackwell Science
    Call number: M 98.0416 ; AWI G1-00-0131
    Type of Medium: Monograph available for loan
    Pages: xi, 404 S.
    ISBN: 0632035072
    Classification:
    A.3.1.
    Language: English
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  • 15
    Monograph available for loan
    Monograph available for loan
    Königstein : Koeltz Scientific Books
    Associated volumes
    Call number: M 97.0424 ; AWI Bio-99-0086
    In: Iconographia diatomologica
    Type of Medium: Monograph available for loan
    Pages: 390 S. : zahlr. Ill.
    ISBN: 3874293866
    Classification:
    Paleontology
    Language: English
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  • 16
    Monograph available for loan
    Monograph available for loan
    Cambridge : Cambridge Univ. Press
    Associated volumes
    Call number: M 97.0113 ; AWI S1-98-0212
    In: Cambridge monographs on applied and computational mathematics
    Type of Medium: Monograph available for loan
    Pages: xxii, 685 S.
    ISBN: 0521496721
    Series Statement: Cambridge monographs on applied and computational mathematics 2
    Classification:
    C.1.9.
    Language: English
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  • 17
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-95/14
    In: CRREL Report, 95-14
    Description / Table of Contents: Current protocols for decontaminating devices used to sample groundwater for organic contaminants are re­viewed. Most of the methods given by regulatory agencies provide little scientific evidence that justify the recommended protocols. In addition, only a few studies that actually compared various decontamination proto­cols could be found in the open literature, and those studies were limited in their scope. Various approaches for decontamination and criteria that are important in determining how effectively a surface could be decontami­nated are discussed.
    Type of Medium: Series available for loan
    Pages: iii, 15 Seiten , Illustrationen
    Series Statement: CRREL Report 95-14
    Language: English
    Note: CONTENTS Preface Introduction Sorption and desorption of organic contaminants Decontamination methods Aqueous cleaning methods Cleaning or rinsing with organic solvents Chemical neutralization methods Current protocols to decontaminate groundwater sampling devices Variations in methodology Special instructions for cleaning pumps Effectiveness of various decontamination methods Low-temperature considerations Conclusions Literature cited
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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-201-95/11
    In: CRREL Report, 95-11
    Description / Table of Contents: A pavement joint seal prevents the passage of liquids into the pavement base and the intrusion of solids into the joint. The primary mechanical requirements of a pavement seal are that it respond elastically or viscoelastically to any movement of the joint without failure and that it withstand indentation of hard objects like rocks. Because pavement joint movements and seal deformations can be large, elastomeric sealants are often used to form seals. Winter conditions are recognized as the most critical for a seal because of the possibility that failure stresses will be reached as the joint opens to a maximum and the material stiffens in response to the temperature reduction. This report reviews the specific problems and requirements that cold climates create for the performance of elastomeric seals. Emphasis is placed on the material response behavior that can lead to failure of a seal. In an attempt to clarity the mechanics of sealant and seal performance associated with low-temperature pavement applications and to address the issue of low-temperature stiffening That should be a dominant factor in the selection of a sealant, this report presents background information on the formulation and mechanical properties of elastomeric seal materials and the structural behavior of field-molded joint and crack seals.
    Type of Medium: Series available for loan
    Pages: iv, 20 Seiten , Illustrationen
    Series Statement: CRREL Report 95-11
    Language: English
    Note: CONTENTS Page Preface Introduction Elastomers and sealant formulations Mechanical behavior of sealants Phenomenological behavior of rubbers and elastomers Hyperelastic constitutive model Examples of sealant behavior Mechanical response of seals Basic structural geometry and loading configurations of seals Conventional performance testing for studying the load and deformation response of joint and crack seals Response of seals to joint movements Summary and recommendations Literature cited Abstract
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  • 19
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-95/7
    In: CRREL Report, 95-7
    Description / Table of Contents: Before vehicle mobility in snow can be reliably predicted, a complete understanding of motion resistance in snow is required. This report examines several aspects of wheeled vehicle motion resistance using results obtained with the CRREL instrumented vehicle. Resistances of leading and trailing tires are examined. Limited data are presented for undercarriage drag, and third and fourth wheel passes in the same rut are initially analyzed, as is how snow deforms around a wheel. For the CRREL instrumented vehicle, a trailing tire has a resistance coefficient of about 0.017 for snow depths less than about 22cm. For deeper snow, the disruption of the snowpack caused by a preceding wheel causes snow to fall into the rut, resulting in higher trailing tire coefficients. For larger vehicles, which in some cases have trailing tires carrying larger loads than preceding tires, the trailing tire coefficients are on the order of 0.048 and 0.025 for second and third trailing wheels respectively. Since there are no trailing tire data available for these larger vehicles, these values are based on nonlinear regression analysis, which includes a prediction of the leading tire resistance. The results and observations of this study are applied in a reanalysis of the towed resistance data obtained during the U.S. Army's Wheels vs. Tracks study. An improved algorithm is presented for predicting wheeled vehicle motion resistance caused by snow.
