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  • 1
    Call number: MOP S 8484
    Description / Table of Contents: Die Redaktion der Zeitschrift "Ugol" hatte im Juli 1958 zu einer Diskussion über Fragen der Entwicklung der Gebirgsdrucktheorie aufgerufen. Diese Diskussion, die auf Grund einer Arbeit von K. V. Ruppenejt ausgelöst wurde, hat ein breites Echo unter den sowjetischen Gebirgsdruckforschern hervorgerufen. In einer kurzen Einleitung bemerkte damals die Redaktion, daß trotz der vielen Forschungen und Veröffentlichungen die Theorie der Entstehung und Auswirkung des Gebirgsdruckes noch schwach entwickelt sei. K. V. Ruppenejt hat nun 1957 gemeinsam mit anderen Mitarbeitern des WUGI (Unionsforschungsinstitut Kohle, jetzt Bergbauinstitut der Akademie der Wissenschaften der UdSSR) eine analytische Methode der Bestimmung der Verschiebungen des Hangenden und des Druckes auf den Ausbau in Abbauen der flachen Lagerung vorgeschlagen, deren Inhalt zweifelsohne eine breite Diskussion lohnt, ungeachtet dessen, ob die Grundtendenzen anerkannt werden können oder nicht. Die Hauptergebnisse dieser Forschungsarbeit wurden 1958 auf der Internationalen Gebirgsdrucktagung in Leipzig von K. V. Ruppenejt und A. D. Panov dargelegt. Im folgenden kann man sich deshalb darauf beschränken, ergänzende Erläuterungen zu dieser Arbeit und die nach ihrer Veröffentlichung erfolgte Diskussion, die im Januar 1960 abgeschlossen wurde, zu geben.
    Type of Medium: Series available for loan
    Pages: 55 Seiten
    Edition: Sonderdruck
    Series Statement: Montanwissenschaftliche Literaturberichte. Abteilung A - Bergbau 2. Beiheft
    Language: German
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  • 2
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-83/11
    In: CRREL Report, 83-11
    Description / Table of Contents: Investigations of ground radar performance over thawed and seasonally frozen silts, and sands and gravels containing artificial and natural reflectors were carried out in Alaska. The radar emitted 5-10 ns pulses, the center frequency of which was approximately 150 MHz. The artificial reflectors were metal sheets and discs and the natural reflectors were the groundwater table and interfaces between frozen and thawed material. The water table was profiled at three sites where the subsurface material was coarse-grained alluvium. Dielectric constants of 16 to 18 were measured for the thawed silts, 6 to 7 for the frozen silts and 3 to 9 for the sands and gravels. Signal penetration in the thawed high moisture content silts may be achieved only by use of a lower frequency radar, whereas in the sands and gravels greater depths may be detected with more sophisticated signal processing.
    Type of Medium: Series available for loan
    Pages: 16 Seiten , Illustrationen
    Series Statement: CRREL Report 83-11
    Language: English
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  • 3
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-83/17
    In: CRREL Report, 83-17
    Description / Table of Contents: A sea ice model was applied to the East Greenland Sea to examine a 60-day ice advance period beginning 1 October 1979. This investigation compares model results using driving geostrophic wind fields derived from three sources. Winds calculated from sea-level pressures obtained from the National Weather Service's operational analysis system resulted in strong velocities concentrated in a narrow band adjacent to the Greenland coast, with moderate velocities elsewhere. The model showed excessive ice transport and thickness build-ups in the coastal region. The extreme pressure gradient parallel to the coast resulted partially from a pressure reduction procedure that was applied to the terrain-following sigma coordinate system to obtain sea-level pressures. Additional sea-level pressure fields were obtained from an independent optimal interpolation analysis that merged FGGE buoys drifting in the Arctic basin with high latitude land stations and from manual digitization of the NWS hand-analyzed Northern Hemisphere Surface Charts. Modeling results using winds from both of these fields agreed favorably.
    Type of Medium: Series available for loan
    Pages: 19 Seiten , Illustrationen
    Series Statement: CRREL Report 83-17
    Language: English
    Note: CONTENTS Abstract Preface Introduction Description of study Model results The problem Conclusions Literature cited
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  • 4
    Call number: ZSP-201-83/24
    In: CRREL Report, 83-24
    Description / Table of Contents: Secondary recovery of oil at Prudhoe Bay, Alaska, will involve transporting large quantities of seawater in elevated pipelines across tundra for injection into oil-bearing rock strata. The possibility of a pipeline rupture raises questions concerning the effects of seawater on tundra vegetation and soils. To evaluate the relative sensitivities of different plant communities to seawater, eight sites representing the range of vegetation types along the pipeline route were treated with single, saturating applications of seawater during the summer of 1980. Within a month of the treatment 30 of 37 taxa of shrubs and forbs in the experimental plots developed clear symptoms of stress, while none of the 14 graminoid taxa showed apparent adverse affects. Live vascular plant cover was thus reduced by 89 and 91% in the two dry sites and by 54, 74 and 83% in the three moist sites, respectively. Live(green) bryophyte cover was markedly reduced in the moist experimental sites in 1981. Bryophytes in all but one of the wet-site experimental plots were apparently unaffected by the seawater treatment. Two species of foliose lichens treated with seawater showed marked deterioration in 1981. All other lichen taxa were apparently unaffected by the seawater treatment. The absorption and retention of salts by the soil is inversely related to the soil moisture regime. In the wet sites, conductivities approached prespill levels within about 30 days. In such sites, spills at the experimental volumes are quickly diluted and the salts flushed from the soil. In the dry sites, on the other hand, salts are retained in the soil, apparently concentrating at or near the seasonal thaw line.
    Type of Medium: Series available for loan
    Pages: 43 Seiten , Illustrationen
    Series Statement: CRREL Report 83-24
    Language: English
    Note: CONTENTS Abstract Preface Introduction Methods Site selection and preparation Prespill assessment Seawater application Postspill assessment Enzyme assay and analysis of soil flora Results and discussion Soil-solution conductivities Vascular plant response Cryptogam response Site factors and plant response Soil flora and extracellular soil enzymes Limitations of this study Summary and conclusions Literature cited Appendix: Plant taxa included in this study
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  • 5
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-83/29
    In: CRREL Report, 83-29
    Description / Table of Contents: A literature review indicated that the effects or permafrost on streambank erodibility and stability are not yet understood because systematic and quantitative measurements are seriously lacking. Consequently, general controversy exists as to whether perennially frozen ground inhibits lateral erosion and bankline recession, or whether it increases bank recession rates. Perennially frozen streambanks erode because of modification of the bank's thermal regime by exposure to air and water, and because of various erosional processes. Factors that determine rates and locations of erosion include physical, thermal and structural properties of bank sediments, stream hydraulics and climate. Thermal and physical modification of streambanks may also induce accelerated erosion within permafrost terrain removed from the immediate river environment. Bankline or bluffline recession rates are highly variable, ranging from less than 1 m/year to over 30 m/year and, exceptionally, to over 60 m/year. Long-term observations of the physical and thermal erosion processes and systematic ground surveys and measurements of bankline-bluffline recession rates are needed.
    Type of Medium: Series available for loan
    Pages: iv, 26 Seiten , Illustrationen
    Series Statement: CRREL Report 83-29
    Language: English
    Note: CONTENTS Abstract Preface Introduction Stream bank erosional processes Permafrost and related factors Permafrost and erosion General Erosional processes Bank zone processes Bluff zone processes Factors affecting perm afrost erodibility Exposure to currents and wind waves Texture and stratigraphy Ice content, distribution and type Slope aspect Coriolis force Timing and depth of thaw Water level and temperature Vegetation Ice and snow cover Groundwater Rates and timing of erosion and recession Overall effects of permafrost Recommendations for research Literature cited Appendix A : Processes of stream bank modifications
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  • 6
    Monograph available for loan
    Monograph available for loan
    München : Selbstverlag
    Call number: MOP 46297 / Mitte
    Description / Table of Contents: Die erste zusammenfassende Darstellung internationaler Forschungsergebnisse und Erfahrungen über alle Erscheinungsformen und Wirkungsarten des Blitzes, angefangen vom Altertum bis in die Gegenwart, ferner über den Blitzschutz und über Grundlagen für Versuche zur Gewinnung der Luftelektrizität und Blitzenergie.
    Type of Medium: Monograph available for loan
    Pages: mit 158 Abbildungen, 21 Tabellen, 5 Verzeichnissen und 454 Literaturstellen auf 228 Seiten
    Language: German
    Location: MOP - must be ordered
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  • 7
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-83/4
    In: CRREL Report, 83-4
    Description / Table of Contents: Measurements and analysis of seasonal ice growth and decay on Post Pond, New Hampshire, for the period 1973-1982 are presented. Observations included ice thickness measurements, examination of the various ice types contributing to the ice cover, and measurements of meteorological parameters for correlation with and modeling of the ice growth process. The overall nature of ice growth and decay (ice loss) on the Post Pond has been ascertained, the seasonal variability in the timing of freeze-up and ice-out and the duration of the ice cover have been determined, and the relationship of ice growth to freezing-degree-day (deg C) records evaluated on the basis of a Stefan conduction equation modified to deal with ice sheets covered with or free of snow. Ice growth occurs predominantly by the direct freezing of lake water, but snow ice may compose as much as 50% of the ice cover in winters with higher than average snowfall. Freeze-up leading to the establishment of a stable ice cover occurs during the 4-week period from the end of November to the end of December. Maximum seasonal ice thicknesses were from 45 to 67 cm and are generally attained during the first two weeks of March; ice-out, marking the final disappearance of ice from Post Pond, usually occurs by the third week of April. The overall rate of the ice loss is three to four times that of ice growth, and is dominated initially by melting from the top. As much as 50% of the ice may be lost in this way before the onset of any bottom melting. Final dissipation of the ice cover is usually expedited by candling resulting from preferential melting and disintegration of the ice at crystal boundaries.
    Type of Medium: Series available for loan
    Pages: iv, 30 Seiten , Illustrationen
    Series Statement: CRREL Report 83-4
    Language: English
    Note: CONTENTS Abstract Preface Introduction Location of study Study methods Ice thickness Ice-cover composition Surface air temperatures Freeze-up and ice-out characteristics Results and discussion Ice-growth record Freezing-degree-day records Ice-growth predictions Summary and conclusions Literature cited Appendix A: Ice-growth records Appendix B: Measured and computed ice-growth curves
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  • 8
    Call number: AWI A3-20-93434
    In: Meteorologische Abhandlungen / Institut für Meteorologie und Geophysik der Freien Universität Berlin, Band XXXII, Heft 1
    Type of Medium: Series available for loan
    Pages: 121 Seiten , Illustrationen
    Series Statement: Meteorologische Abhandlungen / Institut für Meteorologie und Geophysik der Freien Universität Berlin 32,1
    Language: German
    Note: Zugleich: Dissertation, Freie Unversität Berlin, [ca. 1963] , INHALTSVERZEICHNIS PROBLEMSTELLUNG UND ZIELSETZUNG 1. BEMERKUNGEN ZUM BEOBACHTUNGSGELÄNDE UND ZUM BEOBACHTUNGSMATERIAL 1.1 Das Beobachtungsgelände 1.2 Das Beobachtungsmaterial 2. HOMOGENITÄTSBETRACHTUNGEN 2.1 Temperatur 2.2 Niederschlag 2.3 Wind 2.4 Sonnenschein und Bewölkung 3. TEMPERATURVERHÄLTNISSE 3.1 Monats- und Jahreswerte 3.2 Tageswerte 3.3 Pentadenwerte 3.4 Häufigkeitsbetrachtungen 3.5 Interdiurne Veränderlichkeit 3.6 Der tägliche Gang 3.7 Vorkommen bestimmter Schwellenwerte 3.71 Frost- und Eistage 3.72 Sommer- und Tropentage 4. DER WASSERGEHALT DER LUFT 4.1 Monats- und Jahreswerte 4.2 Tageswerte 4.3 Häufigkeitsbetrachtungen 4.4 Interdiurne Veränderlichkeit 4.5 Der tägliche Gang 5. BEWÖLKUNGSVERHÄLTNISSE 5.1 Monats- und Jahreswerte 5.2 Tageswerte 5.3 Häufigkeitsbetrachtungen 5.4 Der tägliche Gang 5.5 Heitere und trübe Tage 5.6 Nebel 6. SONNENSCHEIN 6.1 Monats- und Jahreswerte 6.2 Tageswerte 6.3 Der tägliche Gang 7. NIEDERSCHLAGSVERHÄLTNISSE 7.1 Monats- und Jahreswerte 7.2 Niederschlagsbereitschaft 7.3 Tageswerte 7.4 Der tägliche Gang 7.5 Häufigkeitsbetrachtungen 7.6 Niederschlags- und Trockenperioden 7.7 Niederschlag und Wind· 7.8 Schneeverhältnisse 7.81 Schneefall und Schneedecke 7.82 Schneehöhe 7.9 Gewitter 8. WINDVERHÄLTNISSE 8.1 Windrichtung 8.2 Windgeschwindigkeit 8.21 Der jährliche Gang 8.22 Häufigkeitsbetrachtungen 8.23 Sturmtage und Windstillen 8.24 Der tägliche Gang 9.ZUSAMMENFASSUNG VERZEICHNIS DER TEXTTABELLEN VERZEICHNIS DER ABBILDUNGEN LITERATURVERZEICHNIS TABELLENANHANG
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  • 9
    Series available for loan
    Series available for loan
    Wilmette, Ill. : Snow Ice and Permafrost Research Establishment, Corps of Engineers, U.S. Army
    Associated volumes
    Call number: ZSP-202-53
    In: Research report / Cold Regions Research and Engineering Laboratory, 53
    Description / Table of Contents: Summary: The results of investigations on the structural changes of Greenland snow during age-hardening in the first 49 hr after ejection by a Peter snow miller from a trench 4.7 ft deep are reported, and the method of study is described. The samples of snow were taken at various distances from the trench 1, 3, 14, 25, and 49 hr after deposition, and their changes were studied as a function of time and distance from the trench. The porosity remained constant at an average of 50 ± 3%. The number of grains/cm^2 decreased with time and increased with distance from the trench because of the different speeds of sedimentation and wind sifting. The mean grain cross-section showed a similar dependence. The relative length of grain boundaries increased with time and slightly with distance from the trench, while the mean length of new grain-to-grain boundaries increased with age and decreased with distance from the trench. The mean number of adjacent grains per grain vs. relative length of grain boundaries showed a linear relation. A slight increase of new boundaries with increasing number of neighbors was also observed. Suggestions for a precise study of the age-hardening process of snow are made.
