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  • 1960-1964  (195)
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  • Books  (192)
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  • 1
    Monograph available for loan
    Monograph available for loan
    København : Reitzel
    Associated volumes
    Call number: ZSP-553-171,1
    In: Meddelelser om Grønland
    Type of Medium: Monograph available for loan
    Pages: 77 S. : Ill., graph. Darst., Kt.
    Series Statement: Meddelelser om Grønland 171,1
    Language: English
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  • 2
    Call number: ZSP-553-159,9
    In: Meddelelser om Grønland
    Type of Medium: Monograph available for loan
    Pages: 40 S., II Taf. : Ill., Kt.
    Series Statement: Meddelelser om Grønland 159,9
    Language: English
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  • 3
    Monograph available for loan
    Monograph available for loan
    København : Reitzel
    Associated volumes
    Call number: ZSP-553-159,11
    In: Meddelelser om Grønland
    Type of Medium: Monograph available for loan
    Pages: 74 S., XXI Taf. : zahlr. Ill.
    Series Statement: Meddelelser om Grønland 159,11
    Language: English
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  • 4
    Call number: ZSP-553-159,10
    In: Meddelelser om Grønland
    Type of Medium: Monograph available for loan
    Pages: 45 S. : Ill., Kt.
    Series Statement: Meddelelser om Grønland 159,10
    Language: English
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  • 5
    Series available for loan
    Series available for loan
    Oslo : Univ. Press [in Komm.]
    Associated volumes
    Call number: ZSP-597-123
    In: Skrifter
    In: Scientific results
    Type of Medium: Series available for loan
    Pages: 47 S
    Series Statement: Skrifter / Norsk Polarinstitutt 123
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  • 6
    Series available for loan
    Series available for loan
    Oslo : Univ. Press [in Komm.]
    Associated volumes
    Call number: ZSP-597-126
    In: Skrifter
    Type of Medium: Series available for loan
    Pages: 242 S.
    Series Statement: Skrifter / Norsk Polarinstitutt 126
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  • 7
    Call number: ZSP-597-128
    In: Skrifter
    Type of Medium: Series available for loan
    Pages: 32 S. : graph. Darst.
    Series Statement: Skrifter / Norsk Polarinstitutt 128
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  • 8
    Call number: ad ZSP-597-114
    In: Skrifter
    Type of Medium: Series available for loan
    Pages: 35 S. : Ill., graph. Darst., Kt.
    Series Statement: Skrifter / Norsk Polarinstitutt 114
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  • 9
    Call number: ZSP-597-131
    In: Skrifter
    In: Scientific results
    Type of Medium: Series available for loan
    Pages: 63 S. : Ill.
    Series Statement: Skrifter / Norsk Polarinstitutt 131
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  • 10
    Series available for loan
    Series available for loan
    London : H.M.Stat.Off.
    Associated volumes
    Call number: ZSP-164-34
    In: Scientific reports
    Type of Medium: Series available for loan
    Pages: 69 S. : Ill., graph. Darst., Kt.
    Series Statement: Scientific reports / Falkland Islands Dependencies Survey 34
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  • 11
    Series available for loan
    Series available for loan
    Associated volumes
    Call number: ZSP-164-35
    In: A magnetic survey of North-East Trinity Peninsula, Graham Land
    Description / Table of Contents: An area of about 200 square miles, covering Tabarin Peninsula and Duse Bay in the north-eastern part of the Graham Land peninsula, has been surveyed with a vertical intensity magnetometer, with the object of delineating bodies of the Andean Intrusive Suite and determining the nature of the contact between the mid-Miocene James Ross Island Volcanic Group and the ? Carboniferous sediments of the Trinity Peninsula Series. The outcrops of intrusive diorite in the northern half of Tabarin Peninsula are shown to be parts of a single intrusive body, extending over the width of the peninsula and as far south as the volcanic outcrops of Buttress Hill and Brown Bluff and northward at least as far as Mount Taylor and Blade Ridge. Three configurations of the intrusive body which explain the observed magnetic anomalies are given; the most likely from the intrusion is that of a laccolith. The magnetic anomalies over the volcanic rocks are attributed to basalt lava flows of both normal and reversed magnetizations. Some evidence is given which suggests that the James Ross Island Volcanic Group is at least 4,000 ft. thick, but it has not been possible to determine the nature of the contact between the volcanics and the sediments in southern Tabarin Peninsula or in Duse Bay.
    Type of Medium: Series available for loan
    Pages: 35 S. : Ill., graph. Darst., Kt.
    Series Statement: 35
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  • 12
    Series available for loan
    Series available for loan
    London : Brit. Antarctic Survey
    Associated volumes
    Call number: ZSP-164-36
    In: Scientific reports
    Description / Table of Contents: The geology of the Loubet Coast of Graham Land is described. The rocks are nearly all igneous and comprise mainly volcanic rocks of an Upper Jurassic age and plutonics of the Andean Intrusive Suite. The Orford Cliff Suite, a distinctive suite of intrusive rocks occurring in the Lallemand Fjord area, is believed to be early Palaeozoic in age. Undoubted pre-Upper Jurrassic intrusive rocks crop out near Detaille Island and occur as fragments in Upper Jurassic pyroclastic rocks. Rocks of the Orford Cliff Suite contain xenoliths of the Basement Complex and screens of early Palaeozoic volcanic and hypabyssal rocks. Two other phases of hypabyssal intrusion are recognized. The first forms an integral part of the Upper Jurassic vulcanicity but the second is later in age than the Andean Intrusive Suite. The sequence of intrusion in both of the plutonic suites is from femic to salic. There is some thermal metamorphism, assimilation and metasomatism of the volcanic and earlier plutonic rocks by later intrusions. Hydrothermal alteration is almost ubiquitous. Rocks of the Orford Cliff Suite have undergone intense deformation but the Upper Jurassic volcanic and the Andean intrusive rocks are little deformed. A comparison is made with the geology of adjacent regions which are very similar.
    Type of Medium: Series available for loan
    Pages: 50 S. : Ill., graph. Darst., Kt.
    Series Statement: Scientific reports / British Antarctic Survey 36
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  • 13
    Call number: ZSP-164-46
    In: Scientific reports
    Type of Medium: Series available for loan
    Pages: 43 S.
    Series Statement: Scientific reports / British Antarctic Survey 46
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  • 14
    Series available for loan
    Series available for loan
    London : Brit. Antarctic Survey
    Associated volumes
    Call number: ZSP-164-39
    In: Scientific reports
    Description / Table of Contents: A study has been made of the remanent magnetism of more than 400 samples collected from 104 localities in Graham Land and several of the nearby islands. The directions of the remanent magnetism of these samples have been measured and analysed in the standard manner. The stability of the magnetism has been investigated by tests involving the storage of specimens and their partial demagnetization in alternating magnetic fields. The study was restricted to the investigation of igneous rocks as the few sediments available for collection were found to be too weakly magnetic to be measurable. The magnetism of Tertiary and Recent lavas, collected from 12 localities, and of Andean intrusive rocks (late Cretaceous to early Tertiary age) from another 12 localities, is aligned on average along the axial gecentric dipole field direction, but both normally and reversely magnetized rocks have been found. The stability and the dispersion of magnetic directions indicate the remanent magnetism was probably acquired when the rocks were first formed. The magnetism of the Upper Jurassic Volcanic Group and the older intrusives (?Lover Palaeozoic) has been found to be either unstable or widely scattered in direction. It is suspected that the intrusion of the Andean suite so affected all the pre-existing rocks as to destroy their original magnetism. From these results it is possible to infer the condition of the Earth's past magnetic field only in connection with the Andean and younger rocks. This is that the Earth's magnetic field in the region of Graham Land has been, on average, in the same direction as the axial geocentric dipole field, or its exact reverse, since the intrusion of the Andean suite. Unfortunately there is no information from pre-Andean rocks in this area that can be used for comparison with the interesting results obtained elsewhere in Antarctica.
    Type of Medium: Series available for loan
    Pages: 24 S.
    Series Statement: Scientific reports / British Antarctic Survey 39
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  • 15
    Series available for loan
    Series available for loan
    London : British Antarctic Survey
    Associated volumes
    Call number: ZSP-164-41
    In: Scientific reports
    Description / Table of Contents: The petrology of the Argentine Islands is described in detail. The oldest rocks are lavas and pyroclastic members of the Upper Jurassic Volcanic Group which have been intruded by pre-Andean dykes and sills. The Andean Intrusive Suite has metamorphosed and metasomatized the volcanic and hypabyssal rocks. There is a later dyke phase which cuts both the volcanic and plutonic rocks; finally, there are a few late comparatively unaltered Tertiary dykes. Eight new analyses of hypabysaal rocks are included, but the composition range is too small to show conclusive trends.
    Type of Medium: Series available for loan
    Pages: 31 S. : Ill., graph. Darst., Kt.
    Series Statement: Scientific reports / British Antarctic Survey 41
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  • 16
    Call number: ZSP-164-42
    In: Scientific reports
    Type of Medium: Series available for loan
    Pages: 45 S. : Ill.
    Series Statement: Scientific reports / British Antarctic Survey 42
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  • 17
    Series available for loan
    Series available for loan
    Oslo : Univ. Press [in Komm.]
    Associated volumes
    Call number: ZSP-597-114
    In: Skrifter
    Type of Medium: Series available for loan
    Pages: 291 S. : Ill., graph. Darst., Kt. + 7 Kt.-Beil.
    Series Statement: Skrifter / Norsk Polarinstitutt 114
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  • 18
    Call number: ZSP-164-27
    In: The Geology of the South Shetland Islands
    Description / Table of Contents: Decption Island is a caldera formed by the subsidence of a group of overlapping volcanoes along arcuate and radial faults. Three volcanic episodes occured after the formation of the caldera and the location of those post-caldera volcanoes is controlled by the fault pattern which limits the caldera. Although it is possible to establish the relative ages of the four volcanic episodes, there is little information as to their absolute ages. It is probable that the latest eruptions occurred in historic times. Petrographically the Deception Island suite is a local alkaline deviation from the normal andesite-rhyolite association of the South Shetland Islands. Its lavas are characterized by an unusually high soda content. The sequence of crystallization is analogous to that of melts of certain composition in the system MgO-FeO-SiO2 crystallizing under conditions of strong fractionation. The geochemistry of the Deception Island volcanic rocks is reviewed and four new chemical analyses are presented.
    Type of Medium: Series available for loan
    Pages: 43 S. : Ill., graph. Darst., Kt. + 2 Kt.-Beil.
    Series Statement: 27
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  • 19
    Series available for loan
    Series available for loan
    Associated volumes
    Call number: ZSP-164-26
    In: The Geology of the South Shetland Islands
    Description / Table of Contents: King George Island is almost entirely composed of igneous rocks; four volcanic episodes and one intrusive phase are represented. The oldest volcanics, which are believed to be Upper Jurassic in age, form a calc-alkaline suite with an andesite-rhyolite association. Recent field investigations indicate there is no evidence for the extensive areas of sedimentary rocks previously recorded. The presence of regionally metamorphosed xenoliths in the Jurassic Volcanos indicates that they rest upon a Basement Complex. The early Tertiary Andean Intrusive Suite, which is petrographically similar to that of Graham Land, forms an axial core to the island. The majority of the Jurassic Volcanics have been metasomatized by these intrusions and the significance of the resultant secondary minerals is discussed. A linear pattern of Tertiary and Quaternary vulcanicity has been demonstrated and lavas of three distinct episodes are described. One of these volcanic groups is of unknown age, whilst the others are known to be Middle Miocene and Recent. The lavas include dominant pyroxene-andesites, basaltic andesites, olivine-basalts and rare trachyandesites. The petrogenesis of the volcanic site is discussed and crystal separation is suggested as the most important factor in their evolution. A geological map, compiled from all the available rock collections and field notes, shows the distribution of the volcanic and intrusive groups.
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    Pages: 28 S. : Ill., Kt.
    Series Statement: 26
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  • 20
    Call number: ZSP-697/B
    Former Title: Vorg. ---〉 [Rezul'taty issledovanij po mezdunarodnym geofiziceskim proektam / 9 / Gljaciologija i sejsmologija]
    Subsequent Title: Forts. ---〉 [Rezul'taty issledovanij po mezdunarodnym geofiziceskim proektam / Gljaciologiceskie issledovanija]
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  • 21
    Call number: AWI G7-83-0193
    In: Katalog dannych i publikacij po Arktike i Antarktike
    Type of Medium: Monograph available for loan
    Pages: 209 S.