    Type of Medium: Series available for loan
    Pages: v, 39 Seiten , Illustrationen
    Series Statement: CRREL Report 95-7
    Language: English
    Note: CONTENTS Page Preface Nomenclature Introduction Experimental procedure Results and analysis Leading tire resistance Trailing tire resistance Deep snow Undercarriage drag Multiple passes Shallow snow resistance model Summary Literature cited Appendix A: Snow data Appendix B: Observations of snow deformation by a wheel Appendix C: Wheeled vehicle motion resistance data Abstract
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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-201-95/1
    In: CRREL Report, 95-1
    Description / Table of Contents: This report annotates the cold regions mobility prediction routines included in the CAMMS/ALBE mobility models. It further explains the development of the algorithms that are used in these models to describe the interaction of a vehicle with terrain that has been affected by cold weather. The following terrain conditions are discussed: undisturbed snow (shallow and deep); disturbed snow (moderately trafficked and hard packed); ice; and thawing soils. Several combinations of substrates are also considered. A stand-alone computer model is included.
    Type of Medium: Series available for loan
    Pages: v, 72 Seiten , Illustrationen
    Series Statement: CRREL Report 95-1
    Language: English
    Note: CONTENTS Page Preface Nomenclature Introduction Background Shallow snow Undisturbed snow on a firm substrate Undisturbed snow on a soft substrate Undisturbed snow over ice Disturbed, processed and packed snow Deep snow Ice Freezing or thawing ground conditions Bearing capacity of freezing ground Effect of thawing conditions on vehicle performance Speed made good Internal motion resistance Slopes Summary and recornmendations Literature cited Appendix A: Cold Regions Mobility Model CRM-1.F Appendix B: FORTRAN code using NRMM/CAMMS variables and format Appendix C: Traction coefficients on packed snow Appendix D: NRMM checkout data Abstract
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  • 21
    Call number: M 96.0550 ; AWI G6-96-0128
    Description / Table of Contents: A lake, as a body of water, is in continuous interaction with the rocks and soils in its drainage basin, the atmosphere, and surface and groundwaters. Human industrial and agricultural activities introduce new inputs and processes into lake systems. This volume is a selection of ten contributions dealing with diverse aspects of lake systems, including such subjects as the geological controls of lake basins and their histories, mixing and circulation patterns in lakes, gaseous exchange between the water and atmosphere, and human input to lakes through atmospheric precipitation and surficial runoff. This work was written with a dual goal in mind: to serve as a textbook and to provide professionals with in-depth expositions and discussions of the more important aspects of lake systems.
    Type of Medium: Monograph available for loan
    Pages: XVI, 334 Seiten , Illustrationen
    Edition: 2. ed.
