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  • 1980-1984  (647)
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  • AWI Library  (804)
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  • 1
    Series available for loan
    Series available for loan
    Hanover, NH
    Associated volumes
    Call number: ZSP-204-65
    In: CRREL Technical Report
    Type of Medium: Series available for loan
    Pages: iv, 8 S. : graph. Darst.
    Series Statement: CRREL Technical Report 65
    Location: AWI Reading room
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  • 2
    Series available for loan
    Series available for loan
    Wilmette, Ill. : Snow, Ice and Permafrost Research Establishment
    Associated volumes
    Call number: ZSP-201-30
    In: SIPRE report, 30
    Description / Table of Contents: Mining Research Corporation, Inc., under contract with Snow Ice, and Permafrost Research Establishment, Corps of Engineers, U.S. Army, conducted explosion tests in frozen Keweenaw silt, to determine; (1) the most efficient type of explosive for blasts in frozen ground, (2) the fundamental relation between weight of explosive and depth of charge, (3) the proper position of the charge relative to the frozen-ground interface, (4) the feasibility of fracturing the frozen layer by placing a charge in the underlying unfrozen material, and (5) the effect of the diameter of the borehole and of the shape of the charge upon the resultsof blasting. Information obtained from the tests applies to the specific problem of excavating in frozen ground and to fundamental explosives research. Conclusions and recommendations based on this information are presented here concerning the feasibility of using explosives for fox-holes in frozen ground; methods of placing the charge; mechanics of crater formation; the crater equation; future instrumentation; classification of explosives; and correlation of blast data.
    Type of Medium: Series available for loan
    Pages: 97 Seiten , Illustrationen
    Series Statement: SIPRE report 30
    Language: English
    Note: CONTENTS Preface Abstract Chapter I. Introduction to problem 1. Previous attempts at blasting frozen ground 2. Necessity for fundamental approach 3. Terminology 4. Description, objectives, and scope of the Keweenaw Tests 5. Selection of explosives 6. Classification and properties of commercial explosives 7. Characteristics of explosives in the Keweenaw Tests 8. Comparison of Atlas, Hercules, and Du Pont nitroglycerine-base explosives Chapter II. Test program Section I. Field tests 1. General 2. Test site 3. Field test procedure a. Site preparation b. Instrumentation c. Snow removal d. Determining depth of frozen ground e. Soil sampling and coring f. Layout of the test site g. Spacing of blast holes h. Blast-hole drilling i. Blasting procedure j. Field analysis and crater surveys k. Data-sheet computations l. Photography Section II. Laboratory tests 1. Soil handling and storage 2. Soil classification tests a. Specimen preparation b. Test procedure c. Test results 3. Tests to determine stress-strain relationship a. General b. Specimen preparation for unconfined compression tests c. Test procedure d. Results e. Observations Chapter III. Analysis of blast tests Section I. Mechanics of crater formation in frozen Keweenaw silt 1. Introduction 2. Shock phenomena 3. Expansion of the gas bubble 4. Rupture of surface and conversion of pressure head to velocity head Section II. Blast Test A - Relationships of explosive, radius of crater, volume of crater, and depth of crater 1. Introduction 2. Description 3. Results and analysis 4. Summary of observations Section Ill. Blast Test B - Energy utilization in blasting 1. Introduction 2. Description 3. Results and analysis 4. Summary of observation Section IV. Blast Test C - The frozen-ground interface 1. Introduction 2. Relation of frozen-ground interface to scaling laws 3. Relation between the ratio of chamber volume to crater volume and the volume-utilization factor 4. Increase in volum.e-utilization factor for charges placed below the frozen layer 5. Position of the gas bubble relative to the frozen-ground interface 6. Igloo-type foxhole construction Section V. Blast Test D - Foxhole construction 1. Introduction 2. Application of shaped charges to foxhole construction 3. Application of hand-auget drilling to foxhole construction 4. Conclusions Section VI. Blast Test E - Temperature effect 1. Introduction 2. Description 3. Results and analysis 4. Summary of observations Section VII. Blast Test F - Effect of charge shape 1. Introduction 2. Description 3. Conclusions Chapter IV. Summary of objectives; conclusions and recommendations Section I. Summary of objectives 1. Introduction 2. Objective 1: Most efficientt type of explosive for blasts in frozen ground 3. Objective 2: Fundamental relation between weight of explosive and depth of charge 4. Objective 3: Proper position of charge relative to the frozen-ground interface 5. Objective 4: Feasibility of fracturing the frozen layer by placing a charge in the underlying unfrozen material 6. Objective 5: Effect of diameter of the borehole and shape of charge on results of blasting Section II. Conclusions and recommendations 1. Feasibility of using explosives for constructing foxholes in frozen ground 2. Methods of placing the charge 3. Mechanics of crater formation 4. The crater equation 5. Future instrumentation 6. Classification of explosives 7. Correlation of blast data Appendix: Data sheets, Experiments 1-13
    Location: AWI Archive
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  • 3
    Series available for loan
    Series available for loan
    Leipzig : Acad. of Sciences of the GDR, Central Inst. for Isotope and Radiation Research
    Associated volumes
    Call number: MOP 46290 / Mitte ; ZSP-980-51 ; ZSP-980-51(2. Ex.)
    In: ZfI-Mitteilungen ; 51, Nr. 51
    Type of Medium: Series available for loan
    Pages: 140 S. , Ill., graph. Darst., Kt.
    ISSN: 0323-8776
    Series Statement: ZfI-Mitteilungen 51
    Note: Contents: Foreword. - Isotopes in Antarctic Research / K. Fröhlich, H. Schütze. - Deuterium variations in maritime atmospheric moisture / P. Kowski, G. Strauch, H. Schütze. - On the influence of degradation processes on the isotopic composition of Antarctic precipitations / R. Der. - Extractive method for obtaining gas inclusions from ice / G. Strauch, P. Kowski. - Global monitoring of atmospheric CO2: activities planned by the GDR in Antarctica / P. Harting, U. Wand. - Deuterium and 18O variations in lakes of the Schirmacher Oasis (East Antarctica) / W. Richter, G. Strauch. - Environmental studies in Antarctica on the basis of tritium and radiocarbon measurements / D. Herbert, K. Fröhlich. - Isotope variations of hydrogen, carbon and nitrogen in florae from the Schirmacher Oasis, East Antarctica / G. Strauch, D. Haendel, I. Maaß, K. Mühle, A. Runge. - The ecology and chemistry of some Antarctic lichens / W. Richter, S. Huneck. - Another seal find in the Schirmacher Oasis (Queen Maud Land, Antarctica) / A. Hiller, W. Richter, R. Trettin. - Survey on hitherto published numbers of ZfI-Mitteilungen.
    Location: MOP - must be ordered
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    Location: AWI Archive
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  • 4
    Call number: AWI A4-81-1093 ; MOP 45275 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 211 S. : graph. Darst.
    Language: Russian
    Note: In kyrill. Schr.
    Location: AWI Reading room
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  • 5
    Call number: SR 90.0018(139) ; ZSP-183-139
    In: Bulletin
    Type of Medium: Series available for loan
    Pages: 56 S. : Ill., Kt.
    Series Statement: Bulletin / Grønlands Geologiske Undersøgelse 139
    Location: Lower compact magazine
    Location: Lower compact magazine
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  • 6
    Series available for loan
    Series available for loan
    Oslo : Univ. Press [in Komm.]
    Associated volumes
    Call number: ZSP-597-110
    In: Skrifter
    Type of Medium: Series available for loan
    Pages: 34 S. : Ill. + 3 Kt.-Beil.
    Series Statement: Skrifter / Norsk Polarinstitutt 110
    Branch Library: AWI Library
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  • 7
    Call number: ZSP-599-15
    In: Rapportserie
    Type of Medium: Series available for loan
    Pages: 27 S. : Ill., graph. Darst., Kt.
    Edition: Torgny E. Vinje
    Series Statement: Rapportserie / Norsk Polarinstitutt 15
    Branch Library: AWI Library
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  • 8
    Series available for loan
    Series available for loan
    Associated volumes
    Call number: ZSP-595-1983
    In: Årbok
    Type of Medium: Series available for loan
    Pages: 49 S. : Ill., graph. Darst.
    ISBN: 8290307314
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  • 9
    Call number: ZSP-329-15
    In: Glaciological data
    Type of Medium: Series available for loan
    Pages: VII, 69 S. : graph. Darst.
    Series Statement: Glaciological data : GD 15
    Branch Library: AWI Library
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  • 10
    Call number: ZSP-329-16
    In: Glaciological data
    Type of Medium: Series available for loan
    Pages: VII, 300 S. : graph. Darst
    Series Statement: Glaciological data : GD 16
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  • 11
    Series available for loan
    Series available for loan
    Kingston : Antarctic Division, Dept. of Science and Technology
    Associated volumes
    Call number: ZSP-124-14
    In: ANARE research notes
    Description / Table of Contents: The variation of a Southern Hemisphere absolute vorticity area index about solar sector boundary crossings is examined by the superposed epoch method. It is concluded that the Southern Hemisphere results do not confirm the winter decrease in vorticity near sector crossings found by researchers using Northern Hemisphere data. There is, however, limited indication that the following southern hemisphere effects may exist: (a) A vorticity decrease in the summer months showing a shape similarity to the Northern Hemisphere winter response. (b) A winter peak in vorticity on the boundary crossing date for the Australian quadrant of the Southern Hemisphere.
    Type of Medium: Series available for loan
    Pages: iv, 49 S. : Ill.
    ISBN: 0642877335
    Series Statement: ANARE research notes 14
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  • 12
    Series available for loan
    Series available for loan
    Kingston : Antarctic Division, Dept. of Science and Technology
    Associated volumes
    Call number: ZSP-124-11
    In: ANARE research notes
    Description / Table of Contents: A guide to the Decapoda of the Southern Ocean is presented, with emphasis on those species which have been recorded south of the Antarctic Convergence. Despite being well represented in all other oceans the decapod fauna of Antarctic waters is depauperate, with only eleven species having been reported from south of the Antarctic Convervence (Petalidium foliaceum, Notocrangon antacticus, Pasiphaea longispina, Pasiphaea scotiae, Nematocarcinus longirostris, Nematocarcinus lanceopes, Hymenodora gracilis, Chorismus antarcticus, Lebbeus antarcticus, Acanthephyra pelagica and Paralomis spectabilis). Species found in the subarctic waters north of the Convergence are also included in the key as their ranges may overlap with those of the Antarctic species. A key is also provided to the larvae of decapod families which are known to have Antarctic representatives. Short descriptions, with figures and records of occurence, are presented for each of the eleven Antarctic species to enable the reader to confirm identifications from the keys. A glossary of technical terms has also been compiled.
    Type of Medium: Series available for loan
    Pages: iv, 47 S. : Ill.
    ISBN: 0642879699
    Series Statement: ANARE research notes 11
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  • 13
    Series available for loan
    Series available for loan
    Kingston : Antarctic Division, Dept. of Science and Technology
    Associated volumes
    Call number: ZSP-124-15
    In: ANARE research notes
    Description / Table of Contents: The history of the Antarctic Names and Polar Medals Committee is given. Place names principles and criteria are outlined and the procedure for proposing new names is described. The names list contains the decisions of the Committee approved by the Minister for Science and Technology until July 1983. Name and position only are listed.
    Type of Medium: Series available for loan
    Pages: iv, 50 S.