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  • 22
    Call number: AWI E2-13-0068-3
    In: Materialy nabljudenij naučno-issledovatel'skich drejfujuščich stancij "Severnyj Poljus-6", "Severnyj Poljus-7" 1957/58 goda, Tom 3
    Type of Medium: Monograph available for loan
    Pages: 670 Seiten
    Series Statement: Materialy nabljudenij naučno-issledovatel'skich drejfujuščich stancij "Severnyj Poljus-6", "Severnyj Poljus-7" 1957/58 goda 3
    Language: Russian
    Note: СОДЕРЖАНИЕ = Soderžanie = Table of Contents. - Предисловие = Predislovie = Foreword. - Аэрология = Aėrologija = Aerology. - Методика и результаты аэрологических наблюдений = Metodika i rezul'taty aėrologičeskich nabljudenij = Method and results of upper-air observations. - Таблица 1. Географические координаты станций = Tablica 1. Geografičeskie koordinaty stancij = Table 1. Geographical coordinates of stations. - Таблица 2. Среднее месячное давление = Tablica 2. Srednee Mesjačnoe davlenie = Table 2. Average monthly pressure. - Таблица 3. Средняя месячная высота и температура изобарических поверхностей = Tablica 3. Srednjaja mesjačnaja vysota i temperatura izobaričeskich poverchnostej = Table 3. Average monthly height and temperature of isobaric surfaces. - Таблица 4. Средняя месячная плотность воздуха = Tablica 4. Srednjaja mesjačnaja plotnost' vozducha = Table 4. Average monthly air density. - Таблица 5. Средняя месячная температура = Tablica 5. Srednjaja mesjačnaja temperatura = Table 5. Average monthly temperature. - Таблица 6. Максимальная температура = Tablica 6. Maksimal'naja temperatura = Table 6. Maximum temperature. - Таблица 7. Минимальная температура = Tablica 7. Minimal'naja temperatura = Table 7. The minimum temperature. - Таблица 8. Средняя высота изотермических поверхностей = Tablica 8. Srednjaja vysota izotermičeskich poverchnostej = Table 8. The average height of isothermal surfaces. - Таблица 9. Повторяемость высоты нижней границы инверсий и изотермий и числа дней с инверсиями и изотермиями = Tablica 9. Povtorjaemost' vysoty nižnej granicy inversij i izotermij i čisla s inversijami i izotermijami = Table 9. Repeatability of the height of the lower boundary of inversions and isotherms and the number of days with inversions and isotherms Таблица 10. Средняя мощность инверсий и изотермий = Tablica 10. Srednjaja moščnost' inversij i izotermij = Table 10. The average power of inversions and isotherms. - Таблица 11. Средняя интенсивность инверсий и изотермий = Tablica 11. Srednaja intensivnost' inversij i izotermij = Table 11. The average intensity of inversions and isotherms. - Таблица 12. Средняя высота и температура нижней границы тропопаузы = Tablica 12. Srednjaja vysota i temperatura nižnej granicy tropopauzy = Table 12. The average height and temperature of the lower border of the tropopause. - Таблица 13. Повторяемость высоты нижней границы тропопаузы = Tablica 13. Povtorjaemost' vysoty nižnej granicy tropopauzy = Table 13. Repeatability of the height of the lower tropopause border. - Таблица 14. Повторяемость температуры нижней границы тропопаузы = Tablica 14. Povtorjaemost' temperatury nižnej granicy tropopauzy =Table 14. Repeatability of temperature of the lower tropopause border. - Таблица 15. Средняя месячнан относительная влажность = Tablica 15. Srednjaja mesjačnan otnositel'naja vlažnost' = Table 15. Average monthly relative humidity. - Таблица 16. Средняя месячная удельная влажность = Tablica 16. Srednjaja mesjačnaja udel'naja vlažnost' = Table 16. Average monthly specific humidity. - Таблица 17. Средняя высота нижней границы облаков = Tablica 17. Srednaja vysota nižnej granicy oblakov = Table 17. The average height of the lower boundary of the clouds. - Таблица 18. Средняя месячная скорость ветра = Tablica 18. Srednjaja mesjačnaja skorost' vetra = Table 18. Average monthly wind speed. - Таблица 19. Максимальная скорость ветра = Tablica 19. Maksimal'naja skorost' vetra = Table 19. Maximum wind speed. - Таблица 20. Повторяемость направления ветра = Tablica 20. Povtorjaemost' napravlenija vetra = Table 20. Wind direction repeatability. - Таблица 21. Результаты температурно-ветрового зондирования атмосферы = Tablica 21. Rezul'taty temperaturno-vetrovogo zondirovanija atmosfery = Table 21. Results of temperature-wind sounding of the atmosphere. - , In kyrillischer Schrift
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  • 23
    Series available for loan
    Series available for loan
    Tokyo : Polar Section, National Science Museum
    Associated volumes
    Call number: ZSP-594/E-23
    In: Japanese Antarctic research expedition
    Type of Medium: Series available for loan
    Pages: 14 S. : Ill.
    Series Statement: Japanese Antarctic research expedition : Scientific Reports Series E, Biology 23
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  • 24
    Series available for loan
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    Tokyo : Polar Section, National Science Museum
    Associated volumes
    Call number: ZSP-594/E-21
    In: Japanese Antarctic research expedition
    Type of Medium: Series available for loan
    Pages: 16 S.
    Series Statement: Japanese Antarctic research expedition : Scientific Reports Series E, Biology 21
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  • 25
    Series available for loan
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    Sirahama, Wakayama-ken : Seto Marine Biological Laboratory
    Associated volumes
    Call number: ZSP-594/E-15
    In: Biological results of the Japanese Antarctic Research Expedition
    Type of Medium: Series available for loan
    Pages: 10 S. : Ill., graph. Darst.
    Series Statement: Biological results of the Japanese Antarctic Research Expedition 15
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  • 26
    Series available for loan
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    Sirahama, Wakayama-ken : Seto Marine Biological Laboratory
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    Call number: ZSP-594/E-13
    In: Biological results of the Japanese Antarctic Research Expedition
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    Pages: 7 S. : Ill.
    Series Statement: Biological results of the Japanese Antarctic Research Expedition 13
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  • 27
    Series available for loan
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    Sirahama, Wakayama-ken : Seto Marine Biological Laboratory
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    Call number: ZSP-594/E-10
    In: Biological results of the Japanese Antarctic Research Expedition
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    Pages: 176 S. : Ill.
    Series Statement: Biological results of the Japanese Antarctic Research Expedition 10
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  • 28
    Series available for loan
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    Tokyo : Polar Section, National Science Museum
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    Call number: ZSP-594/E-20
    In: Japanese Antarctic research expedition
    Type of Medium: Series available for loan
    Pages: 10 S.
    Series Statement: Japanese Antarctic research expedition : Scientific Reports : Series E, Biology 20
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  • 29
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    Tokyo : Polar Section, National Science Museum
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    Call number: ZSP-594/C-2
    In: Japanese Antarctic Research Expedition
    Description / Table of Contents: The East Ongul Island on the coast of the Lutzow-Holm Bukt, East Antarctica, was investigated from the tectonical and petrographical points of view. The rocks exposed in the island are petrographically classified into the following seven types : 1) Metabasites, 2) Pyroxene gneisses, 3) Hornblende gneisses, 4) Garnet gneisses, 5) Granites, 6) Feldspathic rocks, and 7) Pegmatites. It is verified that the unique structural feature of the island is represented by the isoclinal fold recumbent to the west with the frontal zone in which many small anticlinal as well as synclinal folds occur. The inner core of the main anticline is generally composed of the garnet gneisses with the pyroxene gneisses forming the outer mantle. The hornblende gneisses, which are distributed in front of the recumbent anticline, occur in the same horizon as the pyroxene gneiss, so the former may have been converted from the latter. This is also confirmed by the geological and petrographical observations. Besides, the hornblende gneiss zone coincides with the zone of granite and subsequent microcline pegmatite emplacement. The lineation of the rocks, represented by the undulating foliation, is defined to be a b-lineation parallel to the fold axis, but another lineation with the same character but perpendicular to the fold axis is also found. The fracture systems indicated by the pegmatite and joint patterns were analyzed by tectonic dating. The pegmatite intruded at the earlier folding stage, whereas the joint pattern was formed at the later upwarping stage. The gneisses and granites are classified mainly by the characteristic mafic minerals, and their modes of occurrence as well as the optical mineralogy are described. The optical data of the constituent minerals revealed that there is a tendency that the Fe/Mg ratio of the mafic minerals such as pyroxene, hornblende, biotite and garnet, may increase with acidity of the rocks, from the matabasites to the granites. The anorthite content of plagioclase is restricted within a rather narrow range between 22% and 35% when feldspar coexists with potash-feldspar, although that of plagioclase in metabasite and basic enderbitic pyroxene gneiss free from potash-feldspar ranges widely from 42% to 93%. The triclinicity of the potash-feldspar may become higher in the granite than the gneisses judging from the data of their 2V values. It is probable that the gneisses were formed originally under the condition of a granulite facies in the regional metamorphism. At the same time, the widespread developement of hornblende and biotite in the metabasites and gneisses suggests subsequent changes in temperature and pressure or the presence of water as well as changes in chemical composition which facilitated the mobilization and plastic deformation of the rocks. It is considered that two phases of metamorphism may be detected in the area; the granulite facies at an earlier phase and the amphibolite facies at a later phase. This has been suggested by the investigations not only in other regions of the East Antarctica but also in other Precambrian shields of the world.
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    Pages: 24 S.
    Series Statement: Japanese Antarctic Research Expedition : Scientific reports : Series C, Geology 2
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  • 30
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    Sirahama, Wakayama-ken
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    Call number: ZSP-594/E-17
    In: Biological results of the Japanese Antarctic Research Expedition
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    Pages: 6 S. : Ill.
    Series Statement: Biological results of the Japanese Antarctic Research Expedition 17
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  • 31
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    Sirahama, Wakayama-ken : Seto Marine Biological Laboratory
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    Call number: ZSP-594/E-14
    In: Biological results of the Japanese Antarctic Research Expedition
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    Pages: 9 S. : Ill.
    Series Statement: Biological results of the Japanese Antarctic Research Expedition 14
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  • 32
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    Sirahama, Wakayama-ken : Seto Marine Biological Laboratory
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    Call number: ZSP-594/E-12
    In: Biological results of the Japanese Antarctic Research Expedition
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    Pages: 20 S. : Ill., graph. Darst.
    Series Statement: Biological results of the Japanese Antarctic Research Expedition 12
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  • 33
    Call number: ZSP-594/C-1
    In: Japanese Antarctic Research Expedition
    Description / Table of Contents: The chemical compositions of constituent minerals of metamorphic rocks of the area around Lutzow-Holm Bay in Antarctica are described along with their optic properties. The mineralogy and paragenesis of metamorphic rocks are interpreted as that the metamorphic rocks in this terrane belong to the granulite facies.
    Type of Medium: Series available for loan
    Pages: 12 S.
    Series Statement: Japanese Antarctic Research Expedition : Scientific reports : Series C, Geology 1
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  • 34
    Series available for loan
    Series available for loan
    London : H.M.Stat.Off.
    Associated volumes
    Call number: ZSP-164-24
    In: Scientific reports
    Description / Table of Contents: Recent collections of decapod crustaceans and serpulid worms from the Upper Cretaceous of James Ross Island have facilitated the re-description of three species previously recorded from the area and have contributed four new species. The decapods include Hoploparia stokesi (Weller), Meyeria crofti sp. nov. and Callianassa meridionalis sp. nov., and the serpluids Rotularia callosa (Stoliczka), Rotularia shackletoni (Wilckens), Rotularia dorsolaevis sp. nov. and Ditrupa varicosa sp. nov. The diagnosis of the subfamily Homarinae Mertin, 1941 is amended and observations are made on the taxonomic position and stratigraphical range of the genus Meyeria. In addition, the structure of the tube-wall of the genera Rotularia Defrance, 1827 and Ditrupa Berkeley, 1832-34, and their stratigraphical range are discussed. The age of the fauna is shown by associated ammonites to be of Lower to Middle Campanian age.
    Type of Medium: Series available for loan
    Pages: 30 S., 7 Bl. : Ill., graph. Darst., Kt.
    Series Statement: Scientific reports / Falkland Islands Dependencies Survey 24
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  • 35
    Series available for loan
    Series available for loan
    London : British Antarctic Survey
    Associated volumes
    Call number: ZSP-164-43
    In: Scientific reports
    Description / Table of Contents: The general stratigraphy of the Neny Fjord area of Marguerite Bay is described with specific reference to the Basement Complex metamorphic rocks. The scattered nature of the rock outcrops in this area precludes far-reaching petrological correlations and a form of metamorphic correlation has been used. The Basement Complex rocks have been subdivided into three major groups: banded biotite-gneisses, dioritic gneisses and granite-gneisses, of which the latter two groups are undoubtedly ortho-gneisses. The banded biotite-gneisses, which are the oldest and are believed to be of a sedimentary origin, formed a basement into which the dioritic gneisses and the granite-gneisses were successively intruded later. After the further intrusion of a series of basic dykes, metamorphism , potash metasomatism and local mobilization of the granite-gneisses took place. This metamorphism reached the lower stages of the almandine-amphibolite facies, and after the intrusion of a second group of basic rocks there followed another metamorphism of the albite-epidote-amphibolite facies. During the intrusion of the (?) early Palaeozoic plutonic rocks, the Basement Complex was locally mobilized, but when the Andean Intrusive Suite was emplaced the Basement Complex was rigid and block-faulting occurred in this area. At Randall Rocks the contact metamorphic aureole aurrounding the Andean biotite-granite has been traced in the granite-gneiss. A major fault line which passes through Roman Four Promontory, Neny Island and Millerand Island subdivides this whole area into two distinct petrological parts.
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    Pages: 49 S.
    Series Statement: Scientific reports / British Antarctic Survey 43
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  • 36
    Series available for loan
    Series available for loan
    Associated volumes
    Call number: ZSP-138-4,1 ; ZSP-138-4,2
    In: Antarktika
    Type of Medium: Series available for loan
    Pages: 174 S. : Ill., graph. Darst.
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  • 37
    Call number: ZSP-697/B
    Parallel Title: 2=2; 3=3; 10=5a von [Rezul'taty issledovanij po mezdunarodnym geofiziceskim proektam / 12 / Sejsmologiceskie issledovanija]
    Subsequent Title: Forts. ---〉 [Rezul'taty issledovanij po mezdunarodnym geofiziceskim proektam / Gljaciologija]
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  • 38
    Monograph available for loan
    Monograph available for loan
    Associated volumes
    Call number: AWI G7-92-0551
    In: Gljaciologiceskie issledovanija v period MGG
    Type of Medium: Monograph available for loan
    Pages: 233 S. : Ill., Kt.
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  • 39
    Call number: AWI E2-13-0068-2
    In: Materialy nabljudenij naučno-issledovatel'skich drejfujuščich stancij "Severnyj Poljus-6", "Severnyj Poljus-7" 1957/58 goda, Tom 2
    Type of Medium: Monograph available for loan
    Pages: 653 Seiten
    Series Statement: Materialy nabljudenij naučno-issledovatel'skich drejfujuščich stancij "Severnyj Poljus-6", "Severnyj Poljus-7" 1957/58 goda 2
    Language: Russian
    Note: СОДЕРЖАНИЕ = Soderžanie = Contents: Предисловие = Predislovie = Foreword. - Метеорология = Meteorologija = Meteorology. - Метеорологические наблюдения = Meteorologičeskie nabljudenija = Meteorological observations. - Таблицы = Tablicy = Tables. - Актинометрия = Aktinometrija = Actinometry. - Актинометрические наблюдения = Aktinometričeskie nabljudenija = Actinometric observations. - Некоторые результаты наблюдений = Nekotorye rezul'taty nabljudenij = Some results of observations. - Таблицы = Tablicy = Tables. - , In kyrillischer Schrift
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  • 40
    Series available for loan
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    Call number: ZSP-594/E-18
    In: Variations on some pennate diatoms from Antarctica
    Type of Medium: Series available for loan
    Pages: 20 S. : Ill., graph. Darst.