    ISBN: 3540578919
    Classification:
    Sedimentology
    Language: English
    Note: Contents: 1 Global Distribution of Lakes / M. MEYBECK. - 1 Introduction. - 2 Background Material and Approaches to Global Lake Census. - 2.1 Data Used. - 2.2 Approaches to Global Lake Census. - 3 General Laws of Lake Distribution. - 3.1 Lake Density . - 3.2 Limnic Ratio. - 4 Distribution of Lakes of Tectonic Origin. - 5 Lakes of Glacial Origin. - 5.1 Lake Densities. - 5.2 Global Deglaciated Area. - 5.3 Total Number of Glacial Lakes. - 6 Fluvial Lakes. - 7 Global Distribution of Crater Lakes. - 8 Global Distribution of Saline Lakes. - 8.1 Coastal Lagoons. - 8.2 Salinized Lakes due to Evaporation. - 9 Global Lake Distribution. - 9.1 Extrapolation Approach. - 9.2 Lake Type Approach. - 9.3 Climatic Typology Approach. - 9.4 Lake Distribution in Endorheic Areas. - 9.5 Global Dissolved Salt Distribution in Lakes. - 10 Major Changes in Global Lake Distribution in the Geological Past. - 10.1 Lake Ages. - 10.2 Historical Changes. - 10.3 Postglacial Changes. - 11 Discussion and Conclusions. - References. - 2 Hydrological Processes and the Water Budget of Lakes / T. C. WINTER. - 1 Introduction. - 2 Hydrological System with Regard to Lakes. - 2.1 Interaction of Lakes with Atmospheric Water. - 2.2 Interaction of Lakes with Surface Water. - 2.3 Interaction of Lakes with Subsurface Water. - 2.4 Change in Lake Volume. - 3 Summary. - References. - 3 Hydrological and Thermal Response of Lakes to Climate: Description and Modeling / S. W. HOSTETLER. - 1 Introduction. - 2 Hydrological Response. - 3 The Hydrological Budget. - 4 Hydrological Models. - 5 Thermal Response. - 5.1 Energy Budget and Energy Budget Models. - 5.2 Models and Modeling. - 6 Use of Models to Link Lakes with Climate Change. - 7 Input Data Sets. - 8 Sample Applications. - 9 Summary. - References. - 4 Mixing Mechanisms in Lakes / D. M. IMBODEN and A. WÜEST. - 1 Transport and Mixing. - 2 Lakes as Physical Systems. - 3 Fluid Dynamics: Mathematical Description of Advection and Diffusion. - 3.1 Equations of Fluid Motion. - 3.2 Turbulence, Reynolds' Stress, and Eddy Diffusion. - 3.3 Vertical Momentum Equation. - 3.4 Nonlocal Diffusion and Transilient Mixing. - 4 Density and Stability of Water Column. - 4.1 Equation of State of Water. - 4.2 Potential Temperature and Local Vertical Stability. - 5 Energy Fluxes: Driving Forces Behind Transport and Mixing. - 5.1 Thermal Energy. - 5.2 Potential Energy. - 5.3 Kinetic Energy. - 5.4 Turbulent Kinetic Energy Balance in Stratified Water. - 5.5 Internal Turbulent Energy Fluxes: Turbulence Cascade. - 6 Mixing Processes in Lakes. - 6.1 Waves and Mixing. - 6.2 Mixing in the Surface Layer. - 6.3 Diapycnal Mixing. - 6.4 Boundary Mixing. - 6.5 Double Diffusion. - 6.6 Isopycnal Mixing. - 7 Mixing and Its Ecological Relevance. - 7.1 Time Scales of Mixing. - 7.2 Reactive Species and Patchiness. - 7.3 Mixing and Growth: The Search for an Ecological Steering Factor. - References. - 5 Stable Isotopes of Fresh and Saline Lakes / J. R. GAT. - 1 Introduction. - 1.1 Isotope Separatio During Evaporation. - 2 Small-Area Lakes. - 2.1 Seasonal and Annual Changes. - 2.2 Deep Freshwater Lakes. - 2.3 Transient Surface-Water Bodies. - 3 Interactive and Feedback Systems. - 3.1 Network of Surface-Water Bodies. - 3.2 Recycling of Reevaporated Moisture into the Atmosphere. - 3.3 Large Lakes. - 3.4 Large-Area Lakes with Restricted Circulation. - 4 Saline Lakes. - 4.1 Isotope Hydrology of Large