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  • 1
    Monograph available for loan
    Monograph available for loan
    Amsterdam [u.a.] : Elsevier
    Associated volumes
    Call number: 9/M 13.0083
    In: Developments in sedimentology
    Type of Medium: Monograph available for loan
    Pages: 471 S., Ill., graph. Darst., kt-.
    Series Statement: Developments in sedimentology 9A
    Language: English
    Location: Reading room
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  • 2
    Call number: MOP 45332 / Mitte
    In: NUREG CR
    In: BNL
    Type of Medium: Monograph available for loan
    Pages: V, 23 S.
    Series Statement: NUREG CR 1954
    Language: English
    Location: MOP - must be ordered
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  • 3
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Materiel Command, Terrestrial Sciences Center, Cold Regions Research & Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-249
    In: Research report
    Description / Table of Contents: CONTENTS: Preface. - Abstract. - Introduction. - Analytical procedures. - Results and discussion. - Bubbles in ice. - Conclusions. - Literature cited.
    Description / Table of Contents: Application of the gas law to fourth-place density measurements of ice samples from two deep drill holes at Byrd Station and Little America V, Antarctica, shows that virtually all density increase beyond the pore close-off density (0.830 g/cm^3) can be attributed to compression of the entrapped bubbles of air. Data from Byrd Station also indicate that the lag between overburden pressure and bubble pressure, initially 4-5 kg/cm^2 at pore close-off, diminishes to less than 1.0 kg/cm^2 at about 200-m depth. By substituting the overburden pressure for the bubble pressure in the pressure-density relationship based on the gas law, ice densities below 200 m can be calculated more accurately than they can be measured per se on cores because of the relaxation that occurs in samples recovered from high confining pressures. This relaxation, resulting in a progressive increase in the bulk volume of the ice with time, is generally attributed to decompression of the entrapped air bubbles following removal of the ice from high confining pressures. However, calculations of the stress in ice due to bubble pressure, together with measurements of bubble sizes in cores from various depths at Byrd Station, both tend to indicate that there has'been negligible decompression of the inclosed bubbles. It is suggested that most of this relaxation may be due to the formation of microcracks in the ice. Anomalous bubble pressure-density relations at Little America V tend to confirm abundant stratigraphic evidence of the existence of considerable deformation in the upper part of the Ross Ice Shelf. Studies of crystal-bubble relations at Byrd Station revealed that the concentration of bubbles in ice remains remarkably constant at approximately 220 bubbles per cm^3. Bubbles and crystals were found to be present in approximately equal numbers at pore close-off at 64-m depth, at which level the average bubble diameter was 0.95 mm, decreasing to 0.49 mm at 116 m and to 0.33 mm at 279 m. Despite a tenfold increase in the size of crystals between 64 and 279 m, the bubbles showed no tendency to migrate to grain boundaries during recrystallization of the ice. The observation that most of the bubbles had assumed substantially spherical shapes by 120-m depth points to essentially hydrostatic conditions in the upper layers of the ice sheet at Byrd Station.
    Type of Medium: Series available for loan
    Pages: iv, 16 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 249
    Language: English
    Location: AWI Archive
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  • 4
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Corps of Engineers, Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-276
    In: Research report
    Description / Table of Contents: CONTENTS: Introduction. - Test site. - Test procedures. - Equipment. - Unconfined compression tests. - Ring tensile tests. - Test results. - Unconfined compression tests. - Ring tensile tests. - Discussion. - Literature cited. - Appendix A. Calculation of the effect of nonaxial loading of unconfined compression specimens. - Appendix B. Camp Century unconfined compressive strength data at -25C. - Appendix C. Camp Century ring-tensile strength data at -25C. - Appendix D. Unconfined compressive strength of Camp Century vertical snow samples 8.25 in. length, 3.0 in. diam at -25C. - Abstract.
    Description / Table of Contents: The unconfined compressive strengths [Sigma]c and the ring-tensile strengths [Sigma]T of snow and ice specimens from the Inclined Drift at Camp Century, Greenland, were determined. The specimen densities varied over essentially the complete natural density range of polar snow and ice (0.340 to 0.890 g/cm^3). The specimens were loaded rapidly to failure with times varying between 0.2 and 1.4 sec. During loading, head speeds varied between 5.1 and 23.6 cm/min, although during individual tests they were constant. Even the low density specimens failed in the brittle mode. Although a plot of [Sigma]T vs [Gamma] is linear, [Sigma]c vs [Gamma] is clearly nonlinear. This nonlinearity may result from either changes in the level of the internal stress concentrations associated with the voids in the snow or from changes in the ratio (bulk porosity/effective porosity of the failure surface) with density. Both tangent and secant moduli are linear functions of [Gamma]. There is no pronounced change in [Sigma]c with changes in strain rate. A significant increase in [Sigma]T, [Sigma]c and the modulus values was noted at bulk densities greater than 0.830 g/cm^3. This increase is presumably caused by the close-off of the air passages.
    Type of Medium: Series available for loan
    Pages: 35 Seiten , Illustrationen, graphische Darstellungen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 276
    Language: English
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  • 5
    Series available for loan
    Series available for loan
    Hanover, NH : Corps of Engineers, U.S. Army Cold Regions Research & Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-269
    In: Research report
    Description / Table of Contents: CONTENTS: Preface. - List of symbols. - Introduction. - Structure of ice and ice sheets. - Ice as a mineral. - Lake and sea ice. - Chemistry and phase relations. - Dislocations,cracks,and stress concentrators. - Direct observation of dislocations. - Crackformation. - Stress concentration. - Theoretical considerations. - Experimental results. - Compressive strength. - Indentation failure. - Tensile strength. - Flexural strength. - Shear strength. - Impact strength. - Scale effects. - Strength deterioration in the spring. - Recommended research. - Summary. - Selected bibliography. - Abstract.
    Description / Table of Contents: The increased activity in cold regions has made a thorough understanding of fracture in lake and sea ice quite desirable, inasmuch as this information has application to a number of problems of geophysical as well as engineering importance. This survey starts with a discussion of the structure of ice I and the macro- and microstructure of sea and lake ice as well as their chemistry and phase relations. Recent work on the direct observation of dislocations as well as the formation of cracks in ice is summarized. Formal ice-brine-air models for analyzing variations in ice strength are also reviewed. The results of the different types of tests are discussed and cornpared (compressive, indentation, direct and ring-tension, small beam flexure and in situ cantilevers and simple beams, shear, and impact). Scale effects are considered as well as the rapid strength deterioration experienced by ice sheets in the spring. Finally, a number of recommendations are made concerning future research in this field.
    Type of Medium: Series available for loan
    Pages: viii, 79 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 269
    Language: English
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  • 6
    Series available for loan
    Series available for loan
    Hanover, NH : Corps of Engineers, U.S. Army, Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-267
    In: Research report
    Description / Table of Contents: CONTENTS: Introduction. - Regional variations in density. - Monthly increase in density. - Nomograph to estimate average snow-cover density. - Test and application of the nomograph. - Discussion. - Literature cited. - Appendix A: Observed, weighted snow-cover densities for stations in Table 1.
    Description / Table of Contents: Analysis of snow-cover observations made during November - March at 27 stations in Alaska, Canada and the northern United States for a 2 to 11 year period showed that the average snow density can be classified in four general categories: Category 1 (density 0.20 to 0.23 g/cm^3 ), inland stations reporting light winds; Category 2 (0.24 to 0.27 g/cm^3), stations reporting moderate winds; Category 3 (0.28 to 0.30 g/cm^3), inland and coastal locations with stronger winds; Category 4 (0.32 to 0.36 g/cm^3), cold and windy stations of the Arctic. Skewness coefficients computed for each station showed bias toward lower densities for cat. 1 and 2, and bias toward higher densities for cat. 3 and 4. A nomograph in which the average winter air temperature and wind speed are the independent variables makes it possible to estimate the average snow-cover density for any location in the Arctic, subarctic and North Temperate Zones. A comparison between observed and estimated densities for ten other test stations yielded a correlation coefficient of 0.91 with a standard error of estimate of 0.016 g/cm^3. An average snow density map of North America was drawn and the continent was divided into areas based on the four categories.
    Type of Medium: Series available for loan
    Pages: iii, 21 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 267
    Language: English
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  • 7
    Series available for loan
    Series available for loan
    Hanover, NH : Corps of Engineers, U.S. Army Cold Regions Research & Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-271
    In: Research report
    Description / Table of Contents: CONTENTS: Introduction. - Previous work. - Conduct of the research. - Fundamental properties of snow. - Derived properties of snow. - Environmental effects. - Conclusions. - Literature cited. - Abstract.
    Description / Table of Contents: One of the great deficiencies in snow science is the lack of an analytical framework for much of the snow cycle. Snow research to date has largely consisted of measuring index properties of snow, such as bulk density and snow strength, and correlating them. This is useful, particularly for engineering purposes, but it does not grapple with the basic problem of what fundamental properties of snow determine the magnitude of the index properties and how these properties respond to environmental conditions. This study was an attempt to measure, quantitatively, the fundamental properties of grain size, shape, and fabric (relationship between grains) and relate these to the index or derived properties of bulk density, shear and tensile strength, permeability for air, and the dielectric static permittivity and loss tangent. Despite numerous difficulties in defining fabric and quantifying it, it was possible to show that: 1) snow strength is a function of bond area with a relationship in the low density range that is described by: [Sigma]f = [Sigma]i exp - (0.14nf) where [Sigma]f is failure strength, [Sigma]i is the final strength of ice, and nf is the porosity on the failure surface; and 2) the rate of densification of low density snow can be explained in part by high stress concentrations (on the order of 10^7 dynes /cm^2) at intergranular contacts and by such factors as riming on crystals. The effect of the environmental factors of time, temperature, and gravitational stress is difficult to study in situ because they are not independent variables. However, it appears that their study is simplified when we study the fundamental properties of snow as opposed to index properties.