    Series Statement: 18
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  • 41
    Series available for loan
    Series available for loan
    Tokyo : Polar Section, National Science Museum
    Associated volumes
    Call number: ZSP-594/E-19
    In: Japanese Antarctic research expedition
    Type of Medium: Series available for loan
    Pages: 41 S. : Ill.
    Series Statement: Japanese Antarctic research expedition : Scientific Reports : Series E, Biology 19
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  • 42
    facet.materialart.
    Unknown
    Oslo : Norsk Polarinstitutt
    Call number: K-13-0038
    Pages: 1 Kt. in 4 Bl. ; 86 x 251 cm., sheets 66 x 79 cm or smaller
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  • 43
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    Associated volumes
    Call number: AWI G7-92-0552
    In: Gljaciologiceskie issledovanija v period MGG
    Type of Medium: Monograph available for loan
    Pages: 208 S.
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  • 44
    Call number: AWI E2-13-0068-4
    In: Materialy nabljudenij naučno-issledovatel'skich drejfujuščich stancij "Severnyj Poljus-6", "Severnyj Poljus-7" 1957/58 goda, Tom 4
    Type of Medium: Monograph available for loan
    Pages: 607 Seiten
    Series Statement: Materialy nabljudenij naučno-issledovatel'skich drejfujuščich stancij "Severnyj Poljus-6", "Severnyj Poljus-7" 1957/58 goda 4
    Language: Russian
    Note: СОДЕРЖАНИЕ = Soderžanie = Contents: Предисловие = Predislovie = Foreword. - Геофизина = Geofizika = Geophysics. - Ионосферные наблюдения = Ionosfernye nabljudenija = Ionospheric observations. - Таблица. Ионосферные данные = Tablica. Ionosfernye dannye = Table. Ionospheric data. - Магнитные наблюдения = Magnitnye nabljudenija = Magnetic observations. - Таблица 1. Ежечасные значения магнитных элементов D, Н, Z = Tablica 1. Ežečasnye značenija magnitnych ėlementov D, H, Z = Table 1. Hourly values of the magnetic elements D, H, Z. - Таблица 2. Ежечасные значения амплитуд горизонтальной составляющей rγH = Tablica 2. Ežečasnye značenija amplitud gorizontal'noj sostavljajuščej rγH = Table 2. Hourly values of amplitudes of the horizontal component rγH. - Таблица 3. Наблюденные значения магнитных элементов D, Н, Z = Tablica 3. Nabljudennye značenija magnitnych ėlementov D, H, Z = Table 3. Observed values of the magnetic elements D, H, Z. , In kyrillischer Schrift
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  • 45
    Call number: AWI G7-84-0845
    In: Katalog dannych i publikacij po Arktike i Antarktike
    Type of Medium: Monograph available for loan
    Pages: 265 S.
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  • 46
    Monograph available for loan
    Monograph available for loan
    Canada : Directorate of Scientific Information Services
    Call number: AWI G9-84-1168
    Type of Medium: Monograph available for loan
    Pages: 2, iii S. : Ill., Kt.
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  • 47
    Series available for loan
    Series available for loan
    New York : IGY World Data Center A, Glaciology
    Associated volumes
    Call number: AWI G7-85-0723
    In: IGY Glaciological Report
    Type of Medium: Series available for loan
    Pages: xiv, 197 p. : Ill.
    Series Statement: IGY Glaciological Report 5
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  • 48
    Call number: AWI G2-13-0066
    In: Ergebnisse der Limnologie
    Type of Medium: Series available for loan
    Pages: 90 Seiten , Illustrationen
    Series Statement: Ergebnisse der Limnologie 1
    Language: German
    Note: Inhaltsübersicht: A. Die Problemstellungen. - B. Überblick über die geomorphologische Entwicklung des Ostseeraumes. - 1. Der Baltische Schild und die ihn flankierenden Depressionen. - 2. Die Entwicklung des Ostseebeckens im Quartär. - I. Die Faktoren, die entscheidend die Morphologie Nordeuropas mitgestalteten. - II. Der Anteil der Weichsel-(Würm-)Vereisung an der morphologischen Formung. - III. Interglaziale Meerestransgressionen im Ostseeraum; Entwicklungsphasen der Ostsee im Spät- und Postglazial. - C. Eisstauseen des eurasischen Vergletscherungsgebietes als wesentliche Elemente des Smmelzwasserstromnetzes vor der Front des pleistozänen Inlandeises. - 1. Die Eisstauseen. - a) Im Gebiete des nordwesteuropäischen Kontinentalschelfes; die Reliktvorkommen in Großbritannien und Irland. - b) Entwicklungsgeschichte und Charakter des Südbaltischen Eisstausees. - c) Weichselzeitliche Stauseebildungen im Bereiche des Baltischen Landrückens. - d) Der Eisstausee im oberen Onega-Tal. - e) Das Becken des Weißen Meeres und seine Randgebiete. - f) Eisstauseen im östlichen Eurasien. - 2. Die Bedeutung der Lage und Verbreitung der Eisstauseen für die Lösung des Problems. - 3. Die Wasserscheiden im Raume des einstigen Pommersehen Stadiums und seines Hinterlandes. - 4. Die Abflußverhältnisse vor der Front des Inlandeises. - 5. Die Bedeutung der Richtung der Rückzugsbewegung des nordeuropäischen Inlandeises auf die Eiszentren in Fennoskandia. - D. Einwanderungsmöglichkeiten von Faunenelementen des Nördlichen Eismeeres in den Südbaltischen Eisstausee und in Binnengewässer Mittel- und Nordeuropas. - 1. Übersicht. - 2. Einwanderungsmöglichkeiten auf westlichen Wegen. - I. Der südwestliche Weg zwischen Jütland und Südschweden. - II. Die West-Ost-Verbindung vom Skagerrak-Kattegat über die mittelschwedischen Seen zum Ostseebecken. - 3. Einwanderungsmöglichkeiten auf östlichen Wegen. - I. Der nordöstliche Weg vom Weißen Meer über den Onega- und Ladoga-See zum Finnischen Meerbusen. - lI. Der Weg von der Kandalakscha-Bucht des Weißen Meeres zum Finnischen Meerbusen. - III. Der nordöstliche Weg unter Benutzung von Eisstauseen im Bereiche des Baltischen Landrückens und in den Küstenbezirken des Weißen Meeres. - a) Die Bedeutung der Brackwasser-Transgression beim Vorrücken der Kola- und Nowaja-Semlja-Gletscher. - b) Die Bedeutung des Langelancl-Vorstoßes für die Bildung von Eisstauseen und für die Hochschleusung von Reliktpopulationen aus dem Südbaltischen Eisstausee. - IV. Der Weg durch das Europäische Nordmeer entlang der norwegischen Küste zur Nord- und Ostsee. - 4. Der Einwanderungsweg von Pallasea quadrispinosa G. O. SARS. - E. Eisstauseen auf dem nordamerikanischen Kontinent und ihre Bedeutung für die Verbreitung mariner Glazialrelikte. - F. Die Vorkommen mariner Glazialrelikte an der Ostküste Gränlands. - G. Die Lebensmöglichkeiten während der weichselzeitlichen Rückzugsphasen. - H. Anlagen: I. Die Hauptstadien der Weichsel-Vereisung (Waldai-Vereisung der sowjetisehen Autoren) in Mittel- und Osteuropa. - II. Das nordamerikanische Vergletscheru:ngsgebiet: die Laurentische Inlandeisdecke. - III. Übersicht über die Hauptgliederung des Pleistozäns in Eurasien und Nordamerika. - I. Zusammenfassung. - K. Résumé. - L. Summary. - M. Schriftenverzeichnis (Auswahl).
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  • 49
    Call number: ZSP-594/E-16
    In: Biological results of the Japanese Antarctic Research Expedition
    Type of Medium: Series available for loan
    Pages: 8 S. : Ill.
    Series Statement: Biological results of the Japanese Antarctic Research Expedition 16
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  • 50
    Series available for loan
    Series available for loan
    Tokyo : Polar Section, National Science Museum
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    Call number: ZSP-594/A-2
    In: Japanese Antarctic Research Expedition
    Type of Medium: Series available for loan
    Pages: 38 S.
    Series Statement: Japanese Antarctic Research Expedition : Scientific reports : Series A, Aeronomy 2
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  • 51
    Series available for loan
    Series available for loan
    Sirahama, Wakayama-ken : Seto Marine Biological Laboratory
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    Call number: ZSP-594/E-11
    In: Biological results of the Japanese Antarctic Research Expedition
    Type of Medium: Series available for loan
    Pages: 10 S. : Ill.
    Series Statement: Biological results of the Japanese Antarctic Research Expedition 11
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  • 52
    Series available for loan
    Series available for loan
    Tokyo : Polar Section, National Science Museum
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    Call number: ZSP-594/F-1 ; ZSP-594/F-1(2. Ex.)
    In: Japanese Antarctic Research Expedition
    Type of Medium: Series available for loan
    Pages: 12 S. : Ill.
    Series Statement: Japanese Antarctic Research Expedition : Scientific reports : Series F, Logistics 1
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  • 53
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    Tokyo : Polar Section, National Science Museum
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    Call number: ZSP-594/E-22
    In: Japanese Antarctic research expedition
    Type of Medium: Series available for loan
    Pages: 20 S. : Ill.
    Series Statement: Japanese Antarctic research expedition : Scientific Reports : Series E, Biology 22
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  • 54
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    Tokyo : Polar Section, National Science Museum
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    Call number: ZSP-594/A-1
    In: Japanese Antarctic Research Expedition
    Type of Medium: Series available for loan
    Pages: 82 S. : graph. Darst.
    Series Statement: Japanese Antarctic Research Expedition : Scientific reports : Series A, Aeronomy 1
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  • 55
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    Tokyo : Polar Section, National Science Museum
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    Call number: ZSP-594/D-1
    In: Japanese Antarctic Research Expedition
    Type of Medium: Series available for loan
    Pages: 12 S.
    Series Statement: Japanese Antarctic Research Expedition : Scientific reports : Series D, Oceanography 1
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  • 56
    Series available for loan
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    Hanover, NH
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    Call number: ZSP-204-103
    In: CRREL Technical Report
    Type of Medium: Series available for loan
    Pages: vi, 13 S. : Ill., graph. Darst., Kt.
    Series Statement: CRREL Technical Report 103
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  • 57
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    Mannheim : Bibliograph. Inst.
    Call number: AWI S5-92-0353
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    Language: German
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  • 58
    Call number: ZSP-204-121
    In: CRREL Technical Report
    Type of Medium: Series available for loan
    Pages: iii, [81] S. : zahlr. graph. Darst.
    Series Statement: CRREL Technical Report 121
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  • 59
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    Hanover, NH
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    Call number: ZSP-204-104
    In: CRREL Technical Report
    Type of Medium: Series available for loan
    Pages: vi, 15 S. : Ill., graph. Darst., Kt.
    Series Statement: CRREL Technical Report 104
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  • 60
    Call number: ZSP-553-164,6 ; AWI P8-88-0281
    In: Meddelelser om Grønland
    Type of Medium: Monograph available for loan
    Pages: 105 S., 4 Taf. : Ill., Kt.
    Series Statement: Meddelelser om Grønland 164,6
    Language: English
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  • 61
    Call number: ZSP-553-163,6
    In: Meddelelser om Grønland
    Type of Medium: Monograph available for loan
    Pages: 64 S., V Taf. : Ill.
    Series Statement: Meddelelser om Grønland 163,6
    Language: English
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  • 62
    Call number: ZSP-204-78
    In: CRREL Technical Report
    Type of Medium: Series available for loan
    Pages: iv, 12 S. : graph. Darst.
    Series Statement: CRREL Technical Report 78
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  • 63
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    Hanover, NH
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    Call number: ZSP-204-102
    In: CRREL Technical Report
    Type of Medium: Series available for loan
    Pages: vi, 14 S. : Ill., graph. Darst., Kt.
    Series Statement: CRREL Technical Report 102
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  • 64
    Call number: ZSP-204-97
    In: CRREL Technical Report
    Type of Medium: Series available for loan
    Pages: iv, 56 S.
    Series Statement: CRREL Technical Report 97
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  • 65
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    Hanover, NH
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    Call number: ZSP-204-106
    In: CRREL Technical Report
    Type of Medium: Series available for loan
    Pages: vi, 13 S. : Ill., graph. Darst., Kt.
    Series Statement: CRREL Technical Report 106
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  • 66
    Monograph non-lending collection
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    Hanover, NH
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    Call number: ZSP-204-80
    In: CRREL Technical Report
    Type of Medium: Monograph non-lending collection
    Pages: iv, 6 S. : Ill., graph. Darst.
    Series Statement: CRREL Technical Report 80
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  • 67
    Monograph available for loan
    Monograph available for loan
    Associated volumes
    Call number: M 93.0087/1 ; AWI G2-96-0026 ; MOP 34194
    In: The sea ; 1, Vol. 1
    Type of Medium: Monograph available for loan
    Pages: xv, 864 S. , Ill., graph. Darst., Kt.
    Edition: 1. publ.
