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  • English  (1,920)
  • German  (1,010)
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  • 1975-1979  (2,920)
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  • 101
    Monograph available for loan
    Monograph available for loan
    Amsterdam [u.a.] : Elsevier
    Associated volumes
    Call number: 13/M 97.0131
    In: Elsevier oceanography series
    Type of Medium: Monograph available for loan
    Pages: XIII, 231 S.
    ISBN: 0444414908
    Series Statement: Elsevier oceanography series 14
    Classification:
    Oceanology
    Language: English
    Location: Reading room
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  • 102
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-79/3
    In: CRREL Report, 79-3
    Type of Medium: Series available for loan
    Pages: ii, 7 Seiten , Illustrationen
    Series Statement: CRREL Report 79-3
    Language: English
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  • 103
    Series available for loan
    Series available for loan
    Hannover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-79/2
    In: CRREL Report, 79-2
    Description / Table of Contents: The stress-density relaionships of snow-water mixtures were investigated and are shown as functions of water content, initial snow density, initial snow-water mixture density and rate of deformation. An increase in water content in snow at a particular density or a decrease in the rate of deformation (or strain rate) decreases the stress, but apparently not the specific energy required to reach a specific mixture density.
    Type of Medium: Series available for loan
    Pages: v, 26 Seiten , Illustrationen
    Series Statement: CRREL Report 79-2
    Language: English
    Note: CONTENTS Abstract Preface Nomenclature Introduction Description of study Sample preparation Test equipment and procedure Test sample characteristics Discussion of results Data presentation format Effect of water content and mixture density Effect of water content and initial snow density Effect of deformation rate Effect of water content and rate of deformation on specific energy Summary Literature cited Appendix A. Derivation of equations Appendix B. Load-deformation traces
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  • 104
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-78/18
    In: CRREL Report, 78-18
    Description / Table of Contents: The primary objective of this project was to demonstrate the utility of remote sensing techniques as an operational tool in the acquisition of data required by the U.S. Army Corps of Engineers, Seattle District, in the Grays Harbor dredging effects project, and related projects. Aerial imagery was used to map surface circulation and suspended sediment patterns near the hopper dredge pump site at the harbor entrance and near pulpmill outfalls in Aberdeen, and to map the areal distribution and extent of intertidal habitats. The surface circulation maps prepared from the aerial photographs and thermal imagery compared favorably with the large-scale circulation patterns observed in the Grays Harbor hydraulic model at the U.S. Army Engineer Waterways Experiment Station. Of the imagery provided by NASA, the thermal imagery was more useful than the color or color infrared (CIR) photographs for mapping circula­tion, while the CIR photographs were more useful than the thermal imagery or the color photographs for mapping intertidal habitats. Current velocities estimated from dye dispersion patterns and drifting dye drogues were comparable at some locations to velocities measured by in situ current meters and in the hydraulic model. Based on a cursory evaluation of LANDSAT-1 imagery acquired in January, February, and October 1973, it had limited utility in providing data on surface circulation patterns in Grays Harbor. The areal distribution and extent of nine wetland vegetation types, dune vegetation, and three types of eelgrass were mapped using primarily aerial C IR photographs and ground sur­veys. Color photographs were also used for areas not covered by the C IR photographs. Wetland vegetation types mapped were: low silty marsh, low sandy marsh, sedge marsh, high immature marsh, high mature marsh, salt marsh, diked pasture, freshwater marsh, and wooded swamp. Undiked salt marsh (first five types) covered 5540 acres (22.3 km2) in Grays Harbor.
    Type of Medium: Series available for loan
    Pages: vi, 85 Seiten , Illustrationen
    Series Statement: CRREL Report 78-18
    Language: English
    Note: CONTENTS Abstract Preface Introduction Site description Background and objectives Project history Approach General Aircraft imagery and sensor data LANDSAT imagery Ground truth data Results and discussion Remote sensing techniques Conventional techniques Comparison of results Conclusions Advantages and disadvantages Applications Recommendations Literature cited
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  • 105
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-78/17
    In: CRREL Report, 78-17
    Description / Table of Contents: Abstract: This investigation utilized historical and recent aerial photographs and satellite imagery in 1) estimating changes in positions of the high-water line and sea cliff break and base, in rates of accretion and/or erosion, and in volumes of transported sediment, and 2) providing a preliminary evaluation of the direction of littoral transport along the outer Cape Cod coast. Using aerial photographs acquired in 1938, 1952, 1971 and 1974 with manual photointerpretation techniques, changes in the distances from selected reference points to the cliff break, cliff base and the high-water line were measured. LANDSAT-1 and -2 imagery acquired from 1 September 1972 to 28 May 1975 was evaluated for use in determining the directions of littoral transport that are active the predominant amount of time. Although the imagery has been very useful for this purpose at other locations, it proved to be useless along the outer shore of Cape Cod. Largest net migrations of the high water line from 1938 to 1974 occurred in the northern and southern portions of this coast. The northern maximum high water line was 321.4 ft, the southern was 1794.6 ft. The central portion of the coast was generally more stable with changes varying from 6.8 to 157.6 ft. Cliff-base recession rates varied from 0.4 to 7.3 ft/yr. Maximum estimated net volume of sediment deposited per linear foot of beach from 1938 to 1974 was 334 yd^3 (based on 2 yd^3/ft of recession or accretion); maximum eroded was 914 yd^3. Changes in the configuration of spits were used to evaluate directions of littoral transport since suspended sediment concentrations were generally not sufficient to act as natural tracers of surface currents. Based on the literature and a determination of the portion of the coast perpendicular to the direction of dominant wave approach, the location of the nodal zone for predominant littoral directions of drift probably shifts between the area near Spectacle Pond and North Truro Air Force Station. This investigation has illustrated a photo interpretation technique that is useful in performing a reconnaissance of coastal change. The data obtained from this method can be used to supplement those acquired by ground surveys and are valid as first approximations for planning subsequent, more detailed surveys.
    Type of Medium: Series available for loan
    Pages: vi, 49 Seiten , Illustrationen
    Series Statement: CRREL Report 78-17
    Language: English
    Note: CONTENTS Abstract Preface Conversion factors: U.S. customary to metric units of measurement Introduction Background Previous investigations Analytical procedures Results and discussion Shoreline changes: High-water line Shoreline changes: Cliff recession Volumetric changes Nodal zone location and direction of littoral transport Error evaluation Summary and conclusions Future research Selected bibliography Appendix A: Maps of shoreline with overlays for 1938, 1952, 1971 and 1974 Appendix B: Supplementary data for estimating shoreline change
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  • 106
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-78/16
    In: CRREL Report, 78-16
    Description / Table of Contents: A model investigation of drifting snow conditions was conducted in a hydraulic flume using a sand-water analog. Model results were evaluated to define modeling parameters that would allow quantitative correlation between measured prototype drift conditions and the model. The modeled structure was the standard plan snow fence designed by the Wyoming Highway Department and installed along Interstate Highway 80 in 1971. The performance of this system was documented by the Rocky Mountain Forest and Range Experiment Station of the U.S. Forest Service. Models of the fence were constructed for three heights and two geometric scales. Geometric scaling was based on terrain roughness and boundary layer thickness considerations, while velocity scaling was based on particle fall velocity and threshold of motion characteristics. Simulation of the atmospheric boundary layer was found to be of primary importance. Velocity scaling analysis suggested the use of a 'significant wind' concept based on a combination of velocity magnitude and frequency. Similarity of precipitation rate was not essential, and could be altered within limits to adjust the time scale. The response of the model to the shape of model elements was significant. Although the model is distorted and inexact similarity is achieved, it appears useful on a practical basis.
    Type of Medium: Series available for loan
    Pages: vi, 26 Seiten , Illustrationen
    Series Statement: CRREL Report 78-16
    Language: English
    Note: CONTENTS Abstract Preface Nomenclature Introduction Background Experimental design Similitude considerations The model Model operation Results Velocity Fence height Porosity Model correlation Summary and conclusions Recommeqdations for future work Literature cited Appendix A
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  • 107
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-78/15
    In: CRREL Report, 78-15
    Description / Table of Contents: This report first discusses the general approach for calculating the horizontal forces an ice cover exerts on a structure. Ice force determination consists of two parts: (1) the analysis of the in-plane forces assuming that the ice cover remains intact and (2) the use of a failure criterion, since an ice force cannot be larger than the force capable of breaking up the ice cover. For an estimate of the largest ice force, an elastic plate analysis and a failure criterion are often sufficient. A review of the literature revealed that, in the majority of the analyses, it is assumed that the failure load is directly related to a 'crushing strength' of the ice cover. However, observations in the field and tests in the laboratory show that in some instances the ice cover fails by buckling. This report reviews the ice force analyses based on the buckling failure mechanism and points out their shortcomings. The report then presents a new method of analysis which is based on the buckling mechanism
    Type of Medium: Series available for loan
    Pages: iv, 13 Seiten , Illustrationen
    Series Statement: CRREL Report 78-15
    Language: English
    Note: CONTENTS Abstract Preface Introduction and statement of problem Review of relevant analyses and tests Determination of the largest ice force on an isolated structure Preliminary remarks The buckling analysis of a floating wedge Proposed method to determine Literature cited
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  • 108
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-78/14
    In: CRREL Report, 78-14
    Description / Table of Contents: The analytical solution and the numerical study of the eigenvalue problem for determining the buckling pressure of an infinite elastic plate floating on water and stressed uniformly along the periphery of an internal hole is presented. The boundary conditions considered are the clamped-, simple-, and free-edge conditions. Small buckling pressure occurs only for the free-edge condition. The shape of the deflection for the free-edge condition suggests that buckling is an important mechanism of failure.
    Type of Medium: Series available for loan
    Pages: v, 55 Seiten , Illustrationen
    Series Statement: CRREL Report 78-14
    Language: English
    Note: CONTENTS Abstract Preface Nomenclature Introduction 1. The problem 2. Abstract of the result Part I. Fundamental solutions 3. Fuchsian type solutions 4. Contour integral solution 5. Integration of the integral solution 6. Fundamental solutions for α = 1 7. Fundamental solutions for α = 0 8. Eigenvalues for α = 0 9. Fundamental solutions for α 〉 1 Part II. Asymptotic expansions 10. Asymptotic expansion for 0 〈 α ⩽1 11. Asymptotic expansion for 1 ≦ α ≦ 2 12. Asymptotic expansion for 2 ≦ α ≦ ∞ Part III. Eigenvalues 13. Range of eigenvalues 14. Eigenvalues for the free-edge condition 15. Eigenvalues for the clamped-edge and simple-edge conditions 16. Deflection Acknowledgement Literature cited Appendix A. Analytical continuation at the singular point Appendix B. Tensorial transformations Appendix C. Comparison of the semi-infinite plate buckling with the asymptotic buckling
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  • 109
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-78/10
    In: CRREL Report, 78-10
    Description / Table of Contents: The compressibility of wet snow is described in terms of pressure melting and nonlinear viscous deformation at grain contacts. The results of experiments with different salinities and liquid water contents are compared with computed densities. The decreasing compressibility of wet snow with increasing salinity and decreasing liquid content is quantified and explained. Simultaneous particle growth and the doubly charged layer at phase boundaries are included in the model. The results show that the density of wet snow increases approximately as a power of time but is highly dependent on the stress, initial particle size, liquid water content, and ionic impurity content of the snow.
    Type of Medium: Series available for loan
    Pages: vi, 23 Seiten , Illustrationen
    Series Statement: CRREL Report 78-10
    Language: English
    Note: CONTENTS Abstract Preface Nomenclature Introduction Experimental procedure Grain growth Stressed particle contacts Fluid pressure Packing geometry Temperature distribution and heat flow Fluid and impurity flows Results The liquid film Conclusions Literature cited
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  • 110
    Call number: ZSP-201-78/12
    In: CRREL Report, 78-12
    Description / Table of Contents: Road test sections of membrane-enveloped silt and clay soils overlain with asphalt cement concrete were subjected to repetitive dynamic plate-bearing loadings to determine their strength variations during freeze-thaw cycles. The recoverable surface deformations in the load deflection bowl were continuously measured during the loading cycles and analyzed using the Chevron layered elastic computer program to obtain the in situ resilient deformation modulus of the various section layers at different stages of the freeze-thaw cycles. The resilient stiffness of the pavement system (the total load per unit of resilient load plate deflection) was also calculated for the various freeze-thaw conditions. The modulus values of the asphalt cement concrete varied inversely with its temperature by an order of magnetide (90,000 psi to 1,300,000 psi). The resilient stiffness of the pavement system varied in the same manner by nearly a factor of eight (228.4 kips/in. to 1740.2 kips/in.). Despite the wide strength variations of the sections during freeze-thaw cycles, membrane-enveloped fine-grained soils can be utilized instead of granular materials as base and subbase layers in flexible pavements in cold regions where moisture migration is a major concern. Moisture migration did not occur at saturation levels up to 75%, thus there was no strength loss during thawing.