Salt Lakes. - 4.2 Ephemeral Salt Lakes and Sabkhas. - 5 Isotopie Paleolimnology. - 6 Conclusions: From Lakes to Oceans. - References. - 6 Exchange of Chemicals Between the Atmosphere and Lakes / P. VLAHOS, D. MACKAY, S. J. EISENREICH, and KC. HORNBUCKLE. - 1 Introduction. - 2 Air-Water Partitioning Equilibria. - 3 Diffusion Between Water and Air. - 4 Volatilization and Absorption: Double-Resistance Approach. - 5 Factors Affecting Mass-Transfer Coefficients. - 6 Partitioning of Chemical to Paniculate Matter in Air and Water. - 6.1 Air. - 6.2 Water. - 7 Atmospheric Deposition Processes. - 7.1 Dry Deposition. - 7.2 Wet Deposition. - 8 Specimen Calculation. - 8.1 Step 1: Physicochemical Properties. - 8.2 Step 2: Mass-Transfer Coefficients. - 8.3 Step 3: Sorption in Air and Water. - 8.4 Step 4: Equilibrium Status. - 8.5 Step 5: Volatilization and Deposition Rates. - 9 Role of Air-Water Exchange in Lake Mass Balances. - 10 Case Studies. - 10.1 Mass Balance on Siskiwit Lake, Isle Royale. - 10.2 Mass Balance on Lake Superior. - 10.3 Air-Water Exchange in Green Bay, Lake Michigan. - 10.4 Air-Water Exchange in Lake Superior. - 11 Conclusions. - References. - 7 Atmospheric Depositions: Impact of Acids on Lakes / W. STUMM and J. SCHNOOR. - Abstract. - 1 Introduction: Anthropogenic Generation of Acidity. - 1.1 Genesis of Acid Precipitation. - 2 Acidity and Alkalinity: Neutralizing Capacities. - 2.1 Transfer of Acidity (or Alkalinity) from Pollution Through the Atmosphere to Ecosystems. - 3 Acidification of Aquatic and Terrestrial Ecosystems. - 3.1 Disturbance of H+ Balance from Temporal or Spatial Decoupling of the Production and Mineralization of the Biomass. - 3.2 In Situ H+ Ion Neutralization in Lakes. - 3.3 Krug and Frink Revisited. - 4 Brønsted Acids and Lewis Acids: Pollution by Heavy Metals, as Influenced by Acidity. - 4.1 Cycling of Metals. - 4.2 Pb in Soils. - 5 Impact of Acidity on Ecology in Watersheds. - 5.1 Soils. - 5.2 Lakes. - 5.3 Nitrogen Saturation of Forests. - 6 Critical Loads. - 6.1 Critical Load Maps. - 6.2 Models for Critical Load Evaluation. - 7 Case Studies. - 7.1 Chemical Weathering of Crystalline Rocks in the Catchment Area of Acidic Ticino Lakes, Switzerland. - 7.2 Watershed Manipulation Project at Bear Brooks, Maine. - 8 Summary. - References. - 8 Redox-Driven Cycling of Trace Elements in Lakes / J. HAMILTON-TAYLOR and W. DAVISON. - 1 Introduction. - 2 Major Biogeochemical Cycles and Pathways. - 3 Iron and Manganese. - 3.1 Transformations and Cycling. - 3.2 Iron and Manganese Compounds as Carrier Phases. - 4 Sediment-Water Interface. - 4.1 Diffusive Flux from Sediments. - 4.2 Evidence of Little or No Diffusive Efflux from Sediments. - 4.3 Transient Remobilization. - 4.4 Diffusive Flux into Sediments. - 5 Pathways Involving Redox Reactions Directly: Case Studies. - 5.1 Arsenic. - 5.2 Chromium. - 5.3 239,240Pu. - 5.4 Selenium 6 Pathways Involving Redox Reactions Indirectly: Case Studies. - 6.1 137Cs. - 6.2 Stable Pb, 210Pb, and 210Po. - 6.3 Zinc. - 7 Summary and Conclusions. - References. - 9 Comparative Geochemistry of Marine Saline Lakes / F. T. MACKENZIE, S. VINK, R. WOLLAST, and L. CHOU. - 1 Introduction. - 2 General Characteristics of Marine Saline Lakes. - 3 Comparative Sediment-Pore-Water Reactions. - 3.1 Mangrove Lake, Bermuda. - 3.2 Solar Lake, Sinai. - 4 Conclusions. - References. - 10 Organic Matter Accumulation Records in Lake Sediments / P. A. MEYERS and R. ISHIWATARI. - 1 Introduction. - 1.1 Significance