    ISBN: 0642877270
    Series Statement: ANARE research notes 15
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  • 14
    Series available for loan
    Series available for loan
    Kingston : Publ. Off. Antarctic Division
    Associated volumes
    Call number: ZSP-124-20
    In: ANARE research notes
    Description / Table of Contents: The bryoflora of the Vestfold Hills and Ingrid Christensen Coast includes six moss species and one hepatic. Moss species represented in the flora are Grimmia antarctici, Grimmia lawiana, Ceratodon purpureus, Sarconeurum glaciale, Bryum algens, Bryum argenteum. The one hepatic Cephaloziella exiliflora, from the Larsemann Hills, represents the most southerly record of an hepatic. A discussion of the Antarctic distribution and taxonomic problems associated with the recognition of individual species is included. All species are illustrated.
    Type of Medium: Series available for loan
    Pages: 30 S. : Ill.
    ISBN: 0642872171
    Series Statement: ANARE research notes 20
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  • 15
    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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  • 16
    Series available for loan
    Series available for loan
    Oslo : Univ. Press [in Komm.]
    Associated volumes
    Call number: ZSP-597-154/C
    In: Geological map of Svalbard 1:500 000
    Type of Medium: Series available for loan
    Pages: 1 Kt.
    Series Statement: Geological map of Svalbard 1:500 000 3G
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  • 17
    Series available for loan
    Series available for loan
    Kingston : Antarctic Division, Department of Science
    Associated volumes
    Call number: ZSP-124-19
    In: ANARE research notes
    Description / Table of Contents: Invariant geomagnetic co-ordinates were calculated for points on a 5° x 5° grid over the earth, at altitudes of 105 km and 250 km. The calculation was based on the International Geomagnetic Reference Field (IGRF) for 1975, updated to 1977.25 to correspond approximately to the middle of the International Magnetosphere Survey period. Global charts of the invariant co-ordinates at 105 km altitude are presented. The invariant co-ordinates were expanded into a set of spherical harmonic co-efficients and FORTRAN subroutines are described which allow the rapid re-calculation of the invariant co-ordinates form the co-efficients.
    Type of Medium: Series available for loan
    Pages: iv, 44 S. : Kt. + 3 Kt.-Beil.
    ISBN: 0642874824
    Series Statement: ANARE research notes 19
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  • 18
    Series available for loan
    Series available for loan
    Kingston : Antarctic Division, Dept. of Science and Technology
    Associated volumes
    Call number: ZSP-124-23
    In: ANARE research notes
    Description / Table of Contents: Body length , wet weight and maturity stage of krill (Euphausia superba) collected with RMT and bongo nets during the cruise of MS Nella Dan to Prydz Bay, Antarctica in January - February 1984 are reported. Non-krill zooplankton data from RMT samples (density and biomass), and euphausiid larvae (density) data from bongo samples are also presented.
    Type of Medium: Series available for loan
    Pages: 32 S. : Kt.
    ISBN: 0642073449
    Series Statement: ANARE research notes 23
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  • 19
    Series available for loan
    Series available for loan
    London : British Antarctic Survey
    Associated volumes
    Call number: ZSP-164-102
    In: Scientific reports
    Type of Medium: Series available for loan
    Pages: 50 S. : Ill., graph. Darst., Kt.
    ISBN: 085665082X
    Series Statement: Scientific reports / British Antarctic Survey 102
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  • 20
    Monograph available for loan
    Monograph available for loan
    Associated volumes
    Call number: AWI P2-88-0760 (4)
    In: Antarctica and international law
    Type of Medium: Monograph available for loan
    Pages: 194 S.
    ISBN: 0379203243
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  • 21
    Call number: AWI E2-99-0134 (1b)
    In: The Norwegian north polar expedition with the "MAUD" 1918 - 1925
    Type of Medium: Monograph available for loan
    Pages: 525 S. : Ill., graph. Darst.
    Series Statement: The Norwegian north polar expedition with the "MAUD" 1918 - 1925 : Scientific Results
    Language: English
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  • 22
    Monograph available for loan
    Monograph available for loan
    Bergen : Grieg
    Associated volumes
    Call number: AWI E2-99-0133 (1a)
    In: The Norwegian north polar expedition with the "MAUD" 1918 - 1925
    Type of Medium: Monograph available for loan
    Pages: 279 S. : Ill., graph. Darst., Kt.
    Series Statement: The Norwegian north polar expedition with the "MAUD" 1918 - 1925 : Scientific Results
    Language: English
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  • 23
    Call number: ZSP-553-5
    In: Meddelelser om Grønland
    Type of Medium: Monograph available for loan
    Pages: 19 S.
    ISBN: 8717028736
    ISSN: 0106-1046
    Series Statement: Meddelelser om Grønland : Geoscience 5
    Language: English
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  • 24
    Call number: ZSP-553-10
    In: Meddelelser om Grønland
    Type of Medium: Monograph available for loan
    Pages: 28 S., 11 Beil.
    ISBN: 8717051118
    ISSN: 0106-1046
    Series Statement: Meddelelser om Grønland : Geoscience 10
    Language: English
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  • 25
    Monograph available for loan
    Monograph available for loan
    København : Lunos
    Associated volumes
    Call number: ZSP-553-156,5
    In: Meddelelser om Grønland
    Type of Medium: Monograph available for loan
    Series Statement: Meddelelser om Grønland 156,5
    Language: English
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  • 26
    Call number: AWI P9-94-0237
    In: Skrifter om Svalbard og Ishavet
    Type of Medium: Monograph available for loan
    Pages: 195 S., VII Taf. : Ill., graph. Darst.
    Series Statement: Skrifter om Svalbard og Ishavet 57
    Language: English
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  • 27
    Call number: AWI P6-82-0001
    Type of Medium: Monograph available for loan
    Pages: 45 S.
    Language: German
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  • 28
    Call number: ZSP-553-159,4
    In: Meddelelser om Grønland
    Type of Medium: Monograph available for loan
    Pages: 17 S. : Ill.
    Series Statement: Meddelelser om Grønland 159,4
    Language: English
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  • 29
    Monograph available for loan
    Monograph available for loan
    Scientific Committee on Antarctic Research
    Call number: AWI P6-09-0028
    Type of Medium: Monograph available for loan
    Pages: 15 S. : graph. Darst.
    Edition: 2nd Ed.
    ISBN: 0642514755
    Language: English
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  • 30
    Monograph available for loan
    Monograph available for loan
    Copenhagen : Nyt Nordisk Forl.
    Associated volumes
    Call number: ZSP-553-9
    In: Meddelelser om Grønland
    Type of Medium: Monograph available for loan
    Pages: 36 S. : Ill.
    ISBN: 8717029635
    ISSN: 0106-1054
    Series Statement: Meddelelser om Grønland : Bioscience 9
    Language: English
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  • 31
    Call number: ZSP-558-1
    In: Middle atmosphere program
    Type of Medium: Series available for loan
    Pages: V, 104 S. : graph. Darst.
    Language: English
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  • 32
    Call number: ZSP-597-15
    In: Skrifter om Svalbard og Ishavet ; 15, No. 15
    Type of Medium: Series available for loan
    Pages: X, 152 S. : Ill, Kt. + 10 Beil.
    Series Statement: Skrifter om Svalbard og Ishavet 15
    Note: Contents: Preface. - Introductory. - Geography. - Topography. - Valleys and Rivers. - Lakes. - Coast. - Landslips. - Surface. - Soil. - Frozen Ground. - Stratigraphy. - Hecla Hoek. - Devonian. - Culm. - Middle Carboniferous. - Upper Carboniferous. - Triassic. - Structure. - Post-Triassic History. - Jurassic-Tertiary. - The Quaternary Period. - Coal Deposits. - Devonian. - The Misery Series. - The Tunheim Series. - Culm. - Sections of Boreholes. - Quality of Coals. - Coal Reserves. - Fireclay . - Minerals. - Mining. - Drilling. - History of Bear Island. - Probable Norse Discovery in the Middle Ages. - Dutch Discovery, and Dutch and English Hunting in the 16th and 17th Centuries. - Russian Hunting in the 18th Cent. - Norwegian Hunting in the 18th and 19th Centuries and Keilhau's Voyage in 1827. - Scientific Expeditions in the 19th and 20th Centuries. - Scientific Investigations, Exploitation of the Coal Deposits, and Hunting in the 20th Century. - German Activity. - Russian Activity. - Norwegian Activity. - Summary. - Literature.
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  • 33
    Series available for loan
    Series available for loan
    Associated volumes
    Call number: ZSP-595-1981
    In: Årbok
    Type of Medium: Series available for loan
    Pages: 63 S. : Ill., graph. Darst.
    ISBN: 8290307225
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  • 34
    Call number: ZSP-329-10
    In: Glaciological data
    Type of Medium: Series available for loan
    Pages: VII, 68 S. : Ill.
    Series Statement: Glaciological data : GD 10
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  • 35
    Series available for loan
    Series available for loan
    Oslo : Dybwad [in Komm.]
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    Call number: ZSP-597-1,1
    In: Resultater av de Norske statsunderstøttede Spitsbergenekspeditioner
    Type of Medium: Series available for loan
    Pages: 104 S.
    Series Statement: Resultater av de Norske statsunderstøttede Spitsbergenekspeditioner 1,1
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  • 36
    Series available for loan
    Series available for loan
    Kingston : Australian Nat. Antarctic Research Expeditions
    Associated volumes
    Call number: ZSP-124-21
    In: ANARE research notes
    Description / Table of Contents: The various rock lithologies present on Macquarie Island are described in detail together with their mode of occurence and field relations. The four predominant rock types are pillow basalts, dolerite dykes, troctolites and gabbros, and ultramafics (mainly harzburgite). This sequence represents a section through the earth's oceanic crust. The dominant structural geological feature is faulting at any scale. Faulting also controls the evolution of the Macquarie Ridge complex, of which the uppermost part is the Island. It is concluded that the sequence of rock units present on Macquarie Island generated at the Australian-Antarctic spreading ridge.
    Type of Medium: Series available for loan
    Pages: IV, 15 S. : Ill., graph. Darst. + 1 Kt.-Beil.
    ISBN: 0642871000
    Series Statement: ANARE research notes 21
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  • 37
    Call number: ZSP-124-22
    In: ANARE research notes
    Description / Table of Contents: Tables of mean monthly surface temperature and plots of mean annual temperature are presented for most of the permanent Antarctic and Southern Ocean stations. Because of the geographic sparcity of meteorological stations, particularly in the Pacific sector, data from some more northerly stations are also included.
    Type of Medium: Series available for loan
    Pages: iv, 98 S. : Ill., Kt.
    ISBN: 0642868727
    Series Statement: ANARE research notes 22
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  • 38
    Series available for loan
    Series available for loan
    Oslo : Dybwad
    Associated volumes
    Call number: ZSP-597-60
    In: Skrifter om Svalbard og Ishavet
    Type of Medium: Series available for loan
    Pages: 44 S. : Ill., graph. Darst.
    Series Statement: Skrifter om Svalbard og Ishavet 60
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  • 39
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    Series available for loan
    Oslo : Univ. Press [in Komm.]
    Associated volumes
    Call number: ZSP-597-154/D
    In: Geological map of Svalbard 1:500 000
    Type of Medium: Series available for loan
    Pages: 1 Kt. + Erl.-H.
    Series Statement: Geological map of Svalbard 1:500 000 4G
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  • 40
    Series available for loan
    Series available for loan
    Oslo : Univ. Press [in Komm.]
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    Call number: ZSP-597-182
    In: Skrifter
    Type of Medium: Series available for loan
    Pages: 41 S. : Ill., graph. Darst., Kt.
    ISBN: 8290307322
    Series Statement: Skrifter / Norsk Polarinstitutt 182
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  • 41
    Call number: ZSP-599-3
    In: Rapportserie
    Type of Medium: Series available for loan
    Pages: [29] S. : Ill., Kt.