    Type of Medium: Series available for loan
    Pages: v, 70 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 271
    Language: English
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  • 8
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Materiel Command, Terrestrial Sciences Center, Cold Regions Research & Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-248
    In: Research report
    Description / Table of Contents: CONTENTS: Preface. - Abstract. - Introduction. - Analytical procedures. - Results and discussion. - Literature cited.
    Description / Table of Contents: Conductivity measurements have been made on snow and ice samples from pits and deep drillholes at a number of localities in Antarctica and Greenland. Conductivities of the order 1-2 [My]mho/cm only were recorded at the inland sites. Data from deep cores representing more than 1900 years of continuous snow accumulation at Byrd Station, Antarctica, and more than 400 years deposition at Inge Lehmann, Greenland, showed no significant variations of conductivity with time. Measurements of freshly precipitated snow from a single coastal location in McMurdo Sound, Antarctica, also yielded relatively low conductivities of the order 3-4 [My]mho/cm. The substantial increase observed in the conductivity of core samples from near the surface of the Ross Ice Shelf at Little America V can be attributed most probably to windborne salts of marine origin that had accumulated on the surface after the snow was deposited. A peak conductivity of 49 [My]mho/cm was recorded in snow estimated to have been deposited within 20 km of the seaward edge of the Ross Ice Shelf and the maritime effect could still be detected in samples deposited more than 40 km from the ice front. For samples deposited at distances of greater than 200 km from the edge of the Ross Ice Shelf conductivities never exceeded 2 [My]mho/cm. The very low conductivities observed in ice cores from near the bottom of the Ross Ice Shelf confirm earlier conclusions based on detailed petrographic studies oi the cores that the 258-m-thick ice shelf at Little America V is composed entirely of glacial ice.
    Type of Medium: Series available for loan
    Pages: iv, 8 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 248
    Language: English
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  • 9
    Series available for loan
    Series available for loan
    Hanover, NH : Corps of Engineers, U.S. Army, Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-259
    In: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command, 259
    Description / Table of Contents: CONTENTS: Preface. - Introduction. - Previous work. - Study area. - Field procedures. - Results and discussion. - Conclusions. - Literature cited. - Abstract.
    Description / Table of Contents: A modern ice-push ridge on the northwest shore of Gardner Lake in southeastern Connecticut is 0.6 - 1.2 m high and 1.2 - 3.1 m wide. In February and March 1967, the positions of survey stakes placed on the lake ice were measured periodically. During the same period, air and ice temperature and solar radiation intensity were also recorded. Analysis of the data supports the hypothesis that thermal expansion of the lake ice rather than wind action, was the principal cause of ice push. An ice temperature change of approximately 1°C/hr increase for 6 hr was sufficient to induce ice thrust. In a 30-day period, the average net shoreward movement of the surveyed area of the ice surface was 1.0 m. During the 1966-67 winter, approximately 14 m^3 of beach material was reworked and deposited, forming a discontinuous ice-push ridge along 260 m of shoreline.
    Type of Medium: Series available for loan
    Pages: iii, 15 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 259
    Language: English
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  • 10
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Materiel Command, Terrestrial Sciences Center, Cold Regions Research & Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-255
    In: Research report
    Description / Table of Contents: CONTENTS: Preface. - Abstract. - Introduction. - Previous work on unsteady rectilinear motion of a sphere. - Experiments with a circular path. - Conclusion. - Literature cited. - Appendix A: Comparisons of the measured and calculated forces.
    Description / Table of Contents: Forces on a sphere moving unsteadily along a circular path in a viscous fluid are measured, and it is found that within the experimental range the formula valid for rectilinear motion has to be modified to account for the curvature of the path.
    Type of Medium: Series available for loan
    Pages: iv, 10 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 255
    Language: English
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  • 11
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Materiel Command, Terrestrial Sciences Center, Cold Regions Research & Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-252
    In: Research report
    Description / Table of Contents: CONTENTS: Preface. - Abstract. - Introduction. - Theory. - Discussion. - Conclusion. - Literature cited.
    Description / Table of Contents: A diffusion equation is obtained that describes the mechanical dispersion of a dilute mixture of solid particles within an ice matrix that is undergoing deformation. It is shown that within the limits of time intervals and strain rates appropriate to the movement of glaciers and ice sheets the dispersal distance usually is no larger than a distance about one order of magnitude greater than the size of the particles themselves.
    Type of Medium: Series available for loan
    Pages: iv, 6 Seiten , Illistrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 252
    Language: English
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  • 12
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Materiel Command, Terrestrial Sciences Center, Cold Regions Research & Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-254
    In: Research report
    Description / Table of Contents: CONTENTS: Preface. - Abstract. - Introduction. - Description of the anemometer. - Temperature effects and their compensation. - Input-output relations. - Vibration isolation and compensation. - Wind tunnel tests. - Conclusions.
    Description / Table of Contents: A triaxial semiconductor strain-gage anemometer measuring wind velocities in three directions and thereby also determining the direction of the wind was designed and subjected to many crucial tests under various conditions. It was found that the measurements were affected by temperature and vibrations. Temperature compensation in two directions was made and wind tunnel tests on an almost vibration-free platform were performed. The results show that this type of instrument can be successfully used to measure large-scale turbulences. Throughout this report, emphasis is placed on the compensation necessary for temperature and vibration effects and the determination of input-output relationships. It is concluded that it is possible to design a practical triaxial strain-gage anemometer with high-frequency response and high sensitivity and to measure wind velocities accurately with this type of instrument when temperature and vibration compensations are properly made.
    Type of Medium: Series available for loan
    Pages: iv, 15 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 254
    Language: English
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  • 13
    facet.materialart.
    Unknown
    East Melbourne : Department of Energy and Minerals Government of Victoria
    Call number: K 96.0075
    Pages: 1 Kt. + Erl.-H. (68 S.)
    Series Statement: Geological Survey of Victoria report 92
    Language: English
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  • 14
    Monograph available for loan
    Monograph available for loan
    Eglewood Cliffs, NJ : Prentic Hall
    Call number: M 92.1365
    Type of Medium: Monograph available for loan
    Pages: XXVI, 270 S.
    ISBN: 0130929417
    Series Statement: Prentic Hall series in innovative technology
    Classification:
    C.2.7.
    Language: English
    Location: Upper compact magazine
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  • 15
    Call number: 9/M 92.1323(6)
    In: Global geoscience transect
    Type of Medium: Monograph available for loan
    Pages: 30 S. + 2Kt.-Beil.
    ISBN: 0875907830
    Series Statement: Publication of the International Lithosphere Program 192
    Classification:
    A.3.1.
    Language: English
    Location: Reading room
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  • 16
    Call number: SR 90.0001(1995-D,E)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: IV, D21, E7 S.
    Series Statement: U.S. Geological Survey bulletin 1995-D,E
    Language: English
    Location: Lower compact magazine
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  • 17
    facet.materialart.
    Unknown
    Delft ; 1.1969-76.2010
    Call number: S 90.0083
    ISSN: 0165-1706
    Language: English
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  • 18
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Materiel Command Cold Regions Research & Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-251
    In: Research report
    Description / Table of Contents: CONTENTS: Preface. - Abstract. - Introduction. - Theory. - Application to ice sheets and ice shelves. - Summary. - Literature cited.
    Description / Table of Contents: An analysis is made of the rate of bubble coalescence in a deforming ice mass. A total strain of at least 8 is required before appreciable coalescence occurs, The analysis has.been applied to deforming ice shelves and ice sheets. No appreciable coalescence is expected in ice shelves but coalescence should occur in ice sheets (or glaciers) if the shear strain rate at the bottom surface is of the order of 0.075/yr or larger. Measurements of bubble concentration are capable of setting limits on paleo-strain rates of the present ice sheets. Bubble migration down temperature gradients presents complications to the study of bubble coalescence.
    Type of Medium: Series available for loan
    Pages: iv, 5 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 251
    Language: English
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  • 19
    Series available for loan
    Series available for loan
    Hanover, NH : Corps of Engineers, U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-277
    In: Research report
    Description / Table of Contents: CONTENTS: Preface. - Nomenclature. - Introduction. - Basic equations. - Constitutive relations. - Elastic region. - Plastic region. - Stability of the differential equation. - Stability of the difference equation. - Literature cited.
    Description / Table of Contents: An analysis is made of the stability of difference approximation to one-dimensional shock wave propagation in elastic-plastic media. The necessary condition for stability is obtained.
    Type of Medium: Series available for loan
    Pages: iv, 9 Seiten
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 277
    Language: English
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  • 20
    Monograph available for loan
    Monograph available for loan
    New York [u.a.] : Wiley [u.a.]
    Call number: PIK N 456-11-0232
    Description / Table of Contents: Contents: General Circulation and Weather Systems over China ; Air Temperature ; Precipitation ; Humidity and Evaporation ; Cloud Amount, Sunshine Duration and Total Solar Radiation ; Wind Velocity ; Earth Temperature and Frozen Soil ; Weather Phenomena ; Delineation of Climatic Regions in China ; Climatic Variation over China ; Causes of Formation and Variations of Climate ; Climatic Resources and Adversities of China
    Type of Medium: Monograph available for loan
    Pages: VII, 376 S. : Ill., graph. Darst., Kt.
    ISBN: 0471519138
    Uniform Title: Zhongguo qihou
    Language: English
    Location: A 18 - must be ordered
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  • 21
    Series available for loan
    Series available for loan
    Washington, DC : U.S. Gov. Print. Off.
    Associated volumes
    Call number: MOP Per 603(80-1)
    In: Natural disaster survey report, 80-1
    Type of Medium: Series available for loan
    Pages: V, 60 S.
