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  • Books  (502)
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  • 1
    Series available for loan
    Series available for loan
    Berlin : Nationalkomitee für Geodäsie und Geophysik bei der Akademie der Wissenschaften der DDR
    Associated volumes
    Call number: MOP Per 581 ; MOP Per 581(1/11) ; ZSP-319/A-11
    In: Geodätische und geophysikalische Veröffentlichungen : Reihe 1, Heft 11
    Type of Medium: Series available for loan
    Pages: 63 Seiten , Illustrationen
    ISSN: 0533-7577
    Series Statement: Geodätische und geophysikalische Veröffentlichungen : Reihe 1 11
    Language: German
    Note: Inhalt: I. Untersuchungen zur Avifauna von King George / R. Bannasch und U. Lundberg. - II. Robbenbeobachtungen im Gebiet von King George / R. Bannasch. - III. Beobachtungen der marinen Fauna im Litoral und Benthal von King George (Südshetlandinseln, Antarktis) / M. Rauschert. - IV. Untersuchungen zum Helminthenbefall und zur Nahrung verschiedener Tiergruppen / K. Feiler. - , Zusammenfassung in englischer, deutsche und russischer Sprache , Teilweise in kyrillischer Schrift
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  • 2
    Series available for loan
    Series available for loan
    Karlsruhe : Braun ; 1.1941(1940) - 59.1999(1997); 2000(1999) -
    Call number: S 91.0710 ; S 91.0710 (2020) ; S 91.0710 (2021) ; S 91.0710 (2022) ; S 91.0710 (2023)
    Type of Medium: Series available for loan
    ISSN: 0174-254X
    Location: Archive - must be ordered
    Location: Archive - must be ordered
    Location: Archive - must be ordered
    Location: Archive - must be ordered
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  • 3
    Call number: MOP Per 581 ; MOP Per 581(1/8) ; ZSP-319/A-1(Sonderheft) ; ZSP-319/A-1(Sonderheft, 2. Ex.)
    In: Geodätische und geophysikalische Veröffentlichungen : Reihe 1, Heft 8, Sonderheft 1
    Type of Medium: Series available for loan
    Pages: 107 Seiten , Illustrationen
    Edition: Sonderheft des NKSCAR der DDR
    Series Statement: Geodätische und geophysikalische Veröffentlichungen : Reihe 1 8
    Language: German , English
    Note: Inhalt: I. Zoologische Untersuchungen im Gebiet der sowjetischen Antarktisstation "Bellinghausen" / R. BANNASCH und K. ODENING. - II. Deuterium- und 18O-Variationen in Seen der Schirmacher-Oase (Ostantarktika) / W. RICHTER und G. STRAUCH. - III. Stable isotope investigations in Antarctica / H. SCHÜTZE, G. STRAUCH, K. WETZEL. - IV. The influence of degradation processes on the isotopic composition of Antarctic precipitation / R. DER. - V. Sommerliche Eisvariationen in der Olaf-Prydz-Bucht / H. GERNANDT. - VI. Zur Geologie des nördlichen Teils des Neptune Range / Pensacola-Gebirges (Antarktika) / W. WEBER und L. V. FEDOROV. - VII. Beobachtungen am Krill (Euphausia superba DANA) im atlantischen Sektor der Antarktis in der Sommersaison 1978 und 1979 / S. HOLZLÖHNER. - VIII. Forschungsreise eines Zubringertrawlers in die Antarktis / G. GUBSCH und U. HOFFMANN.
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  • 4
    Monograph available for loan
    Monograph available for loan
    Leipzig : Akad.-Verl.-Ges.
    Associated volumes
    Call number: 655 / Regal 12
    In: Mathematik für Physiker und Ingenieure
    Type of Medium: Monograph available for loan
    Pages: X, 247 S. : Ill., graph. Darst.
    Series Statement: Mathematik für Physiker und Ingenieure 1
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  • 5
    Monograph available for loan
    Monograph available for loan
    Wien : Springer
    Call number: 767 / Regal 12
    Type of Medium: Monograph available for loan
    Pages: XI, 323 S. : Ill.
    Edition: 2., erw. Aufl.
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  • 6
    Monograph available for loan
    Monograph available for loan
    Leipzig : Quelle & Meyer
    Call number: 1501/2 Regal 12
    Type of Medium: Monograph available for loan
    Pages: 298 S.
    Location: Archive - must be ordered
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  • 7
    Monograph available for loan
    Monograph available for loan
    Berlin
    Call number: MOP 34586 ; AWI P6-17-69233
    Type of Medium: Monograph available for loan
    Pages: 125 S. : Ill.
    Note: Inhaltsverzeichnis: 1. Allgemeiner Teil. - 1.1 Vorbereitung der Expedition. - 1.2 Reise in das Einsatzgebiet. - 1.3 Ablösung durch die 8. SAE. - 1.4 Allgemeiner Ablauf der Überwinterung. - 1.5 Abschluß der meteorologischen Arbeiten und Vorbereitung der Rückreise. - 1.6 Die Rückreise. - 2. Mirny. - 2.1 Unterkunft. - 2.2 Arbeitsplatz der Meteorologen im Wetterbüro. - 2.3 Ausrüstung. - 2.4 Allgemeine Lebensbedingungen. - 2.4.1 Ernährung. - 2.4.2 Stromversorgung und Telefon. - 2.4.3 Verbindung nach Deutschland. - 2.4.4 Medizin und Hygiene. - 2.4.5 Teilnahme an Arbeitseinsätzen. - 2.4.6 Freizeitgestaltung. - 2.4.7 Schutzeinrichtungen. - 2.4.8 Lagerung der Transportkisten. - 3. Molodjoschnaja. - 3.1 Anreise. - 3.2 Die Station. - 3.2.1 Aufenthalt. - 3.2.2 Allgemeine Beschreibung. - 3.2.3 Aufbau. - 3.2.4 Allgemeine Lebensbedingungen. - 3.2.5 Nebenarbeiten. - 3.2.6 Witterungsbedingungen. - 3.3 Abreise. - 4. Geologenlager. - 4.1 Anreise. - 4.2 Das Zeltlager. - 4.2.1 Aufenthalt. - 4.2.2 Allgemeine Beschreibung. - 4.2.3 Allgemeine Lebensbedingungen. - 4.2.4 Witterungsbedingungen. - 5. Wostok. - 5.1 Anreise. - 5.2 Die Station. - 5.2.1 Allgemeine Beschreibung. - 5.2.2 Allgemeine Lebensbedingungen. - 5.2.3 Nebenarbeiten. - 5.2.4 Witterungsbedingungen. - 5.3 Abreise. - 6. Heimreise. - 6.1 Mirny. - 6.2 Flug nach Molodjoschnaja. - 6.3 Molodjoschnaja. - 6.4 Schiffsreise Molodjoschnaja - Lasarew - Molodjoschnaja - Mirny. - 6.5 Schiffsreise Mirny - Leningrad. - 6.6 Leningrad. - 6.7 Rückflug Leningrad - Berlin. - 7. Betreuung durch das NKGG. - 8. Die Arbeiten der meteorologischen Arbeitsgruppe. - 8.1 Aufgabenstellung und Arbeitsprogramm. - 8.2 Durchführung der Arbeiten. - 8.2.1 Umfang der eingegangenen Meldungen. - 8.2.2 Bearbeitung der Meldungen. - 8.2.3 Über die Klimadaten von Mirny. - 8.2.4 Durchführung der Sonderarbeiten. - 8.3 Zusammenstellung des vorliegenden Materials. - 8.4 Teilnahme am Radiosondendienst. - 8.4.1 Zielstellung. - 8.4.2 Präparierung der Ballonhülle. - 8.4.3 Wasserstoffherstellung. - 8.4.4 Ein neuer Expeditions-Wasserstoffgenerator. - 8.4.5 Die sowjetische Radiosonde A-22-IV. - 8.4.6 Aufstiegstechnik bei starkem Wind. - 8.4.7 Bearbeitung und Verschlüsselung der Werte. - 8.5 Druck- und Temperaturänderungen über Mirny. - 8.6 Witterungsbericht von Mirny 1963. - 9. Die Arbeiten der astronomisch-geodätischen Arbeitsgruppe. - 9.1 Aufgabenstellung. - 9.2 Vorbereitung. - 9.2.1 Gerätebeschaffung. - 9.2.2 Gerätevorbereitung. - 9.3 Astropunkt II. Ordnung Molodjoschnaja. - 9.3.1 Aufgabenstellung. - 9.3.2 Auswahl des Beobachtungspunktes. - 9.3.3 Vorbereitung. - 9.3.4 Geräte. - 9.3.5 Breitenbestimmung. - 9.3.6 Längenbestimmung. - 9.3.7 Simultanbestimmung. - 9.3.8 Anschluß an trigonometrisches Lokalnetz. - 9.3.9 Vermarkung. - 9.4 Astropunkt III. Ordnung im Gebiet der Scott- und Tulaberge. - 9.4.1 Aufgabenstellung. - 9.4.2 Vorbereitung. - 9.4.3 Geräte. - 9.4.4 Beobachtung. - 9.4.5 Auswertung. - 9.4.6 Vermarkung. - 9.5 Astropunkt I. Ordnung Mirny. - 9.5.1 Aufgabenstellung. - 9.5.2 Vorbereitung. - 9.5.3 Geräte. - 9.5.4 Breitenbestimmung. - 9.5.5 Längenbestimmung. - 9.5.6 Anschlußmessung zur Koordinatenübertragung. - 9.5.7 Vermarkung. - 9.6 Astropunkt I. Ordnung Wostok. - 9.6.1 Aufgabenstellung. - 9.6.2 Auswahl des Beobachtungspunktes. - 9.6.3 Vorbereitung. - 9.6.4 Geräte. - 9.6.5 Uhrvergleiche. - 9.6.6 Orientierung und Justierung der Instrumente. - 9.6.7 Breitenbestimmung. - 9.6.8 Längenbestimmung. - 9.6.9 Simultanbestimmung. - 9.6.10 Beobachtungen zur Berechnung der astronomischen Refraktion. - 9.6.11 Vermarkung. - 9.7 Zusammenfassung. - 9.8 Zusammenstellung der Ergebnisse.
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  • 8
    Call number: O 1086
    Type of Medium: Monograph available for loan
    Pages: XII, 700 S. : zahlr. Ill., Taf.
    Edition: 2., umgearb. u. verm. Aufl
    Location: Archive - must be ordered
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  • 9
    Call number: O 1176
    In: Beiträge zum Problem der Massenverteilung im Erdkörper
    Type of Medium: Monograph available for loan
    Pages: 60 S. : graph. Darst.
    Series Statement: Beiträge zum Problem der Massenverteilung im Erdkörper 1
    Location: Archive - must be ordered
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  • 10
    Call number: O 1089
    Type of Medium: Monograph available for loan
    Pages: 253 S.
    Location: Archive - must be ordered
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  • 11
    Monograph available for loan
    Monograph available for loan
    Berlin [u.a.] : deGruyter
    Associated volumes
    Call number: O 1208(1)
    In: Minerva-Handbücher
    Type of Medium: Monograph available for loan
    Pages: 999 S.