    Series Statement: Rapportserie / Norsk Polarinstitutt 3
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  • 42
    Series available for loan
    Series available for loan
    London : British Antarctic Survey
    Associated volumes
    Call number: ZSP-164-96
    In: Scientific reports
    Type of Medium: Series available for loan
    Pages: 45, VIII S. : Ill., graph. Darst., Kt.
    Edition: by P. Stone
    ISBN: 0856650501
    Series Statement: Scientific reports / British Antarctic Survey 96
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  • 43
    Series available for loan
    Series available for loan
    Kingston : Antarctic Division, Dept. of Science and Technology
    Associated volumes
    Call number: ZSP-124-13
    In: ANARE research notes
    Description / Table of Contents: A computer technique is described for digitising data from the sea ice maps distributed weekly by the U.S. Navy-NOAA Joint Ice Centre. Monthly maps of the Antarctic region outlining extent of sea ice cover have been available from this source since January 1973. Computer programs for the analysis of this data are described. Maps are presented which illustrate the mean, over ten years, of the extent each month and at maximum. These data have been used as climate monitor using the relation between sea ice extent and the distribution of anticyclones, Antarctic and ocean temperatures, and atmospheric CO2 levels which have been the topics of many recent studies. The data are also of revelance to polar transport studies. Ships may need to penetrate, and aircraft may need to overfly, many kilometre of sea ice in order to carry out scientific programs or to gain access to Antarctic stations.
    Type of Medium: Series available for loan
    Pages: iv, 54 S. : Ill., Kt.
    ISBN: 0642877742
    Series Statement: ANARE research notes 13
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  • 44
    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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  • 45
    Series available for loan
    Series available for loan
    Hannover : Schweizerbart
    Associated volumes
    Call number: SR 90.0068(24) ; ZSP-320(E,24)
    In: Geologisches Jahrbuch
    Type of Medium: Series available for loan
    Pages: 13 S. + 1 Beil.
    Series Statement: Geologisches Jahrbuch : Reihe E 24
    Language: German
    Location: Lower compact magazine
    Location: Lower compact magazine
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  • 46
    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.
    Location: Upper compact magazine
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  • 47
    Call number: AWI G2-98-0365 ; M 93.0402
    In: Contributions to sedimentology
    Type of Medium: Monograph available for loan
    Pages: IV, 210 S. : Ill., graph. Darst.
    ISBN: 3510570138
    ISSN: 0343-4125
    Series Statement: Contributions to sedimentology 13
    Classification:
    Petrology, Petrography
    Language: English
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  • 48
    Monograph available for loan
    Monograph available for loan
    Moskva : Izdat. Moskovsk. Univ.
    Call number: AWI G3-94-0079
    Type of Medium: Monograph available for loan
    Pages: 202 S.
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  • 49
    Monograph available for loan
    Monograph available for loan
    Associated volumes
    Call number: AWI P2-88-0760 (1)
    In: Antarctica and international law
    Type of Medium: Monograph available for loan
    Pages: 703 S.
    ISBN: 0379203200
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  • 50
    Monograph available for loan
    Monograph available for loan
    Breslau : Hirt
    Call number: AWI P8-88-0817
    Type of Medium: Monograph available for loan
    Pages: 175 S. : Ill.
    Series Statement: Veröffentlichungen der Schleswig-Holsteinischen Universitätsgesellschaft 28/2
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  • 51
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    Series available for loan
    Bremerhaven : Alfred-Wegener-Inst. für Polar- und Meeresforschung
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    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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  • 52
    Monograph available for loan
    Monograph available for loan
    Leningrad : Gidrometeoizdat
    Call number: AWI A2-07-0040 ; MOP 45173 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 359 S. : graph. Darst., Kt.
    Uniform Title: Climatic Change
    Language: Russian
    Location: MOP - must be ordered
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  • 53
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    Canberra ; 132.1984-147.2002
    Call number: ZSP-123
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  • 54
    Call number: AWI G4-07-0060 ; AWI G6-97-0319
    Type of Medium: Monograph available for loan
    Pages: XI, 268 S. : Ill., graph. Darst., Kt.
    ISBN: 0387908854
    Series Statement: Springer series on environmental management
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  • 55
    Call number: ZSP-168/A-4
    In: Berichte zur Polarforschung
    Type of Medium: Series available for loan
    Pages: 303 S. : Ill., graph. Darst., Kt.
    Series Statement: Berichte zur Polarforschung : Sonderheft 4
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  • 56
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    Series available for loan
    Tokyo : Inst.
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    Call number: ZSP-403-74
    In: Jare Data Reports
    Type of Medium: Series available for loan
    Pages: 8 S. : graph. Darst.
    Series Statement: Jare Data Reports 74 : Aurora 10
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  • 57
    Call number: ZSP-403-77
    In: Jare Data Reports
    Type of Medium: Series available for loan
    Pages: 48 S. : graph. Darst.
    Series Statement: Jare Data Reports 77 : Meteorology 12
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  • 58
    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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  • 59
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    Tokyo : Inst.
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    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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  • 60
    Call number: ZSP-403-89
    In: Jare Data Reports
    Type of Medium: Series available for loan
    Pages: 87 S. : graph. Darst.
    Series Statement: Jare Data Reports 89 : Earth science 1
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  • 61
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    London : H.M.Stat.Off.
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    Call number: ZSP-164-19
    In: Scientific reports
    Type of Medium: Series available for loan
    Pages: 48 S. : Ill.
    Series Statement: Scientific reports / Falkland Islands Dependencies Survey 19
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  • 62
    Monograph available for loan
    Monograph available for loan
    Associated volumes
    Call number: AWI A5-98-0100-3
    In: Linkes meteorologisches Taschenbuch
    Type of Medium: Monograph available for loan
    Pages: XVI, 441 S. : Ill., graph. Darst., Kt.
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  • 63
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    Series available for loan
    London : British Antarctic Survey
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    Call number: ZSP-164-77 ; ZSP-164-77(2.Ex.)
    In: Scientific reports
    Type of Medium: Series available for loan
    Pages: 99 S. : Ill., Kt.
    ISBN: 0856650188
    Series Statement: Scientific reports / British Antarctic Survey 77
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  • 64
    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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  • 65
    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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  • 66
    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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  • 67
    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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  • 68
    Series available for loan
    Series available for loan
    Canberra : Australian Gov. Publ. Service
    Associated volumes
    Call number: ZSP-123-132
    In: ANARE Reports
    Description / Table of Contents: One of the weakest links in present ice dynamics models is the lack of an adequate empirical flow law for polycrystalline ice in its natural state. Inadequacies include a paucity of creep data relevant to cold ice masses and a general neglect of the effects of preferred crystal orientation fabrics. The present study reports the results of 150 000 hours of creep tests on isotropic aggregates replicating conditions of temperature and shear stress relevant to polar ice masses, from which an extended isotropic flow law has been constructed. It is shown how anisotropic crystal orientation fabrics can be incorporated into such a flow law. The quantitative model developed for this purpose is made possible by: (a) the definition of a normalised third deviatoric stress invariant as a configuration parameter describing the geometrical distribution of shear stress; and (b) a reinterpretation of the scalar geometric factor employed in the analysis of monocrystalline creep as a tensor coefficient of correlation between the orientation fabric and the stress configuration parameter. Laboratory experiments are presented to substantiate the validity of the model.
    Type of Medium: Series available for loan
    Pages: V, 93 S. : Ill., graph. Darst.
    ISBN: 0644005602
    Series Statement: ANARE Reports 132
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  • 69
    Monograph available for loan
    Monograph available for loan
    Associated volumes
    Call number: Q 1175(2) / Regal 50 ; AWI E2-99-0135 (2)
    In: Meteorology
    Type of Medium: Monograph available for loan
    Pages: XV, 331 S.
    Series Statement: 2
    Location: Magazine - must be ordered
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  • 70
    Monograph non-lending collection
    Monograph non-lending collection
    [Berlin : Springer]
    Associated volumes
    Call number: AWI PY-90-0189
    In: Naturwissenschaftliche Monographien und Lehrbücher ; 8, Bd. 8
    In: Einführung in die Geophysik ; 2, Bd. 2
    Type of Medium: Monograph non-lending collection
    Pages: 168 S , Ill., graph. Darst
    Edition: Sonderabdr.
    Series Statement: Naturwissenschaftliche Monographien und Lehrbücher 8
    Language: German
    Note: Inhaltsverzeichnis: Einleitung. - Instrumentelles. - Grundbegriffe. - Natürliche Magnete, künstliche Magnete und künstliche Magnetfelder. - Die gegenseitige Einwirkung zweier Magnete. - Grundlagen der Messung der erdmagnetischen Elemente. - Die Bestimmung der Deklination. - Die Bestimmung der Inklination. - Die Bestimmung der Horizontalintensität. - Absolute und relative Messungen. - Beobachtung der zeitlichen Variationen. - Das beharrliche Magnetfeld der Erde. - Allgemeines. - Kartographische Darstellung. - Darstellung der Reihenentwicklungen. - Das quasi-homogene Magnetfeld der Erde. - Das Feld der höheren Glieder. - Das überbleibende Feld. - Die säkulare Variation des beharrlichen Feldes. - Innere und äußere Kräfte. - Der potentiallose Anteil des Gesamtfeldes. - Erklärungsversuche des erdmagnetischen Feldes. - Das beharrliche Feld in einzelnen Ländern. Allgemeines über Landesaufnahmen. - Verteilung des Erdmagnetismus in Europa. - Zusammenhang der Anomalien mit dem Bau des Untergrundes. - Ursachen der Anomalien. - Die Fernwirkung störender magnetischer Massen. - Praktische Lösungen der Aufgabe. - Magnetische Störungen und Schwerestörungen. - Der Magnetismus der Sonne. - Die zeitlichen Variationen. - Der tägliche Gang. - Die Mondvariationen. - Die Störungen. - Theorie der Elektronenbahnen nach der Erde. - Aktivität, Ringstrom, äußerer Anteil der Sälularvariation. - Zusammenhang mit der Sonnentätigkeit. - Der innere Anteil der Variationen: Erdstrom. - Über die Verbindung erdmagnetischer Variationen mit erdelektrischen. - Das Polarlicht. - Allgemeines. - Verteilung über die Erde. - Verteilung am Himmelsgewölbe. - Verteilung in der Höhe. - Birkeland-Störmersche Theorie des Polarlichts. - Spektrum des Polarlichts. - Birkelands Versuche.
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  • 71
    Monograph available for loan
    Monograph available for loan
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    Call number: Q 1175(3) / Regal 50 ; AWI E2-99-0136 (3)
    In: Meteorology
    Type of Medium: Monograph available for loan
    Pages: IX, 527 S.