    Series Statement: Natural disaster survey report 80-1
    Language: English
    Location: MOP - must be ordered
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  • 22
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Materiel Command, Terrestrial Sciences Center, Cold Regions Research & Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-256
    In: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command, 256
    Description / Table of Contents: The flow of a compressible fluid through a deep layer of a porous medium with non-uniform permeability was analyzed. The volumetric behavior of the fluid was described first by the perfect gas law, then by the van der Waal's equation of state. Darcy's law was assumed to be valid. For illustration, the model of air flowing through a deep bed of naturally compacted snow was used to carry out numerical computation. The permeability of snow was considered as a function of depth. The nonlinear partial differential equation obtained by combining the continuity equation with Darcy's law was solved by finite difference technique. A time dependent exponential decay boundary condition was used which included the step-rise constant boundary condition as a limiting case. Pressure distributions in the porous medium calculated from the assumption of ideal gas and van der Waal's gas were compared. The data were presented in dimensionless variables.
    Type of Medium: Series available for loan
    Pages: iv, 13 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 256
    Language: English
    Note: CONTENTS: Preface. - Abstract. - Introduction. - Theory. - Computation and results. - Conclusions. - Literature cited.
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  • 23
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Materiel Command, Terrestrial Sciences Center, Cold Regions Research & Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-253
    In: Research report
    Description / Table of Contents: CONTENTS: Preface. - Abstract. - Introduction. - Theoretical considerations. - Method of canopy evaluation. - Application to forest problems. - Forest blowdown. - Radioactivity gradient. - Phenology. - Forest types and structure. - Distribution of leaves and canopy gaps. - Light quality. - Discussion and summary. - Literature cited.
    Description / Table of Contents: A technique for evaluating forest canopies was developed based on the use of a divergent lens system to obtain hemispherical photographs of tree crowns. The photography was processed from 35 mm film and enlarged as a silhouette, and the light transmission was measured with a specially fabricated macrodensitometer. It is concluded that the amount of forest canopy can be expressed as canopy closure index (CCI) at a precision of approximately 5%. It is shown by application to a variety of problems in diverse geographical areas that this technique can be used for measuring both temporal and spatial changes in the canopy, for estimating the shade light climate, and for specifying the probability of target detection through a canopy. Data are presented to analyze changes caused by explosions, radioactivity, growing season, and vegetation types. The geometry of gaps in tree crowns is discussed and the nature of shade light quality under forests is illustrated.
    Type of Medium: Series available for loan
    Pages: v, 20 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 253
    Language: English
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  • 24
    Series available for loan
    Series available for loan
    Hanover, NH : Corps of Engineers, U.S. Army, Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-266
    In: Research report
    Description / Table of Contents: CONTENTS: Preface. - Introduction. - Review of dielectric properties of soils and rocks. - Methods and measurements. - Introduction. - Dispersion. - Experimental procedures. - Introduction. - Apparatus. - Correction for stray fields. - Material. - Results. - The dielectric properties of Na-montmorillonite suspensions as a function of concentration. - The dielectric properties of K-montmorillonite water suspension. - Conclusions. - Outlook. - Literature cited.
    Description / Table of Contents: The dielectric properties of Na- and K- montmorillonite suspensions with concentrations varying from 2.5% to 0.10% by weight were measured at 25°C in the frequency range of 50 Hz to 20 kHz. Effects of electrode polarization were minimized by using the same stainless steel electrodes at different interelectrode distances and a correction was applied to compensate for stray fields. This investigation establishes the fact that the high dielectric constants of clay suspensions at audio frequencies are real and not the result of electrode polarization. The polarization that determines the dispersion is an interfacial phenomenon between the ionic atmosphere and the negatively charged clay particle. The results of this study show that clay suspensions have the same dispersion as soil samples, indicating the probability that the dispersion of wet soils in the frequency range from 50 Hz to 20 kHz is similar for most soils. The actual value of the dielectric constant, however, cannot yet be predicted.
    Type of Medium: Series available for loan
    Pages: iii, 17 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 266
    Language: English
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  • 25
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Materiel Command, Terrestrial Sciences Center, Cold Regions Research & Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-263
    In: Research report
    Description / Table of Contents: CONTENTS: Preface. - Abstract. - Introduction. - Theoretical background. - Experimental apparatus and procedures. - Results and discussion. - Conclusions. - Literature cited.
    Description / Table of Contents: The transition in the mode of heat transfer from conduction to convection in a layer of water formed continuously by melting ice from below has been determined experimentally. This was accomplished by locating the inflection point on the curve relating the water-ice interface (or melting front) and time. Thus, the critical Rayleigh number, Rac, at which convective heat transfer started can be correlated empirically as a function of warm plate temperature, Ts, by Rac= 14,200 exp(-6.64 x 10^-2 Ts). This relation is valid for Ts varying from 7.72 to 25.50°C. The initial ice temperature T0 was varied from -4.8 to -22.00°C. The effect of T0 was found to be insignificant. Homogeneous, bubble-free ice was prepared and used in all the experiments.
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    Pages: iv, 12 Seiten , Illustrations
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 263
    Language: English
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  • 26
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Materiel Command, Terrestrial Sciences Center, Cold Regions Research & Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-260
    In: Research report
    Description / Table of Contents: CONTENTS: Preface. - Abstract. - Introduction and statermnt of problem. - Solution of problem shown in Figure 3. - Solution of problem shown in Figure 4. - The negligibility of the effects of buoyancy and incompressibility of the sealed liquid. - Literature cited.
    Description / Table of Contents: After a brief description of the circumstances which led to the investigation of the title problem and discussion of some related previous investigations, exact solutions are derived for a circular plate which seals an incompressible liquid, is clamped along the boundary and is subjected at an arbitrary point to a lateral concentrated force P. For the case when the plate is covered by a thin liquid layer the solution is obtained in closed form. When this liquid layer is absent, the solution is obtained as an infinite series. The paper concludes with a study of the range of the parameter ([Lambda] a) for which the effort of buoyancy is negligible upon the deflections and stresses in the plate.
    Type of Medium: Series available for loan
    Pages: iv, 11 Seiten , Illustartionen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 260
    Language: English
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  • 27
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    Series available for loan
    Hanover, NH : U.S. Army Materiel Command, Terrestrial Sciences Center, Cold Regions Research & Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-245
    In: Research report
    Description / Table of Contents: CONTENTS: Preface. - Abstract. - Introduction. - Snow crystals in Greenland. - Microspherules. - Microspherules in snow and ice-fog crystals. - Concentration and radii of spherules. - Discussion and conclusions. - Literature cited.
    Description / Table of Contents: Spherules found in snow crystals, ice-fog crystals, fallout particles, and fly ash were studied with an electron microscope using the electron diffraction method. The central part of the residues of 1004 specimens of natural snow crystals from Greenland, the United States, and Japan were examined; 14 spherules 0.1 to 1.5? in radius were found among them. The residues of 658 artificial ice-fog crystals formed from water vapor in flue gases of coal-burning electric power plants at Fairbanks, Alaska, were also examined; nine spherules were found. Spherules similar to those found in ice-fog residues were found in furnace-produced fly ash fallout at Fairbanks, Alaska. Electron and optical microscope examination of spherules found in Greenland snow reveals a size distribution of the form dN/d(log r) = Cr-ß where ß approximately 3. The properties of spherules and the mean mass of snow crystals from Greenland are described. The electron microscope study indicated that less than 0.7% of the 1004 snow crystals contained spherules of possible extraterrestrial origin, and that snow crystals are formed mainly on clay mineral particles by heterogeneous nucleation.
    Type of Medium: Series available for loan
    Pages: iv, 10 Seite , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 245
    Language: English
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  • 28
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Corps of Engineers, Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-250
    In: Research report
    Description / Table of Contents: CONTENTS: Introduction. - Methods. - Results. - Ground and aerial photography. - Hemispherical photography. - Light quality. - Discussion. - Literature cited. - Abstract.
    Description / Table of Contents: Aerial and ground photographs were taken over a 2-year period of sites in the El Verde rain forest to record the consistency of the vegetational patterns in untreated sites and the changes that occurred following gamma irradiation. Four emulsions were used: panchromatic infrared, false color transparency and color transparency. Densitometry was used to evaluate color film and the vegetation response to 3 months of radiation. The color emulsions provided the sharpest indication of damage to vegetation and the succession following treatment. Hemispherical photography of the canopy was evaluated in terms of a canopy cover index defined as percent of light passing through the negative in a 90-degree cone area. Control stations were remarkably constant in all photography, establishing the stability and slow natural changes in rain forest structure. Spectral light measurements within the forest confirmed the predominance of far red shade light. Compared to similar studies on the chronic irradiated forest at Brookhaven National Laboratory the El Verde results were less distinct.
    Type of Medium: Series available for loan
    Pages: iii, 21 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 250
    Language: English
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  • 29
    Monograph available for loan
    Monograph available for loan
    Washington : American Geophysical Union
    Associated volumes
    Call number: 9/M 92.1323(4)
    In: Global geoscience transect
    Type of Medium: Monograph available for loan
    Pages: 20 S. + 2 Kt.-Beil.
    ISBN: 0875907814
    Series Statement: Publication of the International Lithosphere Program 190
    Classification:
    A.3.1.