    Series Statement: Minerva-Handbücher : 1. Abt.: Die Bibliotheken 1
    Location: Archive - must be ordered
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  • 12
    Call number: SR 99.0015(371) ; ZSP-292-371
    In: Freiberger Forschungshefte, 371
    Type of Medium: Series available for loan
    Pages: 117 Seiten , Illustrationen
    Edition: 1. Auflage
    ISSN: 0071-9404
    Series Statement: Freiberger Forschungshefte : C 371 : Geowissenschaften - Geologie
    Language: German
    Note: Enthält 3 Beiträge , Inhaltsverzeichnis: Annotation Tektonische Untersuchungen in den Herbert Mountains (Shackleton Range, Antarktika) / Joachim Hofmann Beitrag zur Geologie des Pensacola-Gebirges (Antarktika) / Wolfgang Weber Tektonische Untersuchungen in der Patuxent-Formation der Schmidt Hills (Pensacola Mts. (Antarktika)) / Joachim Hofmann und V. V. Samsonov
    Location: Lower compact magazine
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  • 13
    Call number: 91.0851 ; MOP Per 581(3/3) ; ZSP-319/C-3
    In: Geodätische und Geophysikalische Veröffentlichungen : Reihe 3, Physik der festen Erde, Nr. 3
    Type of Medium: Series available for loan
    Pages: 77 Seiten
    ISSN: 0435-6187
    Series Statement: Geodätische und Geophysikalische Veröffentlichungen : Reihe 3, Physik der festen Erde 3
    Language: English , English
    Note: Inhaltsverzeichnis = Contents Inhalt = Contents Vorwort = Foreword A. Seismologie = A. Seismology B. Physik des oberen Erdmantels = B. Physics of the Upper Mantle of the Earth C. Gravimetrie, Geodäsie, Erdgezeiten und rezente Erdkrustenbewegungen = C. Gravimetry, Geodesy, Tides of the Earth and Recent Movements of the Earth' s Crust. D. Magnetismus = D. Magnetism E. Theorie und Berechnungsanlagen = E. Theory and· Computers F. Tiefbohrungen für wissenschaftliche Zwecke = F. Deep Drilling for Scientific Purposes G. Petrologie = G. Petrology H. Tektonik = H. Tectonics J. Geochemie = J. Geochemistry , Text deutsch und englisch
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  • 14
    Call number: MR 90.1062 ; MOP Per 469(13) ; AWI P8-90-0342
    In: Veröffentlichungen des Geophysikalischen Instituts der Universität Leipzig
    Type of Medium: Monograph available for loan
    Pages: 219 S. , zahlr. Ill., graph. Darst. und Kt. , 24 cm
    Series Statement: Veröffentlichungen des Geophysikalischen Instituts der Universität Leipzig : Zweite Serie, Spezialarbeiten aus dem Geophysikalischen Institut und Observatorium 13
    Language: German
    Note: Zugl.: Leipzig, Univ., Diss., 1940 , Inhaltsverzeichnis: Einleitung. - Abschnitt 1. - Geographisch-expeditionstechnischer Bericht. - 1: Geographischer Überblick. - 1. Beschreibung des Gebietes. - 2. Die Fjorde. - 3. Das eisfreie Hinterland. - 4. Das Sukkertoppen-Hochlandeis. - 5. Klima und Pflanzenwelt. - 6. Bewegungen des Eises und der Küstenlinie in jüngster Zeit. - 2: Plan, Vorbereitung und Ausrüstung der Oxford-Grönland-Expedition 1938. - 1. Der ursprüngliche Plan. - 2. Die Vorbereitungen. - 3. Überblick über die instrumentelle Ausrüstung. - 4. Änderungen des Arbeitsprogrammes im Verlauf der Expedition. - 5. Übersicht über die durchgeführten Untersuchungen. - 3: Der Verlauf der Expedition. - 1. Die Ausreise. - 2. Transporte, Einrichtung der Lager. - 3. Weiterarbeit zu dritt. - 4. Bei den Grönländern. - 5. Heimkehr. - Abschnitt 2. - Die Strahlungsmessungen. - 4: Die Messung der direkten Sonnenstrahlung. - 1. Instrument und Arbeitsmethode. - 2. Die Eichung. - 3. Die Ergebnisse der Messungen. - 4. Vergleich der Ergebnisse mit früheren Messungen in arktischen Gebieten. - 5. Berechnung des Trübungsfaktors. - 5: Die Registrierung der Totalstrahlung auf die Horizontalfläche. - 1. Das Instrument und seine Aufstellung. - 2. Die Eichung. - 3. Answertung der Registrierungen. - 4. Vergleiche nit anderen Messungen. - 5. Über das Verhältnis der Einstrahlung an heiteren und an bewölkten Tagen. - 6. Beziehung zwischen Bewölkungsgrad und Totalstrahlung. - 6: Strahlungsbilanzmessungen. - 1. Das Instrument und die Arbeitsmebhoden. - 2. Die Eichung. - 3. Theoretische Betrachtungen. - 4. Die Ergebnisse der Messungen. - 5. Der Einfluß der Bewölkung auf die Strahlungsbilanz. - 6. Der Tagesgang der Strahlungsbilanz an heiteren und an bewölkten Tagen. - 7. Betrachtung über die Ausstrahlung einer Schneeoberfläche. - 8. Vergleiche mit anderen Messungen. - Abschnitt 3. - Glaziologlsche Arbeiten an der Firnstation auf dem Sukkertoppen·Hochlandeis. - 7: Überblick über die Arbeiten an der Firnstation. - 1. Die Station: Aufbau, Einrichtung, Arbeitsplan. - 2. Der Schachtbau. - 8: Die Dichtebestimmungen von Firn- und Eisproben. - 1. Die Arbeitsmethoden. - 2. Die Ergebnisse. - 9: Die Feinstruktur des Firns und der Eisschichten. - 1. Arbeitsmethoden2. Die Ergebnisse A: Die Feinstruktur des Firns. - 3. Die Ergebnisse B: Die Feinstruktur der Eisschichten. - 4. Mikrophotographien von Firn- und Eisproben aus verschiedenen Tiefen. - 10: Versuch der experimentellen Bestimmung der Wärmeleitfähigkeit des Firns. - 1. Überblick über die bisher bekannten Werte der Wärmeleitfähigkeit von Schnee und Eis. - 2. Beschreibung des Instrumentes. - 3. Die Eichung der Instrumente. - 4. Die Ergebnisse. - 11: Temperaturmessungen im Firn. - 1. Die Arbeitsmethoden. - 2. Die Ergebnisse. - 12: Zusammenfassung aller Ergebnisse zu einer Analyse der Firnschichtung. - 1. Genaue Betrachtung der Firnstruktur: Können Jahresschichten festgestellt werden. - 2. Festlegung der Jahresschichten unter Zuhilfenahme der Dichtemessungen und der meteorologischen Beobachtungen der westgrönländischen Küstenstationen in vergangenen Jahren. - 3. Die Struktur des Firns als Bild des Klimas. - Abschnitt 4. - Meteorologische Arbeiten. - 13: Die Beobachtungen an den meteorologischen Stationen. - 1. Die Stationen. - 2. Die Beobachtung der verschiedenen meteorologischen Elemente. - 3. Beispiele einiger interessanter Registrierungen. - Abschnitt 5. - Gletschergeschwindigkeitsmessungen und photogrammetrische Arbeiten / von P. G. Mott. - 14: GIetschergeschwindigkeitsmessungen. - 1. Arbeitsplan und -methode. - 2. Die Ergebnisse. - 3. Fehlerbetrachtung. - 4. Die Schwankungen der Gletschergeschwindigkeit während der Meßperiode und ihre Ursachen. - 5. Die mittlere tägliche Geschwindigkeit als Funktion des Randabstandes. Gletschertiefe und Form des Untergrundes. - 6. Allgemeine gletscherkundliche Beobachtungen. - Anhang III: Die photogrammetrisch aufgenommene Karte vom Taterat-Gletscher 1 : 40 000. - Anhang I: Tabellen und Abb. 85 und 86. - Anhang II: Literaturverzeichnis.
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  • 15
    Call number: SR 90.0944(120) Schrank 9
    In: Abhandlungen
    Type of Medium: Series available for loan
    Pages: 22 S.
    Series Statement: Abhandlungen / Bayerische Akademie der Wissenschaften : Mathematisch- Naturwissenschaftliche Klasse N.F.; 120
    Language: German
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  • 16
    Call number: SR 90.0944(125) Schrank 9
    In: Abhandlungen
    Type of Medium: Series available for loan
    Pages: 138 S.
    Series Statement: Abhandlungen / Bayerische Akademie der Wissenschaften : Mathematisch- Naturwissenschaftliche Klasse N.F.; 125
    Language: German
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  • 17
    Monograph available for loan
    Monograph available for loan
    Ottawa : Geological Survey of Canada
    Associated volumes
    Call number: SR 90.0007(317) ; AWI G6-06-0042
    In: Bulletin
    Type of Medium: Monograph available for loan
    Pages: 49 S. + 4 pl.
    ISBN: 066010637X
    Series Statement: Bulletin / Geological Survey of Canada 317
    Language: English
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  • 18
    Monograph available for loan
    Monograph available for loan
    Dordrecht [u.a.] : Kluwer
    Call number: M 99.0101 ; AWI G7-86-0694
    Description / Table of Contents: This book is designed as a comprehensive mathematical introduction to the science of the behaviour of glaciers and ice sheets in their geophysical environment. Its main objective is to provide a better fundamental understanding of the problems of ice mechanics and fluid mechanics of large ice masses, and to connect and unify some of the approaches that have been developed in different disciplines concerned with glaciers and ice sheets. The first two chapters provide the physical background by treating ice within the framework of continuum physics and material science. The central part of the book deals with the conceptualization and mathematical formulation of glacier and ice sheet flow. Considerations concerning fluid mechanics and thermodynamics are given equal attention. The aim is to deduce common glaciological formulae from first principles and to state clearly the assumptions which lie behind the approximations. This allows the extension of the results - known to glaciologists in plane flow only - to three dimensions, thus paving the way for further research.
    Type of Medium: Monograph available for loan
    Pages: xxxvii, 510 S.
    ISBN: 9027714738
    Series Statement: Mathematical approaches to geophysics
    Classification:
    Meteorology and Climatology
    Language: English
    Note: TABLE OF CONTENTS: ACKNOWLEDGEMENTS. - PREFACE. - INTRODUCTION. - SYMBOLS AND NOTATION. - PART I. FUNDAMENTAL PHYSICS AND MATERIALS TECHNOLOGY OF ICE. - 1.General Concepts. - 1. Introduction. - 2. Equations of Balance. - 3. Material Response. - (a) General constitutive relations, simple materials. - (b) The rule of material objectivity. - (c) Material symmetry. - (d) Constitutive response for isotropie bodies. - (e) Materials with bounded memory-some constitutive representations. - (f) Incompressibility. - (g) Some representations of isotropic functions. - 4. The Entropy Principle. - (a) The viscous heat-conducting compressible fluid. - (b) The viscous heat-conducting incompressible fluid. - (c) Pressure and extra stress as independent variables. - (d) Thermoelastic solid. - (e) Final remarks. - 5. Phase Changes. - (a) Phase changes for a viscous compressible heat-conducting fluid. - (b) Phase changes for a viscous incompressible heat-conducting fluid. - References. - 2. A Brief Summary of Constitutive Relations for Ice. - 1. Preliminary Remarks. - 2. The Mechanical Properties of Hexagonal Ice. - (a) The crystal structure of ordinary ice. - (b) The elastic behavior of hexagonal ice. - (c) The inelastic behavior of single-crystal ice. - 3. The Mechanical Properties of Polycrystalline Ice. - (a) The elastic behavior of polycrystalline ice. - (b) Linear viscoelastic properties of polycrystalline ice. - (α) General theory. - (β) Experimental results. - (c) Non-linear viscous deformation and creep. - (α) Results of creep tests. - (β) Generalization to a three-dimensional flow law. - (γ) Other flow laws. - 4. The Mechanical Properties of Sea Ice. - (a) The phase diagram of standard sea ice and its brine conten. - (b) Elastic properties. - (c) Other material properties. - References. - PART II. THE DEFORMATION OF AN ICE MASS UNDER ITS OWN WEIGHT. - 3. A Mathematical Ice-flow Model and its Application to Parallel-sided Ice Slabs. - 1. Motivation and Physical Description. - 2. The Basic Model - Its Field Equations and Boundary Conditions. - (a) The field equations. - (α) Cold ice region. - (β) Temperate ice region. - (b) Boundary conditions. - (α) At the free surface. - (β) Along the ice-water interface. - (γ) Along the bedrock surface. - (δ) Along the melting surface. - 3. The Response of a Parallel-sided Ice Slab to Steady Conditions. - (a) Dimensionless forms of the field equations. - (b) Parallel-sided ice slab, a first approximation to glacier and ice-shelf flow dynamics. - (α) Velocity and temperature fields x-independent. - (β) Extending and compressing flow. - (γ) Floating ice shelves 4. Concluding Remark. - References. - 4. Thermo-mechanical Response of Nearly Parallel-sided Ice Slabs Sliding over their Bed. - 1. Motivation. - 2. The Basic Boundary-value Problem and its Reduction to Linear Form. - 3. The Solution of the Boundary-value Problems. - (a) Zeroth-order problem. - (b) First-order problem. - (α) Harmonic perturbation from uniform flow for a zero accumulation rate. - (β) Analytic solution for a Newtonian fluid. - (γ) Numerical solution for non-linear rheology. - (δ) Effect of a steady accumulation rate. - (ε) A historical note on a previous approach. - (η) The first-order temperature problem. - (c) Numerical results for steady state. - (α) Transfer of bottom protuberances to the surface. - (β) Basal stresses. - (γ) Surface velocities. - (δ) Effect of a steady accumulation rate. - 4. Remarks on Response to a Time-dependent Accumulation Rate. - 5. Surface-wave Stability Analysis. - (a) The eigenvalue problem. - (b) Discussion of results. - 6. Final Remarks. - References. - 5. The Application of the Shallow-ice Approximation. - 1. Background and Previous Work. - 2. Derivation of the Basal Shear-stress Formula by Integrating the Momentum Equations over Ice Thickness. - (a) Derivation. - (b) The use of the basal shear-stress formula in applied glaciology. - 3. Solution of the Ice-flow Problem using the Shallow-ice Approximation. - (a) Governing equations. - (b) Shallow-ice approximation. - (c) Construction of the perturbation solution. - (d) Results. - (e) Temperature field. - 4. Theoretical Steady-state Profiles. - (a) Earlier theories and their limitations. - (b) Surface profiles determined by using the shallow-ice approximation. - 5. An Alternative Scaling - a Proper Analysis of Dynamics of Ice Sheets with Ice Divides. - (a) Finite-bed inclination. - (b) Small-bed inclination. - (c) Illustrations. - References. - 6. The Response of a Glacier or an Ice Sheet to Seasonal and Climatic Changes. - 1. Statement of the Problem. - 2. Development of the Kinematic Wave Theory. - (a) Full non-linear theory. - (b) Perturbation expansion-linear theory. - (c) An estimate for the coefficients C and D. - (d) Boundary and initial conditions. - 3. Theoretical Solutions for a Model Glacier. - (a) Solutions neglecting diffusion. - (b) Theoretical solutions for a diffusive model. - (α) Coefficient functions for the special model. - (β) Solution for a step function. - (γ) General solution for uniform accumulation rate. - (δ) The inverse problem - calculation of climate from variations of the snout. - 4. General Treatment for an Arbitrary Valley Glacier. - (a) Fourier analysis in time. - (α) Low-frequency response. - (β) High-frequency response. - (γ) Use of the results. - (b) Direct integration methods. - 5. Derivation of the Surface-wave Equation from First Principles Non-linear Theory. - (a) Surface waves in the shallow-ice approximation. - (α) Integration by the methods of characteristics. - (β) An illustrative example. - (γ) A remark on linearization. - (δ) Effects of diffusion. - (b) Remarks regarding time-dependent surface profiles in ice sheets. - (c) Long waves in an infinite ice slab - Is accounting for diffusion enough?. - (α) Basic equations. - (β) Construction of perturbation solutions. - (γ) Numerical results. - 6. Concluding Remarks. - References. - 7. Three-dimensional and Local Flow Effects in Glaciers and Ice Sheets. - 1. Introduction. - 2. Effect of Valley Sides on the Motion of a Glacier. - (a) Solutions in special cases. - (α) Exact solutions for the limiting cases. - (β) Solution for a slightly off-circular channel. - (γ) A note on very deep and wide channels. - (b) A useful result for symmetrical channels with no boundary slip. - (c) Numerical solution - discussion of results. - 3. Three-dimensional Flow Effects in Ice Sheets. - (a) Basic equations. - (b) Decoupling of the stress-velocity problem from the problem of surface profile. - (c) The equation describing the surface geometry. - (d) The margin conditions. - 4. Variational Principles. - (a) Fundamental variational theorem. - (b) Variational principle for velocities. - (c) Reciprocal variational theorem. - (d) Maximum and minimum principles. - (e) Adoption of the variational principles to ice problems. - 5. Discussion of Some Finite-element Solutions. - References. - Appendix: Detailed Calculations Pertaining to Higher-order Stresses in the Shallow-ice Approximation. - AUTHOR INDEX. - SUBJECT INDEX.