    Type of Medium: Series available for loan
    Pages: v, 24 Seiten , Illustrationen
    Series Statement: CRREL Report 78-12
    Language: English
    Note: CONTENTS Abstract Preface Conversion factors: U.S.customary to metric units of measurement Introduction Freeze-thaw system Construction materials Controlled environment test section Outdoor sections Temperature monitoring instrumentation Repetitive plate bearing test apparatus Test results and analyses Conclusions Literature cited
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  • 111
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-78/26
    In: CRREL Report, 78-26
    Description / Table of Contents: Ice fog suppression experiments on the Fort Wainwright Power Plant cooling pond were conducted during the winters of 1974-76. Baseline information studies occupied a sizable portion of the available ice fog weather in 1974-75. Then hexadecanol was added to the pond and dramatically improved visibility by reducing fog generated from water vapor released by the pond at -14 C. Although this temperature was not low enough to create ice fog, the cold vapor fog created was equally as devastating to visibility in the vicinity of the pond. During the winter of 1975-76, suppression tests were continued using films of hexadecanol, mixes of hexadecanol and octadecanol, and ethylene glycol monobutyl ether (EGME). Suppression effectiveness at colder temperatures was stuided and limits to the techniques were probed. A reinforcing grid was constructed that prevented breakup of the film by wind and water currents. Lifetime tests indicated that EGME degrades much more slowly than either hexadecanol or the hexadecanol-octadecanol mix. The films were found to be very effective fog reducers at warmer temperatures but still allowed 20% to 40% of normal evaporation to occur. The vapor thus produced was sufficient to create some ice fog at lower temperatures, but this ice fog occurred less frequently and was more quickly dispersed than the thick fog that was present before application of the films.
    Type of Medium: Series available for loan
    Pages: iv, 27 Seiten , Illustrationen
    Series Statement: CRREL Report 78-26
    Language: English
    Note: CONTENTS Abstract Preface Introduction Ice fog from cooling ponds Evaporation Relative humidity and cold air Ice fog suppression Air movement Plastic films Rafts Injection wells Cooling towers Chemical films Reinforced film experiments Meteorological data collection Floating reinforcement grid Application of the hexadecanol film Hexadecanol, octadecanol mixes Ethylene glycol monobutyl ether Laboratory tests of suppression effectiveness Conclusions Literature cited Appendix A. Design for an automatic thin chemical film applicationsystem Appendix B. Meteorological data
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  • 112
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-78/25
    In: CRREL Report, 78-25
    Description / Table of Contents: The objectives of this investigation were to describe channel characteristics and geographic settings of ice jam sites from aerial photographic interpretation, to indicate which characteristics may be important in causing ice jams, and to suggest additional uses of aerial photographs. Aerial photographs were taken of 19 sites with a Zeiss RMK 15/23 aerial camera on 17, 19, and 21 April 1976. Uncontrolled photomosaics of each site were assembled and major river characteristics were delineated on the photomosaics. Characteristics described include: manmade structures, falls, rapids, changes in channel depths, channel islands, mid-channel shoals or bars, river bed material, river sinuosity, meanders, floodplain width, riparian vegetation, and types of development on the floodplain. River channel widths were measured from the photographs along rivers where ground truth data were available for comparison. Lengths of channel riffles and pools were measured along the rivers where variations in river depths were evident on the photographs. Seventy-nine percent of the sites have some form of flow control structure which causes a pool with a backwater condition of low velocity. The low flow condition in the pool allows a solid ice cover to form which impedes ice movement and initiates ice jams. Aerial photographs provide a regional perspective for evaluating channel characteristics at an ice jam site and for analyzing the geographic setting at each site during ice-free conditions. Photographs taken after ice jams have formed are useful in monitoring ice jam formation, in analyzing ice characteristics, and in documenting ice jam breakup and movement.
    Type of Medium: Series available for loan
    Pages: iii, 60 Seiten , Illustrationen
    Series Statement: CRREL Report 78-25
    Language: English
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  • 113
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-78/24
    In: CRREL Report, 78-24
    Type of Medium: Series available for loan
    Pages: v, 12 Seiten , Illustrationen
    Series Statement: CRREL Report 78-24
    Language: English
    Note: CONTENTS Abstract Preface Introduction Comparison of winters Ship effects Measured forces Sequential breaking of the structure Discussion Conclusions Recommendations Literature cited Appendix A. Force level fluctuations in west ice boom, 20 January 1977
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  • 114
    Call number: ZSP-201-78/23
    In: CRREL Report, 78-23
    Type of Medium: Series available for loan
    Pages: vi, 53 Seiten , Illustrationen
    Series Statement: CRREL Report 78-23
    Language: English
    Note: CONTENTS Abstract Preface Nomenclature Conversion factors: Metric (SI) to U.S. customary units of measurement Introduction Selection of experimental approach Previous investigations of effect of freeze-thaw on soil deform ability Selection of laboratory test method Selection of method of field validation tests Field repeated-load plate-bearing tests Test pavements, soils and materials Test procedures and results Resilient modulus of subgrade calculated from field tests Mathematical model Characterization of asphalt concrete Characterization of frozen silt Calculated resilient modulus of silt within the zone of freezing Laboratory repeated-load triaxial tests Specimens, equipment and testing procedures Apparatus Procedures Resilient properties calculated from laboratory tests Calculation methods Asphalt concrete - test results Asphalt concrete - statistical analysis and discussion Silt - test results Silt - statistical analysis Discussion and conclusions Literature cited Appendix A. Repeated-load plate-bearing test results Appendix B. Laboratory repeated-load triaxial test results Appendix C. Regression equation coefficients for resilient modulus and Poisson’s ratio from repeated-load triaxial test data on asphalt concrete and silt Appendix D. Detailed procedures for repeated-load triaxial testing
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  • 115
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-78/22
    In: CRREL Report, 78-22
    Description / Table of Contents: Special environmental factors that influence the design, laying and maintenance of undersea pipelines and cables in polar waters are described. Various approaches to the protection of submarine pipes and cables are considered, and prime emphasis is given to burial techniques for shallow water. A wide range of methods for trenching and burying are discussed, and technical data are given.
    Type of Medium: Series available for loan
    Pages: v, 36 Seiten , Illustrationen
    Series Statement: CRREL Report 78-22
    Language: English
    Note: CONTENTS Abstract Preface Conversion factors Introduction Types of pipelines and cables Potential hazards to pipelines and cables Areas of concern Waterdepth Sea ice Icebergs and ice islands Submarine permafrost Ice gouging Seabed erosion by water jets Protection methods Protection of unburied pipes and cables Protection by burial Backhoe digging Wireline equipment Plowing and ripping from the surface Plowing and ripping by self-propelled seabed vehicles Bucket ladder dredges Suction dredging Conventional cutterhead dredges Low pressure water jetting Bottom-traveling cutterhead dredges Explosive methods Novel methods Disc saws, wheel ditchers and milling drums Ladder trenchers and chain saws Repetitive impulse devices High pressure water jets Flame jets and plasma torches Electrical discharge and electromagnetic radiation Chemical methods Conclusions Literature cited
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  • 116
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-78/20
    In: CRREL Report, 78-20
    Description / Table of Contents: Abstract: Measurements of the concentrations of Aitken nuclei in maritime air were made near Barrow, Alaska, in June 1975 with a modified Nolan-Pollack small-particle detector. The concentrations varied from 50 to 300 particles cm^-3 depending upon meteorological conditions. The mean Aitken nuclei count was 100 particles cm^-3 for diameters greater than 2 x 10^-3 μm. Transmission electron micrographs of aerosols in maritime air near Barrow were taken. The size range was measured to be 0.01 to 2.5 μm in diameter with the most frequently observed diameter being 0.04 μm. The volume of the maritime air and the collection efficiency of aerosol particles on filmed grids for electron microscopy were measured. The aerosol concentrations were found to be 76 to 101 particles cm^-3 ; the mean concentration was calculated to be 87 particles cm^-3. The aerosol particles in the maritime air were identified by electron microscopy and selected area electron diffraction analysis. About 20% of the aerosol particles were identified, and 80% of the particles were too small for electron diffraction analysis. Sea salt particles constituted 2% of the total, and clay minerals 3%; these particles were considered to be of natural origin. Solid combustion by-products such as coagulated carbon particles and fly ash particles constituted 16%. Despite the comparative remoteness of the sampling site, the measurements indicate that many anthropogenic aerosols were found using an electron microscope.
    Type of Medium: Series available for loan
    Pages: iv, 48 Seiten , Illustrationen
    Series Statement: CRREL Report 78-20
    Language: English
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  • 117
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-77/28
    In: CRREL Report, 77-28
    Description / Table of Contents: Tests were conducted to assess the extent of surface degradation resulting from the application of non-chloride deicing chemicals on three types of airfield pavements. The chemicals tested were proprietary mixtures of urea, formamide, and ethylene glycol; sodium chloride, distilled water, and dry specimens were used as controls and for comparison. Pavements included new and old specimens of open-graded asphaltic concrete and old specimens of dense-graded asphaltic concrete. Portland cement concrete specimens used were new and old, with and without air-entrainment. New and old tar rubber concrete specimens were also tested. Samples were subjected to up to 60 freeze-thaw cycles with deicing chemicals flooding their upper surface. Each specimen was rated on a scale of 0-5 after every five freeze-thaw cycles. All PCC specimens showed some surface degradation, whereas the dense- and open-graded asphaltic concretes were largely unaffected.
    Type of Medium: Series available for loan
    Pages: v, 16 Seiten , Illustrationen
    Series Statement: CRREL Report 77-28
    Language: English
    Note: CONTENTS Abstract Preface Conversion factors: U.S. customary to metric (SI) Units of measurement Introduction Test procedure Pavement types Deicing chemicals Description of tests Discussion Literature cited Appendix A: Test results Appendix B: Portland cement concrete materials data
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  • 118
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    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-77/27
    In: CRREL Report, 77-27
    Description / Table of Contents: The spectral reflectance of natural snow in the range of 0.20- to about 0.40-micrometers wavelengths was studied in the laboratory using both continuous spectral scanning and fixed bandpass measurements. White barium sulfate pressed powder was used as a standard for comparison. The reflectance of fresh snow was found to be very high (usually nearly 100%) and only weakly wavelength dependent from 0.24 micrometers to the visible range. In the 0.20- to 0.24-micrometers portion of the spectrum, the reflectance was found to be quite erratic. Possible reasons for the irregularities in reflectance measurements are discussed.
    Type of Medium: Series available for loan
    Pages: v, 19 Seiten , Illustrationen
    Series Statement: CRREL Report 77-27
    Language: English
    Note: CONTENTS Abstract Preface Introduction Experimental procedure Snow collection Spectrophotometric methods Data analysis Potential sources of error Presentation of results Continuous-scan measurements Comparison of sequential bandpass and continuous-scan measurements Theoretical calculations Discussion of results Differences in amplitude of reflectance measurements Irregularities in the shape of spectral reflectance curves The true spectral reflectance of snow in the ultraviolet region Conclusions Literature cited Appendix A. Absolute reflectance values of pressed BaSO4 powder
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  • 119
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    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-77/25
    In: CRREL Report, 77-25
    Description / Table of Contents: Results of a study to determine the feasibility of using an impulse radar to detect moisture variations in the built-up roof at CRREL and to monitor the curing of concrete are presented. The results indicate that impulse radar can be used to detect wide variations in roof moisture associated with built-up roof surface deterioration and that this technique has the potential of providing a nondestructive test method for measuring the strength of concrete during curing.