    Language: English
    Note: CONTENTS: PHYSICAL OCEANOGRAPHY. - SECTION I. FUNDAMENTALS. - 1. PHYSICAL PROPERTIES OF SEA-WATER / BY N. P. FOFONOFF. - 1. The equilibrium thermodynamic state. - 2. Equation of state for sea-water. - 3. Entropy. - 4. Chemical potential difference. - 5. The non-equilibrium state. - 6. Other physical properties of sea-water. - 2. THE EQUATIONS OF MOTION OF SEA-WATER / BY CARL ECKART. - 1. Introduction. - 2. Thermodynamics. - 3. Hydrodynamics. - 4. The irreversible processes. - 5. Transformation of the equation. - 6. The zeroth approximation. - 7. The first approximation. - 8. Definitions related to convective motion. - 9. The field equations. - SECTION II. INTERCHANGE OF PROPERTIES BETWEEN SEA AND AIR. - 3. SMALL-SCALE INTERACTIONS / BY E. L. DEACON AND E. K. WEBB. - 1. General considerations of transfer. - 2. Momentum transfer and the wind-profile. - 3. Drag coefficients of the sea surface. - 4. Transfer of heat and water vapour. - 4. LARGE-SCALE INTERACTIONS / BY JOANNE S. MALKUS. - 1. Introduction. - 2. How the whole system works. - 3. Determination of air-sea fluxes. - 4. Climatology of energy exchange and the global heat and water budgets. - 5. Heat and water exchange and its role in tropical circulations. - 6. Large-scale momentum relations. - 7. Exchange mechanisms and fluctuations. - 8. Exchange fluctuations in mid-latitudes and long-period interaction anomalies. - 9. Concluding remarks. - 5. INSOLUBLES / BY R. W. REX AND E. D. GOLDBERG. - 1. Meteorology of transport. - 2. Eolian materials in marine sediments. - 6. SOLUBLES / BY A. H. WOODCOCK. - 7. GASES / BY R. REVELLE AND H. E. SUESS. - 1. Introduction. - 2. Oxygen and nitrogen. - 3. Rare gases. - 4. Carbon dioxide. - SECTION III. DYNAMICS OF OCEAN CURRENTS / BY N. P. FOFONOFF. - 1. Conservation equations for momentum and mass. - 2. Separation into steady and time-dependent motion. - 3. Magnitude of forces. - 4. Steady-state circulation. - 5. Steady inertial circulation. - 6. Convective circulation. - 7. Time-dependent motion. - SECTION IV. TRANSMISSION OF ENERGY WITHIN THE SEA. - 8. LIGHT / BY J. E. TYLER AND R. W. PREISENDORFER. - 1. Physical constructs. - 2. Instrumentation for the measurement of the underwater light field and the determination of the optical properties of the sea. - 3. Radiance distribution. - 4. Attenuation coefficient. - 5. Volume scattering functions and total scattering coefficient. - 6. Irradiance. - 7. Diffuse attenuation function and reflectance function. - 8. Scalar irradiance (spherical irradiance). - 9. Absorption coefficient. - 10. Path function. - 11. Data. - 12. Applications. - 13. List of symbols. - 9. UNDERWATER VISIBILITY / BY S. Q. DUNTLEY. - 1. Image transmission. - 2. Inherent contrast. - 3. Sighting range. - 10. LIGHT AND ANIMAL LIFE / BY G. L. CLARKE AND E. J. DENTON. - 11. OTHER ELECTROMAGNETIC RADIATION / BY L. N. LIEBERMANN. - 1. Introduction. - 2. Electromagnetic properties of sea-water. - 3. Propagation through sea-water. - 4. The effect of the sea-surface on electromagnetic propagation. - 5. Natural electromagnetic radiation or "noise" in the sea. - 12. SOUND IN THE SEA / BY P. VIGOUREUX and J. B. HERSEY. - 1. The nature of sound. - 2. Propagation of sound in water. - 3. Noise. - 4. Instruments and applications of sound to oceanography. - 13. SOUND SCATTERING BY MARINE ORGANISMS / BY J. B. HERSEY AND R. H. BACKUS. - 1. Introduction. - 2. Occurrence and description of scattering layers. - 3. Identification of sound scatterers. - 4. Sound-scattering theory. - 5. Sound-scattering observations. - 6. What is "the deep scattering layer"?. - 7. Ideas and miscellaneous observations. - 14. SOUND PRODUCTION BY MARINE ANIMALS / BY W. E. SCHEVILL, R. H. BACKUS, AND J. B. HERSEY. - 1. Introduction. - 2. History. - 3. Instrumentation. - 4. Identification of source. - 5. Purposeful and adventitious sounds. - 6. Sound-producing mechanisms. - 7. Spectra of sounds. - 8. Functions of sound. - 9. Hearing as related to sound production. - 10. Eliciting and suppressing marine animal sounds. - 11. Exploitation of marine animal sounds by the oceanographer. - SECTION V. WAVES. - 15. ANALYSIS AND STATISTICS / BY D. E. CARTWRIGHT. - 1. Introduction. - 2. Fundamental equations of wave motion. - 3. Statistical formulation. - 4. Properties of a wave system in terms of its directional energy spectrum. - 5. Estimating the directional energy spectrum. - 6. Waves recorded by a single detector. - 7. Spectral measurement. - 8. Second-order approximations to energy spectra. - 16. LONG-TERM VARIATIONS IN SEA-LEVEL / BY J. R. ROSSITER. - 1. Introduction. - 2. The determination of mean sea-level. - 3. Causes of variations in sea-level. - 4. The analysis of observations. - 5. Some geophysical implications of long-term variations in sea-level. - 6. Conclusion. - 17. SURGES / BY P. GROEN AND G. W. GROVES. - 1. Introduction. - 2. Description. - 3. Dynamics and forecasting. - 18. LONG OCEAN WAVES / BY W. H. MUNK. - 1. Introduction. - 2. The instruments. - 3. The spectrum. - 4. Surf beat. - 5. Shelf waves. - 6. Tsunamis. - 19. WIND WAVES / BY N. F. BARBER AND M. J. TUCKER. - 1. Kinematics of waves. - 2. The description of a complicated wave pattern: the wave spectrum. - 3. Theories of wave generation by wind. - 4. Wave prediction. - 5. Waves from distant storms. - 6. Waves approaching the shore. - 7. The surf zone. - 8. Ships and waves. - 9. Methods of observation and analysis-methods taking no account of direction of travel. - 10. Methods of observation and analysis - the directional power spectrum. - 20. MICROSEISMS / BY J. DARBYSHIRE. - 1. Relation between sea waves and microseisms. - 2. The nature of microseisms. - 3. Refraction of microseisms. - 4. Storm tracking and estimation of the direction of approach of microseisms. - 5. Estimation of direction from the nature of microseisms. - 6. Instruments. - 7. Other work. - 21. RIPPLES / BY C. S. COX. - 1. Spectrum and mean square slope. - 2. Effect of slicks. - 3. Shape of a rippled water surface. - 4. Growth of ripples. - 22. INTERNAL WAVES : Part I / BY E. C. LAFOND. - 1. Introduction. - 2. Measurements. - 3. Observed relations. - 22. INTERNAL WAVES : Part II / BY C. S. COX. - 4. Differential equations. - 5. Spectrum. - 6. Internal waves and turbulence. - 23. TIDES / BY W. HANSEN. - 1. Introduction. - 2. The hydrodynamic equations and their application to tidal problems. - 3. Tidal observation. - 4. Tidal charts. - 5. Classical theory. - 6. Numerical methods for ascef!.aining the tides and tidal currents. Boundary-value problems. - 7. The application of difference methods to initial-boundary problems. - 8. Numerical solutions of initial-boundary-value problems of tides in one and two dimensions. - 9. Internal tides. - SECTION VI. TURBULENCE / BY K. F. BOWDEN. - 1. General properties of turbulence. - 2. Turbulence in the sea. - 3. Turbulent fluctuations and turbulent transports. - 4. Vertical turbulence. - 5. Horizontal turbulence. - SECTION VII. THE PHYSICS OF SEA-ICE / BY E. R. POUNDER. - 1. Introduction. - 2. Mechanical properties. - 3. Thermal properties. - 4. Electrical properties. - 5. Growth and disintegration of an ice cover. - 6. Theory of sea-ice structure and properties. - AUTHOR INDEX. - SUBJECT INDEX.
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  • 68
    Call number: M 93.0087/2 ; AWI G2-96-0027
    In: The sea ; 2, Vol. 2
    Type of Medium: Monograph available for loan
    Pages: xv, 554 S. , Ill., graph. Darst.
    Language: English
    Note: CONTENTS: THE COMPOSITION OF SEA-WATER. - SECTION I. CHEMISTRY. - 1. THE OCEANS AS A CHEMICAL SYSTEM / BY E. D. GOLDBERG. - 1. The composition of sea-water. - 2. Reactivities of the elements. - 3. Chemical reaction in the oceans and the compositions of the end-products. - 4. Space and time distributions of the elements. - 2. THE INFLUENCE OF ORGANISMS ON THE COMPOSITION OF SEAWATER / BY A. C. REDFIELD, B. H. KETCHUM AND F. A. RICHARDS. - 1. Introduction. - 2. The biochemical cycle. - 3. The biochemical circulation. - 3. ARTIFICIAL RADIOACTIVITY IN THE SEA / BY Y. MIYAKE. - 1. Artificial radioactivity in oceanic waters. - 2. Enrichment of radioactive substances in marine products. - 3. Artificial radioactivity as a tracer of water movements in the ocean. - 4. Disposal of radioactive waste in the ocean. - 4. RADIOISOTOPES AND LARGE-SCALE OCEANIC MIXING / W. BROECKER. - 1. Introduction. - 2. Useful isotopes. - 3. Steady-state distribution of 14C. - 4. Ocean-atmosphere CO2 exchange rates. - 5. Oceanic mixing models. - 6. Industrial CO2 effect. - 7. 226Ra distribution. - 8. 90Sr distribution. - 9. Non-steady-state conditions. - 10. Conclusion. - 5. CHEMICAL INSTRUMENTATION / BY D. E. CARRITT. - 1. Introduction. - 2. Chlorinity, salinity, density and related properties. - 3. Water tagging and tracer techniques. - 4. Measurement of dissolved gases. - 6. WATER SAMPLING AND THERMOMETERS / BY H. F. P. HERDMAN. - 1. Sampling. - 2. Thermometry. - SECTION II. FERTILITY OF THE OCEANS. - 7. PRODUCTIVITY, DEFINITION AND MEASUREMENT / BY E. STEEMANN NIELSEN. - 1. Introduction. - 2. Definitions. - 3. Methods for measuring primary production. - 4. The relation between the rate of gross production and net production below a surface unit. - 5. Transparency of the water versus organic production. - 6. The significance of single individual measurements of primary production. - 7. The influence of weather conditions. - 8. ORGANIC REGULATION OF PHYTOPLANKTON FERTILITY / BY L. PROVASOLI. - 1. Introduction. - 2. Data from chemical analysis. - 3. Organic products of algae and bacteria. - 4. Nutritional requirements of marine algae. - 5. Crustacea and organic solutes. - 6. Data from biological analysis of sea-water. - 7. Prospects. - 8. Addendum. - 9. BIOASSAY OF TRACE SUBSTANCES / BY W. L. BELSER. - 1. Introduction. - 2. Vitamins. - 3. Amino acids. - 4. Purines and pyrimidines. - 5. Perspectives. - COMPARATIVE AND DESCRIPTIVE OCEANOGRAPHY. - SECTION III. CURRENTS. - 10. EQUATORIAL CURRENT SYSTEMS / BY J. A. KNAUSS. - 1. Methods of study of ocean currents. - 2. Gross circulation pattern. - 3. A two-layer ocean - the thermocline. - 4. Zonal fiow-geostrophic currents. - 5. Meridional flow-upwelling. - 6. Conclusions and speculations. - 11. EASTERN BOUNDARY CURRENTS / BY W. S. WOOSTER AND J. L. REID, JR. - 1. Introduction. - 2. Common features of eastern boundary currents. - 3. Coastal upwelling. -4. Poleward eastern boundary currents. - 5. Biological implications. - 12. THE SOUTHERN OCEAN / BY G. E. R. DEACON. - 1. Topography. - 2. Oceanographic data. - 3. Wind zones. - 4. The water-masses. - 5. Climatology and zoogeography. - 6. Nutrient salts. - 7. Future needs. - 13. DEEP-CURRENT MEASUREMENTS USING NEUTRALLY BUOYANT FLOATS / BY G. H. VOLKMANN. - 1. Introduction. - 2. The pinger. - 3. Measurements. - 14. DROGUES AND NEUTRAL-BUOYANT FLOATS / BY J. A. KNAUSS. - 15. ESTUARIES / BY W. M. CAMERON AND D. W. PRITCHARD. - 1. Definition of estuaries. - 2. General considerations. - 3. Estuarine circulation patterns. - 4. Some variations on the estuarine sequence. - 5. Flushing in estuaries. - 6. Dynamics of estuaries. - 7. Kinematic description of the distribution of properties in an estuary. - 16. APPLICATIONS OF THE GYROPENDULUM / BY W. S. VON ARX. - 1. Introduction. - 2. The gyropendulum. - 3. The problem of time variations. - SECTION IV. BIOLOGICAL OCEANOGRAPHY. - 17. GEOGRAPHIC VARIATIONS IN.PRODUCTIVITY / BY J. H. RYTHER. - 1. Introduction. - 2. Incident radiation. - 3. Transparency. - 4. Nutrients. - 5. Latitudinal variations in the stability of surface water. - 6. Productivity of the major oceanic regions. - 7. Hydrodynamic features which influence productivity. - 8. Plankton production in coastal and inshore waters. - 9. Production of benthic plant communities. - 18. BIOLOGICAL SPECIES, WATER-MASSES AND CRRRENTS / BY M. W. JOHNSON AND E. BRINTON. - 1. Introduction. - 2. Water-masses and biological species. - 3. Water currents and biological species. - 19. COMMUNITIES OF ORGANISMS / BY E. W. FAGER. - 1. Introduction. - 2. Definition of community. - 3. Identification of communities. - 4. Community structure. - 5. Community function. - 6. Community theory. - 20. THEORY OF FOOD-CHAIN RELATIONS IN THE OCEAN / BY G. A. RILEY. - 1. Introduction. - 2. Mathematical models of plankton populations. - 3. Complex versus simple models. - 4. Prognosis for mathematical models. - 5. Higher elements of the food chain. - 21. FISHERY DYNAMICS - THEIR ANALYSIS AND INTERPRETATION / BY M. B. SCHAEFER AND R. J. H. BEVERTON. - 1. Introduction. - 2. The Beverton-Holt approach. - 3. The Schaefer approach. - 4. Concluding remarks. - SECTION V. OCEANOGRAPHICAL MISCELLANEA. - 22. SEASONAL CHANGES IN SEA-LEVEL / BY JUNE G. PATTULLO. - 1. Introduction. - 2. The observed seasonal variations. - 3. Factors influencing variations in sea-level. - 4. Summary. - 5. Conclusions. - 23. BATHYSCAPHS AND OTHER DEEP SUBMERSIBLES FOR OCEANOGRAPHIC RESEARCH / BY R. S. DIETZ. - 1. Introduction. - 2. Diving chambers. - 3. Bathyscaphs. - 4. Diving saucer. - 5. Buoyant-hulled deep ships or bathynauts. - 6. Deep-research vessel (D.R.V.). - 7. Remote underwater manipulator (RUM). - 8. Concluding remarks. - 24. DEEP-SEA ANCHORING AND MOORING / BY JOHN D. ISAACS. - 1. Introduction. - 2. Historical background. - 3. Problems of taut-mooring. - 4. Remarks on components of moorings. - 5. Mooring cables. - 6. The anchors. - 7. Fittings. - 8. Performance. - AUTHOR INDEX. - SUBJECT INDEX.