    Language: English
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  • 30
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    Unknown
    Kiev : Gosudarstvennyj Komitet Ukrainy po Geologii i Ispol'zovaniju Nedr
    Call number: K 95.0027
    Language: English
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  • 31
    Call number: SR 90.0001(1970-A,B)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: Getr. Zählung
    Series Statement: U.S. Geological Survey bulletin 1970-A,B
    Language: English
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  • 32
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    Unknown
    Berlin : Technische Fachhochschule Berlin
    Call number: K 96.0195
    Language: English
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  • 33
    Call number: AWI P5-15-0006
    Type of Medium: Monograph available for loan
    Pages: XIII, 495 Seiten
    Edition: printed original edition 1967
    ISBN: 0-8047-0272-1
    Language: English
    Note: Contents: 1 Introduction. - 2 Geology of the Floor of Bering and Chukchi Seas - American Studies. - 3 Late Quaternary Sediments of Bering Sea and the Gulf of Alaska. - 4 Quaternary Marine Transgressions in Alaska. - 5 Quaternary Geology of the Alaskan Shore of Chukchi Sea. - 6 Quaternary Geology of Western Seward Peninsula, Alaska. - 7 Paleogeography of Chukotka During Late Neogene and Quaternary Time. - 8 Radiocarbon Chronology in Siberia. - 9 Neogene and Early Quaternary Vegetation of Northwestern North America and Northeastern Asia. - 10 Quaternary Vegetational History of Arctic Alaska. - 11 Vegetation of Eastern Siberia During the Anthropogene Period. - 12 Distribution, Ecology, and Cytology of the Ogotoruk Creek Flora and the History of Beringia. - 13 Mammal Remains of Pre-Wisconsin Age in Alaska. - 14 On the Origin of the Mammalian Fauna of Canada. - 15 The Effect of the Bering Land Bridge on the Quaternary Mammalian Faunas of Siberia and North America. - 16 Palearctic-Nearctic Mammalian Dispersal in the Late Cenozoic. - 17 The Stratigraphy of Tjbrnes, Northern Iceland, and the History of the Bering Land Bridge. - 18 Cenozoic Migrations of Marine Invertebrates Through the Bering Strait Region. - 19 Marine Mammals and the History of Bering Strai. - 20 Depth Changes in Bering Sea During the Upper Quaternary, as Indicated by Benthonic Foraminifera. - 21 Diatom Floras and the History of Okhotskand Bering Seas. - 22 On Migrations of Hunters across the Bering Land Bridge in the Upper Pleistocene. - 23 Human Migration and Permanent Occupation in the Bering Sea Area. - 24 The Cenozoic History of Beringia - A Synthesis. - General Index. - Index to Faunal and Floral Taxa.
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  • 34
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Materiel Command, Terrestrial Sciences Center, Cold Regions Research & Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-242
    In: Research report, 242
    Description / Table of Contents: The attenuation of visible light by falling snow was studied by making simultaneous attenuation measurements and snow concentration measurements. The attenuation coefficient was calculated from photometric measurements and from visual observations. Snow concentration in the air was evaluated by two methods: from Formvar replicas collected during the snowfall, and by mass accumulation of snow in collecting pans. The snowflakes were arbitrarily classified by crystal types according to their estimated fall velocity. It was found that the correlation between extinction coefficient (attenuation) and snow concentration was generally much higher by types than when all snowflakes were considered together regardless of crystal components and degree of riming. Two types, apparently improperly classified, displayed lower correlations than the overall group. When no fog is present during the snowfall, the experimental results coincide well with attenuation theory if a reasonable correction is applied to the values obtained in the measurement of snowflake diameters. Measurements of mass flux indicate that for a given intensity the attenuation caused by snow is an order of magnitude greater than that caused by the same mass flux of rain.
    Type of Medium: Series available for loan
    Pages: iv, 27 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 242
    Language: English
    Note: CONTENTS: Preface. - Abstract. - Introduction. - Initial theoretical considerations. - Light attenuation by particles. - Basis of attenuation meter measurements. - Contrast reduction and visual range. - Transmissometer theory, Pritchard photometric method. - Terminal velocity of snowflakes. - Methods of measurement: Light attenuation. - Duntley (Scripps Institution) attenuation meter. - "Meteorological range" observations. - Pritchard photometric method. - Methods of measurement: Atmospheric concentration of snowflakes. - Replication method. - Mass accumulation method. - Analysis of snow samples. - Terminal velocity of snowflakes. - Flux density and atmospheric concentration. - Mass accumulation rate. - Concurrent attenuation due to fog. - Discussion of results. - Computational methods. - Correlations: Attenuation coefficient vs area concentration. - Correlations: Attenuation coefficient vs are a flux. - Correlations: Attenuation coefficient vs mass concentration and mass flux. - Comparison of sampling methods for mass flux. - Attenuation of visible light by snow compared to rain. - Literature cited. - Appendix A.
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  • 35
    Call number: AWI G2-15-0023
    In: Coastal and estuarine studies, 40
    Type of Medium: Monograph available for loan
    Pages: XV, 647 S. : Ill., zahlr. graph. Darst., Kt.
    ISBN: 0875902545
    Series Statement: Coastal and estuarine studies 40
    Language: English
    Note: Contents: Acknowledgement. - Contributors List. - PART I. INTRODUCTION. - Introduction / D. Prandle. - PART II. BAROCLINIC DYNAMICS. - The influence of coastally trapped waves on the circulation in Jervis Bay, New South Wales / P. D. Craig and P. E. Holloway. - Tidal mixing near the sill of a Scottish sea loch / A. J. Elliott, P. A. Gillibrand and W. R. Turrell. - A topographically induced internal wave and mixing in the Tamar Estuary / D. R. Sturley and K. R. Dyer. - Turbulence and shear induced mixing processes in estuaries / E. J. Derbyshire & J. R. West. - Dynamically-active models in the prediction of estuarine stratification / J. H. Simpson and J. Sharples. - PART III. CIRCULATION. - Circulation Residual flow in Naples Bay and its effect on constituent concentration, constituent flux and residence time / J. Van de Kreeke. - The stratified hydrodynamics of the Palmiet - a prototypical bar-built estuary / J. L. Largier, J. H. Slinger and S. Talijaard. - Salinity structure of a shallow, tributary estuary / W. W. Schroeder, S. P. Dinnel and W. J. Wiseman Jr. - On meteorologically induced subtidal motion in Hangzhou Bay / J. L. Su and W. Chen. - Water level fluctuations in the Atchafalaya Delta, Louisiana: tidal forcing versus river forcing / E. M. Swenson and C. E. Sasser. - Modelling of low-frequency salinity variations in the St. Lawrence Estuary / K. T. Tee. - On the estuatine circulation within the Kattegat / N. Winkel-Steinberg, J. O. Backhaus and T. Pohlmann. - PART IV. SEDIMENTATION. - Sedimentation Observations of fine-sediment concentrations and transport in the turbidity maximum region of an estuary / R. J. Uncles, J. A. Stephens and M. L. Barton. - Velocity asymmetries in frictionally-dominated tidal embayments: longitudinal and lateral variability / C. T. Friedrichs, D. R. Lynch and D. G. Aubrey. - Effects of sea-level rise on muddy coastal margins / R. Kirby. - Acoustic measurements of suspended sediment over sandwaves / P. D. Thome, R. L. Soulsby and P. J. Hardcastle. - Some observations on fluid mud response to water waves / F. Jiang and A. J. Mehta. - The reflection of waves off beaches / J. Darbyshire. - PART V. MODELLING (SEDIMENT). - Dispersion in tidally-averaged transport equation / R. T. Cheng and V. Casulli. - Effect of bends on dilution rates / R. Smith. - Modelling the vertical distribution of suspended sediment in combined wave-current flow / A. G. Davies. - Some considerations on mathematical modelling of morphological processes in tidal regions / Z. B. Wang. - A three-dimensional transport model for dissolved and suspended matter in estuaries and coastal seas / G. C. van Dam and R. A. Louwersheimer. - An estuatine and coastal sand transport model / B. A. O'Connor and J. Nicholson. - PART VI. APPLIED STUDIES. - Current and density structure in the Netherlands coastal zone / W. P. M. de Ruijter, A. van der Giessen and F. C. Groenendijk. - On the distribution of suspended matter and the density driven circulation in the Dutch coastal area / M. Visser. - Coastal dynamics along a rugged coastline / B. King and E. Wolanski. - Transport of hypoxic waters: an estuary-subestuary exchange / A. Y. Kuo and K. Park. - Interdisciplinary study on the tidal front in the Bungo Channel, Japan / T. Yanagi, O. Matsuda, S. Tanabe and S. Uye. - Hydrodynamic modelling for a tidal power project / T. L. Shaw.
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  • 36
    Series available for loan
    Series available for loan
    Vienna : International Atomic Energy Agency
    Associated volumes
    Call number: AWI G2-15-0024
    In: Reports and studies
    Type of Medium: Series available for loan
    Pages: 191 S.
