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  • 1
    Monographie ausleihbar
    Monographie ausleihbar
    New York [u.a.] : Academic Press
    Signatur: MOP B 13421
    Materialart: Monographie ausleihbar
    Seiten: IX, 234 S. : graph. Darst.
    Originaltitel: V vedeniye v Kolichestvennyy Ul'tramikroanaliz
    Sprache: Englisch
    Standort: MOP - Bitte bestellen
    Zweigbibliothek: GFZ Bibliothek
    Standort Signatur Erwartet Verfügbarkeit
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  • 2
    Schriftenreihen ausleihbar
    Schriftenreihen ausleihbar
    Dazugehörige Bände
    Signatur: ZSP-387-13
    In: International project on paleolimnology and late cenozoic climate
    Materialart: Schriftenreihen ausleihbar
    Seiten: 132 S. : Ill., graph. Darst.
    Sprache: Englisch
    Zweigbibliothek: AWI Bibliothek
    Standort Signatur Erwartet Verfügbarkeit
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  • 3
    Monographie ausleihbar
    Monographie ausleihbar
    Oxford [u.a.] : Butterworth-Heinemann
    Signatur: PIK N 411-10-0084
    Beschreibung / Inhaltsverzeichnis: Contents: Ch. 1: Plate tectonics ; Ch. 2: The Earth's crust ; Ch. 3: Tectonic settings ; Ch. 4: The Earth's mantle and core ; Ch. 5: Crustal and mantle evolution ; Ch. 6: The atmosphere, oceans, climates, and life ; Ch. 7: Comparative planetary evolution
    Materialart: Monographie ausleihbar
    Seiten: X, 282 S. : Ill., graph. Darst., Kt.
    Ausgabe: 4. ed., reprint
    ISBN: 0750633867
    Sprache: Englisch
    Standort: A 18 - Bitte bestellen
    Zweigbibliothek: PIK Bibliothek
    Standort Signatur Erwartet Verfügbarkeit
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  • 4
    Monographie ausleihbar
    Monographie ausleihbar
    Cambridge [u.a.] : MIT Press
    Signatur: PIK B 100-11-0060
    Beschreibung / Inhaltsverzeichnis: Contents: Introduction ; The Effects of Taxation ; Tax Incidence ; Distortions and Welfare Losses ; Optimal Taxation ; Indirect Taxation ; Direct Taxation ; Mixed Taxation ; The Taxation of Capital ; Criticisms of Optimal Taxation ; Some Current Debates ; Low-Income Support ; The Consumption Tax ; Environmental Taxation ; App. A: Some Basic Microeconomics ; App. B: Optimal Control
    Materialart: Monographie ausleihbar
    Seiten: VII, 226 S. : graph. Darst.
    ISBN: 0262194864 , 978-0-262-19486-0
    Originaltitel: Théorie économique de la fiscalité
    Sprache: Englisch
    Standort: A 18 - Bitte bestellen
    Zweigbibliothek: PIK Bibliothek
    Standort Signatur Erwartet Verfügbarkeit
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  • 5
    Monographie ausleihbar
    Monographie ausleihbar
    Oxford [u.a.] : Butterworth-Heinemann
    Signatur: PIK N 410-10-0083
    Beschreibung / Inhaltsverzeichnis: Contents: Introduction ; The Shape of Ocean Basins ; The Evolution of Ocean Basins ; The Structure and Formation of Oceanic Lithosphere ; Hydrothermal Circulation in Oceanic Crust ; Palaeoceanography and Sea-Level Changes ; The Broader Picture ; The Stratigraphic Column
    Materialart: Monographie ausleihbar
    Seiten: 185 S. : Ill., graph. Darst., Kt.