    Type of Medium: Series available for loan
    Pages: v, 15, A5 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 53
    Language: English
    Note: CONTENTS Preface Summary Methods of testing Sampling Preparation of samples Preparation of structure pictures Results Influence of time and place Porosity Number of grains/cm2 Mean grain cross section Relative length of grain boundaries (KM ratio) Mean number of adjacent grains per grain Number of new boundaries/cm 2 Mean length of new grain-to-grain boundaries Some interrelations of the structure data Structure of a 1-yr old Peter snow Suggestions for an exact study of the age-hardening process of snow References Appendix: Structure pictures
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  • 10
    Journal available for loan
    Journal available for loan
    Washington, D.C. : National Aeronautics and Space Administration
    Call number: MOP 47316 / Mitte
    Type of Medium: Journal available for loan
    Pages: 83 Seiten
    Language: English
    Location: MOP - must be ordered
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  • 11
    Series available for loan
    Series available for loan
    Wilmette, Ill. : Snow Ice and Permafrost Research Establishment, Corps of Engineers, U.S. Army
    Associated volumes
    Call number: ZSP-202-63
    In: Research report / Cold Regions Research and Engineering Laboratory, 63
    Description / Table of Contents: Summary: Experiments have been carried out on the plastic deformation of thick-walled snow-ice cylinders under hydrostatic pressure as a function of pressure and temperature. At constant circumferential stress and temperature the natural strain rate of closure is a constant. This constant varies with the circumferential stress according to a sine function and is exponentially dependent on temperature with an energy of activation of 14.1 kcal/mole at an average circumferential stress of 3.1 kg/cm^2. The mechanism of the plastic flow is in agreement with a mechanism proposed previously, that is, flow between grain boundaries takes place.
    Type of Medium: Series available for loan
    Pages: iv, 7 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 63
    Language: English
    Note: CONTENTS Preface Summary Experimental Materials Apparatus Experimental results Deformation under constant hydrostatic pressure Deformation as a function of hydrostatic pressure Deformation as a function of temperature at constant pressure Discussion References
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  • 12
    Series available for loan
    Series available for loan
    Wilmette, Ill. : Snow Ice and Permafrost Research Establishment, Corps of Engineers, U.S. Army
    Associated volumes
    Call number: ZSP-202-64
    In: Research report / Cold Regions Research and Engineering Laboratory, 64
    Description / Table of Contents: Summary: The distribution of temperature throughout an idealized ice cap is studied. The idealized ice cap is considered as one with a constant growth rate, without internal movement, subject to a linear climatic change and to a constant geothermal influx. The problem is treated as a Stefan-type problem and the solution is obtained by the principle of superposition. The results indicate that the temperature at the base of the ice cap rises with time and eventually would reach the melting point of the ice. Under such conditions, it is concluded that the ice cap is not resting on a permafrost base as suggested by previous investigation.
    Type of Medium: Series available for loan
    Pages: iv, 8 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 64
    Language: English
    Note: CONTENTS Preface Summary Introduction Mathematical development Method of solution Discussion of results Base temperature Minimum temperature Effect of rate of growth Effect of geothermal influx Comparison with observed results References
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  • 13
    Series available for loan
    Series available for loan
    Wilmette, Ill. : Snow Ice and Permafrost Research Establishment, Corps of Engineers, U.S. Army
    Associated volumes
    Call number: ZSP-202-67
    In: Research report / Cold Regions Research and Engineering Laboratory, 67
    Description / Table of Contents: Summary: The temperature distribution in snow subjected to gamma radiation from an operating nuclear reactor is analyzed mathematically, assuming that the effect of radiation is equivalent to a continuous heat source, the intensity of which is a function of the radial distance from the reactor. Steady-state solutions are derived for two cases: when the radial distance is 13 ft and when it is 19.1 ft. The results indicate that the temperature of the snow in certain regions in the several feet immediately below the foundation will exceed the design limit of 20°F. Increasing the shielding of the reactor will reduce the intensity of the radiation and snow temperature. Other possible ways to reduce the snow temperature include the use of refrigeration coils and the forcing of the atmospheric air through the snow.
    Type of Medium: Series available for loan
    Pages: iii, 4 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 67
    Language: English
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  • 14
    Monograph available for loan
    Monograph available for loan
    Dresden : Ingenieurschule für Geodäsie und Kartographie
    Associated volumes
    Call number: MOP 47524 / Mitte
    In: Meteorologische Messtechnik
    Type of Medium: Monograph available for loan
    Pages: 50 Seiten
    Series Statement: Meteorologische Messtechnik
    Language: German
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  • 15
    Series available for loan
    Series available for loan
    Moscow : Academy of Sciences of the USSR, Soviet Committee on Antarctic Research
    Associated volumes
    Call number: MOP 46294/A / Mitte
    In: USSR national report to SCAR, No. 25
    Type of Medium: Series available for loan
    Series Statement: USSR national report to SCAR 25
    Language: English
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  • 16
    Series available for loan
    Series available for loan
    Wilmette, Ill. : Snow Ice and Permafrost Research Establishment, Corps of Engineers, U.S. Army
    Associated volumes
    Call number: ZSP-202-69
    In: Research report / Cold Regions Research and Engineering Laboratory, 69
    Description / Table of Contents: Summary: The relations between rate of snow accumulation, snow density, snow age, and depth below the surface are formulated in terms of a compactive viscosity factor, which is assumed to be a function of only density and temperature, with parameters which will vary with the snow-type sequences of different climatic areas of high polar glaciers. The theory could be useful in an analysis of the data obtained from the large number of snow pits in Greenland, Ellesmere Island,and Antarctica.
    Type of Medium: Series available for loan
    Pages: iv, 8 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 69
    Language: English
    Note: CONTENTS Preface Summary Introduction The Sorge depth-density curve Generalization for time-variable rate of accumulation Path of a particle on the surface y=B(h,t) Effect of temperature Computational procedure Densification under high loads References
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  • 17
    Series available for loan
    Series available for loan
    Wilmette, Ill. : Snow Ice and Permafrost Research Establishment, Corps of Engineers, U.S. Army
    Associated volumes
    Call number: ZSP-202-66
    In: Research report / Cold Regions Research and Engineering Laboratory, 66
    Description / Table of Contents: Summary: A simple theory is proposed for crack formation and development by soil desiccation on the basis of laboratory experiments utilizing soil samples (Bloomington till) with max particle size of 1 mm diam. held in flat wooden containers. The crack pattern is more dependent on the thickness of the soil sample than on temperature or humidity. Some effect is caused also by differences in the bottom material of the containers. The area of cells made by crack patterns has a log normal size distribution. Total length of cracks decreases with increase in sample thickness. The number of sides of cells also depends on the thickness. Cracking was found to begin from the center of the soil layer and to propagate to the surface or bottom with non-uniform speed.
    Type of Medium: Series available for loan
    Pages: vi, 48, A4 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 66
    Language: English
    Note: CONTENTS Preface Summary Introduction Soil material Soil Preparation of the soil material Containers Temperature and humidity of the air Moisture content and dry density of the soil Experimental procedures and results General procedures Definition of the characteristics of cracking of soil Cracking moisture content Size of cells made by cracking of the soil Length of cracks Number of sides of cells Development of cracks Additional experiments Interfacial fracture markings Method of auxilliary tests on physical properties of the soil Elastic constants of the soil Shrinkage of soil due to desiccation Tests of the adhesion between the soil and the bottom material Results of auxiliary tests Elastic constants of the soil Free shrinkage process of the soil due to desiccation Adhesion between the soil and glass or wood Mechanism of crack formation due to the desiccation of soil Geometric interpretation Mechanical interpretation Conclusions References Appendix: Table of experiments
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  • 18
    Call number: MOP 46292/A / Mitte
    In: United Kingdom Antarctic research report, 1983
    Type of Medium: Series available for loan
    Series Statement: United Kingdom Antarctic research report 1983
    Language: English
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  • 19
    Call number: AWI Bio-21-94346
    In: Bibliotheca diatomologica, 3
    Type of Medium: Monograph available for loan
    Pages: 386 Seiten
    ISBN: 3768213757
    Series Statement: Bibliotheca diatomologica 3
    Language: English
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  • 20
    Monograph available for loan
    Monograph available for loan
    Leningrad : Gidrometeoizdat
    Call number: AWI A4-19-92407
    Type of Medium: Monograph available for loan
    Pages: 127 Seiten , Illustrationen
    Language: Russian
    Note: In kyrillischer Schrift
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  • 21
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-83/18
    In: CRREL Report, 83-18
    Description / Table of Contents: An evaluation of an impulse radar system for detecting cavities under concrete pavement is discussed, and field results are presented. It was found that a dual antenna mode of surveying was ideal for void detection. In this mode one antenna operated in a transceive mode and a second, offset from the first, operated in a receive-only mode. This arrangement allowed a refraction-type profile survey to be performed, which enabled subpavement voids to be easily detected. Field trails were held at Plattsburgh Air Force Base, where 28 cavities were detected and mapped. Drilling of holes verified that a cavity existed and allowed cavity depth to be measured. The cavities varied from 1.5 in. to 23 in, depth and were up to 20 ft. long.
    Type of Medium: Series available for loan
    Pages: 49 Seiten , Illustrationen
    Series Statement: CRREL Report 83-18
    Language: English
    Note: CONTENTS Abstract Preface Introduction Plattsburgh Air Force Base Radar sounding system Survey procedure Cavity inspection Radar cavity detection test Radar profile results Falling-weight deflectometer tests Discussion and conclusions Literature cited
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  • 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-201-83/13
    In: CRREL Report, 83-13
    Description / Table of Contents: A review on past experimental and theoretical work indicates a need for additional experimentation to characterize the response of snow to inelastic pressure waves. Pressure data from previously conducted explosion tests are analyzed to estimate the elastic limit of snow of 400 -kg/cu m density to be about 36 kPa. This pressure corresponds to a scaled distance of 1.6 m/cu.rt.kg for charges fired beneath the surface of the snow, and to a scaled distance of 1.2 m/cu.rt.kg for charges fired in the air. The effects of a snow cover on the method of clearing a minefield by using an explosive charge fired in the air above the snow surface are also discussed and recommendations are given for further work in this area. Explosive pressure data are used to estimate the maximum effective scaled radius for detonating buried mines at shallow depth to be 0.8 m/cu.rt.kg. Fuel-air explosive will increase this effective radius significantly because of the increase in the size of the source region.