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  • 19
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    Berlin : Akademie-Verlag
    Call number: O 3364/2 ; 1.2/WE 42 ; 6664 ; 1.2/WE 44 ; AWI S5-98-0234 ; AWI S5-17-49878
    Type of Medium: Monograph available for loan
    Pages: XII, 508 Seiten , 30 cm
    Language: German , Russian
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  • 20
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    Call number: O 1088(2)
    In: Die Differential- und Integralgleichungen der Mechanik und Physik
    Type of Medium: Monograph available for loan
    Pages: XXIII, 863 S.
    Language: German
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  • 21
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    Call number: O 1182
    Type of Medium: Monograph available for loan
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  • 22
    Call number: 691 / Regal 12
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    Pages: VII, 152 S. : Taf.
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  • 23
    Call number: G 7860 ; AWI E1-92-0156 ; AWI E1-09-0010
    Type of Medium: Monograph available for loan
    Pages: 60 S. : zahlr. Ill., Kt.
    ISBN: 3496010088
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  • 24
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    Wien [u.a.] : Springer [u.a.]
    Associated volumes
    Call number: 13254 ; 13321 ; G 8407 ; AWI G8-92-0396
    In: Angewandte Geophysik
    Type of Medium: Monograph available for loan
    Pages: 353 S. : graph. Darst.
    ISBN: 3211817409
    Language: German
    Note: Inhaltsverzeichnis: 1. Theoretische Grundlagen der angewandten Gravimetrie und Magnetik / Dr. rer. nat. habil. Rolf Rösler. - 1.1. Einleitung. - 1.1.1. Zielstellung. - 1.1.2. Die potentielle Energie. - 1.1.3. Die Potentialfunktion. - 1.2. Das NEWTONsche Volumenpotential. - 1.2.1. NEWTONsches Gravitationspotential. - 1.2.1.1. Das Gravitationsgesetz und die Bestandteile des Schwerevektors. - 1.2.1.2. Einige Eigenschaften der Äquipotentialflächen. - 1.2.2. Die räumliche und flächenhafte Massenverteilung. - 1.2.2.1. Das Potential einer räumlichen Massenverteilung. - 1.2.2.2. Die Ableitungen des Volumen- und des Flächenpotentials. - 1.2.3. Das Potential im Inneren. - 1.2.3.1. Die Existenz des Potentials. - 1.2.3.2. Das Potential einer masseerfüllten Kugel. - 1.2.4. Die BOUGUER-Plattenwirkung. - 1.2.4.1. Die Schwerewirkung einer Kreisscheibe. - 1.2.4.2. Die ebene BOUGUER-Platte. - 1.2.4.3. Die sphärische BOUGUER-Platte. - 1.2.5. Einige Störkörperformeln. - 1.2.5.1. Die Kugel. - 1.2.5.2. Der Quader. - 1.2.5.3. Die vertikale halbunendliche Säule. - 1.2.5.4. Die horizontale halbunendliche Säule. - 1.2.5.5. Die Viertel-Platte. - 1.2.5.6. Höhere Potentialableitungen für den Quader und seine Spezialfalle. - 1.2.5.7. Weitere Störkörperformeln. - 1.3. Dipol- und Multipol-Potentiale. - 1.3.1. Das Dipolpotential. - 1.3.2. Das Potential einer Doppelschicht. - 1.3.3. Die Entwicklung des Volumenpotentials in Multipolpotentiale. - 1.3.3.1. Das Multipolpotential. - 1.3.3.2. Eine Reihenentwicklung des reziproken Abstandes. - 1.3.3.3. Die Reihenentwicklung des Gravitationspotentials der Erde. - 1.3.3.4. Die Entwicklung des Magnetfeldes der Erde nach Kugelfunktionen. - 1.3.4. Das Potential und das Magnetfeld magnetisierter Körper. - 1.3.4.1. Das Problem der Berechnung geomagnetischer Anomalien. - 1.3.4.2. Der Zusammenhang mit dem Schwerepotential. - 1.3.4.3. Die Anomalien des magnetischen Feldes. - 1.3.5. Einige Störkörperformeln für magnetische Anomalien. - 1.3.5.1. Die Kugel. - 1.3.5.2. Der Quader. - 1.3.5.3. Spezialfälle des Quaders. - 1.4. Ebene Potentialfelder. - 1.4.1. Das logarithmische Potential. - 1.4.2. Die Ableitungen des Potentials. - 1.4.2.1. Körper beliebigen Querschnitts. - 1.4.2.2. Die ebene Flächenmasse. - 1.4.2.3. Die Darstellungen des Potentialgradienten mittels komplexer Funktionen. - 1.4.3. Einige Störkörperformeln. - 1.4.3.1. Horizontaler, homogener Kreiszylinder. - 1.4.3.2. Die halbunendliche, dünne Platte. - 1.4.3.3. Das horizontale Rechteck-Prisma. - 1.4.3.4. Die senkrechte Stufe. - 1.4.3.5. Die geneigte Stufe. - 1.4.3.6. Das Prisma mit Polygonquerschnitt. - 1.4.3.7. Die geneigte Platte. - 1.4.4. Störkörperformeln für magnetische Anomalien (ebener Fall). - 1.4.4.1. Der horizontale Kreiszylinder. - 1.4.4.2. Die geneigte Stufe. - 1.4.4.3. Weitere Störkörperformeln. - 1.5. Grundlagen der Interpretation. - 1.5.1. Die Mehrdeutigkeit der Interpretation. - 1.5.2. Feldtransformationen. - 1.5.2.1. Die Aufgabe der Feldtransformationen. - 1.5.2.2. Die Feldfortsetzung. - 1.5.2.3. Die Berechnung höherer vertikaler Ableitungen. - 1.5.2.4. Die Spektraldarstellung des Potentials und seiner Ableitungen mittels FOURIER-Transformation. - 1.5.2.5. Die Transformation magnetischer Anomalien. - 1.5.2.6. Die Glättung der transformierten Feldgrößen. - 1.5.2.7. Anwendung auf ebene Probleme. - 1.5.3. Inverse Aufgaben. - 2. Angewandte Gravimetrie / Dr. rer. nat. Harald Lindner ; Dr. rer. nat. habil. Heinz Militzer ; Dr. mont. Georg Walach. - 2.1. Geophysikalische, geologische und ingenieurtechnische Grundlagen. - 2.1.1. Das Schwerefeld der Erde. - 2.1.2. Ursache und Größenordnung von Schwereanomalien. - 2.1.3. Aufgabenstellung, Einsatzkriterien und Grenzen der Anwendung. - 2.2. Meßgrößen und Meßgeräte. - 2.2.1. Meßgrößen. - 2.2.2. Gravimeter. - 2.2.3. Gradientenmesser. - 2.3. Vorbereitung und Durchführung von Messungen. - 2.3.1. Eichung. - 2.3.2. Bezugs- und Anschlußpunkte, Schwerenetze. - 2.3.3. Gangbestimmung. - 2.3.4. Punktabstand. - 2.3.5. Regionalaufnahme. - 2.3.6. Spezialaufnahme. - 2.3.7. Mikroaufnahme. - 2.3.8. Messungen unter besonderen Bedingungen. - 2.3.8.1. See- und Flugzeugmessungen. - 2.3.8.2. Schacht- und Bohrlochmessungen. - 2.3.8.3. Untertagemessungen. - 2.3.9. Gradientenmessungen. - 2.4. Reduktionen und Anomalien. - 2.4.1. Zielstellung. - 2.4.2. Normalschwerereduktion. - 2.4.3. Freiluftreduktion. - 2.4.4. Geländereduktion für Messungen über- und untertage. - 2.4.5. BOUGUER-Reduktion. - 2.4.6. Isostatische Reduktion. - 2.4.7. BOUGUER-Anomalie. - 2.4.8. Freiluft-Anomalie. - 2.4.9. Isostatische Anomalie. - 2.5. Petrophysikalische Grundlagen der angewandten Gravimetrie. - 2.5.1. Klassifikation von Dichten. - 2.5.2. Dichtewerte verschiedener Gesteine. - 2.5.3. Dichtebestimmung mit Labormethoden. - 2.5.4. Dichtebestimmung mit gravimetrischen Methoden. - 3. Angewandte Magnetik / Dr. rer. nat. habil. Heinz Militzer ; Dipl.-Geophys. Reiner Scheibe ; Dr. phil. Wolfgang Seiberl. - 3.1. Geophysikalische, geologische und ingenieurtechnische Grundlagen. - 3.1.1. Magnetfeld der Erde und magnetische Anomalien. - 3.1.2. Aufgabenstellung und Einsatzkriterien. - 3.2. Meßgrößen und Meßgeräte. - 3.2.1. Meßkomponenten. - 3.2.2. Mechanisch-optische Magnetometer (Feldwaagen). - 3.2.3. Sättigungskernmagnetometer (Ferrosonde, FÖRSTER-Sonde, fluxgate-Magnetometer). - 3.2.4. Kernpräzessionsmagnetometer (Protonenmagnetometer, Kerninduktionsmagnetometer). - 3.2.5. Absorptionszellenmagnetometer (Quantenmagnetometer, Magnetometer mit optisch gepumpten Gasen). - 3.2.6. Apparative, zweckgebundene Besonderheiten. - 3.3. Vorbereitung und Durchführung von Messungen. - 3.3.1. Eichung. - 3.3.2. Anschluß der Messungen, magnetische Netze. - 3.3.3. Fehlerbestimmung. - 3.3.4. Profil- und Punktabstand. - 3.3.5. Regionalaufnahme. - 3.3.6. Spezialaufnahme. - 3.3.7. Mikroaufnahme. - 3.3.8. Gradientenmessung. - 3.3.9. Messungen unter besonderen Bedingungen. - 3.3.9.1. Aeromessungen. - 3.3.9.1.1. Magnetometereinbau im Fluggerät. - 3.3.9.1.2. Flugwegbestimmungen. - 3.3.9.1.3. Flughöhenbestimmung. - 3.3.9.1.4. Aeromagnetisches Flugnetz. - 3.3.9.2. Seemessungen. - 3.3.9.3. Untertagemessungen. - 3.3.9.4. Bohrlochmessungen. - 3.4. Korrekturen und Reduktionen. - 3.4.1. Zielstellung. - 3.4.2. Variationskorrektur. - 3.4.3. Instrumentengangkorrektur. - 3.4.4. Normalfeldreduktion. - 3.4.5. Höhenreduktion. - 3.4.6. Geländereduktion. - 3.4.7. Kompilation von aeromagnetischen und seemagnetischen Messungen. - 4. Paläo- und Archäomagnetik / Dr. mont. Hermann Mauritsch. - 4.1. Einleitung. - 4.2. Physikalische Grundlagen. - 4.3. Physikalische Theorie des Gesteinsmagnetismus. - 4.4. Remanente Magnetisierung natürlicher Gesteine. - 4.5. Spannungseffekte und Anisotropie. - 4.6. Die magnetischen Mineralien. - 4.7. Die Magnetisierung natürlicher Gesteine. - 4.8. Die Probennahme. - 4.9. Messung der Remanenz. - 4.10. Verfahren der magnetischen Reinigung. - 4.11. Feldfreier Raum. - 4.12. Zuverlässigkeitstest paläomagnetischer Ergebnisse. - 4.13. Statistische Analyse. - 4.14. Vergleich paläomagnetischer Daten. - 4.15. Berechnung des paläomagnetischen Pols. - 4.16. Darstellung paläomagnetischer Ergebnisse. - 4.17. Paläointensitätsmessungen. - 4.18. Ergebnisse paläomagnetischer Untersuchungen. - 4.18.1. Magnetostratigraphie. - 4.18.2. Polwanderung und Kontinentaldrift. - 4.18.3. Paläogeographie. - 4.19. Praktische Anwendungsbeispiele. - 4.20. Archäomagnetik. - 5. Bearbeitung und Interpretation der gravimetrischen und magnetischen Meßergebnisse / Dr. rer. nat. Harald Lindner ; Dr. rer. nat. habil. Heinz Militzer ; Dr. rer. nat. habil. Rolf Rösler ; Dipl.-Geophys. Reiner Scheibe. - 5.1. Zielstellung. - 5.2. Bearbeitungsverfahren und Interpretationsbeispiele. - 5.2.1. Verfahren der Feldtransformation. - 5.2.1.1. Regional- und Lokalfeld. - 5.2.1.2. Wellenlängenfilt
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  • 25
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    Stuttgart : Wiss. Verl.-Ges.