of Organic Matter in Lake Sediments. - 1.2 Origins of Organic Matter to Lake Sediments. - 1.3 Alterations of Organic Matter During Deposition. - 1.4 Similarities and Differences Between Organic Matter in Sediments of Lakes and Oceans. - 1.5 Dating of Lake-Sediment Records. - 2 Indicators of Sources and Alterations of Total Organic Matter in Lake Sediments. - 2.1 Source Information Preserved in C/N Ratios of Sedimentary Organic Matter. - 2.2 Source Information from Carbon-Stable Isotopic Compositions. - 2.3 Source Information from Nitrogen-Stable Isotopic Compositions. - 3 Origin and Alterations of Humic Substances. - 4 Sources and Alterations of Lipid Biomarkers. - 4.1 Alteration of Lipids During Deposition. - 4.2 Changes in Sources vs Selective Diagenesis. - 4.3 Effects of Sediment Grain Size on Geolipid Compositions. - 4.4 Source Records of Alkanes in Lake Sediments. - 4.5 Preserv
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  • 22
    Monograph available for loan
    Monograph available for loan
    Washington : National Academy Press
    Call number: M 96.0505 ; AWI A3-96-0700 ; PIK N 456-96-0328
    Type of Medium: Monograph available for loan
    Pages: xiv, 630 S.
    ISBN: 0309054494
    Classification:
    Meteorology and Climatology
    Language: English
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  • 23
    Monograph available for loan
    Monograph available for loan
    Cambridge : Cambridge Univ. Press
    Call number: M 95.0452 ; AWI A17-96-0042
    Type of Medium: Monograph available for loan
    Pages: xv, 253 S.
    ISBN: 0521467829
    Classification:
    C.1.9.
    Language: English
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  • 24
    Call number: M 96.0159 ; M 96.0160 ; AWI G9-96-0124 ; AWI ad G9-96-0124
    In: Petermanns Geographische Mitteilungen : Ergänzungsheft, 289
    Description / Table of Contents: The monograph "The Schirmacher Oasis, Queen Maud Land, East Antarctica, and its surroundings" describes a region lying in a unique geographical position on the edge of East Antarctica. This area plays a key role for geological, paleoenvironmental and ecological studies for the understanding of regional and global changes. The book is the first complex multidisciplinary description of various geospheres within an Antarctic region. It presents a comprehensive summary of the results of two decades of German and three decades of international research efforts in this area, referring extensively also to sources never published before or which are difficult of access. Additionally, the monograph presents a very detailed photographic documentation and various map presentations of this area of East Antarctica, of its land and ice forms, its erosion, deposition and drainage features, its weather and climate as well as of its aurora features. The ozone soundings taken in the Schirmacher Oasis were the only year-round observations of vertical ozone distributions over Antarctica in 1985, the year of the "discovery'' of the "Antarctic Ozone Hole". For students and scientists interested in Antarctic regions and problems related to global change this book will serve as a source of references and as a guide for future expeditions as well.
    Type of Medium: Monograph available for loan
    Pages: 448 Seiten , Illustrationen , Annexes , 25 cm
    Edition: 1. Auflage
    ISBN: 3623007609
    Series Statement: Petermanns Geographische Mitteilungen : Ergänzungsheft 289
    Classification:
    A.0.3.