    Type of Medium: Series available for loan
    Pages: 33 Seiten , Illustrationen
    Series Statement: CRREL Report 83-13
    Language: English
    Note: CONTENTS Abstract Preface List of symbols Introduction Objectives Background Problems in describing the response of snow to an applied stress Methods of determining the dynamic behavior of materials Review of previous studies on snow Experimental measurements on snow Summary of snow experiments Theoretical studies Confirmation of the theory Discussion Applications Recommendations Summary Literature cited Appendix A. Selected data from Wisotski and Snyder (1966) Appendix B. Pressure data from Livingston (1964)
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  • 23
    Call number: ZSP-980-70
    In: 2nd Working Meeting "Radioisotope Application and Radiation Processing in Industry", Part 2, 50 to 97
    In: ZfI-Mitteilungen, Nr. 70
    Type of Medium: Series available for loan
    Pages: 355 Seiten , Illustrationen
    ISSN: 0323-8776
    Series Statement: ZfI-Mitteilungen 70
    Language: English
    Note: Contents of Part 2 Hecht, K. Gerber, R. Otto: Studies on the drying of paints by means of 14C-labelled compounds K. Wagner, F. Brutschin, I. Ritter, T. Gritsch, H. Zimmermann, H. Borchert: Investigations by the aid of radioisotope methods on the technology of the production of carbon and silicon carbide materials K. Gloe, P. Mühl: Determination of metal extraction process parameters using tracer technique W. Migdał, W. Łada, K. Malec-Czechowska: Studies on liquid-liquid extraction of noble metals using radiotracers L. Petryka, K. Przewłocki: Radiotracer investigations of benefication copper ore in the industrial flotation process Z. Bazaniak, J. Palige: Determination of Cu recovery degree from slags in shaft process by means of radiotracers R. Burek, J .K. Zurawicz: On the optimization of concentration measurements in heterogeneous materials based on β-backscatter measurements B. Heinrich: Analysis of carbon content in crude brown coal by inelastic scattering of neutrons and the method of time correlated associated particles P. Urbańaki, D. Wagner, M. Jankowska, E. Kowalska: Determination of calcium and iron and measurements of ash content in the brown coal H.-W. Thümmel: Some considerations relating to the prediction of the efficiency of radiometric methods for the continuous ash content determination of coal L. Wawrzonek: Monitor of ash content of coal with X-ray source I. Pavlicsek, V. Stenger, A. Veres: Apparatus for gamma activation analysis I. Végvári, I. Juhász: Determination of PbO content of lead-glass samples on the ground of gamma-absorption E. Schöntube, H.-J. Große: Aerosol ionization gas analysis as a monitoring for waste halothane in the atmosphere of operating theatre S. Mothes, P. Popp, G. Oppermann, W.-D. Herberg: Measurement of fluorocarbons with the ECD P. Popp, E. Schöntube, G. Oppermann: The usability of radiation ionization detectors for the determination of N2O concentrations in the air of operating theatres P. Popp, G. Arnold, G. Oppermann: A hydrocarbon-sensitized argon ionization detector for the detection of inorganic compounds R. Szepke, W. Lisieski, J. Harasimczuk: Automatic dust monitor AMIZ G. Vormum: Sealed sources - problems of design, measurement and quality control L. Gąsiorowski: New trends in developments of ratioisotope gauges in Poland G. Brunner: Direct chemical information from special radio tracers as well as from outer X-ray excitation J. Hirling: Experience and future trend in industrial application of nuclear methods in Hungary I. N. Ivanov, O. K. Nikolaenko, Yu. V. Phecktistov, V. L. Chulkin: Use of short-lived nuclides in activation analysis Kl.-P. Rudolph, J. Flachowsky, A. Lange: Trace element determination in semiconducter selenium by neutron activation analysis (NAA) W. Lisieski, J. Mirowicz: Some industrial applications of instruments with neutron sources R. Dybczyński, H. Maleszewaka, S. Sterliński, Z. Szopa, M. Wasek: Some problems in neutron activation determination of gold and silver in ores and concentrates of copper industry L. Jankowski: Cost-benefit aspects of radioisotope application in industry B. Manouchev, T. Boschkova, L. Tsankov, V. Gurev, I. Kojucharov, G. Grozev: On the possibilities of the direct gamma-spectremetry in natural waters P. Morgenstern, D. Müller, W. Riedel: A parallel grid proportional scintillation counter for the X-ray region from 3 to 20 keV with regard to high count rates N. A. Anders, V. S. Isaev, V. I. Filatov, B. E. Kolesnikov, D. Müller, P. Morgenstern, W. Riedel, V. P. Varvaritsa: X-ray fluroescence analyzer of light elements with proportional scintillation counter D. Müller, P. Morgenstern, W. Riedel, W. Warwariza, B. E. Kolesnikow, N. A. Anders, W. J. Filatov: General considerations concerning the use of the X-ray analyzer "RALE" in industry
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  • 24
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    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-83/9
    In: CRREL Report, 83-9
    Description / Table of Contents: Recent observations of shore ice pile-up and ride-up along the coast of the Alaska Beaufort Sea are presented. Information is given to show that sea ice movement on shore has overridden steep coastal bluffs and has thrust inland over 150 m, gouging into and pushing up mounds of beach sand, gravel, boulders and peat and, inland, the tundra material. The resulting ice scar morphology was found to remain for tens of years. Onshore ice movements up to 20 m are relatively common, but those over 100 m are very infrequent. Spring is a dangerous time, when sea ice melts away from the shore, allowing ice to move freely. Under this condition, driving stresses of less than 100 kPa can push thick sea ice onto the land.
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    Pages: v, 59 Seiten , Illustrationen
    Series Statement: CRREL Report 83-9
    Language: English
    Note: Contents Abstract Preface Introduction Winter 1979-80 observations Winter 1980-81 and summer 1981 observations Winter 1981-82 and summer 1982 observations Old ice ride-up features Discussion Literature cited Appendix A. The boulder rampart and rock littered shore west of Konganevik Pt. Appendix B. Site location maps
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  • 25
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    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-83/6
    In: CRREL Report, 83-6
    Description / Table of Contents: During the austral summers of 1976-77 and 1978-79, several ice cores were taken from the McMurdo Ice Shelf brine zone to investigate its thermal, physical and chemical properties. This brine zone consists of a series of super-imposed brine layers (waves) that originate at the seaward edge of the ice shelf and migrate at various rates, depending upon their age and position in the ice shelf. The brine in these layers becomes increasingly concentrated as the waves migrate inland through the permeable ice shelf firn. Chemical analyses of brine samples from the youngest (uppermost) brine wave show that it contains sea salts in normal seawater proportions. Further inland, deeper and older brine layers, though highly saline (S 〉 200 ‰), are severely depleted in SO2-4 with the SO2-4/Na+ ratio being an order of magnitude less than that of normal seawater. Analyses of Na+, K+, Ca2+, Mg2+, SO2-4 and CI-, together with solubility and temperature considerations, show that the sulfate depletion is due to selective precipitation of mirabilite, Na2SO4*10H2O. The location of the inland boundary of brine penetration is closely related to the depth at which the brine en-counters the firn/ice transition. However, a small but measurable migration of brine is still occurring in otherwise impermeable ice; this is attributed to eutectic dissolution of the ice by concentrated brine as it moves into deeper and warmer parts of the McMurdo Ice Shelf.
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    Pages: iii, 16 Seiten , Illustrationen
    Series Statement: CRREL Report 83-6
    Language: English
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  • 26
    Call number: ZSP-201-83/7
    In: CRREL Report, 83-7
    Description / Table of Contents: Peak power generation with hydropower creates tailwater flow conditions characterized by high and low flows with abrupt transitions between these states. Flows occurring in tailwaters typically form sharp-fronted, large-amplitude waves of relatively short period. An understanding of the mechanics of downstream propagation of these waves is important both for direct application in studies of the tailwater and because of the similarity of these waves to those following a dam break. An analysis of the dynamic equations of open channel flow is used to quantify the relative importance of flow wave convection, diffusion and dispersion in rivers. The relative importance of each process is re­lated to the relative magnitude of terms in the dynamic equations, providing a physical basis for model formulation. A one-dimensional diffusion wave flow routing model, modified for tailwaters, simulates the important physical pro­cesses affecting the flow and is straightforward to apply. The model is based upon a numerical solution of the kine­matic wave equation. The “modified equation,” Hirt, and von Neumann analyses are used to gain insight into the stability and dissipative and dispersive behavior of the numerical solution, and results of these analyses are compared. A set of linear routings is used to demonstrate the dissipative and dispersive behavior predicted by the analyses and to verify the accuracy of an expression that quantifies the numerical diffusion of the model. The analyses provide a basis for selection of numerical parameters for model applications. The capability and accuracy of the model are enhanced when physical wave diffusion is balanced by numerical diffusion in the model. Maintaining the diffusion balance re­quires that the time derivative weighting parameter 0 be variable and in some instances negative. Though some amount of phase error is introduced, negative 0 values have no adverse effect upon model stability. Field studies were con­ducted to demonstrate the benefits of careful model development and analysis, and to verify the diffusion wave model for rapidly varying tailwater flow. The bed slope and roughness characteristics of the field study reaches (below Apalachia and Norris Dams) differ greatly, spanning those of a large number of rivers of practical interest. The accurate simulation of flow in both of these tailwaters attests to the soundness of both the physical basis of the model and the numerical solution technique. The field studies confirm, for the extreme case of rapidly varying flow in a mildly sloped river, that inertia has a negligible effect upon unsteady flow waves at low Froude numbers. Additionally, these studies verify that diffusion of short-period waves in rivers is generally significant.
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    Pages: vi, 41 Seiten , Illustrationen
    Series Statement: CRREL Report 83-7
    Language: English
    Note: CONTENTS Abstract Preface Nomenclature Introduction Physical diffusion and dispersion in open channel flow Modeling approach Description of the diffusion wave flow routing model Analysis of the numerical model Modified equation and Hirt analyses of diffusion wave model von Neumann analysis of the diffusion wave model Linear case studies Accuracy considerations of the numerical solution Field studies Apalachia Dam tailwater Norris Dam tailwater Conclusions Literature cited
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  • 27
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    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
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    Call number: ZSP-201-83/5
    In: CRREL Report, 83-5
    Description / Table of Contents: This report presents the results of dynamic ice-structure interaction model tests conducted at the CRREL Ice Engineering Facility. A flexible, single-pile, bottom-founded offshore structure was simulated by a test pile with about a one-to-ten scale ratio. Urea (instead of sodium chloride) was used as dopant to scale down the ice properties, resulting in good model ice properties. Six ice fields were frozen and 18 tests carried out. In all cases distinctive dynamic ice structure interaction vibrations appeared, from which abundant data were collected. In tests with linear ice velocity sweep, sawtooth-shaped ice force fluctuations occurred first. With increasing velocity the natural modes of the test pile were excited, and shifts from one mode to another occurred. The maximum ice force values appeared mostly with low loading rates, but high forces appeared random'y at high ice velocities. As a general trend, ice force maximums, averages and standard deviations decreased with increasing ice velocities. The aspect ratio effect of the ice force in continuous crushing follows the same dependence as in static loadings. The frequency of observed ice forces is strongly dominated by the natural modes of the structure. Dynamically unstable natural modes tend to make the developing ice force frequencies the same as the natural frequencies. Otherwise the resulting frequency depends directly on structural stiffness and ice velocity and inversely on the ice force range. During vibrations the displacement rates of the structure overcome the velocity of ice, making low loading rates and hence high ice forces possible. During crushing, ice induces both positive and negative damping.
