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  • 2025-2025  (9)
  • 1980-1984  (196,689)
  • 1975-1979  (183,559)
  • 1981  (196,679)
  • 1979  (183,559)
Collection
Language
Years
Year
  • 1
    Monograph available for loan
    Monograph available for loan
    Leipzig : Teubner
    Call number: MOP 45209 / Mitte ; MOP 45210
    Type of Medium: Monograph available for loan
    Pages: 460 S.
    Edition: 6. Aufl.
    Location: MOP - must be ordered
    Location: MOP - must be ordered
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    Branch Library: GFZ Library
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  • 2
    Call number: S 91.1183(84)
    In: Annalen
    Type of Medium: Series available for loan
    Pages: xiv, 56 S.
    Series Statement: Annalen / Koninklijk Museum voor Midden-Afrika : Reeks in 8°, Geologische wetenschappen nr. 84
    Location: Lower compact magazine
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  • 3
    Call number: MOP Per 747
    Type of Medium: Monograph available for loan
    Pages: 50 S.
    Series Statement: Arbeiten aus der Zentralanstalt für Meteorologie und Geodynamik 47
    Location: MOP - must be ordered
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  • 4
    Monograph available for loan
    Monograph available for loan
    Melbourne : Commonwealth Scientific and Industrial Research Organization
    Call number: MOP Per 301/B
    Type of Medium: Monograph available for loan
    Pages: 21 S. , Ill.
    ISBN: 0643003428
    Series Statement: Division of Entomology technical paper 16
    Language: English
    Location: MOP - must be ordered
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  • 5
    Monograph available for loan
    Monograph available for loan
    Leipzig : Fachbuchverl.
    Call number: MOP 45109
    Type of Medium: Monograph available for loan
    Pages: 80 S.
    Edition: 3., neubearb. Aufl.
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  • 6
    Monograph available for loan
    Monograph available for loan
    Garmisch-Partenkirchen : Institut für atmosphärische Umweltforschung der Fraunhofer- Gesellschaft
    Call number: MOP 44829 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 25 S. , graph. Darst.
    Language: English
    Location: MOP - must be ordered
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  • 7
    Monograph available for loan
    Monograph available for loan
    Jena : Gustav Fischer Verl.
    Call number: PIK N 456-16-90127
    Type of Medium: Monograph available for loan
    Pages: 160 S. , mit 65 Abb. u. 13 Tab.
    Edition: 1. Aufl.
    Series Statement: Umweltforschung
    Location: A 18 - must be ordered
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  • 8
    Monograph available for loan
    Monograph available for loan
    Leningrad : Gidrometeoizdat
    Call number: AWI A10-17-90636
    Description / Table of Contents: The book "Radiation in cloudy atmosphere" is devoted to description of the radiative peculiarities of the cloudy atmosphere which depends on the large-scale and microphysical properties of clouds. The data of micro- and macrophysical and optical characteristics of clouds are widely presented. The various methods for calculations of shortwave and longwave radiative fluxes in cloudy and clear atmosphere are described. There are shown some regularities of variations of albedo, absorbability and heat fluxes of clouds and cloudy atmosphere in dependence on their properties. The empirical radiation models of atmosphere in dependence on their properties. The empirical radiation models of atmosphere are presented. The results of measurements and calculations are compared. The book may be of interest for specialists in atmospheric physics, oceanology and some adjacent sciences. It has a reference character and so may be useful to scientists who take interest in radiation and cloudiness structure of the atmosphere. It may be used also by students, post-graduate students and lectureres of corresponding specialities.
    Type of Medium: Monograph available for loan
    Pages: 279 S.
    Language: Russian
    Note: In kyrill. Schr. , Zsfassung in engl. Sprache
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  • 9
    Call number: (DE-599)GBV03709842X
    Type of Medium: Monograph available for loan
    Language: German
    Location: MOP - must be ordered
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  • 10
    Monograph available for loan
    Monograph available for loan
    Moskva : Nauka
    Call number: 12256
    Type of Medium: Monograph available for loan
    Pages: 191 S
    Language: Russian
    Note: In kyrill. Schr.
    Location: Upper compact magazine
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  • 11
    Monograph available for loan
    Monograph available for loan
    Leipzig : VEB Deutscher Verlag für Grundstoffindustrie
    Call number: 8174
    Type of Medium: Monograph available for loan
    Pages: 246 Seiten , Illustrationen
    Edition: 1. Auflage
    ISBN: 3871446270
    Language: Undetermined
    Location: Upper compact magazine
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  • 12
    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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  • 13
    Monograph available for loan
    Monograph available for loan
    Bonn : Federal Republic of Germany, Press and Public Relations Department
    Call number: AWI P6-18-91970
    Type of Medium: Monograph available for loan
    Pages: iv, 169 Seiten
    Language: English
    Note: CONTENTS: Introduction. - International co-operation. - Intergovernmental co-operation. - Non-governmental co-operation. - I. Scientific Programme. - 1. Astronomy. - 2. Biological Sciences. - 2.1 The marine ecosystem and its living resources. - 2.1.1 Food resources, phytoplankton production and zooplankton. - 2.1.2 The role of the benthos. - 2.1.3 The role of micro-organisms. - 2.1.4 Distribution and incidence of seals in the pack-ice of the Weddell Sea. - 2.1.5 Distribution and life history of fishes. - 2.1.6 Large-scaie distribution and drift of krill. - 2.1.7 Composition and behaviour of krill shoals. - 2.1.8 Preservation and processing of krill. - 2.2 The adaptation of antarctic marine organisms to their environment. - 2.2.1 Experiments and marine studies on .the ecophysiology of krill. - 2.2.2 Temperature regulation and food requirements of warm-blooded antarctic animals. - 2.2.3 Growth, digestive system and food economy of antarctic fishes. - 2.2.4 Freezing resistance of sea animals. - 2.2.5 Taxonomy of antarctic marine organisms. - 2.3 Terrestrial biology in Antarctica. - 2.3.1 Temperature adjustments in the reproductive biology of antarctic birds. - 2.3.2 Biochemical bases of growth processes in poikilothermic organisms at very low temperatures. - 2.3.3 Nutritional biology of poikilothermic herbivora. - 2.3.4 Study of lichens, fungi and bacteria in Antarctica and on offshore islands. - 2.3.5 Photosynthesis and heterotrophic life cycle of plants at very low temperatures. - 2.4 Environmental protection in Antarctica. - 2.5 Human biology and medicine in polar regions. - 3. Geodesy, Cartography and Remote Sensing. - 3.1 Satellite geodesy. - 3.2 Doppler satellite positioning. - 3.3 Geodetic mapping of ice-free areas. - 3.4 Remote-sensing by satellite. - 4. Geology and Geophysics. - 4.1 Study of drift processes as a contribution to the geological history of Antarctica. - 4.1.1 Study of magnetic structures by means of aeromagnetic photography. - 4.1.2 Paleomagnetic studies of drift evolution. - 4.1.3 Micro-earthquakes as indicators of tectonic activity. - 4.1.4 Earth tides and natural oscillations of the earth. - 4.2 Studies of the structure of crust and mantle. - 4.2.1 Structure of the basement complex of the transantarctic mountain chain in the area east of the Filchner Ice Shelf. - 4.2.2 Structure of the basement of the Weddell Sea, the Filchner/Ronne Ice Shelf, and the peripheral area. - 4.2.3 Oldest and highly metamorphous rocks of the East Antarctic. - 4.3 Stratigraphy, tectonics and magmatism in the mobile areas. - 4.3.1 Mobile fringe areas of the East Antarctic. - 4.3.2 Paleozoic and mesozoic mountains(Beacon upper group) in the transantarctic mountains. - 4.3.3 Early paleozoic to cainozoic orogenes in the area around the Filchner/Ronne Ice Shelf. - 4.4 Study of exogenous processes under extremely cold conditions. - 4.4.1 Glacial geology and geomorphology. - 4.4.2 Weathering and detrital formation. - 4.5 Geoscientific marine research. - 5. Glaciology. - 5.1 Volume and dynamics of the Filchner/Ronne Ice Shelf. - 5.2 Determining the extent and thickness of the ice and its temporal variation in the Filchner/Ronne Ice Shelf sector and peripheral areas. - 5.3 Determining the composition and inner structure of the Filchner/Ronne Ice Shelf on the basis of geophysical surface measurements. - 5.4 Studies of the dynamics of the pack-ice in the Weddell Gyre. - 5.5 Physical characteristics of ocean ice. - 5.6 Glaciological drillings. - 5.7 Chemical composition and accumulation genesis of antarctic background aerosol; global transport of trace gases and aerosols. - 5.8 Study of the elastic and rheological characteristics of ice, its heat conductability and texture affected by deformation. - 6. Upper Atmosphere and Extraterrestrial Physics. - 6.1 Investigation of whistlers and VLF radio emissions (chorus, hiss, etc) at conjugated points. - 6.2 Study of terresterial magnetic pulsations at conjugated points. - 6.3 Study of atmospherics to obtain more precise data on worldwide thunderstorms. - 6.4 Measurements of the aero-electric field. - 6.5 Balloon-based study of the ionosphere in the light of Mg t resonance lines. - 6.6 Measurement of the vertical distribution of ozone, steam and aerosol up to an altitude of 30 km. - 6.7 Measurements of emission in the infrared 9.6 µ ozone band from the ground. - 6.8 Other projects which may be carried out simultaneously with the above or later. - 6.9 Proposed basic terrestrial magnetic equipment for the Antarctic Station. - 6.10 Meteorite search expedition. - 6.11 Study of micrometeorites and cosmic dust. - 7. Meteorology and Oceanography. - 7.1 Meteorology. - 7.1.1 Atmospheric boundary stratum. - 7.1.2 Study of stratospheric circulation. - 7.1.3 Measurement of trace gases over long periods. - 7.1.4 Other research projects. - 7.1.5 Weather service observations and consultations. - 7.1.6 Basic meteorological equipment for the Antarctic Station. - 7.2 Physical oceanography. - 7.2.1 Formation and extent of bottom water in the Atlantic sector of the circumantarctic ocean. - 7.2.2 Numeric simulation of the vertical flows of material, energy and impulses. - 7 2.3 Time scales of transportation in deep water with the aid of radioactive trace elements. - 7.2.4 Detection of heavy metals in the Antarctic Ocean. - 7.2.5 Fishery oceanography in circumantarctic waters. - 7.2.6 Other research projects. - 8. Engineering Sciences. - 8.1 Shipbuilding technology. - 8.1.1 Measuring and testing programme regarding the performance of vessels in ice and technical developments in the construction of ice-going vessels. - 8.2 Iceberg location and navigation. - 8.2.1 Iceberg location. - 8.2.2 Development of precision positioning systems (also for dynamic positioning) to ensure noninterference with signals transmitted through ice and water masses of different thicknesses. - 8.3 Construction techniques. - 8.4 Exploration techniques. - 8.5 Other topics. - The Antarctic Research Station. - The Polar Research and Supply Ship. - The Polar Research Institute. - Institutions contributing to the Programme.
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  • 14
    Call number: ZSP-SCAR-570-3
    In: National Antarctic Research Report to SCAR, No. 3
    Type of Medium: Series available for loan
    Pages: 16 Seiten
    ISSN: 0179-0072
    Series Statement: National Antarctic Research Report to SCAR 3
    Language: English
    Note: Contents: Membership of the National Committee on Antarctic Research in the Federal Republic of Germany. - Introduction. - Stations. - I. Record of Activities (past and ongoing), April 80-October 81. - II. Planned Activities, October 81-October 82. - References.
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  • 15
    Monograph available for loan
    Monograph available for loan
    [Erscheinungsort nicht ermittelbar] : [Verlag nicht ermittelbar]
    Call number: AWI P2-19-92186
    Type of Medium: Monograph available for loan
    Pages: 23 Seiten
    Language: English
    Location: AWI Reading room
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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-201-85/19
    In: CRREL Report, 85-19
    Description / Table of Contents: Ground-probing radar can be an effective tool for exploring the top 10 to 20 m of ground, especially in cold regions where the freezing of water decreases signal absorption. However, the large electrical variability of the surface, combined with the short wavelengths used, can often cause severe ground clutter that can mask a desired, deeper return. In this study a model facility was constructed consisting of a metallic reflector covered by sand. Troughs of saturated sand were emplaced at the surface to vary surface electrical properties and to act as a noise source to interfere with the bottom reflections. Antenna polarization and height, and signal stacking in both static (antennas stationary) and dynamic (antennas moving) modes were then investigated as methods for reducing the surface clutter. Polarization parallel to the profile direction (perpendicular to the troughs' axes) gave profiles superior to the perpendicular case because of the directional sensitivity of the antenna radiation. Dynamic stacking greatly improved the signal-to-noise ratio because noise sources were averaged as the antennas moved, while the desired reflector, buried at constant depth, was enhanced. Raising the antennas above the surface also reduced noise because the surface area over which reflections were integrated increased. All three noise reduction techniques could be effective in surveys for reflectors at nearly constant depth such as groundwater tables or ice/water interfaces if the lateral variation in undesired ground propertiesis sufficiently random.