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  • 69
    Monograph available for loan
    Monograph available for loan
    Call number: AWI P9-90-0343b
    Type of Medium: Monograph available for loan
    Pages: II, 44 S. + 6 Ktn.
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  • 70
    Call number: ZSP-204-85
    In: CRREL Technical Report
    Type of Medium: Series available for loan
    Pages: iv, 14 S. : Ill., graph. Darst.
    Series Statement: CRREL Technical Report 85
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  • 71
    Series available for loan
    Series available for loan
    Hanover, NH
    Associated volumes
    Call number: ZSP-204-100
    In: CRREL Technical Report
    Type of Medium: Series available for loan
    Pages: vi, 14 S. : graph. Darst., Kt.
    Series Statement: CRREL Technical Report 100
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  • 72
    Series available for loan
    Series available for loan
    Hanover, NH
    Associated volumes
    Call number: ZSP-204-107
    In: CRREL Technical Report
    Type of Medium: Series available for loan
    Pages: vi, 14 S. : Ill., graph. Darst., Kt.
    Series Statement: CRREL Technical Report 107
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  • 73
    Call number: ZSP-204-69
    In: CRREL Technical Report
    Type of Medium: Series available for loan
    Pages: iv, 36 S.
    Series Statement: CRREL Technical Report 69
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  • 74
    Series available for loan
    Series available for loan
    Hanover, New Hampshire : U.S. Army Material Command, Cold Regions Research & Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-145
    In: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command, 145
    Description / Table of Contents: An analysis is made of the time required to build up an ice-age ice sheet and of the time required to destroy such an ice sheet. The calculations are based on the approximation that the theory of perfect plasticity is valid. It is concluded that the time required to eliminate it. If it is assumed that the accumulation rate of an ice-age ice sheet lies of a large ic sheet is of the order of 15.000 to 30.00 years. Ablation rates of 1 to 2 meters/year lead to shrinkage times of the order of 2000 to 4000 years, provided ablation occurs over an appreciable area of the ice sheet.
    Type of Medium: Series available for loan
    Pages: 16 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 145
    Language: English
    Note: Contents: Preface. - Summary. - Introduction. - Basis of theory. - Basic equations. - Ice sheets with only accumulation or ablation. - Growing ice sheets which contain only an accumulation zone. - Shrinking ice sheets which contain only an ablation zone. - Comments. - Ice sheet with both accumulation and ablation zones. - Growing ice sheets. - Shrinking ice sheets. - Conclusions. - References.
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  • 75
    Series available for loan
    Series available for loan
    Wilmette, Ill. : Snow Ice and Permafrost Research Establishment, Corps of Engineers, U.S. Army
    Associated volumes
    Call number: ZSP-202-70
    In: Research report / Cold Regions Research and Engineering Laboratory, 70
    Type of Medium: Series available for loan
    Pages: 93 Seiten , Karten
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 70
    Language: English
    Note: CONTENTS: Preface. - Summary. - Chapter I. Introduction. - Operations and logistics. - Chapter II. Methods of investigation. - Region of investigation. - Pit studies. - Elevation measurements. - Chapter Ill. Stratigraphy and accumulation. - Introduction. - Diagenesis without melt. - Diagenesis with melt. - Diagenetic facies defined on glaciers. - Grain size. - Description of three stratigraphic features. - Principles of stratigraphic interpretation. - Selection of a reference datum in the annual stratigraphic sequence. - Stratigraphic correlation. - Distribution of annual accumulation. - Independent checks on the stratigraphic interpretations. - Chapter IV. Temperature distribution. - Seasonal temperature variation on the snow surface. - Seasonal temperature variation below the snow surface. - Distribution of mean annual temperature on the ice sheet. - Chapter V. Diagenetic facies- a classification of glaciers. - Temperature. - Hardness. - Density. - Glacier facies - a classification of glaciers. - Chapter VI. Densification of snow and firn. - Load-volume relationship. - Depth-density relationship. - Chapter VII. Climatological implications. - Introduction. - Katabatic winds and accumulation. - Annual heat exchange. - The balance of the Greenland Ice Sheet. - References. - Appendix A: Stratigraphy, meteorology and glaciology. - Appendix B: Mean annual temperature. - Appendix C: The data sheets.
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  • 76
    Monograph available for loan
    Monograph available for loan
    Leningrad : Izdatel'stvo Leningradskogo Universiteta
    Call number: AWI G1-19-92227
    Type of Medium: Monograph available for loan
    Pages: 445 Seiten , Illustrationen
    Series Statement: Zemnoj magnetizm / B.M. Janovskij 1
    Language: Russian
    Note: In kyrillischer Schrift
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  • 77
    Call number: AWI A3-20-93434-2
    In: Meteorologische Abhandlungen / Institut für Meteorologie und Geophysik der Freien Universität Berlin, Band XXXII, Heft 2
    Type of Medium: Series available for loan
    Pages: 218 Seiten , Illustrationen
    Series Statement: Meteorologische Abhandlungen / Institut für Meteorologie und Geophysik der Freien Universität Berlin 32,2
    Language: German
    Note: Zugleich: Dissertation, Freie Unversität Berlin, [ca. 1963] , INHALTSVERZEICHNIS PROBLEMSTELLUNG UND ZIELSETZUNG 1. BEMERKUNGEN ZUM BEOBACHTUNGSGELÄNDE UND ZUM BEOBACHTUNGSMATERIAL 1.1 Das Beobachtungsgelände 1.2 Das Beobachtungsmaterial 2. HOMOGENITÄTSBETRACHTUNGEN 2.1 Temperatur 2.2 Niederschlag 2.3 Wind 2.4 Sonnenschein und Bewölkung 3. TEMPERATURVERHÄLTNISSE 3.1 Monats- und Jahreswerte 3.2 Tageswerte 3.3 Pentadenwerte 3.4 Häufigkeitsbetrachtungen 3.5 Interdiurne Veränderlichkeit 3.6 Der tägliche Gang 3.7 Vorkommen bestimmter Schwellenwerte 3.71 Frost- und Eistage 3.72 Sommer- und Tropentage 4. DER WASSERGEHALT DER LUFT 4.1 Monats- und Jahreswerte 4.2 Tageswerte 4.3 Häufigkeitsbetrachtungen 4.4 Interdiurne Veränderlichkeit 4.5 Der tägliche Gang 5. BEWÖLKUNGSVERHÄLTNISSE 5.1 Monats- und Jahreswerte 5.2 Tageswerte 5.3 Häufigkeitsbetrachtungen 5.4 Der tägliche Gang 5.5 Heitere und trübe Tage 5.6 Nebel 6. SONNENSCHEIN 6.1 Monats- und Jahreswerte 6.2 Tageswerte 6.3 Der tägliche Gang 7. NIEDERSCHLAGSVERHÄLTNISSE 7.1 Monats- und Jahreswerte 7.2 Niederschlagsbereitschaft 7.3 Tageswerte 7.4 Der tägliche Gang 7.5 Häufigkeitsbetrachtungen 7.6 Niederschlags- und Trockenperioden 7.7 Niederschlag und Wind· 7.8 Schneeverhältnisse 7.81 Schneefall und Schneedecke 7.82 Schneehöhe 7.9 Gewitter 8. WINDVERHÄLTNISSE 8.1 Windrichtung 8.2 Windgeschwindigkeit 8.21 Der jährliche Gang 8.22 Häufigkeitsbetrachtungen 8.23 Sturmtage und Windstillen 8.24 Der tägliche Gang 9.ZUSAMMENFASSUNG VERZEICHNIS DER TEXTTABELLEN VERZEICHNIS DER ABBILDUNGEN LITERATURVERZEICHNIS TABELLENANHANG
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  • 78
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-79
    In: Research report / Cold Regions Research and Engineering Laboratory, 79
    Description / Table of Contents: Summary: The theory of a plate on an elastic foundation will closely predict the radial cracks observed in loading tests on floating ice sheets. However, the plate theory does not predict accurately the circumferential crack which forms ultimately with increased loading. The wedge theory is developed in an attempt to better predict the location and magnitude of the stresses causing the circumferential crack. The results obtained can be applied to help predict the ultimate bearing capacity of an ice sheet, provided the modulus of elasticity and flexural strength of the ice are known.
    Type of Medium: Series available for loan
    Pages: Getrennte Zählung , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 79
    Language: English
    Note: CONTENTS Preface Summary Introduction Solution Applications Conclusions References Appendix A Computer program Graphs of nev functions, derivatives, and integrals Tables of nev functions, derivatives, and integrals
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  • 79
    Series available for loan
    Series available for loan
    Wilmette, Ill. : Snow Ice and Permafrost Research Establishment, Corps of Engineers, U.S. Army
    Associated volumes
    Call number: ZSP-202-62
    In: Research report / Cold Regions Research and Engineering Laboratory, 62
    Description / Table of Contents: Summary: Adhesive strength of ice for the systems ice/stainless steel and ice/optically flat fused quartz has been investigated as a function of surface roughness of steel surfaces and rates of shear for steel and quartz. The adhesive strength decreases with decreasing roughness of steel surfaces and the force vs time curves for smooth steel plates resemble those of two solids sliding over each other with a liquid layer sandwiched between them. This is particularly so in the case of quartz. The adhesive strength as a function of rate of shear is linear both for ice/stainless steel and ice/quartz; however, there are indications of yield values. The experimental results are in agreement with the assumption of a liquidlike layer on ice. Ratios of viscosity coefficient to the thickness of the layer have been evaluated for both systems and viscosity coefficients are estimated. The importance of interfacial free energy considerations is pointed out.
    Type of Medium: Series available for loan
    Pages: iii, 10 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 62
    Language: English
    Note: CONTENTS Preface Summary Introduction Experimental Materials Apparatus Experimental results Ice/metal interface Ice/quartz interface Discussion References
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  • 80
    Series available for loan
    Series available for loan
    Wilmette, Ill. : Snow Ice and Permafrost Research Establishment, Corps of Engineers, U.S. Army
    Associated volumes
    Call number: ZSP-202-64
    In: Research report / Cold Regions Research and Engineering Laboratory, 64
    Description / Table of Contents: Summary: The distribution of temperature throughout an idealized ice cap is studied. The idealized ice cap is considered as one with a constant growth rate, without internal movement, subject to a linear climatic change and to a constant geothermal influx. The problem is treated as a Stefan-type problem and the solution is obtained by the principle of superposition. The results indicate that the temperature at the base of the ice cap rises with time and eventually would reach the melting point of the ice. Under such conditions, it is concluded that the ice cap is not resting on a permafrost base as suggested by previous investigation.
    Type of Medium: Series available for loan
    Pages: iv, 8 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 64
    Language: English
    Note: CONTENTS Preface Summary Introduction Mathematical development Method of solution Discussion of results Base temperature Minimum temperature Effect of rate of growth Effect of geothermal influx Comparison with observed results References
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  • 81
    Series available for loan
    Series available for loan
    Wilmette, Ill. : Snow Ice and Permafrost Research Establishment, Corps of Engineers, U.S. Army
    Associated volumes
    Call number: ZSP-202-66
    In: Research report / Cold Regions Research and Engineering Laboratory, 66
    Description / Table of Contents: Summary: A simple theory is proposed for crack formation and development by soil desiccation on the basis of laboratory experiments utilizing soil samples (Bloomington till) with max particle size of 1 mm diam. held in flat wooden containers. The crack pattern is more dependent on the thickness of the soil sample than on temperature or humidity. Some effect is caused also by differences in the bottom material of the containers. The area of cells made by crack patterns has a log normal size distribution. Total length of cracks decreases with increase in sample thickness. The number of sides of cells also depends on the thickness. Cracking was found to begin from the center of the soil layer and to propagate to the surface or bottom with non-uniform speed.