    Type of Medium: Series available for loan
    Pages: iv, 9 Seiten , Illustrationen
    Series Statement: CRREL Report 77-25
    Language: English
    Note: CONTENTS Abstract Preface Conversion factors: U.S. customary to metric units of measurement Introduction Impulse radar system Results and discussion Conclusions and recommendations Literature cited ILLUSTRATIONS Figure Relative locations where impulse radar measurements were made andsamples for moisture determinations were obtained on the CRREL roof Impulse radar signal reflected from metal sheet resting on roof Impulse radar signal reflection from roof at station A Impulse radar surface reflection coefficient versus moisture contentofroof Impulse radar signal reflection from aluminum foil on bottom of con-crete form and from aluminum sheet metal resting on top of form Unconfined compressive strength of concrete versus time Examples of X-Y plots of impulse radar signals obtained during thesounding of concrete slab Impulse radar signal reflection coefficients versus time for acuring concrete slab Calculated impulse radar signal attenuation in concrete slab versuselapsed time Dielectric constants versus time calculated from impulse radar signalInformation obtained during curing of concrete slab Unconfined compressive strength of concrete versus corrected reflec-tion coefficient calculated from impulse radar signal data obtainedduring the curing of concrete slab TABLES Comparison of roof moisture content with radar surface reflection coefficient and dielectric constant
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  • 120
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-77/21
    In: CRREL Report, 77-21
    Description / Table of Contents: Cold weather limits the successful application of built-up roofing, but often a roof installation must be completed late in the fall or in the winter. The loose-laid protected membrane roof with a synthetic sheet membrane can be installed in the middle of the winter with complete reliability. A synthetic membrane is traditionally more expensive than built-up roofing (rising crude oil prices, however, have reversed this condition), but it has two special features besides its suitability for winter installation: it can be placed on a damp deck, if necessary, and, being losse-laid, it does not split because of deck movement. This report documents information on the installation of two roofs in Anchorage, Alaska, during January and February 1972, including a discussion of the necessary snow removal from the bare deck and the use of portable shelters for preparing the lap joints between sheets during very cold weather. The winter installation caused no special construction problems and the advantages of the synthetic membrane make it an attractive alternative to built-up roofing. The cost of loose-laid protected membrane roofs in Alaska was, in 1972, nearly $300 per square ($28/sq.m), including insulation. Prices are rising as labor costs rise and as more insulation is specified.
    Type of Medium: Series available for loan
    Pages: 5 Seiten , Illustrationen
    Series Statement: CRREL Report 77-21
    Language: English
    Note: CONTENTS Abstract Preface Introduction The protected membrane roof Winter construction considerations Construction costs Conclusion
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  • 121
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-78/5
    In: CRREL Report, 78-5
    Description / Table of Contents: The viscoelastic deflection of an infinite floating ice plate subjected to a circular load was solved, assuming the Maxwell-Voigt type four-element model. An effective method of numerical integration of the solution integrals was developed, of which each integrand contains a product of Bessel functions extending to infinity. The theoretical curve was fitted to the field data, but the material constants thus found varied with time and location.
    Type of Medium: Series available for loan
    Pages: iii, 32 Seiten , Illustrationen
    Series Statement: CRREL Report 78-5
    Language: English
    Note: CONTENTS Abstract Preface Introduction The problem The solution Method of numerical integration Ramp/steady loading Curve fitting to time lapse deflections Asymptotic deflection Deflection profiles Acknowledgement Literature cited Appendix I. Analytical background Appendix II. Computer programs, ramp time profiles and steady time profiles
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  • 122
    Call number: ZSP-201-77/9
    In: CRREL Report, 77-9
    Description / Table of Contents: This report presents experimental results on the conditions of initiation of an ice jam by a simple surface obstruction, on the equilibrium thickness of an ice jam formed by accumulation and submergence of ice floes, and on the compression strength of floating, fragmented ice cover. In the study on ice jam initiation, it was found that the minimum concentration of floes in the opening of the obstruction at which a jam occurs is nearly independent of the ratio of width of constricted passage to channel width, and is proportional to a negative power of the ratio of floe length to width of constricted passage. From energy analysis of floe submergence, a relationship relating the thickness of a jam formed by accumulation and submergence of floes to the approach flow characteristics was derived and found to fit satisfactorily the experimental data. In experiments on compression strength of floating, fragmented ice cover it was found that the compressive strength is inversely proportional to compression velocity and independent of cover length.
    Type of Medium: Series available for loan
    Pages: vii, 45 Seiten , Illustrationen
    Series Statement: CRREL Report 77-9
    Language: English
    Note: CONTENTS Abstract Preface List of symbols Introduction I. Initiation of ice jams by partial surface obstructions A. Introductory remarks B. Experimental apparatus and procedure C. Dimensional analysis D. Presentation of results and discussion ΙΙ. Thickness of ice jams due to accumulation and transport of ice floes A. Introductory remarks B. Experimental apparatus and procedures C. Presentation of results E. Conclusion III. Compressive strength of floating fragmented ice covers A. Introductory remarks B. Experimental setup and procedure C. Presentation of results and discussion D. Conclusions Literature cited Appendix A: Experimental results on ice jam initiation Appendix B: Effect of surface tension on submergence velocity of ice floes Appendix C: Experimental results for ice jam thickness study Appendix D: Experimental results on compressive strength of fragmented ice cover
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  • 123
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-78/1
    In: CRREL Report, 78-1
    Description / Table of Contents: The results of axial double point-load tests on disk samples of snow and ice obtained from the area of McMurdo Sound, Antarctica, are presented. They show the effects of temperature, sample length, load point diameter and specific gravity on failure load. It was determined that 13 samples should be tested to obtain a representative mean strength index. The results show that the axial double point-load test has good possibilities as a rapid field test for determining the unconfined comrpessive strength of snow and ice but that further evaluation of the variables affecting test results must be made.
    Type of Medium: Series available for loan
    Pages: iii, 11 Seiten , Illustrationen
    Series Statement: CRREL Report 78-1
    Language: English
    Note: CONTENTS Abstract Preface Introduction Test procedure Test program Test samples Number of test for determining strength index Effect of temperature Effect of sample length Effect of load point size Tests on snow Discussion Recommendations Literature cited
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  • 124
    Call number: ZSP-201-78/4
    In: CRREL Report, 78-4
    Description / Table of Contents: The use of radio-echo sounding records to indicate the presence of internal layers within large ice sheets is of interest to glaciologists because it offers a means of tracking the internal properties of the ice sheets over large distances. The interpretation of the reflections obtained in this manner is more valuable, however, if a physical property change relating to the glaciological regime can be related to the dielectric property change producing the radio-echo reflections. In this report, we use the measured physical properties of core to bedrock taken at Cape Folger, East Antarctica (66 deg 22 min s, 111 deg (E), 324-m depth), to compute a profile of dielectric properties and from this, a depth-reflection coefficient profile for comparison with observed radio-echo reflections. The measurements available on physical properties are: density variations, bubble size and shape changes, and crystal fabric variations. The depths of the strong reflections shown on the available radio-echo records are in reasonable agreement with the depths corresponding to the highest reflection coefficients computed from the combined physical property measurements. In calculations to differentiate the separate effects of different physical properties, it appears that density variations account for the primary contributions to the calculated dielectric property changes corresponding to the highest reflection coefficients. However, bubble changes alone can also account for reasonable, though lower, reflection coefficients at the appropriate depths. Crystal fabric variations correspond poorly with the reflection locations. Density variations are normally associated with depositional events in the history of the ice sheet.
    Type of Medium: Series available for loan
    Pages: vi, 12 Seiten , Illustrationen
    Series Statement: CRREL Report 78-4
    Language: English
    Note: CONTENTS Abstract Preface Nomenclature Introduction Derivation of the power reflection coefficient-depth variation Possible sources of dielectric constant variation with depth in ice sheets Ice density variations Effect of macroscopic impurity layers Effect of microscopic impurtty layers Changes in inclusion geometry Effect of crystal orientation changes Physical properties of the Cape Folger core Density-depth profile Air bubble-geometry depth profile Crystal orientation-depth profile Radio-echo sounding data Results and conclusions Literature cited
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  • 125
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-78/2
    In: CRREL Report, 78-2
    Description / Table of Contents: Many of the technical questions relating to iceberg transport are given brief, but quantitative, consideration. These include iceberg genesis and properties, the mechanical stability of icebergs at sea, towing forces and tug characteristics, drag coefficients, ablation rates, and handling and processing the iceberg at both the pick-up site and at the final destination. In particular the paper attempts to make technical information on glaciological and ice engineering aspects of the problem more readily available to the interested planner or engineer. Specific conclusions include: (1) No unprotected iceberg, no matter how long or wide, would be likely to survive the ablation caused by a long trip to low latitudes. (2) Icebergs that have a horizontal dimension exceeding 2 km may well be prone to breakup by long wavelength swells. (3) To avoid the dangers associated with an iceberg capsizing, the width of a 200-m thick iceberg should always be more than 300 m. (4) For towing efficiency the length/width ratio of a towed iceberg should be appreciably greater than unity. (5) For a pilot project, the selected iceberg would have to be quite small, if for no other reason than the practical availability of tug power.
    Type of Medium: Series available for loan
    Pages: v, 31 Seiten , Illustrationen
    Series Statement: CRREL Report 78-2
    Language: English
    Note: CONTENTS Abstract Preface Introduction Sources and properties of tabular icebergs Sources Characteristics of ice shelves near the ice front Characteristics of tabular icebergs Towing Geophysical and engineering considerations Tug characteristics Handling and processing Cutting and boring with thermal devices Penetration with electrothermal devices Electrothermal cutting Making vertical cuts by pre-split blasting Primary fragmentation by blasting Primary fragmentation by mechanical sawing Comminuting ice with machines Slurry pipelines Conclusion Literature cited
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  • 126
    Monograph available for loan
    Monograph available for loan
    Wageningen : Centre for Agricultural Publ. and Documentation
    Call number: PIK M 370-91-0161 ; MOP 44707 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 175 Seiten , Illustrationen
    Edition: 2., revised and extended edition
    ISBN: 9022006522
    Series Statement: Simulation monographs
    Language: English
    Note: Contents 1 Introduction 1.1 Purpose 1.2 Some terminology 1.3 Electrical analogues 1.4 State determined systems 1.5 Simulation languages 2 Exponential growth 2.1 Analytical and numerical integration 2.2 Simulation 2.3 Time constant and time interval of integration 2.4 Integration method and time interval 3 The growth of yeast 3.1 Description of the system 3.2 Relational diagrams 3.3 Simulation 3.4 Logistic growth 4 Interference of plants 4.1 Replacement series 4.2 Density of sowing 4.3 Simulation of plant interference 4.4 Further modelling aspects 4.4.1 The INDEX and MACRO feature 4.4.2 The INITIAL and DYNAMIC section 5 Growth and competition of Paramecium 5.1 Description of the system 5.2 A simulation program 5.3 Preliminary estimation of parameters 5.4 Final determination of parameters 5.5 Stochastic aspects 5.6 The programming of probability functions 6 Modelling of development, dispersion and diffusion 6.1 Introduction 6.2 Physiological age and development stage 6.3 Demographic models 6.3.1 Age-classes 6.3.2 Errors of approximation 6.3.3 The matrix method 6.4 Germination models 6.4.1 Boxcar train without dispersion 6.4.2 Boxcar train with constant relative dispersion 6.4.3 Boxcar train with controlled dispersion 6.4.4 Refinements 6.5 The flow of heat in soils 7 Growth and development of Helminthosporium maydis 7.1 Introduction 7.2 The weather 7.3 Appearance and growth of lesions 7.4 Sporophore or stalk formation 7.5 Sporulation of green stalks 7.6 Sporulation of dried stalks 7.7 Dispersal of spores 7.8 Germination of spores and penetration of germtubes 7.9 Timing, initialization and output organization 7.10 Results and sensitivity analyses 8 Population models for fruit-tree red spider miteand predatory mites 8.1 Fruit-tree red spider mite 8.2 Predatory mite, Amblyseius potentillae 8.3 Relations between predator and prey 8.4 Preference as a competitive process 8.5 Verification 9 Solutions of the exercises References Appendix A Appendix B Index
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  • 127
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-76/21
    In: CRREL Report, 76-21
    Description / Table of Contents: The effects of snow temperature and initial density on the stress vs density and stress vs deformation relationships were investigated for shallow compacted snow in the density range of 0.28 to 0.76 g/cu m, for stress range of 0.5 to 72 bars and a temperature range of -1 to -34 C at a deformation rate of 40 cm/s. A decrease in temperature increases the resistance to stress, the effect increasing with applied stress. For any stress, an increase in the initial density results in an increase in the resulting density, the effect decreasing with an increase in stress. The approximate yield envelopes, which define the stress required to initiate any deformation of snow of a particular density and temperature, were determined. Rapid compaction of snow results in extensive recrystallization, significantly different from that of naturally compacted snow. At a stress of 72 bars, transformation to ice occurs only at temperature above -10C.