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    Pages: iv, 53 Seiten , Illustrationen
    Series Statement: CRREL Report 83-5
    Language: English
    Note: CONTENTS Abstract Preface Introduction Test arrangements Ice properties Crushing patterns Maximum ice force vs velocity Dynamic aspect ratio effect and crushing strength Measured ice force frequencies Calculated ice force frequencies Accelerations, velocities and displacements Damping Ice-induced negative damping Limit cycles Buckling load Conclusions Literature cited
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  • 28
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    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-83/16
    In: CRREL Report, 83-16
    Description / Table of Contents: The presence of snow on the ground can impose limitations on the mobility of wheeled and tracked vehicles. Snow depth and density are the two most easily measured snow properties that can be related to mobility over snow. Existing models of snowpack accumulation and ablation processes and models of internal snowpack structure were examined to determine if a model of the snowpack can be developed for use in predicting the snow parameters that affect mobility. Simple models, such as temperature index models, do not provide sufficient snowpack details, and the more detailed models require too many measured inputs. Components of the various models were selected from a basis of a snowpack model for predicting snow properties related to mobility over snow. Methods of obtaining the input data from some components are suggested, and areas where more development is needed are described.
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    Pages: 34 Seiten , Illustrationen
    Series Statement: CRREL Report 83-16
    Language: English
    Note: CONTENTS Abstract Preface Nomenclature Conversion of metric units Introduction Review of existing models Accumulation models Ablation models Using existing models for studying mobility Proposed snowpack model for mobility studies Model components Implementation of the model Developing input data Conclusions Literature cited
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  • 29
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    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
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    Call number: ZSP-201-83/23
    In: CRREL Report, 83-23
    Description / Table of Contents: The problems associated with measuring stresses in ice are reviewed. Theory and laboratory test results are then presented for a stiff cylindrical sensor made of steel that is designed to measure ice stresses in a biaxial stress field. Loading tests on freshwater and saline ice blocks containing the biaxial ice stress sensor indicate that the sensor has a resolution of 20 kPa and an accuracy of better than 15% under a variety of uniaxial and biaxial loading conditions. Principal stress directions can also be determined within 5 degrees. The biaxial ice stress sensor is not significantly affected by variations in the ice elastic modulus, ice creep or differential thermal expansion between the ice and gauge. The sensor also has a low temperature sensitivity (5 kPa/deg C).
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    Pages: 38 Seiten , Illustrationen
    Series Statement: CRREL Report 83-23
    Language: English
    Note: CONTENTS Abstract Preface Introduction Previous work Stress measurements Design considerations Stress sensors Biaxial ice stress sensor Biaxial stress sensor theory Gauge deformation Stresses associated with cylindrical sensors Determination of ice stresses Gauge calibration Evaluation of the biaxial ice stress sensor Temperature sensitivity Biaxial loading test equipment Biaxial loading test results Differential thermal expansion Long-term drift Discussion of test results Conclusions Literature cited
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  • 30
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    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
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    Call number: ZSP-201-83/26
    In: CRREL Report, 83-26
    Description / Table of Contents: Ice accreted on high-speed rotors operating in supercooled fog can be thrown off by centrifugal force, creating severe unbalance and dangerous projectiles. A simple force balance analysis indicates that the strength of accreted ice and its adhesive strength can be obtained by measuring the thickness of the accretion, the location of the separation, the rotor speed, and the density. Such an analysis was applied to field and laboratory observations of self-shedding events. The results agree reasonably well with other observations.
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    Pages: 13 Seiten , Illustrationen
    Series Statement: CRREL Report 83-26
    Language: English
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  • 31
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    Braunschweig : Vieweg & Sohn
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    Call number: MOP 41240 / Mitte
    In: Sammlung Vieweg, 96
    Type of Medium: Monograph available for loan
    Pages: 74 Seiten , Illustrationen
    Series Statement: Sammlung Vieweg 96
    Language: German
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  • 32
    Call number: AWI A3-20-93434-2
    In: Meteorologische Abhandlungen / Institut für Meteorologie und Geophysik der Freien Universität Berlin, Band XXXII, Heft 2
    Type of Medium: Series available for loan
    Pages: 218 Seiten , Illustrationen
    Series Statement: Meteorologische Abhandlungen / Institut für Meteorologie und Geophysik der Freien Universität Berlin 32,2
    Language: German
    Note: Zugleich: Dissertation, Freie Unversität Berlin, [ca. 1963] , INHALTSVERZEICHNIS PROBLEMSTELLUNG UND ZIELSETZUNG 1. BEMERKUNGEN ZUM BEOBACHTUNGSGELÄNDE UND ZUM BEOBACHTUNGSMATERIAL 1.1 Das Beobachtungsgelände 1.2 Das Beobachtungsmaterial 2. HOMOGENITÄTSBETRACHTUNGEN 2.1 Temperatur 2.2 Niederschlag 2.3 Wind 2.4 Sonnenschein und Bewölkung 3. TEMPERATURVERHÄLTNISSE 3.1 Monats- und Jahreswerte 3.2 Tageswerte 3.3 Pentadenwerte 3.4 Häufigkeitsbetrachtungen 3.5 Interdiurne Veränderlichkeit 3.6 Der tägliche Gang 3.7 Vorkommen bestimmter Schwellenwerte 3.71 Frost- und Eistage 3.72 Sommer- und Tropentage 4. DER WASSERGEHALT DER LUFT 4.1 Monats- und Jahreswerte 4.2 Tageswerte 4.3 Häufigkeitsbetrachtungen 4.4 Interdiurne Veränderlichkeit 4.5 Der tägliche Gang 5. BEWÖLKUNGSVERHÄLTNISSE 5.1 Monats- und Jahreswerte 5.2 Tageswerte 5.3 Häufigkeitsbetrachtungen 5.4 Der tägliche Gang 5.5 Heitere und trübe Tage 5.6 Nebel 6. SONNENSCHEIN 6.1 Monats- und Jahreswerte 6.2 Tageswerte 6.3 Der tägliche Gang 7. NIEDERSCHLAGSVERHÄLTNISSE 7.1 Monats- und Jahreswerte 7.2 Niederschlagsbereitschaft 7.3 Tageswerte 7.4 Der tägliche Gang 7.5 Häufigkeitsbetrachtungen 7.6 Niederschlags- und Trockenperioden 7.7 Niederschlag und Wind· 7.8 Schneeverhältnisse 7.81 Schneefall und Schneedecke 7.82 Schneehöhe 7.9 Gewitter 8. WINDVERHÄLTNISSE 8.1 Windrichtung 8.2 Windgeschwindigkeit 8.21 Der jährliche Gang 8.22 Häufigkeitsbetrachtungen 8.23 Sturmtage und Windstillen 8.24 Der tägliche Gang 9.ZUSAMMENFASSUNG VERZEICHNIS DER TEXTTABELLEN VERZEICHNIS DER ABBILDUNGEN LITERATURVERZEICHNIS TABELLENANHANG
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  • 33
    Call number: MOP 45384/4 / Mitte
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    Language: English
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  • 34
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    Wilmette, Ill. : Snow Ice and Permafrost Research Establishment, Corps of Engineers, U.S. Army
    Associated volumes
    Call number: ZSP-202-60
    In: Research report / Cold Regions Research and Engineering Laboratory, 60
    Description / Table of Contents: Summary: This report presents numerical results on the feasibility study of the use of in-ice cooling for a power plant. As a result of this type of arrangement, a water pond under ice is formed. The pond size as a function of time for various operating conditions has been computed. The associated problems such as water temperature, power consumption, etc., are also studied.
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    Pages: iv, 17, A6 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 60
    Language: English
    Note: CONTENTS Preface Summary Introduction Open-loop system Method of analysis Time dependence of pond size Temperature of water in the pond Effect of inlet water temperature Effect of convection duct Power consumption for circulation of cooling water Condlusions Closed-loop system Method of analysis Time dependence of pond size Flow conditions of glycol solutions inside coil Discussion and conclusions References Appendix: Examples of calculations
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  • 35
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    Wilmette, Ill. : Snow Ice and Permafrost Research Establishment, Corps of Engineers, U.S. Army
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    Call number: ZSP-202-61
    In: Research report / Cold Regions Research and Engineering Laboratory, 61
    Description / Table of Contents: Summary: The results of experiments on the bonding of polished and microtomed surfaces of bubble-free ice samples at -5°C with various loads are reported. Only a small part of the available surface area appeared to be bonded, this area increasing with the bonding load. Surfaces apposed immediately after preparation showed an appreciably higher force of separation than those joined after a time interval. The force of separation for surfaces placed together at 0% relative humidity was higher than that at 100% relative humidity. A simplified theory of bonding of irregular ice surfaces is formulated in the appendix. The calculations are based on the assumption of a distribution of small ice cylinders of equal cross sections but different heights located on a non-deformable plate. The cylinders are deformed by a constant force which is applied by another completely non-deformable flat plate. The deformation as a function of force and time and the force of separation as a function of load are derived, assuming that the distribution of heights is given by a box distribution (i.e., frequency of heights is constant).
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    Pages: iv, 6, A4 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 61
    Language: English
    Note: CONTENTS Preface Summary Introduction Materials Apparatus and procedure Results Discussion References Appendix: Compression of an assembly of cylinders
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  • 36
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    Wilmette, Ill. : Snow Ice and Permafrost Research Establishment, Corps of Engineers, U.S. Army
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    Call number: ZSP-202-62
    In: Research report / Cold Regions Research and Engineering Laboratory, 62
    Description / Table of Contents: Summary: Adhesive strength of ice for the systems ice/stainless steel and ice/optically flat fused quartz has been investigated as a function of surface roughness of steel surfaces and rates of shear for steel and quartz. The adhesive strength decreases with decreasing roughness of steel surfaces and the force vs time curves for smooth steel plates resemble those of two solids sliding over each other with a liquid layer sandwiched between them. This is particularly so in the case of quartz. The adhesive strength as a function of rate of shear is linear both for ice/stainless steel and ice/quartz; however, there are indications of yield values. The experimental results are in agreement with the assumption of a liquidlike layer on ice. Ratios of viscosity coefficient to the thickness of the layer have been evaluated for both systems and viscosity coefficients are estimated. The importance of interfacial free energy considerations is pointed out.
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    Pages: iii, 10 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 62
    Language: English
    Note: CONTENTS Preface Summary Introduction Experimental Materials Apparatus Experimental results Ice/metal interface Ice/quartz interface Discussion References
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  • 37
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    Dresden : Ingenieurschule für Geodäsie und Kartographie
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    Call number: MOP 47523/1 / Mitte
    In: Spezielles Lehrmaterial für die Aus- und Weiterbildung von Ingenieuren der Fachrichtung Meteorologie
    Type of Medium: Monograph available for loan
    Pages: 44 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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  • 38
    Call number: MOP 43551/1,2 / Mitte
    In: Quellentexte zur Witterungsgeschichte Europas von der Zeitenwende bis zum Jahr 1850, Band 1, Teil 2
    Type of Medium: Monograph available for loan
    Pages: 486 Seiten
    Series Statement: Quellensammlung zur Hydrographie und Meteorologie 1,2
    Language: German
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  • 39
    Call number: MOP 46593 / Mitte
    Type of Medium: Monograph available for loan
    Pages: iii, 372 Seiten , Illustrationen
    Language: English
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  • 40
    Dissertations
    Dissertations
    Lille : Université des Sciences et Techniques de Lille
    Call number: MOP 46577 / Mitte
    Description / Table of Contents: Réalisation d'un modèle climatique simple tenant compte des principaux processus d'échanges énergétiques (le transfert radiatif est traité en ondes courtes et en ondes longues) dans l'atmosphère et permettant de restituer à l'équilibre les propriétés du profil de température. Un schéma de génération de la nébulosité (la génération de l'épaisseur optique est faite en distinguant 3 étages de nuages) est couplé à la procédure d'ajustement convectif, pour tenir compte de la réponse de la couverture nuageuse. Tests de sensibilité à la constante solaire et à la couverture nuageuse. Attention particulière accordée à la sensibilité de la température et du bilan radiatif de surface à une augmentation de la concentration en CO2. Il serait intéressant de poursuivre le travail en incluant un schéma de dissipation indépendante des flux de chaleur latente et sensible, de façon à se libérer de la contrainte d'un gradient de température convectif.