    Type of Medium: Series available for loan
    Pages: iv, 23 Seiten , Illustrationen
    Series Statement: CRREL Report 85-19
    Language: English
    Note: CONTENTS Abstract Preface Introduction Objective and procedures Materials and methods Subsurface radar Model facility Results Isolated disturbances-surface and raised analog profiles Multiple disturbances Discussion and conclusions Literature cited
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  • 17
    Call number: MOP 45206 / Mitte
    In: Daily Global Analyses
    Type of Medium: Monograph available for loan
    Pages: 5, 368 Seiten , graphische Darstellungen
    Series Statement: Daily Global Analyses Part 1
    Language: English
    Location: MOP - must be ordered
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  • 18
    Call number: MOP 45206 / Mitte
    In: Daily Global Analyses
    Type of Medium: Monograph available for loan
    Pages: 6, 371 Seiten , graphische Darstellungen
    Series Statement: Daily Global Analyses Part 3
    Language: English
    Location: MOP - must be ordered
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  • 19
    Call number: MOP 45809/3 / Mitte
    In: Fortschritte in der hydrologischen und wasserwirtschaftlichen Forschung der DDR
    Type of Medium: Monograph available for loan
    Pages: 48 Seiten , graphische Darstellungen
    Series Statement: Fortschritte in der hydrologischen und wasserwirtschaftlichen Forschung der DDR 3
    Language: German
    Location: MOP - must be ordered
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  • 20
    Call number: MOP 45809/5 / Mitte
    In: Fortschritte in der hydrologischen und wasserwirtschaftlichen Forschung der DDR
    Type of Medium: Monograph available for loan
    Pages: 70 Seiten , graphische Darstellungen
    Series Statement: Fortschritte in der hydrologischen und wasserwirtschaftlichen Forschung der DDR 5
    Language: German
    Location: MOP - must be ordered
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  • 21
    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
    Location: MOP - must be ordered
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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-201-79/14
    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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  • 23
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-79/15
    In: CRREL Report, 79-15
    Description / Table of Contents: This report discusses the application of several modern geophysical techniques to groundwater exploration in areas in permafrost. These methods utilize the principles of magnetic induction and radiowave surface impedance in the 10- to 400-kHz band, the techniques of impulse and side-looking radar in the 50- to 10,000-MHz band, and also some optical techniques using imagery obtained from a satellite. Low frequency case studies demonstrate the use of the techniques for detecting free water under an ice cover in shallow, almost completely frozen lake basins, and thaw zones within lake beds, stream channels, and in permafrost in general. The radar studies demonstrate the use of these techniques for determining depth of free water and ice cover thickness on lakes and rivers
    Type of Medium: Series available for loan
    Pages: iv, 30 Seiten , Illustrationen
    Series Statement: CRREL Report 79-15
    Language: English
    Note: CONTENTS Abstract Preface Introduction Part I. Low frequency resistivity methods Resistivity of earth materials Theory and description of techniques Surface impedance technique Airborne radiowave technique Magnetic induction technique Case studies Location of thaw zones beneath lakes and rivers Location of permeable materials in unfrozen ground Delineating permafrost boundaries Part II. High frequency dielectric methods Dielectric properties of earth materials Theory and description of equIpment Profiling radar Imaging radar Case studies Radar profile of a river channel Impulse radar profile of a freshwater lake SLAR imagery of Arctic lakes Literature cited Appendix A: Satellite imagery for subsurface water exploration
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  • 24
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-79/22
    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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  • 25
    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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  • 26
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-79/21
    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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  • 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-201-79/20
    In: CRREL Report, 79-20
    Description / Table of Contents: A volumetric constitutive equation was developed to characterize the behavior of snow subjected to large compressive volumetric deformations. By treating the material as a suspension of air voids in a matrix material of polycrystalline ice, a rate-dependent volumetric constitutive law was formulated and found to accurately predict material response to pressure loads for a wide range of load rates. Comparison of the theory with shock wave data was not considered in this paper, although the constitutive law appears to be valid for such load situations. One application to oversnow mobility of tracked vehicles was made. In this case, power requirements due to snow compaction were calculated parametrically in terms of vehicle speed, track loading, and snow density.
    Type of Medium: Series available for loan
    Pages: v, 13 Seiten , Illustrationen
    Series Statement: CRREL Report 79-20
    Language: English
    Note: CONTENTS Abstract Preface Nomenclature Introduction Material representation of ice Development of the volumetric constitutive law for snow Fully elastic phase Elastic-plastic phase Fully plastic phase Simplified equation Comparison with experimental data Application to vehicle mobility problems Conclusions Literature cited
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  • 28
    Call number: MOP 45476 / Mitte
    Type of Medium: Monograph available for loan
    Pages: [400] Seiten , Illustrationen , 28 cm
    Language: English
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  • 29
    Call number: MOP 45321 / Mitte
    In: Antarctic research activities of the German Democratic Republic
    Type of Medium: Monograph available for loan
    Pages: 15 Seiten
    Series Statement: Antarctic research activities of the German Democratic Republic : report to SCAR No 2
    Language: English
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  • 30
    Monograph available for loan
    Monograph available for loan
    Leningrad : Gidrometeoizdat
    Call number: MOP 45344 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 222 Seiten , 1 Beilage
    Language: Russian
    Note: In kyrillischer Schrift
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  • 31
    Call number: MOP 45483 / Mitte
    Description / Table of Contents: The reality of subregional variability in tornado occurrence density as evidenced in the county to county variability in Missouri is examined. Reported tornadoes for the period from 1916 through 1975 were used. Demographic and geographic factors known to impact on tornado reporting efficiencies and accuracies are related to county tornado report densities by step-wise multiple linear regression techniques. The analysis suggests that over 75 percent of the county to county apparent variability in reported tornado densities in Missouri is explainable in terms of variability in population density, other related demographic variables and regional scale geographic factors.
    Type of Medium: Monograph available for loan
    Pages: xi, 86 Seiten , Illustrationen, Karten , 28 cm
    Language: English
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  • 32
    Call number: MOP 45287 / Mitte
    Type of Medium: Journal available for loan
    Pages: Seiten 87-222
    ISSN: 0001-513x , 0541-9425
    Series Statement: Acta Agronomica Academiae Scientiarum Hungaricae 30
    Language: English
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  • 33
    Call number: MOP 45809/1 / Mitte
    In: Fortschritte in der hydrologischen und wasserwirtschaftlichen Forschung der DDR
    Type of Medium: Monograph available for loan
    Pages: 86 Seiten , graphische Darstellungen
    Series Statement: Fortschritte in der hydrologischen und wasserwirtschaftlichen Forschung der DDR 1
    Language: German
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  • 34
    Call number: MOP 45809/2 / Mitte
    In: Fortschritte in der hydrologischen und wasserwirtschaftlichen Forschung der DDR
    Type of Medium: Monograph available for loan
    Pages: 70 Seiten , graphische Darstellungen
    Series Statement: Fortschritte in der hydrologischen und wasserwirtschaftlichen Forschung der DDR 2
    Language: German
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  • 35
    Call number: MOP 45809/4 / Mitte
    In: Fortschritte in der hydrologischen und wasserwirtschaftlichen Forschung der DDR
    Type of Medium: Monograph available for loan
    Pages: 74 Seiten , graphische Darstellungen
    Series Statement: Fortschritte in der hydrologischen und wasserwirtschaftlichen Forschung der DDR 4
    Language: German
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  • 36
    Monograph available for loan
    Monograph available for loan
    Leningrad : Gidrometeoizdat
    Call number: MOP 45558 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 231 Seiten , Illustrationen , 22 cm
    Language: Russian
    Note: In kyrillischer Schrift
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  • 37
    Monograph available for loan
    Monograph available for loan
    [Rockville, Md.] : U.S. Department of Commerce, National Oceanic and Atmospheric Administration, Office of Research and Development
    Call number: MOP 44980 / Mitte
    Type of Medium: Monograph available for loan
    Pages: ii, 73 Seiten , Illustrationen , 27 cm
    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-201-79/30
    In: CRREL Report, 79-30
    Description / Table of Contents: The ice suppression resulting from discharge of warm water into rivers during winter is analyzed with emphasis on two different cases. In Part 1 the case of a thermal effluent fully mixed across the flow section is analyzed to include the effects of unsteadiness in the effluent temperature and the meteorological variations. The location of the ice edge is determined either by a 0 C water temperature criterion or an equilibrium ice melting analysis. The choice of the applicable criterion emerges naturally from the analysis even though the location of the ice edge may be considerably different when a steady-state analysis is done. In Part 2 the case of a side discharge of heated effluent is analyzed, also in an unsteady manner, and the effects of transverse dispersion are included in the analysis. Comparisons are made in both Parts 1 and 2 to limited field data that are available.
    Type of Medium: Series available for loan
    Pages: iv, 23 Seiten , Illustrationen
    Series Statement: CRREL Report 79-30
    Language: English
    Note: CONTENTS Abstract Preface Part I. Unsteady suppression of river ice by fully mixed thermal effluents Introduction Governing equations Outline of analysis Location of ice edge Numerical simulation Uncertainties and Imitations Literature cited Part II. Effect of transverse mixing on ice suppression Introduction Analysis of dispersion and heat loss Analysis of ice thickening and melting Numerical simulation Example simulations Field comparison Uncertainties and limitations Literature Cited Appendix A: Computer program for unsteady fully mixed ice suppression Appendix B: Computer program for unsteady lateral mixing ice suppression
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  • 39
    Monograph available for loan
    Monograph available for loan
    [Genève] : Organisation Météorologiques Mondiale
    Call number: MOP 45533 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 107 Seiten , Illustrationen
    Language: French
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  • 40
    Monograph available for loan
    Monograph available for loan
    Stutgart : Wissenschaftliche Verlagsgesellschaft
    Call number: MOP 48074 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 56 Seiten , Illustrationen
    ISBN: 3804706118
    Language: German
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  • 41
    Monograph available for loan
    Monograph available for loan
    Washington, D.C. : Mineralogical Society of America
    Associated volumes
    Call number: 11/M 19.92807
    In: Reviews in mineralogy, 3
    Type of Medium: Monograph available for loan
    Pages: viii, L1-L88; R1-R24, Hg1-Hg100, EG1-EG72, SH1-SH17, Hg101-Hg300 , Illustrationen, Diagramme
    Edition: second printing
    ISBN: 0-939950-03-0
    Series Statement: Reviews in mineralogy 3
    Language: English
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  • 42
    Monograph available for loan
    Monograph available for loan
    Washington, D.C. : Mineralogical Society of America
    Associated volumes
    Call number: 11/M 19.92815
    In: Reviews in mineralogy, 1
    Type of Medium: Monograph available for loan
    Pages: vi, diverse Seitenangaben , Illustrationen, Diagramme
    Edition: fourth printing
    ISBN: 0-939950-01-4
    Series Statement: Reviews in mineralogy 1
    Language: English
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  • 43
    Monograph available for loan
    Monograph available for loan
    Geneva : World Meteorological Organization
    Call number: MOP 44781/1 / Mitte ; MOP 44781/2 / Mitte
    Description / Table of Contents: Content: Provisional Programme Introduction: Climate and society: lessons from recent events / Robert R. Kates Overview Paper 1: Climatic change and human strategy / E. K. Fedorov Overview Paper 2: Global ecology and man / Bert Bolin Overview Paper 3: Climatic variation and variability: empirical evidence from meteorological and other sources / F. Kenneth Hare Overview Paper 4: Climates of past geological epochs / I. P. Gerasimov Overview Paper 5: The physical basis of climate / W. Lawrence Gates Overview Paper 6:Modelling of climatic changes and the problem of long-range weather forecasting / G. I. Marchuk Overview Paper 7: Climate monitoring and climatic data collection services for determining climatic changes and variations / Ju. A. Izrael Overview Paper 8: Human activities that affect climate / R. E. Munn and L. Machta Overview Paper 9: Some results of climate experiments with numerical models / B. J. Mason Overview Paper 10: A scenario of possible future climates - natural and man-made / H. Flohn Overview Paper 11: missing Overview Paper 12: Climate variability and the design and operation of water resource systems Overview Paper 13: Climate, health and disease / Wolf H. Weihe Overview Paper 14: Global aspects of food production / M. S. Swaminathan Overview Paper 15: Climatic variability and agriculture in the temperate regions / James D. McQuigg Overview Paper 16: Climatic variability and agriculture in tropical moist regions / Hayao Fukui Overview Paper 17: Climatic variability and agriculture in the semi-arid tropics / Francesco Mattei Overview Paper 18: Climatic change and the exploitation of climatic resources in china / Chang Chia-cheng, Wang Shao-wu, Cheng Szu-chung Overview Paper 19 (2x): Climatic variability and land use : an african perspective / Julius S. Oguntoyinbo and Richard S. Odingo Overview Paper 20: Renewable resources and agriculture in Latin America in relation to the stability of climate / Juan J. Burgos Overview Paper 21: Climatic variability and forestry / A. Baumgartner Overview Paper 22: Climatic variation and marine fisheries / D. H. Cushing Overview Paper 23: Climatic variability, marine resources and offshore development / T. F. Gaskell Overview Paper 24: Climate and economic activity / Ralph C. d'Arge
    Type of Medium: Monograph available for loan
    Pages: 2 Ordner
    Language: English
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  • 44
    Series available for loan
    Series available for loan
    Geneva : WMO
    Call number: MOP 45420 / Mitte
    Type of Medium: Series available for loan
    Pages: Getrennte Zählung , Illustrationen , 28 cm
    Language: English
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  • 45
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-79/17
    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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  • 46
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-81/18
    In: CRREL Report, 81-18
    Description / Table of Contents: During the growing seasons of 1977, 1978, and 1979, revegetation techniques were studied on the Chena River Lakes Project, a flood control dam and levee near Fairbanks, Alaska, to find an optimal treatment for establishing permanent vegetation cover on the gravel structures. The treatments tested on plots at the dam andor levee involved three main variables 1 vegetation grass and clover seed andor willow cuttings, 2 mulch, mulch blanket, andor sludge, and 3 substrate gravel or fine-grained soil over the gravel base. The mulches were hay, wood-cellulose-fiber, peat moss, and Conwed Hydro Mulch 2000, which is a wood-cellulose-fiber mulch with a polysaccharide tackifier. A constant rate of fertilizer was applied to all plots except the control. A section of each plot was refertilized again in their third growing season to compare annual and biannual fertilization. The high fertilization rate produced above-average growth. Fescue, brome, and foxtail were the most productive species on the dam, while alsike cover was the most productive on the wetter levee site. When grass seed and willow cuttings were planted at the same time, willow survival and growth were reduced. Fertilization is required for at least two years to produce an acceptable permanent vegetation cover, although fine- grained soil or sludge reduces the amount of fertilizer needed in the second year. Third-year fertilization may not be necessary since the benefits of the second fertilization continue for at least two years. A sludge treatment refertilized during its second growing season produces the highest biomass recorded in this study.