    Series Statement: 3
    Location: Magazine - must be ordered
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  • 72
    Call number: ZSP-980-30
    In: ZfI-Mitteilungen, Nr. 30
    Type of Medium: Series available for loan
    Pages: 340 Seiten
    ISSN: 0323-8776
    Series Statement: ZfI-Mitteilungen 30
    Language: German
    Note: Inhaltsverzeichnis Band 2b: Neue Ergebnisse zum Kohlenstoff-Isotopenaustausch im System CH4-CO2 / P. Harting ; I. Maaß. - Modelluntersuchungen zur Isotopenfraktionierung des Stickstoffs während der Metamorphose von Gesteinen / H.-M. Nitzsche ; K. Mühle ; A. Krause ; G. Schlegel ; K. Wetzel. - Variationen der Stickstoffisotope in regionalmetamorphen Gesteinen / D. Haendel ; K. Mühle ; G. Stiehl ; U. Wand. - Isotopenuntersuchungen an graphitischer Substanz von Metaschwarzschiefern des Erzgebirges und anderer Gebiete der DDR / U. Wand ; G. Stiehl ; I. Winkler ; P. Ossenkopf. - Zu einigen isotopengeochemischen Aspekten bei der Modellierung des globalen Sauerstoffkreislaufes / G. Weise ; W.-D. Hermichen. - Über die Isotopenzusammensetzung des Schwefels in sedimentären Sulfiden und Sulfaten / K. Wetzel. - Zur Schwefelisotopengeochemie basaltischer Gesteine / H.-W. Hubberten ; H. Puchelt. - Ein dynamisches Modell der Bleiisotopenevolution in der Erdkruste und im Erdmantel (russ.) = A dynamic model for lead isotope evolution in the earth's crust and mantle / B. G. Amov. - Kohlenstoff- und Wasserstoffisotopenvariationen in Methan aus Erdgasen und in Methan aus Crackreaktionen / A. Runge ; U. Wand. - Isotopische Zusammensetzung des Kohlenstoffs als ein Kriterium der Typisierung von Erdölen des Karna-Gebietes (russ.) / A. Z. Koblowa ; M. G. Frik ; W. M. Proworow. - Die isotopische Zusammensetzung des Kohlenstoffs als Fazieskriterium für organische Substanzen / I. Maaß. - Nitrogen isotope composition in natural diamonds - first results / U. Wand ; H.-M. Nitzsche ; K. Mühle ; K. Wetzel. - Über einige Isotopieeffekte des Stickstoffs in der Bodenzone / H. Hübner. - Das geologische Bild der Kohlenstoffisotopenvariation organischer Substanzen in paläozoischen Sedimentgesteinen der DDR / I. Maaß ; E. P. Müller ; P. Thomaser. - Beziehungen zwischen δ18O-Werten und stofflich-strukturellen Parametern von Silicaten / K. Wetzel ; D. Mißbach ; K. Mühle. - Richtungsaussagen über Isotopieeffekte mit Hilfe der Inkrementenmethode - Allgemeine Theorie / G. Christoph. - Richtungsaussagen über Isotopieeffekte mit Hilfe der Inkrementenmethode - 18O/16O-Isotopieeffekte in Silikaten / G. Christoph. - Vulkanogenes Kohlendioxid: Aussagen zur Herkunft aufgrund von Isotopenuntersuchungen / H. Puchelt ; H.-W. Hubberten. - Zur Druckabhängigkeit des Isotopieeffekts bei Verteilungsgleichgewichten - experimentelle und theoretische Untersuchungen an Modellsystemen / J. Heybey ; P. Harting. - Zum CO2-Austausch zwischen der nördlichen und der südlichen Hemisphäre / G. Weise ; K. Wetzel. - Fraktionierung der Quecksilberisotope in der Natur (russ.) / E. F. Doilnizyn ; W. I. Sjusin ; A. A. Obolenskij ; A. P. Perzewa. - Isotopic identification of Saharian groundwaters, groundwater formation in the past / Ch. Sonntag ; U. Thorweihe ; J. Rudolph ; E. P. Löhnert ; Chr. Junghans ; K. O. Münnich ; E. Klitzsch ; E. M. El Shazly ; F. M. Swailem. - Probleme der Auswertung von Isotopenanalysen an konzentrierten Salzlösungen im Kalibergbau / H.-D. Schmiedl. - Radiocarbon dating of the thermal waters in the Budapest area / J. Deák. - Untersuchungen zur regionalen Ausbreitung von Schadstoffen mit Hilfe technogener Isotopenvariationen / G. Weise ; I. Maaß. - Über die isotope Zusammensetzung des Stickstoffs in Gesteinen der Charnockitserie von Madras, Südindien / W. F. Wolynez ; R. D. Gawrilin ; N. L. Rao ; B. R. Reddi ; D. Haendel ; G. Stiehl ; U. Wand. - Erkenntnismöglichkeiten über natürliche Prozesse aus der Element- und Isotopenverteilung des Osmiums / H. Gerstenberger ; M. Geisler ; M. Herrmann ; H. Schelhorn. - Isotopenphysikalische Untersuchungen im Rahmen der Antarktisforschung der Bergakademie Freiberg / D. Hebert ; K. Froehlich. - Isotopenuntersuchungen zur Klärung der Genese der Grundwasserressourcen Ostsibiriens / E. V. Pinneker. - Autorenregister.
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  • 73
    Call number: AWI G6-18-91535
    Type of Medium: Dissertations
    Pages: Getr. Zählung: Ill., graph. Darst.
    Language: German
    Note: Karlsruhe, Univ., Diss., 1981 , INHALT: Zusammenfassung. - 1. Einleitung. - 1.1 Stand der Carbonatitforschung: experimentelle Untersuchungen und Bildungshypothesen. - 1.2 Mikrothermische Untersuchungen an fluiden Einschlüssen in Carbonatitmineralen. - 1.3 Der Carbonatit des Kaiserstuhls. - 1.4 Problemstellung, Methodisches. - 2. Das Probenmaterial. - 2.1 Proherrnahme und Aufbereitung. - 2.2 Probenpräparation für die Einschlußuntersuchungen. - 2.3 Optische Untersuchung, Phänomenologie. - 2.31 Anordnung, Verwachsungen und Habitus der Apatite. - 2.32 Die Einschlüsse der Apatite. - 2.321 Cavitätenformen, Füllungen, Dimensionen. - 2.322 Kriterien für primäre Einschlußbildung und sekundäre Veränderungen. - 2.323 Unterschiedliche Einschlußführung in Apatiten und anderen Mineralen. - 3. Apparaturen. - 3.1 Die mikrothermische Apparatur. - 3.11 Konzeption und Ausführung des Beiz-Kühltisches. - 3.12 Eichung des Beiz-Kühltisches. - 3.13 Präzision und Probleme im Meßbetrieb. - 3.2 Kühlplatte. - 3.3 Quetschtisch. - 4. Zur Theorie der Einschlußuntersuchungen. - 4.1 Geometrische Berechnungen. - 4.11 Berechnung des Cavitätenvolumens. - 4.12 Fehlerdiskussion. - 4.13 Grenzen der optischen Auflösung. - 4.2 Zur Theorie der Phasenverhältnisse. - 4.21 Einschlußbildung und Phasentrennung. - 4.22 Phasenverhältnisse in Einkomponentensystemen, Homogenisierungskurven. - 4.23 Phasenverhältnisse in Wasser-Salz-Systemen: H2O-NaCl; H2O-NaCl-KCl. - 4.24 Phasenverhältnisse in Wasser-Gas-Systemen: CO2-H2O. - 5. Konstruktion der Phasendiagramme. - 5.1 H2O. - 5.2 CO2. - 5.3 H2O-NaCl. - 5.4 CO2-H2O. - 5.5 Wasser-Salzsysteme mit kritischen Endpunkten (PQ-Systeme). - 5.6 Wasser-Salzsysteme bei stark positivem Temperaturkoeffizient der Löslichkeit der Salzkomponente: H2O-KCl, H2O-NaCl-KCl. - 5.7 System CO2-H2O-NaCl. - 6. Untersuchungsergebnisse. - 6.1 Experimentelle Untersuchungen an einzelnen Einschlüssen: Mikrothermometrie und destruktive Methoden. - 6.11 Einphasige Einschlüsse mit Gasfüllung. - 6.12 Calcit als Einphaseneinschluß im Apatit. - 6.13 Zweiphaseneinschlüsse L+V. - 6.14 Dreiphaseneinschlüsse LH2O + LCO2 +V. - 6.15 Einschlüsse mit übersättigten Lösungen (Multiphaseneinschlüsse). - 6.16 Fluide Einschlüsse im Calcit des Carbonatits. - 6.2 Analytische Untersuchungen. - 6.21 Kationen und Anionen in wäßrigen Extrakten des Apatitmahlgutes. - 6.22 Bitumenphasen in organischen Solventextrakten. - 6.23 Gasanalytische Messungen. - 7. Genetische Interpretation der Einschlußresultate. - 7.1 Das Subsystem H2O-Salzphasen. - 7.11 H2O-NaCl. - 7.12 H2O-NaCl-Na2SO4/Na2CO3. - 7.13 H2O-NaCl-KCl. - 7.2 Druckmodelle im seichten, subvulkanischen Niveau. - 7.21 Hydrostatische Bedingungen. - 7.22 Lithostatische Bedingungen. - 7.3 Das Subsystem CO2-H2O 7.4 Kombination der Teilsysteme, das System CO2-H2O-NaCl bei volumenkontrollierten Bedingungen. - 7.5 Zusammenfassung und Vergleich mit den Resultaten aus anderen Carbonatitlokalitäten. - 8. Petrogenetische Schlußfolgerungen. - 8.1 Magmatische Carbonatitintrusion und autometasomatische Folgeprozesse. - 8.2 Hydrothermaltransport des Calcits. - 8.3 Überlegungen zur Herkunft der Salzphasen. - 8.4 Künftige, weiterführende Untersuchungen. - 8.5 Zusammenfassung. - 9.0 Anhang I Abbildungen. - 10.0 Anhang II Originalmeßwerte.
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  • 74
    Monograph available for loan
    Monograph available for loan
    Berlin : Walter de Gruyter
    Call number: AWI G2-18-91886
    Type of Medium: Monograph available for loan
    Pages: VIII, Seiten [768-940] , Illustrationen
    Edition: Nachdruck
    ISBN: 3110072815
    Language: German
    Note: Inhalt: 8. Meereis. - Phänomene, Genese und Morphologie. - Zur Erforschung des Meereises. - Das Meereis als komplexe Erscheinung. - Das Meereis als Substrat. - Eisbildung und Gefriervorgänge. - Eisbildung auf dem Meere und Struktur der Meereisdecke. - Eisnomenklatur. - Formen des Meereises und Definitionen (Klassifikation). - Ejsbildungsphänomene an der oberen Grenzschicht des Meeres. - Schiffsvereisung, eine Erscheinung der Grenzschicht Hydrosphäre - Atmosphäre (Ozean - Luft). - Meereis an Küsten. - Eisbildung am Strand. - Eis und Eisbildung auf Watten. - Eisbildung an Steilküsten. - Das Meereis des Nordpolarmeeres und seiner Randmeere. - Zur Erforschung des Nordpolarmeeres und des polaren Meereises. - Nansen's Drift mit der „Fram" im Nordpolarmeer. - Die Driftbewegungen des arktischen Meereises des Nordpolarmeeres mit seinen Randmeeren. - Die Dynamik des Meereises im Nordpolarmeer nach Drifteis-Stationen. - Die jahreszeitliche Schwankung der Eisbedeckung des Nordpolarmeeres. - Form des Meeresbodens des Nordpolarmeeres. - Bilanz und Wassermassenaustausch des Nordpolarmeeres mit dem Atlantischen und Pazifischen Ozean. - Die Vereisung des Nordpolarmeeres und seiner Randmeere in ihrem Zusammenhang mit dem Wasserhaushalt. - Anthropogene Eingriffe und Projekte zur Veränderung der polaren Umwelt. - Eis des Meeres als Hindernis für den Seeverkehr. - Das Eis als besondere Grenzschicht des Meeres für die Schiffahrt. - Die Nordostpassage, arktischer Seeweg zwischen Atlantischem und Pazifischem Ozean innerhalb des eurasischen Kontinents: der sibirische Seeweg. - Der sibirische Seeweg. - Die Nordwestpassage - arktische Seeverbindung zwischen Atlantischem und Pazifischem Ozean um den nordamerikanischen Kontinent. - Erdöl in den Randmeeren des Nordpolarmeeres: Transportproblem und Ausbeute. - Umweltbedingungen und Nutzung der arktischen Region. - Meereis im Nordatlantischen Ozean und Nebenmeeren. - Eisberge im Nordatlantischen Ozean und Eis um Grönland. - Eiserkundung mit Luft- und Satellitenbildern. - Die Vereisung der Ostsee. - Zur Vereisung von Nebenmeeren in Nordamerika. - Das Meereis im Jahreshaushalt. - Wirkung und Mechanismus von Flußsystemen auf Wasser und Eis des Nordpolarmeeres. - Eisbedeckung des Nordpolarmeeres und Klimaschwankungen. - Das Meereis der Antarktis. - Zur Erforschung des Meereises um die Antarktis. - Die Eisschelfe: Größe, Form, Entstehung, Haushalt. - Eisberge der Antarktis. - Packeis der antarktischen Meeresregionen. - Eisgrenzen und Wassermassen des Südpolarmeeres. - Das Meereis, besonders der Antarktis, als klimatischer Faktor. - Die Polkappen der Erde im Satellitenbild. - Nachtrag (Ergänzung). - Mehrjährige Variation der antarktischen Meereisbedeckung (Südpolarregion). - Antarktischer Meereisaufbruch im Satellitenbild. - Die Eiskappe der Antarktis. - Der Meeresboden des Südpolarmeeres in bathymetnschen Profilen. - Rechtsverhältnisse der Antarktis und des südlichen Polarmeers. - Zur gegenwärtigen Polarforschung der BRD. - Polarexpeditionen der BRD. - Zu den Rechtsverhältnissen im Nordpolarmeer. - Das Polarmeer in morphographischer Darstellung. - Dynamik von Packeisfeldern (Ergänzung). - Literatur. - Institutionen zur Polarforschung. - Eisschlüssel und Eissymbole. - Sachregister.