    Type of Medium: Dissertations
    Pages: 158 Seiten , Illustrationen
    Language: French
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  • 41
    Call number: MOP 46293 / Mitte
    In: United States Antarctic Research Report to SCAR, No. 25
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    Series Statement: United States Antarctic Research Report to SCAR 25
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  • 42
    Call number: MOP 46292 / Mitte
    In: United Kingdom Antarctic research report, 1982
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    Series Statement: United Kingdom Antarctic research report 1982
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  • 43
    facet.materialart.12
    Oxford : Blackwell Scientific Publications
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    Call number: 10.1144/GSL.SP.1983.011.01.01
    In: Special publications / the Geological Society, London, Volume 11
    Description / Table of Contents: This volume contains papers presented at the Geological Society on March 25th and 26th 1981, plus three additional contributions by researchers who were unable to be present at the meeting. The meeting brought together earth scientists with interests in geomorphology, geochemistry, pedology, sedimentology and applied geology. The multidisciplinary approach to the study of residual deposits is reflected in the 25 chapters of this book, which are arranged in four main groups: Weathering processes (chapters 1-3); Kaolinites, laterites and bauxites (chapters 4-11); Red beds (chapters 12-14); Duricrusts: calcretes, silcretes and gypcretes (chapters 15-25). The last two chapters of the book deal with karst related fluorite-baryte deposits, and Cenozoic pedogenesis and landform develop- ment in south-east England. Richard Crockett, Andrew Goudie and Don Highley provided invaluable suggestions during the planning of the meeting that led to this book. R. C. L. WILSON,Department of Earth Sciences, The Open University, Walton Hall, Milton Keynes MK7 6AA.
    Type of Medium: 12
    Pages: 1 Online-Ressource (258 Seiten)
    ISBN: 063201072X
    Series Statement: Special publications / the Geological Society, London 11
    Language: English
    Note: Weathering Processes Lichen weathering of minerals: implications for pedogenesis M. J. Wilson D. Jones https://doi.org/10.1144/GSL.SP.1983.011.01.01 Porewater reactions in the unsaturated zone with special reference to groundwater quality in England D. A. Spears https://doi.org/10.1144/GSL.SP.1983.011.01.02 A review of experimental weathering of basic igneous rocks David C. Cawsey and Paul Mellon https://doi.org/10.1144/GSL.SP.1983.011.01.03 Kaolinites, Laterites and Bauxites Kaolinisation and the formation of silicified wood on late Jurassic Gondwana surfaces H. Wopfner https://doi.org/10.1144/GSL.SP.1983.011.01.04 Kaolinitic weathering profiles in Brittany: genesis and economic importance J. Esteoule-Choux https://doi.org/10.1144/GSL.SP.1983.011.01.05 The origin and occurrence of Devon Ball Clays A. Vincent https://doi.org/10.1144/GSL.SP.1983.011.01.06 The Ayrshire Bauxitic Clay: an allochthonous deposit? S. K. Monro F. C. Loughnan and M. C. Walker https://doi.org/10.1144/GSL.SP.1983.011.01.07 Base metal concentrations in kaolinised and silicified lavas of the Central Burma volcanics T. R. Marshall B. J. Amos D. Stephenson https://doi.org/10.1144/GSL.SP.1983.011.01.08 A low level laterite profile from Uganda and its relevance to the question of parent material influence on the chemical composition of laterites M. J. McFarlane https://doi.org/10.1144/GSL.SP.1983.011.01.09 Palaeoenvironment of lateritic bauxites with vertical and lateral differentiation Ida Valeton https://doi.org/10.1144/GSL.SP.1983.011.01.10 Geochemistry of a nickeliferous laterite profile, Liberdade, Brazil J. Esson https://doi.org/10.1144/GSL.SP.1983.011.01.11 Red Beds Reddening of tropical coastal dune sands R. Gardner https://doi.org/10.1144/GSL.SP.1983.011.01.12 Post-depositional reddening of late Quaternary coastal dune sands, north-eastern Australia K. Pye https://doi.org/10.1144/GSL.SP.1983.011.01.13 Origin of red beds in a moist tropical climate (Etruria Formation, Upper Carboniferous, UK) B. M. Besly P. Turner https://doi.org/10.1144/GSL.SP.1983.011.01.14 Duricrusts: Calcretes, Silcretes and Gypcretes Environment of silcrete formation: a comparison of examples from Australia and the Cologne Embayment, West Germany H. Wopfner https://doi.org/10.1144/GSL.SP.1983.011.01.15 Silcrete in Western Australia: geomorphological settings, textures, structures, and their genetic implications W. J. E. van de Graaff https://doi.org/10.1144/GSL.SP.1983.011.01.16 Geochemistry of weathering profile silcretes, southern Cape Province, South Africa M. A. Summerfield https://doi.org/10.1144/GSL.SP.1983.011.01.17 Pliocene channel calcrete and suspenparallel drainage in West Texas and New Mexico C. C. Reeves, Jr https://doi.org/10.1144/GSL.SP.1983.011.01.18 Concentration of uranium and vanadium in calcretes and gypcretes Donald Carlisle https://doi.org/10.1144/GSL.SP.1983.011.01.19 Ancient duricrusts and related rocks in perspective: a contribution from the Old Red Sandstone John Parnell https://doi.org/10.1144/GSL.SP.1983.011.01.20 A process-response model for the formation of pedogenic calcretes Colin F. Klappa https://doi.org/10.1144/GSL.SP.1983.011.01.21 Stable isotope abundances in calcretes A. S. Talma F. Netterberg https://doi.org/10.1144/GSL.SP.1983.011.01.22 A Geotechnical classification of calcretes and other pedocretes F. Netterberg J. H. Caiger https://doi.org/10.1144/GSL.SP.1983.011.01.23 Karstic residual fluorite-baryte deposits at two localities in Derbyshire R. P. Shaw https://doi.org/10.1144/GSL.SP.1983.011.01.24 Cenozoic pedogenesis and landform development in south-east England John A. Catt https://doi.org/10.1144/GSL.SP.1983.011.01.25
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  • 44
    Call number: AWI G3-24-95571-11
    In: Tektonika Sibiri, Tom 11
    Description / Table of Contents: Представлены материалы XIII сессии Научного совета по тектонике Сибири и Дальнего Востока (Якутск, 1980 г.). Подробно рассмотрены вопросы современного состояния теоретической геотектоники и закономерности формирования земной коры в докембрии и фанерозое. Приведены новые материалы по региональной тектонике платформенных и подвижных областей Сибири и Дальнего Востока СССР. Приведенные модели строения и эволюции земной коры с достаточной полнотой отражают современное состояние теоретической геотектоники. Сборник рассчитан на широкий круг геологов.
    Description / Table of Contents: Translation of the abstract: The materials of the XIII session of the Scientific Council on Tectonics of Siberia and the Far East (Yakutsk, 1980) are presented. The issues of the current state of theoretical geotectonics and the patterns of formation of the earth's crust in the Precambrian and Phanerozoic are considered in detail. New materials on the regional tectonics of platform and mobile regions of Siberia and the Far East of the USSR are presented. The presented models of the structure and evolution of the earth's crust sufficiently reflect the current state of theoretical geotectonics. The collection is intended for a wide range of geologists.
    Type of Medium: Monograph available for loan
    Pages: Seiten , Illustrationen
    Series Statement: Tektonika Sibiri / Akademija Nauk SSSR, Sibirskoe Otdelenie, Naučnyj Sovet po Tektonike Sibiri i Dalʹnego Vostoka Tom 11
    Language: Russian
    Note: СОДЕРЖАНИЕ Предисловие Теоретические вопросы геотектоники Некоторые методологические вопросы геологии / Ю. А. Косыгин Краткий методологический анализ современных глобальных тектонических гипотез / В. Ю. Забродин Главные этапы эволюции процесса рифтогенеза в истории Земли / Е. E. Милановский Закономерности формирования континентальной земной коры / М. С. Марков, Ю. М. Пущаровский Структурно-формационные парагенезы как индикаторы стадийности формирования континентальной коры / Б. М. Чиков Сдвиги и трансформные разломы литосферы / С. И. Шерман Структурная эволюция геосинклинальных складчатых систем / В. С. Буртмаи Механизм образования складчатости и ее морфология / А. В. Вихерт О формировании и локализации концентрических комплексов в связи с развитием разломов / Ю. А. Косыгин, В. В. Юшманов, Л. А. Маслов О тектонике и минерагении Восточной Сибири и Дальнего Востока / Л. И. Красный Становление земной коры в докембрии О процессах, образующих и преобразующих земную кору континентального типа / Ч. Б. Борукаев Закономерности формирования земной коры континентов в нижнем докембрии / М. А. Гилярова Особенности тектонического развития подвижных зон Гондваны и Евразии в позднем докембрии / Н. А. Божко Главные этапы становления континентальиой земной коры / В. И. Шульдинер Тентоника и этапы становления земной коры территории Янутии / Г. С. Гусев, Г. А. Гринберг, В. В. Ковальский, Б. В. Олейников, А. Ф. Петров, Г. С. Фрадкии, Н. В. Черский Модели строения и глубинной эволюции коры юго-востока Сибирской платформы / Л. П. Карсаков, Ю. Ф. Малышев Эволюция слоев земной коры в геологической истории архея Алданского щита / И. М. Фрумкин К проблеме пангеосинклинали / Р. Ф. Черкасов Этапы формирования земной коры Алданского щита в докембрии / Л. М. Реутов, А. Ф. Петров Этапы формирования земной коры и докембрийский рифтогенез на северо-востоке Сибирской платформы / Б. Р. Шпунт, Д. В. Аброскин, Ю. Х. Протопопов Этапы и факторы становления континентальной коры на территории Восточной Сибири / А. А. Бухаров К проблеме происхождения среднепротерозойских грабенов юго-востока Сибирской платформы и ее складчатого обрамления / А. А. Константиновский Тектоника платформенных областей Геоблоки Сибири и этапы их формирования / Е. П. Миронюк, И. А. Загрузииа Соотношение структурных этажей - критерий тектонического районироnания платформенных областей / К. И. Микуленко, В. С. Старосельцев, Г. С. Фрадкин Общая корреляция эндогенных процессов на Сибирской платформе / С. М. Замараев О мантийных абиссолитах и природе сводовых поднятий на древних платформах / П. Ф. Иванкин, А. А. Фельдман Становление земной коры молодых плит и ранние этапы их развития (на примере Западно-Сибирского сеrмента) / В. С. Бочкарев Тектоника подвижных областей Офиолитовые зоны палеозоид Казахстана и геодинамические реконструкции / Е. И. Паталаха Современная тектоника Байкальской рифтовой системы и концепция тектоники плит / В. П. Солоненко Современные представления о глубинном строении северо-восточноrо фланга Байкальской рифтовой зоны / М. М. Мандельбаум, И. П. Шпак Пространственно-временные связи и геодинамические соотношения мезозойских структур на Алданском щите и в Джугджуро-Становой области / В. Г. Ветлужских Офиолиты и олистостромы Верхояно-Колымской складчатой системы / Ю. В. Архипов, И. Г. Волкодав Литосферные плиты в Верхояно-Чукотской складчатой области / В. Б Спектор Структура и геодинамика Курило-Камчатскоrо желоба / Г. С. Гнибиденко, Т. Г. Быкова, О. В. Веселов, В. М. Воробьев, А. С. Сваричевский Литература , Translation of Contents Preface Theoretical issues of geotectonics Some methodological issues of geology / Yu. A. Kosygin Brief methodological analysis of modern global tectonic hypotheses / V. Yu. Zabrodin The main stages of the evolution of the rifting process in the history of the Earth / E. E. Milanovsky Patterns of formation of the continental crust / M. S. Markov, Yu. M. Pushcharovsky Structural-formational parageneses as indicators of the stages of formation of the continental crust / B. M. Chikov Shifts and transform faults of the lithosphere / S. I. Sherman Structural evolution of geosynclinal folded systems / V. S. Burtmai The mechanism of formation of folding and its morphology / A. V. Wikhert On the formation and localization of concentric complexes in connection with the development of faults / Yu. A. Kosygin, V. V. Yushmanov, L. A. Maslov On tectonics and minerageny of Eastern Siberia and the Far East / L. I. Krasny Formation of the earth's crust in the Precambrian On the processes that form and transform the earth's crust of continental type / Ch. B. Borukaev Patterns of formation of the continental crust in the Lower Precambrian / M. A. Gilyarova Features of the tectonic development of mobile zones of Gondwana and Eurasia in the Late Precambrian / N. A. Bozhko The main stages of the formation of the continental crust / V. I. Shuldiner Tentonics and stages of formation of the earth's crust in the territory of Janutia / G. S. Gusev, G. A. Grinberg, V. V. Kovalsky, B. V. Oleinikov, A. F. Petrov, G. S. Fradkii, N. V. Chersky Models of the structure and deep evolution of the crust of the southeast of the Siberian Platform / L. P. Karsakov, Yu. F. Malyshev Evolution of layers of the earth’s crust in the geological history of the Archean of the Aldan Shield / I. M. Frumkin On the problem of pangeosyncline / R. F. Cherkasov Stages of formation of the earth's crust of the Aldan shield in the Precambrian / L. M. Reutov, A. F. Petrov Stages of crust formation and Precambrian rifting in the northeast of the Siberian Platform / B. R. Shpunt, D. V. Abroskin, Yu. Kh. Protopopov Stages and factors of formation of the continental crust in Eastern Siberia / A. A. Bukharov On the problem of the origin of Middle Proterozoic grabens in the southeast of the Siberian Platform and its folded framing / A. A. Konstantinovsky Tectonics of platform areas Geoblocks of Siberia and stages of their formation / E. P. Mironyuk, I. A. Zagruzia The ratio of structural floors is a criterion for tectonic zoning of platform areas / K. I. Mikulenko, V. S. Staroseltsev, G. S. Fradkin General correlation of endogenous processes on the Siberian platform / S. M. Zamaraev On mantle abysolites and the nature of arched uplifts on ancient platforms / P. F. Ivankin, A. A. Feldman Formation of the earth's crust of young plates and early stages of their development (using the example of West Siberian cement) / V. S. Bochkarev Tectonics of mobile regions Ophiolite zones of the paleozoids of Kazakhstan and geodynamic reconstructions / E. I. Patalakha Modern tectonics of the Baikal rift system and the concept of plate tectonics / V. P. Solonenko Modern ideas about the deep structure of the northeast flank of the Baikal rift zone / M. M. Mandelbaum, I. P. Shpak Spatio-temporal connections and geodynamic relationships of Mesozoic structures on the Aldan shield and in the Dzhugdzhur-Stanovoy region / V. G. Vetluzhskikh Ophiolites and olistostromes of the Verkhoyansk-Kolyma fold system / Yu. V. Arkhipov, I. G. Volkodav Lithospheric plates in the Verkhoyansk-Chukotka folded region / V. B Spektor Structure and geodynamics of the Kuril-Kamchatka trench / G. S. Gnibidenko, T. G. Bykova, O. V. Veselov, V. M. Vorobyov, A. S. Svarichevsky Literature , In kyrillischer Schrift
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  • 45
    Call number: MOP 9642
    Type of Medium: Monograph available for loan
    Pages: 7 S.