    Type of Medium: Series available for loan
    Pages: ix, 59 Seiten , Illustrationen
    Series Statement: CRREL Report 81-18
    Language: English
    Note: CONTENTS Abstract Preface Abbreviations Conversion factors Summary Introduction Background Site characterization Climate Purpose Materials and methods General Moose Creek Dam site Tanana Levee site Sampling and measurement Abiotic controls on vegetation Meteorological data Soil moisture as a limiting factor Soil chemical analysis Vegetation growth and survival Moose Creek Dam site Tanana Levee site Biomass by species Roof penetration Seedling density of invading woody species Weeds Supplemental observations Sediment loss Sludge and runoff-water composition Cost analysis Conclusions Literature cited Appendix A: 1977 grass growth on 1977 dam treatments Appendix B: 1978 grass growth on 1977 dam treatments Appendix C: 1979 grass growth on 1977 dam treatments Appendix D: Grass growth on 1978 dam treatments Appendix E: 1977, 1978, and 1979 survival of willow treatments Appendix F: Grass growth on Tanana levee treatments Appendix C: Chemical analysis of sludge and runoff water
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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-201-81/22
    In: CRREL Report, 81-22
    Description / Table of Contents: Development of the hydropower potential of Bradley Lake, Alaska, would greatly increase winter freshwater discharge from the Bradley River into Kachemak Bay, which may result in increased ice formation and related ice-induced problems. The objectives of this investigation were to describe winter surface circulation in the bay and document ice distribution patterns for predicting where additional ice might be transported if it forms. Landsat MSS bands 5 and 7 and RBV imagery with 70% cloud cover or less, taken between 1 November and 30 April each year from 1972 to 1980, were analyzed. Surface circulation patterns inferred from suspended sediment patterns and ice distribution and movement were observed and mapped from the Landsat imagery. The generalized circulation patterns indicate that any additional ice formed due to future increased winter discharge from Bradley River would be likely to accumulate along Homer Spit and to be blown into the outer bay by the dominant northerly winter winds.
    Type of Medium: Series available for loan
    Pages: vi, 43 Seiten , Illustrationen
    Series Statement: CRREL Report 81-22
    Language: English
    Note: CONTENTS Abstract Preface Metric conversion factors Introduction Physical setting Hydrology Climate Bathymetry PhysIcal oceanography Wind effects on circulatIon Previous investigations Approach Imagery analyzed Wind and tidal data Results Suspended sediment patterns Ice distribution Generaltzed surface circulation Conclusions Literature cited Appendix A. Keys to Figures 2, 3 and 4 Appendix B. Observations made from usable Landsat Imagery Appendix C. Selected landsat images used to make observations and interpretations of surface water patterns and ice distribution
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  • 48
    Call number: 13259/I,1 ; 13259/I, 2
    Type of Medium: Monograph available for loan
    Pages: 327 Seiten
    ISBN: 0125251017
    Language: Undetermined
    Location: Upper compact magazine
    Location: Upper compact magazine
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  • 49
    Monograph available for loan
    Monograph available for loan
    Berlin : Dt. Verl. der Wissenschaften
    Associated volumes
    Call number: 12345
    In: Hochschulbücher für Physik
    Type of Medium: Monograph available for loan
    Pages: 807 Seiten , Illustrationen
    Edition: 2., unveränd. Aufl.
    Series Statement: Hochschulbücher für Physik 42
    Language: German
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  • 50
    Monograph available for loan
    Monograph available for loan
    Leipzig : Akademische Verlagsgesellschaft Geest u. Portig
    Associated volumes
    Call number: 11539
    In: Technisch-physikalische Monographien
    Type of Medium: Monograph available for loan
    Pages: 467 Seiten , Illustrationen , 22 cm
    Edition: 1. Aufl
    Series Statement: Technisch-physikalische Monographien 37
    Language: Undetermined
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  • 51
    Call number: MOP 45523 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 58 Seiten
    Series Statement: Division of Applied Physics technical papers 3
    Language: English
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  • 52
    Monograph available for loan
    Monograph available for loan
    [Edgecumbe, N.Z.] : A. Muller
    Call number: M 15.89146
    Description / Table of Contents: An account of the results of the 2 March 1987 earthquake in the eastern Bay of Plenty and the aftermath's effects on the people and places on the Rangitaiki Plains
    Type of Medium: Monograph available for loan
    Pages: 223 S., , Ill.
    Language: English
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  • 53
    Call number: MOP 44305
    Type of Medium: Monograph available for loan
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  • 54
    Call number: MOP 44977
    Type of Medium: Monograph available for loan
    Pages: 70 S.
    Language: German
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  • 55
    Monograph available for loan
    Monograph available for loan
    London [u.a.] : Academic Pr.
    Call number: PIK N 456-16-90117
    Type of Medium: Monograph available for loan
    Pages: XII, 611 S , Ill., graph. Darst
    ISBN: 0125881800
    Language: English
    Location: A 18 - must be ordered
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  • 56
    Call number: 12023/1
    In: Proceedings / Fourth International Congress on Rock Mechanics, Vol. 1
    Type of Medium: Monograph available for loan
    Pages: XXXVI, 846 S. , Ill., graph. Darst.
    ISBN: 9061910471
    Language: English , French
    Note: Contents: THEME I RHEOLOGIC BEHAVIOUR OF ROCK MASSES = COMPORTEMENT RHEOLOGIQUE DES ROCHES ET DES MASSIFS ROCHEUX = RHEOLOGISCHES VERHALTEN DES FELSENS UND DES GEBIRGES. - Geotechnical properites of the carboniferous limestone of the Bristol area : the influence of petrography and chemistry = Propriétés géotechniques des calcaires du carbonifère de la région de Bristol : Influence de la composition chimique et minéralogique = Geotechnische Eigenschaften des Karbonkalks im Gebiet von Bristol : Einfluss von Petrographie und Chemismus / S.H. Al-Jassar ; A. B. Hawkins. - Evolution des properietes mechaniques d'une roche stratifiee sous pression de confinement = Evolution of mechanical properties of a stratified rock under confining pressure = Änderungen der mechanischen Eigenschaften eines geschichteten Felsen unter Seitendruck / D. Allirot ; J. P. Boehler. - Le renforement des massifs rocheux par armatures passives / Rock Mass Reinforcement by Passive Rebars = Gebirgsverstärkung durch passive Armierung / Azuar ; Debreuille ; Habib ; Londe ; Panet ; Rochet ; Salembier. - Effets thermiques dans les cavites en couche salifere = Thermic Effects in Cavities in Salt Rock = Wärmeeffekte in Salzkavernen / P. Berest ; E. Ledoux ; B. Legait ; G. de Marsily. - An inference of crustal rheology from stress observations = L'inférence des caractéristiques rhéologiques des roches d'écorce, déterminé des mesures in situ des contraintes = Folgerungen für das Fliessverhalten der Erdkruste aufgrund von Kraft/Dehnungsmessungen / R. L. Blackwood. - Experimental determination of the residual stress field in a basaltic column = Détermination expérimentale du champ des contraintes résiduelles d'une colonne de basalte = Experimentelle Bestimmung des Restspannungszustandes einer Basaltsäule / H. Bock. - Berechnungen von Verformungen und Spannungen in Salzkavernen unter Berücksichtigung eines visko-plastischen Materialverhaltens = Evaluation of Deformations and Stresses in Salt Caverns with Account of Visco-Plastic Material Behaviour = Calcul des contraintes et des déformations autour des excavations dans le sel gemme en tenant compte du comportement visco-plastique du matériau / K.-M. Borchert ; H. Klapperich ; T. Richter ; B. Walz. - L'appareil triaxal F. P. Ms - Modele 700/40-1 = The triaxial cell F.P.Ms - model 700/40-1 = Das Triaxialdruckgerät F.P.Ms - Modell 700/40-1 / J. Brych ; C. Schröder. - Mechanical behaviour of rocks under fatigue = Réaction mécanique des roches soumises à la fatigue = Mechanisches Verhalten der Felsen unter Beanspruchung / G. Brighenti. - Changes in rock strength caused by water = Variation de résistance de roche avec la saturation d'eau = Änderungen in Felsfestigkeiten verursacht von Wasser / E. Broch. - Contribution a l'etude des parametres physico-mechaniques fondamentaux des roches = Contribution to the Study of the Fundamental Physical Mechanical Rock Parameters = Beitrag zum Studium der fundamentalen physikalisch-mechanischen Gesteinsparameter / J . Brych. - Change in residual stresses due to rheology = Variation des contraintes résiduelles à cause de la rhéologie = Änderung der Restspannungen durch rheologische Prozesse / B. Buen. - A Pilot heater test for the swedish nuclear fuel safety program = Une expérience pilote de réchauffement pour le programme suédois de sécurité contre les déchets radioactifs = Erwärmungsversuch fur das schwedische Kerbrennstoffsicherheits-Programm / H. Carlsson ; O. Stephansson ; B. Leijon. - Path dependency of rough joints in bi-directional shearing = Effets du cheminement des forces de cisaillement sur des diaclases rugueuses soumises à un cisaillement bi-directionnel = Abhängigkeit des Schervorganges in zwei Richtungen von rauhen Trennflachen um Fels infolge veränderlicher Lasten / T. B. Celestino ; R. E. Goodman. - Foundations on expansive rocks in Brazil = Fondations sur des roches expansives au Brésil = Gründungen auf expansiven Böden in Brasilien / A. J. Da Costa Nunes. - Rheologic behaviour of heterogeneous salt rocks = Comportement rhéologique des roches salines hétérogènes = Rheologisches Verhalten inhomogener Salzgesteinen / C. Dinis da Gama. - Les vides, principal facteur du comportement mechanique =The Voids, Main Factor for the Mechanical Behaviour of Rocks = Die Hohlräume, Hauptfaktor fur das mechanische Gebirgsverhalten / P. Duffaut ; F. Wojtkowiak ; J. P. Josien ; J. L. Pineau. - Das Dreiphasensystem Ton, Anhydrit, Gips und dessen zeitabhängiges Verhalten bei Zugabe von wässrigen Lösungen = The three-phase-system clay-anhydrit-gypsum and its time-dependent behaviour on saturation with water-based solutions = Le système en trois phases argile-anhydrite-gypse et son comportement relatif au temps à l'ajoutage de solutions aqueuses / H.-C. Einfalt ; E. Fecker ; H.-P. Götz. - Rock mechanics studies of proposed underground mining of potash in Sergipe, Brazil = Etude de la mécanique des roches d' une future mine de potasse à Sergipe, Brésil = Untersuchungen nach Untertagbau von Kali in Sergipe, Brasilien / C. Fairhurst ; C. M. St. John ; N. F. Midea ; S. M. de Eston ; A. C. Fernandes ; L. A. Bongiovanni. - Determination experimentale de quelques parameters elasto-viscoplastiques des roches = Experimental Determination of Some Elasto-Visco-Plastic Rock Parameters = Versuchsmässige Bestimmung einiger elasto-visko-plastischer Felsparameter / J. Fine ; S. M. Tijani ; G. Vouille ; P. Boucly. - Gesteinsphysikalisches Modell für Gesteine mit Zementationstextur = Rock-physical model for rocks with cemented texture = Modèle pétrophysique des roches à texture cimentée / M. Gálos ; P. Kertesz ; I. Kürti. - Time-dependent behaviour of granitic rocks related to their alteration grade = Comportement dans le temps des granites en fonction de leur degré d'altération = Zeitabhängiges Verhalten von Granitsteinen in Abhängikeit vom Verwitterungsgrad / R. Genevois ; A. Prestininzi. - Numerical modeling of the geochemical response of a rock mass to a radioactive waste repository = Modèles numériques pour la réponse géomécanique du massif rocheux au stockage de déchets radioactifs = Numerisches Modellieren des geomechanischen Gebirgsverhaltens bei Lagerung radioaktiver Abfälle / M. P. Hardy ; C. M. St. John ; G. Hocking. - Dilatan effects of rock joints = Effets de la dilatance des joints dans la roche = Dilatanzeffekte von Felsklüften / F. E. Heuze. - Influence de la temperature sur le comportement mechanique des roches = Influence of temperature on the mechanical behaviour of rocks = Einfluss der Temperatur auf das mechanische Verhalten der Gesteine / R. Houpert ; F. Homand-Etienne. - Effects formerly acted stress on stress-strain behaviour of rock and its anisotropical property = Recherches sur l'anisotropie de la roche et contrainte jadis agi à la roche stratifiée = Untersuchungen über die Anisotropie und den frühen aufwirkenden Lasten des Lagerschitengebirges / T. Isobe ; Y. Tominaga. - Coal behaviour in the rocky mountain belt of Canada = Comportement mécanique de charbon à la ceinture des Montagnes Rocheuses du Canada = Verhalten der Kohle in der Rocky Mountain von Kanada / M. L. Jeremic. - Time-dependent deformation of jointed rock near failure = Déformation en fonction du temps d'une roche fissurée lors de sa rupture = Zeitabhängiges Deformationsverhalten von geklüftetem Fels in der Nähe des Bruches / P. K. Kaiser ; N. R. Morgenstern. - Control of fracturing in mine rock passes = Contrôle des fracturations de gisements dans lea puits de mines = Bruchkontrolle in Grubengesteinstunnel / H. A . D. Kirsten ; J. W. Klokow. - Effect of geological compaction on the deformation of sedimentary rocks = Effet de la compaction géologique sur la déformation des roches sédimentaires = Die Wirkung der geologischen Verdichtung auf der Verformung der Sedimentgesteine / H. Koide ; K. Hoshino ; G. Endo ; M. Kitaoka. - Certain laws of creep in fissured rock and semirock = Quelques lois du glissement des semi-roches et des roches fissu , Contents: THEME III DESIGN OF UNDERGROUND STRUCTURES WITH RESPECT TO MODERN CONSTRUCTION METHODS = PROJET D'OUVRAGES SOUTERRAINS EN LIAISON AVEC LES MÈTHODES MODERNES DE CONSTRUCTION = ENTWURF VON FELSHOHLRAUMBAUTEN IM HINBLICK AUF MODERNE BAUVERFAHREN. - Criteres adoptes pour l'execution de deux tunnels routiers dans les argiles pliocenes des Apennins du Sud et pour le projet d'une galerie de derivation dans les memes formations = Criteria for the Execution of two Road Tunnels in Pliocene Clays of Southern Appenins and a Derivation Tunnel in the same Ground Types = Kriterien fur die Herstellung zweier Strassentunnel in den pliozänen Tonen des Südappenins und für einen Wasserumleitungsstollen in denselben Formationen / M. Beomonte ; A. Lupo ; F. Perretta. - Verankerte Spritzbetonschale als endgültige Auskleidung von Felshohlräumen = Anchored shotcrete used as permanent lining of underground openings' in rock = Béton projeté et ancrages utilisés comme revêtement définitif pour ouvrages souterrains en rocher / N. Bischoff ; J. Kellenberger ; A. J. Hagmann. - Criteria for the selection of fullface tunnel boring or conventional