    Series Statement: Reports and studies / Joint Group of Experts on the Scientific Aspects of Marine Pollution 43
    Language: English
    Note: CONTENTS: EXECUTIVE SUMMARY. - 1. INTRODUCTION. - 1.1. Background. - 1.2. Definition of the coastal zone. - 1.3. Modelling for marine pollution studies. - 2. MODELLING FRAMEWORK. - 2.1. lntroduction. - 2.2. Questions to be answered. - 2.3. Other model dependencies on the nature of the questions. - 2.3.1. Near-field models. - 2.3.2. Far-field models. - 2.4. Conceptual model of contaminant dispersion. - 2.4.1. Description of water column processes. - 2.4.2. Description of the sea bed processes. - 2.4.3. Sources and sinks. - 2.5. Selection of components of the conceptual model. - 3. MODEL CONSTRUCTION. - 3.1. Modelling approach. - 3.1.1. Deterministic modelling approach. - 3.1.2. Stochastic modelling. - 3.2. Hydrodynamic model. - 23.2.1. From simple to complex models . - 3.2.2. Model complexity and predictability. - 3.2.3. Dealing with the problern of open boundaries. - 3.3. Sub-models. - 3.3.1. Sediment transport model. - 3.3.2. Biological transport model. - 3.3.3. Benthic transport model. - 4. MODEL FORMULATION AND PARAMETERIZATION OF PROCESSES. - 4.1. lntroduction. - 4.1.1. Philosophy. - 4.1.2. Levels of parameterization. - 4.2. Parameterization in transport models. - 4.2.1. Hydrodynamical model. - 4.2.2. Pollutant transport model: advection-diffusion equation. - 4.2.3. Sediment transport models. - 4.2.4. Biological transport models. - 4.3. Contaminant transport model: couplings between transport models. - 4.3.1. Biota-water interactions. - 4.3.2. Biota-particle interactions. - 4.3.3. Particle-water interactions. - 4.4. Decay and production. - 4.5. Parameterization in transport models for the sea bed. - 4.6. Characterizing source terms. - 5. CASE STUDIES. - 5 .1. Introduction. - 5.2. Cadmium in an estuary. - 5.2.1. Statement of the management problem. - 5.2.2. Model construction. - 5.2.3. Example calculations. - 5.2.4. Additional comments. - 5.3. Monazite sand dregded from an estuary. - 5.3.1. Statement of the management problern. - 5.3.2. Model construction. - 5.3.3. Specific examples. - 5.4. Impact of the disposal of titanium dioxide wastes into coastal waters. - 5.4.1. Statement of the management problem. - 5.4.2. Model construction. - 5.4.3. Example calculations. - 5.4.4. Additional comments. - 5.5. Nutrient inputs to Osaka Bay. - 5.5.1. Statement of the management problem. - 5.5.2. Model construction. - 5.5.3. Example calculations. - 5.5.4. Additional comments. - 5.6. Sewage discharge near a beach. - 5.6.1. Statement of the management question. - 5.6.2. Model construction. - 5.6.3. Example calculations. - 5.6.4. Additional comments. - 5.7. Model for the Dutch North Sea water quality management plan. - 5. 7 .1. Statement of the management problem. - 5.7.2. Model construction. - 5.7.3. Example calculations. - 5.7.4. Additional comments. - 5.8. Radioactive discharges from a nuclear reprocessing plant. - 5.8.1. Statement of the management problem. - 5.8.2. Model construction. - 5.8.3. Additional comments. - 5.9. Overall observations. - 6. QUALITY ASSURANCE PROCEDURES. - 6.1. Introduction. - 6.2. Verification. - 6.3. Sensitivity analysis. - 6.4. Validation. - 7. SUMMARY AND CONCLUSIONS. - REFERENCES. - ANNEX I. COASTAL REGIMES. - A1.1. Estuaries. - A1.1.1 Stratified estuaries. - A1.1.2. Partially-mixed and well-mixed estuaries. - A1.1.3. Fjords. - A1.1.4. Hybrid estuaries. - A1.1.5. Transverse characteristics of estuaries. - A1.2. Inshore embayments. - A1.3. Open continental shelf. - A1.3.1. Example of a wide shelf. - A1.3.2. Example of a narrow shelf. - A1.4. Marginal seas. - A1.4.1. Example of a marginal sea with a sill: the Baltic Sea. - A1.4.2. Example of a marginal semi-constrained sea: the North Sea. - A1.5. The Arctic shelves. - References to Annex 1. - ANNEX 2. DETAILS ON PARAMETERIZATION OF PROCESSES. - A2.1. Introduction. - A2.2. Hydrodynamic transport models: momentum transfer. - A2.3. Sediment transport models. - A2.3.1. Bed-load transport. - A2.3.2. Suspended sediment transport. - A2.3.3. Grain size distributions. - A2.3.4. Gravitational settling. - A2.3.5. Critical bed shear stress. - A2.4. Biological transport models. - A2.5. Benthic transport models. - A2. 6. Coupling between transport models. - A2.6.1. Biota-water interactions. - A2.6.2. Sediment-water interactions. - A2.7. Diagenesis: water-sediment interactions. - A2.8. Parameterization of the source term. - A2.8.1. Nature of source. - A2.8.2. Bulk sources. - A2.8.3. Disposal procedure. - A2.8.4. Specific chemical compounds. - References to Annex 2. - LIST OF WORKING GROUP MEMBERS, SECRETARIAT AND MEETINGS. - GESAMP REPORTS AND STUDIES.
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  • 37
    Series available for loan
    Series available for loan
    Hanover, NH : US Army Materiel Command, Cold Regions Research & Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-240
    In: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command, 240
    Description / Table of Contents: A 4-summer hydrologic record from a 1.6 km^2 drainage basin at Barrow, Alaska is analyzed. The watershed, a drained lake basin, is underlain by continuous permafrost within 0.3m of the tundra surface and is covered by ice-wedge polygons and numerous small shallow ponds. Considerable variations from the 20-yr means of summer climate (thaw period 88 days, precipitation 67 mm) are represented in the data: 1963 - cold, extremely wet; 1964 - cold, extremely dry; 1965 - cool, dry; 1966 - cool, wet. Runoff varied greatly from storm to storm, occurring primarily through and over the tundra mat and through an intricate system of polygonal troughs and ponds. As a result of the subdued coastal topography, varying areas (0.3 km^2 to 1.6 km^2) contribute to runoff from different storms. Analyses of hydrographs revealed: 1) lag times generally from 3 to 10 hr; 2) recession constants of about 50 hr, but occasionally as much as 160 hr; and 3) runoff from individual storms between 1 and 70%. About 5% of the thaw season precipitation normally runs off. Comparison of total thaw season precipitation between the U.S. Weather Bureau and a shielded gage located on the watershed indicated no major differences. If "trace" precipitation is considered, only 90% of the actual precipitation may be recorded. Pan evaporation for an average thaw season is about 160 mm and evapotranspiration which is essentially in balance with precipitation is about 60 mm. Conductivity of runoff water varied from 250 [My]mhos during sustained discharge to more than 500 [My]mhos during low flows in dry years. Precipitation chemistry showed no correlation with storm direction. Assuming all winter precipitation runs off, and the data are spatially and temporally representative, about 50% of the measured annual precipitation in this region runs off into the Arctic Ocean.
    Type of Medium: Series available for loan
    Pages: IV, 18 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 240
    Language: English
    Note: CONTENTS: Preface. - Summary. - Introduction. - Regional setting. - Description of watershed. - Climatic record. - Methods. - Precipitation. - Water and air temperatures. - Discharge. - Evaporation and pond levels. - Water chemistry. - Soil thaw. - Results and discussion. - Precipitation. - Runoff. - Evaporation and transpiration. - Water chemistry. - Conclusions. - Literature cited.
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  • 38
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Materiel Command, Terrestrial Sciences Center, Cold Regions Research & Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-264
    In: Research report
    Description / Table of Contents: CONTENTS: Preface. - Abstract. - Introduction. - Physical properties of ice fog. - Mie scattering computations. - Results. - Literature cited.
    Description / Table of Contents: Ice-fog crystals consisting of many spherical particles, and some hexagonal plates and columns, were observed at ambient temperatures of about -40°C in the Fairbanks, Alaska area during mid-winter. The concentrations and the size distributions of the ice-fog crystals were measured. The attenuation and backscattering of infrared radiation by ice-fog crystals were computed for optical wavelengths of 2.2[My], 2.7[My], 4.5[My], 5.75[My], 9.7[My] and 10.9[My] using the Mie theory. The minimum attenuation coefficients and backscattering functions of ice fog were found to be at 9.7[My] wavelength in the observed wavelengths. Optical attenuation coefficients and volume backscattering functions of water fogs were also computed using the Mie theory. The minimum attenuation coefficients and backscattering functions of water fog were found to be at 10.9[My] wavelength in the region of 2.2[My], 2.7[My], 4.5[My], 5.75[My], 9.7[My] and 10.9[My]. Both the attenuation coefficients and backscattering functions of ice fog are within the same order of magnitude as water fog for equivalent fog concentrations and wavelengths.
    Type of Medium: Series available for loan
    Pages: iv, 7 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 264
    Language: English
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  • 39
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Materiel Command, Cold Regions Research & Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-246
    In: Research report
    Description / Table of Contents: CONTENTS: Preface. - Summary. - Introduction. - Theory. - Discussion. - Literature cited.
    Description / Table of Contents: Steady-state temperature profiles are calculated for the borehole drilled through the Greenland ice sheet at Camp Century. The profiles are found by modifying Robin's theory through the addition of several correction terms. One of these terms is the internal heating arising from creep deformation. The importance of this term was emphasized by Lliboutry. The new theoretical profiles do not differ appreciably from the profile derived from Robin's theory. The theoretical profiles do differ substantially from the Camp Century profile measured by Hansen. It is concluded that Hansen's observations are evidence that factors such as accumulation rate and the upper surface temperature are not in a long-term steady-state condition. Better agreement between theoretical and measured curves is obtained if it is assumed that the accumulation rate was about 40% smaller in the past and that the mean annual surface temperature varied by about 0.5°C over the past 1000 years.
    Type of Medium: Series available for loan
    Pages: iv, 13 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 246
    Language: English
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  • 40
    Monograph available for loan
    Monograph available for loan
    Englewood Cliffs, N.J. : Prentice-Hall
    Associated volumes
    Call number: PIK M 039-92-0688/a
    In: Internetworking with TCP/IP
    Type of Medium: Monograph available for loan
    Edition: 2nd ed
    ISBN: 0134743210
    Classification:
    C.2.7.
    Language: English
    Location: A 18 - must be ordered
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  • 41
    Call number: ZSP-387-8
    In: International project on paleolimnology and late cenozoic climate
    Type of Medium: Series available for loan
    Pages: 128 S.
    Language: English
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  • 42
    Call number: SR 90.0001(1808-J,K)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: Getr. Zählung + 2 pl.
    Series Statement: U.S. Geological Survey bulletin 1808-J,K
    Language: English
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  • 43
    facet.materialart.
    Unknown
    Helsinki [u.a.] ; 326.1984 -
    Call number: Z 92.0098
    ISSN: 0367-522X
    Former Title: Bulletin / Geologinen Tutkimuslaitos
    Language: English
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  • 44
    Monograph available for loan
    Monograph available for loan
    Berlin ; New York : de Gruyter
    Call number: M 92.0170 ; M 15.27529
    Type of Medium: Monograph available for loan
    Pages: x, 264 S. : 137 fig. and 4 tab.
    Edition: 2nd ed.
    ISBN: 3110124084
    Uniform Title: Geodäsie
    Classification:
    A.1.1.