    Type of Medium: Series available for loan
    Pages: vi, 47 Seiten , Illustrationen
    Series Statement: CRREL Report 76-21
    Language: English
    Note: CONTENTS Abstract Preface Nomenclature Introduction Description of study Sample preparation Test equipment and procedure Discussion of results Stress-density relationship Stress-deformation relationship Summary and conclusions Microstructural examination of artifically compacted snow Analytical techniques Results and discussion Conclusions Literature cited Appendix: Photographs of oscilloscope traces
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  • 128
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-76/7
    In: CRREL Report, 76-7
    Description / Table of Contents: This report covers a series of cantilever beam tests designed to determined the efficacy of adding reinforcement to an ice cover. Tests were run using 1-in.-diam tree branches, 3/16-in.-diam wire rope and 9/16-in. half-round wood dowels as reinforcement for both seawater and freshwater ice. The results show a definite advantage derived from using reinforcement, even when poorly placed. The results also show that reinforced ice carries a load even after it cracks. Thus, after the initial cracks there is time to remove people and equipment before final breakthrough. One must bear in mind, however, that reinforcement has disadvantages. The darker reinforcement absorbs solar radiation and thereby causes earlier weakening of the ice cover. Also, in many cases the time and effort required to place reinforcement may exceed those required to achieve equal strength by additional thickening of the ice sheet. This study has shown that understanding of the failure mechanism of ice under repetitive loading is poor and that future studies should be performed on this problem. Also, this study covered only cantilever beams. The actual field problem is strengthening a three-dimensional sheet. Hence, distribution and orientation of the reinforcement should be addressed in future studies.
    Type of Medium: Series available for loan
    Pages: v, 12 Seiten , Illustrationen
    Series Statement: CRREL Report 76-7
    Language: English
    Note: Contents Abstract Preface Summary Conversion factors: U.S. customary to SI metric units Introduction Typical methods of constructing ice bridges Current knowledge Test program Objectives Equipment Procedure Data General Specific ice sheets Test results Conclusions Recommendations Literature cited
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  • 129
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-76/9
    In: CRREL Report, 76-9
    Description / Table of Contents: Access to study areas may be an important factor in long-term field-oriented research, particularly in-regions without well-developed road and communications systems. In a wildland hydrometeorology research project in subarctic Alaska, access to and within a 40-square-mile research watershed has been developed both in accordance with a general plan prepared at project inception and in response to developing research requirements. Foot trails, trails for 'off-road' low-ground-pressure tracked vehicles, helicopter transport, long-term data recorders, and radio telemetry of data have all been incorporated in an access and communications system. Cost estimates indicate that incorporation of gravel roads into the system would be economically advantageous, given adequate funding for initial road construction.
    Type of Medium: Series available for loan
    Pages: iv, 9 Seiten , Illustrationen
    Series Statement: CRREL Report 76-9
    Language: English
    Note: Contents Abstract Preface Conversion factors for U.S. customary and SI units Introduction Access within the Caribou-Poker Creeks Research Watershed Trail access Helicopter access Road access Alternative approaches Long-term recorders Telemetry systems Remote sensing Relative costs A desirable system Selected bibliography
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  • 130
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-76/13
    In: CRREL Report, 76-13
    Description / Table of Contents: The thermal structure and ice conditions of Lake Champlain, a mid-latitude large lake, near Shelburne Point, Vermont, were studied during the winter of 1974-75. The lake was instrumented to a depth of 8.5 m with a string of highly calibrated thermistors, connected to a data logger on shore which recorded water temperatures every four hours. An ice mooring system was developed to anchor the thermistor string so that ice and water temperatures could be obtained at known levels. This temperature recording system measured vertical and horizontal variations in ice and water temperature regimes during ice formation, growth and decay. Meteorological data were measured during the winter period November 1974 through March 1975 at the site. Ice stratigraphy was determined for the ice at the site at its maximum seasonal growth for comparison with ice from St. Albans Bay (at the northern end of Lake Champlain) which had formed earlier. Correlations were determined between ice growth and accumulated degree days of freezing. The operation of a bubbler system installed near the measurement site around a service dock was observed.
    Type of Medium: Series available for loan
    Pages: vii, 22 Seiten , Illustrationen
    Series Statement: CRREL Report 76-13
    Language: English
    Note: CONTENTS Abstract Preface Summary Introduction Climate Site selection Instrumentation, measurements and calibration Installation of automatic water temperature recording system Visual observations and ice structure St. Albans Shelburne Analysis Temperature comparison Water temperature measuring system Changes in water temperature Wind Degree-days of freezing Prediction of ice formation Bubbler system Conclusions Recommendations Literature cited
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  • 131
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-76/3
    In: CRREL Report, 76-3
    Description / Table of Contents: A world-wide review of the literature applicable to the design of harbors and channels in cold regions was conducted. Forces due to ice movement present the dominant factor in the design of marine structures in cold regions. Expressions for calculating the ice force are presented. Other factors relating to design criteria such as construction materials, structure geometry, and methods of ice suppression are discussed.
    Type of Medium: Series available for loan
    Pages: iii, 32 Seiten
    Series Statement: CRREL Report 76-3
    Language: English
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  • 132
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-76/22
    In: CRREL Report, 76-22
    Description / Table of Contents: Several membrane materials used or considered for MESL (membrane-enveloped soil layer) utilization of poor soils in road construction have been tested for cold effect on puncture and stiffness. PE (polyethylene) film was also tested for solvent soak effects. A simple blunt needle apparatus was devised for puncture testing. For plastic films (mainly PE), both puncture resistance and stiffness increase at low temperature (0 F, -18 C). For non-woven, spunbonded fabrics these properties are little affected by cold. For both non-wovens and PE film, puncture and bending strengths increase linearly with weight or thickness. The slope is steeper for the non-wovens, which generally are stronger on a per unit weight basis. PE film soaked in a hydrocarbon solvent swelled approximately 17% and lost about 30-40% its puncture strength. These effects are apparently reversible upon drying. Consideration has been given to sealing and patching requirements and to the drying of sealant liquids when adhering film to film. Also considered have been pos­sible slippage related to the reported low angle of friction of plastic films in soil and the possibility of lamination for improved membrane properties.
    Type of Medium: Series available for loan
    Pages: v, 60 Seiten , Illustrationen
    Series Statement: CRREL Report 76-22
    Language: English
    Note: CONTENTS Page Abstract Preface Introduction Experimental Materials Apparatus Procedure Results Discussion PE solvent soak and swelling PE solvent soak and puncture Film puncture rate effect Bending orientation Comparative tables and graphs Puncture and temperature Bending and temperature Test result vs thickness and weight General considerations Conclusion and recommendations Literature cited Appendix Detailed data tables Denier explanation
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  • 133
    Call number: ZSP-553-197,4
    In: Meddelelser om Grønland
    Type of Medium: Monograph available for loan
    Pages: 25 S.
    ISBN: 8717022185
    Series Statement: Meddelelser om Grønland 197,4
    Language: English
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  • 134
    Monograph available for loan
    Monograph available for loan
    Berlin : Staatsverl.d.DDR
    Call number: MOP 44902
    Type of Medium: Monograph available for loan
    Pages: 218 S.
    Uniform Title: Naucno-techniceskaja integracija socialisticeskich stran
    Language: German
    Location: MOP - must be ordered
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  • 135
    Monograph available for loan
    Monograph available for loan
    Basel [u.a.] : Birkhäuser
    Call number: MOP 44180
    Type of Medium: Monograph available for loan
    Pages: XI, 264 S.
    ISBN: 3764307889
    Series Statement: Lehrbücher und Monographien aus dem Gebiete der exakten Wissenschaften : Mathematische Reihe 53
    Uniform Title: Kurs teorii verojatnostej
    Language: German
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  • 136
    Monograph available for loan
    Monograph available for loan
    Associated volumes
    Call number: M 94.0014/2
    In: Der Chemielaborant
    Type of Medium: Monograph available for loan
    Pages: 256 S.
    ISBN: 3441910540
    Classification:
    C.4.1.
    Language: German
    Location: Upper compact magazine
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  • 137
    Call number: AWI Bio-99-0172
    Description / Table of Contents: Die langerwartete 2. Auflage des Handbuch der Samenkunde - in der Art der Gestaltung wohl einmalig - gibt allen Saatguterzeugern, -käufern und -verkäufern, allen Botanikern, Biologen, Genetikern, Züchtern und Beratern eine unerschöpfliche Quelle der Wissensvermittlung in die Hand. Das Handbuch ist Nachschlagewerk, Fachlexikon und Bestimmungsbuch zugleich. Die über 2500 Samenbeschreibungen - des besseren Auffindens wegen nach den Familien Gattungen und Arten geordnet - werden durch 1672 Feinstrichzeichnungen, die das Charakteristische der einzelnen Samen klarer als Photographien hervorheben können, in bester Weise veranschaulicht und helfen so, die notwendigen Kenntnisse über den Samen zu vermitteln. Die Familien- und Artnamen erscheinen jeweils in lateinischer, deutscher und englischer Sprache, das gleiche gilt auch für das umfangreiche Register der Pflanzennamen und botanischen Kunstausdrücke, so daß das Werk über Deutschlands Grenzen hinaus internationale Bedeutung hat.
    Type of Medium: Monograph available for loan
    Pages: 655 S. , Ill.
    Edition: 2. Aufl.
    ISBN: 3769002725
    Language: German
    Note: Inhaltsverzeichnis: Frucht und Same, Allgemeines. - Früchte und Samen bei den einzelnen Familien und Arten. - Bestimmungsschlüssel der landwirtschaftlich wichtigen Arten. - Literaturverzeichnis. - Register der lateinischen, deutschen und englischen Pflanzennamen und von botanischen Kunstausdrücken. - Berichtigungen.
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  • 138
    Monograph available for loan
    Monograph available for loan
    Moskva : Izdatel'stvo "Planeta"
    Call number: AWI P7-83-0402
    Description / Table of Contents: Arktis und Antarktis - diese beiden Begriffe bringen wir sogleich mit den Namen berühmter Entdecker in Zusammenhang. Die Arktis wird heute häufig als ,,warme Arktis" bezeichnet, denn sie ist zum Teil bewohnt, hier wird Erz und Erdgas gefördert, wird Holz geschlagen, werden Fische gefangen. Auch ,,nahe Arktis" wird sie genannt, denn Schiffskonvois ziehen auf dem Nördlichen Seeweg dahin, und mit dem Flugzeug ist jeder Punkt der Arktis das ganze Jahr hindurch erreichbar. Doch wie sehr der Mensch in den Polargebiefen auch heimisch werden und wie man diese Gebiete auch immer nennen mag, das Leben und die Arbeit fern von der ,,häuslichen Heimat" ist stets schwierig und riskant, erfordert stets großen Mut. Dieses Buch schildert nur einzelne Episoden aus der Entdeckungsgeschichte und dem Leben der beiden Pole unserer Erde, berichtet nur kurz von den kühnen Menschen, die in die Polargebiete vorgedrungen sind und dort arbeiten. Nach der Arktis und der Antarktis führt uns der Fotojournalist Gennadi Kopossow.
    Description / Table of Contents: Arctica and Antarctica, two words which have become associated with the exploration of new lands. Now people refer to parts of Arctica as the Warm Arctica, having in mind its inhabited regions where ores, gas, timber and fish are obtained. There is also the Near Arctlca, where caravans of ships safely sail the Northern Sea Route, and, with the help of aircraft, any part of which is accessible the year round. However, much as the people settled these polar regions, whatever they call them, living and working far from mainland is accompanied by risk, courage and hardships. This book gives only a few pages from the history of the two poles of the planet, a few brief sketches of the courageous men who live and work in these regions, merely separate episodes seen and recorded by the press photographer Gennady Koposov in the Arctic and Antarctic.