    Type of Medium: Series available for loan
    Pages: vi, 48, A4 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 66
    Language: English
    Note: CONTENTS Preface Summary Introduction Soil material Soil Preparation of the soil material Containers Temperature and humidity of the air Moisture content and dry density of the soil Experimental procedures and results General procedures Definition of the characteristics of cracking of soil Cracking moisture content Size of cells made by cracking of the soil Length of cracks Number of sides of cells Development of cracks Additional experiments Interfacial fracture markings Method of auxilliary tests on physical properties of the soil Elastic constants of the soil Shrinkage of soil due to desiccation Tests of the adhesion between the soil and the bottom material Results of auxiliary tests Elastic constants of the soil Free shrinkage process of the soil due to desiccation Adhesion between the soil and glass or wood Mechanism of crack formation due to the desiccation of soil Geometric interpretation Mechanical interpretation Conclusions References Appendix: Table of experiments
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  • 82
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-107
    In: Research report / Cold Regions Research and Engineering Laboratory, 107
    Description / Table of Contents: Summary: The formation of lake ice was studied during the winter of 1956-57 at Post Pond, Lyme, N. H. Tabular, columnar, granular, and crenulate textures of 36 blocks of ice observed are discussed in terms of relative growth velocity and shown in a classification chart. Ice structures are characterized by Forel striations, Tyndall figures, bubbles and strain shadows. Average crystal areas increased with ice thickness, the rate of increase being greater toward lake center, and ceased to enlarge when in a continuous bubble layer. The lake-ice sheet grew both from top and bottom, .downward growth resulting from crystals in a favorable vertical orientation of a-axes and upward growth coming about by water flowing on the original upper ice surface and freezing. Exception to this type of growth was found in the lake area which froze first, where individual crystal areas were larger at the surface and there was no upper surface ice accretion. Fabric diagrams of ice outside the anomolous area show a change of optic axis orientation from a high percentage of c-axes vertical near the surface to a high percentage horizontal at the bottom.
    Type of Medium: Series available for loan
    Pages: iv, 22, A2, B1 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 107
    Language: English
    Note: CONTENTS Preface Summary Description of the lake Cli rna te of the lake Methods of study Ice textures Crystal size Ice structures Crystal fabric studies Growth of an ice sheet References Appendix A: Weather data Appendix B: Sample data
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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-202-112
    In: Research report / Cold Regions Research and Engineering Laboratory, 112
    Description / Table of Contents: Summary: The age hardening of artificially and naturally compacted snow has been investigated at the South Pole. Results show that the age-hardening process is greatly retarded at low temperatures. Artificially compacted samples of density 0.55 g/cm^3 attained a compressive strength of less than 3.0 kg/cm^2 after one year's aging at -49°C. Exposure to solar radiation accelerated the age hardening. Irradiated samples attained a strength of 6.0 kg/cm^2 after 100 hr, increasing to a virtual maximum of 8.0 kg/cm^2 at 600 hr. Compressive strengths increased witha decrease in snow-particle size and with an increasing angularity of the particles. Below 3 m the strength of naturally compacted snow was found to increase rapidly with an increase in density. Naturally compacted snow of density 0.55 g/cm^3 possessed considerably greater strength than any of the age-hardened samples of artificially compacted snow of the same density. Thin-section studies show that age hardening can be correlated with the formation and growth of intergranular bonds, and that bond growth falls off rapidly with decreasing temperature. In view of the low strength found in both naturally and artificially compacted snow at the South Pole, "cut-and-cover" undersnow camp construction may not prove practical at the South Pole.
    Type of Medium: Series available for loan
    Pages: v, 19, A6 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 112
    Language: English
    Note: CONTENTS Preface Summary Introduction Previous work Experimental methods Experimental results Series A Series B Series C Series D Series E Discussion Conclusions References Appendix A
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  • 84
    Call number: ZSP-202-111,1
    In: Research report / Cold Regions Research and Engineering Laboratory, 111,1
    Description / Table of Contents: Summary: Optical scintillation, visual resolution, and wind and temperature profiles were measured over snow, ice and frozen ground. The data were analyzed to determine relationships between (1) scintillation and visual resolution and (2) scintillation and meteorological and surface conditions. The experimental results included (1) estimates of the limit of visual resolution, (2) telephotometer measurements of the apparent fluctuations in brightness (scintillation) of an artificial light source, and (3) measurements of wind direction and of the vertical distributions of wind speed and temperature. The optical path was 543 m long and 1.5 m above uniform horizontal surfaces. All scintillation and meteorological data are given in an appendix. The principal results of the analysis showed that for turbulent flow in stable stratification over snow (1) visual resolution deteriorated systematically as scintillation increased in intensity and (2) scintilliation intensity increased with increase in vertical temperature gradient. Scintilliation was at a minimum in the absence of thermal stratification and at a maximum (in very stable thermal stratification) during the sudden transition from laminar to turbulent flow. For a given temperature gradient, scintilliation increased with increase in wind speed. When wind and temperature gradients were combined in terms of the Richardson number and related to scintilliation, the data obtained over snow indicated a critical Richardson number of about 0.35. Scintilliation power spectra for eight periods revealed characteristics that could be related to visual resolution, the Richardson number and the mean wind speed component normal to the optical path. NOTE: This file is large. Allow your browser several minutes to download the file.
    Type of Medium: Series available for loan
    Pages: iii, 32, A17, B44 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 111,1
    Language: English
    Note: CONTENTS Preface Page Summary Introduction The problem Previous work Plan of the investigation Conclusions Visual resolution and scintillation Visual resolution and wind, temperature, and surface conditions Visual resolution and height and length of optical path Results Measurements Analysis and discussion Visual resolution and scintillation relationships Scintillation and micrometeorological parameters Index of refraction fluctuations Scintillation and the temperature profile Scintillation and average wind speed Combined effects of wind speed and temperature gradient Scintillation and surface roughness Scintillation power spectra Scintillation and path length References Appendix A: Equipment and procedures Appendix B: Micrometeorological and scintillation data
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  • 85
    Call number: AWI G3-24-95691
    Description / Table of Contents: В 1960 г. в Канаде состоялся Первый международный симпозиум по геологии Арктики, в котором привяли участие советские, канадские, американские, английские, датские и норвежские ученые. Итогом работ симпозиума явился настоящий сборник, в котором сведены новейшие материалы по геологии, океанологии, гляциологии и климатологии северных полярных областей земного шара. Эти работы дают отчетливое представление о геологическом строении огромных территорий Канады и Аляски, о рельефе и характере осадков два Северного Ледовитого океана, о ледовом режиме Арктики. Необходимо отметить, что до недавнего времени многие области зарубежной Арктики были белыми пятнами на геологических картах; первые сведения о них содержатся в статьях этого сборника. Новые материалы сборника дают ценнейшие сведения для сравнительных оценок геологических условий и обстановки оруденения северных областей советской и зарубежной Арктики.
    Description / Table of Contents: Translation of abstract: In 1960, the First International Symposium on Arctic Geology was held in Canada, in which Soviet, Canadian, American, English, Danish and Norwegian scientists took part. The result of the symposium was this collection, which brings together the latest materials on geology, oceanology, glaciology and climatology of the northern polar regions of the globe. These works give a clear idea of the geological structure of the vast territories of Canada and Alaska, the relief and nature of precipitation in the two Arctic Oceans, and the ice regime of the Arctic. It should be noted that before recently, many areas of the foreign Arctic were blank spots on geological maps; the first information about them is contained in the articles in this collection. New materials in the collection provide valuable information for comparative assessments of geological conditions and mineralization conditions in the northern regions of the Soviet and foreign Arctic.
    Type of Medium: Monograph available for loan
    Pages: 515 Seiten , Illustrationen
    Uniform Title: Geology of the Arctic proceedings of the first International Symposium on Arctic Geology
    Language: Russian
    Note: СОДЕРЖАНИЕ Предисловие Предисловие к английскому изданию Введение ШПИЦБЕРГЕН Схема структурной истории Шпицбергена / В. Б. Харланд ГРЕНЛАНДИЯ Обзор геологии северной и восточной Гренландии Докембрийские и нижнепалеозойские структурные элементы и осадконакопление в северной и восточной Гренландии / Л. Кох Каролиниды: орогенический пояс позднедокембрийского возраста в северо-восточной Гренландии / Дж. Халлер Нижний палеозой Гренландии / Дж. Коуи Значение каледонской орогении в Гренландии / Дж. Халлер Девонские отложения центральной части восточной Гренландии / Х. Бютлер Континентальные иаменноугольные и нижнепермские отложения центральной части восточной Гренландии / Х. Бютлер Пермь Гренландии / В. Майнц Триас восточной Гренландии / Р. Трюмпи Юрские отложения восточной Гренландии / Дж. Х. Калломон Меловые отложения восточной Гренландии / Д. Т. Донован Третичные отложения Гренландии / Э. Венк Стратиграфия позднего докембрия восточной Гренландии / Х. Р. Кац О хронологии докембрия западной Гренландии / А. Бертельсен КАНАДА Структурная истории Канадского арктического архипелага с докембрийского времени / Р. Topcтeйнccoн, Е. T. Тозер Общий обзор геологии докембрии арктической части Канады / Р. Г. Блакадар, Дж. А. Фрейзер Стратиграфия нижнего палеозоя Канадского арктического архипелага / Р. Торетейнссон Общий очерк стратиграфии мезозойских и третичных отложений Канадского арктического архипелага / Е. T. Тозер Соотношение дислокаций складчатого пояса островов Парри и корнуоллисских складчатых структур на востоке острова Батерст Канадского арктического архипелага / Э. Н. Мак-Нейр Геологическая интерпретация аэромагнитных профилей, проведенных через Канадский арктический архипелаг / А. Ф. Грегори, М. Е. Бауэр, Л. В. Морлей Тектоническое строение северной Канады / Л. Дж. Мартин Каледонские или акадийские граниты северной части территории Юкон / Х. Бадегард, Р. И. Фолинеби, Дж. Липсон Стратиграфия девона района среднего течения реки Макензи, Северо-Западные территории, Канада / Х. Г. Бacceт Стратиграфия девонских отложений района Нориан-Уэлс / Т. Cтopu АЛЯСКА Изучение тектоники Аляски / Г. Грик Корреляция палеозойских пород Аляски / Дж. Т. Дутромл Новые данные о распространении верхнетретичных континентальных отложений на Аляске и в северо-западной Канаде / В. С. Бениннгхоф, Г. В. Холмс, Д. М. Гопкинс АРКТИЧЕСКИЙ БАССЕЙН Истории геологических знаний о происхождении Арктинеского бассейна / А. Дж. Ирдли Срединно-океанический хребет и его продолжение через Арктический бассейн / Б. К. Хейзен, М. Юииг Продолжение горных цепей в Арктике в прошлом / Дж. T. Вилъсон Сейсмическое исследование дна Арктического океана / К. Ханкинс Гальки, поднятые при драгировании в центральной части Северного Ледовитого океана / В. Шварцахер, К. Ханкинс Батиметрия моря Бофорта / А. Дж. Kapcoла, Р. Л. Фишер, К. Дж. Шипек, Г. Шамвей Предварительные результаты исследований арктической дрейфующей станции Чарли / В. Дж. Кроми Геофизические исследования на дрейфующей станции МГГ Браво, Т-3, 1958-1959 гr. / Д. Плоуфф, Г. В. Келлер, Ф. Ц, Фришкнехт, Р. Р. Уол Морские геологические наблюдения в Баренцовом море / Х. Игнатиус Морская геология и батиметрия шельфа Чукотского моря в районе Оготорук-Крик, северо-западная Аляска / Д. В. Схолл, К. Л. Сайнсбери Геоморфология Арктического бассейна / Р. Дитц, Дж. Шамвей Предметный указатель Указатель географических названий , Translation of Content Preface Preface to the English edition Introduction SPITSBERGEN Scheme of the structural history of Spitsbergen / W. B. Harland GREENLAND Review of the geology of northern and eastern Greenland Precambrian and Lower Paleozoic structural elements and sedimentation in northern and eastern Greenland / L. Koch Carolinids: Late Precambrian orogenic belt in northeastern Greenland / J. Haller Lower Paleozoic of Greenland / J. Cowie The significance of the Caledonian orogeny in Greenland / J. Haller Devonian deposits of the central part of eastern Greenland / H. Bütler Continental Carboniferous and Lower Permian deposits of the central part of eastern Greenland / H. Bütler Perm Greenland / V. Mainz Triassic of eastern Greenland / R. Trumpy Jurassic deposits of eastern Greenland / J. H. Callomon Cretaceous deposits of eastern Greenland / D. T. Donovan Tertiary deposits of Greenland / E. Wenk Late Precambrian stratigraphy of eastern Greenland / H. R. Katz On the chronology of the Precambrian of western Greenland / A. Bertelsen CANADA Structural history of the Canadian Arctic archipelago since Precambrian time / R. Topsteinson, E. T. Tozer General overview of the Precambrian geology of the Canadian Arctic / R. G. Blakadar, J. A. Fraser Stratigraphy of the Lower Paleozoic of the Canadian Arctic Archipelago / R. Thoreteinsson General outline of the stratigraphy of Mesozoic and Tertiary deposits of the Canadian Arctic Archipelago / E. T. Tozer The relationship between the dislocations of the Parry Islands fold belt and the Cornwallis fold structures in the east of Bathurst Island in the Canadian Arctic Archipelago / E. N. McNair Geological interpretation of aeromagnetic profiles drawn through the Canadian Arctic Archipelago / A. F. Gregory, M. E. Bauer, L. V. Morley Tectonic structure of northern Canada / L. J. Martin Caledonian or Acadian granites of the northern Yukon Territory / H. Badegard, R. I. Folineby, J. Lipson Devonian stratigraphy of the middle Mackenzie River region, Northwest Territories, Canada / H. G. Basset Stratigraphy of Devonian deposits of the Norian-Wells region / T. Stopu ALASKA Study of Alaska tectonics / G. Grik Correlation of Paleozoic Rocks of Alaska / J. T. Dutroml New data on the distribution of Upper Tertiary continental sediments in Alaska and northwestern Canada / V. S. Beninghof, G. W. Holmes, D. M. Hopkins ARCTIC POOL Stories of geological knowledge about the origin of the Arctic Basin / A. J. Eardley Mid-ocean ridge and its continuation through the Arctic basin / B. K. Hazen, M. Huig The continuation of mountain ranges in the Arctic in the past / J. T. Wilson Seismic exploration of the Arctic ocean floor / K. Hankins Pebbles raised during dredging in the central part of the Arctic Ocean / V. Schwarzacher, K. Hankins Bathymetry of the Beaufort Sea / A. J. Kapcola, R. L. Fisher, K. J. Shipek, G. Shumway Preliminary results of studies of the Arctic drifting station Charlie / W. J. Cromie Geophysical research at the drifting station MGG Bravo, T-3, 1958-1959. / D. Plouffe, G. W. Keller, F. Z, Frischknecht, R. R. Wahl Marine geological observations in the Barents Sea / H. Ignatius Marine geology and bathymetry of the Chukchi Sea shelf in the Ogotoruk Creek area, northwestern Alaska / D. W. Scholl, K. L. Sainsbury Geomorphology of the Arctic Basin / R. Dietz, J. Shumway Subject index Index of geographical names , In kyrillischer Schrift