    Language: English
    Note: Contents Foreword Preface Editors' remarks The authors 1. The Schirmacher Oasis as a part of Queen Maud Land / (D. FRITZSCHE & P. BORMANN) 1.1. About Antarctic oases in general and the geographical setting of the Schirmacher Oasis in particular 1.2. History of discoveries and first investigations in Queen Maud Land 1.3. Systematic investigations of the Schirmacher Oasis and its surroundings since 1959 1.3.1. Contributions of the Norwegian Antarctic Expedition in 1958-59 1.3.2. Investigations of the Soviet Antarctic Expedition 1.3.2.1. The wintering stations Lasarev and Novolazarevskaya - their observatory registrations and field programmes 1.3.2.1.1. Logistical bases 1.3.2.1.2. Regular Soviet observatory programmes 1.3.2.1.3. Field studies in the surroundings of the stations 1.3.2.1.3.1. Glaciological studies at the Lazarev and Novolazarevskaya Ice Shelves 1.3.2.1.3.2. Geophysical investigations 1.3.2.1.3.3 Hydrological studies of lakes within the Schirmacher Oasis 1.3.2.1.3.4. Physico-geographical and geological studies of the Schirmacher Oasis 1.3.2.1.3.5. Biological investigations 1.3.2.2. Major geographic-geological surveys and geophysical and aerophotogrammetric mapping of the eastern mountain region of Queen Maud Land 1.3.3. Investigations of the Indian Antarctic Expedition 1.3.3.1. India 's interest in Antarctica 1.3.3.2. Indian Antarctic Expeditions and main results of investigations in the area of the Schirmacher Oasis and its surroundings 1.3.4. Contributions by German investigators 1.3.4.1. Origin of scientific interest in the Schirmacher Oasis and the establishment of the Georg Forster Station 1.3.4.2. Observational programmes at Georg Forster Station 1.3.4.3. Field observations within and in the surroundings of the Schirmacher Oasis 2. Geophysical investigations / (P. BORMANN, U. SCHÄFER, C. KOPSCH & S. WAGNER) 2.1. Permanent geomagnetic recordings 2.1.1. Recording environment, requirements and facilities 2.1.2. Recording of the total intensity F 2.1.3. Recording of the variation field 2.2. Geophysical field investigations 2.2.1. Review of former geophysical field investigations in Queen Maud Land 2.2.2. Geomagnetic field measurements by GDR teams 2.2.2.1. Measuring of variation differences 2.2.2.2. Geomagnetic mapping of the Schirmacher Oasis and profile measurements in its surroundings: data, results and geological implications 3. Geology / (H.-J. PAECH & W. STACKEBRANDT) 3.1. Geological setting and former investigations / (H.-J. PAECH) 3.2. Schirmacher Oasis 3.2.1. Lithostratigraphy / (W. STACKEBRANDT) 3.2.2. Tectonics / (W. STACKEBRANDT) 3.2.2.1. Planar structures 3.2.2.2. Linear structures 3.2.2.3. Fault structures and dykes 3.2.2.4. Structure and kinematics of the Lake 55 m fault zone by means of petromagnetic fabric analysis / (V. DAMM) 3.2.3. Petrography and petrochemistry 3.2.3.1. Metamorphics / (G. ANDREHS & P. BORMANN) 3.2.3.1.1. Methodology 3.2.3.1.2. Classification of rock types 3.2.3.1.3. Investigation of rock deformation 3.2.3.1.4. Mylonitization in fault zones 3.2.3.1.5. Characterization of metamorphism 3.2.3.1.6. Conclusions 3.2.3.2. Dykes / (U. WAND) 3.2.4. Photogeological indications / (E. BANKWITZ & P. BANKWITZ) 3.2.4.1. Rock series 3.2.4.2. Fault zones 3.3. The Nunatak region / (H.-U. WETZEL) 3.3.1. The Nunatak Metamorphic Complex 3.3.1.1. Nunatak Palets 3.3.1.2. Nunatak Aerodromnaya 3.3.1.3. Nunatak 870 m 3.3.1.4. Nunatak Südnachbar 3.3.1.5. Southern IGA Rocks 3.3.2. The Schirmacher Oasis Metamorphic Complex 3.3.2.1. Nunatak Basisniy 3.3.2.2. Nunatak Kit 3.4. Generalization of the geological history of the Schirmacher Oasis and Nunatak Metamorphic Complexes / (H.-J. PAECH, W. STACKEBRANDT & H.-U. WETZEL) 3.4.1. Lithostratigraphic succession 3.4.2. History of endogenic processes 3.5. Wohlthat Massif / (H. KÄMPF, W. STACKEBRANDT, K. HAHNE, H.