    Language: English
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  • 45
    Monograph available for loan
    Monograph available for loan
    Paris : European Space Agency
    Associated volumes
    Call number: M 97.0145
    In: ESA PSS
    Type of Medium: Monograph available for loan
    Pages: vi, 85 S.
    Edition: Issue 1.
    Series Statement: ESA PSS 01-736
    Classification:
    E.3.
    Language: English
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  • 46
    Monograph available for loan
    Monograph available for loan
    Paris : European Space Agency
    Associated volumes
    Call number: M 97.0154
    In: ESA PSS
    Type of Medium: Monograph available for loan
    Pages: vi, 60 S.
    Edition: Issue 1.
    Series Statement: ESA PSS 05-04
    Classification:
    E.3.
    Language: English
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  • 47
    Monograph available for loan
    Monograph available for loan
    Oak Ridge, Tenn. : ORNL
    Associated volumes
    Call number: PIK N 076-93-0191
    In: Publication
    Type of Medium: Monograph available for loan
    Pages: 59 S.
    Series Statement: Publication
    Language: English
    Location: A 18 - must be ordered
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  • 48
    Call number: S 90.0065(1)
    In: Berliner geowissenschaftliche Abhandlungen
    Type of Medium: Series available for loan
    Pages: 155 S.
    ISBN: 3927541443
    Series Statement: Berliner geowissenschaftliche Abhandlungen : Reihe D, Geoinformatik 1
    Classification:
    A.1.1.
    Language: English
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  • 49
    Call number: PIK N 076-93-0119 ; MOP 47760 / Mitte ; AWI A2-23-4557
    Type of Medium: Monograph available for loan
    Pages: 578 Seiten , Illustrationen
    Edition: First published 1991
    ISBN: 0521426308 , 0-521-42630-8 , 0521416310 , 0-521-41631-0
    Language: English
    Note: Contents Foreword xi OPENING ADDRESSES Professor G.O.P. Obasi, Secretary General, World Meteorological Organization Dr M.K. Tolba, Executive Director, United Nations Environment Programme Dr F. Mayor, Director General, United Nations Educational, Scientific and Cultural Organization Professor M.G.K. Menon, President, International Council of Scientific Unions Dr H. de Haen, Assistant Director General, Food and Agriculture Organization SCIENTIFIC AND TECHNICAL SESSIONS HIGHLIGHTS OF THE IPCC ASSESSMENT The Intergovernmental Panel on Climate Change (IPCC) / B. Bolin Scientific Assessment of Climate Change: Summary of the IPCC Working Group I Report / J.T. Houghton Greenhouse Gases and Other Climate Forcing Agents / U. Siegenthaler and E. Sanhueza Climate Change Prediction / J. F. B. Mitchell and Zeng Qingcun Climate Trends and Variability / M. Coughian and B.S. Nyenzi Climate Change Impact Studies: The IPCC Working Group II Report / Yu. Izrael Impacts on Hydrology and Water Resources / H.E. Lins, I.A. Shiklomanov and E.Z. Stakhiv Impact of Climate Change on Agriculture, A Critical Assessment / S.K. Sinha Potential Impacts of Climate Change on Human Settlements, the Energy, Transport and Industrial Sectors; Human Health and Air Quality / M. Hashimoto and S. Nishioka The Response Strategies Working Group of the IPCC / F. Bernthal The Greenhouse Marathon: Proposal for a Global Strategy / P. Vellinga and R.J. Swart Adaptation Measures / K.M. Sarma Limitation Strategies / K. Yokobori Report of the IPCC Special Committee on the Participation of Developing Countries / J. Ripert OVERVIEW OF THE WORLD CLIMATE PROGRAMME The World Climate Programme: Achievements and Challenges / J.P, Bruce Modern Data and Applications: World Climate Data Programme, World Climate Applications Programme / V.G. Boldirev Overview of the World Climate Research Programme / P. Morel World Climate Impact Studies Programme / J.C.I. Dooge CLIMATE RESEARCH Global Climate, Energy and Water Cycle / G.A. McBean Remote Sensing and Global Climate Change: Water Cycle and Energy Budget / H. Grassl World Ocean Circulation and Climate Change: Research Programmes and a Global Observing System / D.J. Baker Short Term Climate Variability and Predictions / J. Shukia Paleodata, Paleoclimates and the Greenhouse Effect / H. Oeschger Climate Prediction Based on Past and Current Analogues / M.I. Budyko Detection of the Enhanced Greenhouse Effect on Climate / T.M.L. Wigley and S.C.B. Raper CLIMATE CHANGE AND SOCIO-ECONOMIC ACTIVITIES Water Climate, Water and Development / J. Sircoulon Drought Issues for the 1990s / M.H. Glantz and W. Degefu Agriculture and Food Agriculture and Food Systems / M.S. Swaminathan The Potential Effect of Climate Changes on Agriculture / M. Parry and Zhang Jiachen Oceans, Fisheries and Coastal Zones Effects of Global Climatic Change on Marine Ecosystems and Fisheries / T. Kawasaki Sea Level Rise and Coastal Zone Management / E.M. Eid and C.H. Huisbergen Energy Beginning to Reduce Greenhouse Gas Emissions need not be Expensive: Examples from the Energy Sector / E. Mills, D. Wilson and TB. Johansson Land Use and Urban Planning Climate and Land Use in North Africa / M. Kassas Climate and Urban Planning / R. Taesler Human Dimensions Human Well-being, Diseases and Climate / W.H. Weihe and R. Mertens Population and Global Climate Change / D. Norse Public Information and Attitudes / R. Lamb Environment and Development Climate, Environment and Ecology / W.H. Schlesinger Climate, Tropical Ecosystems and the Survivability of Species / P. Olindo Some Possible Impacts of Climate Change on African Ecosystems / C.H.D. Magadza Forests Forests: Their Role in Global Change, with Special Reference to the Brazilian Amazon / E. Salati, R.L. Victoria, L.A. Martinelli and J. E. Richey Integrated Studies Climate Change and Risk Management / K. Turner, T. ORiordan and R. Kemp Climate, Climate Change, and the Economy / N.S. Jodha and W.J. Maunder Assessing the Regional Implications of Climate Variability and Change / W.E. Riebsame and A. Magalhaes SPECIAL PRESENTATION Climate Change and the United Nations Conference on Environment and Development / M.F. Strong TASK GROUPS AND CONSULTATION GROUP REPORTS Task Group I Climate, Hydrology and Water Resources Task Group 2 Agriculture and Food Task Group 3 Oceans, Fisheries and Coastal Zones Task Group 4 Energy Task Group 5 Land Use and Urban Planning Task Group 6 Human Dimensions of Climate Change Task Group 7 Environment and Development Task Group 8 Forests Task Group 9 WCP Overview Task Group 10 The World Climate Programme: Overview and Future Task Group 11 Scientific Components of International Agreements Task Group 12 Synthesis Consultation Group on the Special Needs of Developing Countries SUMMARIES OF PANEL DISCUSSIONS Global Climate Analogues and Global Climate Models Climate and Environmentally Sustainable Economic Development Industry's Response Co-operation in International Research Programmes CONFERENCE STATEMENT MINISTERIAL SESSIONS OPENING CEREMONY Introduction by Prof. G.O.P. Obasi, Secretary General, WMO H.E. Mr. Arnold Koller, President of the Swiss Confederation His Majesty King Hussein Bin Talal, of the Royal Hashemite Kingdom of Jordan The Rt. Hon. Margaret Thatcher, Prime Minister of the United Kingdom of Great Britain and Northern Ireland H.E. Mr. Michel Rocard, Prime Minister of France The Rt. Hon. Edward Fenech-Adami, Prime Minister of Malta The Rt. Hon. Bikenibeu Paeniu, Prime Minister of Tuvalu Statement by Dr. E. Saouma, Director General, FAO CLOSING CEREMONY Statement by Dr. F. Mayor, Director General, UNESCO MINISTERIAL DECLARATION Appendix 1 SWCC Inter-Agency Committees Appendix 2 Poster Session Papers Appendix 3 Statement by Environmental Non-Governmental Organizations Appendix 4 Participants at the Scientific/Technical Sessions Appendix 5 Countries and Organizations Represented at the Ministerial Sessions Appendix 6 Participating Non-Governmental Organizations Appendix 7 Acronyms Appendix 8 Units
    Location: A 18 - must be ordered
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    Monograph available for loan
    Paris : European Space Agency
    Associated volumes
    Call number: M 97.0149
    In: ESA PSS
    Type of Medium: Monograph available for loan
    Pages: vi, 31 S.
    Edition: Issue 2.
    Series Statement: ESA PSS 01-726
    Classification:
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    Language: English
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    Monograph available for loan
    Paris : European Space Agency
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    Call number: M 97.0153
    In: ESA PSS
    Type of Medium: Monograph available for loan
    Pages: iv, 6 S.
    Series Statement: ESA PSS 05-01
    Classification:
    E.3.
    Language: English
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    Monograph available for loan
    Paris : European Space Agency
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    Call number: M 97.0151
    In: ESA PSS
    Type of Medium: Monograph available for loan
    Pages: Getr. Zählung
    Edition: Issue 1., rev.3.
    Series Statement: ESA PSS 01-701
    Classification:
    E.3.
    Language: English
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    Monograph available for loan
    New York [u.a.] : Wiley & Sons
    Associated volumes
    Call number: M 97..0205
    In: Common object services specification
    Type of Medium: Monograph available for loan
    Pages: xiii, 111 S.
    Edition: Revision 1.0
    ISBN: 0471076848
    Classification:
    E.8.
    Language: English
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    Monograph available for loan
    Oberschleissheim near Munich : GSF Research Centre for Environment and Health
    Call number: M 97.0220
    Type of Medium: Monograph available for loan
    ISBN: 9280714074
    Classification:
    Ecology
    Language: English
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    Monograph available for loan
    Chicago : Rand McNally
    Call number: M 97.0183
    Type of Medium: Monograph available for loan
    Pages: XIII, 381 S.