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  • 86
    Call number: AWI G3-24-95571-2
    In: Tektonika Sibiri, Tom 2
    Type of Medium: Monograph available for loan
    Pages: 385 Seiten , Illustrationen , 1 Kartenbeilage, 1 Errata
    Series Statement: Tektonika Sibiri / Akademija Nauk SSSR, Sibirskoe Otdelenie, Naučnyj Sovet po Tektonike Sibiri i Dalʹnego Vostoka Tom 2
    Language: Russian
    Note: Kartenbeilage unter dem Titel: Tektoničeskaja Karta : Central'nogo sektora Sovetskoj Arktiki 〈1: 5 000 000〉 , CONTENTS Foreward Tectonics of Siberian Platform and Its Borderland Bounding Structures of Siberian Platform / Yu. A. Kosygin, I. V. Luchitski History of Development of Structure of North-Western Part of Siberian Platform / Ya. I. Polkin Tectonic Structure of Western Part of Siberian Platform / N. V. Drenov To the Problem of Structure of Pre-Yenisei Marginal Part of Siberian Platform / A. S. Kirillov History of Tectonic Development of South-Western Part of Siberian Platform and Rybinsk Depression / M. A. Zharkov On Peculiarities of Tectonics of Rydinsk Depression / A. I. Anatoljeva Some Relations of Siberian Platform with Its Borderlands / D. I. Musatov Tectonics of Yenisei Ridge / G. I. Kirichenko Structural-Facial Zones of Riphean and Lower Cambrian of Yenisey Ridge and North-Western Part of Eastern Sayan / M. A. Semikhatov On Tectonics of Southern Part of Yenisei Ridge / Yu. Parfenov Tectonics of Bakhta and Ucham River Basin / N. S. Malich On Mechanism of Horst-Formation in Tungussk Syneclise / L. M. PIotnikov On Forms of Structural Connections of Siberian Platform and West-Siberian Plate / K. V. Bogolepov Structure of Basement of Eastern Margin of West-Siberian Plate in Connection with Its General Tectonic Zoning / V. N. SoboIevskaya Structure of Folded Basement of Minusa Intermontane Downwarp and South-Eastern Part of West-Siberian Plate by Geophysical Data / V. S. Surkov Some New Information on Structures of Cretaceous the Eastern Margin of West-Siberian Plate / Yu. F. Pogonya-Stefanovich Tectonics of Sayano-Altai Folded Region Main Principles of Tectonic Classification of Depressions and Downwarps of Orogenic Stage of Development of Eastern Part of Sayano-Altai Region / B. N. Krasilnikov, G. M. Volontey Some Peculiarities of Deep Fractures on the Example of Folded Regions on the South of Krasnoyarsk Territory / D. I. Musatov Principal Features of Tectonics and History of Geologic Development of Eastern Sayan / A. L. Dodin On Tectonic Zonation of Eastern Sayan / V. B. Lyatski Main Features of Tectonics of Eastern Part of Eastern Sayan / O. P. AIexeyeva, V. D. Titov Some Problems of Tectonics of North-Western Part of Eastern Sayan / K. V. Radugin Tectonics of Proterozoic Era of East-Sayan (Derbinsk) Anticlinorium / A. A. SaveIyev Tectonics of Pre-Cambrian Blocks of Eastern Sayan and Khamar-Daban and Their Absolute Age / V. Ya. Khiltova, L. P . Nikitina, I. P. Buzikov, N. A. Avdontsev Main Features of Tectonics of Near-Sayan Structural-Facial Zone / P. I. Shames Problems of Tectonic Development of South-Western Part of Eastern Sayan and Adjacent Regions of Minusa Depressions / E. A. Shneider, B. P. Zubkus Tectonics of Minusa Depressions and of Their Basement / A. A. Mossakovski Some Features of Structure and Development of Western Sayan / L. P. Zonenshain On «Butt-End» (T-form) Conjugation of Structures of Western Sayan, Western Tuva and Mountain Altai / A. M. Borovikov Some Features of Tectonic Development of Territory of Tuva during Late Cambrian and Lower Paleozoic / G. A. Kudryavtsev Main Types of Development of Large Structures of Tuva Intermontane Downwarp / G. M. Volontey Tectonics of Central Sector of Soviet Arctic Tectonic Map of the North of Siberia at the Scale of 1:2 500 000 / I. P. Atlasov The Map of Neotectonics of the North of Siberia at the Scale of 1:2 500 000 / M. T. Kiryushina Tectono-Magmatic Stages of Development of Taimyr-Severnaya Zemlya Folded Region and Connection of Commercial Minerals with them / V. A. Vakar, B. Kh. Egiazarov Pre-Cambrian Basement of Taimyr and Its Deformation during Formation of Folded Region / Yu. E. Pogrebitski Tectonics and Metallogeny On Principles of Tectonic Zoning on the Example of Southern Regions of Krasnoyarsk Territory (in Connection with Problems of Metallogeny) / V. V. Bogatski On Structural-Metallogenic Zoning of Eastern Siberia and the North-East of USSR / S. V. Levchenko Tectonic Control of Trappean Ore-Bearing Intrusions of North-Western Part of Siberian Platform / A. M. ViIenski, G. I. Kavardin Tectonics of Igarka-Norilsk Region and Ore-Controling Structures / G. D. MasIov Laws Governing Localization of Ore Deposits in Norilsk-Igarka Region / V. N. Egorov Internal Structure of Early Caledonian Downwarp of Northern Part of West Sayan and Peculiarities of Its Magmatism / Sh. D. Kurtseraite Index of Regional Tectonic Nomendature Summary , СОДЕРЖАНИЕ Предисловие Тектоника Сибирской платформы и структуры ее обрамления Структуры ограничения Сибирской платформы / Ю. А. Косыгин, И. В. Лучицкий История развития структуры северо-западной: части Сибирской платформы / Я. И. Полькин Тектоническое строение западной части Сибирской платформы / Н. В. Дренов К вопросу о структуре приенисейской окраины Сибирской платформы / А. С. Кириллов История тектонического развития юго-западной части Сибирской платформы и Рыбинской впадины / М. А. Жарков Об особенностях тектоники Рыбинской впадины / А. И. Анатольева Некоторые вопросы соотношения Сибирской платформы с ее обрамлением / Д. И. Мусатов Тектоника Енисейского кряжа / Г. И. Кириченко Структурно-фациальные зоны рифея и нижнего кембрия Енисейского кряжа и северо -западной части Восточного Саяна / М А. Семихатов О тектонике южной части Енисейского кряжа / Ю. И. Парфенов Тектоника бассейна рек Бахты и Учами / Н. С. Малич О механизме горстообразования в Тунгусской синеклизе / Л. М. Плотников О формах структурной связи Сибирской платформы и Западно-Сибирской плиты / К. В. Боголепов Строение фундамента восточной окраины Западно-Сибирской плиты в связи с ее общим тектоническим районированием / В. Н. Соболевская Строение складчатого фундамента Минусинского межгорного прогиба и юго-восточной части Западно-Сибирской плиты по геофизическим данным / В. С. Сурков Некоторые новые данные по структурам мела на восточной окраине Западно-Сибирской плиты / Ю. Ф. Погоня-Стефанович Тектоника Саяио-Алтайской складчатой области Основные принципы тектонической классификации впадин и прогибов орогенного этапа развития восточной части Саяно-Алтайской области / В. Н. Красильников, Г. М . Волонтэй Некоторые особенности глубинных разломов на примере складчатых областей юга Красноярского края / Д. И. Мусатов Основные черты тектоники и истории геологического развития Восточного Саяна / А. Л. Додин К тектоническому районированию Восточного Саяна / В. Б. Ляцкий Основные черты тектоники восточной части Восточного Саяна / О. П. Алексеева, Д. В. Титов Некоторые вопросы тектоники северо-западной части Восточного Саяна / R. В. Радугин Тектоника протерозоя Восточно-Саянского (Дербинского) антиклинория / А. А. Савельев Тектоника докембрийских глыб Восточного Саяна и Хамар-Дабана и их абсолютный возраст / В. Я. Хильтова, Л. П. Никитина, И. П. Бузиков, Н. А. Авдонцев Основные черты тектоники Присаянской структурно-фациальной зоны / И. П. Шамес Вопросы тектонического развития юго-западной части Восточного Саяна и прилегающих районов Минусинских впадин / Е. А. Шнейдер, Б. П. 3убкус Тектоника Минусинских впадин и их фундамента / А. А. Моссаковский Некоторые черты структуры развития Западного Саяна / Л. П. Зоненшайн О торцовом сопряжении структур Западного Саяна, Западной Тувы и Горного Алтая / А. М. Боровиков Некоторые черты тектонического развития территории Тувы в позднем докембрии и нижнем палеозое / Г. А. Кудрявцев Основные типы развития крупных структур Тувинского межгорного прогиба / Г. М. Волонтэй Тектоника центрального сектора Советской Арктики Тектоническая карта севера Сибири масштаба 1:2 500 000 / И. П. Атласов Карта новейшей тектоники севера Сибири масштаба 1:2 500 000 / М. Т. Кирюшина Тектоно-магматические этапы развития Таймыро-Североземельской складчатой области и связь с ними полезных ископаемых / В. А. Вакар, Б. Х. Егиазаров Докембрийский фундамент Таймыра и его деформации в период образования снладчатой области / Ю. Е. Погребицкий Тектоника н металлоrения О принципах тектонического районирования на примере южных районов Красноярского края (в связи с проблемами металлогении) / В. В. Богацкий О структурно-металлогеническом районировании Восточной Сибири и Северо-Востока СССР / С. В. Левченко Тектонический контроль трапповых рудоносных интрузий северо-западной части Сибирской платформы / А. М. Виленский, Г. И. Кавардин Тектоника Игарско-Норильского района и рудоконтролирующие структуры / Г. Д. Маслов Закономерности размещения рудных месторождений в Норильско-Игарском районе / В. Н. Егоров Внутренняя структура раннекаледонского прогиба северной части Западного Саяна и особенности его магматизма / Ш. Д. Курцерайте Указатель региональных тектонических терминов Краткое содержание сборника Резюме , In kyrillischer Schrift , In russischer Sprache mit englischer Zusammenfassung
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  • 87
    Monograph non-lending collection
    Monograph non-lending collection
    Bruxelles
    Associated volumes
    Call number: AWI PY-5831
    In: Expédition Antarctique Belge 1957-1958 : Résultats Scientifiques ; Vol. 3, Fasc. 1, Vol. 3, Fasc. 1
    Type of Medium: Monograph non-lending collection
    Pages: 174 S , graph. Darst., Kt
    Series Statement: Expédition Antarctique Belge 1957-1958 : résultats sientifiques ; Vol. 3, Fasc. 1
    Language: French
    Note: Table des Matières: Liste des figures. - Avant propos. - Préambule. - Introduction. - 1. Programme du Géomagnétisme. - 2. Situation de la base Roi Baudouin et plans des installations. - 3. Installation de la station de Géomagnétisme. - Pavillon des mesures absolues. - Pavillon des enregistreurs. - Le géomagnétisme au bâtiment "Science". - Installations électriques. - 4. Les instruments. - Nomenclature et description. - Etablissement du méridien magnétique et orientation des aimants des variomètres. - Installation et réglage des instruments. - 5. Les températures. - Variations journalières pour chaque variomètre. - Moyennes et écarts max. - Humidité relative. - 6. Les temps. - Controle et correction du temps. - Temps vrai de la station. - 7. Les magnétogrammes. - Marquage et magnétogrammes disponibles. - Magnétogramme du 8/9/1958 et description de l'aurore. - 8. Méthodes d'observation. - Constantes, méthodes de mesure utilisées, calculs. - Valeurs d'echelle et parallaxes. - Valeurs tabulées des mesures absolues. - 9. Mesures magnétiques en campagne. - Etablissement des stations. - Températures, durée et nombre des mesures. - Azimuts et temps. - Valeurs tabulées des mesures. - 10. Difficultés rencontrées et propositions. - Choix du terrain et installation des pavillons. - Solutions proposées pour la stabilité des pilliers. - Résumé des caractéristiques principales de la station. - Bibliographie.
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  • 88
    Series available for loan
    Series available for loan
    Wilmette, Ill. : Snow Ice and Permafrost Research Establishment, Corps of Engineers, U.S. Army
    Associated volumes
    Call number: ZSP-202-61
    In: Research report / Cold Regions Research and Engineering Laboratory, 61
    Description / Table of Contents: Summary: The results of experiments on the bonding of polished and microtomed surfaces of bubble-free ice samples at -5°C with various loads are reported. Only a small part of the available surface area appeared to be bonded, this area increasing with the bonding load. Surfaces apposed immediately after preparation showed an appreciably higher force of separation than those joined after a time interval. The force of separation for surfaces placed together at 0% relative humidity was higher than that at 100% relative humidity. A simplified theory of bonding of irregular ice surfaces is formulated in the appendix. The calculations are based on the assumption of a distribution of small ice cylinders of equal cross sections but different heights located on a non-deformable plate. The cylinders are deformed by a constant force which is applied by another completely non-deformable flat plate. The deformation as a function of force and time and the force of separation as a function of load are derived, assuming that the distribution of heights is given by a box distribution (i.e., frequency of heights is constant).