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    Call number: G 8130 ; AWI E1-82-0083
    In: Große Naturforscher
    Description / Table of Contents: In seiner Doktorarbeit behandelte er ein Thema aus der Astronomie. Sein Lehrbuch "Thermodynamik der Atmosphäre", das in mehreren Auflagen erschien, wies ihn als Meteorologen aus. In Graz erhielt er eine Professur nicht nur für die Wetterkunde, sondern auch für Geophysik. Bei vier großen Grönlandexpeditionen verwirklichte er seinen Jugendtraum, Polarforschung zu treiben. Und fast nur am Rande gehört hierher, daß er in jungen Jahren einen Weltrekord im Ballondauerflug aufgestellt hatte ... Von einer der großen, vielseitigen Forscherpersönlichkeiten unseres Jahrhunderts ist hier die Rede: von Alfred Wegener, der seinen dauerhaften Ruhm 1912 mit der revolutionären Hypothese begründete, wonach die Festländer gar nicht so "fest" seien, wie man bis dahin angenommen hatte, sondern daß sie im Laufe der Erdgeschichte langsam wanderten. Zu seinen Lebzeiten für die meisten ein "Märchenerzähler", wurde Wegener in jüngster Zeit, Jahrzehnte nach seinem tragischen Tod in Grönland, für viele ein "neuer Kopernikus": an Wegener schieden sich die Geister. Selten hat ein neues Gedankengebäude über die Entstehung der Erdkruste, ihrer Gebirge und Ozeane so anregend für Geologen und Geophysiker gewirkt wie die "Drifthypothese". Die von Professor M. Schwarzbach verfaßte Biographie zeichnet nicht nur ein Lebensbild Wegeners, sondern umfaßt damit gleichzeitig ein Stück Wissenschaftsgeschichte, ein herausragendes Kapitel der Erforschung der Erde - von der Verschiebung der Kontinente und der heute im Vordergrund stehenden "Plattentektonik" bis hin zur Eiszeitforschung, den Strahlungskurven von Milankovitch und der "nächsten Eiszeit".
    Type of Medium: Monograph available for loan
    Pages: 159 S. , Ill., Kt.
    ISBN: 3-8047-0582-0
    Series Statement: Große Naturforscher 42
    Language: German
    Note: Inhaltsverzeichnis: Vorwort. - 1. Alexander v. Humboldt und die Vorfahren von Alfred Wegener. - 2. Der Lebensweg von Alfred Wegener. - Berlin und die Studienjahre (1880-1904). - Lindenberg (1905-1906). - Marburg (1908-1918). - Hamburg (1919-1924). - Graz (1924-1930). - 3. Die Grönland-Reisen. - Die dänische "Danmark"-Expedition unter Leitung von L. Mylius-Erichsen (1906-08). - Die Durchquerung Nordgrönlands mit J. P. Koch (1912/13). - Die Vorexpedition nach Westgrönland unter Leitung von A. Wegener (1929). - Deutsche Grönland-Expedition Alfred Wegener, Hauptexpedition (1930/31). - Eine Schuldfrage?. - Rückblick auf die Grönland-Reisen. - 4. Alfred Wegener und Island. - Islands "Spalten" und die Drifthypothese. - 5. Das wissenschaftliche Lebenswerk von Alfred Wegener. - Der vielseitige Meteorologe. - Das Hauptwerk: Die wandernden Kontinente. - Kontinentalverschiebung und das Klima der Vorzeit. - Der ideale Schwiegervater. - Paläoklima und Kontinentalverschiebung. - Die Strahlungskurven von Milankovitch. - Warum Eiszeiten und Eiszeitalter?. - Ein Rückblick auf Köppen. - 6. Die ersten 40 Jahre der "wandernden Kontinente". - Der erste Vortrag und das erste Buch über kontinentale Drift. - Der Prophet gilt nichts in seinem Vaterlande. - Continental drift debate in New York, 1926. - Konvektionsströmungen: Ampferer, Schwinner, Holmes. - Africa forms the key. - Geodätische Beweise. Wegeners Irrtum. - 7. Die Wiedergeburt der "Kontinentalverschiebung": die Plattentektonik. - Tiefseeforschung und Paläomagnetismus. - Plattentektonik und Wegeners "Kontinentalverschiebungshypothese. - Gebirgsbildung und Pangaea. - Von der abstrakten Kunst zur Demoskopie. - Ein faszinierendes Gesamtbild. - 8. Ruhm und Nachruhm von Alfred Wegener. - 9. Schrifttum. - Verzeichnis der wichtigsten Schriften von A. Wegener. - Größere Veröffentlichungen über A. Wegener und seine letzte Grönlandfahrt. - Nachrufe, Gedenkaufsätze, Kurzbiographien, Film. - Einige Veröffentlichungen zur allgemeinen Einführung in die Plattentektonik. - Herkunft der Abbildungen. - 10. Anmerkungen. - Lebensdaten von A. Wegener. - 11. Register. - Namensverzeichnis. - Sachverzeichnis.
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  • 26
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    Berlin [u.a.] : Springer
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    Call number: 710 / Regal 12
    In: Ergebnisse der Mathematik und ihrer Grenzgebiete
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    Leipzig [u.a.] : Deuticke
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    Call number: 1237/3 / Regal 12
    In: Lehrbuch der Geologie
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    Halle (Saale) : Knapp
    Call number: 1046 / Regal 12
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    New York [u.a.] : Charles Scribner's Sons
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    Berlin : Springer
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    London : Oxford University Press
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    Leipzig : Brockhaus
    Call number: G 8204 ; AWI E3-83-0644
    Description / Table of Contents: Siebenundzwanzig Antarktisfahrer hat Herausgeber Gert Lange um ihre Erlebnisberichte gebeten. Die Forscher - es sind Vertreter der verschiedensten Fachrichtungen, wie Geodäsie, Strahlungsmessung, Ionosphärenuntersuchung, Glaziologie, Geologie, Meteorologie, Zoologie - erläutern in allgemein-verständlicher Form ihre wissenschaftlichen Aufgaben und Ergebnisse, schildern ebenso gefahrenvolle wie absonderliche Begebenheiten und beeindruckende Naturerscheinungen. So erlebte zum Beispiel Dr. Klaus Dreßler, Teilnehmer der 17. SAE, eine besonders schöne Fata Morgana: "... Auf der Gegenstation in 1,2km Entfernung erschien hoch über unserem Kettenfahrzeug eine große Flagge oder Rauchfahne, die sich nach unten ausdehnte, bis das Fahrzeug plötzlich dreifach überhöht erschien. Ebenso alle anderen Gegenstände. Durchs Fernrohr sah ich Artur ein zweites Mal über sich selbst, aber auf dem Kopfe stehend und mitunter so lang gestreckt wie in einem Zerrspiegel ... Gegenstände, sonst nicht sichtbar, kamen über dem Horizont zum Vorschein. Besonders schön: die roten und schwarzen Tafeln der Landebahnmarkierung. Sie waren sonst hinter einem Schneerücken verborgen, jetzt tauchten sie in ihrer normalen Grüße etwas zehn Meter über der Oberfläche auf. Dann verwandelten sie ich in schlanke Säulen. Der eigenartigste Effekt war, daß die Traktoren, Bulldozer und anderen Geräte für die Flugplatzunterhaltung, sonst in derselben Entfernung deutlich sichtbar, zeitweise ganz verschwanden. Alle diese Erscheinungen wechselten langsam innerhalb von ein bis fünf Minuten..." Derartige, auf Grund besonders starker Ablenkung des Lichtes in der Antarktis vorkommende Erscheinungen beeinträchtigen natürlich die Meßarbeiten, ebenso wie tiefe Temperaturen und häufige Schneestürme sehr hinderlich für topographische und andere Arbeiten sind. Seit 1959 überwinterten mehr als siebzig DDR-Wissenschaftler im Rahmen der SAE (Sowjetische Antarktisexpeditionen) auf dem weißen Kontinent, der mit seinen Schönheiten und Widrigkeiten von Mensch und Maschie immer wieder Bewährung in schwierigen Situationen verlangt.