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  • 75
    Monograph available for loan
    Monograph available for loan
    Bonn : Federal Republic of Germany, Press and Public Relations Department
    Call number: AWI P6-18-91970
    Type of Medium: Monograph available for loan
    Pages: iv, 169 Seiten
    Language: English
    Note: CONTENTS: Introduction. - International co-operation. - Intergovernmental co-operation. - Non-governmental co-operation. - I. Scientific Programme. - 1. Astronomy. - 2. Biological Sciences. - 2.1 The marine ecosystem and its living resources. - 2.1.1 Food resources, phytoplankton production and zooplankton. - 2.1.2 The role of the benthos. - 2.1.3 The role of micro-organisms. - 2.1.4 Distribution and incidence of seals in the pack-ice of the Weddell Sea. - 2.1.5 Distribution and life history of fishes. - 2.1.6 Large-scaie distribution and drift of krill. - 2.1.7 Composition and behaviour of krill shoals. - 2.1.8 Preservation and processing of krill. - 2.2 The adaptation of antarctic marine organisms to their environment. - 2.2.1 Experiments and marine studies on .the ecophysiology of krill. - 2.2.2 Temperature regulation and food requirements of warm-blooded antarctic animals. - 2.2.3 Growth, digestive system and food economy of antarctic fishes. - 2.2.4 Freezing resistance of sea animals. - 2.2.5 Taxonomy of antarctic marine organisms. - 2.3 Terrestrial biology in Antarctica. - 2.3.1 Temperature adjustments in the reproductive biology of antarctic birds. - 2.3.2 Biochemical bases of growth processes in poikilothermic organisms at very low temperatures. - 2.3.3 Nutritional biology of poikilothermic herbivora. - 2.3.4 Study of lichens, fungi and bacteria in Antarctica and on offshore islands. - 2.3.5 Photosynthesis and heterotrophic life cycle of plants at very low temperatures. - 2.4 Environmental protection in Antarctica. - 2.5 Human biology and medicine in polar regions. - 3. Geodesy, Cartography and Remote Sensing. - 3.1 Satellite geodesy. - 3.2 Doppler satellite positioning. - 3.3 Geodetic mapping of ice-free areas. - 3.4 Remote-sensing by satellite. - 4. Geology and Geophysics. - 4.1 Study of drift processes as a contribution to the geological history of Antarctica. - 4.1.1 Study of magnetic structures by means of aeromagnetic photography. - 4.1.2 Paleomagnetic studies of drift evolution. - 4.1.3 Micro-earthquakes as indicators of tectonic activity. - 4.1.4 Earth tides and natural oscillations of the earth. - 4.2 Studies of the structure of crust and mantle. - 4.2.1 Structure of the basement complex of the transantarctic mountain chain in the area east of the Filchner Ice Shelf. - 4.2.2 Structure of the basement of the Weddell Sea, the Filchner/Ronne Ice Shelf, and the peripheral area. - 4.2.3 Oldest and highly metamorphous rocks of the East Antarctic. - 4.3 Stratigraphy, tectonics and magmatism in the mobile areas. - 4.3.1 Mobile fringe areas of the East Antarctic. - 4.3.2 Paleozoic and mesozoic mountains(Beacon upper group) in the transantarctic mountains. - 4.3.3 Early paleozoic to cainozoic orogenes in the area around the Filchner/Ronne Ice Shelf. - 4.4 Study of exogenous processes under extremely cold conditions. - 4.4.1 Glacial geology and geomorphology. - 4.4.2 Weathering and detrital formation. - 4.5 Geoscientific marine research. - 5. Glaciology. - 5.1 Volume and dynamics of the Filchner/Ronne Ice Shelf. - 5.2 Determining the extent and thickness of the ice and its temporal variation in the Filchner/Ronne Ice Shelf sector and peripheral areas. - 5.3 Determining the composition and inner structure of the Filchner/Ronne Ice Shelf on the basis of geophysical surface measurements. - 5.4 Studies of the dynamics of the pack-ice in the Weddell Gyre. - 5.5 Physical characteristics of ocean ice. - 5.6 Glaciological drillings. - 5.7 Chemical composition and accumulation genesis of antarctic background aerosol; global transport of trace gases and aerosols. - 5.8 Study of the elastic and rheological characteristics of ice, its heat conductability and texture affected by deformation. - 6. Upper Atmosphere and Extraterrestrial Physics. - 6.1 Investigation of whistlers and VLF radio emissions (chorus, hiss, etc) at conjugated points. - 6.2 Study of terresterial magnetic pulsations at conjugated points. - 6.3 Study of atmospherics to obtain more precise data on worldwide thunderstorms. - 6.4 Measurements of the aero-electric field. - 6.5 Balloon-based study of the ionosphere in the light of Mg t resonance lines. - 6.6 Measurement of the vertical distribution of ozone, steam and aerosol up to an altitude of 30 km. - 6.7 Measurements of emission in the infrared 9.6 µ ozone band from the ground. - 6.8 Other projects which may be carried out simultaneously with the above or later. - 6.9 Proposed basic terrestrial magnetic equipment for the Antarctic Station. - 6.10 Meteorite search expedition. - 6.11 Study of micrometeorites and cosmic dust. - 7. Meteorology and Oceanography. - 7.1 Meteorology. - 7.1.1 Atmospheric boundary stratum. - 7.1.2 Study of stratospheric circulation. - 7.1.3 Measurement of trace gases over long periods. - 7.1.4 Other research projects. - 7.1.5 Weather service observations and consultations. - 7.1.6 Basic meteorological equipment for the Antarctic Station. - 7.2 Physical oceanography. - 7.2.1 Formation and extent of bottom water in the Atlantic sector of the circumantarctic ocean. - 7.2.2 Numeric simulation of the vertical flows of material, energy and impulses. - 7 2.3 Time scales of transportation in deep water with the aid of radioactive trace elements. - 7.2.4 Detection of heavy metals in the Antarctic Ocean. - 7.2.5 Fishery oceanography in circumantarctic waters. - 7.2.6 Other research projects. - 8. Engineering Sciences. - 8.1 Shipbuilding technology. - 8.1.1 Measuring and testing programme regarding the performance of vessels in ice and technical developments in the construction of ice-going vessels. - 8.2 Iceberg location and navigation. - 8.2.1 Iceberg location. - 8.2.2 Development of precision positioning systems (also for dynamic positioning) to ensure noninterference with signals transmitted through ice and water masses of different thicknesses. - 8.3 Construction techniques. - 8.4 Exploration techniques. - 8.5 Other topics. - The Antarctic Research Station. - The Polar Research and Supply Ship. - The Polar Research Institute. - Institutions contributing to the Programme.
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  • 76
    Monograph available for loan
    Monograph available for loan
    Stuttgart : Franckh
    Associated volumes
    Call number: AWI E2-16-90308
    In: Der Kampf um den Nordpol / Karl H. Salzmann
    In: Die Kosmos-Bibliothek ; 220
    Type of Medium: Monograph available for loan
    Pages: 79 S. , Ill.
    Series Statement: Kosmos-Bibliothek 220
    Language: German
    Note: Inhaltsverzeichnis: Einleitung. - Die Anfänge der Arktisforschung. - Mit Segelschiffen von Spitzbergen über die Polregion nach Ostasien (1607-1818). - Mit Schlittenbooten, Hundeschlitten und Dampfschiffen dem Pol entgegen (1827-1882).
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  • 77
    Call number: AWI G1-17-90940
    Type of Medium: Monograph available for loan
    Pages: XXXI, 475 S. , Ill., Kt., graph. Darst. , 6 Kt.