    Ausgabe: 2. ed., repr. with corrections
    ISBN: 0750639830
    Serie: Oceanography series 1
    Sprache: Englisch
    Standort: A 18 - Bitte bestellen
    Zweigbibliothek: PIK Bibliothek
    Standort Signatur Erwartet Verfügbarkeit
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  • 6
    Schriftenreihen ausleihbar
    Schriftenreihen ausleihbar
    Hanover, NH : Corps of Engineers, U.S. Army, Cold Regions Research and Engineering Laboratory
    Dazugehörige Bände
    Signatur: ZSP-202-266
    In: Research report
    Beschreibung / Inhaltsverzeichnis: CONTENTS: Preface. - Introduction. - Review of dielectric properties of soils and rocks. - Methods and measurements. - Introduction. - Dispersion. - Experimental procedures. - Introduction. - Apparatus. - Correction for stray fields. - Material. - Results. - The dielectric properties of Na-montmorillonite suspensions as a function of concentration. - The dielectric properties of K-montmorillonite water suspension. - Conclusions. - Outlook. - Literature cited.
    Beschreibung / Inhaltsverzeichnis: The dielectric properties of Na- and K- montmorillonite suspensions with concentrations varying from 2.5% to 0.10% by weight were measured at 25°C in the frequency range of 50 Hz to 20 kHz. Effects of electrode polarization were minimized by using the same stainless steel electrodes at different interelectrode distances and a correction was applied to compensate for stray fields. This investigation establishes the fact that the high dielectric constants of clay suspensions at audio frequencies are real and not the result of electrode polarization. The polarization that determines the dispersion is an interfacial phenomenon between the ionic atmosphere and the negatively charged clay particle. The results of this study show that clay suspensions have the same dispersion as soil samples, indicating the probability that the dispersion of wet soils in the frequency range from 50 Hz to 20 kHz is similar for most soils. The actual value of the dielectric constant, however, cannot yet be predicted.
    Materialart: Schriftenreihen ausleihbar
    Seiten: iii, 17 Seiten , Illustrationen
    Serie: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 266
    Sprache: Englisch
    Zweigbibliothek: AWI Bibliothek
    Standort Signatur Erwartet Verfügbarkeit
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  • 7
    Schriftenreihen ausleihbar
    Schriftenreihen ausleihbar
    Hanover, NH : U.S. Army Materiel Command, Terrestrial Sciences Center, Cold Regions Research & Engineering Laboratory
    Dazugehörige Bände
    Signatur: ZSP-202-264
    In: Research report
    Beschreibung / Inhaltsverzeichnis: CONTENTS: Preface. - Abstract. - Introduction. - Physical properties of ice fog. - Mie scattering computations. - Results. - Literature cited.
    Beschreibung / Inhaltsverzeichnis: Ice-fog crystals consisting of many spherical particles, and some hexagonal plates and columns, were observed at ambient temperatures of about -40°C in the Fairbanks, Alaska area during mid-winter. The concentrations and the size distributions of the ice-fog crystals were measured. The attenuation and backscattering of infrared radiation by ice-fog crystals were computed for optical wavelengths of 2.2[My], 2.7[My], 4.5[My], 5.75[My], 9.7[My] and 10.9[My] using the Mie theory. The minimum attenuation coefficients and backscattering functions of ice fog were found to be at 9.7[My] wavelength in the observed wavelengths. Optical attenuation coefficients and volume backscattering functions of water fogs were also computed using the Mie theory. The minimum attenuation coefficients and backscattering functions of water fog were found to be at 10.9[My] wavelength in the region of 2.2[My], 2.7[My], 4.5[My], 5.75[My], 9.7[My] and 10.9[My]. Both the attenuation coefficients and backscattering functions of ice fog are within the same order of magnitude as water fog for equivalent fog concentrations and wavelengths.
    Materialart: Schriftenreihen ausleihbar
    Seiten: iv, 7 Seiten , Illustrationen
    Serie: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 264
    Sprache: Englisch
    Zweigbibliothek: AWI Bibliothek
    Standort Signatur Erwartet Verfügbarkeit
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  • 8
    Schriftenreihen ausleihbar
    Schriftenreihen ausleihbar
    Hanover, NH : U.S. Army Materiel Command, Terrestrial Sciences Center, Cold Regions Research & Engineering Laboratory
    Dazugehörige Bände
    Signatur: ZSP-202-263
    In: Research report
    Beschreibung / Inhaltsverzeichnis: CONTENTS: Preface. - Abstract. - Introduction. - Theoretical background. - Experimental apparatus and procedures. - Results and discussion. - Conclusions. - Literature cited.