-J. PAECH & V. S. LEPIN) 3.5.1. Introduction 3.5.2. Eliseev Anorthosite Complex 3.5.2.1. Introduction 3.5.2.2. Magmatic features 3.5.2.3. Metamorphic structures and textures 3.5.2.4. Chemical composition 3.5.2.5. Fracture tectonics and non-metamorphic dyke rocks 3.5.2.6. Ages and isotopie compositions 3.5.3. Rock assemblages covered by ice / (K. HAHNE, P. VOGLER & R. LEWIS) 3.5.4. Photogeological structures of the basement of the Wohlthat Massif / (P. BANKWITZ & E. BANKWITZ) 3.5.4.1. Structural features 3.5.4.2. Folding and schistosity 3.5.4.3. Fracture tectonics 3.5.4.4. Magmatic veins 3.6. Mineralizations in central Queen Maud Land / (H. KÄMPF) 3.6.1. Mineralization associated with metamorphics 3.6.2. Mineralization associated with anorthosite and gabbro 3.6.3. Mineralizations in granitoids and pegmatites 3.6.4. Hydrothermal mineralizations 3.7. Conclusions on the structure, composition and history of the Earth's crust in central Queen Maud Land / (P. BORMANN, H.-J. PAECH & W. STACKEBRANDT) 4. Geomorphology / (W. RICHTER & P. BORMANN) 4.1. Introduction 4.2. Overview of the macro-relief between the ice shelf barrier and the Wegener Inland Ice 4.3. Characterization of landformsin the Schirmacher Oasis 4.3.1. General characterization of landforms 4.3.2. Structural geomorphology 4.3.3. Surface forms due to glacial erosion and deposition 4.3.4. Surface water geomorphology 4.4. Weathering processes 4.4.1. Background and scope 4.4.2. Frost and insolation weathering 4.4.2.1. Measuring programme / (W. KRÜGER) 4.4.2.2. Results / (W. KRÜGER & P. BORMANN) 4.4.2.2.1. Data for bedrock 4.4.2.2.2. Temperature data for unconsolidated rock and soil 4.4.2.2.3. Soil moisture data for unconsolidated rock and soil 4.4.2.2.4. Discussion of results on rock and soil temperature as well as soil moisture measurements with regard to frost and insolation weathering in the Schirmacher Oasis / (W. KRÜGER & P. BORMANN) 4.4.3. Special forms of weathering 4.4.3.1. Chemical weathering and initial processes of pedogenesis 4.4.3.2. Salt efflorescences / (U. WAND) 4.4.3.3. Cavernous weathering / (J. BALKE & W. RICHTER) 4.4.3.4. Wind action (W. RICHTER) 5. Weather and climate / (W. RICHTER & P. BORMANN) 5.1. General climatic conditions 5.2. Local climatic conditions and variability of essential elements of the macro-climate in the Schirmacher Oasis 5.2.1. General peculiarities of oasis climate 5.2.2. Elements of macro-climate in the Schirmacher Oasis and their variability 5.2.2.1. Solar radiation 5.2.2.2. Air temperature 5.2.2.3. Wind direction and velocity 5.2.2.4. Precipitation 5.2.2.5. Humidity 5.2.2.6. Cloudiness 5.3. Isotope variations in atmospheric moisture and precipitation / (P. KOWSKI) 6. The continental ice cover in the surroundings of the Schirmacher Oasis / (W.-D. HERMICHEN) 6.1. Antarctic ice and world climate 6.2. Regional survey 6.3. Survey of former glaciological investigations 6.4. Present structure and dynamics of the regional ice cover 6.5. Isotope studies on the glacio-climatic history of the area 6.6. Some remarkable morphological minor forms of the snow and ice surface / (W. RICHTER) 6.7. Moraines around Lake Untersee - indicators of the Late-Quaternary regional glacial history / (W. STACKEBRANDT) 7. Satellite sea ice observations in the Atlantic sector of the Southern Ocean / (H. GERNANDT) 7.1. General introduction 7.2. Long-term variations of the sea ice edge / (H. GERNANDT, K. DRESCHER & L. THARANG) 7.2.1. Data evaluation 7.2.2. Mean seasonal variations 7.2.3. Anomalies of sea ice distribution 7.2.4. Interannual variations 7.2.5.Conclusions 7.3. The break-up of ice shelf areas / (H. GERNANDT, P. GLÖDE & J. SCHMECHEL) 7.3.1. Introduction 7.3.2. Satellite observations of the Filchner Ice Shelf's break-up 7.4. Typical sea ice distribution as a response to the circulation of the Southern Ocean / (H. GERNANDT & P. GLÖDE) 7.4.1. Data interpretation 7.4.2. Typical sea ice distributions 7.4.3. Discussion 7.4.4. Conclusions 8. Hydrology / (W. RICHTER & P. BORMANN) 8.1. General remarks 8.2. Fundamentals of physical geography 8.2.1. Hydrographic relevance of geol
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  • 25
    Monograph available for loan
    Monograph available for loan
    San Diego [u.a.] : Acad. Press
    Associated volumes
    Call number: 5/M 00.0182 ; M 02.0084 ; AWI S2-98-0072 ; PIK N 456-02-0374
    In: International geophysics series
    Type of Medium: Monograph available for loan
    Pages: XI, 467 S.