    Type of Medium: Monograph available for loan
    Pages: 218 Seiten , Illustrationen
    Edition: 1. Auflage
    Language: German
    Note: Inhaltsverzeichnis Vorwort 5. SAE Gefangene der Insel / Günter Skeib 6. SAE Hauptobservatorium Mirny / Stephan Klemm Auf Empfangsstation an der Prawda-Küste / Peter Glöde 7. SAE Ein ganz unnormaler schöner Tag / Joachim England 8. SAE Südliche Sterne im Fadenkreuz / Joachim Liebert Das Inferno / Günter Leonhardt 10. SAE Schwereanschlußmessung Potsdam-Mirny / Claus Elstner Unterwegs auf dem Inlandeis / Tankred Schmidt 13. SAE Wie die ersten Bilder entstanden / Peter Glöde Antarktika aus kosmischer Sicht / Hartwig Gernandt, Joachim Hofmann 14. SAE Wostok - ein Jahr im Inneren des Kontinents / M. Manfred Schneider Nachts, wenn der Himmel leuchtet / Hans Driescher 17. SAE Das Lager am Abendberg / Reinhard Dietrich 8000 Kilometer über Eis und Schnee / Artur Zielke Kreuz und quer über die Berge der Freundschaft / Klaus Dreßler Helikopter-Sprünge / Siegfried Meier 19. SAE Das Hüttendreieck auf dem Inlandeis / Georg Dittrich Temperaturprofile im Gletscherwind / Alfred Helbig An den Nunatakkern der Prinz-Charles-Berge / Joachim Hofmann 20. SAE Beobachtungen eines Arztes / Georg Schrader 21. SAE Ein Observatorium entsteht / Hartwig Gernandt Radionuklide in Antarktika / Detlef Hebert 22. SAE Als Geologe in den Read Mountains / Hans-Jürgen Paech 23. SAE Im Spaltennetz des Hays-Gletschers / Rainer Hoyer Der Marsch durch die Oase / Gerhard Strauch 24. SAE Expeditionsglück, Expeditionsleid / Klaus Peukert 25. SAE Warum Robben und Pinguine gezählt werden / Klaus Odening Auf in neue unbekannte Gebiete / Werner Passehl 26. SAE Aus der Werkstatt der Expeditionen / Bodo Tripphan Die Antarktis im Licht der Weltpolitik / M. Manfred Schneider Register
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  • 33
    Call number: O 1020(2) / Regal 11 ; G 1040 / Regal 12 ; MOP 41368 / Mitte
    In: Einführung in die Geophysik
    In: Naturwissenschaftliche Monographien und Lehrbücher
    Description / Table of Contents: Dem ersten Bande der "Einführung in die Geophysik" folgt hiermit ein zweiter Band, der in drei Abschnitten den "Erdmagnetismus mit seinen Nebengebieten, dem Erdstrom und den Polarlichtern", die "Wärme- und Temperaturverhältnisse der obersten Bodenschichten" und die "Luftelektrizität" behandelt. Wieder haben die drei Teile verschiedene Verfasser. Es entspricht dies dem Werdegang der Geophysik als Wissenschaft. Ursprünglich aus weit voneinander liegenden Sondergebieten bestehend, mit verschiedenen Aufgaben und verschiedenen Arbeitsweisen, fangt die Geophysik erst in unseren Tagen an, zu einem einheitlichen Wissensgebiet zu verschmelzen. Noch sind wir Zuschauer dieses Vorganges, noch bahnt sich die Verschmelzung erst an, und so ware es vorzeitig, jetzt schon das an Umfang so sehr gewachsene Feld von einem einzigen Bearbeiter darstellen lassen zu wollen. Der aufmerksame Leser wird jedoch leicht finden, wie die verschiedenen Einzelzweige sich schon innerhalb der Darstellung unserer Einführung in die Geophysik begegnen. Es ist das Ziel der einzelnen Verfasser und des Verlages, ein Werk zu schaffen, das auf dem Wege zur Verschmelzung aller Einzelfächer einen neuen Ausgangspunkt abgeben kann. Dementsprechend werden besonders die neuesten Fragen und Probleme behandelt, und die Richtung gezeigt, in der sich die heutige Wissenschaft weiter bewegt.
    Type of Medium: Monograph available for loan
    Pages: IX, 388 Seiten , Illustrationen
    ISBN: 978-3642894510
    Series Statement: Naturwissenschaftliche Monographien und Lehrbücher 8
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  • 34
    Monograph available for loan
    Monograph available for loan
    Dresden [u.a.] : Steinkopff
    Associated volumes
    Call number: O 987
    In: Wissenschaftliche Forschungsberichte
    Type of Medium: Monograph available for loan
    Pages: XII, 258 S. : graph. Darst.
    Series Statement: Wissenschaftliche Forschungsberichte 15
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  • 35
    Monograph available for loan
    Monograph available for loan
    Dresden [u.a.] : Steinkopff
    Call number: 804 / Regal 12
    Type of Medium: Monograph available for loan
    Pages: XII, 368 S. : Ill.
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  • 36
    Monograph available for loan
    Monograph available for loan
    Berlin : Springer
    Associated volumes
    Call number: 1123 / Regal 12 ; O 2202/1 / Regal 12
    In: Vorlesungen über Integral- und Differentialrechnung
    Type of Medium: Monograph available for loan
    Pages: XI, 436 S. : Ill.
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  • 37
    Call number: MOP A4 43249/2
    Type of Medium: Monograph available for loan
    Pages: 232 S.
    Edition: 3. Aufl.
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  • 38
    Series available for loan
    Series available for loan
    Bremerhaven : Alfred-Wegener-Inst. für Polar- und Meeresforschung
    Associated volumes
    Call number: ZSP-168-1
    In: Berichte zur Polarforschung
    Type of Medium: Series available for loan
    Pages: 50 S. : Ill., graph. Darst., Kt.
    Series Statement: Berichte zur Polarforschung 1
    Language: German
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  • 39
    facet.materialart.
    Unknown
    Canberra ; 132.1984-147.2002
    Call number: ZSP-123
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  • 40
    Call number: ZSP-403-54
    In: Jare Data Reports
    Type of Medium: Series available for loan
    Pages: 31 S. : graph. Darst.
    Series Statement: Jare Data Reports 54 : Seismology 13
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  • 41
    Call number: ZSP-403-53
    In: Jare Data Reports
    Type of Medium: Series available for loan
    Pages: 23 S. : Ill.
    Series Statement: Jare Data Reports 53 : Ionosphere 21
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  • 42
    Call number: MOP 12884/5+7 / DG ; AWI P8-91-0001
    In: Wissenschaftliche Ergebnisse der deutschen Grönland-Expedition Alfred Wegener 1929 und 1930/1931
    Type of Medium: Monograph available for loan
    Pages: 91, 73 S.
    Series Statement: Wissenschaftliche Ergebnisse der deutschen Grönland-Expedition Alfred Wegener 1929 und 1930/1931 5 + 7
    Note: Inhalt Band 5: Vorbemerkung. - 1. Die geographischen Ortsbestimmungen / Karl Weiken. - 1.1. Allgemeines. - 1.2. Die Instrumente. - a) Der Theodolit. - b) Ein Sextant mit künstlichem Horizont. - 1.3. Die Uhren. - 1.4. Beobachtungen zur geographischen Ortsbestimmung. - 1.5. Ergebnise der geographischen Ortsbestimmung. - 1.6. Die Berechnung der Uhrstände. - 1.7. Die geographischen Koordinaten. - 1.8. Die geographischen Koordinaten von Eismitte. - 2. Schwerkraftmessungen mit Pendeln / Karl Weiken. - Einleitung. - 2.1. Die Pendelstationen. - 2.2. Die Pendelapparatur. - 2.3. Die Uhren. - 2.4.Die Reduktion der gemessenen Schwingungszeiten. - 2.5. Die Messungen. - 2.6. Die Ausgleichung der Schwingungszeiten und die Berechnung der Schwerewerte. - 2.7. Die Genauigkeit der Messungen. - a) Die Genauigkeit der Messungen auf der Anschlußstation Potsdam. - b) Die Genauigkeit der Messungen auf den grönländischen Stationen. - c) Die Veränderlichkeit der Pendel. - d) Fehler in der Bestimmung der Pendeltemperatur. - e) Fehler der Temperaturkonstanten. - f) Fehler in der Bestimmung der relativen Luftdichte. - g) Fehler in der Bestimmung des Uhrganges. - h) Zusammenfassung der Fehler. - 2.8. Die Schwerewerte und ihre mittleren Fehler. - 2.9. Die Berechnung der Schwereanomalien. - 3. Ergebnisse der Registrierung der Windgeschwindigkeit an der Weststation / Rupert Holzapfel. , Inhalt Band 7: Zusammenfassung der wissenschaftlichen Ergebnisse / Kurt Wegener. - Einleitung. - 1. Die meteorologischen Ergebnisse. - A. Statistische Meteorologie. - 1. Der Inlandeiswind. - 2. Die Temperatur. - 3. Der Luftdruck. - 4. Die Strahlung. - 5. Die Feuchte. - 6. Die Wolken. - B. Ergänzungen zur Frage von Temperatur und Luftdruck. - C. Die "glaziale Antizyklone". - D. Das Wetter. - E. Die Aussichten eines Luftverkehrs über Grönland. - 2. Das Inlandeis. - A. Der Zuwachs des Eises. - B. Das Spalten- oder Randgebiet. - C. Die Dichte des Firns. - D. Die Temperatur des Eises. - E. Die Eisdicke nach seismischen Beobachtungen. - 1. Die Grundlagen. - 2. Die Wirkung der Anisotropie auf die seismischen Wellen. - 3. Die Aufeinanderfolge der Messungen. - 4. Die Laufzeitkurven. - 5. Die gemessenen Eisdicken. - 6. Die Korrektur für Temperatur und Dichte zugleich. - F. Die Beobachtungen der Gletscherfronten im Bezirk Umanak. - Berichtigungen zu den bereits erschienenen Bänden nach Angaben der Verfasser.
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  • 43
    Call number: ZSP-403-59
    In: Jare Data Reports
    Type of Medium: Series available for loan
    Pages: 34 S. : graph. Darst.
    Series Statement: Jare Data Reports 59 : Seismology 14
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  • 44
    Call number: ZSP-403-63
    In: Jare Data Reports
    Type of Medium: Series available for loan
    Pages: 43 S. : Ill.
    Series Statement: Jare Data Reports 63 : Glaciology 7
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  • 45
    Call number: ZSP-403-67
    In: Jare Data Reports
    Type of Medium: Series available for loan
    Pages: 42 S. : Kt.
    Series Statement: JARE data reports 67 : Marine biology 3
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  • 46
    Series available for loan
    Series available for loan
    Tokyo : Inst.
    Associated volumes
    Call number: ZSP-403-97
    In: Jare Data Reports
    Type of Medium: Series available for loan
    Pages: 80 S. : Ill.
    Series Statement: Jare Data Reports 97 : Aurora 12
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  • 47
    Call number: ZSP-403-96
    In: Jare Data Reports
    Type of Medium: Series available for loan
    Pages: 80 S.
    Series Statement: Jare Data Reports 96 : Glaciology 11
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  • 48
    Call number: ZSP-403-95
    In: Jare Data Reports
    Type of Medium: Series available for loan
    Pages: 39 S.
    Series Statement: Jare Data Reports 95 : Oceanography 4
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  • 49
    Call number: ZSP-403-94
    In: Jare Data Reports
    Type of Medium: Series available for loan
    Pages: 117 S.
    Series Statement: Jare Data Reports 94 : Glaciology 10
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  • 50
    Series available for loan
    Series available for loan
    Tokyo : Inst.
    Associated volumes
    Call number: ZSP-403-92
    In: Jare Data Reports
    Type of Medium: Series available for loan
    Pages: 75 S. : graph. Darst.
    Series Statement: Jare Data Reports 92 : Seismology 17
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  • 51
    Call number: ZSP-403-91
    In: Jare Data Reports
    Type of Medium: Series available for loan
    Pages: 38 S.
    Series Statement: Jare Data Reports 91 : Oceanography 3
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  • 52
    Call number: ZSP-403-90
    In: Jare Data Reports
    Type of Medium: Series available for loan
    Series Statement: Jare Data Reports 90 : Marine biology 5
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  • 53
    Call number: AWI A4-89-0036-3 ; MOP 45231/C / Mitte
    In: Spravočnik po klimatu Antarktidy / pod red. I. M. Dolgina, Tom 3
    Type of Medium: Monograph available for loan
    Pages: 270 Seiten , Illustrationen
    Series Statement: Spravočnik po klimatu Antarktidy / pod red. I. M. Dolgina 3
    Language: Russian
    Note: In kyrillischer Schrift
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  • 54
    Call number: AWI A4-90-0142
    In: Trudy sovetskoj antarktičeskoj ėkspedicii, 74
    Type of Medium: Monograph available for loan
    Pages: 151 S.