    Description / Table of Contents: Арктика и Антарктида. Эти слова стали символом мужества и отваги первооткрывателей, осваивающих суровые полюсы Земли. Сейчас говорят про Арктику — "Теплая Арктика", имея в виду ее обжитые районы, где люди добывают руду и газ, лес и рыбу. Говорят, "Близкая Арктика", видя, как караваны судов уверенно идут по Северному морскому пути и как в любое время года на любой ее участок прилетают самолеты полярной авиации. Антарктида. Природа наделила ее чертами мужественными и властными. Это "жестокий" край, и все же метеорологи, аэрологи, геофизики, биологи, медики, научные сотрудники десятков других специальностей стремятся в эту суровую страну. Однако как бы не обжили люди полярные районы планеты, какими эпитетами не называли их, жизнь и работа "вдали от Большой земли" сопровождается там трудностями и риском. Эта книга — лишь отдельные страницы из истории открытий и жизни двух полюсов планеты, короткие рассказы об отважных людях, обживающих полярные земли, и отдельные фотоочерки, запечатленные одним из ведущих фотокорреспондентов журнала "Огонек" Геннадием Колосовым в Арктике и Антарктиде. Творчество Колосова неразрывно связано с Арктикой и Антарктидой, с завидным постоянством возвращается он в полюбившиеся ему полярные районы, привозит из командировки все новые и новые фотоработы. Результатом этих поездок и явилась настоящая книга.
    Type of Medium: Monograph available for loan
    Pages: [200 Seiten] , Illustrationen
    Language: Russian , English , German
    Note: Inhaltsverzeichnis = Contents = Soderžanie Die Flagge der Heimat = The flag of the motherland = Flag rodiny Arktis = Arctic = Arktika Die Drift geht weiter = Drift-ice research continues = Drejf prodolžaetsja Eisbezwinger = Ice fighters = Ledovye bojcy Auf fernen Inseln = On distant islands = Na dalekich ostrovach Antarktis = Antarctic = Antarktida Der sechste Erdteil = The sixth continent = Šestoj kontinent Polarflieger = Polar region pilots = Poljarnye letčiki Der Kältepol = The pole of cold = Poljus choloda Spuren im Schnee = Tracks on the snow = Sledy na snegu , Text in russischer, englischer und deutscher Sprache
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  • 139
    Call number: AWI Bio-89-0001
    Type of Medium: Monograph available for loan
    Pages: XLIV, 1252 S. : Ill. ; 25 cm
    ISBN: 0872010007
    Language: English , French
    Note: Contents: Preface / G. A. Llano. - Welcoming Remarks / W. S. Benninghoff. - The Third Symposium in Historical Perspective / G. A. Knox. - Sir George E. R. Deacon: An Appreciation / K. J. Bertrand. - The Southern Ocean: History of Exploration / Sir George E. R. Deacon. - The Symposium. - Part I: The Structure and Function of Antarctic Marine Phytoplankton Ecosystems. - The Antarctic Marine Ecosystem / Joel W. Hedgpeth. - Primary Production and the Factors Controlling Phytoplankton Growth in the Southern Ocean / O. Holm-Hansen, S. Z. El-Sayed, G. A. Franceschini, and R. L. Cuhel. - Phytoplankton Biomass and Productivity in the Subtropical Convergence Area and Shelves of the Western Indian Subantarctic Islands / Jacqueline Plancke. - Sea Ice Habitats of Signy Island (South Orkneys) and Their Primary Productivity / Terence M. Whitaker. - Dissolved Oxygen and pH Increases by Primary Production in the Surface Water of Arthur Harbor, Antarctica, 1970-1971 / S. V. Shabica, J. W. Hedgpeth, and P. K. Park. - Heterotrophic Activity of Microorganisms in Antarctic Waters / R. Y. Morita, R. P. Griffiths, and S. S. Hayasaka. - Vitamins in the South Polar Seas: Distribution and Significance of Dissolved and Particulate Vitamin B12, Thiamine, and Biotin in the Southern Indian Ocean / A. F. Caducei and R. L. Cuhel. - Discussion. - Part II: The Structure and Function of Antarctic Marine Benthic Ecosystems. - Adaptations within the Antarctic Marine Benthic Ecosystem / Patrick M. Arnaud. - Bacterial Sulfur and Nitrogen Cycles in Sedimentary Deposits of "Fjord Bossière" (Kerguelen Archipelago) / D. Delille. - Antarctic Soft-Bottom, Macrobenthic Community Adaptations to a Cold, Stable, Highly Productive, Glacially Affected Environment / Michael D. Richardson and Joel W. Hedgpeth. - Ecological Adaptations by Antarctic Poikilotherms to the Polar Marine Environment / Martin G. White. - Scoloplos marginatus mcleani: Life Cycle and Adaptations to the Antarctic Benthic Environment / P. Hardy. - Benthic Bionomy of the Continental Shelf of the Kerguelen Archipelago, Macrofauna 2, Diversity of Benthic Annelid Population in a Fjord Close to the Morbihan Gulf / D. Desbruyeres. - Seasonal Variations in the Structure of Populations of Antarctic Polynoids and the Part Played by Polychaetes in the Biocenoses of the Arctic and Antarctic / V. G. Averincev. - Benthic Bionomy of the Continental Shelf of the Kerguelen Islands: Quantitative Data on the Echinoderms of the Morbihan Gulf / Alain Guille. - Seasonal Alterations in Coastal Communities in the Davis Sea / E. N. Gruzov. - First Investigations on the Density of Soft Bottom Meiofauna in Morbihan Bay (Kerguelen Islands) / J. Soyer and F. de Bovee. - Foods and Feeding Characteristics of Antarctic Asteroids and Ophiuroids / John H. Dearborn. - Analysis of the Gigantism and Dwarfness of Antarctic and Subantarctic Gammaridean Amphipoda / Claude De Broyer. - The Breeding Biology of Chorismus antarcticus (Pfeffer) and Notocrangon antarcticus (Pfeffer) (Crustacea, Decapoda) and Its Bearing on the Problems of the Impoverished Antarctic Decapod Fauna / J. Garrey H. Maxwell. - A Preliminary Investigation of the Lipids of Chorismus antarcticus (Pfeffer) (Crustacea, Decapoda) at South Georgia / Andrew Clarke. - Some Additions to Schemes of the Vertical Zonation of Marine Bottom Fauna / A. P. Andriashev. - Quantitative Studies on the Soft-Bottom Macrobenthic Animal Communities of Shallow Antarctic Bays / V. A. Gallardo, J. G. Castillo, M. A. Retamal, A. Yáñez, H. l. Moyano, and J. G. Hermosilla. - Discussion. - Part Ill: Adaptations in Antarctic Vertebrates (Physiology). - Mechanisms of Cold Adaptation in Polar Marine Animals / Bruce L. Umminger. - The Significance of Vertebrates in the Antarctic Marine Ecosystem / Richard M. Laws. - The Role of Glycoprotein Antifreezes in the Survival of Antarctic Fishes / Arthur L. DeVries and Yuan Lin. - New Cytological, Biochemical, and Physiological Data on the Colorless Blood of the Channichthyidae (Pisces, Teleosteans, Perciformes) / J. C. Hureau, J. M. Fine, M. Marneux, and D. Petit. - Respiratory and Circulatory Adaptations to the Absence of Hemoglobin in Chaenichthyid Fishes / Edvard A. Hemmingsen and Everett L. Douglas. - Thermo- and Osmoregulatory Responses Induced by Heating and Cooling the Rostral Brainstem of the Adelie Penguin / H. T. Hammel, J. E. Maggert, E. Simon, L. Crawshaw, and R. Kaul. - Body Temperature Regulation of the Emperor Penguin (Aptenodytes forsteri G.) During Physiological Fasting / Yvon Le Maho, Philippe Delclitte, and René Groscolas. - Cardiovascular Adaptations of the Giant Petrel, Macronectes giganteus, to the Antarctic Environment / David E. Murrish and Charles L. Guard. - Temperature Regulation in the Newborn Weddell Seal, Leptonychotes weddelli / R. Elsner, D. D. Hammond, D. M. Denison, and R. Wyburn. - Discussion. - Part IV: Adaptations in Antarctic Vertebrates (Ecology). - Evolution Within Pelagic Ecosystems: Aspects of the Distribution and Evolution of the Family Myctophidae / Richard F. McGinnis. - Aspects of the Diet of the Antarctic Silverfish, Pleuragramma antarcticum / H. H. DeWitt and T. L. Hopkins. - The Bacterial Microflora in the Digestive Tracts of Penguins and Fishes from the Kerguelen Islands / R. Lesel and J. P. Menet. - The Rockhopper Penguin (Eudyptes chrysocome moseleyi), of Saint Paul and New Amsterdam Islands / T. Duroselle and B. Tollu. - Adaptive Significance of the Reoccupation Period of the Adelie Penguin / E. B. Spurr. - Interactions Between South Polar Skuas and Adelie Penguins / Dietland Müller-Schwarze and Christine Müller-Schwarze. - Comparative Feeding Ecology of the Giant Petrels Macronectes giganteus (Gmelin) and M. halli (Mathews) / G. W. Johnstone. - Feeding Methods in Seabirds: A Comparison of Polar and Tropical Nesting Communities in the Eastern Pacific Ocean / David G. Ainley. - Adaptations of Arctic Terns and Antarctic Terns Within Antarctic Ecosystems / D. F. Parmelee. - Distribution and Abundance of Seals in the Pack Ice of the Pacific Sector of the Southern Ocean / James R. Gilbert and Albert W. Erickson. - Adaptations of Weddell and Ringed Seals to Exploit the Polar Fast Ice Habitat in the Absence or Presence of Surface Predators / Ian Stirling. - Food Consumption of Seals in the Antarctic Pack Ice / Torger Øritsland. - The Leopard Seal (Hydrurga leptonyx) at Palmer Station, Antarctica / R. J. Hofman, R. A. Reichle, D. B. Siniff, and D. Müller-Schwarze. - Distribution of Toothed Whales in the Antarctic Ocean / Masaharu Nishiwaki. - Discussion. - Part V: The Structure and Function of Antarctic Freshwater Ecosystems. - Antarctic Freshwater Ecosystems: Review and Synthesis / Ronald B. Heywood. - Production and Periodicity of Antarctic Freshwater Phytoplankton / J. J. Light. - Studies on Some Saline Lakes of the Vestfold Hills, Antarctica / K. R. Kerry, D. R. Grace, R. Williams, and H. R. Burton. - Nitrogen and Phosphorus Availability to Plankton: and Benthic Communities in Lake Bonney, Southern Victoria Land, Antarctica / Robert C. Hoehn, Bruce C. Parker, Richard D. Fortner, Barron L. Weand, James A. Craft, Larry S. Lane, Robert W. Stavros, Harold G. Sugg, Jr., and Jeffrey T. Whitehurst. - Changes in Dissolved Organic Matter, Photosynthetic Production, and Microbial Community Composition in Lake Bonney, Southern Victoria Land, Antarctica / Bruce C. Parker, Robert C. Hoehn, Robert A. Paterson, James A. Craft, Larry S. Lane, Robert W. Stavros, Harold G. Sugg, Jr., Jeffrey T. Whitehurst, Richard D. Fortner, and Barron L. Weand. - Discussion. - Part VI: The Structure and Function of Antarctic Terrestrial Ecosystems. - Climatic Relationships in Antarctic and Northern Hemisphere Populations of a Cosmopolitan Moss, Bryum argenteum Hedw. / R. E. Longton and Marjorie A. Maclver. - The Growth of Mosses in Two Contrasting Communities in the Maritime Antarctic: Measurement and Pre , Includes some contributions in French
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  • 140
    Call number: 11/M 95.0041
    Type of Medium: Monograph available for loan
    Pages: 215 S.
    Edition: 3. Aufl., 61.-80. Tsd.