    Classification:
    Tectonics
    Language: English
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  • 56
    Call number: M 97.0272
    In: Bulletin / International Commission on Large Dams
    Type of Medium: Monograph available for loan
    Pages: 233 S.
    ISSN: 0534-8293
    Series Statement: Bulletin / International Commission on Large Dams 82
    Classification:
    Applied Geology
    Language: English
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  • 57
    Call number: AWI P2-88-0760-3
    In: Antarctica and international law, Volume 3
    Type of Medium: Monograph available for loan
    Pages: XI, 551 Seiten
    ISBN: 0379203325
    Language: English
    Note: Arrangement of Volume III: Part VIII Germany. - Part IX Federal Republic of Germany. - Part X Japan. - Part XI New Zealand. - Part XII Norway. - Part XIII Peru. - Part XIV Poland. - Part XV South Africa. - Part XVI Union of Soviet Socialist Republics. - Part XVII United Kingdom of Great Britain and Northern Ireland. - Part XVIII United States of America. - Part XIX Uruguay.
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    Monograph available for loan
    Monograph available for loan
    New York [u.a.] : Wiley & Sons
    Call number: M 97.0354
    Type of Medium: Monograph available for loan
    Pages: xvii, 393 S.
    ISBN: 0471637319
    Classification:
    C.4.6.
    Language: English
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  • 59
    Call number: ZSP-553-8
    In: Meddelelser om Grønland
    Type of Medium: Series available for loan
    Pages: 392 S. : Ill., graph. Darst., Kt.
    ISBN: 8717029697
    Series Statement: Meddelelser om Grønland : Geoscience 8
    Language: English
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  • 60
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    Monograph available for loan
    Ädermannsdorf : Trans Tech Publications Ltd.
    Associated volumes
    Call number: M 97.0380/1
    In: ICOTOM
    Type of Medium: Monograph available for loan
    Pages: xxxv, 1116 S.
    ISBN: 0878496815
    ISSN: 0255-5476
    Classification:
    C.5.2.
    Language: English
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    Monograph available for loan
    Ädermannsdorf : Trans Tech Publications Ltd.
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    Call number: M 97.0380/2
    In: ICOTOM
    Type of Medium: Monograph available for loan
    Pages: xxix, S. 1120-2097
    ISSN: 0255-5476
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    C.5.2.
    Language: English
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  • 62
    Call number: ZSP-686-143
    In: Report
    Type of Medium: Monograph available for loan
    Pages: 42 S. : Ill.
    ISSN: 0937-1060
    Series Statement: Report / Max-Planck-Institut für Meteorologie 143
    Language: English
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    Warrendale, Pennsylvania : TMS
    Call number: M 97.0455
    Type of Medium: Monograph available for loan
    Pages: XI, 272 S.
    ISBN: 0873391802
    Classification:
    C.2.8.
    Language: English
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  • 64
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    New York : Geological Soc. of America
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    Call number: 97.0498/3
    In: Geology of the Alaska Peninsula - Island Arc and continental margin
    Pages: Part 1-3
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    Regional Geology
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    Call number: 97.0498/2
    In: Geology of the Alaska Peninsula - Island Arc and continental margin
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    Regional Geology
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  • 66
    Call number: ZSP-553-11
    In: Meddelelser om Grønland
    Type of Medium: Monograph available for loan
    Pages: 24 S.
    ISBN: 8717051193
    ISSN: 0106-1046
    Series Statement: Meddelelser om Grønland : Geoscience 11
    Language: English
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  • 67
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    Monograph available for loan
    Beijing : Geological Publishing House
    Associated volumes
    Call number: M 98.0012/2
    In: Geology of the Himalayas
    Type of Medium: Monograph available for loan
    Pages: V, 544 S.
    ISBN: 7116007482
    Classification:
    Regional Geology
    Language: English
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  • 68
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    Monograph available for loan
    Utrecht
    Call number: AWI P6-09-0023
    Type of Medium: Monograph available for loan
    Pages: XIII, 106 S.
    ISBN: 9039304238
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  • 69
    Call number: ZSP-558-10 ; MOP 46209 / Mitte
    In: Middle atmosphere program
    Type of Medium: Series available for loan
    Pages: 220 S. : Ill., graph. Darst.
    Language: English
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  • 70
    Call number: ZSP-558-11 ; MOP 46209 / Mitte
    In: Middle atmosphere program
    Type of Medium: Series available for loan
    Pages: 146 S.
    Language: English
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  • 71
    Call number: ZSP-558-9 ; MOP 46209 / Mitte
    In: Middle atmosphere program
    Type of Medium: Series available for loan
    Pages: 579 S. : Ill., graph. Darst.
    Language: English
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  • 72
    Call number: ZSP-558-32 ; MOP 46209 / Mitte
    In: Middle atmosphere program
    Type of Medium: Series available for loan
    Pages: 212 S. : Ill., graph. Darst.
    Language: English
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  • 73
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    Monograph available for loan
    New York [u.a.] : Springer
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    Call number: M 98.0140/2
    In: Electrodynamics of continua
    Type of Medium: Monograph available for loan
    Pages: xi, S. 437-782
    ISBN: 0387970053
    Classification:
    Physics
    Language: English
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  • 74
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    Monograph available for loan
    Genève : International Organization for Standardization
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    Call number: M 98.0173
    In: Industrial automation systems - product data representation and exchange
    Type of Medium: Monograph available for loan
    Pages: xii, 207 S.
    Classification:
    E.5.
    Language: English
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  • 75
    Call number: 15/M 04.0176 ; 15/M 98.0262
    In: NATO ASI series
    Type of Medium: Monograph available for loan
    Pages: xvii, 329 S.
    ISBN: 0792329147
    Series Statement: NATO ASI series : E, Applied sciences 271
    Classification:
    B.3.1.
    Language: English
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    Call number: M 98.0360
    In: NATO ASI series
    Type of Medium: Monograph available for loan
    Pages: xii, 415 S.
    ISBN: 0792330781
    Series Statement: NATO ASI series : C, Mathematical and physical sciences 442
    Classification:
    C.2.9.
    Language: English
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  • 77
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    Monograph available for loan
    San Diego [u.a.] : Academic Press
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    Call number: 5/M 98.0397
    In: International geophysics series
    Type of Medium: Monograph available for loan
    Pages: x, 399 S.
    ISBN: 0122821203
    Series Statement: International geophysics series vol. 55
    Classification:
    Seismology
    Language: English
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    Call number: AR 98/21
    Classification:
    Geochemistry
    Language: English
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  • 79
    Call number: M 97.0155
    In: ESA PSS
    Type of Medium: Monograph available for loan
    Pages: vi, 52 S.
    Edition: Issue 2.
    Series Statement: ESA PSS 01-301
    Classification:
    E.3.
    Language: English
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    Madrid : Instituto Tecnológico Geominero de España ; Leiden : Nationaal Natuurhistorisch Museum
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    Call number: 9/M 97.0173/1
    In: The carboniferous of the world
    Type of Medium: Monograph available for loan
    Pages: 242 S.
    Classification:
    Historical Geology
    Language: English
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    Call number: S 90.0065(5)
    In: Berliner geowissenschaftliche Abhandlungen
    Type of Medium: Series available for loan
    Pages: 119 S.
    ISBN: 392754177X
    Series Statement: Berliner geowissenschaftliche Abhandlungen : Reihe D, Geoinformatik 5
    Classification:
    A.1.1.
    Language: English
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    Monograph available for loan
    London : Arnold
    Call number: M 97.0181
    Type of Medium: Monograph available for loan
    Pages: ix, 342 S.
    Classification:
    Geography and Geomorphology
    Language: English
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  • 83
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    Monograph available for loan
    London : The Geological Society
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    Call number: 9/M 97.0214
    In: Geological Society special publication
    Description / Table of Contents: Geological fluids are a central theme linking the petrography and chemistry of all rock types, deformation processes on the microscopic to the continental scale, and the concentration of economic resources. The fundamental importance of fluid migration and evolution to rock composition and structure is reflected in a growing interest in fluid processes, including a series of successful conferences on water-rock interaction. he papers in this volume are intended to give a review of the whole spectrum of current geofluids research. The papers include international case studies and are written by leading experts in the field. - First overview of fluids research - Examples of commercial applications of fluids research - Reviews research for the non-specialist - Up-to-date extensive bibliographies - Promotes methodological transfer between oil and minerals industries - Explains theory behind and consequences of fluid flow processes
    Type of Medium: Monograph available for loan
    Pages: IX, 372 S. , Ill., graph. Darst., Kt.
