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  • Wissenschaftspark Albert Einstein  (2)
  • Bildungsgesch. Forschung
  • VIZ Charlottenburg-Wilmersdorf
  • 1980-1984
  • 1970-1974  (2)
  • Cold Regions Research and Engineering Laboratory 〈Hanover, NH〉  (2)
Type of Medium
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  • Wissenschaftspark Albert Einstein  (2)
  • Bildungsgesch. Forschung
  • VIZ Charlottenburg-Wilmersdorf
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Year
Keywords
  • 1
    Book
    Book
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
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    UID:
    kobvindex_GFZ123002
    Format: v, 32 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 320
    Content: CONTENTS: Preface. - Summary. - lntroduction. - 1. Sources and effects of cadmium in the environment: a brief review. - Sources of cadmium. - Health aspects of cadmium pollution. - Air pollution by cadmium. - Water pollution by cadmium. - Cadmium in soils. - Effect of cadmium on sewage treatment processes. - 2. The interaction of cadmium with some native New Hampshire soils. - Introduction. - Materials and methods. - Results and discussion. - Reversibility. - Conclusions. - Suggestions for further research. - 3. The flow of cadmium through soils: an experimental method. - Introduction. - Design criteria and detector performance. - Mathematical analysis of curves. - Conclusions. - Literature cited. - Abstract.
    Content: A brief review of the literature on cadmium in the environment, with emphasis on its role in soils and water, is presented. Experimentally, the interaction of cadmium with two soils and one naturally occurring zeolite was examined using calcium-saturated and potassium-saturated samples. The soils preferentially bound cadmium in the presence of either calcium or potassium with decreasing cadmium selectivity as the fractional cadmium surface coverage increased. Cadmium sorption was relatively higher with the potassium soils as compared with the calcium soils. For the loamy fine sand this increase was accounted for by electroselectivity principles, while such reasoning was inadequate to explain the increases observed with the Charleton loam sample. The preference for cadmium over calcium, as measured by the selectivity coefficient, was higher for the sandy soil. The zeolite was found to be calcium-selective. A method for monitoring the flow of cadmium through soil columns was examined. The use of spatial filtering, involving Fourier transforms, was found to be a suitable technique for monitoring the changes in cadmium concentration as it flows through soils. The experimental technique involves the use of gamma-emitting metal isotopes in conjunction with an external scintillation counter; thus the soil column remains undisturbed and may be used for several experiments.
    Note: MAB0014.001: ZSP-202-320 , Online frei verfügbar
    In: Research report
    Keywords: Forschungsbericht
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  • 2
    UID:
    kobvindex_GFZ122981
    Format: vi, 33 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 325
    Content: CONTENTS: Preface. - Symbols. - Introduction. - Physical properties of ice, water and snow. - Electrical relations affecting the problem. - The dielectric constant. - Deloor's theory. - Wet snow application. - Experimental procedure. - Measurement technique. - Sample preparation. - Glass bead preparation. - Experimental results. - Wet snow results. - Glass bead results. - Experimental error. - Discussion. - Conclusions. - Recommendations. - Literature cited. - Selected bibliography. - Appendix A. The measurement of the complex dielectric constant in a shorted wave guide. - Appendix B. Evaluation of the effective particle shape factor and the effective dielectric properties in the immediate vicinity of average liquid and solid particles. - Appendix C. Experimental data. - Abstract.
    Content: An accurate method of measuring liquid water in snow covers is required to determine the properties of wet snow. The dielectric properties of wet snow must be utilized to adequately measure its liquid water content. In this study the effect of liquid water on the complex dielectric constant of natural snow is determined in the microwave frequency range. Deloor's method for calculating the dielectric constant for mixtures and the results of waveguide experiments on samples of wet snow and glass beads are used to construct a calibration curve relating the measured dielectric loss factor directly to the water content of wet snow. The results are independent of porosity, past history and chemical impurities. A relation between the effective dielectric constant and the porosity and water content is proposed and tested, experimentally. The general nature of this relation is described and suggestions are made for the development of a more precise relation. It is concluded that the dielectric constant is a function of porosity and water content only.
    Note: MAB0014.001: ZSP-202-325 , Online frei verfügbar
    In: Research report
    Keywords: Forschungsbericht
    Library Location Call Number Volume/Issue/Year Availability
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