    Series Statement: Trudy sovetskoj antarktičeskoj ėkspedicii 74
    Language: Russian
    Note: Contents: Preface. - PART 1. GENERAL DESCRIPTION. - Chapter 1. Organization and implimentation of observations. - Chapter 2. Engineering activity on the SAE. - Appendix. - PART 2. SCIENTIFIC RESULTS. - On the initial data set for the long-range H500 hydrodynamic forecast for the Southern Hemisphere / M. P. Yevseyev. - To the forecast of weather elements in Antarctica / R. G. Panchugin. - Method of spectral zoning on the 4-dimensional analysis of upper-air data on the Southern Hemisphere / S. A. Petrusenko. - On the structure of air mass transport on the Southern Hemisphere atmosphere / E. P. Lysakov. - Aerial-synoptic analysis of the conditions leading to strong katabatic winds, observed on Molodezhnaya station on 1976 / S. T. Sokolov, N. N. Shirokov. - Some results of the study of the atmospheric nourishment of Antarctic Sea ice sheets / A. I. Voskresensky , N. N. Bryazgin. - The assessment of the advective and dynamic processes on the formation of the thermal regime of Antarctic atmosphere / E. P. Lysakov. - The study of physical / acoustical and rheological properties of the ice sheet on the vicinity of the Novolazarevskaya Station / V. A. Nikitin, V. K. Stepanov. - On the temperature field of the Novolazarevskaya Ice Shelf / L. I. Yeskin. - The primary production on the lakes of Schirmacher Oasis / E. B. Kaup. - On the computer processing of the Antarctic geomagnetic data / A. F. Maloletkin. - Hydrometeorological and sea ice conditions at the Bellingshausen Station, 1975/76 / A. A. Lebedev. - Biochemical changes on the blood serum under cold impact / P. Ye. Vloshchinsky, Yu. A. Sidorov. - The study of the elasticity of the vegetative system on the wintering-over personnel in Antarctica / Yu. A. Sidorov. , In kyrill. Schr. - Engl. Inhaltsverzeichnis S. 5-6
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  • 55
    Series available for loan
    Series available for loan
    Hanover, NH : US Army Materiel Command, Cold Regions Research & Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-240
    In: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command, 240
    Description / Table of Contents: A 4-summer hydrologic record from a 1.6 km^2 drainage basin at Barrow, Alaska is analyzed. The watershed, a drained lake basin, is underlain by continuous permafrost within 0.3m of the tundra surface and is covered by ice-wedge polygons and numerous small shallow ponds. Considerable variations from the 20-yr means of summer climate (thaw period 88 days, precipitation 67 mm) are represented in the data: 1963 - cold, extremely wet; 1964 - cold, extremely dry; 1965 - cool, dry; 1966 - cool, wet. Runoff varied greatly from storm to storm, occurring primarily through and over the tundra mat and through an intricate system of polygonal troughs and ponds. As a result of the subdued coastal topography, varying areas (0.3 km^2 to 1.6 km^2) contribute to runoff from different storms. Analyses of hydrographs revealed: 1) lag times generally from 3 to 10 hr; 2) recession constants of about 50 hr, but occasionally as much as 160 hr; and 3) runoff from individual storms between 1 and 70%. About 5% of the thaw season precipitation normally runs off. Comparison of total thaw season precipitation between the U.S. Weather Bureau and a shielded gage located on the watershed indicated no major differences. If "trace" precipitation is considered, only 90% of the actual precipitation may be recorded. Pan evaporation for an average thaw season is about 160 mm and evapotranspiration which is essentially in balance with precipitation is about 60 mm. Conductivity of runoff water varied from 250 [My]mhos during sustained discharge to more than 500 [My]mhos during low flows in dry years. Precipitation chemistry showed no correlation with storm direction. Assuming all winter precipitation runs off, and the data are spatially and temporally representative, about 50% of the measured annual precipitation in this region runs off into the Arctic Ocean.
    Type of Medium: Series available for loan
    Pages: IV, 18 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 240
    Language: English
    Note: CONTENTS: Preface. - Summary. - Introduction. - Regional setting. - Description of watershed. - Climatic record. - Methods. - Precipitation. - Water and air temperatures. - Discharge. - Evaporation and pond levels. - Water chemistry. - Soil thaw. - Results and discussion. - Precipitation. - Runoff. - Evaporation and transpiration. - Water chemistry. - Conclusions. - Literature cited.
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  • 56
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Materiel Command, Terrestrial Sciences Center, Cold Regions Research & Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-242
    In: Research report, 242
    Description / Table of Contents: The attenuation of visible light by falling snow was studied by making simultaneous attenuation measurements and snow concentration measurements. The attenuation coefficient was calculated from photometric measurements and from visual observations. Snow concentration in the air was evaluated by two methods: from Formvar replicas collected during the snowfall, and by mass accumulation of snow in collecting pans. The snowflakes were arbitrarily classified by crystal types according to their estimated fall velocity. It was found that the correlation between extinction coefficient (attenuation) and snow concentration was generally much higher by types than when all snowflakes were considered together regardless of crystal components and degree of riming. Two types, apparently improperly classified, displayed lower correlations than the overall group. When no fog is present during the snowfall, the experimental results coincide well with attenuation theory if a reasonable correction is applied to the values obtained in the measurement of snowflake diameters. Measurements of mass flux indicate that for a given intensity the attenuation caused by snow is an order of magnitude greater than that caused by the same mass flux of rain.
    Type of Medium: Series available for loan
    Pages: iv, 27 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 242
    Language: English
    Note: CONTENTS: Preface. - Abstract. - Introduction. - Initial theoretical considerations. - Light attenuation by particles. - Basis of attenuation meter measurements. - Contrast reduction and visual range. - Transmissometer theory, Pritchard photometric method. - Terminal velocity of snowflakes. - Methods of measurement: Light attenuation. - Duntley (Scripps Institution) attenuation meter. - "Meteorological range" observations. - Pritchard photometric method. - Methods of measurement: Atmospheric concentration of snowflakes. - Replication method. - Mass accumulation method. - Analysis of snow samples. - Terminal velocity of snowflakes. - Flux density and atmospheric concentration. - Mass accumulation rate. - Concurrent attenuation due to fog. - Discussion of results. - Computational methods. - Correlations: Attenuation coefficient vs area concentration. - Correlations: Attenuation coefficient vs are a flux. - Correlations: Attenuation coefficient vs mass concentration and mass flux. - Comparison of sampling methods for mass flux. - Attenuation of visible light by snow compared to rain. - Literature cited. - Appendix A.
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  • 57
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Materiel Command, Terrestrial Sciences Center, Cold Regions Research & Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-255
    In: Research report
    Description / Table of Contents: CONTENTS: Preface. - Abstract. - Introduction. - Previous work on unsteady rectilinear motion of a sphere. - Experiments with a circular path. - Conclusion. - Literature cited. - Appendix A: Comparisons of the measured and calculated forces.
    Description / Table of Contents: Forces on a sphere moving unsteadily along a circular path in a viscous fluid are measured, and it is found that within the experimental range the formula valid for rectilinear motion has to be modified to account for the curvature of the path.
    Type of Medium: Series available for loan
    Pages: iv, 10 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 255
    Language: English
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  • 58
    Call number: ZSP-697/C-26 ; MOP Per 434(26)
    In: Rezul'taty issledovanij po mezdunarodnym geofiziceskim proektam
    Type of Medium: Series available for loan
    Pages: 107 S. : graph. Darst., Kt.
    Series Statement: Rezul'taty issledovanij po mezdunarodnym geofiziceskim proektam : Meteorologiceskie issledovanija 26
    Note: Contents: The role of atmospheric circulation in the formation of air temperature anomalies on climatic scale in the Arctic / A. I. Voskresensky, A. A. Girs. - Some features of contemporary climatic variations in the Arctic / A. N. Lyubarsky, L. S. Petrov. - Structure of long-term variations of the snowless period in the Soviet Arctic / E. I. Aleksandrov, N. N. Briazgin, A. N. Lyubarsky. - Seasonal display of turbulent heat transfer in the Arctic Ocean / K. I. Chukanin. - Nature of causal relationship between the polar ice and the thermal conditions in the atmosphere / V. F. Zakharov. - Climate modelling and polar regions / A. I. Voskresensky, A. P. Nagurny. - Climatic change forecasting and polar regions / A. P. Nagurny. - Some features of the present evolution of the Arctic ice sheet / V. F. Zakharov, A. A. Kirillov. - Determination of the synchronous climate variation regions by the method of expansion in natural orthogonal functions (by example of the northern area of Ob' river basin) / E. I. Aleksandrov, N. N. Briazgin, A. N. Lyubarsky. - Climatic variations in the northern areas of Ob' and Yenisey river basins and in Karskoye more (Kara Sea) during the last decades / L. S. Petrov, V. V. Subbotin. , In kyrill. Schr.
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  • 59
    Call number: AWI P6-12-0011
    Type of Medium: Monograph available for loan
    Pages: 104 S.
    Edition: 2. Aufl.
    ISBN: 3881350829
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  • 60
    Call number: ZSP-403-57
    In: Jare Data Reports
    Type of Medium: Series available for loan
    Pages: 92 S.
    Series Statement: Jare Data Reports 57 : Meteorology 7
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  • 61
    Call number: ZSP-403-58
    In: Jare Data Reports
    Type of Medium: Series available for loan
    Pages: 28 S. : zahlr. Ill.
    Series Statement: Jare Data Reports 58 : Ionosphere 23
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  • 62
    Call number: ZSP-403-61
    In: Jare Data Reports
    Type of Medium: Series available for loan
    Pages: 350 S.
    Series Statement: Jare Data Reports 61 : Meteorology 8
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  • 63
    Call number: ZSP-697/B
    Former Title: Vorg. ---〉 [Rezul'taty issledovanij po mezdunarodnym geofiziceskim proektam / 9 / Gljaciologija i sejsmologija]
    Subsequent Title: Forts. ---〉 [Rezul'taty issledovanij po mezdunarodnym geofiziceskim proektam / Gljaciologiceskie issledovanija]
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  • 64
    Call number: ZSP-403-93
    In: Jare Data Reports
    Type of Medium: Series available for loan
    Pages: 206 S. : zahlr. graph. Darst.
    Series Statement: Jare Data Reports 93 : Upper atmosphere physics 1
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  • 65
    Call number: ZSP-403-88
    In: Jare Data Reports
    Type of Medium: Series available for loan
    Pages: 28 S. : graph. Darst.
    Series Statement: Jare Data Reports 88 : Ionosphere 30
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  • 66
    Call number: ZSP-403-87
    In: Jare Data Reports
    Type of Medium: Series available for loan
    Pages: 86 S. : graph. Darst.
    Series Statement: Jare Data Reports 87 : Ionosphere 29
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  • 67
    Call number: ZSP-403-80
    In: Jare Data Reports
    Type of Medium: Series available for loan
    Pages: 94 S. : graph. Darst.
    Series Statement: Jare Data Reports 80 : Ionosphere 27
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  • 68
    Call number: ZSP-403-81
    In: Jare Data Reports
    Type of Medium: Series available for loan
    Pages: 28 S. : graph. Darst.
    Series Statement: Jare Data Reports 81 : Ionosphere 28
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  • 69
    Call number: ZSP-403-82
    In: Jare Data Reports
    Type of Medium: Series available for loan
    Pages: 81 S.
    Series Statement: Jare Data Reports 82 : Glaciology 9
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  • 70
    Monograph available for loan
    Monograph available for loan
    Jena : Zeiss-Aerotopograph
    Associated volumes
    Call number: AWI E3-14-0024
    In: Deutsche antarktische Expedition 1938/39 mit dem Flugzeugstützpunkt der Deutschen Lufthansa A. G. M. S. "Schwabenland", Kapitän A. Kottas, ausgeführt unter der Leitung von Kapitän A. Ritscher
    Type of Medium: Monograph available for loan
    Pages: Seite 157-230 , Illustrationen , 3 Kartenbeilagen, 2 Stereobrillen, 1 Beilage ([26] S.)
    Series Statement: Deutsche Antarktische Expedition 1938/39 Band 1: Wissenschaftliche und fliegerische Ergebnisse
    Language: German
    Note: In Fraktur
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  • 71
    Call number: AWI A4-85-0427
    Description / Table of Contents: Приводятся основные результаты докладов на совещании-семинаре "Изучение Арктики, Антарктики и Мирового океана - на службу людям", проводившемся в Москве, на ВДНХ 9 - 13 февраля 1981 г. = The main results of the reports at the workshop-seminar "The study of the Arctic, Antarctic and the World Ocean - for people", held in Moscow, at the Exhibition of Economic Achievements, February 9 - 13, 1981.
    Type of Medium: Monograph available for loan
    Pages: 182 S. : Ill., graph. Darst.