    ISBN: 1897799055
    Series Statement: Geological Society special publication 78
    Classification:
    Geodynamics
    Language: English
    Note: John Parnell: Geofluids: introduction / Geological Society, London, Special Publications, 78:vii-ix, doi:10.1144/GSL.SP.1994.078.01.01 --- W.S. Fyfe: The water inventory of the Earth: fluids and tectonics / Geological Society, London, Special Publications, 78:1-7, doi:10.1144/GSL.SP.1994.078.01.02 --- Large-Scale Fluid Flow --- R. Van Balen and S. Cloetingh: Tectonic control of the sedimentary record and stress-induced fluid flow: constraints from basin modelling / Geological Society, London, Special Publications, 78:9-26, doi:10.1144/GSL.SP.1994.078.01.03 --- David Deming: Fluid flow and heat transport in the upper continental crust / Geological Society, London, Special Publications, 78:27-42, doi:10.1144/GSL.SP.1994.078.01.04 --- Alan M. Jessop and Jacek A. Majorowicz: Fluid flow and heat transfer in sedimentary basins / Geological Society, London, Special Publications, 78:43-54, doi:10.1144/GSL.SP.1994.078.01.05 --- G. Neil Phillips, Patrick J. Williams, and Geoffrey De Jong: The nature of metamorphic fluids and significance for metal exploration / Geological Society, London, Special Publications, 78:55-68, doi:10.1144/GSL.SP.1994.078.01.06 --- Deformation and Fluid Flow --- Richard H. Sibson: Crustal stress, faulting and fluid flow / Geological Society, London, Special Publications, 78:69-84, doi:10.1144/GSL.SP.1994.078.01.07 --- R. Muir Wood: Earthquakes, strain-cycling and the mobilization of fluids / Geological Society, London, Special Publications, 78:85-98, doi:10.1144/GSL.SP.1994.078.01.08 --- R.J. Knipe and A.M. McCaig: Microstructural and microchemical consequences of fluid flow in deforming rocks / Geological Society, London, Special Publications, 78:99-111, doi:10.1144/GSL.SP.1994.078.01.09 --- E.L. Stephenson, A.J. Maltman, and R.J. Knipe: Fluid flow in actively deforming sediments: ‘dynamic permeability’ in accretionary prisms / Geological Society, London, Special Publications, 78:113-125, doi:10.1144/GSL.SP.1994.078.01.10 --- Fluid Flow and Reservoir Evolution --- Knut Bjørlykke: Fluid-flow processes and diagenesis in sedimentary basins / Geological Society, London, Special Publications, 78:127-140, doi:10.1144/GSL.SP.1994.078.01.11 --- P.S. Ringrose and P.W.M. Corbett: Controls on two-phase fluid flow in heterogeneous sandstones / Geological Society, London, Special Publications, 78:141-150, doi:10.1144/GSL.SP.1994.078.01.12 --- Fluid Chemistry; Metal-Organic Interactions --- Jeffrey S. Hanor: Origin of saline fluids in sedimentary basins / Geological Society, London, Special Publications, 78:151-174, doi:10.1144/GSL.SP.1994.078.01.13 --- Thomas H. Giordano and Yousif K. Kharaka: Organic ligand distribution and speciation in sedimentary basin brines, diagenetic fluids and related ore solutions / Geological Society, London, Special Publications, 78:175-202, doi:10.1144/GSL.SP.1994.078.01.14 --- Royston H. Filby: Origin and nature of trace element species in crude oils, bitumens and kerogens: implications for correlation and other geochemical studies / Geological Society, London, Special Publications, 78:203-219, doi:10.1144/GSL.SP.1994.078.01.15 --- Keith Nicholson: Fluid chemistry and hydrological regimes in geothermal systems: a possible link between gold-depositing and hydrocarbon-bearing aqueous systems / Geological Society, London, Special Publications, 78:221-232, doi:10.1144/GSL.SP.1994.078.01.16 --- Fluid Evolution: Migration and Precipitation of Hydrocarbons and Metals --- Ulrich Mann: An integrated approach to the study of primary petroleum migration / Geological Society, London, Special Publications, 78:233-260, doi:10.1144/GSL.SP.1994.078.01.17 --- Bernd R.T. Simoneit: Organic matter alteration and fluid migration in hydrothermal systems / Geological Society, London, Special Publications, 78:261-274, doi:10.1144/GSL.SP.1994.078.01.18 --- John Parnell: Hydrocarbons and other fluids: paragenesis, interactions and exploration potential inferred from petrographic studies / Geological Society, London, Special Publications, 78:275-291, doi:10.1144/GSL.SP.1994.078.01.19 --- Anthony D. Fowler: The role of geopressure zones in the formation of hydrothermal Pb-Zn Mississippi Valley type mineralization in sedimentary basins / Geological Society, London, Special Publications, 78:293-300, doi:10.1144/GSL.SP.1994.078.01.20 --- R. Metcalfe, C.A. Rochelle, D. Savage, and J.W. Higgo: Fluid-rock interactions during continental red bed diagenesis: implications for theoretical models of mineralization in sedimentary basins / Geological Society, London, Special Publications, 78:301-324, doi:10.1144/GSL.SP.1994.078.01.21 --- Tracers of Fluid Evolution --- I.R. Duddy, P.F. Green, R.J. Bray, and K.A. Hegarty: Recognition of the thermal effects of fluid flow in sedimentary basins / Geological Society, London, Special Publications, 78:325-345, doi:10.1144/GSL.SP.1994.078.01.22 --- C.J. Ballentine and R.K. O’nions: The use of natural He, Ne and Ar isotopes to study hydrocarbon-related fluid provenance, migration and mass balance in sedimentary basins / Geological Society, London, Special Publications, 78:347-361, doi:10.1144/GSL.SP.1994.078.01.23
    Location: Reading room
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  • 84
    Call number: 4/M 97.0210
    In: NATO ASI series
    Type of Medium: Monograph available for loan
    Pages: xix, 261 S.
    ISBN: 0792334884
    Series Statement: NATO ASI series : C, Mathematical and physical sciences
    Classification:
    C.2.8.
    Language: English
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  • 85
    Monograph available for loan
    Monograph available for loan
    London [u.a.] : Elsevier Applied Science
    Call number: M 97.0215
    Type of Medium: Monograph available for loan
    Pages: xv, 494 S.
    ISBN: 1858610117
    Language: English
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  • 86
    Call number: M 97.0309
    Type of Medium: Monograph available for loan
    Pages: 305 S.
    ISBN: 920100592X
    ISSN: 0074-1876
    Series Statement: Panel proceedings series
    Classification:
    Geochemistry
    Language: English
    Location: Upper compact magazine
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  • 87
    Monograph available for loan
    Monograph available for loan
    Edmonton : Mineralogical Association of Canada
    Associated volumes
    Call number: M 97.0356
    In: Short Course Handbook / Mineralogical Association of Canada
    Type of Medium: Monograph available for loan
    Pages: xii, 485 S.
    Series Statement: Short Course Handbook / Mineralogical Association of Canada vol. 21
    Classification:
    A.2.1.
    Language: English
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  • 88
    Call number: M 97.0394
    Type of Medium: Monograph available for loan
    Pages: xxi, 303 S.
    ISBN: 0412618605
    Classification:
    Paleontology
    Language: English
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  • 89
    Call number: S 99.0056(1/93)
    In: Terra nostra
    Type of Medium: Series available for loan
    Pages: X, 59 S.
    Series Statement: Terra nostra 1/93
    Classification:
    A.0.8.
    Language: English
    Location: Lower compact magazine
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  • 90
    Monograph available for loan
    Monograph available for loan
    Copenhagen : Munksgaard International Booksellers and Publishers
    Associated volumes
    Call number: M 97.0482
    In: Ecological Bulletins
    Type of Medium: Monograph available for loan
    Pages: 495 S. + 1 Kt.-Beil.
    ISBN: 8716110498
    Series Statement: Ecological Bulletins no. 41
    Classification:
    Geography and Geomorphology
    Language: English
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  • 91
    Monograph available for loan
    Monograph available for loan
    Jerusalem : Israel Program for Scientific Transl.
    Call number: M 97.0501
    Type of Medium: Monograph available for loan
    Pages: X, 614 S.
    Uniform Title: Processy sovremennogo osadkoobrazovanija v Beringovom More
    Classification:
    Regional Geology
    Language: English
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  • 92
    Call number: AR 97/02
    Type of Medium: Monograph available for loan
    Pages: 176 S.
    Classification:
    A.0.8.
    Language: English
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  • 93
    Call number: AR 97/03
    Type of Medium: Monograph available for loan
    Pages: 155 S. : graph. Darst.
    Classification:
    Regional Geology
    Language: English
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  • 94
    Monograph available for loan
    Monograph available for loan
    Copenhagen : Nyt Nordisk Forl.
    Associated volumes
    Call number: ZSP-553-9
    In: Meddelelser om Grønland
    Type of Medium: Monograph available for loan
    Pages: 36 S. : Ill.
    ISBN: 8717029635
    ISSN: 0106-1054
    Series Statement: Meddelelser om Grønland : Bioscience 9
    Language: English
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  • 95
    Call number: ZSP-553-36
    In: Meddelelser om Grønland
    Type of Medium: Monograph available for loan
    Pages: 102 S. : zahlr. Kt.
    ISBN: 8750399721
    ISSN: 0106-1054
    Series Statement: Meddelelser om Grønland : Bioscience 36
    Language: English
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  • 96
    Call number: ZSP-553-5
    In: Meddelelser om Grønland
    Type of Medium: Monograph available for loan
    Pages: 19 S.
    ISBN: 8717028736
    ISSN: 0106-1046
    Series Statement: Meddelelser om Grønland : Geoscience 5
    Language: English
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  • 97
    Call number: ZSP-553-10
    In: Meddelelser om Grønland
    Type of Medium: Monograph available for loan
    Pages: 28 S., 11 Beil.
    ISBN: 8717051118
    ISSN: 0106-1046
    Series Statement: Meddelelser om Grønland : Geoscience 10
    Language: English
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  • 98
    Call number: AR 97/15
    Classification:
    Seismology
    Language: English
    Branch Library: GFZ Library
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  • 99
    Call number: ZSP-553-159,12
    In: Meddelelser om Grønland
    Type of Medium: Monograph available for loan
    Pages: 114 S., 38 Taf. : Ill., graph. Darst.
    Series Statement: Meddelelser om Grønland 159,12
    Language: English
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  • 100
    Call number: AWI P6-09-0022 ; ZSP-597-175 ; ZSP-597-175(2. Ex.) ; ZSP-597-175(3. Ex.)
    In: Skrifter
    Type of Medium: Monograph available for loan
    Pages: 130 S. : Ill., graph. Darst., Kt. + 2 Kt.-Beil.
    ISBN: 8290307160
    Series Statement: Skrifter / Norsk Polarinstitutt 175
    Language: English
    Branch Library: AWI Library
    Branch Library: AWI Library
    Branch Library: AWI Library
    Branch Library: AWI Library
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