    Series Statement: Natural History of Central Asia 2
    Language: English
    Note: CONTENTS: PREFACE. - LIST OF PLATES. - LIST OF FIGURES. - PART I. - GENERAL INTRODUCTION. - I. - Geological objectives and methods of the expedition with a review of former explorations. - Introduction. - The approach to Mongolia. - The Gobi Region. - Prehistoric adventure. - Historic travel and modern exploration. - Earlier studies of special significance. - II. - Boundaries of the Gobie Region. - Introduction. - The Northern Boundary. - Northern boundary - western section. - Northern boundary - central section. - Northern boundary - eastern section. - Summary of the Transbaikal border. - The Eastern Boundary. - Summary of the eastern boundary. - The Southern Boundary. - Southern boundary - eastern section. - Southern boundary - central section. - Southern boundary - western section. - The Western Boundary. - PART II. - ROUTE STUDIES OR ITINERARY. - Introduction. - The task of a geological reconnaisance expedition. - Recording observations. - III. - From Kalgan to Iren Dabasu. - Kalgan to Wan Ch'uan Pass. - The lower pass. - Wan Ch'uan basin and the upper pass. - The Pacific divide to P'ang Kiang. - The granite hills of Chakhar. - The P'ang Kiang hollow. - P'ang Kiang to Iren Dabasu. - The first fossils. - IV. - From Iren Dabasu to Urga. - Iren Dabasu to Camp Jurassic. - The structural relations at Camp Jurassic. - Camp Jurassic to Mount Tuerin. - The granites of Mount Tuerin. - Mount Tuerin to Bolkuk Gol. - The Arctic divide. - Observations in the vicinity of Camp Bolkuk Gol. - Course of the Bolkuk Gol. - Glacial evidence in the Gangin Daba. - Ground ice. - Local culture. - Side traverse toward Urga. - Mineral resources. - V. - From Urga to Tsetsenwan Traverse along the Tola River. - The vicinity of five Antelope Camp. - From the Tola River to Tsetsenwan. - The vicinity of Tsetsenwan. - A side traverse north of Tsetsenwan. - The serpent-form dikes. - Contact effects of the granite margin. - Jurassic structural relations. - A side traverse south of Tsetsenwan. - VI. - From Tsetsenwan to Sain Noin and the Arctic divide. - Wastward from Tsetsenwan. - The vicinity of Camp Canyon Brook. - From Camp Canyon Brook to the Ongin Gol. - Rock-bound hollows. - Continuation of the traverse. - The Ongin Gol. - From the Ongin Gol to Sain Noin. - The vicinity of Sain Noin. - From Rainy Gulch to the Arctic Divide. - A step across the divide. - VII. - From the hot springs of Sain Noin to Mount Uskuk. - Arishan to Gorida. - The Gorida basin. - The old Uliassutai trail. - Old Uliassutai Trail to Mount Uskuk. - The saltpan of Guchu Burt. - Ondai Sair. - VII. - The return journey from Tsagan Nor to Artsa Bogdo. - Choosing a route. - Tsagan Nor to the volcanic cliffs. - Desert hollows. - Volcanic cliffs to Artsa Bogdo. - North Margin of Artsa Bogdo. - Picture writings. - IX. - From Artsa Bogdo to Sair Usu. - Artsa Bogdo to Djadokhta. - The flaming cliffs of Djadokhta. - Djadokhta to Ongin Gol in Sumu. - Ongin Gol in Sumu. - Ongin Gol to Sair Usu. - X. - From Sair Usu to Kalgan. - Palaeozoic strata. - Continuation of traverse to Ardyn Obo. - Sediments of Ardyn Obo. - Ardyn Obo to Shara Murun. - Palaeozoic strata of Jisu Honguer. - Tertiary sediments of Shara Murun. - Shara Murun to Kalgan. - Chinese settlements. - The return to Kalgan. - PART III. - SPECIAL AND LOCALITY STUDIES. - Introduction. - Method of Mapping. - XI. - Eren Dabasu and Irdin Manha. - Introduction. - General aspect and larger relations of the basin. - Origin of the hollow at Iren Dabasu. - General Rock structure. - The Iren Dabasu formation. - Variegated Tertiary beds. - The Houldjin formation. - The Arshanto and Irdin Manha formations. - Shara Murun. - Age and correlation. - XII. - Arishan, the sacred mountain of Sain Noin. - Introduction. - Features of the locality. - Geological formations. - Graywacke series. - The granite. - The Jurassic formation. - Special products. - Structural features. - The spring waters and their origin. - XIII. - Mount Uskuk and the Tsagan Nor Basin. - Principal structural features. - The rock formations. - Rocks of the ancient floor. - The crystalline metamorphics. - The graywacke series. - Bathylithic granite. - Jurassic strata. - Post-Jurassic intrusives. - Rocks of the sedimentary cover. - Cretaceous strata. - Fossil content. - Tertiary strata. - Fossil content. - Former extent of later sediments. - Evidence of the faulted margins. - Evidence of the sedimentary remnants. - Evidence of the basalt remnants. - Evidence of planation. - Erosional history of the south block of Uskuk. - Deformation of the Mount Uskuk region. - The Saltpan of Guchu Burt. - Tsagan Nor. - XIV. - The Gurbun Saikhan Ranges. - The journey. - A desert well. - The return journey. - Geological observations at Artsa Bogdo. - The south.basin. - Approach to the Gurbun Saikhan. - The formations of the Gurbun Saikhan. - Ancient rocks. - Limestones. - Serpentine. - Graywacke-slate series. - Topographic character of the Gurbun Saikhan. - XV. - Artsa Bogdo and Oshih. - The Artsa Bogdo Mountain Block. - The marginal shelf. - History of the shelf. - Rock formations of the mountain. - Ancient meta-crystallines and intrusives. - Folded sediments and associated eruptives. - Later igneous rocks. - Tectonic features. - Traces of former sedimentary cover. - Topographic features. - Stream pattern. - Glaciation. - The Oshih Hollow. - Features of the locality. - The geologic column. - XVI. - Problems and areas deserving special study. - Introduction. - Sedimentary basins and potential fossil fields. - The area of the great pass. - P'ang Kiang. - The paper-shales of mile 299. - The flaming cliffs of Uskuk. - Oshih (Ashile) basin. - Djadokhta. - Ardyn Obo. - Shara Muraci. - Ulan Nor. - The badlands of the Ongin Gol. - Structural and historical problems. - The Camp Jurassic area. - The crystalline upland east of the Ongin Gol. - The transition country of Gangin Daba. - Sair Usu. - Los in Sumu. - Jisu Honguer. - Genral problems. - PART IV. - SUMMARIES AND DISCUSSIONS. - Introduction. - XVII. - Structural elements of the Oldrock floor. - Two major divisions. - Subdivision of the Oldrock floor. - Mesozoic intrusives. - Jurassic sediments. - Paloeozoic strata. - The great Mongolian bathylith. - The Khangai graywacke series. - The ancient crystalline complex. - The Wu T'ai system. - The T'ai Shan complex. - XVIII. - Surface features and their origin. - Basins and mountains. - The basin of Mongolia. - Deserts in general. - The shaping processes. - Major subdivisions of the Mongolian Basin. - Talas of the eastern and southern province. - The western faulted talas. - Mountains. - Fault-block mountains of the Altai type. - Ikhe Bogdo. - Baga Bogdo. - Artsa Bogdo. - Gurbun Saikhan. - The mountains of the eastern province. - Volcanic mountains. - The structure lines of Mongolia. - XIX. - Surface features and their origin (continued). - Plateaus, plains and flatlands. - Introduction - the level lands of the desert. - Agencies which carve the erosion plane. - Erosion by wind. - Rainfall. - Drainage. - Immigrant streams. - Native streams. - Erosive work of running water. - The Piedmont Slope. - The Gobi erosion plane. - Original slopes of the erosion plane. - Deformation of the Gobi surface. - Deposits on the Gobi upland. - Redissection of the Gobi erosion plane. - Summary of the Gobi erosion plane. - Desert Hollows. - The older Peneplanes. - The pre-Cretaceous peneplane. - The Mongolian peneplane. - The Khangai peneplane. - Relations of the Khangai and Mongolian peneplanes . - Relations of the Mongolian peneplane and the Gobi erosion plane. - Relations between the Gobi erosion plane and the lowlands of the P'ang Kiang stage. - Comparison of peneplanes with those of surrounding regions. -
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  • 78
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    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
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    Call number: ZSP-201-83/29
    In: CRREL Report, 83-29
    Description / Table of Contents: A literature review indicated that the effects or permafrost on streambank erodibility and stability are not yet understood because systematic and quantitative measurements are seriously lacking. Consequently, general controversy exists as to whether perennially frozen ground inhibits lateral erosion and bankline recession, or whether it increases bank recession rates. Perennially frozen streambanks erode because of modification of the bank's thermal regime by exposure to air and water, and because of various erosional processes. Factors that determine rates and locations of erosion include physical, thermal and structural properties of bank sediments, stream hydraulics and climate. Thermal and physical modification of streambanks may also induce accelerated erosion within permafrost terrain removed from the immediate river environment. Bankline or bluffline recession rates are highly variable, ranging from less than 1 m/year to over 30 m/year and, exceptionally, to over 60 m/year. Long-term observations of the physical and thermal erosion processes and systematic ground surveys and measurements of bankline-bluffline recession rates are needed.
    Type of Medium: Series available for loan
    Pages: iv, 26 Seiten , Illustrationen
    Series Statement: CRREL Report 83-29
    Language: English
    Note: CONTENTS Abstract Preface Introduction Stream bank erosional processes Permafrost and related factors Permafrost and erosion General Erosional processes Bank zone processes Bluff zone processes Factors affecting perm afrost erodibility Exposure to currents and wind waves Texture and stratigraphy Ice content, distribution and type Slope aspect Coriolis force Timing and depth of thaw Water level and temperature Vegetation Ice and snow cover Groundwater Rates and timing of erosion and recession Overall effects of permafrost Recommendations for research Literature cited Appendix A : Processes of stream bank modifications
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  • 79
    Call number: AWI P6-17-90984
    In: Geographische Handbücher
    Description / Table of Contents: Dieses Werk gibt erstmalig eine geschlossene Länderkunde des Südpolarkontinents und seiner vorgelagerten Inseln nach neuestem Stand, wie sie in solcher Ausführlichkeit einmalig in der bisherigen Literatur ist. In zwölf Abschnitten werden Forschungsgang, Geologie, Vereisung und Klima der Antarktis, die ozeanographischen Verhältnisse der umgebenden Meere, die Lebewelt und die wirtschaftlichen wie politischen Verhältnisse behandelt. Der zweite Teil bietet eine ausführliche regionale Darstellung der einzelnen natürlichen Großräume des Kontinents. Die beigegebenen Karten stellen einen kleinen länderkundlichen Atlas des Gebietes dar, wie er in ähnlicher Form ebenfalls noch nicht existiert. Von besonderer Wichtigkeit sind die Angaben über alle bisher durchgeführten Expeditionen und den Walfang, die Klimatabellen, Listen von Hütten und Leuchtfeuern sowie der beigegebene wissenschaftliche Apparat. Diese Länderkunde ist im Zusammenwirken mit Polarinstituten und Forschern aller an der Antarktis interessierten Länder entstanden und wird sich bei der künftigen Erschließung des Südpolkontinents und den Vorbereitungen für das Geophysikalische Jahr 1957/58 als unentbehrlich erweisen.
    Type of Medium: Monograph available for loan
    Pages: 310 S. , Ill., Kt. , 1 Kt.-Beil.
    Series Statement: Geographische Handbücher [5]
    Language: German
    Note: Inhalt: 1. Einleitung. - 2. Grenzen, Einteilung und Namengebung. - 3. Forschungsgang. - 4. Bau und Oberflächenformen des eisfreien Gebietes. - 5. Klima. - 6. Erdmagnetismus und Polarlicht. - 7. Das Südpolarmeer. - 8. Die Vereisung des Südpolargebietes. - 9. Pflanzen- und Tierwelt in der Antarktis. - 10. Die Wirtschaft des Südpolargebietes. - 11. Politische Ansprüche und Besiedlung. - 12. Akklimatisation und Möglichkeiten der Besiedlung in der Zukunft. - 13. Die einzelnen Teilgebiete der Antarktis. - A. Die subantarktischen Streuinseln. - 1. Bouvet. - 2. Truls und Pagoda-Felsen. - 3. Prinz-Edward-lnseln. - 4. Crozet-lnseln. - 5. Kerguelen. - 6. Heard-Gruppe. - 7. Royal Company und Emerald. - 8. Macquarie. - 9. Nimrod, Swains und Dougherty. - B. Die subantarktischen Inseln des Südantillenbogens. - 1. Südgeorgien. - 2. Süd-Sandwich-Gruppe. - C. Die polaren Inseln des Südantillenbogens. - 1. Süd-Orkney-Gruppe. - 2. Süd-Shetland-lnseln. - D. Die polaren Streuinseln. - 1. Peter-l.-lnsel. - 2. Scott-lnsel. - 3. Balleny-Inseln. - E. Ostantarktis. - 1. Das ostantarktische Horstgebirge. - 2. Zentralplateau und Wilkesland. - 3. Die Bergländer des afrikanischen Quadranten. - 4. Neu-Schwabenland. - 5. Die Ostküste des Weddell-Meeres. - F. Westantarktis. - 1. Das nördliche Grahamland. - 2. Südliches Grahamland und vorgelagerte Inseln. - 3. James-Ellsworth-Land. - 4. Marie-Byrd-Land 233. - 5. Das Gebiet der antarktischen Depression. - 14. Ziele und Aufgaben der künftigen antarktischen Forschung. - 15. Literatur. - Tabellen. - Namen- uud Sachverzeichnis. - Verzeichnis der Karten und Figuren. - Bildtafeln. - Übersichtskarte.