    ISBN: 3440040739
    Series Statement: Kosmos-Naturführer
    Classification:
    Mineralogy
    Language: German
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  • 141
    Monograph available for loan
    Monograph available for loan
    Hamburg : Deutscher Wetterdienst, Seewetteramt
    Associated volumes
    Call number: AWI A19-96-0477 ; MOP Per 278(96)
    In: Einzelveröffentlichungen / Deutscher Wetterdienst, Seewetteramt Hamburg, Nr. 96
    Type of Medium: Monograph available for loan
    Pages: 128 Seiten
    ISSN: 0072-1603
    Series Statement: Einzelveröffentlichungen / Deutscher Wetterdienst, Seewetteramt Hamburg 96
    Language: German
    Note: Inhaltsverzeichnis: Die Unternehmen "Sachsen" 1940 und 1942 Unternehmen "Knospe" Spitzbergen 1941/42 Unternehmen "Nussbaum" Spitzbergen 1942/43 Unternehmen "Holzauge" Ostgrönland 1942/43 Unternehmen "Kreuzritter" Spitzbergen 1943/44 Unternehmen "Bassgeiger" Ostgrönland 1943/44 Unternehmen "Schatzgräber" Franz-Joseph-Land 1943/44 Unternehmen "Edelweiss" Ostgrönland 1944 Unternehmen "Edelweiss II" Ostgrönland 1944 Unternehmen "Haudegen" Spitzbergen 1944/45 Literaturverzeichnis Karte der Einsatzorte der Unternehmen
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  • 142
    Monograph available for loan
    Monograph available for loan
    San Diego : Academic Press
    Call number: AWI A5-96-0587
    Type of Medium: Monograph available for loan
    Pages: 467 Seiten , Illustrationen
    ISBN: 0127329501
    Language: English
    Note: Contents Preface Units and Numerical Values Chapter 1 A BRIEF SURVEY OF THE ATMOSPHERE 1.1 Introduction 1.2 Origin and Composition of the Atmosphere 1.3 The Distribution of Atmospheric Mass and Gaseous Constituents 1.4 Charged Particles in the Atmosphere 1.5 The Temperature Distribution 1.6 Winds in the Earth's Atmosphere 1.7 Precipitation Problems Chapter 2 ATMOSPHERIC THERMODYNAMICS 2.1 The Gas Laws 2.2 The Hydrostatic Equation and Its Applications 2.3 The First Law of Thermodynamics 2.4 Latent Heats 2.5 Adiabatic Processes 2.6 Water Vapor in the Air 2.7 The Concept of Static Stability 2.8 The Second Law of Thermodynamics and Entropy 2.9 Thermodynamic Functions and Equilibrium Conditions Problems Chapter 3 EXTRATROPICAL SYNOPTIC-SCALE DISTURBANCES 3.1 The 500-mb Flow 3.2 Surface Weather Elements 3.3 Interpretation of Synoptic Surface Reports 3.4 Upper Level Structure 3.5 Thickness and Its Relationship to Vertical Structure Problems Chapter 4 ATMOSPHERIC AEROSOL AND CLOUD MICROPHYSICAL PROCESSES 4.1 Atmospheric Aerosol 4.2 Nucleation of Water Vapor Condensation 4.3 The Microstructure of Warm Clouds 4.4 Growth of Cloud Droplets in Warm Clouds 4.5 The Microphysics of Cold Clouds 4.6 Thunderstorms Problems Chapter 5 CLOUDS AND STORMS 5.1 Cloud Morphology 5.2 The Air-Mass Thunderstorm 5.3 Severe Storms 5.4 Hurricanes 5.5 Extratropical Cyclonic Storms 5.6 Artificial Modification of Clouds and Precipitation Problems Chapter 6 RADIATIVE TRANSFER 6.1 The Spectrum of Radiation 6.2 Absorption and Emission of Radiation by Molecules 6.3 Quantitative Description of Radiation 6.4 Blackbody Radiation 6.5 Absorptivity and Emissivity 6.6 Atmospheric Absorption of Solar Radiation 6.7 Atmospheric Absorption and Emission of lnfrared Radiation 6.8 Scattering of Solar Radiation 6.9 The Role of Radiative Transfer in the Global Energy Balance Problems Chapter 7 THE GLOBAL ENERGY BALANCE 7.1 The Globally Averaged Atmospheric Energy Balance 7.2 The Energy Balance of the Upper Atmosphere 7.3 The Tropospheric Energy Balance 7.4 The Energy Balance at the Earth's Surface 7.5 Time Variations in the Energy Balance Problems Chapter 8 ATMOSPHERIC DYNAMICS 8.1 Coordinate Systems 8.2 Apparent Forces in a Rotating Coordinate System 8.3 Real Forces 8.4 The Horizontal Equation of Motion 8.5 The Vertical Equation of Motion 8.6 The Thermal Wind 8.7 The Thermodynamic Energy Equation 8.8 The Continuity Equation 8.9 The Primitive Equations Problems Chapter 9 THE GENERAL CIR CU LA TION 9.1 Introduction 9.2 Thermally Driven Circulations in the Absence of Rotation 9.3 The Influence of Planetary Rotation upon Thermally Driven Circulations 9.4 Thermally Driven Circulations in the Tropics 9.5 Baroclinic Disturbances 9.6 The Dissipation of Kinetic Energy 9.7 The Kinetic Energy Cycle 9.8 The Role of the Atmospheric General Circulation in the Hydrologic Cycle 9.9 The Atmospheric Transport of Energy 9.10 The Atmosphere as a Heat Engine Problems Index
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  • 143
    Call number: M 95.0200/3 ; AWI Bio-95-0065-3
    In: Die Kieselalgen Deutschlands, Österreichs und der Schweiz
    Type of Medium: Monograph available for loan
    Pages: 816 S. : mit 609 Abb.
    Edition: Reprint [der Ausg.] 1961-1966
    ISBN: 3874291154
    Classification:
    Paleontology
    Language: German
    Location: Upper compact magazine
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  • 144
    Series available for loan
    Series available for loan
    Berlin : Nationalkomitee für Geodäsie und Geophysik der Deutschen Demokratischen Republik
    Associated volumes
    Call number: MOP Per 581(3/40) ; ZSP-319/C-40 ; ZSP-319/C-40(2.Ex.)
    In: Geodätische und Geophysikalische Veröffentlichungen : Reihe 3, Physik der festen Erde, Heft 40
    Type of Medium: Series available for loan
    Pages: 68 Seiten , Illustrationen
    ISSN: 0435-6187
    Series Statement: Geodätische und Geophysikalische Veröffentlichungen : Reihe 3, Physik der festen Erde 40
    Language: German , Russian
    Note: Inhaltsverzeichnis Summary, Rezjume 1. Einleitung 2. Das Bewegungsverhalten von Eismassen, seine Untersuchung und Modellierung 2.1. Zum Modellbegriff 2.2. Typische Eismassen und ihr Bewegungsverhalten 2.2.1. Zur Theorie der Eisbewegung 2.2.2. Gletscher 2.2.3. Schelfeis und Eiskappe 2.3. Die Ermittlung von Eisbewegungen durch geodätische Verfahren 2.3.1. Die Vorplanung der Messungen 2.3.2. Die Durchführung der Messungen 2.3.3. Reduktion der Beobachtungen 2.3.4. Berechnung der Eisbewegungen 2.4. Das trendbehaftete vektorielle Zufallsfeld - Modell zur Beschreibung des Geschwindigkeitsfeldes einer Eismasse - in der Theorie stochastischer Prozesse 2.4.1. Definition des Vektorfeldes 2.4.2. Das Geschwindigkeitsfeld einer Eismasse - trendbehaftetes vektorielles Zufallsfeld 2.4.3. Definition eines vektoriellen Zufallsfeldes 2.4.4. Wahrscheinlichkeitsdichte und Verteilungsfunktion 2.4.5. Die Momente und die Korrelationsfunktionen 2.4.6. Vektorielle Zufallsfelder mit Hormalverteilungsgesetz 2.4.7. Homogene und isotrope vektorielle Zufallsfelder 2.4.8. Das Ergodenproblem 3. Das Konzept der Kollokation und seine Anwendung auf die Bearbeitung von Eisbewegungsmessungen 3.1. Zur Theorie der Kollokation 3.1.1. Das Kollokationsmodell von Moritz [40] 3.1.2. Nichtlineare Prädiktion nach Grafarend [12] 3.1.3. Kollokation von Vektorgrößen 3.2. Analyse und Bearbeitung des Datenmaterials 3.2.1. Die Trendbestimmung 3.2.2. Die Analyse des Zufallsfeldes 3.3. Das Kollokationsmodell bei der Bearbeitung von Eisbewegungsmessungen 3.3.1. Zuordnung und Interpretation der Größen 3.3.2. Zur zeitlichen Variation des Geschwindigkeitsfeldes einer Eismasse 3.3.3. Kollokation mit den ursprünglichen reduzierten Beobachtungen 4. Praktische Untersuchungen 4.1. Geschwindigkeitsquerprofile des Fedtschenko-Gletschers (Pamir) 4.2. Geschwindigkeitslängsprofil des Kongsvegen-Gletschers (Spitzbergen) 4.3. Geschwindigkeitslängsprofil des Hays-Gletschers (Antarktika) 4.4. Geschwindigkeitsquerprofil des Ross-Schelfeises (Antarktika) 4.5. Vergleich mit früheren Untersuchungen zur Abschätzung von Geschwindigkeitskorrelationen natürlicher Eismassen 5. Zusammenfassung 6. Literaturverzeichnis , Zusammenfassung in englischer und russischer Sprache
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  • 145
    Call number: M 94.0014/1
    In: Der Chemielaborant
    Type of Medium: Monograph available for loan
    Pages: 222 S.
    ISBN: 3441910532
    Classification:
    C.4.1.
    Language: German
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  • 146
    Call number: MOP Per 719(47,2)
    In: Abhandlungen und Berichte
    Type of Medium: Monograph available for loan
    Pages: 51 S. , Ill., graph. Darst.
    ISBN: 3486240412 , 3-486-23511-7
    Series Statement: Abhandlungen und Berichte / Deutsches Museum 47,2
    Language: German
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  • 147
    Series available for loan
    Series available for loan
    Boulder : The Geological Society of America
    Associated volumes
    Call number: S 90.0095(158)
    In: Special paper
    Type of Medium: Series available for loan
    Pages: 82 S.
    ISBN: 081372158X
    Series Statement: Special paper / Geological Society of America 158
    Language: English
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  • 148
    Monograph available for loan
    Monograph available for loan
    Oxford [u.a.] : Pergamon Press
    Call number: AWI A6-01-0208
    Type of Medium: Monograph available for loan
    Pages: XVI, 241 S. , graph. Darst.
    Edition: 1. Aufl.