    Series Statement: Ergebn. Met. Beob. Potsdam, 1928, S. V
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  • 46
    Monograph available for loan
    Monograph available for loan
    Elmer, NJ : C. W. Thornthwaite Associates, Laboratory of Climatology
    Associated volumes
    Call number: MOP 26658
    In: Publications in climatology
    Type of Medium: Monograph available for loan
    Pages: 97-154 S.
    Series Statement: Publications in climatology 13,2
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  • 47
    Call number: MOP 37988
    Type of Medium: Monograph available for loan
    Pages: 23 S.
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  • 48
    Monograph available for loan
    Monograph available for loan
    Tokyo : Geographical Institute University Tokyo
    Call number: MOP B 5685
    Type of Medium: Monograph available for loan
    Pages: 58 S.
    Series Statement: Science report Section C Geology of the Takyo Ky¯oiku Daigaku 7,64
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  • 49
    Monograph available for loan
    Monograph available for loan
    Leipzig : Teubner
    Associated volumes
    Call number: MOP 46066 / Mitte
    In: Mathematisch-naturwissenschaftliche Bibliothek
    Type of Medium: Monograph available for loan
    Pages: 276 S. : graph. Darst.
    Edition: 1. Aufl.
    Series Statement: Mathematisch-naturwissenschaftliche Bibliothek 62
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  • 50
    Series available for loan
    Series available for loan
    Oslo : Dybwad [in Komm.]
    Associated volumes
    Call number: ZSP-597-1,1
    In: Resultater av de Norske statsunderstøttede Spitsbergenekspeditioner
    Type of Medium: Series available for loan
    Pages: 104 S.
    Series Statement: Resultater av de Norske statsunderstøttede Spitsbergenekspeditioner 1,1
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  • 51
    Call number: MOP 46226 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 90 S.
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  • 52
    Monograph available for loan
    Monograph available for loan
    Associated volumes
    Call number: MOP 26274
    In: Meteorologičeskij ezegodnik
    Type of Medium: Monograph available for loan
    Pages: 292 S.
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  • 53
    Series available for loan
    Series available for loan
    Kingston : Antarctic Division, Department of Science
    Associated volumes
    Call number: ZSP-124-19
    In: ANARE research notes
    Description / Table of Contents: Invariant geomagnetic co-ordinates were calculated for points on a 5° x 5° grid over the earth, at altitudes of 105 km and 250 km. The calculation was based on the International Geomagnetic Reference Field (IGRF) for 1975, updated to 1977.25 to correspond approximately to the middle of the International Magnetosphere Survey period. Global charts of the invariant co-ordinates at 105 km altitude are presented. The invariant co-ordinates were expanded into a set of spherical harmonic co-efficients and FORTRAN subroutines are described which allow the rapid re-calculation of the invariant co-ordinates form the co-efficients.
    Type of Medium: Series available for loan
    Pages: iv, 44 S. : Kt. + 3 Kt.-Beil.
    ISBN: 0642874824
    Series Statement: ANARE research notes 19
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  • 54
    Call number: MOP Per 278(105)
    In: Meteorologische Beobachtungen von deutschen Feuerschiffen der Nordsee
    In: Einzelveröffentlichungen
    Type of Medium: Monograph available for loan
    Pages: 116 S.
    Series Statement: 105
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  • 55
    Call number: MOP Per 500/II
    Type of Medium: Monograph available for loan
    Former Title: Vorg. ---〉 [Deutsches meteorologisches Jahrbuch / Russische Zone / 2]
    Subsequent Title: Forts. ---〉 [Meteorologisches Jahrbuch der Deutschen Demokratischen Republik / 2]
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  • 56
    Monograph available for loan
    Monograph available for loan
    's-Gravenhage : Kgl. Nederlands Meteorologisch Instituut
    Call number: MOP 27020
    Type of Medium: Monograph available for loan
    Pages: 200 S. : graph. Darst.
    Series Statement: Rapport Deltacommissie 2 : Beschouwingen over stormvloeden en getijbeweging 1
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  • 57
    Call number: Per 287
    Parallel Title: 1933=408 von Deutschland 〈Deutsches Reich〉 / Reichsamt für Wetterdienst: Veröffentlichungen des Reichsamtes für Wetterdienst
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  • 58
    Series available for loan
    Series available for loan
    London : H.M.Stat.Off.
    Associated volumes
    Call number: ZSP-164-24
    In: Scientific reports
    Description / Table of Contents: Recent collections of decapod crustaceans and serpulid worms from the Upper Cretaceous of James Ross Island have facilitated the re-description of three species previously recorded from the area and have contributed four new species. The decapods include Hoploparia stokesi (Weller), Meyeria crofti sp. nov. and Callianassa meridionalis sp. nov., and the serpluids Rotularia callosa (Stoliczka), Rotularia shackletoni (Wilckens), Rotularia dorsolaevis sp. nov. and Ditrupa varicosa sp. nov. The diagnosis of the subfamily Homarinae Mertin, 1941 is amended and observations are made on the taxonomic position and stratigraphical range of the genus Meyeria. In addition, the structure of the tube-wall of the genera Rotularia Defrance, 1827 and Ditrupa Berkeley, 1832-34, and their stratigraphical range are discussed. The age of the fauna is shown by associated ammonites to be of Lower to Middle Campanian age.
    Type of Medium: Series available for loan
    Pages: 30 S., 7 Bl. : Ill., graph. Darst., Kt.
    Series Statement: Scientific reports / Falkland Islands Dependencies Survey 24
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  • 59
    facet.materialart.
    Unknown
    Berlin : Behrend ; 1890/91(1894); 1901(1905) - 1928(1930)
    Call number: Per 287/B
    Parallel Title: 1892 - 1900 ---〉 [Ergebnisse der magnetischen Beobachtungen in Potsdam und Seddin / 2]
    Parallel Title: 1892/1900 ---〉 [Ergebnisse der magnetischen Beobachtungen in Potsdam und Seddin / Ergänzungsband zu den Jahrgängen ...]
    Parallel Title: Zugl. einzelne Bd. von Preußisches Meteorologisches Institut 〈Berlin〉: Veröffentlichungen des Preussischen Meteorologischen Instituts
    Subsequent Title: Forts. ---〉 Ergebnisse der magnetischen Beobachtungen in Seddin
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  • 60
    Monograph available for loan
    Monograph available for loan
    Leipzig : Geest & Portig
    Associated volumes
    Call number: MOP 11146 ; MOP 34374
    In: Probleme der kosmischen Physik
    Type of Medium: Monograph available for loan
    Pages: VIII, 168 S. : Ill., graph. Darst.
    Series Statement: Probleme der kosmischen Physik 12
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  • 61
    Journal available for loan
    Journal available for loan
    Associated volumes
    In: Journal of Geology
    Type of Medium: Journal available for loan
    Pages: 733 S.
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  • 62
    facet.materialart.
    Unknown
    Moskva : Nauka ; Nachgewiesen [1.]1960/61,2 -
    Call number: ZSP-550
    ISSN: 0130-3686
    Language: Russian
    Note: Erscheinungsjahr in Vorlageform:1960- , Zählungssprung , In kyrill. Schr
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  • 63
    Call number: S 12.0222(73)
    In: Acta phytogeographica Suecica
    Type of Medium: Series available for loan
    Pages: 96 S. : Ill., graph. Darst., Kt.
    ISBN: 9172100737 , 91-7210-473-2
    Series Statement: Acta phytogeographica Suecica 73
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  • 64
    Monograph available for loan
    Monograph available for loan
    Prag
    Call number: MOP 26462
    Type of Medium: Monograph available for loan
    Pages: 76 S. : graph. Darst.
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  • 65
    Call number: MOP 25929
    Type of Medium: Monograph available for loan
    Pages: 30 S. : Ill.
    Note: Inhaltsverzeichnis: 1. Kurzreferat. - 2. Ausführlicher textlicher Bericht. - A.2.1 Bedeutung und Herkunft des Kohlendioxyds. - A.2.2 Lösungsweg. - A.2.3 Durchführung der Arbeit. - A.2.4 Ergebnisse der CO2-Bestimmungen. - B.2.1 Bedeutung und Herkunft der Schwefelspuren. - B.2.2 Methode. - B.2.4 Ergebnisse. - C.2.1 Herkunft und Bedeutung der Ammoniak- und Nitratspuren. - C.2.2 und C.2.3 Bestimmungsmethoden. - C.2.4 Ergebnisse. - 2.5 Vergleich der in Wahnsdorf gemessenen Werte mmit denen von Luftanalysen anderer europäischer Meßstellen. - 2.6 Zusammenfassung. - 3. Literaturverzeichnis. - 4. Verzeichnis der Abbildungen. - 5. Verzeichnis der Anlagen.
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  • 66
    Series available for loan
    Series available for loan
    Tokyo : National Institute of Polar Research
    Associated volumes
    Call number: ZSP-592-27
    In: Memoirs of National Institute of Polar Research
    Type of Medium: Series available for loan
    Pages: IV, 247 S. : Ill., graph. Darst.
    Series Statement: Memoirs of National Institute of Polar Research : Special issue 27
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  • 67
    Call number: MOP Per 867(20)
    In: Tropical Meteorology Research Programme report series
    Type of Medium: Monograph available for loan
    Pages: ii, 123 p.
    Series Statement: Tropical Meteorology Research Programme report series 20
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  • 68
    Call number: MOP Per 841(18)
    In: German Democratic Republic : national report : IAMAP
    Type of Medium: Monograph available for loan
    Pages: 29 S.
    Series Statement: German Democratic Republic : national report : IAMAP 18
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  • 69
    Call number: MOP 46433
    Type of Medium: Monograph available for loan
    Pages: div. S.
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  • 70
    facet.materialart.
    Unknown
    Bremerhaven ; 1.1981 - 5.1984; damit Ersch. eingest.
    Call number: ZSP-168/A
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  • 71
    Monograph available for loan
    Monograph available for loan
    Berlin : Forschungsinst. für Hydrometeorologie
    Call number: MOP 45853
    Type of Medium: Monograph available for loan
    Pages: 30 S.