tunnelling = Critères de sélection du forage des tunnels par machine ou par construction conventionnelle des tunnels = Kriterien zur Auswahl von vollschnitt Tunnel Bohren oder konventionell Tunnel Vortrieb / O. T. Blindheim ; E. Dahl Johansen ; O. Johannessen. - Design of underground openings for oil storage = Projet de cavités souterraines pour stockage d'hydrocarbures = Entwurf von untertägigen Hohlräumen für Ölspeicherung / E. Dahl Johansen. - Determination of material parameters in cemented fill = Détermination des paramètres des matériaux dans les remblais cimentés = Bestimmung von Materialparameter in zementierten Bergversatz / P. M. Dight ; R. Cowling. - Dinorwic power station rock support of the underground caverns = Centrale de Dinorwic - Soutènement des cavités = Kraftwerk Dinorwic - Felssicherung in den Kavernen / T. H. Douglas ; L. R. Richards ; L. J. Arthur. - The role of geotechnical factors in the cutting performance of tunnelling machines in rocks = Le rôle des propriétés géotechniques à l'action de coupe des machines à percement de tunnels aux roches = Die Rolle geotechnischer Faktoren in der Schneiderate von Tunnelsmaschinen in Gesteinen / I. W. Farmer ; H. J. Hignett ; J. A. Hudson. - Preliminary underground excavations at Sayago Nuclear Power Plant = Préexcavations pour l'usine nucléaire de Sayago = Baugrund-Voraushubsarbeiten für das Kernkraftwerk Sayago / J. Feijoo ; P. Llamas. - Using data of full-scale measurement in lining desing for underground structures = Utilisation des résultats de mesures obtenus in situ pour le calcul des soutènements des ouvrages souterrains = Verwendung der Ergebnisse von den Naturmessungen für die Berechnung des Ausbaus der unterirdischen Anlagen / N. N. Fotieva ; N. S. Bulychev. - Complicated portal blasting: principles and methods based on experience = Minage compliqué dans zone de portail: Principes et méthodes basées sur expérience = Schwierige Portalsprengungen: Prinzipien und Methoden gestützt auf Erfahrungen / K. Garshol. - Anpassung von Teilschnitvortriebsmaschinen an durch von Gebirge und Bauwerk vorgegebene Bedingungen = Adaption of Partial Cutting Road Headers on Conditions given by Rock and Construction = Adaption des machines de forage à section partielle sur les conditions en cas de roes et de bâtiments / K. Gehring. - Prediction des taux de penetration d'une foreuse pleine section utilisee dans l'ile de Montreal = Prediction of penetration rates of a full face boring machine on Montreal Island = Voraussage der Vortriebsgeschwindigkeiten von Vollquerschnittsbohrmaschinen im Gebirge der Insel von Montreal / D.E. Gill ; C. Lafrance. - Stabilization systems for excavations in rock masses: results obtained in railway tunnels under construction in Brazil = Systèmes de stabilisation des excavations des massifs rocheux: les résultats obtenus en tunnels ferroviaires en construction = Sicherheits Systeme der Ausschachtung in felsigem Gestein: Tunnels in Brasilien / M. Gitelman ; A. R. Martins. - Provisional support, primary and permanent lining at the construction of the stations of the Budapest Underground = Soutènement provisoire, revêtement permanent des stations de Métro de Budapest = Sicherung und Ausbau der Stationen der Budapester U-Bahn / G. K. Greschik. - Adhesion of shotcrete to various types of rock surfaces = L'adhésion du béton projeté à des types différents de surfaces de roches = Adhäsion von Spritzbeton an verschiedenen Typen von Felsflächen / T. Hahn ; J. Holmgren. - Felsankerungen im Hohlraumbau und deren Dauerbeständigkeit = Rock anchors in underground excavations and their durability = Ancrages au rocher dans les excavations souterraines et leur durabilité / T. F. Herbst ; G. Kern. - Application of a finite element model to mining desgin at the Stekenjokk Mine, Northern Sweden = Utilisation de la méthode des éléments finis pour l'établissement d'un modèle d'exploitation de la mine de Stekenjokk, dans le nord de la Suède = Verwendung von Finite-Element Modellen auf die Abbauauslegung der Grube Stekenjokk, Nordschweden / N. Krauland. - Influence of tectonic stresses on the caving process - mining by block caving methods = Influence des efforts tectoniques dans le processus d'éboulement - Travail des mines par éboulement = Einfluss der tektonischen Spannungen auf den Erzabbauerz - Abbauverfahren nach Kammerbruchbaumethode / G. Krstulovic. - Abteufen und Sicherung eines 80 M tiefen Kraftwerksschachtes von 30 M Durchmesser = Sinking and Supporting of an 80 m deep Power Situation Shaft of 30 M Diameter = Fonçage et mesures de sécurité pour un puits d'usine électrique de 80 m de profondeur et de 30 m de diamètre / H. Lauffer ; W. Pircher. - L'influence de la methode de construction sur l'equilibre final d'un tunnel = Influence of the Constructional Method on the Final Equilibrium of a Tunnel = Einfluss der Baumethode auf das Endgleichgewicht eines Tunnels / G. Lombardi ; W. Amberg. - Weiterentwicklung der Tunnelbauverfahren durch Stahlfaserbeton = Development of New Tunnelling Methods using Steel Fibre Shotcrete = Développement d'une nouvelle méthode d e soutènement: le béton projeté armé de fibres d'acier / B. Maidl ; R. Rapp. - Excavation mechanique, soutenement et impermeabilisation des tunnels de turumo au Venezuela = Mechanized excavation supporting and sealing of Turumo Tunnels in Venezuela = Maschinelle Aushebung, Unterhaltung und Wasserdichtmachen der Turumo Tunnel in Venezuela / F. Mendana ; R. Fernandez-Gonzalez. - Untersuchung unterirdischer wassertechischer Bauwerke an Modellen aus aequivalenten Stoffen = Investigations of Underground Hydraulic Structures on Models of Equivalent Materials = Etudes des ouvrages hydrauliques souterrains sur modèles en materiaux équivalents / W. M. Mostkow ; N. S. Chatschaturjan ; P. D. Stefanow ; M. N. Belkin. - Die Bedeutung der Ringschlusslänge und Ringschlusszeit im Tunnelbau = The Importance of the Length and Time of Closing the Ring in Tunnelling = L'importance de la longueur et du temps de fermeture de l'anneau dans la construction de tunnels / L. Müller. - Die Beherrschung grosser Querschnitte in schwierigen Gebirgsarten = The control of large cross sections in difficult grounds = Le contrôle des grandes sections tranversales dans les roches difficiles / F. Pacher ; N. Ayaydin. - Stresses and strains at the contact of rigid tunnel lining and soft rock = Contraintes et déformations au contact du revêtement raide du tunnel et des roches tendres = Spannung und Verformungen am Kontakt der steifen Tunnelauskleidung mit weichem Fels / B. Popović ; O. Marković ; M. Manojlović. - Die Schäden im Hattelberg-Druckstollen als Folge eines aussergewöhnlichen Primärspannungszustandes = Damages at Hattelberg Pressure Tunnel Caused by Extraordinary Natural Stresses = Les dégâts causés à la galerie en charge de Hattelber g par , Contents: THEME IV SURFACE DISPLACEMENTS AS A CONSEQUENCE OF EXCAVATION ACTIVITIES = MOUVEMENTS EN SURFACE PROVOQUÉS PAR DES TRAVAUX D'EXCAVATION = OBERFLÄCHENBEWEGUNGEN INFOLGE VON AUSBRUCHSARBEITEN. - Model studies of very large underground openings at shallow depth = Etude sur modèle de très grandes ouvertures souterraines à faible profondeur = Modellstudien über Felskavernen mit sehr grossen Spannweiten in geringer Tiefe / N. Barton. - A case history of pit slope design = Fouille à ciel ouvert: étude d'un cas particulier = Fallstudie eines Böschungsentwurfes für einen Tagbau / D. F. Coates, M. Gyenge. - Affaissements miniers et deformation du sol influence de la lithologie du recouvrement = Mining Subsidence and Ground Deformations. Influence of the Lithology of the Overburden = Senkungen und Baugrundverformungen infolge Bergbaus. Einfluss der Lithologie des Deckgebirges / M. Dejean, J. Arcamone. - Prediction of rock mass deformability = Méthode pour déterminer la déformabilité des massifs rocheux = Methode zur Bestimmung der Gebirgsverformbarkeit / W. Dershowitz, G. Baecher, H. Einstein. - Rupture progressive en versant rocheux stratifie et fissure = Progressive failure in a stratified and fissurated rock slope = Progressiver Bruch in einer geschichteten und geklüfteten Felsböschung / F . Descoeudres, M. Gencer. - Bestimmung der Oberflächendeformation und der Aussenbelastung der Auskleidung an physikalischen Modellen = Determination of surface Deformation and Outside Load of Lining on Physical Models = Détermination de la déformation de la surface du terrain et de la charge extérieure de revêtement sur les modèles physiques / v. Dolezel. - Underground driving below a speedway = Tunnel du métro creusé sous une autoroute = U-Bahn Ausbruch unter einer Autobahn / A. Dvorák. - Surface movements due to grouting pressure = Soulèvement en surface à cause de pression d'injection = Oberflächenbewegung wegen des Injektionsdruckes / L. Fingerhut. - Method of probabilistic analysis of rock slopes stability (slopes of quarries and foundation pits, natural rock slopes) = Evaluation probabiliste de la stabilité des talus rocheux (talus de carrières, de fouilles et versants rocheux naturels) = Wahrscheinlichkeitsberechnungsverfahren der Standsicherheit von Felsböschungen (Tagebaurändern, Baugruben und natürlichen Böschungen) / E. G. Gaziev, V. I. Rechitski. - Cave-in and subsidence at the Rodsand Mine, Western Norway = Contrôle d'éboulement à la mine de Rodsand, Norvège occidentale = Kontrolle von Verbrüchen bei der Grube Rodsand, Westnorwegen / H.-P. Geis. - Slope failure in expansive marls = Rupture de talus dans des marnes expansives = Böschungsbruch in quellfähigen Mergeln / L. Gonzalez de Vallejo, J. A. Campos de Orellana, J. L. Berzal, A. Linares-Rivas. - Designing primary blasts for increased slope stability = Contrôle du tir des mines pour augmenter la stabilité des parements = Entwurf von Primärsprengungen zur Erhöhung der Böschungssicherheit / T. N. Hagan. - Surface subsidence and horizontal displacement caused by mining inclined coal seams = L'affaissement du sol et le déplacement horizontal causés par l'extraction des couches houillères inclinées = Bodensenkung und horizontale Verschiebung, die der Abbau des geneigten Kohlenflözes verursacht / Y. Hiramatsu, H. Okamura, K. Sugawara. - Der Abbau von Braunkohle aus einem Bergrutsch in Tagebau "Kosovo"-Belacevac = The exploitation of lignite from a landslide in the opencast mine "Kosovo"-Belacevac = Exploitation de lignite en terrain instable dans la mine à ciel ouvert "Kosovo''-Belacevac / L. J. Ilić, N. Spasić. - Surface displacements caused by tunnel driving in anisotropic viscoelastic ground = Tassements superficiels induits par le creusement d'un tunnel dans un sol visco-élastique anisotropique = Die oberflächlichen Verschiebungen verursacht durch den Graben des Tunnels in einem anisotropen viskoelastischen Grund / T. Ito, M. Hisatake. - Neuere Erkenntnisse zur Reduzierung der Oberflächensetzungen bei der Auffahrung von seichtliegenden Tunnelröhren = Progress in Reducing Surface Settlements Due to Tunnels at Small Depth = Mesures tendant à diminuer les tassements en surface causés par l'excavation des tunnels à faible profondeur / O. Jagsch, L. Müller, A. Hereth. - The observed results of displacements during the excavation of slope and the numerical analysis of its stability = Les résultats observés des déplacements pendant l'excavation de talus et l'analyse numérique des stabilités = Die Beobachtungsresultate der Verschiebungen bei Böschungseinschnitten und die numerische Analyse ihrer Standsicherheit / Y. Kitahara, T. Tokue, H. Ito, M. Motojima, M. Akashi. - The stability study of unstable wedges caused by large excavations at Itaparica Dam = Etude de la stabilité de coins potentiellement instables créés par les grandes fouilles du barrage Itaparica = Standsicherheitsuntersuchungen von Keilen bei Grossaushubsarbeiten am Itaparica-Damm / F. A. S. Nazario, S. Shayani, M. Lucas. - Stresses amd displacements around an advancing face of a tunnel = Tension et déplacements autour de la taille d'un tunnel = Spannungen und Verschiebungen um einen nach vorne bewegten Tunnel / Y. Niwa, S. Kobayashi, T. Fukui. - Slope stability in deep open pit mine with tension cracks = Stabilité des talus et fissures de traction dans une mine à ciel ouvert = Böschungssicherheit in einem tiefen Tagbau mit Zugrissen / M. Osmanagić, M. Redzepagić. - Settlements induced by a tunnel in miocenic soft rocks of Madrid = Tassements produits par la construction d'un tunnel dans des roches molles = Unterführungsabsenkungen auf weichen miozanischen Felsen in Madrid / C. S. Oteo, J. F. Moya. - Analysis of the stability of slopes in weathered rocks = Analyse de stabilité des pentes en roches décomposées = Die Analyse der Abhang-Stabilität in gewittertem Gestein / R. T. Sancio, R. E. Goodman. - Some investigations into the surface movement due to underground mining by bord and pillar method = Mesures des tassements en surface causés par les exploitations minières en "chambre et pilier" = Einige Untersuchungen der Oberflächenbewegungen infolge Bergbaus nach der Pfeilermethode / R. D. Singh. - Downhill movements of the slopes at the Idrija Ore Deposit = Mouvements descendants des pentes des dépôts minerais d'Idrija = Talseitige Hangbewegungen im Idrija Bergbau Gebiet / I. Sovinc. - Arching in hanging walls over leached deposits of rock salt = Les effets d'arc dans le toit du sel gemme exploité par solution = Bogenwirkung im mergligen Hangenden eines durch Lösung exploitierten Steinsalzlagers / M. Stević, I. Jasarević, F. Ramiz. - Ancrages "Cabra Corral" = Anchoring at "Cabra Corral" = Verankerungen in "Cabra Corral" / S. Vallespir, F. Barrionuevo, J. M. Sanz Saracho, V. Cid, F. Suva. , Contents: GROUP PAPERS = COMMUNICATIONS DE GROUPE = GRUPPENBERICHTE. - Rock mechanics in Sweden - a survey = La mécanique des roches en Suède - vues générales = Gebirgsmechanik in Schweden - eine Übersicht / S. G. A. Bergmann, S. Bjurström. - Role de l'auscultation dans la conception et l'excution d'ouvrages souterrains = Role of monitoring in the design and execution of underground works = Rolle der Kontrollmessungen beim Entwurf und bei der Herstellung von Untertagarbeiten / Comité Français de Mécanique des Roches. - Recents developments dans l'approche geotechnique de l'abattage mecanise en France = Recent geotechnical works in the field of mechanical rock cutting in France = Neue geotechnische Entwicklung des mechanischen Abbaus in Frankreich / Pechalat, Vienne, Chambon, Lebrun, Tincelin, Comes, Cordel, Marin, Fourmaintreaux, Louis, Raffoux. - Rock mechanics for engineering problems in India = Mécanique des roches appliquée à différents problèmes en Inde = Felsmechanik für Ingenieuraufgaben in Indien / Indian National Group. - Recent tunneling experiences in Italy = Récentes expériences dans l'excavation de galeries en Italie = Letzte italienische Erfahrungen in Tunnelbauten / AGI. - Some Italian experiences on the mechanical characterization of structurally complex formations = Expériences italiennes sur la caractérisation mécanique de formations structurellement complexes = Einige italienische Erfahrungen über Felsen mit complexer Struktur / AGI.