    Language: Russian
    Note: Soderžanie: Predislovie. - Osnovnye rezul'taty 25-letnego issledovanija Antarktiki / N. A. Kornilov. - Poljarnaja klimatologija na službe narodnogo chozjajstva / A. I. Voskresenskij, G. U. Karimova, L. S. Petrov. - Sostojanie i perspektivy okeanologičeskogo obespečenija narodnogo chozjajstva v Arktike / N. V. Mustafin, E. N. Dvorkin. - Sostojanie i perspektivy gidrochimičeskich issledovanij dlja obsluživanija naučnych i chozjajstvennych učreždenij Arktiki / V. P. Rusanov. - Obespečenie ledovoj informaciej ledokol'no-transportnych sudov v Arktike / V. E. Borodačev, A. V. Bušuev, A. A. Kirillov. - Izučenie prirodnych uslovij dlja obespečenija tranzitnogo plavanija po Severnomu Morskomu Puti / A. Ja. Buzuev, V. B. Fedjakov. - Ispol'zovanie novych metodov v monitoringe termičeskogo režima Arktiki / I. B. Eserkepova, K. M. Lugina, N. A. Speranskaja, R. L. Kagan, I. P. Smirnova, V. V. Subbotin. - Izučenie vysokich sloev atmosfery v Arktike, Antarktike, i nad Mirovym okeanom s pomošč'ju meteoraket / G. A. Kokin, K. E. Speranskij, S. S. Gajgerov. - Optičeskie svojstva atmosfery nad Atlantičeskim okeanom / E. E. Artemkin, S. I. Avdjušin, A. E. Mikirov. - Voprosy soveršenstvovanija sinoptičeskogo obespečenija sudochodstva i rybopromyslovych rabot v Južnom okeane / L. Ju. Ryžakov. - Radiolokacionnye issledovanija oblakov v različnych rajonach Mirovogo okeana / A. I. Korotov, A. E. Mjagkov, A. B. Ščupjackij. - Osnovnye itogi i perspektivy naučnych issledovanij Severozemel'skogo gljaciologičeskogo stacionara AANII "Kupol Vavilova" / L. S. Govorucha. - Nekotorye rezul'taty issledovanij po programme Meždunarodnogo antarktičeskogo gljaciologičeskogo proekta (MAGP) / V. G. Aver'janov. - Prilivnye javlenija vo l'dach Severnogo Ledovitogo okeana (po kosmičeskim dannym) / V. V. Bogorodskij, M. G. Nazirov. - Nekotorye čerty prostranstvennoj struktury ledjanogo pokrova arktičeskich morej v svjazi s turbulentnym treniem i geostrofičeskim zachvatom prilivnoj volny / M. G. Nazirov, V. G. Trofimova. - Primenenie model'nych naturnych ėksperimentov pri izučenii vzaimodejstvija nefteproduktov s okeanom i atmosferoj / V. V. Izmajlov, V. S. Račkov. - Neftjanye uglevodorody v vodach mirovogo okeana i metody bor'by s nimi / M. P. Nestepova, I. A. Nemirovskaja, O. S. Močalova. - Osnovnye rezul'taty issledovanij vozmožnych izmenenij gidrometeorologičeskich uslovij severnych morej pod vlijaniem vodochozjajstvennych meroprijatij / V. A. Potanin, A. A. Dement'ev. - Issledovanie struktury gidrofizičeskich polej v central'noj časti Arktičeskogo bassejna / L. I. Zubkov, A. V. Gusev, P. V. Bogorodskij. - Ispol'zovanie infrakrasnych (IK) aėrokosmičeskich nabljudenij Arktičeskich morej v navigacii i pri rešenii drugich narodnochozjajstvennych zadač / A. I. Paramonov, V. A. Čebotareva. - Set' avtomatičeskich magnitografov po proektu "Geografičeskij poligon v Antarktide" dlja izučenija okolozemnogo kosmičeskogo prostranstva / A. N. Zajcev, G. A. Timofeev, V. O. Papitašvili. - Prognozirovanie chodkosti sudov vo l'dach / V. I. Kašteljan, D. D. Maksutov, O. V. Faddeev. , In kyrill. Schr.
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  • 72
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Materiel Command, Terrestrial Sciences Center, Cold Regions Research & Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-260
    In: Research report
    Description / Table of Contents: CONTENTS: Preface. - Abstract. - Introduction and statermnt of problem. - Solution of problem shown in Figure 3. - Solution of problem shown in Figure 4. - The negligibility of the effects of buoyancy and incompressibility of the sealed liquid. - Literature cited.
    Description / Table of Contents: After a brief description of the circumstances which led to the investigation of the title problem and discussion of some related previous investigations, exact solutions are derived for a circular plate which seals an incompressible liquid, is clamped along the boundary and is subjected at an arbitrary point to a lateral concentrated force P. For the case when the plate is covered by a thin liquid layer the solution is obtained in closed form. When this liquid layer is absent, the solution is obtained as an infinite series. The paper concludes with a study of the range of the parameter ([Lambda] a) for which the effort of buoyancy is negligible upon the deflections and stresses in the plate.
    Type of Medium: Series available for loan
    Pages: iv, 11 Seiten , Illustartionen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 260
    Language: English
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  • 73
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Materiel Command Cold Regions Research & Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-251
    In: Research report
    Description / Table of Contents: CONTENTS: Preface. - Abstract. - Introduction. - Theory. - Application to ice sheets and ice shelves. - Summary. - Literature cited.
    Description / Table of Contents: An analysis is made of the rate of bubble coalescence in a deforming ice mass. A total strain of at least 8 is required before appreciable coalescence occurs, The analysis has.been applied to deforming ice shelves and ice sheets. No appreciable coalescence is expected in ice shelves but coalescence should occur in ice sheets (or glaciers) if the shear strain rate at the bottom surface is of the order of 0.075/yr or larger. Measurements of bubble concentration are capable of setting limits on paleo-strain rates of the present ice sheets. Bubble migration down temperature gradients presents complications to the study of bubble coalescence.
    Type of Medium: Series available for loan
    Pages: iv, 5 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 251
    Language: English
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  • 74
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Materiel Command, Terrestrial Sciences Center, Cold Regions Research & Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-249
    In: Research report
    Description / Table of Contents: CONTENTS: Preface. - Abstract. - Introduction. - Analytical procedures. - Results and discussion. - Bubbles in ice. - Conclusions. - Literature cited.
    Description / Table of Contents: Application of the gas law to fourth-place density measurements of ice samples from two deep drill holes at Byrd Station and Little America V, Antarctica, shows that virtually all density increase beyond the pore close-off density (0.830 g/cm^3) can be attributed to compression of the entrapped bubbles of air. Data from Byrd Station also indicate that the lag between overburden pressure and bubble pressure, initially 4-5 kg/cm^2 at pore close-off, diminishes to less than 1.0 kg/cm^2 at about 200-m depth. By substituting the overburden pressure for the bubble pressure in the pressure-density relationship based on the gas law, ice densities below 200 m can be calculated more accurately than they can be measured per se on cores because of the relaxation that occurs in samples recovered from high confining pressures. This relaxation, resulting in a progressive increase in the bulk volume of the ice with time, is generally attributed to decompression of the entrapped air bubbles following removal of the ice from high confining pressures. However, calculations of the stress in ice due to bubble pressure, together with measurements of bubble sizes in cores from various depths at Byrd Station, both tend to indicate that there has'been negligible decompression of the inclosed bubbles. It is suggested that most of this relaxation may be due to the formation of microcracks in the ice. Anomalous bubble pressure-density relations at Little America V tend to confirm abundant stratigraphic evidence of the existence of considerable deformation in the upper part of the Ross Ice Shelf. Studies of crystal-bubble relations at Byrd Station revealed that the concentration of bubbles in ice remains remarkably constant at approximately 220 bubbles per cm^3. Bubbles and crystals were found to be present in approximately equal numbers at pore close-off at 64-m depth, at which level the average bubble diameter was 0.95 mm, decreasing to 0.49 mm at 116 m and to 0.33 mm at 279 m. Despite a tenfold increase in the size of crystals between 64 and 279 m, the bubbles showed no tendency to migrate to grain boundaries during recrystallization of the ice. The observation that most of the bubbles had assumed substantially spherical shapes by 120-m depth points to essentially hydrostatic conditions in the upper layers of the ice sheet at Byrd Station.
    Type of Medium: Series available for loan
    Pages: iv, 16 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 249
    Language: English
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  • 75
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Materiel Command, Terrestrial Sciences Center, Cold Regions Research & Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-248
    In: Research report
    Description / Table of Contents: CONTENTS: Preface. - Abstract. - Introduction. - Analytical procedures. - Results and discussion. - Literature cited.
    Description / Table of Contents: Conductivity measurements have been made on snow and ice samples from pits and deep drillholes at a number of localities in Antarctica and Greenland. Conductivities of the order 1-2 [My]mho/cm only were recorded at the inland sites. Data from deep cores representing more than 1900 years of continuous snow accumulation at Byrd Station, Antarctica, and more than 400 years deposition at Inge Lehmann, Greenland, showed no significant variations of conductivity with time. Measurements of freshly precipitated snow from a single coastal location in McMurdo Sound, Antarctica, also yielded relatively low conductivities of the order 3-4 [My]mho/cm. The substantial increase observed in the conductivity of core samples from near the surface of the Ross Ice Shelf at Little America V can be attributed most probably to windborne salts of marine origin that had accumulated on the surface after the snow was deposited. A peak conductivity of 49 [My]mho/cm was recorded in snow estimated to have been deposited within 20 km of the seaward edge of the Ross Ice Shelf and the maritime effect could still be detected in samples deposited more than 40 km from the ice front. For samples deposited at distances of greater than 200 km from the edge of the Ross Ice Shelf conductivities never exceeded 2 [My]mho/cm. The very low conductivities observed in ice cores from near the bottom of the Ross Ice Shelf confirm earlier conclusions based on detailed petrographic studies oi the cores that the 258-m-thick ice shelf at Little America V is composed entirely of glacial ice.
    Type of Medium: Series available for loan
    Pages: iv, 8 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 248
    Language: English
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  • 76
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Materiel Command, Terrestrial Sciences Center, Cold Regions Research & Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-256
    In: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command, 256
    Description / Table of Contents: The flow of a compressible fluid through a deep layer of a porous medium with non-uniform permeability was analyzed. The volumetric behavior of the fluid was described first by the perfect gas law, then by the van der Waal's equation of state. Darcy's law was assumed to be valid. For illustration, the model of air flowing through a deep bed of naturally compacted snow was used to carry out numerical computation. The permeability of snow was considered as a function of depth. The nonlinear partial differential equation obtained by combining the continuity equation with Darcy's law was solved by finite difference technique. A time dependent exponential decay boundary condition was used which included the step-rise constant boundary condition as a limiting case. Pressure distributions in the porous medium calculated from the assumption of ideal gas and van der Waal's gas were compared. The data were presented in dimensionless variables.
    Type of Medium: Series available for loan
    Pages: iv, 13 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 256
    Language: English
    Note: CONTENTS: Preface. - Abstract. - Introduction. - Theory. - Computation and results. - Conclusions. - Literature cited.
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  • 77
    Series available for loan
    Series available for loan
    Moskva : Mežduvedomstvennyj Geofizičeskij Komitet
    Associated volumes
    Call number: ZSP-697/C-27 ; MOP Per 434(27)
    In: Rezul'taty issledovanij po mezdunarodnym geofiziceskim proektam, 27
    Description / Table of Contents: Contents: Foreword. - Seasonal variations of the atmospheric electric field potential gradient and their relationships to the atmospheric circulation forms / V. A. Kamyshanova. - Measurements of electric field over the Atlantic and Indian Oceans / V. P. Kolokov, V. A. Kurilov, Yu. V. Shamansky. - The electrical conductivity air over the Indian Ocean / V. P. Kolokov, V. A. Kurilov, Yu. V. Shamansky. - The upper atmosphere potential / A. V. Latyshev, E. V. Chubarina. - On the methods high-altitude atmospheric electricity measurements / A. V. Latyshev, E. V. Chubarina. - Some results of regular measurements of electrical conductivity of air / L. V. Oguryaeva, Ya. M. Shwarts. - On the analysis of the observation data concerning many-year behaviour of the atmospheric electricity parameters near the earth's surface / L. V. Oguryaeva, Ya. M. Shwarts. - On the recurrent processes in the atmospheric electric field / A. V. Tsvetkov. - The results of regular observations of electrical conductivity of air over Verkhnee Dubrovo / L. K. Cheremiskin. - On the variability of the atmospheric electricity parameters / Ya. M. Swartz, L. V. Oguraeva, A. H. Filippov. - The development of the methods for measuring the atmospheric electricity parameters / V. P. Gordyuk, L. G. Sokolenko
    Type of Medium: Series available for loan
    Pages: 85 S. : graph. Darst.