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  • 80
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    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-82/31
    In: CRREL Report, 82-31
    Description / Table of Contents: Information on sea ice conditions in the Bering Strait and the icefoot formation around Fairway Rock, located in the strait, is presented. Cross-sectional profiles of Fairway Rock and the relief of the icefoot are given along with theoretical analyses of the possible forces active during icefoot formation. It is shown that the ice cover most likely fails in flexure as opposed to crushing or buckling, as the former requires less force. Field observations reveal that the Fairway Rock icefoot is massive, with ridges up to 15 m high, a seaward face only 20 degrees from vertical, and interior ridge slopes averaging 33 degrees. The icefoot is believed to be grounded and its width ranges from less than 10 to over 100 m.
    Type of Medium: Series available for loan
    Pages: 44 Seiten , Illustrationen
    Series Statement: CRREL Report 82-31
    Language: English
    Note: CONTENTS Abstract Preface Introduction Bering Strait Field reconnaissance Estimation of ice forces on Fairway Rock 1. Creep deformation 2. Crushing failure 3. Flexural failure 4. Forces required to form floating or grounded pressure ridges along therock or to pile ice on the beaches 5. Buckling failure Driving forces Angle of internal friction of sea ice Summary Literature cited Appendix A: April 1982 field observations at Fairway Rock
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  • 81
    Series available for loan
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    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-82/33
    In: CRREL Report, 82-33
    Description / Table of Contents: Arctic sea ice is freckled with melt ponds during the ablation season; Antarctic sea ice has few, if any. On the basis of a simple surface heat budget, we investigate the meteorological conditions necessary for the onset of surface melting in an attempt to explain these observations. The low relative humidity associated with the relatively dry winds off the continent and an effective radiation parameter smaller than that characteristic of the Arctic are primarily responsible for the absence of melt features in the Antarctic. Together these require a surface-layer air temperature above 0 C before Antarctic sea ice can melt. A ratio of the bulk transfer coefficients C sub H/C sub E less than 1 also contributes to the dissimilarity in Arctic and Antarctic ablation seasons. The effects of wind speed and of the sea-ice roughness on the absolute values of C sub H and C sub E seem to moderate regional differences, but final assessment of this hypothesis awaits better data, especially from the Antarctic.
    Type of Medium: Series available for loan
    Pages: 16 Seiten , Illustrationen
    Series Statement: CRREL Report 82-33
    Language: English
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  • 82
    Series available for loan
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    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-82/32
    In: CRREL Report, 82-32
    Description / Table of Contents: Low-frequency (10 Hz) volcanic earthquakes originate at a wide range of depths and occur before, during, and after magmatic eruptions. The characteristics of these earthquakes suggest that they are not typical tectonic events. Physically analogous processes occur in hydraulic fracturing of rock formations, low-frequency icequakes in temperate glaciers, and autoresonance in hydroelectric power stations. We propose that unsteady fluid flow in volcanic conduits is the common source mechanism of low-frequency volcanic earthquakes (tremor). The fluid dynamic source mechanism explains low-frequency earthquakes of arbitrary duration, magnitude, and depth of origin, as unsteady flow is independent of physical properties of the fluid and conduit. Fluid transients occur in both low-viscosity gases and high-viscosity liquids. A fluid transient analysis can be formulated as generally as is warranted by knowledge of the composition and physical properties of the fluid, material properties, geometry and roughness of the conduit, and boundary conditions. To demonstrate the analytical potential of the fluid dynamic theory, we consider a single-phase fluid, a melt of Mount Hood andeside at 1250 deg C, in which significant pressure and velocity variations occur only in the longitudinal direction.
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    Pages: 15 Seiten , Illustrationen
    Series Statement: CRREL Report 82-32
    Language: English
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  • 83
    Series available for loan
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    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-83/9
    In: CRREL Report, 83-9
    Description / Table of Contents: Recent observations of shore ice pile-up and ride-up along the coast of the Alaska Beaufort Sea are presented. Information is given to show that sea ice movement on shore has overridden steep coastal bluffs and has thrust inland over 150 m, gouging into and pushing up mounds of beach sand, gravel, boulders and peat and, inland, the tundra material. The resulting ice scar morphology was found to remain for tens of years. Onshore ice movements up to 20 m are relatively common, but those over 100 m are very infrequent. Spring is a dangerous time, when sea ice melts away from the shore, allowing ice to move freely. Under this condition, driving stresses of less than 100 kPa can push thick sea ice onto the land.
    Type of Medium: Series available for loan
    Pages: v, 59 Seiten , Illustrationen
    Series Statement: CRREL Report 83-9
    Language: English
    Note: Contents Abstract Preface Introduction Winter 1979-80 observations Winter 1980-81 and summer 1981 observations Winter 1981-82 and summer 1982 observations Old ice ride-up features Discussion Literature cited Appendix A. The boulder rampart and rock littered shore west of Konganevik Pt. Appendix B. Site location maps
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  • 84
    Monograph available for loan
    Monograph available for loan
    Sosnowiec : Uniwersytet Śląski, Instytut Geografii
    Call number: AWI P9-83-1079
    Type of Medium: Monograph available for loan
    Pages: 248 Seiten , Illustrationen, Karten
    Language: Polish
    Note: Contents: A snow cover in the region of Fiord Hornsund on Spitsbergen / J. Pereyma. - Temperature rations in summer on the Waldemar Glacier and on the Waldemar sea lowland / G. Wójcik, K. Marciniak, R. Przybylak. - Precipitation and evaporation in Werenskiold Glacier district / A. Szczepankiewicz-Szmyrka. - Biometeorological conditions on the Werenskiold Glacier forefield in summer of 1980 / A. Szczepankiewicz-Szmyrka. - Some notes on wind directions in the West Spitsbergen in 1980 / K. Gerstmann. - Radar measurements of the thickness of the Werenskiold Glacier / R. Czajkowski - The analysis of movements of the Werenskiold Glacier based on dating of fossil moss / H. Chmal - Increase in the mass of the firn snow in the glacial amphiteatre of the Penck Glacier in the period 1934 to 1958 / C. Lipert - Some automatic systems to collect and transmission stored data using various radio-links / J. Molski. - Würm and Holocene glaciations of North-Western Sörkappland exemplified by the Slakli Valley, Spitsbergen / P. Kłysz, L. Lindner. - The marine origin of Lisbetdalen mezorelief SW Spitsbergen / W. Stankowski - Raised marine terraces of Kulmstranda North-Western Sörkappland / P. Kłysz, L. Lindner - The geomorphological sketch map of the Gåsdalen region, South Spitsbergen / J. Jania, Z. Lentowicz, T. Szczypek, J. Wach. - Last deglaciation of Treskelen Peninsula, Hornsund, Svalbard / L. Marks. - The recession of Vitkovski Glacier as recorded in its marginal zone / L. Andrzejewski, w. Stankowski. - Degradation processes on the end moraine of the Werenskiold Glacier / J. Cegła, J. Kida. - Studies of the dessication crack on the forefield of the Werenskiold Glacier / J. Cegła. - The beginning and evolution of the marginal outwash on the forefield of the Eliza Glacier / A. Olazewski. K. Sendobry. - Summer thawing of the ground in the Kaffiöyra, SW Spitsbergen / K. Marciniak, W. Szczepanik, R. Przybylak - Morphology and sedimentary environments of the Baszkara ·and Dzankuat Glaciers in the High Kaukas / A. Karczewski, A. Kostrzewski,P. W. Kowalew. - Stratigraphic position and remarks on sedimentation of the Brentskardhaugen Bed, Spitsbergen / A. Wierzbowski, G. Biernat, C. Kulicki. - Some remarks concerning the structure of groups of the bottom fauna of the Admiralty Bay - King George Island, South Shetland / P. Presler, K. Jażdżewski·, W. Jurasz, W. Kittel, J. Siciński. - Biological indexes of the hydrological conditions - observations from Hornsund region, Spitsbergen / J. M. Węsławski. - The habitability of the littoraly rocks in region Steinvika and Hyttevika Bays, Vestspitsbergen / O. Różycki, M. Gruszczynski. - Some aspects of the acoustical estimation of the krill abundance / M. Brzozowska. - Liberation of carbon dioxide from tundra soils / H. Dziadowiec. - Exploration in the Hornsundfiord region / J. Szupryczyński. - , In polnischer Sprache
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  • 85
    Call number: AWI G9-19-92232
    Type of Medium: Monograph available for loan
    Pages: 28 Seiten
    Language: German
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  • 86
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    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-82/43
    In: CRREL Report, 82-43
    Description / Table of Contents: The radar signatures of ice wedges and wedge-like structures have been investigated for a variety of soil conditions. The radar used for this study emitted short sinusoidal pulses of about 10-ns duration with an approximate center frequency of 150 MHz. Most of the ice wedges existed at depths of about 1 m in a variety of silty and sandy soils with both frozen and thawed active layers. The position of the wedges was usually identified from corresponding surface features. An artificial ice wedge in coarse-grained alluvium was also profiled as well as wedge-like structures of fine silt in a coarse-grained glacial outwash. All wedges and wedge-like structures produced a hyperbolic reflection profile except when an active layer of thawed, saturated silt was present which eliminated returns from the wedges. The peaks of the hyper-bolas were sometimes masked by reflections from the permafrost table or other material interfaces, and multiple hyperbolas occurred at some sites. The dielectric constant of the host medium was often calculated from the linear portions of the hyperbolas and the results were verified by laboratory time domain reflectometry measurements per-formed on field samples. In some cases, hyperbolic profiles originated at several meters depth suggesting that deep ice wedges could be detected in areas of cold permafrost.
    Type of Medium: Series available for loan
    Pages: iv, 19 Seiten , Illustrationen
    Series Statement: CRREL Report 82-43
    Language: English
    Note: CONTENTS Abstract Preface Introduction Background Objectives and procedures Equipment used Radar TDR Definitions Massive ice Results Artificial wedge: Norwich, Vermont Ice wedges in sand: Fish Creek, Alaska Ice wedges: Prudhoe Bay, Alaska Ice wedges under thawed fine-grained soils: North Slope, Alaska Wedge-like soil structures: Ft. Greely, Alaska TDR measurements Summary and concluding remarks Literature cited Appendix A: Brief discussion of dispersion
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  • 87
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-82/41
    In: CRREL Report, 82-41
    Description / Table of Contents: Many of the important factors influencing the choice of appropriate aquifer test procedures are presented. The concepts of bias, accuracy and spatial variabil­ity are explained. The definitions of a number of aquifer parameters are devel­oped from basic principles demonstrating the underlying assumptions and limita­tions. The parameters considered are: piezometric head, hydraulic conductiv­ity/intrinsic permeability, flow direction, specific discharge magnitude, transmissivity, volumetric flow rate, total porosity, effective porosity, aver­age linear velocity, storage coefficient, specific yield, dispersion coefficient-aquifer dispersivity. For each parameter several techniques are described, evaluated and ranked in terms of perceived potential accuracy, simplicity and value to contaminant transport studies. It must be stressed, however, that the evaluations are based principally upon theoretical grounds, and not upon actual conduct of the described procedures.
    Type of Medium: Series available for loan
    Pages: iv, 111 Seiten , Illustrationen
    Series Statement: CRREL Report 82-41
    Language: English
    Note: CONTENTS Abstrac Preface Introduction Purpose Scope Concept of accuracy Test selection Definition of parameters Piezometric head Use of piezometers Hydraulic conductivity Flow direction Specific discharge magnitude Transmissivity Volumetric flow rate Porosity Average linear velocity Storage coefficient-specific yield Aquifer dispersivity Parameter estimation techniques Piezometric head Hydraulic conductivity Direction and magnitude of specific discharge vector Transmissivity Volumetric flow rate Total porosity Average linear velocity Storage coefficient Specific yield Effective porosity Aquifer dispersivity-dispersion coefficients Conclusions Literature cited
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  • 88
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    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-82/40
    In: CRREL Report, 82-40
    Description / Table of Contents: The use of explosives to break floating ice sheets is described, and test data are used to develop design curves that predict explosives effects as ice thickness, charge size, and charge depth vary. Application of the curves to practical problems is illustrated by numerical examples. The general features of underwater explosions are reviewed and related to ice blasting. Quasi-static plate theory is considered, and is judged to be inapplicable to explosive cratering of ice plates. The specific energy for optimized ice blasting is found to compare quite favorably with the specific energy of icebreaking ships. All available field data for ice blasting are tabulated in appendices, together with details of the re­gression analyses from which the design curves are generated.