    Beschreibung / Inhaltsverzeichnis: The transition in the mode of heat transfer from conduction to convection in a layer of water formed continuously by melting ice from below has been determined experimentally. This was accomplished by locating the inflection point on the curve relating the water-ice interface (or melting front) and time. Thus, the critical Rayleigh number, Rac, at which convective heat transfer started can be correlated empirically as a function of warm plate temperature, Ts, by Rac= 14,200 exp(-6.64 x 10^-2 Ts). This relation is valid for Ts varying from 7.72 to 25.50°C. The initial ice temperature T0 was varied from -4.8 to -22.00°C. The effect of T0 was found to be insignificant. Homogeneous, bubble-free ice was prepared and used in all the experiments.
    Materialart: Schriftenreihen ausleihbar
    Seiten: iv, 12 Seiten , Illustrations
    Serie: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 263
    Sprache: Englisch
    Zweigbibliothek: AWI Bibliothek
    Standort Signatur Erwartet Verfügbarkeit
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  • 9
    Schriftenreihen ausleihbar
    Schriftenreihen ausleihbar
    Hanover, NH : US Army Materiel Command, Cold Regions Research & Engineering Laboratory
    Dazugehörige Bände
    Signatur: ZSP-202-240
    In: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command, 240
    Beschreibung / Inhaltsverzeichnis: A 4-summer hydrologic record from a 1.6 km^2 drainage basin at Barrow, Alaska is analyzed. The watershed, a drained lake basin, is underlain by continuous permafrost within 0.3m of the tundra surface and is covered by ice-wedge polygons and numerous small shallow ponds. Considerable variations from the 20-yr means of summer climate (thaw period 88 days, precipitation 67 mm) are represented in the data: 1963 - cold, extremely wet; 1964 - cold, extremely dry; 1965 - cool, dry; 1966 - cool, wet. Runoff varied greatly from storm to storm, occurring primarily through and over the tundra mat and through an intricate system of polygonal troughs and ponds. As a result of the subdued coastal topography, varying areas (0.3 km^2 to 1.6 km^2) contribute to runoff from different storms. Analyses of hydrographs revealed: 1) lag times generally from 3 to 10 hr; 2) recession constants of about 50 hr, but occasionally as much as 160 hr; and 3) runoff from individual storms between 1 and 70%. About 5% of the thaw season precipitation normally runs off. Comparison of total thaw season precipitation between the U.S. Weather Bureau and a shielded gage located on the watershed indicated no major differences. If "trace" precipitation is considered, only 90% of the actual precipitation may be recorded. Pan evaporation for an average thaw season is about 160 mm and evapotranspiration which is essentially in balance with precipitation is about 60 mm. Conductivity of runoff water varied from 250 [My]mhos during sustained discharge to more than 500 [My]mhos during low flows in dry years. Precipitation chemistry showed no correlation with storm direction. Assuming all winter precipitation runs off, and the data are spatially and temporally representative, about 50% of the measured annual precipitation in this region runs off into the Arctic Ocean.
    Materialart: Schriftenreihen ausleihbar
    Seiten: IV, 18 Seiten , Illustrationen
    Serie: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 240
    Sprache: Englisch
    Anmerkung: CONTENTS: Preface. - Summary. - Introduction. - Regional setting. - Description of watershed. - Climatic record. - Methods. - Precipitation. - Water and air temperatures. - Discharge. - Evaporation and pond levels. - Water chemistry. - Soil thaw. - Results and discussion. - Precipitation. - Runoff. - Evaporation and transpiration. - Water chemistry. - Conclusions. - Literature cited.
    Standort: AWI Archiv
    Zweigbibliothek: AWI Bibliothek
    Standort Signatur Erwartet Verfügbarkeit
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  • 10
    Signatur: SR 90.0001(1117-D)
    In: U.S. Geological Survey bulletin
    Materialart: Schriftenreihen ausleihbar
    Seiten: IV, D-33 S. + 1 pl.
    Serie: U.S. Geological Survey bulletin 1117-D
    Sprache: Englisch
    Standort: Kompaktmagazin unten
    Zweigbibliothek: GFZ Bibliothek
    Standort Signatur Erwartet Verfügbarkeit
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