    Series Statement: Rezul'taty issledovanij po mezdunarodnym geofiziceskim proektam : Meteorologiceskie issledovanija 27
    Language: Russian
    Note: In kyrillischer Schrift , Zusammenfassungen in englischer Sprache
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  • 78
    Call number: AWI S5-12-0051
    Type of Medium: Monograph available for loan
    Pages: 373 Seiten , Illustrationen
    Language: Russian
    Note: In kyrillischer Schrift
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  • 79
    Call number: ZSP-403-62
    In: Jare Data Reports
    Type of Medium: Series available for loan
    Pages: 321 S.
    Series Statement: Jare Data Reports 62 : Meteorology 9
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  • 80
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    Series available for loan
    Tokyo : Inst.
    Associated volumes
    Call number: ZSP-403-66
    In: Jare Data Reports
    Type of Medium: Series available for loan
    Pages: 199 S. : graph. Darst.
    Series Statement: JARE data reports 66 : Marine biology 2
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  • 81
    Call number: ZSP-403-64
    In: Jare Data Reports
    Type of Medium: Series available for loan
    Pages: 9 S. : Ill.
    Series Statement: Jare Data Reports 64 : Aurora 9
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  • 82
    Call number: ZSP-403-65
    In: Jare Data Reports
    Type of Medium: Series available for loan
    Pages: 93 S.
    Series Statement: Jare Data Reports 65 : Meteorology 10
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  • 83
    Call number: AWI P7-12-0065 ; MOP 36330
    In: Die Wissenschaft, Band 128
    Description / Table of Contents: Inhalt: 1. Namen und Grenzen (Begriffsbestimmungen). - 2. Die Pole. - 3. Schwerebestimmungen. - 4. Flächengrößen der Polargebiete. - 5. Küstenlängen. - 6. Höhen- und Tiefenverhältnisse. - 7. Höhe des Felsuntergrundes in Grönland und der Antarktis. - 8. Geologischer Bau. - 9. Bodenbildung, Bodenfrost und "Oasen". - 10. Erdmagnetismus und Polarlicht. - 11. Die Polarmeere. - 12. Gewässer des Festlandes. - 13. Vergletscherung und Glaziologie. - 14. Klima. - 15. Die Pflanzenwelt. - 16. Die niedere Tierwelt. - 17. Die Vogelwelt. - 18. Die Robben. - 19. Die Wale. - 20. Säugetiere des Landes. - 21. - Die Biotope der Polargebiete. - 22. Die politischen Verhältnisse in den Polargebieten. - 23. Bevölkerungsverteilung und -entwicklung. - 24. Die Polarvölker. - 25. Gesundheitsverhältnisse und Akklimatisation. - 26. Erwerbsverhältnisse, Tierzucht. - 27. Erwerbsverhältnisse, Jagd, Fischfang. - 28. Erwerbsverhältnisse, Robbenfang. - 29. Erwerbsverhältnisse, der Walfang. - 30. Erwerbsverhältnisse, Bergbau. - 31. Der Verkehr. - 32. Verwaltung und kulturelle Verhältnisse. - 33. Erforschungsgang und Organisation der Polarforschung. - Schrifttum. - Ergänzungstabellen. - Sachverzeichnis. - Kartenskizzen.
    Type of Medium: Monograph available for loan
    Pages: XV, 471 Seiten , Illustrationen , 1 Karte
    Series Statement: Die Wissenschaft 128
    Language: German
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  • 84
    Call number: ZSP-403-68
    In: Jare Data Reports
    Type of Medium: Series available for loan
    Pages: 28 S. : zahlr. Ill. und graph. Darst.
    Series Statement: Jare Data Reports 68 : Ionosphere 24
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  • 85
    Call number: ZSP-403-69
    In: Jare Data Reports
    Type of Medium: Series available for loan
    Pages: 101 S. : graph. Darst.
    Series Statement: Jare Data Reports 69 : Ionosphere 25
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  • 86
    Call number: ZSP-403-70
    In: Jare Data Reports
    Type of Medium: Series available for loan
    Pages: 97 S. : zahlr. graph. Darst.
    Series Statement: Jare Data Reports 70 : Ionosphere 26
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  • 87
    Call number: ZSP-403-71
    In: Jare Data Reports
    Type of Medium: Series available for loan
    Pages: 45 S. : Ill., graph. Darst.
    Series Statement: Jare Data Reports 71 : Glaciology 8
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  • 88
    Call number: ZSP-403-72
    In: Jare Data Reports
    Type of Medium: Series available for loan
    Pages: 74 S. : zahlr. graph. Darst.
    Series Statement: Jare Data Reports 72 Seismology 15
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  • 89
    Call number: ZSP-403-73
    In: Jare Data Reports
    Type of Medium: Series available for loan
    Pages: 195 S.
    Series Statement: Jare Data Reports 73 : Meteorology 11
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  • 90
    Call number: ZSP-403-16
    In: Jare Data Reports
    Type of Medium: Series available for loan
    Pages: 99 S. : Ill., graph. Darst.
    Series Statement: Jare Data Reports 83 : Seismology 16
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  • 91
    Series available for loan
    Series available for loan
    Tokyo : Inst.
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    Call number: ZSP-403-84 ; ZSP-403-84(2. Ex.)
    In: Jare Data Reports
    Type of Medium: Series available for loan
    Pages: 13 S. : Ill., graph. Darst.
    Series Statement: Jare Data Reports 84 : Aurora 11
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  • 92
    Call number: ZSP-403-85
    In: Jare Data Reports
    Type of Medium: Series available for loan
    Pages: 182 S.
    Series Statement: Jare Data Reports 85 : Meteorology 14
    Location: AWI Reading room
    Branch Library: AWI Library
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  • 93
    Monograph available for loan
    Monograph available for loan
    Leningrad : Gidrometeoizdat
    Call number: AWI G7-85-1035
    Type of Medium: Monograph available for loan
    Pages: 65 S.
    Language: Russian
    Location: AWI Reading room
    Branch Library: AWI Library
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  • 94
    Monograph available for loan
    Monograph available for loan
    Kiev : Izd. Kievskogo Univ.
    Call number: AWI A9-90-0155 ; MOP 33126
    Type of Medium: Monograph available for loan
    Pages: 201 S.
    Series Statement: Kievskaja Knižnaja Tipografija 5
    Language: Russian
    Note: In kyrill. Schr.
    Location: AWI Reading room
    Location: MOP - must be ordered
    Branch Library: AWI Library
    Branch Library: GFZ Library
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  • 95
    Call number: AWI P5-14-0028
    In: Verständliche Wissenschaft ; 48, 48
    Type of Medium: Monograph available for loan
    Pages: VI, 179 S. , zahlr. Ill., graph. Darst., Kt.
    Series Statement: Verständliche Wissenschaft 48
    Note: Contents: 1. Einleitung. - 2. Gliederung, Grenzen, Ausmaße und Aufbau der Arktis. - 3. Gewässer der Arktis. - 4. Klima der Arktis. - 5. Die Lebewelt der Arktis. - 5A. Die Biosphäre. - 5B. Die Pflanzenwelt. - 5C. Die Tierwelt. - 5D. Der Mensch. - 6. Gang der Arktisforschung. - 6A. Atlantisch-europäisches Gebiet. - 6B. Polarsibirien. - 6C. Polaramerika. - 6D. Innerarktis. - 7. Die Arktis als Verkehrsraum. - 7A. Nordsibirischer Seeweg (Nordostpassage). - 7B. Nordwestpassage. - 7C. Luftverkehr. - 7D. Unterseeverkehr. - 8. Ziele und Methoden der Polarforschung. - 9. Schlußwort. - Namen und Sachverzeichnis. - Anhang: Tafel 1. Karte des Golfstrom- und Polarstromsystems. - Tafel 2. Farbige Karte der Arktis und angrenzender Länder.
    Location: AWI Reading room
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  • 96
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Materiel Command, Terrestrial Sciences Center, Cold Regions Research & Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-253
    In: Research report
    Description / Table of Contents: CONTENTS: Preface. - Abstract. - Introduction. - Theoretical considerations. - Method of canopy evaluation. - Application to forest problems. - Forest blowdown. - Radioactivity gradient. - Phenology. - Forest types and structure. - Distribution of leaves and canopy gaps. - Light quality. - Discussion and summary. - Literature cited.
    Description / Table of Contents: A technique for evaluating forest canopies was developed based on the use of a divergent lens system to obtain hemispherical photographs of tree crowns. The photography was processed from 35 mm film and enlarged as a silhouette, and the light transmission was measured with a specially fabricated macrodensitometer. It is concluded that the amount of forest canopy can be expressed as canopy closure index (CCI) at a precision of approximately 5%. It is shown by application to a variety of problems in diverse geographical areas that this technique can be used for measuring both temporal and spatial changes in the canopy, for estimating the shade light climate, and for specifying the probability of target detection through a canopy. Data are presented to analyze changes caused by explosions, radioactivity, growing season, and vegetation types. The geometry of gaps in tree crowns is discussed and the nature of shade light quality under forests is illustrated.
    Type of Medium: Series available for loan
    Pages: v, 20 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 253
    Language: English
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    Branch Library: AWI Library
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  • 97
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Materiel Command, Terrestrial Sciences Center, Cold Regions Research & Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-252
    In: Research report
    Description / Table of Contents: CONTENTS: Preface. - Abstract. - Introduction. - Theory. - Discussion. - Conclusion. - Literature cited.
    Description / Table of Contents: A diffusion equation is obtained that describes the mechanical dispersion of a dilute mixture of solid particles within an ice matrix that is undergoing deformation. It is shown that within the limits of time intervals and strain rates appropriate to the movement of glaciers and ice sheets the dispersal distance usually is no larger than a distance about one order of magnitude greater than the size of the particles themselves.
    Type of Medium: Series available for loan
    Pages: iv, 6 Seiten , Illistrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 252
    Language: English
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  • 98
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Materiel Command, Cold Regions Research & Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-257
    In: Research report
    Description / Table of Contents: CONTENTS: PREFACE. - NOMENCLATURE. - SUMMARY. - INTRODUCTION. - TECHNICAL BACKGROUND. - Rankine-Hugoniot Shock Equations. - The Rayleigh Line. - Release Cross Curves. - Impedance Match Technique for Measuring Hugoniots and Release Isentropes. - EXPERIMENTS. - Sample Materials. - Ottawa Sand. - West Lebanon Glacial Till. - Ice . - Sample Preparation. - Experimental Procedures. - EXPERIMENTAL DATA AND RESULTS. - Ottawa Sand. - West Lebanon Glacial Till. - Ice. - Release Cross Curves. - Dry Ottawa Sand. - Saturated Ottawa Sand. - Ice. - SUMMARY AND RECOMMENDATIONS FOR FUTURE WORK. - REFERENCES.
    Description / Table of Contents: To compute shock wave propagation in frozen soil-water mixtures it is necessary to know a constitutive relation or an equation of state of the medium under consideration. Shock wave techniques provide a powerful tool for the investigation of equations of state at very high stress levels. The stress-volume behavior of frozen soil-water mixtures in the range from 60 to 500 kbar was investigated. Hugoniot data were obtained for Ottawa banding sand (pure quartz sand) and West Lebanon (New Hampshire) glacial till of varying degrees of saturation and for polycrystalline and monocrystalline ice (c-axis oriented in the direction of shock propagation). Release cross curve data were obtained for dry and saturated Ottawa banding sand and for polycrystalline ice. All materials were at an initial temperature of -10°C. In all experiments plane one-dimensional shock waves were used. The Hugoniots and release curves for the soil materials show evidence of a quartz-stishovite phase transition at about 300 kbar. The Hugoniots of single and polycrystalline ice do not differ significantly over the stress range studied - 30 kbar to 300 kbar.
    Type of Medium: Series available for loan
    Pages: vii, 50 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 257
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  • 99
    Call number: ZSP-204-147
    In: CRREL Technical Report
    Type of Medium: Series available for loan
    Pages: iv, 18 S. : graph. Darst.
    Series Statement: CRREL Technical Report 147
    Location: AWI Reading room
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  • 100
    Call number: ZSP-204-159
    In: CRREL Technical Report
    Type of Medium: Series available for loan
    Pages: iv, 32 S. : Ill., graph. Darst., Kt.
    Series Statement: CRREL Technical Report 159
    Location: AWI Reading room
    Branch Library: AWI Library
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