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    Leipzig : Akademie der Wissenschaften der DDR, Zentralinstitut für Isotopen- und Strahlenforschung
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    Call number: ZSP-980-46
    In: ZfI-Mitteilungen, Nr. 46
    Type of Medium: Series available for loan
    Pages: 134 Seiten , Illustrationen
    Series Statement: ZfI-Mitteilungen 46
    Language: German
    Note: Inhaltsverzeichnis: Nichtkonstante relative Atommassen als Folge variierender Isotopenhäufigkeiten polynuklider Elemente und ihre Auswirkungen auf die Richtigkeit analytischer Meßwerte bei der Elementanalytik / H. Gerstenberger. - Massenspektrographische Analyse an Standardgesteinsproben / H.-J. Dietze. - Methodische Untersuchungen zur massenspektrographischen Analyse an geologischen Proben mit relativ hohen Seltenerdengehalten / S. Becker, H.-J. Dietze. - Massenspektrographische Analyse von Calciumfluorid-Einkristallen / H.-J. Dietze, H. Zahn. - Gammaaktivierungsanalyse am Mikrotron MT 22 : analytische Möglichkeiten für geologische Proben und Rohsilizium, Bestimmung von Blei / M. Geisler, H. Gerstenberger. - Zur Korrektur von Inhomogenitäten des Reaktorneutronenflusses bei der Aktivierungsanalyse / M. Geisler, H. Schelhorn. - Instrumentelle Aktivierungsanalyse von Molybdäniten / M. Geisler, H. Schelhorn. - Bestimmung von Osmium in Molybdäniten / H. Schelhorn, M. Geisler. - Instrumentelle Aktivierungsanalyse von Flugstaub / M. Geisler. - Aktivierungsanalytische Kontrolle von Spurenelementen bei der Gallium-Diffusion in Silizium / M. Geisler. - Übersicht über bisher erschienene Hefte der ZfI-Mitteilungen.
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    Warszawa : Państwowe Wydawnictwo Naukowe
    Call number: AWI P6-93-0291
    Type of Medium: Monograph available for loan
    Pages: 224 Seiten , Illustrationen, graphische Darstellungen
    ISBN: 83-01-01231-5
    Series Statement: Biblioteka Problemów 252
    Language: Polish
    Note: In polnischer Sprache
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    New York, NY [u.a.] : Wiley
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    Call number: G 8116
    In: Chemical analysis, 27
    Type of Medium: Monograph available for loan
    Pages: XI, 489 S
    Edition: 2nd. ed.
    ISBN: 047102743X
    Series Statement: Chemical analysis 27
    Language: English
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    [Erscheinungsort nicht ermittelbar] : [Verlag nicht ermittelbar]
    Call number: AWI P6-89-0490
    Type of Medium: Monograph available for loan
    Pages: 124, 5 Seiten
    Edition: Stand: 16. Oktober 1979
    Language: German
    Note: Inhaltsverzeichnis: Einleitung. - Internationale Zusammenarbeit. - Staatliche Zusammenarbeit. - Nichtstaatliche Zusammenarbeit. - I. Wissenschaftliches Programm. - 1. Astronomie. - 2. Biowissenschaften. - 2.1 Das marine Ökosystem und seine lebenden Ressourcen. - 2.1.1 Nährstoffangebot, Phytoplanktonproduktion und Zooplankton. - 2.1.2 Die Rolle des Benthos. - 2.1.3 Die Rolle der Mikroorganismen. - 2.1.4 Verbreitung und Häufigkeit der Robben im Packeis der Weddell-See. - 2.1.5 Verbreitung und Lebensgeschichte von Fischen und Tintenfischen. - 2.1.6 Großskalige Verbreitung und Verdriftung des Krill. - 2.1.7 Zusammensetzung und Verhalten von Krillschwärmen. - 2.1.8 Frischhaltung und Verarbeitung des Krill. - 2.2 Die Anpassung antarktischer Meeresorganismen an ihren Lebensraum. - 2.2.1 Experimentelle Arbeiten und Seeuntersuchungen zur Ökophysiologie des Krill. - 2.2.2 Temperaturregulation und Nahrungsbedarf bei antarktischen warmblütigen Tieren. - 2.2.3 Wachstum, Verdauung und Nahrungsausnutzung bei antarktischen Fischen. - 2.2.4 Frostschutzanpassungen von Meerestieren. - 2.2.5 Taxonomie antarktischer Meeresorganismen. - 2.3 Terrestrische Biologie in der Antarktis. - 2.3.1 Temperaturanpassungen der Brutbiologie antarktischer Vögel. - 2.3.2 Biochemische Grundlagen der Wachstumsvorgänge wechsewarmer Organismen unter sehr niedrigen Temperaturen. - 2.3.3 Nahrungsbiologie wechselwarmer Pflanzenfresser. - 2.3.4 Untersuchung der Flechten, Pilze und Bakterien in der Antarktis und auf den vorgelagerten Inseln. - 2.3.5 Photosynthese und heterotrophe Lebensweise von Pflanzen bei sehr niedrigen Temperaturen. - 2.4 Umweltschutz in der Antarktis. - 2.5 Humanbiologie und Medizin in Polargebieten. - 3. Geodäsie, Kartographie und Fernerkundung. - 3.1 Satelliten-Geodäsie. - 3.2 Geodätische Positionsbestimmung (Doppler Satellite Positioning). - 3.3 Geodätisch-kartographische Aufnahme eisfreier Gebiete. - 3.4 Fernerkundung mit Satelliten. - 4. Geologie und Geophysik. - 4.1 Studium der Driftvorgänge als Beitrag zur Erdgeschichte der Antarktis. - 4.1.1 Untersuchung magnetischer Strukturen mit aeromagnetischen Aufnahmen. - 4.1.2 Paläomagnetische Untersuchungen zur Driftgeschichte. - 4.1.3 Mikroerdbeben als Indikatoren für eine aktive Tektonik. - 4.1.4 Erdgezeiten und Eigenschwingungen der Erde. - 4.2 Untersuchungen über den Aufbau von Kruste und Mantel. - 4.2.1 Aufbau des Felsuntergrundes des transantarktischen Gebirgszuges im Bereich östlich des Filchner-Schelfeises. - 4.2.2 Aufbau des tieferen Untergrundes in der Weddell-See, dem Filchner/Ronne-Schelfeis und der Umrandung. - 4.2.3 Älteste und hochmetamorphe Gesteine der Ostantarktis. - 4.3 Stratigraphie, Tektonik und Magmatismus in den mobilen Bereichen. - 4.3.1 Mobile Randbereiche der Ostantarktis. - 4.3.2 Paläozoisches und mesozdisches Deckgebirge (Beacon-Obergruppe) im Transantarktischen Gebirge. - 4.3.3 Jungpaläozoische bis känozoische Orogene im Umkreis des Filchner/Ronne-Schelfeises. - 4.4 Studium exogener Vorgänge unter extrem kalten Bedingungen. - 4.4.1 Glazialgeologie und -geomorphologie. - 4.4.2 Verwitterung und Schuttbildung. - 4.5 Geowissenschaftliehe Meeresforschung. - 5. Glaziologie. - 5.1 Massenhaushalt und Dynamik des Filchner/Ronne-Schelfeises. - 5.2 Bestimmung der Eismächtigkeiten und ihrer zeitlichen Variation im Filchner/RonneSchelfeis-Sektor und der umrandeten Gebiete. - 5.3 Bestimmung des Aufbaus und der inneren Struktur des Filchner/Ronne-Schelfeises aus geophysikalischen Oberflächenmessungen. - 5.4 Untersuchungen zur Dynamik des Packeises im Weddell-Gyre. - 5.5 Physikalische Eigenschaften des Meereises. - 5.6 Glaziologische Bohrungen 5.7 Chemische Zusammensetzung und Akkumulationsgeschichte des antarktischen Background-Aerosol; globaler Transport von Spurengasen und Aerosolen. - 5.8 Untersuchung der elastischen und rheologischen Eigenschaften von Eis, seiner Wärmeleitfähigkeit und deformationsbedingten Textur. - 6. Hohe Atmosphäre und Extraterrestrische Physik. - 6.1 Untersuchung von Whistlern und VLF-Radioemissionen (Chorus, Hiss usw.), u.a. an konjugierten Punkten. - 6.2 Untersuchung erdmagnetischer Pulsationen an konjugierten Punkten. - 6.3 Untersuchung von Atmospherics zur genaueren Erfassung der weltweiten Gewitter-Aktivität. - 6.4 Messungen des luftelektrischen Feldes. - 6.5 Untersuchung der Ionosphäre vom Ballon aus im Licht der Mg+-Resonanzlinien. - 6.6 Messung der vertikalen Ozon-, Wasserdampf und Aerosolverteilung bis zu 30 km Höhe. - 6.7 Messungen der Emission in der infraroten 9,6 µ Ozonbande vom Boden aus. - 6.8 Weitere eventuell oder später mögliche Projekte. - 6.9 Vorschlag für eine erdmagnetische Grundausrüstung der Antarktisstation. - 6.10 Expedition zur Meteoritensuche. - 6.11 Untersuchung von Mikrometeoriten und kosmischem Staub. - 7. Meteorologie und Ozeanographie. - 7.1 Meteorologie. - 7.1.1 Atmosphärische Grenzschicht. - 7.1.2 Untersuchung der Stratosphären-Zirkulation. - 7.1.3 Langzeitmessungen von Spurengasen. - 7.1.4 Weitere Forschungsvorhaben. - 7.1.5 Wetterdienstliche Beobachtungen und Beratungen. - 7.1.6 Meteorologische Grundausüstung der Antarktisstation. - 7.2 Physikalische Ozeanographie. - 7.2.1 Bildung und Ausbreitung von Bodenwasser im atlantischen Sektor der Zirkum-Antarktischen See. - 7.2.2 Numerische Simulation der vertikalen Flüsse von Stoff, Energie und Impuls. - 7.2.3 Zeitskalen von Transportvorgängen im Tiefenwasser mit Hilfe von radioaktiven Spurenstoffen. - 7.2.4 Bestimmung von Schwermetallen im Antarktischen Ozean. - 7.2.5 Fischereiozeanographie im antarktischen Wasserring. - 7.2.6 Weitere Forschungsvorhaben. - 8. Ingenieurwissenschaften. - 8.1 Schiffstechnik. - 8.1.1 Ingenieurwissenschaftliches Meß- und Erprobungsprogramm über das Verhalten von Schiffen im Eis sowie technische Entwicklungen im Bau eisgehender Schiffe. - 8.2 Eisbergortung und Navigation. - 8.2.1 Eisbergortung. - 8.2.2 Entwicklung präziser Positionierungssysteme (auch für dynamische Positionierung), die eine ungestörte Signalübermittlung durch Eis- und Wasserschichten mit verschiedenen Dichtegehalten ermöglichen. - 8.3 Bautechnik I Einzelprojekte. - 8.4 Explorationstechniken. - 8.5 Weitere Themen.
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  • 61
    Call number: MOP 45462
    Type of Medium: Monograph available for loan
    Language: German
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  • 62
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    Hanover, NH : U. S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-85/21
    In: CRREL Report, 85-21
    Description / Table of Contents: The development of lightweight coring augers for ice is reviewed. Emphasis is on equipment designed by the Cold Regions Research and Engineering Laboratory and its predecessor organizations for sampling to depths less than 20 m or so. Design and operation of the ACFEL/SIPRE/CRREL 3-in. -ID corer is discussed, and modifications of the basic design for powered operation and for drilling in frozen soil are outlined. Recent replacements for the traditional coring auger are described, and details are given for the construction and operation of the new 4 1/4-in-ID coring equipment. A powered 12-in.-ID drill for shallow-depth coring is also described.