    ISBN: 0127519653
    Series Statement: International geophysics series 59
    Classification:
    Meteorology and Climatology
    Language: English
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  • 26
    Series available for loan
    Series available for loan
    Wilmette, Ill. : Snow, Ice and Permafrost Research Establishment
    Associated volumes
    Call number: ZSP-201-11
    In: SIPRE report, 11
    Description / Table of Contents: A commercial deep-freeze unit was modified to serve as a laboratory for growing single crystals, cutting specimens of a given orientation, testing these specimens in compressive creep, and studying thin-sections of the results on a universal stage. A method of growing single crystals of adequate size was developed by adapting the Bridgman method. Fortyone creep tests were made at temperatures ranging from -1° to -18°C. These gave an unexpected form of creep-curve in which the rate of strain continuously increases with time. The mechanism of deformation is dominantly basal translation—consistent with earlier work. The dependence on temperature and stress is expressed empirically.
    Type of Medium: Series available for loan
    Pages: 24 Seiten , Illustrationen
    Series Statement: SIPRE report 11
    Language: English
    Note: Contents Introduction Use of the deep-freeze as a cold laboratory Growing single crystals Creep tests Conclusions References cited
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  • 27
    Call number: ZSP-201-10
    In: SIPRE report, 10
    Type of Medium: Series available for loan
    Pages: 97 Seiten
    Series Statement: SIPRE report 10
    Language: English
    Note: Contents Foreword Synopsis Introduction Authority Purpose and scope SIPRE organization and activities Cryological problems and military end points Present state of knowledge General Introduction Terminology and classification Snow and ice Introduction Physical properties and geometry Density and water equivalent Water holding or storage capacity of snow Water transmission through snow Bound water Crystallography and metamorphism Porosity and permeability Mechanical properties Elasto-plastic properties Friction Strength Hardness Electromagnetic properties Dielectric constants Conductivity Magnetic properties Piezoelectric and pyroelectric effects Triboelectricity Freezing potential Thermodynamic properties Thermal properties Radiation Phase relations Engineering problems Snow and ice removal Snow compaction Snow draft control Trafficability Temporary structures Snow melt and runoff Maps Frozen ground and permafrost Introduction Frost action Theory of frost action Cyclic freezing and thawing Manifestations of frost actions Frost heave on freezing Reduction in load-carrying capacity on thawing Soil movements on slopes Ground properties affecting or affected by frost action Composition, grain size, and grain-size distribution Soil-moisture-movement properties Thermal properties Structure of unfrozen ground Structure of frozen ground Strength of frozen ground Freezing point Ground conditions affecting or affected by frost action Density Degree of saturation Interrelation of climate, position, vegetation, and soil Frost phenomena Climate Position Vegetation Engineering problems Excavation and replacement Subsurface drainage Base courses Insulation courses Surface icing and its control Trafficability Building foundations Maps Current related research Introduction Military cryological research in United States and Canada Non-military cryological research in the Western World Research needed Introduction Subjects for fundamental research Subjects for applied research
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