    ISBN: 0080216153
    Series Statement: Pergamon international library of science, technology, engineering and social studies
    Language: English
    Note: Contents: Preface. - List of Symbols Commonly Used in the Text. - Acknowledgements. - 1 Introduction. - 2 Properties of Sea Water Relevant to Physical Oceanography. - Introduction. - Density. - Measurement of density, temperature and salinity. - Relative density, sigma-t and specific volume. - Tables for density and specific volume as functions of temperature, salinity and pressure. - Sources of data. - 3 The Basic Physical Laws Used in Oceanography and Classifications of Forces and Motions in the Sea. - Basic laws. - Classification of forces and motion. - 4 The Equation of Continuity of Volume. - The concept of continuity of volume. - The derivation of the equation of continuity of volume. - An application of the equation of continuity. - 5 Stability and Double Diffusion. - Static stabiIity. - Criterion for static stability (E). - Numerical values for stability. - Double diffusion. - Dynamic stability. - 6 The Equation of Motion in Oceanography. - The form of the equation of motion. - Obtaining solutions to the equations, including boundary conditions. - The derivation of the terms in the equation of motion. - The pressure term. - Transforming from axes fixed in space to axes fixed in the rotating earth. - Gravitation and gravity. - The Coriolis terms. - Other accelerations. - Coordinate systems. - 7 The Role of the Non-Linear Terms in the Equations of Motion. - The non-linear terms in the equation of motion. - The friction term for the instantaneous velocity. - What is the source of the difficulty?. - Scaling and the Reynolds Number. - Reynolds stresses. - Equations for the mean or average motion. - Reynolds stresses and eddy viscosity. - Scaling the equations of motion. - Dynamic stabiIity. - The effect of density variations on dynamic stability. - Effects of rotation. - 8 Currents Without Friction: Geostrophic Flow. - Hydrostatic equiIibrium. - Inertial flow. - GeopotentiaI. - Geopotential surfaces and isobaric surfaces. - The geostrophic equation. - Why worry about the geostrophic equation?. - The geostrophic method for calculating relative velocities. - An example of the calculation of a geostrophic velocity profile. - An alternative derivation of the geostrophic equation. - The 'thermal wind' equations. - Absolute velocities. - Relations between isobaric and level surfaces. - Relations between isobaric and isopycnal surfaces. - Comments on the geostrophic equation. - Justification for using the geostrophic approach to obtain the speeds of strong currents. - 9 Currents With Friction. - Wind-driven circulations - introduction. - Nansen's qualitative argument. - The equations of motion with friction included. - Ekman's solution to the equations of motion with friction present. - Comments on the above experimental observations. - Transport and upwelling. - Upwelling or downwelling away from boundaries. - Bottom friction and shallow water effects. - Limitations of the Ekman theory. - Sverdrup's solution for the wind-driven circulation. - Orders of magnitude of the terms. - Application of the Sverdrup equation. - The general form of the Sverdrup equation. - The mass transport stream function. - Westward intensification - Stommel's contribution. - The planetary wind field. - Munk's solution. - Comments on Munk's solution. - Vorticity. - Relative vorticity. - Planetary vorticity. - Absolute vorticity. - Potential vorticity. - Westward intensification of ocean currents explained using conservation of potential vorticity. - Equatorial undercurrents. - The boundary layer approach. - The use of the boundary layer approach to obtain a solution to Munk's equation. - A simple inertial theory by Stommel. - 10 Thermohaline Effects. - The deep circulation. - Equations for salt and temperature (heat) conservation. - Equations for the average salinity and temperature. - Reynolds fluxes and eddy diffusivity. - Thermoclines and the thermohaline circulation. - The mixed layer of the ocean. - 11 Numerical Models. - Introduction. - Numerical methods. - General approach to numerical modelling of ocean circulations. - Descriptions of some models of individual oceans. - O'Brien's two-dimensional wind-driven model of the North Pacific. - Cox's model of the Indian Ocean. - Holland and Hirschmann's model of the Atlantic Ocean. - Two models of the circulation of the world ocean. - Models of mesoscale eddies. - Comments on the numerical model solutions. - 12 Waves. - Introduction. - Some general characteristics of waves. - Small amplitude waves. - Orbital motion of the water particles. - Refraction and breaking in shallow water; diffraction. - The generation of waves. - Measurement of waves. - ReaI waves. - Wave generation by the wind; semi-empirical relations. - Energy of waves. - Tsunamis or seismic sea waves. - Internal waves. - Effects of rotation. - Modified gravity waves. - Kelvin waves. - Planetary or Rossby waves. - Topographic effects. - 13 Tides. - Introduction. - Tide-producing forces. - Components of the tide-producing forces. - Ocean responses to the tide-producing forces - tidaI theories. - The practical approach to tide prediction. - The measurement of tides. - Types of tides. - Tidal currents. - Tides in bays-resonance. - Storm surges. - 14 Some Presently Active and Future Work. - APPENDIX I Mathematical Review with Some Elementary Fluid Mechanics. - Introduction. - Scalars and vectors. - Derivatives. - The individual or total derivative. - Integrals. - Fields. - Descriptions of fluid flow. - Convergences and divergences. - Hydrostatic pressure. - Slope effects. - CompressibiIity. - Centripetal and centrifugal forces. - APPENDIX 2 Units Used in Physical Oceanography. - Introduction. - Base units. - Derived and temporary units. - Units used in dynamic oceanography and some numerical values. - SUGGESTIONS FOR FURTHER READING AND FOR REFERENCE. - INDEX.
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  • 149
    Monograph available for loan
    Monograph available for loan
    Berlin [u.a.] : Gebr. Borntraeger
    Associated volumes
    Call number: M 94.0411/1
    In: Experimental and theoretical aspects of induced polarization
    Type of Medium: Monograph available for loan
    Pages: XXI, 250 S.
    ISBN: 3443130097
    Classification:
    Geophysical Exploration, Geophysical Prospecting
    Language: English
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  • 150
    Monograph available for loan
    Monograph available for loan
    London : Edward Arnold
    Call number: AWI G3-95-0152
    Type of Medium: Monograph available for loan
    Pages: VI, 406 Seiten , Illustrationen
    Edition: second edition
    ISBN: 0713161191
    Former Title: Periglacial processes and environments
    Language: English
    Note: Contents 1 Introduction I Definition of geocryology and periglacial II Objectives III Processes IV Environments V References 2 Environmental factors I Introduction II Basic factors Ill Dependent factors 3 Frozen ground I Introduction II Seasonally frozen ground Ill Permafrost 4 General frost-action processes I Introduction II Freezing process Ill Estimates of freezing and thawing IV Frost wedging V Frost heaving and frost thrusting VI Mass displacement VII Frost cracking VIII Sorting by frost action 5 Some periglacial forms I Introduction II Patterned ground Ill Periglacial involutions IV Stone pavements V String bogs VI Palsas VII Pingos 6 Mass-wasting processes and forms I Introduction lI Avalanching Ill Slushflow IV Thaw slumping V Frost creep VI Gelifluction VII Frost-creep and gelifluction deposits VIII Rock glaciers IX Taluses X Protalus ramparts 7 Nivation I Introduction II Nivation benches and hollows Ill Cryoplanation terraces and cryopediments 8 Slopewash I Introduction II Grèzes litées 9 Fluvial action I Introduction II Icings Ill Break-up phenomena IV Flat-floored valleys V Asymmetric valleys VI Dry valleys and dells 10 Lacustrine and marine action I Introduction II Lacustrine action Ill Marine action 11 Wind action I Introduction II Loess Ill Dunes IV Niveo-eolian deposits and forms V Deflation VI Ventifacts 12 Thermokarst I Introduction II Collapsed pingos Ill Thaw slumps IV Linear and polygonal troughs V Beaded drainage VI Thaw lakes VII Alases 13 Environmental overview 14 Environmental reconstructions I Introduction II Britain Ill Continental Europe IV USSR V Japan VI North America VII Southern Hemisphere VIII Some estimated temperature changes References Index
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  • 151
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    Monograph available for loan
    Amsterdam [u.a.] : Elsevier
    Associated volumes
    Call number: AWI A6-00-0093
    In: Elsevier oceanography series
    Type of Medium: Monograph available for loan
    Pages: IX, 249 S.
    ISBN: 0444415467
    Series Statement: Elsevier oceanography series 16
    Uniform Title: Osnovy dinamiki okeana
    Language: English
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  • 152
    Call number: AWI A17-96-0552-1 ; AWI A17-96-0552-2
    Type of Medium: Monograph available for loan
    Pages: Seiten 1-204, 257-526
    Edition: English edition updated, augmented and revised by the authors
    Edition: Fourth printing
    ISBN: 0262130629
    Uniform Title: Statističeskaja gidromechanika
    Language: English
    Note: Enthaltene Kapitel sind: Chapter 1 Laminar and turbulent flows Chapter 3 Reynolds equations and the semiempirical theories of turbulence Chapter 4 Turbulence in a thermally stratified medium
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  • 153
    Monograph available for loan
    Monograph available for loan
    Associated volumes
    Call number: 11/M 93.1114 ; M 93.0250/1
    In: Mineral deposits of Europe
    Type of Medium: Monograph available for loan
    Pages: xi, 362 S.
    ISBN: 0900488441
    Classification:
    Deposits
    Language: English
    Location: Reading room
    Location: Upper compact magazine
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  • 154
    Monograph available for loan
    Monograph available for loan
    New York [u.a.] : Wiley
    Call number: M 94.0290
    Type of Medium: Monograph available for loan
    Pages: xviii, 571 S.
    ISBN: 0471401579
    Classification:
    Tectonics
    Language: English
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  • 155
    Monograph available for loan
    Monograph available for loan
    Moskva : Izd. Russkij Jazyk
    Call number: MOP 44675
    Type of Medium: Monograph available for loan
    Pages: 448 S.
    Language: Russian , German
    Location: MOP - must be ordered
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  • 156
    Call number: MOP 45359/A
    Type of Medium: Monograph available for loan
    Pages: 34 S.
    Uniform Title: Glavnaja geofiziceskaja Observatorija imeni A.I.Voejkova
    Language: English
    Location: MOP - must be ordered
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  • 157
    Monograph available for loan
    Monograph available for loan
    München : Oldenbourg
    Associated volumes
    Call number: MOP Per 719(43,1)
    In: Abhandlungen und Berichte
    Type of Medium: Monograph available for loan
    Pages: 50 S. , Ill.
    ISBN: 3486201018
    Series Statement: Abhandlungen und Berichte / Deutsches Museum 43,1
    Language: German
    Location: MOP - must be ordered
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  • 158
    Monograph available for loan
    Monograph available for loan
    Orsay, France : Les editions de physique
    Call number: M 94.0516
    Type of Medium: Monograph available for loan
    Pages: VIII, 705 S.
    ISBN: 2902731167
    Classification:
    C.3.8.
    Language: English
    Location: Upper compact magazine
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  • 159
    Call number: AWI A10-00-0033 ; MOP 44430 / Mitte
    Type of Medium: Monograph available for loan
    Pages: XXXI, 630 Seiten
    ISBN: 089500027X
    Language: English
    Location: MOP - must be ordered
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  • 160
    Call number: M 94.0676
    In: AMD
    Type of Medium: Monograph available for loan
    Pages: v, 215 S.
    Series Statement: AMD Vol. 35
    Classification:
    C.3.6.
    Language: English
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  • 161
    Monograph available for loan
    Monograph available for loan
    Berlin [u.a.] : Gebr. Borntraeger
    Associated volumes
    Call number: M 94.0411/2
    In: Experimental and theoretical aspects of induced polarization
    Type of Medium: Monograph available for loan
    Pages: XVI, S.252-335
    ISBN: 3443130100
    Classification:
    Geophysical Exploration, Geophysical Prospecting
    Language: English
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  • 162
    Monograph available for loan
    Monograph available for loan
    Leipzig : Brockhaus | Moskau : Verlag Progress
    Call number: AWI E2-89-0421
    Description / Table of Contents: Das größte Landraubtier unserer Erde ist der Eisbär - für die Forschung geradezu ein Modellfall für die Anpassungsfähigkeit des Organismus eines Lebewesens an die rauhen Bedingungen der Arktis. Immer wieder werden daher sowjetische Expeditionen entsandt, die die Aufgabe haben, das Verhalten des Eisbären in freier Wildbahn zu beobachten, einzelne Tiere zu wiegen, zu messen und zu markieren, um so tiefer in die Geheimnisse des „Eisbärendaseins" einzudringen. Besonders geeignet für solche Forschungen ist die Wrangel-lnsel vor der Nordostküste Sibiriens, ist sie doch die größte „Wochenstube" für Eisbären, die hier mitten im arktischen Winter ihre Jungen zur Welt bringen. Der weit über die Grenzen seines Heimatlandes hinaus bekannte Zoologe Prof. Dr. S. Uspenski, Teilnehmer vieler Expeditionen zur Wrangel-lnsel, berichtet hier in anschaulicher Weise über seine schwierige, oftmals nicht ungefährliche Arbeit und über die Rätsel, die der Eisbär auch heute noch der Wissenschaft aufgibt. Er mahnt in seinem Buch, mitzuhelfen, daß der Eisbär - diese größte Zierde der Arktis - auch künftigen Generationen der Menschheit erhalten bleibt. Uspenskis Wirken ist es mit zu danken, daß die Sowjetunion strenge Maßnahmen zum Schutz dieses vom Aussterben bedrohten Raubtieres ergriffen hat.
    Type of Medium: Monograph available for loan
    Pages: 203 Seiten , Illustrationen , 21 cm
    Edition: 3. Auflage
    ISBN: 3325001769 , 5-01-001792
    Uniform Title: Rodina belych medvedej 〈dt.〉
    Language: German
    Note: Inhalt Statt einer Einleitung An der Grenze der beiden Hemisphären Ein "Entbindungsheim" für die Eisbären Auf der Wrangel-Insel markiert Ihre Heimat ist das Eis Wohnheime für Vögel Weiße und Blaue Giganten des Eismeeres Schützt auch sie! Bildnachweis , Aus dem Russischen übersetzt
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  • 163
    Call number: AWI G7-81-0027 ; AWI G5-86-0505
    Type of Medium: Monograph available for loan
    Pages: VIII, 172 S.