    Type of Medium: Series available for loan
    Pages: iii, 27 Seiten , Illustrationen
    Series Statement: CRREL Report 85-21
    Language: English
    Note: CONTENTS Abstract Preface Introduction The 3-inch ice corer The Rand auger Parallel development of comparable drills The Big John 12-inch corer Power drives A simple Russian ice-corer Conclusions Literature cited
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  • 63
    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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  • 64
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    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-79/10
    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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  • 65
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    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-79/11
    In: CRREL Report, 79-11
    Description / Table of Contents: A theory of the optical properties of snow in the 2-20 region of the infrared has been developed. Using this theory it is possible to predict the absorption and scattering coefficients and the emissivity of snow, as a function of the snow parameters of grain size and density, for densities between 0.17 and 0.4 g/cm3. The absorption and scattering coefficients are linearly related to the density and inversely related to the average grain size. The emissivity is independent of grain size and exhibits only a weak dependence upon density.
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    Pages: iii, 9 Seiten , Illustrationen
    Series Statement: CRREL Report 79-11
    Language: English
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  • 66
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    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-79/12
    In: CRREL Report, 79-12
    Description / Table of Contents: An analysis of a point source bubbler system used to induce local melting of an ice cover is presented. The analysis leads to a numerical simulation programmed in FORTRAN which may be used to predict the effectiveness of such systems. An example application is presented using a typical record of average daily air temperatures. The FORTRAN program for the point source simulation as well as a FORTRAN program for line source systems are included in the Appendix.
    Type of Medium: Series available for loan
    Pages: iii, 12 Seiten , Illustrationen
    Series Statement: CRREL Report 79-12
    Language: English
    Note: CONTENTS Abstract Preface Introduction Outline of analysis Plume analysis Heat transfer analysis Temperature of impinging plume Heat transfer coefficient Melting of the ice cover Simulation example Thermal reserve analysis Literature cited Appendix
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  • 67
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    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%.
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    Pages: ii, 5 Seiten , Illustrationen
    Series Statement: CRREL Report 79-13
    Language: English
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  • 68
    Monograph available for loan
    Monograph available for loan
    Leningrad : Gidrometeoizdat
    Call number: MOP 44835 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 239 Seiten , Illustrationen , 22 cm
    Language: Russian
    Note: In kyrillischer Schrift
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  • 69
    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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  • 70
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    Monograph available for loan
    Silver Spring : Central Pacific Hurricane Center
    Call number: MOP 45480
    Type of Medium: Monograph available for loan
    Pages: V, 137 Seiten
    Language: English
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  • 71
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    Washington, D.C. : National Advisory Committee on Oceans and Atmosphere
    Call number: MOP 45479 / Mitte
    Type of Medium: Monograph available for loan
    Pages: II, 28 Seiten
    Language: English
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  • 72
    Call number: MOP 45859 / Mitte
    Type of Medium: Monograph available for loan
    Series Statement: Spravočnik statističeskie charakteristiki polej temperatury i vlažnosti v atmosfere severnogo polušarija 4
    Language: Russian
    Note: In kyrillischer Schrift
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  • 73
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    Dresden : Ingenieurschule für Geodäsie und Kartographie
    Associated volumes
    Call number: MOP 47522/4 / Mitte
    In: Spezielles Lehrmaterial für die Aus- und Weiterbildung von Ingenieuren der Fachrichtung Meteorologie
    Type of Medium: Monograph available for loan
    Pages: I, 26 Seiten , Graphische Darstellungen
    Edition: 1. Auflage
    Series Statement: Spezielles Lehrmaterial für die Aus- und Weiterbildung von Ingenieuren der Fachrichtung Meteorologie
    Language: German
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  • 74
    Call number: MOP 45822 / Mitte
    Type of Medium: Monograph available for loan
    Pages: in Auszügen
    ISBN: 0853122121 , 0470271833
    Series Statement: Ellis Horwood series in environmental sciences
    Language: English
    Note: Table of Contents Preface List of Participants Foreword Introduction Education and training in remote sensing Chapter 1 Background - the physical basis of remote sensing Chapter 2 The EARTHNET data acquisition, processing and distribution faculty Chapter 3 METEOSAT, Europe's contribution to the global weather observing system Chapter 4 Remote sensing from space: review of future plans and prospects Chapter 5 Guide to the design and specification of a primary user receiving station for meteorological and oceanographic satellite data Chapter 6 The design and implementation of DIBIAS, a digital interactive image processing system Chapter 7 A low-cost image data display system for teaching use Chapter 8 Elementary ideas of optical image processing Chapter 9 Geometrical aspects of remote sensing, space cartography Chapter 10 Statistical methods: a selective tutorial survey Chapter 11 The atmospheric correction of remotely sensed data and the quantitative determination of suspended matter in marine water surface layers Chapter 12 Remote sensing of a complex surface Chapter 13 Some legal aspects of remote sensing Chapter 14 Airborne remote sensing experiments with a fluorescent tracer Chapter 15 Remote sensing of pollution Chapter 16 Studies of dust storms from satellites Chapter 17 The use of remote sensing in hydrology in Norway Chapter 18 Radio echo sounding of ice masses: principles and applications Chapter 19 Examples of applications of digital image processing of remotely sensed phenomena Chapter 20 Sea surface fronts and temperatures Chapter 21 Remote sensing of ocean waves, currents and surface winds by dekametric radar Chapter 22 The SEASAT-1 synthetic aperture radar: introduction data reception and processing Chapter 23 Microwave radiometry and applications Chapter 24 Meteorological models and climatological data sets Chapter 25 Use of satellite images and derived meteorological parameters for weather analysis and forecast Chapter 26 The use of cinematographic methods for the presentation of atmospheric motions as revealed by remote sensing techniques from satellites Notes on Field Trips FT1 A field assessment of various forms of remote sensing imagery on theTay Estuary tidal flats FT2 Notes for field work on sea truth measurement for remote sensing verification Worksheets for Laboratory Exercises WS1 Example of an exercise in aerial photograph interpretation WS2 A case study of mid-latitude frontal cyclone structure using TIROS-N upper-air and surface observations WS3 A climatological archive from meteorological satellite data - the problems involved WS4 Interpretation of aerial infrared survey data WS5 Simple spatial filtering experiments WS6 Portable LANDSAT-type radiometer and classification of a LANDSAT scene of the Dundee area WS7 Estimation of the forest area in the County of Norfolk from LANDSAT MSS images WS8 Classification and temporal variation in Wessex using LANDSAT MSS images WS9 Mapping of the Abertay Sands using LANDSAT MSS digital data WS 10 Estimation of snow cover in the Scottish highlands from LANDSAT imagery WS 11 Snow cover determination from TIROS-N and NOAA-6 AVHRR data Index
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  • 75
    Call number: MOP 45384/2 / Mitte
    Type of Medium: Monograph available for loan
    Pages: Getrennte Zählung , Illustrationen
    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-201-79/28
    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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  • 77
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    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-79/26
    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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  • 78
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    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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  • 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-201-79/24
    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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  • 80
    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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  • 81
    Monograph available for loan
    Monograph available for loan
    Washington, D.C. : Mineralogical Society of America
    Associated volumes
    Call number: 11/M 19.92803
    In: Reviews in mineralogy, 6
    Type of Medium: Monograph available for loan
    Pages: ix, 380 Seiten , Illustrationen, Diagramme
    Edition: second printing
    ISBN: 978-0-939950-06-5
    Series Statement: Reviews in mineralogy 6
    Language: English
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  • 82
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    Monograph available for loan
    Washington, D.C. : Mineralogical Society of America
    Associated volumes
    Call number: 11/M 19.92818
    In: Reviews in mineralogy, 20
    Type of Medium: Monograph available for loan
    Pages: xi, 369 Seiten , Illustrationen, Diagramme
    ISBN: 0-939950-24-3
    Series Statement: Reviews in mineralogy 20
    Language: English
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  • 83
    Monograph available for loan
    Monograph available for loan
    Washington, D.C. : Mineralogical Society of America
    Associated volumes
    Call number: 11/M 19.92819
    In: Reviews in mineralogy, 27
    Type of Medium: Monograph available for loan
    Pages: xv, 516 Seiten , Illustrationen, Diagramme
    Edition: second printing
    ISBN: 0-939950-32-4
    Series Statement: Reviews in mineralogy 27
    Language: English
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  • 84
    Call number: MOP 44963 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 20 Seiten
    Language: German
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  • 85
    Monograph available for loan
    Monograph available for loan
    Moskva : Sovetskoe Radio
    Call number: 3207
    Type of Medium: Monograph available for loan
    Pages: 106 Seiten , graphische Darstellungen
    Series Statement: Rezulʹtaty issledovanij po meždunarodnym geofizičeskim proektam
    Language: Russian
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  • 86
    Call number: MOP 44928 / Mitte
    Type of Medium: Dissertations
    Pages: 139 Seiten , graphische Darstellungen
    Language: German
    Note: Inaugural-Dissertation zur Erlangung der Doktorwürde der Hohen Mathematisch-Naturwissenschaftlichen Fakultät der Rheinischen Friedrich-Wilhelms-Universität zu Bonn vorgelegt von Josef Schäfer aus Berge.
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  • 87
    Call number: MOP 44883 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 27 Seiten , Illustrationen , 21 cm
    Language: Russian
    Note: In kyrillischer Schrift
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  • 88
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    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-81/13
    In: CRREL Report, 81-13
    Description / Table of Contents: Electrical properties of frozen ground were measured using radio frequency interferometry (RFI) in the very high frequency (VHF) radiowave band. Ice-rich organic silts and sands and gravels of variable ice content were investigated during early April of both 1979 and 1980. Frequencies between 10 and 150 MHz were used with best results obtained between 40 and 100 MHz. Surface impedance and magnetic induction techniques were also used to obtain an independent measure of low frequency resistivity and to obtain a separate control on vertical inhomogeneity. Soil samples were tested for organic and water content. The dielectric constants determined for the ice-rich organic silts ranged from 4.0 to 5.5 while those for the sands and gravels were about 5.1. Dielectric loss was due to d.c. conduction and was very low for the silts but significant for the sands and gravels. The higher values for the sands and gravels were most likely due to the higher concentrations of salt that are reported to exist in the old beach ridges in this region. All the RFI measurements are believed to be indicative of only the first few meters of the ground although the radiowaves could penetrate to tens of meters.
    Type of Medium: Series available for loan
    Pages: iv, 18 Seiten , Illustrationen
    Series Statement: CRREL Report 81-13
    Language: English
    Note: CONTENTS Abstract Preface Introduction Background Objectives and procedures Theory and instrumentation Radio frequency interferometry Case 1: Homogeneous ground model Case 2: Two-layer ground model RFI instrumentation Low frequency methods Point Barrow sites Results and discussion Site 1: Tundra Site 2: Beach ridge Site 3: Marsh Conclusions Literature cited Appendix A: Discussion of low-frequency geophysical methods
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  • 89
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    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-81/16
    In: CRREL Report, 81-16
    Description / Table of Contents: An air-transportable shelter designed and built at CRREL for use in cold regions underwent testing in Hanover, New Hampshire, and Ft. Greely, Alaska. The shelter demonstrated some of its capabilities for mobility by being towed for more than 60 miles behind various vehicles and by being transported on a C-130 cargo airplane, a CH-47 helicopter, and a trailer truck. The shelter proved to be very easy for a crew of two to four to set up in all weather conditions including -40 F cold. However, the gasoline-powered generator, which was a source for space heat as well as electricity, functioned very poorly. Overall, the prototype successfully demonstrated qualities of self-reliance, ease of operation and thermal efficiency.
    Type of Medium: Series available for loan
    Pages: v, 20 Seiten , Illustrationen
    Series Statement: CRREL Report 81-16
    Language: English
    Note: CONTENTS Abstract Preface Metric conversion factors Summary Introduction Description of shelter Test procedures and results Mobility Ease of erecting and striking Therinal efficiency and performance Heat output Electrical system Habitation Safety features Water system Shelter reliability Structure Performance of other shelters Conclusions Future studies Literature cited
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  • 90
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    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-81/17
    In: CRREL Report, 81-17
    Description / Table of Contents: Environmental conditions are described for the continental shelf of the western Arctic, and for the shelf of Labrador and Newfoundland. Special emphasis is given to the gouging of bottom sediments by ice pressure ridges and icebergs, and an approach to systematic risk analysis is outlined. Protection os subsea pipelines and cables by trenching and direct embedment is discussed, touching on burial depth, degree of protection, and environmental impact. Conventional land techniques can be adapted for trenching across the beach and through the shallows, but in deeper water special equipment is required. The devices discussed include hydraulic dredges, submarine dredges, plows, rippers, water jets, disc saws and wheel ditchers, ladder trenchers and chain saws, routers and slot millers, ladder dredges, vibratory and percussive machines, and blasting systems. Consideration is given to the relative merits of working with seabed vehicles, or alternatively with direct surface support from vessels or from the sea ice
    Type of Medium: Series available for loan
    Pages: 38 Seiten , Illustrationen
    Series Statement: CRREL Report 81-17
    Language: English
    Note: CONTENTS Abstract Preface Introduction The western Arctic of North America The continental shelf of Newfoundland and Labrador Burial depth for pipes and cables Degree of protection offered by burial Environmental impact Trenching the beach and the shallows in the western Arctic Trenching beyond the shallows Suction, or hydraulic, dredging Bottom-t raveling cutterhead dredges Plows Rippers Water jets Subsea disc saws and wheel ditchers Subsea ladder trenchers and chain saws Subsea routers and slot millers Bucket ladder trenchers Vibratory and percussive devices Hard rock excavation under water Control and monitoring of subsea machines Vessels and vehicles Trenching from the sea ice Costs of subsea trenching Reference Appendix: Description of waters off Alaska and Newfoundland
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  • 91
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-81/3
    In: CRREL Report, 81- 3
    Description / Table of Contents: Abstract: A 1:24 scale hydraulic model study of water intake under frazil ice conditions is presented. The intake, located 9 m below the surface of the St. Lawrence River in Massena, New York,has a through flow of 0.14 m^3/s. The model study, conducted in the refrigerated flume facility of the U.S. Army Cold Regions Research and Engineering Laboratory, investigated methods of minimizing the frazil ice blockage on the intake. Two protective structures were modeled and the relative benefits of each are presented. The additional cross-sectional area provided by the protective structures lowered the vertical velocity component of the intake water to 0.0027 m/s. At this velocity the buoyant force acting on the frazil ice particle is larger than the downward drag force, causing the particle to rise. The results demonstrate that under certain low flow conditions a protective structure can minimize frazil ice blockage problems.