    Type of Medium: Series available for loan
    Pages: iv, 68 Seiten , Illustrationen
    Series Statement: CRREL Report 82-40
    Language: English
    Note: CONTENTS Abstract Preface Introduction General behavior of underwater explosions Regression analysis for ice-blasting data General features of the regression curves Use of the regression curves as design curves for ice blasting Row charges and pattern charges Response of floating ice sheets to underwater explosions Specific energy and “powder factor” Summary and conclusions Literature cited Appendix A: Basic data on ice blasting Appendix B: Scaled input data Appendix C: Initial regression analysis using complete polynomial Appendix D: Regression analysis with two coefficients of the original poly­nomial deleted
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  • 89
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    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-83/18
    In: CRREL Report, 83-18
    Description / Table of Contents: An evaluation of an impulse radar system for detecting cavities under concrete pavement is discussed, and field results are presented. It was found that a dual antenna mode of surveying was ideal for void detection. In this mode one antenna operated in a transceive mode and a second, offset from the first, operated in a receive-only mode. This arrangement allowed a refraction-type profile survey to be performed, which enabled subpavement voids to be easily detected. Field trails were held at Plattsburgh Air Force Base, where 28 cavities were detected and mapped. Drilling of holes verified that a cavity existed and allowed cavity depth to be measured. The cavities varied from 1.5 in. to 23 in, depth and were up to 20 ft. long.
    Type of Medium: Series available for loan
    Pages: 49 Seiten , Illustrationen
    Series Statement: CRREL Report 83-18
    Language: English
    Note: CONTENTS Abstract Preface Introduction Plattsburgh Air Force Base Radar sounding system Survey procedure Cavity inspection Radar cavity detection test Radar profile results Falling-weight deflectometer tests Discussion and conclusions Literature cited
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  • 90
    Call number: ZSP-SCAR-570-3
    In: National Antarctic Research Report to SCAR, No. 3
    Type of Medium: Series available for loan
    Pages: 16 Seiten
    ISSN: 0179-0072
    Series Statement: National Antarctic Research Report to SCAR 3
    Language: English
    Note: Contents: Membership of the National Committee on Antarctic Research in the Federal Republic of Germany. - Introduction. - Stations. - I. Record of Activities (past and ongoing), April 80-October 81. - II. Planned Activities, October 81-October 82. - References.
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  • 91
    Monograph available for loan
    Monograph available for loan
    [Erscheinungsort nicht ermittelbar] : [Verlag nicht ermittelbar]
    Call number: AWI P2-19-92186
    Type of Medium: Monograph available for loan
    Pages: 23 Seiten
    Language: English
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  • 92
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-84/17
    In: CRREL Report, 84-17
    Description / Table of Contents: VHF-band radiowave short pulses were transmitted within the permafrost tunnel at Fox, Alaska, over distances between 2.2 and 10.5 m. The propagation medium was a frozen silt containing both disseminated and massive ice with temperatures varying from -7°C near the transmitter to probably -2 C near the center of the tunnel overburden. The short pulses underwent practically no dispersion in the coldest zones but did disperse and refract through the warmer overburden, as suggested by calculations of the effective dielectric constant. Most significantly the measured frequency content decreased as the effective dielectric constant increased. The results indicate that deep, cross-borehole pulse transmissions over distances greater than 10 m might be possible, especially when the ground is no warmer than -4°C. The information thus pined could be used for identifying major subsurface variations, including ground ice features.
    Type of Medium: Series available for loan
    Pages: ii, 14 Seiten , Illustrationen
    Series Statement: CRREL Report 84-17
    Language: English
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  • 93
    Call number: ZSP-201-84/16
    In: CRREL Report, 84-16
    Description / Table of Contents: Phase composition curves are presented for a typical saline silt from Lanzhou, P.R.C., and compared to some silts from Alaska. The unfrozen water content of the Chinese silt is much higher than that of the Alaskan silts due to the large amount of soluble salts present in the silts from China, which are not present in silt from interior Alaska. When the salt is removed, the unfrozen water content is then similar for both the Chinese and Alaskan silt. Here we introduce a technique for correcting the unfrozen water content of partially frozen soils due to high salt concentrations. We calculate the equivalent molality of the salts in the unfrozen water at various temperatures from a measurement of the electrical conductivity of the extract from saturated paste.
    Type of Medium: Series available for loan
    Pages: iii, 25 Seiten , Illustrationen
    Series Statement: CRREL Report 84-16
    Language: English
    Note: Contents Abstract Preface Introduction Background Materials Sample preparation Nuclear magnetic resonance Specific surface area Electrical conductivity Results and discussion Summary Literature cited Appendix A: Unfrozen water content vs temperature data for Lanzhou silt
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  • 94
    Call number: AWI G6-19-92758
    In: 2nd Working Meeting "Radioisotope Application and Radiation Processing in Industry", Abstracts of papers
    Type of Medium: Monograph available for loan
    Pages: 167 Seiten
    Language: English
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  • 95
    Series available for loan
    Series available for loan
    Tokyo : National Institute of Polar Research
    Associated volumes
    Call number: ZSP-714-2
    In: Science in Antarctica, 2.
    Type of Medium: Series available for loan
    Pages: viii, 325 Seiten , Illustrationen , 27 cm
    ISBN: 4-7722-1285-X
    Series Statement: Science in Antarctica 2
    Language: Japanese
    Note: In japanischer Sprache
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  • 96
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-80/27
    In: CRREL Report, 80-27
    Description / Table of Contents: No general, analytical solution exists for phase change around a cylinder, thus, approximate methods have been evaluated. The heat balance integral technique applied to the cylinder gave excellent results when compared to published numerical solutions. Graphical solutions are given for phase change about a cylinder for ranges of the Stefan number, superheat parameter, and property value ratios for typical soils. An approximate, general solution has been derived which is reasonably accurate and can be used for any values of the above-mentioned parameters. The effective thermal diffusivity method has been shown to be useful for practical problems of phase change.
    Type of Medium: Series available for loan
    Pages: v, 18 Seiten , Illustrationen
    Series Statement: CRREL Report 80-27
    Language: English
    Note: CONTENTS Abstract Preface Nomenclature Introduction Zero superheat Constant phase change rate Zero sensible heat Finite sensible heat Finite superheat Quasi-steady solution Heat balance integral solution Approximate methods Conclusions Literature cited
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  • 97
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-80/25
    In: CRREL Report, 80-25
    Description / Table of Contents: Two new types of load cells for attachment to bridge piers and direct measurement of ice forces were developed and tested with one type being installed on a pier of the Yukon River Bridge northwest of Fairbanks, Alaska. Both types of load cells used beams supported by base plates and carried nose plates that were loaded by the ice. The loads were imposed at the beams at locations differing from the support reactions so that the loads developed moments in the beams. By instrumenting them with strain gauges, the loads could be measured. Details of the design of the load cells, the means of calculating the loads and experience obtained with load cells are discussed.
    Type of Medium: Series available for loan
    Pages: iii, 17 Seiten , Illustrationen
    Series Statement: CRREL Report 80-25
    Language: English
    Note: CONTENTS Preface Conversion factors Introduction Estimates and field measurements of ice forces on structures General Indirect estimates Direct measurements Small-scale and laboratory studies Instrumentation plan for measuring ice loads on the Yukon River Bridge Load cell development The single reaction beam system Performance of a single reaction beam load cell The double reation beam load cell Reaction beam design Stress in the beam Deflection Axial tensile stress in the reaction beam Measurement techniques Conclusions Literature cited Appendix A. Finding load magnitude and location with a single reaction beam device Appendix B. Finding load magnitude and location on a double reaction beam device
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  • 98
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-80/26
    In: CRREL Report, 80-26
    Description / Table of Contents: A vital concern to the survivability of hardened underground structures in rock is the relative displacement induced along geologic discontinuities by nearby explosions. Such displacement, commonly termed block motion, can occur along faults, joints, bedding planes and other structural weaknesses in rock. This report documents all occurrences of block motion observed during the development of DIHEST, a series of shallow-buried high explosive experiments designed to simulate the direct induced ground motions from a nuclear surface burst. Instances of block motion are described, along with pertinent details of the explosive arrays, geology and ground motion fields. The influence of these and other factors on the direction and magnitude of block motion is discussed.
    Type of Medium: Series available for loan
    Pages: vi, 62 Seiten , Illustrationen
    Series Statement: CRREL Report 80-26
    Language: English
    Note: CONTENTS Abstract Preface Conversion factors Introduction STARMET Test description Test results PLANEWAVE II Test description Test results DATEX II Test description Test results HANDEC II Test description Test results ROCKTEST II Test description Test results Summary and discussion Literature cited
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  • 99
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-80/24
    In: CRREL Report, 80-24
    Description / Table of Contents: The fluid shear stress applied to the underside of a simulated floating ice cover was measured in a laboratory flume. The measured values were compared with values of the shear stress computed from the von Karman-Prandtl velocity distribution fitted to the velocity profiles measured beneath the cover. For the lower velocity runs (approx 0.079 m/s) the measured and computed values of the shear stress were in close agreement. At the high velocity flows (approx 0.137 m/s) the measured values were roughly one-half those calculated from the velocity distribution. As the underside of the cover became increasingly rougher, the position of maximum velocity moved closer to the bottom of the channel. It was shown that the Darcy friction coefficient is exponentially related to a normalized ice cover thickness, which suggests that it is measure of the roughness of a fragmented ice cover.
    Type of Medium: Series available for loan
    Pages: iv, 11 Seiten , Illustrationen
    Series Statement: CRREL Report 80-24
    Language: English
    Note: CONTENTS Abstract Preface List of symbols Introduction Experimental apparatus Experimental procedures Analysis of forces Experimental results Analysis of data Conclusions Literature cited
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  • 100
    Call number: ZSP-201-80/20
    In: CRREL Report, 80-20
    Description / Table of Contents: Results of impulse radar studies of sea ice give support to the concept of a sea ice model in which the ice bottom is composed of an array of lossy parallel plate waveguides. The fundametal relation between the average bulk brine volume of sea ice and its electrical and strength properties is discussed as is the remote detection of under-ice current alignment. It was found that 1) the average effective bulk dielectric constant is dependent upon the average bulk brine volume of the sea ice; 2) sea ice anisotropy, arising from a bottom structure of crystal platelets with a preferred c-axis horizontal alignment, can be detected by radio echo sounding measurements made not only on the ice surface but also from an airborne platform; 3) the effective coefficient of reflection from the seaiIce bottom decreases with increasing average effective bulk dielectric constant of the ice, decreases with increasing bulk brine volume, and is typically one to two orders of magnitude lower dhan the coefficient of reflection from the ice surface; and 4) the losses In sea ice increase with increasing average bulk brine volume.
    Type of Medium: Series available for loan
    Pages: v, 18 Seiten , Illustrationen
    Series Statement: CRREL Report 80-24
    Language: English
    Note: CONTENTS Abstract Preface Introduction Field program Results and discussion Conclusions Literature cited Appendix: Data analysis procedures
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