    Language: English
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  • 164
    Monograph available for loan
    Monograph available for loan
    Leipzig : Brockhaus
    Call number: AWI E2-84-0767
    Type of Medium: Monograph available for loan
    Pages: 223 S. : Abb. ; 24 cm
    Language: German
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  • 165
    Series available for loan
    Series available for loan
    Ottawa : Geological Survey of Canada
    Associated volumes
    Call number: SR 90.0009(384)
    In: Memoir
    Type of Medium: Series available for loan
    Pages: 84 S. + 4 pl.
    ISBN: 0660008319
    Series Statement: Memoir / Geological Survey of Canada 384
    Language: English
    Location: Lower compact magazine
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  • 166
    Call number: SR 90.0009(396)
    In: Memoir
    Type of Medium: Series available for loan
    Pages: 52 S. + 2 pl.
    ISBN: 0660101661
    Series Statement: Memoir / Geological Survey of Canada 396
    Language: English
    Location: Lower compact magazine
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  • 167
    Call number: SR 92.0580(72)
    In: Arbeiten aus dem Institut für Geologie und Paläontologie an der Universität Stuttgart
    Type of Medium: Series available for loan
    Pages: 244 S.
    Series Statement: Arbeiten aus dem Institut für Geologie und Paläontologie an der Universität Stuttgart N.F., 72
    Language: German
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  • 168
    Call number: SR 91.1179(33)
    In: Abhandlungen der Geologischen Bundesanstalt Wien
    Type of Medium: Series available for loan
    Pages: 124 S. + 1 Kt.-Beil., 1 Beil
    ISBN: 3900312001
    Series Statement: Abhandlungen der Geologischen Bundesanstalt 33
    Language: German
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  • 169
    Series available for loan
    Series available for loan
    Washington, DC : United States Gov. Print. Off.
    Associated volumes
    Call number: SR 90.0002(486-A)
    In: Professional paper
    Type of Medium: Series available for loan
    Pages: IV, A-34 S.
    Series Statement: U.S. Geological Survey professional paper 486-A
    Language: English
    Location: Lower compact magazine
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  • 170
    Series available for loan
    Series available for loan
    Washington, DC : United States Gov. Print. Off.
    Associated volumes
    Call number: SR 90.0002(486-I)
    In: Professional paper
    Type of Medium: Series available for loan
    Pages: III, I-10 S. + 1 pl.
    Series Statement: U.S. Geological Survey professional paper 486-I
    Language: English
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  • 171
    Series available for loan
    Series available for loan
    Clausthal-Zellerfeld : Pilger
    Associated volumes
    Call number: SR 90.0010(Sonderbd. 1)
    In: Clausthaler geologische Abhandlungen
    Type of Medium: Series available for loan
    Pages: XV, 232 S. + 4 Beil.
    Series Statement: Clausthaler geologische Abhandlungen Sonderbd. 1
    Language: German
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  • 172
    Series available for loan
    Series available for loan
    Ottawa : Geological Survey of Canada
    Associated volumes
    Call number: SR 90.0008(75-13)
    In: Paper
    Type of Medium: Series available for loan
    Pages: 39 S. + 2 pl.
    Series Statement: Paper / Geological Survey of Canada 75-13
    Language: English
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  • 173
    Series available for loan
    Series available for loan
    Ottawa : Geological Survey of Canada
    Associated volumes
    Call number: SR 90.0008(75-37)
    In: Paper
    Type of Medium: Series available for loan
    Pages: 12 S.
    Series Statement: Paper / Geological Survey of Canada 75-37
    Language: English
    Location: Lower compact magazine
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  • 174
    Series available for loan
    Series available for loan
    Ottawa : Geological Survey of Canada
    Associated volumes
    Call number: SR 90.0008(75-41)
    In: Paper
    Type of Medium: Series available for loan
    Pages: 20 S. + 2 pl., 13 microfiche
    Series Statement: Paper / Geological Survey of Canada 75-41
    Language: English
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  • 175
    Call number: SR 90.0008(75-32)
    In: Paper
    Type of Medium: Series available for loan
    Pages: 54 S.
    Series Statement: Paper / Geological Survey of Canada 75-32
    Language: English
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  • 176
    Series available for loan
    Series available for loan
    Washington, DC : United States Gov. Print. Off.
    Associated volumes
    Call number: SR 90.0002(521-F)
    In: Professional paper
    Type of Medium: Series available for loan
    Pages: V, F-15 S. + 2 pl.
    Series Statement: U.S. Geological Survey professional paper 521-F
    Language: English
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  • 177
    Series available for loan
    Series available for loan
    Ottawa : Geological Survey of Canada
    Associated volumes
    Call number: SR 90.0008(76-26)
    In: Paper
    Type of Medium: Series available for loan
    Pages: 15 S. + 1 pl.
    ISBN: 0660008424
    Series Statement: Paper / Geological Survey of Canada 76-26
    Language: English
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  • 178
    Series available for loan
    Series available for loan
    Ottawa : Geological Survey of Canada
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    Call number: SR 90.0008(77-27)
    In: Paper
    Type of Medium: Series available for loan
    Pages: 28 S.
    ISBN: 0660015021
    Series Statement: Paper / Geological Survey of Canada 77-27
    Language: English
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  • 179
    Unknown
    Stuttgart : Schweizerbartsche Verlagsbuchhandlung
    Associated volumes
    Call number: O 7189 (V)
    In: Katalog der fossilen Dinoflagellaten, Hystrichosphären und verwandten Mikrofossilien
    Pages: 532 Bl.
    ISBN: 3510650867
    Language: German
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  • 180
    Series available for loan
    Series available for loan
    Ottawa : Geological Survey of Canada
    Associated volumes
    Call number: SR 90.0008(77-20)
    In: Paper
    Type of Medium: Series available for loan
    Pages: 26 S. + 2 pl.
    ISBN: 0660008432
    Series Statement: Paper / Geological Survey of Canada 77-20
    Language: English
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  • 181
    Series available for loan
    Series available for loan
    Ottawa : Geological Survey of Canada
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    Call number: SR 90.0008(79-3)
    In: Paper
    Type of Medium: Series available for loan
    Pages: 98 S.
    Series Statement: Paper / Geological Survey of Canada 79-3
    Language: English
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  • 182
    Call number: SR 90.0008(79-9)
    In: Paper
    Type of Medium: Series available for loan
    Pages: 25 S.
    ISBN: 0660102072
    Series Statement: Paper / Geological Survey of Canada 79-9
    Language: English
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  • 183
    Series available for loan
    Series available for loan
    Ottawa : Geological Survey of Canada
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    Call number: SR 90.0008(79-13)
    In: Paper
    Type of Medium: Series available for loan
    Pages: 32 S.
    ISBN: 066010279X
    Series Statement: Paper / Geological Survey of Canada 79-13
    Language: English
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  • 184
    Series available for loan
    Series available for loan
    Braunschweig : Inst. für Geophysik und Meteorologie der Techn. Univ. Braunschweig
    Associated volumes
    Call number: SR 93.0336(33)
    In: Geophysikalische Arbeiten sowie Mitteilungen aus Meteorologie und Astrophysik
    Type of Medium: Series available for loan
    Pages: 163 S.
    Series Statement: Gamma 33
    Language: German
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  • 185
    Series available for loan
    Series available for loan
    Braunschweig : Inst. für Geophysik und Meteorologie der Techn. Univ. Braunschweig
    Associated volumes
    Call number: SR 93.0336(30)
    In: Geophysikalische Arbeiten sowie Mitteilungen aus Meteorologie und Astrophysik
    Type of Medium: Series available for loan
    Pages: 188 S.
    Series Statement: Gamma 30
    Language: German
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  • 186
    Call number: SR 94.0040(7)
    In: Schriftenreihe für geologische Wissenschaften
    Type of Medium: Series available for loan
    Pages: 163 S.
    Series Statement: Schriftenreihe für geologische Wissenschaften 7
    Language: German
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  • 187
    Series available for loan
    Series available for loan
    Ottawa : Geological Survey of Canada
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    Call number: SR 90.0007(245)
    In: Bulletin
    Type of Medium: Series available for loan
    Pages: 68 S. + 2 pl.
    Series Statement: Bulletin / Geological Survey of Canada 245
    Language: English
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  • 188
    Call number: SR 91.1609(26/3)
    In: Mededelingen
    Type of Medium: Series available for loan
    Pages: S. 39-90
    Series Statement: Mededelingen / Rijks Geologische Dienst N.S., vol.26, no.3
    Language: English
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  • 189
    Series available for loan
    Series available for loan
    Washington, DC : United States Gov. Print. Off.
    Associated volumes
    Call number: SR 90.0002(729-D)
    In: Professional paper
    Type of Medium: Series available for loan
    Pages: X, D-60 S. + 1 pl.
    Series Statement: U.S. Geological Survey professional paper 729-D
    Language: English
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  • 190
    Call number: SR 90.0017(11)
    In: Cruise report
    Type of Medium: Series available for loan
    Pages: 72 S.
    Series Statement: Cruise report / Geological Survey of Japan 11
    Language: English
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  • 191
    Call number: SR 90.0012(208)
    In: Publikation
    Type of Medium: Series available for loan
    Pages: 24 S.
    Series Statement: Publikation / Zentralanstalt für Meteorologie und Geodynamik in Wien 208
    Language: German
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  • 192
    Call number: SR 90.0017(12)
    In: Cruise report
    Type of Medium: Series available for loan
    Pages: 256 S.
    Series Statement: Cruise report / Geological Survey of Japan 12
    Language: English
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  • 193
    Call number: SR 92.0097(41)
    In: Report of investigation = Tutkimusraportti
    Type of Medium: Series available for loan
    Pages: 16 S.
    ISBN: 9516901077
    Series Statement: Report of investigation / Geological Survey of Finland 41
    Language: English
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  • 194
    Series available for loan
    Series available for loan
    Washington, DC : United States Gov. Print. Off.
    Associated volumes
    Call number: SR 90.0002(813-E)
    In: Professional paper
    Type of Medium: Series available for loan
    Pages: IV, E-51 S. + 1 pl.
    Series Statement: U.S. Geological Survey professional paper 813-E
    Language: English
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  • 195
    Series available for loan
    Series available for loan
    Washington, DC : United States Gov. Print. Off.
    Associated volumes
    Call number: SR 90.0002(848-D)
    In: Professional paper
    Type of Medium: Series available for loan
    Pages: IV, D-86 S.
    Series Statement: U.S. Geological Survey professional paper 848-D
    Language: English
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  • 196
    Series available for loan
    Series available for loan
    Washington, DC : United States Gov. Print. Off.
    Associated volumes
    Call number: SR 90.0002(884)
    In: Professional paper
    Type of Medium: Series available for loan
    Pages: III, 29 S.
    Series Statement: U.S. Geological Survey professional paper 884
    Language: English
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  • 197
    Call number: SR 90.0002(902)
    In: Professional paper
    Type of Medium: Series available for loan
    Pages: IV, 85 S.
    Series Statement: U.S. Geological Survey professional paper 902
    Language: English
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  • 198
    Series available for loan
    Series available for loan
    Washington, DC : United States Gov. Print. Off.
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    Call number: SR 90.0002(886)
    In: Professional paper
    Type of Medium: Series available for loan
    Pages: III, 46 S.
    Series Statement: U.S. Geological Survey professional paper 886
    Language: English
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  • 199
    Series available for loan
    Series available for loan
    Bochum : Inst. für Geologie, Ruhr-Univ. Bochum
    Associated volumes
    Call number: SR 93.0590(1)
    In: Bochumer geologische und geotechnische Arbeiten
    Type of Medium: Series available for loan
    Pages: VIII, 184 S.
    Series Statement: Bochumer geologische und geotechnische Arbeiten 1
    Language: German
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  • 200
    Call number: SR 90.0002(939)
    In: Professional paper
    Type of Medium: Series available for loan
    Pages: V, 53 S.
    Series Statement: U.S. Geological Survey professional paper 939
    Language: English
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