    Type of Medium: Series available for loan
    Pages: 11 Seiten , Illustrationen
    Series Statement: CRREL Report 81-03
    Language: English
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  • 92
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    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-81/2
    In: CRREL Report, 81-2
    Description / Table of Contents: Abstract: Many hyperbolic reflections have been observed on marine seismic records obtained during oil exploration in the Beaufort Sea, and on USGS seismic sub-bottom profiles from the Prudhoe Bay vicinity. A hyperbolic projection system was designed to rapidly measure seismic velocities from the curves on the records. The velocities observed were approximately the velocity of sound in water. The hyperbolic signals also showed dispersion properties similar to acoustic normal modes in shallow water. These observations indicate that the signals responsible for the hyperbolic reflections propagate as normal modes within the water layer, with very limited penetration of the seabed. Determinations of the dominant frequency of these signals indicate that the penetration into the seabed has a characteristic attenuation depth (skin depth) of about 1.5 m for the sub-bottom profiles and 12 m for the marine records. It therefore appears that some hyperbolic reflections may be generated by variations in materials that occur near the seabed. There is some evidence of linearity of the anomalies, possibly related to sediment-filled or open ice gouges, or other changes in material properties at shallow depths.
    Type of Medium: Series available for loan
    Pages: iv, 16 Seiten , Illustrationen
    Series Statement: CRREL Report 81-2
    Language: English
    Note: CONTENTS Abstract Preface Introduction Methods of analysis Marine seismic records Seismic sub-bottom profiles Results and discussion Distribution of hyperbolic reflections Hyperbolas on oil exploration records Hyperbolas on sub-bottom profiles Conclusions Literature cited Appendix A: Hyperbola projector
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  • 93
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-81/5
    In: CRREL Report, 81-5
    Type of Medium: Series available for loan
    Pages: 27 Seiten , Illustrationen
    Series Statement: CRREL Report 81-5
    Language: English
    Note: CONTENTS Abstract Preface Introduction Test setup Test results The USCGC Mackinaw The Roger Slough The Cason J. Callaway The imperial St. Clair Vibration levels Discussion Frequency content Magnitude Mode of transmission Opening the channel Flexural waves Duration and occurrence of maximum vibrations Effect of weather Conclusions and recommendations Literature cited
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  • 94
    Call number: ZSP-201-81/6
    In: CRREL Report, 81-6
    Description / Table of Contents: Abstract: A procedure is described for monitoring the microfracturing activity in ice plates subjected to constant loads. Sample time records of freshwater ice plate deflections as well as corresponding total acoustic emission activities are presented. The linear elastic, as well as viscoelastic, response for a simply supported rectangular ice plate is given. Suggested future work using the above procedure is discussed.
    Type of Medium: Series available for loan
    Pages: iv, 19 Seiten , Illustrationen
    Series Statement: CRREL Report 81-6
    Language: English
    Note: CONTENTS Abstract Preface Notation Introduction Experimental procedure and considerations Growth of the ice plate Support of the ice plate Acoustic emission monitoring system Displacement transducers and data recording Mechanical loading System Analysis Experimental results Thin section analysis Summary and discussion Literature cited Appendix A : Ice plate linear elastic response Appendix B: Acoustic emission system sensitivity Appendix C: Ice plate linear viscoelastic response Appendix D: Equipment list
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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-201-81/10
    In: CRREL Report, 81-10
    Description / Table of Contents: Abstract: This treatise thoroughly reviews the subjects of density, thermal expansion and compressibility of ice; snow density change attributed to destructive, constructive and melt metamorphism; and the physics of regelation and the effects on penetration rate of both the thermal properties of the wire and stress level. Heat capacity, latent heat of fusion and thermal conductivity of ice and snow over a wide range of temperatures were analyzed with regression techniques. In the case of snow, the effect of density was also evaluated. The contribution of vapor diffusion to heat transfer through snow under both natural and forced convective conditions was assessed. Expressions representing specific and latent heat of sea ice in terms of sea ice salinity and temperature were given. Theoretical models were given that can predict the thermal conductivities of fresh bubbly ice and sea ice in terms of salinity, temperature and fractional air content.
    Type of Medium: Series available for loan
    Pages: 27 Seiten , Illustrationen
    Series Statement: CRREL Report 81-10
    Language: English
    Note: CONTENTS Abstract Preface Nomenclature Introduction Density, thermal expansion and compressibility of ice Density Thermal expansion Compressibility Density changes in snow Compaction Destructive metamorphism Constructive metamorphism Melt metamorphism Regelation Thermal properties of snow and fresh-water ice Heat capacity of snow and ice Latent heat Thermal conductivity of ice Thermal conductivity of snow Effective thermal diffusivity Heat transfer by water vapor diffusion in snow Heat and vapor transfer with forced convection Thermal properties of sea ice Specific heat of sea ice Heat of fusion of sea ice when 0° 〉 θ 〉 -8.2°C Density and thermal conductivity of sea ice Composition and air bubble content of sea ice above -8.2°C Thermal conductivity model for sea ice Thermal diffusivity of sea ice Method of determining thermal diffusivity Summary Literature cited
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  • 96
    Monograph available for loan
    Monograph available for loan
    Washington : Special Committee for Solar-Terrestrial Physics (SCOSTEP), National Academy of Sciences
    Call number: MOP 43858/3 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 132 Seiten , 28 cm
    Language: English
    Location: MOP - must be ordered
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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-201-81/27
    In: CRREL Report, 81-27
    Description / Table of Contents: Existing classifications for deposits in the glacial environment are inadequate and inconsistent. Deposits should be classified both descriptively and genetically; adequate descriptive classifications already exist. A major problem for previous genetic classifications has been that glacial deposition and the resulting deposits' properties were poorly understood. On the basis of three criteria-sediment source, uniqueness to the glacial environment, and preservation of glacier-derived properties-deposits in the glacial environment result from either of two groups of processes: primary or secondary. Primary processes release the debris of the glacier directly and form deposits that may bear properties related to the glacier and its mechanics. Their deposits are classified genetically as till and are the only deposits indicative of glaciation. In contrast, secondary processes mobilize, rework, transport and resediment debris and deposits in the glacial environment. They develop new, nonglacial properties in their deposits, while destroying or substantially modifying glacier-derived properties. Interpretation of their properties may provide information on the depositional are classified genetically according to the depositional process just as they are in other sedimentary environments. This genetic classification differs from previous classifications in that not all diamictons deposited in the glacial environment are classified as till; it is based strictly on process-related criteria. The origin of properties of glacial deposits in relation to the glacier's mechanics and environment must be recognized if the mechanisms and depositional processes of former glaciers are to be precisely understood.
    Type of Medium: Series available for loan
    Pages: iii, 16 Seiten , Illustrationen
    Series Statement: CRREL Report 81-27
    Language: English
    Note: CONTENTS Abstract Preface Introduction Criteria for process grouping Depositional processes Deposit groups-tills and nontills Comparison of melt-out and sediment flow Melt-out Sediment flow Classification of glacial deposits Conclusions Literature cited
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  • 98
    Call number: MOP 44845 / Mitte
    Type of Medium: Series available for loan
    Pages: [186] Seiten , Illustrationen , 28 cm
    Language: English
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  • 99
    Series available for loan
    Series available for loan
    Boulder, Colo. : The Geological Society of America
    Associated volumes
    Call number: S 90.0095(180)
    In: Special paper / The Geological Society of America, 180
    Type of Medium: Series available for loan
    Pages: 211 Seiten , Illustrationen, graphische Darstellungen
    ISBN: 0-8137-2180-6
    Series Statement: Special paper / The Geological Society of America 180
    Language: English
    Note: Introduction / Charles E. Chapin and Wolfgang E. Elston References cited Ash-flow magmatism / Robert L. Smith Abstract Introduction Volumes of ash-flow sheets Size of magma chambers Zoned magma chambers Crater Lake, Oregon Bandelier Tuff, New Mexico SiO₂ and phenocryst variation in ash-flow sheets Periodicity-volume-composition relationships Discussion of model Summary and conclusions Acknowledgments References cited Cooling units and composite sheets in relation to caldera structure / Robert L. Christiansen Abstract Introduction Examples of ash-flow-caldera relations Mazama eruption and Crater Lake caldera Bandelier Tuff and Valles-Toledo calderas Thirsty Canyon Tuff and Black Mountain caldera Timber Mountain-Oasis Valley caldera complex Yellowstone Plateau volcanic field General pattern of ash-flow-caldera relations Acknowledgments References cited The Bishop Tuff: Evidence for the origin of compositional zonation in silicic magma chambers / Wes Hildreth Abstract Introduction Eruptive sequence Major units Units of uncertain correlation Summary of eruptive sequence Eruptive temperatures Accuracy and precision of T-fₒ₂ data Mineralogy Fe-Ti oxides Quartz Sanidine Plagioclase Biotite Pyroxenes Allanite Zircon Apatite Pyrrhotite Whole-rock chemistry Major elements Trace elements Compositional gaps Origin of the compositional zonation Crystal settling Assimilation Basaltic underplating Liquid immiscibility Progressive partial melting Trace elements during partial melting Convection-driven thermogravitational diffusion Lines of evidence Concluding remarks Acknowledgments References cited Rare-earth-element content of some highly differentiated ash-flow tuffs and lavas / Donald C. Noble, Ward L. Rigot, and Harry R. Bowman Abstract Introduction Specimens studied and methods of chemical analysis Results and discussion Acknowledgments References cited Geochemistry of the Los Chocoyos Ash, Quezaltenango Valley, Guatemala / William I. Rose, Jr., Norman K. Grant, and