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  • 72
    Monograph available for loan
    Monograph available for loan
    Cambridge [u.a.] : MIT Press
    Call number: PIK P 113-12-0325
    Description / Table of Contents: Contents: I The Electric Power Industry: Economic, Technical, and Institutional Background ; 1 Introduction ; 2 Current Industry Structure and Regulation ; 3 Organization, Integration, and Natural Monopoly ; 4 Technology of Electric Power Systems ; 5 Generation of Electricity ; 6 Distribution, Transmission, and Coordination ; 7 Economic Efficiency: Dimensions and Issues ; II Electric Utility Deregulation: Prospects, Problems, and Public Policy Alternatives ; 8 Scenarios for Deregulation ; 9 Contractual Relationships: Theoretical and Empirical Issues ; 10 Contractual Relationships for Wholesale Power Supply under Deregulation ; 11 Equilibrium Efficiency Analysis ; 12 Effectiveness of Competition ; 13 Transition Issues and Problems ; 14 Conclusions
    Type of Medium: Monograph available for loan
    Pages: XI, 269 S.
    ISBN: 9780262600187 , 0-262-60018-8
    Series Statement: MIT Press classic
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  • 73
    Call number: MOP Per 844(59) ; MOP Per 844(59, 2. Ex.)
    In: World Climate Programme
    Type of Medium: Monograph available for loan
    Pages: div. S.
    Series Statement: World Climate Programme 59
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  • 74
    Monograph available for loan
    Monograph available for loan
    Associated volumes
    Call number: MOP Per 746/A(4,1)
    In: Normales climatologiques 1951 - 1980
    Type of Medium: Monograph available for loan
    Pages: 431 S.
    Series Statement: 4,1
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  • 75
    Monograph available for loan
    Monograph available for loan
    Berlin : Akad.-Verl.
    Associated volumes
    Call number: MOP 27371
    In: Abhandlungen der Deutschen Akademie der Wissenschaften, Klasse für Mathematik, Physik und Technik
    Type of Medium: Monograph available for loan
    Pages: 42 S. : graph. Darst.
    Series Statement: Abhandlungen der Deutschen Akademie der Wissenschaften Klasse für Mathematik, Physik und Technik 1960, 9
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  • 76
    Call number: MOP Per 844(40)
    In: World Climate Programme
    Type of Medium: Monograph available for loan
    Pages: 31 S. : Ill.
    Series Statement: World Climate Programme 40
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  • 77
    Monograph available for loan
    Monograph available for loan
    Cambridge, Mass. : Smithsonian Institution, Astrophysical Observatory
    Call number: AWI G7-84-0784
    Type of Medium: Monograph available for loan
    Pages: Getr. Zählung
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  • 78
    Call number: AWI G7-83-1269
    Type of Medium: Monograph available for loan
    Pages: 119, [1] p. : ill.
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  • 79
    Call number: AWI E2-13-0068-3
    In: Materialy nabljudenij naučno-issledovatel'skich drejfujuščich stancij "Severnyj Poljus-6", "Severnyj Poljus-7" 1957/58 goda, Tom 3
    Type of Medium: Monograph available for loan
    Pages: 670 Seiten
    Series Statement: Materialy nabljudenij naučno-issledovatel'skich drejfujuščich stancij "Severnyj Poljus-6", "Severnyj Poljus-7" 1957/58 goda 3
    Language: Russian
    Note: СОДЕРЖАНИЕ = Soderžanie = Table of Contents. - Предисловие = Predislovie = Foreword. - Аэрология = Aėrologija = Aerology. - Методика и результаты аэрологических наблюдений = Metodika i rezul'taty aėrologičeskich nabljudenij = Method and results of upper-air observations. - Таблица 1. Географические координаты станций = Tablica 1. Geografičeskie koordinaty stancij = Table 1. Geographical coordinates of stations. - Таблица 2. Среднее месячное давление = Tablica 2. Srednee Mesjačnoe davlenie = Table 2. Average monthly pressure. - Таблица 3. Средняя месячная высота и температура изобарических поверхностей = Tablica 3. Srednjaja mesjačnaja vysota i temperatura izobaričeskich poverchnostej = Table 3. Average monthly height and temperature of isobaric surfaces. - Таблица 4. Средняя месячная плотность воздуха = Tablica 4. Srednjaja mesjačnaja plotnost' vozducha = Table 4. Average monthly air density. - Таблица 5. Средняя месячная температура = Tablica 5. Srednjaja mesjačnaja temperatura = Table 5. Average monthly temperature. - Таблица 6. Максимальная температура = Tablica 6. Maksimal'naja temperatura = Table 6. Maximum temperature. - Таблица 7. Минимальная температура = Tablica 7. Minimal'naja temperatura = Table 7. The minimum temperature. - Таблица 8. Средняя высота изотермических поверхностей = Tablica 8. Srednjaja vysota izotermičeskich poverchnostej = Table 8. The average height of isothermal surfaces. - Таблица 9. Повторяемость высоты нижней границы инверсий и изотермий и числа дней с инверсиями и изотермиями = Tablica 9. Povtorjaemost' vysoty nižnej granicy inversij i izotermij i čisla s inversijami i izotermijami = Table 9. Repeatability of the height of the lower boundary of inversions and isotherms and the number of days with inversions and isotherms Таблица 10. Средняя мощность инверсий и изотермий = Tablica 10. Srednjaja moščnost' inversij i izotermij = Table 10. The average power of inversions and isotherms. - Таблица 11. Средняя интенсивность инверсий и изотермий = Tablica 11. Srednaja intensivnost' inversij i izotermij = Table 11. The average intensity of inversions and isotherms. - Таблица 12. Средняя высота и температура нижней границы тропопаузы = Tablica 12. Srednjaja vysota i temperatura nižnej granicy tropopauzy = Table 12. The average height and temperature of the lower border of the tropopause. - Таблица 13. Повторяемость высоты нижней границы тропопаузы = Tablica 13. Povtorjaemost' vysoty nižnej granicy tropopauzy = Table 13. Repeatability of the height of the lower tropopause border. - Таблица 14. Повторяемость температуры нижней границы тропопаузы = Tablica 14. Povtorjaemost' temperatury nižnej granicy tropopauzy =Table 14. Repeatability of temperature of the lower tropopause border. - Таблица 15. Средняя месячнан относительная влажность = Tablica 15. Srednjaja mesjačnan otnositel'naja vlažnost' = Table 15. Average monthly relative humidity. - Таблица 16. Средняя месячная удельная влажность = Tablica 16. Srednjaja mesjačnaja udel'naja vlažnost' = Table 16. Average monthly specific humidity. - Таблица 17. Средняя высота нижней границы облаков = Tablica 17. Srednaja vysota nižnej granicy oblakov = Table 17. The average height of the lower boundary of the clouds. - Таблица 18. Средняя месячная скорость ветра = Tablica 18. Srednjaja mesjačnaja skorost' vetra = Table 18. Average monthly wind speed. - Таблица 19. Максимальная скорость ветра = Tablica 19. Maksimal'naja skorost' vetra = Table 19. Maximum wind speed. - Таблица 20. Повторяемость направления ветра = Tablica 20. Povtorjaemost' napravlenija vetra = Table 20. Wind direction repeatability. - Таблица 21. Результаты температурно-ветрового зондирования атмосферы = Tablica 21. Rezul'taty temperaturno-vetrovogo zondirovanija atmosfery = Table 21. Results of temperature-wind sounding of the atmosphere. - , In kyrillischer Schrift
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  • 80
    Monograph available for loan
    Monograph available for loan
    Reading ; 1979 - 1986 nachgewiesen
    Call number: MOP 45206
    Type of Medium: Monograph available for loan
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  • 81
    Call number: MOP 21786/2,1 ; MOP 21786/2,1(2. Ex.) ; MOP 21786/2,1(3. Ex.)
    In: Aeronautical English
    Type of Medium: Monograph available for loan
    Pages: 322 S. : Ill., graph. Darst.
    Location: MOP - must be ordered
    Location: MOP - must be ordered
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  • 82
    Call number: MOP 46060 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 179 S.
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  • 83
    Call number: MOP 46023(3)
    Type of Medium: Monograph available for loan
    Pages: 39 S.
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  • 84
    Monograph available for loan
    Monograph available for loan
    Berlin : Forschungsinstitut für Hydrometeorologie
    Call number: MOP 45852 ; MOP 45852/A
    Type of Medium: Monograph available for loan
    Pages: 77 S. + Anlagenbd.
    Location: MOP - must be ordered
    Location: MOP - must be ordered
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  • 85
    Monograph available for loan
    Monograph available for loan
    Associated volumes
    Call number: MOP 27370
    In: Untersuchungen an Schiffsanstrichen
    Type of Medium: Monograph available for loan
    Pages: 53 S. : Ill., graph. Darst.
    Series Statement: 1960,6
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  • 86
    facet.materialart.
    Unknown
    München : Bayerisches Geologisches Landesamt
    Associated volumes
    Call number: K 94.0116
    In: Geologische Karte
    Pages: 1 Kt. + Erl.-H.
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  • 87
    Monograph available for loan
    Monograph available for loan
    Nr. 1.1968 - 28.1997; damit Ersch. eingest.
    Call number: MOP Per 122/A
    Type of Medium: Monograph available for loan
    ISSN: 0169-3581
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  • 88
    Monograph available for loan
    Monograph available for loan
    [Erscheinungsort nicht ermittelbar] : Department of Science and Technology, Antarctic Division Australia
    Associated volumes
    Call number: AWI P2-86-0256
    In: Antarctic Telecommunications Guidance Manual, Volume 1
    Type of Medium: Monograph available for loan
    Pages: Diverse Seitenangaben (ca. 50 Seiten)
    Language: English
    Note: TABLE OF CONTENTS: Distribution List. - List of acronyms and abbreviations used. - Record of Amendments. - Foreword to 1st Edition. - Foreword to 2nd Edition. - HISTORY AND DEVELOPMENTS OF ANTARCTIC COMMUNICATIONS. - CONSIDERATION OF TELECOMMUNICATIONS BY SCAR AND ANTARCTIC TREATY CONSULTATIVE PARTIES. - OPERATION OF INDIVIDUAL NATIONS' NETWORKS. - Australia's Antarctic Communications. - Japan's Antarctic communications. - UK Antarctic communications. - US Antarctic communications. - ANTARCTIC TREATY RESOLUTIONS ON ANTARCTIC COMMUNICATIONS. - WMO RESOLUTIONS AND PRINCIPLES ON ANTARCTIC COMMUNICATIONS. - Introduction. - Engineering principles of the GTS. - Functions and responsibilities of Meteorological Telecommunications Centres. - Characteristics of the networks of the GTS. - Operational principles of the GTS. - The transmission of meteorological data an the GTS. - Collection and transmission of meteorological data. - Data processing. - Telecommunications system. - Weather reporting by traverse parties. - Automatic weather station in the Antarctic. - AIREP reports. - Mobile ship stations. - OTHER RELEVANT RECOMMENDATIONS AND RESOLUTIONS. - APPENDIXES. - APPENDIX I. - Manual an the Global Data Processing System, Regional Aspects, the Antarctic. - APPENDIX II. - Network of CLIMAT and CLIMAT TEMP reporting stations in the Antarctic. - APPENDIX III. - Results of the monitoring of Antarctic data reception carried out during the period 12-15 March 1982. - APPENDIX IV. - Existing links for the daily international exchange of meteorological data within the Antarctic. - APPENDIX V. - Principal routes by which Antarctic meteorological data enters the GTS. - APPENDIX VI. - List of Antarctic stations and the routing of their meteorological data to the GTS.
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  • 89
    Call number: ZSP-201-83/32
    In: CRREL Report, 83-32
    Description / Table of Contents: Ice forces on a bridge pier in the Ottauquechee River, in Quechee, Vermont, were measured by installing fourpanels-each capable of measuring forces in the normal and tangential direction - on both sides of a vertical V-shaped pier nose. The measured forces are presented for a short period during an ice run. After the ice run, the thickness and sizes of the ice floes were measured and the compressive strength of the ice was determined in the laboratory from the ice samples collected along the river banks. The water level measurements made at several locations along theriver are also presented for the period of the ice run.