John Easter Abstract Introduction Field description Geochemistry Mineralogy and mineral chemistry Sr-isotope data Modeling of crystal fractionation Time required for crystal fractionation Conclusions Acknowledgments Appendix 1. Analytical methods References cited Geochemical correlation of genetically related rhyolitic ash-flow and air-fall ashes, central and western Guatemala and the equatorial Pacific / Gregory A. Hahn, William I. Rose, Jr., and Thomas Meyers Abstract Introduction Previous investigations of chemical fingerprinting The Los Chocoyos Ash and the stratigraphic sequence of the San Cristobal Group Characteristics of the ash-flow member Sample acquisition and preparation Trace-element analyses Chemical correlation Lateral chemical variations Source of the Los Chocoyos Ash Age of the Los Chocoyos Ash Conclusions Acknowledgments References cited Ignimbrites of the Sierra Madre Occidental and their relation to the tectonic history of western Mexico / Fred W. McDowell and Stephen E. Clabaugh Abstract Introduction Volcanic stratigraphy of the Sierra Madre Occidental Pre-Cretaceous volcanic rocks Lower volcanic complex Unconformity between the igneous sequences Upper volcanic supergroup Calderas of the upper volcanic supergroup Structure of the Sierra Madre Occidental Chemistry Tectonic relationships Acknowledgments References cited Emplacement of pyroclastic flows: A review / Michael F. Sheridan Abstract Introduction Eruptions Observed pyroclastic flows Theoretical eruption models Mobility Topographic barriers Energy line Deposits Morphology Depositional sequence Textures Large clasts Deflation Compositional variation Welded peralkaline ignimbrites Emplacement temperatures Models Fluidization Speculation Summary Acknowledgments References cited Primary and secondary flow structures in ash-flow tuffs of the Gribbles Run paleovalley, central Colorado / Charles E. Chapin and Gary R. Lowell Abstract Introduction Paleovalleys and the Wall Mountain Tuff Primary flow structures Gas cavities (lenticules) Lineation Foliation Primary folds Rotated lithic fragments Imbricated crystals Secondary now structures Secondary folds and growth faults Tension cracks Miscellaneous structures Steam spiracles Conclusions Acknowledgments References cited Welded air-fall tuffs / R.S.J. Sparks and J. V. Wright Abstract Introduction Field relationships Santorini, Greece The 1875 Askja welded tuffs, Iceland Other examples Petrology and chemistry Grain-size studies Santorini welded tuffs Askja welded tuff Compaction and welding Strain, bulk density, and porosity measurements Results for Santorini welded tuffs Results for Askja welded tuff Discussion Acknowledgments References cited Globule ignimbrite of Mount Suswa, Kenya / R. L. Hay, W. Hildreth, and R. N. Lambe Abstract Introduction Scope and purpose of study Geologic setting and previous work Description and field relationships Ignimbrite petrography Vitric materials Crystals and rock fragments Devitrification and gas-phase crystallization Low-temperature alteration Nature of lower ignimbrite sheet Nature of the magma Chemical composition Temperature and viscosity Emplacement of ignimbrite and origin of globules Acknowledgments References cited A model of pyroclastic surge / K. H. Wohletz and M. F. Sheridan Abstract Introduction Terminology Objectives and methods of study Deposits Bed forms Locations Results Pyroclastic-surge facies Discussion and conclusions Development of bed forms Reconstruction of the surge cloud A model of pyroclastic surge: Its fluidization and deflation Acknowledgments References cited Significance of the flattening of pumice fragments in ash-flow tuffs / Donald W. Peterson Abstract Introduction Pumice fragments in the Apache Leap Tuff Recognition and description of pumice fragments Flattening of the pumice Applications of the flattening studies Recognition of cooling units Implications of extreme flattening Determination of stratigraphic level and fault displacement Commercial application of flattening ratios Determination of the degree of welding Pumice flattening as a possible guide to relative temperature of emplacement and rate of accumulation Conclusions Acknowledgments References cited Ash-flow sheets and calderas: Their genetic relationship to ore deposits in Nevada / Edwin H. McKee Abstract Introduction Metal deposits in volcanic-tectonic systems Resurgent cauldrons Geologic setting Parameters of study Distribution of mines and ash-flow sheets Distribution of mines and calderas Discussion Acknowledgments References cited
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  • 100
    Monograph available for loan
    Monograph available for loan
    San Francisco : Freeman
    Call number: MR 22.94937
    Type of Medium: Monograph available for loan
    Pages: XI, 677 Seiten , Illustrationen, graphische Darstellungen
    ISBN: 0-7167-1129-X
    Series Statement: A series of books in geology
    Language: English
    Note: Preface Part I DETAILED DESCRIPTION OF COMMON ROCK-FORMING MINERALS CHAPTER 1 Minerals Without Complex Anions NATIVE ELEMENTS Diamond C Sulfur S SULFIDES Sphalerite ZnS Pyrite FeS₂ HALIDES Halite NaCl Sylvite KCl Fluorite CaF₂ Carnallite KMgCl₃ · 6H₂O Cryolite Na₃AlF₆ OXIDES Periclase MgO Rutile TiO₂ Anatase TiO₂ Brookite TiO₂ Cassiterite SnO₂ Corundum Al₂O₃ Hematite Fe₂O₃ Ilmenite FeTiO₃ Perovskite CaTiO₃ THE SPINEL GROUP The Spinel Series (Mg,Fe²⁺ ,Zn,Mn)Al₂O₄ The Chromite Series (Fe²⁺,Mg)Cr₂O₄ The Magnetite Series (Fe²⁺,Mg,Zn,Mn,Ni)Fe₂³⁺ O₄ Chrysoberyl BeAl₂O₄ HYDROXIDES Brucite Mg(OH)₂ Gibbsite Al(OH)₃ The Diaspore-Boehmite Series α-AlO(OH)-γ-AlO(OH) The Goethite-Lepidocrocite Series α-FeO(OH)-γ-FeO(OH) Limonite FeO(OH) · nH₂O CHAPTER 2 Minerals With Complex Anions (Excluding Silicates) CARBONATES Calcite CaCO₃ Magnesite MgCO₃ Siderite FeCO₃ Rhodochrosite MnCO₃ Smithsonite ZnCO₃ The Dolomite-Ankerite Series CaMg(CO₃)₂-Ca(Mg,Fe)(CO₃)₂ Aragonite CaCO₃ Strontianite SrCO₃ Witherite BaCO₃ Cerussite PbCO₃ Malachite Cu₂(OH)₂CO₃ Azurite Cu₃(OH₂)(CO₃)₂ PHOSPHATES Xenotime YPO₄ Monazite (Ce,La,Th)PO₄ Amblygonite LiAl(PO₄)F The Lithiophilite-Triphylite Series Li(Mn,Fe)PO₄ Apatite Ca₅(PO₄)₃(F,OH,Cl) Wavellite Al₃(OH₃)(PO₄)₂ · 5H₂O SULFATES Anhydrite CaSO₄ Gypsum CaSO₄ · 2H2O Barite BaSO₄ Celestite SrSO₄ Anglesite PbSO₄ Alunite KAl₃(SO₄)₂(OH)₆ Jarosite KFe₃(SO₄)₂(OH)₆ BORATES Borax Na₂B₄O₇ · 10H₂O Colemanite Ca₂B₆O₁₁ · 5H₂O The Ludwigite-Vonsenite Series (Mg,Fe²⁺)₂Fe³⁺BO₃ · O₂ CHAPTER 3 The Nesosilicates THE OLIVINE GROUP The Forsterite-Fayalite Series (Mg, Fe)₂SiO₄ The Tephroite-Fayalite Series (Mn, Fe)₂SiO₄ Monticellite CaMgSiO₄ THE GARNET GROUP Pyralspite Garnets (Mg,Fe²⁺,Mn)₃Al₂(SiO₄)₃ Ugrandite Garnets Ca₃(Al,Fe³⁺,Cr)₂(SiO₄)₃ ALUMINOSILICATES Andalusite Al₂SiO₅ Kyanite Al₂SiO₅ Sillimanite Al₂SiO₅ Topaz Al₂SiO₄(F,OH)₂ Mullite 3Al₂O₃ · 2SiO₂ - 2Al₂O₃ · SiO₂ OTHER NESOSILICATES Dumortierite (Al,Fe³⁺)-O₃(BO₃)(SiO₄)₃ Zircon ZrSiO₄ Sphene CaTiSiO₅ Datolite CaB(SiO₄)OH Staurolite Fe₂²⁺Al₋₉O₆(SiO₄)₄(OH)₋₂ Sapphirine (Mg,Fe²⁺)₂Al₄O₆(SiO₄) Chloritoid (Fe²⁺,Mg,Mn)₂(Al,Fe³⁺)AI₃O₂(SiO₄)₂(OH)₄ The Humite Group nMg₂SiO₄Mg₁₋ₓTiₓ(OH,F)₂₋₂ₓO₂ (x 〈 1) CHAPTER 4 Sorosilicates and Cyclosilicates THE EPIDOTE GROUP The Clinozoisite-Epidote Series Ca₂(Al,Fe³⁺)₃O · SiO4 · Si₂O₇ · OH Zoisite Ca₂Al₃O · SiO₄ · Si₂O₇ · OH Piemontite Ca₂(Al,Fe³⁺,Mn³⁺)₃O · SiO₄ · Si₂O₇ · OH Allanite (Ca,Ce,La)₂(Al,Fe³⁺,Fe²⁺)₃O · SiO₄ · Si₂O₇ · OH Pumpellyite Ca₂Al₂(Mg,Fe²⁺,Fe³⁺,Al)(SiO₄)(Si₂O₇)(OH)₂(H₂O,OH) Lawsonite CaAl₂Si₂O₇(OH)₂ · H₂O THE MELILITE GROUP The Gehlenite-Akermanite Series (Ca,Na)₂(Mg,Al)(Si,Al)₂O₇ OTHER SOROSILICATES Idocrase Ca₁₀(Mg,Fe²⁺)₂Al₄(Si₂O₇)₂(SiO₄)₅(OH,F)₄ Hemimorphite Zn₄Si₂O₇(OH)₂ · H₂O CYCLOSILICATES Beryl Be₃Al₂(SiO₃)₆ Cordierite Mg₂Al₃(Si₅Al)O₁₈ Tourmaline Na(Mg,Fe,Li.Al)₃Al₆(Si₆O₁₈)(BO₃)₃(OH,F)₄ Axinite (Ca,Fe²⁺,Mn)₃Al₂BO₃(SiO₃)₄OH CHAPTER 5 Inosilicates THE PYROXENE GROUP The Enstatite-Orthoferrosilite Series Mg₂(SiO₃)₂-Fe₂(SiO₃)₂ The Diopside-Hedenbergite Series CaMg(SiO₃)₂-CaFe(SiO₃)₂ Pigeonite (Mg,Fe²⁺,Ca)(Mg,Fe²⁺)(SiO₃)₂ Augite (Ca,Mg,Fe²⁺,Na)(Mg,Fe²⁺,Fe³⁺,Al,Ti,Cr)(Si,Al)₂O₆ The Aegirine to Aegirine-Augite Series NaFe³⁺(SiO₃)₂-(Na,Ca)(Fe³⁺,Fe²⁺,Mg,Al)(SiO₃)₂ Jadeite NaAl(SiO₃)₂ Omphacite (Ca,Na)(Mg,Fe²⁺,Fe³⁺,Al)(SiO₃)₂ Spodumene LiAl(SiO₃)₂ THE PYROXENOID GROUP Wollastonite CaSiO₃ Rhodonite (Mn,Ca)SiO₃ Pectolite Ca₂NaH(SiO₃)₃ THE AMPHIBOLE GROUP Anthophyllite (Mg,Fe²⁺)₇(Si₄O₁₁)₂(OH)₂ The Cummingtonite-Grunerite Series (Mg,Fe²⁺)₇(Si₄O₁₁)₂(OH)₂ The Tremolite-Actinolite Series Ca₂(Mg,Fe²⁺)₅(Si₄O₁₁)₂(OH)₂ The Hornblende Series ("Common" Hornblende) Ca₂(Mg,Fe²⁺)₄(Al,Fe³⁺)(Si₇Al)O₂₂(OH)₂ Oxyhornblende (Basaltic Hornblende) Ca₂Na(Mg,Fe²⁺,Fe³⁺,Al,Ti)₅[(Si₃Al)O₁₁]₂(OH)₂ The Glaucophane-Crossite-Riebeckite Series Na₂(Mg,Fe²⁺)₃(Al,Fe³⁺)₂(Si₄O₂₂)₂(OH)₂ Katophorite Na(Na,Ca)(Mg,Fe²⁺)₄Fe³⁺(Si₇Al)O₂₂(OH)₂ The Arfvedsonite-Eckermannite Series Na(Na₁.₅,Ca₀.₅)(Fe²⁺,Mg)₄Fe³⁺(Si₇.₅Al₀.₅)O₂₂(OH)₂ Barkevikite (Na,K)Ca₂(Fe²⁺,Mg,Fe³⁺,Mn)₅(Si₇Al )O₂₂(OH)₂ CHAPTER 6 Phyllosilicates THE CLAYS The Kaolin (Kandite) Group Al₂Si₂O₅(OH)₄ The Montmorillonite (Smectite) Group (1/2Ca,Na)₀.₆₇(Al,Mg,Fe)₄₋₆(Si.Al)₈O₂₀(OH)₄ · nH₂O The Illite Group (K,Na,H₃O)₁₋₂Al₄(Si₇₋₆Al₁₋₂)O₂₀(OH)₄ Glauconite (K,H₃O)₂(Fe³⁺,Al,Fe²⁺,Mg)₄(Si₇₋₇.₅Al₁₋₀.₅O₂₀(OH)₄ Vermiculit (Mg,Ca)[(Mg,Fe²⁺)₅(Fe³⁺,Al)](Si₅AI₃)O₂₀(OH)₄ · 8H₂O The Palygorskite-Sepiolite Series (Mg,Al,Fe³⁺)₈Si₁₂O₃₀(OH)₄(OH₂)₄ · 8H₂O THE MICA GROUP Muscovite KAl₂(Si₃Al)O₁₀(OH)₂ Biotite K₂(Mg,Fe²⁺)₆₋₅Al₀₋₁(Si₆₋₅Al₂₋₃)O₂₀(OH,F)₄ Lepidolite K₂(Li₄₋₂Al₂₋₃)(Si₈₋₆Al₀₋₂)O₂₀(OH,F)₄ Zinnwaldite K₂(Fe₁₋₂²⁺Li₂₋₃Al₂)(Si₆₋₇Al₂₋₁)O₂₀(F,OH)₄ Brittle micas Ca₂(Al.Mg)₄(Al,Si)₈O₂₀(OH)₄ THE CHLORITE GROUP The Amesite-Antigorite Series (Mg,Al)₆(Si,Al)₄O₁₀(OH)₈ The Pseudothuringite-Brunsvigite Series (Fe,Al)₆(Si,Al)₄O₁₀(OH)₈ The Klementite-Delessite Series (Mg,Fe³⁺)₆(Si,Al)₄O₁₀(OH)₈ The Thuringite-Strigovite Series (Fe²⁺,Fe³⁺)₆(Si,Al)₄O₁₀(OH)₈ OTHER PHYLLOSILICATES Serpentine Mg₃Si₂O₅(OH)₄ Talc Mg₃Si₄O₁₀(OH)₂ Pyrophyllite Al₂Si₄O₁₀(OH)₂ Stilpnomelane (K,Na,Ca)₀₋₁(Fe³⁺,Fe²⁺,Mg,Mn,Al)₂(O,OH,H₂O)₆₋₇(Fe³⁺,Fe²⁺,Mg,Mn,Al)₅₋₆(Si₈O₂₀)(OH)₄ Prehnite Ca₂Al(AlSi₃)O₁₀(OH)₂ Apophyllite KCa₄(Si₄O₁₀)₂F · 8H₂O CHAPTER 7 Tektosilicates SILICA α-Quartz SiO₂ β-Quartz SiO₂ α-Tridymite SiO₂ α-Cristobalite SiO₂ Chalcedony SiO₂ Opal SiO₂ · nH₂O NATURAL GLASSES FELDSPARS Alkali Feldspars The Sanidine-High Albite Series (K,Na)AlSi₃O₈ The Orthoclase-Low Albite Series (K,Na)AlSi₃O₈ The Microline-Low Albite Series (K,Na)AlSi₃O₈ Plagioclase Feldspars Plagioclase (NaSi,CaAl)AlSi₂O₈ Barium Feldspar The Celsian-Orthoclase Series (BaAl,KSi)AlSi₂O₈ THE FELDSPATHOID GROUP Nepheline Na₃KAl₄Si₄O₁₆ Leucite KAlSi₂O₆ The Sodalite Group Na₈Al₆Si₆O₂₄Cl₂ Cancrinite (Ca,Na)₇₋₈(AlSiO₄)₆(CO₃,SO₄,Cl)₁₋₂ · 1-5H₂O THE ZEOLITE GROUP Analcime Na(AlSi₂)O₆H₂O Natrolite Na₂(AlSi₃)O₁₀ · 2H₂O Mesolite Na₂Ca₂[(Al₂Si₃)O₁₀]₃ · 8H₂O Scolecite Ca(Al₂Si₃)O₁₀ · 3H₂O Thomsonite NaCa₂[(Al,Si)₅O₁₀]₂ · 6H₂O Gonnardite Na₂Ca[(Al,Si)₅O₁₀]₂ · 6H₂O Mordenite (Na₂,K₂,Ca)(Al₂Si₁₀)O₂₄ · 7H₂O Laumontite Ca(Al₂Si₄)O₁₂ · 4H₂O Edingtonite Ba(Al₂Si₃)O₁₀ · 4H₂O Heulandite (Ca,Na₂)(Al₂Si₇)O₁₈ · 6H₂O Stilbite (Ca,Na₂,K₂)(Al₂Si₇)O₁₈ · 7H₂O Phillipsite (Ca,K₂,Na₂)₆[(Al₃Si)₅O₁₆]₂ · 12H₂O Harmotome Ba(Al₂Si₆)O₁₆ · 6H₂O Chabazite Ca(Al₂Si₄)O₁₂ · 6H₂O Gmelinite (Na₂,Ca)(Al₂Si₄)O₁₂ · 6H₂O OTHER TEKTOSILICATES Scapolite (Ca,Na)₄[(Al,Si)₃Al₃Si₆O₂₄](Cl,CO₃) Petalite Li(AlSi₄)O₁₀ Part II Optical and physical constants of the nonopaque minerals Isotropic Minerals Uniaxial Positive Minerals Uniaxial Negative Minerals Biaxial Positive Minerals Biaxial Negative Minerals Index
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