    Type of Medium: Series available for loan
    Pages: ii, 8 Seiten , Illustrationen
    Series Statement: CRREL Report 83-32
    Language: English
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  • 90
    Monograph available for loan
    Monograph available for loan
    Alma-Ata : Nauka
    Call number: MOP 45695 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 192 Seiten , Illustrationen , 20 cm
    Language: Russian
    Note: In kyrillischer Schrift
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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-201-83/2
    In: CRREL Report, 83-2
    Description / Table of Contents: A numerical model of rime ice accretion on an arbitrary two-dimensional airfoil is presented. The physics of the model are described and results are presented that demonstrate, by comparison with other theoretical data and experimental data, that the model predictions are believable. Results are also presented that illustrate the capability of the model to handle time-dependent rime ice accretion, taking into account the feedback between the ice accretion and the airflow and droplet trajectory fields.
    Type of Medium: Series available for loan
    Pages: vi, 81 Seiten , Illustrationen
    Series Statement: CRREL Report 83-2
    Language: English
    Note: CONTENTS Abstract Preface Nomenclature Introduction Methodology Potential flow around an arbitrary airfoil Incompressible velocity field Droplet trajectory equation Computational procedure for trajectories Determining the point of impact Calculation of collision efficiencies Accreting an ice layer Determining the accuracy of the flow field Determining the accuracy of the trajectories Results and discussion Comparing results with and without the history term Collision efficiency of NACA 0015 airfoil at 8° attack angle Time-dependent accretion on NACA 0015 airfoil at 8° attack angle Time-dependent accretion on NACA 0015 airfoil at 0° attack angle Conclusions and recommendations Literature cited Appendix A : Sample input Appendix B: Sample output Appendix C : Program listing
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  • 92
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-83/1
    In: CRREL Report, 83-1
    Description / Table of Contents: Roof snow load case studies gathered throughout the United States over a three-year period are analyzed. The objective of the analysis is to determine a relationship between the snow load on the ground and the corresponding uniform snow load on flat and sloped roofs. The main parameters considered are the thermal characteristics of the roof, the roof slope and the exposure of the structure. Exposure has the strongest effect on the ratio of ground to roof snow loads. Comparisons are made with existing and proposed building codes and standards.
    Type of Medium: Series available for loan
    Pages: iv, 47 Seiten , Illustrationen
    Series Statement: CRREL Report 83-1
    Language: English
    Note: CONTENTS Abstract Preface Metric conversion table Introduction Data base Conversion factor Ground load effects Exposure effects Thermal effects Slope effects Expected value relationship Comparison with existing codes and standards Comparison with relationships proposed in new ANSI standard Summary and conclusions Literature cited Appendix A. Roof snow load case history reports Appendix B. Roofs in the snow load case study data base Appendix C. Ground and roof snow load data Appendix D. Conversion factors from the 1982 ANSI standard
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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-201-83/30
    In: CRREL Report, 83-30
    Description / Table of Contents: Ice sheets are formed and retained in several ways in nature, and an understanding of these factors is needed before most structures can be successfully applied. Many ice sheet retention structures float and are somewhat flexible; others are fixed and rigid or semirigid. An example of the former is the Lake Erie ice boom and of the latter, the Montreal ice control structure. Ice sheet retention technology is changing. The use of timber cribs is gradually but not totally giving way to sheet steel pilings and concrete cells. New structures and applications are being tried but with caution. Ice-hydraulic analyses are helpful in predicting the effects of structures and channel modifications on ice cover formation and retention. Often, varying the flow rate in a particular system at the proper time will make the difference between whether a structure will or will not retain ice. The structure, however, invariably adds reliability to the sheet ice retention process.
    Type of Medium: Series available for loan
    Pages: iv, 39 Seiten , Illustrationen , 1 Beilage
    Series Statement: CRREL Report 83-30
    Language: English
    Note: Contents Abstract Preface Introduction Natural ice sheets Choosing an ice control structure Flexible structures Ice booms Frazil collector lines Fence booms Rigid or semirigid structures Pier-mounted booms Stone groins Artificial islands Removable gravity structures Timber cribs Weirs Pilings and dolphins Structures built for other purposes Hydroelectric dams Wicket dams Light piers and towers Bridge piers Breakwaters Ice control not using Structures Channel improvements Ice sheet tying Ice sheet bridges Conclusions Literature cited Appendix A: Ice control structure
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  • 94
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-83/31
    In: CRREL Report, 83-31
    Description / Table of Contents: A mathematical model is described that is used to determine the maximum ice conveyance capacity of a river channel. Based upon this model, computer programs were developed that enable the ice discharge to be calculated for steady-state flow conditions. For rivers that have uniform flow, the maximum ice-conveying capacity can be described with a simple function expressed in terms of the size of the ice fragments, channel geometry, and the flow of water in the river. For nonuniform flows, the computer program determines the elevation profile of the surface layer in addition to other flow characteristics, such as the velocity and surface concentration of the ice fragments. The location along this surface profile where the ice conveyance capacity becomes less than the upstream supply is determined and is considered to be the position where a surface ice jam or ice bridge will be formed.
    Type of Medium: Series available for loan
    Pages: iv, 21 Seiten , Illustrationen
    Series Statement: CRREL Report 83-31
    Language: English
    Note: CONTENTS Abstract Preface Nomenclature Introduction Constitutive relationships Equations of motion Uniform flow Nonuniform flow Ice transport: Uniform flow Symmetric channel Asymmetric channel Ice transport: Nonuniform flow Further considerations Basis for model improvement Conclusions Literature cited
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  • 95
    Monograph available for loan
    Monograph available for loan
    Leningrad : Gidrometeorologičeskoe Izdatel'stvo
    Call number: MOP 43158 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 159 Seiten , Illustrationen , 26 cm
    Language: Russian
    Note: In kyrillischer Schrift
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  • 96
    Call number: MOP 45321 / Mitte
    In: Antarctic research activities of the German Democratic Republic
    Type of Medium: Monograph available for loan
    Series Statement: Antarctic research activities of the German Democratic Republic : report to SCAR No 4
    Language: English
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  • 97
    Series available for loan
    Series available for loan
    Tokyo : National Institute of Polar Research
    Associated volumes
    Call number: ZSP-714-2
    In: Science in Antarctica, 2.
    Type of Medium: Series available for loan
    Pages: viii, 325 Seiten , Illustrationen , 27 cm
    ISBN: 4-7722-1285-X
    Series Statement: Science in Antarctica 2
    Language: Japanese
    Note: In japanischer Sprache
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  • 98
    Monograph available for loan
    Monograph available for loan
    Moscow : Progress Publishers
    Call number: MOP 47047 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 343 Seiten , Illustrationen
    Uniform Title: Poljanye dnevniki 〈engl.〉
    Language: English
    Note: Aus dem Russischen übersetzt
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  • 99
    Call number: S 90.0006(154)
    In: Memoir / Geological Society of America, 154
    Type of Medium: Series available for loan
    Pages: X, 824 Seiten , Illustrationen, graphische Darstellungen, Karten , 3 Beil. (Mikrofiches)
    Edition: Reprinted
    ISBN: 0-8137-1154-1
    Series Statement: Memoir / Geological Society of America 154
    Language: English
    Note: Preface INTRODUCTION History of the Nazca Plate Project George P. Woollard and La Verne D. Kulm DIVERGENT BOUNDARY Tectonics of the Nazca-Pacific divergent plate boundary David K. Rea Structure and evolution of the Easter plate D. W. Handschumacher, R. H. Pilger, Jr., J. A. Foreman, and J. F. Camphell Petrogenesis and secondary alteration of upper layer 2 basalts of the Nazca plate K. F. Scheidegger and J. B. Corliss Temporal variations in secondary minerals from Nazca plate basalts, diabases, and microgabbros Debra S. Slakes and K. F. Scheidegger METALLIFEROUS SEDIMENTS Geochemistry of Nazca plate surface sediments: An evaluation of hydrothermal, biogenic, detrital, and hydrogenous sources Jack Dymond Metalliferous-sediment deposition in time and space: East Pacific Rise and Bauer Basin, northern Nazca plate G. Ross Heath and Jack Dymond Lead isotopic composition of metalliferous sediments from the Nazca plate E. Julius Dasch Sediment accumulation rate patterns on the northwest Nazca plate G. M. McMurtry. H. H. Veeh, and C. Moser Uranium and thorium isotopic investigations in metalliferous sediments of the northwestern Nazca plate H. Herbert Veeh Formation and growth of ferromanganese oxides on the Nazca plate Mitchell Lyle Sediment and associated structure of the northern Nazca plate D. L. Erlandson, D. M. Hussong, and J. F. Campbell Economic appraisal of Nazca plate metalliferous sediments Cvrus W. Field, Dennis G. Wetherell, and E. Julius Dasch CONTINENTAL MARGIN AND TRENCH Tectonics, structure, and sedimentary framework of the Peru-Chile Trench W. J. Schweller, L. D. Kulm, and R. A. Prince Coastal structure of the continental margin, northwest Peru and southwest Ecuador Glenn L. Shepherd and Ralph Moberly Sedimentary basins of the Peru continental margin: Structure, stratigraphy, and Cenozoic tectonics from 6°S to 16°S latitude T. Thornburg and L. D. Kulm Crustal structures of the Peru continental margin and adjacent Nazca plate, 9°S latitude Paul R. Jones III Crustal structure and tectonics of the central Peru continental margin and trench L. D. Kulm, R. A. Prince, W. French, S. Johnson, and A. Masias Late Cenozoic carbonates on the Peru continental margin: Lithostratigraphy, biostratigraphy, and tectonic history La Verne D. Kulm, Hans Schroder, Johanna M. Resig, Todd M. Thornburg, Antonio Masias, and Leonard Johnson Vertical movement and tectonic erosion of the continental wall of the Peru-Chile Trench near 1 l°30'S latitude Donald M. Hussong and Larry K. Wipperman Shallow structures of the Peru Margin 12°S - 18°S S. H. Johnson and G. E. Ness Clay mineralogy of the Peru continental margin and adjacent Nazca plate: Implications for provenance, sea level changes, and continental accretion Victor J. Rosato and La Verne D. Kulm Structures of the Nazca Ridge and continental shelf and slope of southern Peru Richard Couch and Robert M. Whitsett Tectonics of the Nazca plate and the continental margin of western South America, 18° to 23°S William T. Coulbourn Biogeography of benthic foraminifera of the northern Nazca plate and adjacent continental margin Johanna M. Resig Estimation of depth to magnetic source using maximum entropy power spectra, with application to the Peru-Chile Trench Richard J. Blakely and Siamak Hassanzadeh An active spreading center collides with a subduction zone: A geophysical survey of the Chile Margin triple junction E. M. Herron, S. C. Cande, and B. R. Hall Structures of the continental margin of Peru and Chile Richard Couch, Robert Whit sett, Bruce Huehn, and Luis Briceno-Guarupe ANDEAN CONVERGENCE ZONE Volcanic gaps and the consumption of aseismic ridges in South America Amos Nur and Zvi Ben-Avraham Geological and geophysical variations along the western margin of Chile near lat 33° to 36°S and their reaction to Nazca plate subduction Allen Lowrie and Richard Hey Chile Margin near lat 38°S: Evidence for a genetic relationship between continental and marine geologic features or a case of curious coincidences? E. M. Herron Convergence and mineralization — Is there a relation? C. Wayne Burnham Role of subducted continental material in the genesis of calc-alkaline volcanics of the central Andes David E. James Isotopic composition of Pb in Central Andean ore deposits George R. Tilt on, Robert J. Pollak, Alan H. Clark, and Ronald C. R. Robertson Epilogue: Geostill reconsidered Cyrus W. Field and E. Julius Dasch
    Location: Lower compact magazine
    Branch Library: GFZ Library
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  • 100
    Call number: O 2075/1964 II
    Type of Medium: Journal available for loan
    ISSN: 0367-6684 , 0568-5249 , 0568-5249
    Former Title: Vorg. Akademija nauk SSSR Izvestija Akademii Nauk SSSR / Serija geografičeskaja i geofizičeskaja
    Subsequent Title: Forts. Akademija nauk SSSR Izvestija Akademii Nauk SSSR / Fizika zemli
    Subsequent Title: Forts. Akademija nauk SSSR Izvestija Akademii Nauk SSSR / Fizika atmosfery i okeana
    Language: Russian , English
    Note: Teils mit Jg.-Zählung , In kyrill. Schr
    Location: Magazine - must be ordered
    Branch Library: GFZ Library
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