    Type of Medium: Series available for loan
    Pages: iv, 6, A4 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 61
    Language: English
    Note: CONTENTS Preface Summary Introduction Materials Apparatus and procedure Results Discussion References Appendix: Compression of an assembly of cylinders
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  • 89
    Series available for loan
    Series available for loan
    Wilmette, Ill. : Snow Ice and Permafrost Research Establishment, Corps of Engineers, U.S. Army
    Associated volumes
    Call number: ZSP-202-63
    In: Research report / Cold Regions Research and Engineering Laboratory, 63
    Description / Table of Contents: Summary: Experiments have been carried out on the plastic deformation of thick-walled snow-ice cylinders under hydrostatic pressure as a function of pressure and temperature. At constant circumferential stress and temperature the natural strain rate of closure is a constant. This constant varies with the circumferential stress according to a sine function and is exponentially dependent on temperature with an energy of activation of 14.1 kcal/mole at an average circumferential stress of 3.1 kg/cm^2. The mechanism of the plastic flow is in agreement with a mechanism proposed previously, that is, flow between grain boundaries takes place.
    Type of Medium: Series available for loan
    Pages: iv, 7 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 63
    Language: English
    Note: CONTENTS Preface Summary Experimental Materials Apparatus Experimental results Deformation under constant hydrostatic pressure Deformation as a function of hydrostatic pressure Deformation as a function of temperature at constant pressure Discussion References
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  • 90
    Series available for loan
    Series available for loan
    Wilmette, Ill. : Snow Ice and Permafrost Research Establishment, Corps of Engineers, U.S. Army
    Associated volumes
    Call number: ZSP-202-69
    In: Research report / Cold Regions Research and Engineering Laboratory, 69
    Description / Table of Contents: Summary: The relations between rate of snow accumulation, snow density, snow age, and depth below the surface are formulated in terms of a compactive viscosity factor, which is assumed to be a function of only density and temperature, with parameters which will vary with the snow-type sequences of different climatic areas of high polar glaciers. The theory could be useful in an analysis of the data obtained from the large number of snow pits in Greenland, Ellesmere Island,and Antarctica.
    Type of Medium: Series available for loan
    Pages: iv, 8 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 69
    Language: English
    Note: CONTENTS Preface Summary Introduction The Sorge depth-density curve Generalization for time-variable rate of accumulation Path of a particle on the surface y=B(h,t) Effect of temperature Computational procedure Densification under high loads References
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  • 91
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    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-90
    In: Research report / Cold Regions Research and Engineering Laboratory, 90
    Description / Table of Contents: Summary: A new method is presented for extracting more meaningful information from snow profile data which will simplify the study of the permeability of snow. Earlier analyses normally employed statistical methods to determine property variations with depth, with the line of mean values established by the method of least squares. The mean curves derived in this manner may not represent properly the true nature of the snow pack, or aid in understanding the dynamic processes which are in action. The new graphical methods described distinguish the separate effects of densification and thermal metamorphism on permeability, permitting future advances in the analysis. Profile data obtained in 1954 and 1960 are reanalyzed using the new techniques. For a natural polar pack under conditions when no melting occurs and the accumulation is assumed continuous, the following conclusions may be made: permeability for a given density of snow increases with depth and time except possibly near the surface or at depths below 30 m; the rate of permeability change with depth for given densities decreases in a calculable way relative to the density; and, mean permeability changes with depth in a complex manner.
    Type of Medium: Series available for loan
    Pages: iv, 14, A3, B2, C2 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 90
    Language: English
    Note: CONTENTS Preface Summary Introduction Standard methods of data presentation- A class interval method of data presentation Interpretation of the numerical data Interpretation of thin sections Conclusions References Appendix A Appendix B Appendix C
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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-202-94
    In: Research report / Cold Regions Research and Engineering Laboratory, 94
    Description / Table of Contents: Summary: A new mechanism is described which explains the formation of moraines in the ablation areas of cold ice caps. The mechanism involves the freezing of water onto the bottom surface of an ice cap. This water comes from regions of the bottom surface where the combination of the geothermal heat and the heat produced by sliding of ice over the bed is sufficient to melt ice. A number of criticisms are made of the shear hypothesis, which has been advanced to explain moraines occurring on Baffin Island and near Thule, Greenland. It is concluded that this older hypothesis may be inadequate to account for these moraines. Although in theory the mechanism proposed here undoubtedly would lead to the formation of moraines, the existing field data are insufficient to prove conclusively that actual moraines have originated in this way.
    Type of Medium: Series available for loan
    Pages: iv, 12 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 94
    Language: English
    Note: CONTENTS Preface Summary Introduction Comments on the shear hypothesis Appearance of the debris layers The possibility of cold ice scraping up debris The shear across a debris layer The geometry of the debris layers Freezing model Theory Discussion Conclusion References
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  • 93
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-88
    In: Research report / Cold Regions Research and Engineering Laboratory, 88
    Description / Table of Contents: Summary: Four ground patterns were investigated by means of trenches cut in the outwash near Thule, Greenland: circular and linear depressions in unsorted material, polygonal troughs in unsorted material, sorted circles, and irregular mounds and depressions of low relief formed in unsorted finer grained material. Correlation is made between surface pattern, grain size and structure of the active layer, and type and distribution of ground ice for the patterns investigated. Classification of the active layer as disturbed, slightly disturbed, and undisturbed is based on the condition of primary depositional bedding and the presence or absence of vertical sorting. Other features of the active layer, depending upon its type, are an accumulation of fines at the bottom of the active layer and on top of stones, and a siliceous calcareous evaporite on the under surface and clean washed coarser particles beneath the larger stones. Fabric analysis of four kinds of ground ice is presented: ice wedge, relict ice, ice mass, and ice lens, as well as analysis of the contact of ice wedges with relict and mass ice. Practical applications, based on the conclusions, are given for the selection of foundation sites and the location of non-frost-susceptible building materials. NOTE: This is a very large file. Please give your browser several minutes to download the file.
    Type of Medium: Series available for loan
    Pages: viii, 79 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 88
    Language: English
    Note: CONTENTS Preface Summary Introduction Glossary Part 1 : Surface pattern, structure of the active layer, and type and distribution of ground ice in the permafrost Pattern type 1: Circular and linear depressions in unsorted outwash Circular depressions, area 1 Structure of the active layer Ground ice and its relation to surface morphology Linear depressions, area 5 Structure of the active layer Ground ice and its relation to surface morphology Pattern t ype 2 and 3: Polygonal troughs in unsorted outwash and sorted circles or centers of fines Area 3 Structure of the active layer Ground ice and its relation to surface morphology Area 4 Structure of the active layer Ground ice and its relat ion to surface morphology Pattern type 4: Mounds and depressions of low relief in unsorted outwash Area 4a Structure of the active layer Ground ice and its relatiop. to surface morphology Part 2: Ground ice studies Area 1 Lens ice History Appearance of the ice Fabric analysis Wedge ice History Appearance of the ice Fabric analysis Relict ice History Appearance of the ice Fabric analysis Contact between ice wedge and relict ice Ice sockets Area 5 Wedge ice Fabric analysis Relict ice Fabric analysis Area 3 Ice mass History Appearance of the ice Fabric analysis Ice wedge Fabric analysis Contact between ice mass and wedge Appearance of the ice Fabric analysis Summary and conclusions Pattern type 1: Linear and circular depressions in. unsorted outwash Pattern type 2: Polygonal troughs formed in unsorted outwash Pattern type 3: Sorted circles or centers of fines Pattern type 4: Mounds and depressions of low relief in fine-grained unsorted outwash Engineering applications References Appendix A: Associated studies Appendix B : Recommendations for further field and laboratory work Appendix C: Recommendations for field and laboratory techniques
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  • 94
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-95
    In: Research report / Cold Regions Research and Engineering Laboratory, 95
    Description / Table of Contents: Summary: An investigation was conducted at Camp Century, Greenland, to study the feasibility of using air wells to cool undersnow structures in the arctic during the summer months. From results obtained during the summers of 1959,and 1960 and late November, 1960, it was found that the air well is a practical and effective means of providing a -20°C air supply at volumetric flow rates of 1200 to 1700 ft^3/min. The extent and rate of warming of the snow beneath the trench floor by heat exchange between the air and the snow foundation was found to depend upon trench air temperature, fan capacity, fan arrangement, and casing length. For example, in a well cased to a depth of 17. 5 ft and equipped with a 5 hp fan drawing in air at a rate of 1700 ft^3/min, the maximum warming was found to be 12.5°C during a 42-day period. Snow temperature differences of about 7°C were found between similar trenches with and without a fan installation. The minimum permissible distance between two adjacent fans to eliminate, overlap in warming up the snow foundation is approximately 80 ft.
    Type of Medium: Series available for loan
    Pages: iv, 17 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 95
    Language: English
    Note: CONTENTS Preface Summary Theoretical background Test method and equipment Test operations Effectiveness of the air well Estimation of fan capacity Natural cooling in winter Change of trench foundation temperature Trench wall warm-up Conclusions and recommendations
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  • 95
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    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-100
    In: Research report / Cold Regions Research and Engineering Laboratory, 100
    Description / Table of Contents: From the Summary: During the summer of 1960, observations were made of ground fog on the Greenland Ice Cap and of sea fog in the Thule area in northwestern Greenland. A microscope-stage-fog impactor was designed, and its collection efficiency determined both empirically and by computation from the theoretical work of Langmuir and Blodgett (1946). The empirical efficiency was found to be considerably greater than the theoretical efficiency.
    Type of Medium: Series available for loan
    Pages: iv, 13 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 100
    Language: English
    Note: CONTENTS Preface Summary Introduction Method Design and operation of the impactor Collection efficiency Computation from theoretical values of Langmuir and Blodgett Empirical values Observations and results Fog on the ice cap Sea fog near Thule Discussion Conclusions References
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  • 96
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    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-105
    In: Research report / Cold Regions Research and Engineering Laboratory, 105
    Description / Table of Contents: Summary: A principle of particle segregation by freezing is presented. It is demonstrated experimentally by using a transparent freezing cabinet in which a sample of distilled water freezes from the bottom upward. In this way the freezing front line travels vertically and the particles are carried against gravity. By using the same material with different shapes (glass beads and broken quartz or glass) it is demonstrated that an important factor in particle migration is the shape of the particle or its contact area with the interface. By testing other materials with different shapes and sizes, it is demonstrated that another important factor is particle size and rate of freezing. Fine particles migrate under a wide range of rates of freezing; coarser ones migrate at lower and more limited ranges of rates of freezing. It is suggested that, for determining frost behavior of soils in permafrost regions, freezing from the bottom upward is a more reliable test than freezing from the top down. Freezing from the bottom more closely approximates freezing of the active layer above permafrost; also, friction with the cylinder testing wall is eliminated. The implication of this principle in engineering and studies of soil genesis in cold regions is emphasized.
    Type of Medium: Series available for loan
    Pages: iv, 8 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 105
    Language: English
    Note: CONTENTS Preface Summary Introduction Experimental procedure Experimental results Conclusions and recommendations References
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  • 97
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    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-108
    In: Research report / Cold Regions Research and Engineering Laboratory, 108
    Description / Table of Contents: Summary: The theory of snow densification is further developed on the basis of an exponential relation between viscosity and density. A linear relation between load-stress and strain rate is not valid for high stresses, and is replaced by a hyperbolic sine function. An empirical function is given for the temperature cycle correction. Two equations are derived for calculating depth-density curves with computers, and a simplified one for use with desk calculators. Instructions are given for determination of function parameters from field data. Four depth-density curves for Greenland and Antarctic locations are computed and graphed to show that the theory is useful.
    Type of Medium: Series available for loan
    Pages: iv, 18, A3, B5 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 108
    Language: English
    Note: CONTENTS Preface Summary Introduction Notation Stress analysis Analysis of densification process Non-Newtonian densification Equation for hyperbolic sine densification law Determination of parameters Discussion Glaciological engineering aspects References Appendix A: Example of calculation Appendix B: Snow density profiles
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  • 98
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    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-115
    In: Research report / Cold Regions Research and Engineering Laboratory, 115
    Description / Table of Contents: SUMMARY Between 1 July and 7 August 1960, the U.S. Army Snow Ice and Permafrost Research Establishment, Corps of Engineers, supported a £our-man glaciological expedition on the southern dome of the Greenland ice sheet. Measurements of snow temperature, density, ram hardness, and grain size were made at seven pit ~tudies along 191 mileS of over-snow traverse. In addition to the pit studies, 38 Rammsonde profiles were measured and 166 shallow pits were dug to measure temperature in the first meter of snow. The annual accumulation of snow was found to decrease westward, from 97 em water equivalent 50 miles from tP.e east coast, to 40 em 80 miles from the western margin. A possible precipitation shadow was encountered immediately west of the crest line of the ice sheet. The precipitation shadow and the decrease in accumulation westward indicate that the source area for the precipitation lies to the east of the southern dome, in the. Greenland Sea. Temperature profiles in the firn indicated that summer warming was still in progress. During August, melting at an elevation of 2000 m above se~ level was intense (OC in the top 75 em} •. According to the facies classification of glaciers (Benson, 1959, 1960}, most of the study area is in tfie percolation facies, with the possible exception of the westernmost· s.tation (mile l-138) which is at or near the saturation line. The daily heat exchange in the first meter of snow, near the time of maximum melt conditions, is between 20 and '35 cal/cinZ. This is approxi-mately 25o/o of the heat necessary to raise the temperature of a column of firn of unit cross Section and 1 m deep to the melting point. Effective values of thermal conductivity and diffusivity as determined from the temperature curves with no attempt made to isolate radiation and con-vection are, respectively, 4-6 x 10-3 cgs and 20-30 x 10-3 cgs. Radiation and convection in the first meter of firn cause "effective conductivity" values to be 4 to 7 times greater than the value k = 0. 0068pZ given by Abel's (1892), which is the conductivity at greater depths.
    Type of Medium: Series available for loan
    Pages: v, 22, A4, B1 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 115
    Language: English
    Note: CONTENTS Preface Summary Introduction Method of investigation Location Pit studies Temperature Hardness Density Stratigraphic measurements Thermal studies Stratigraphic features Grain size Grain shape Crusts Discussion of results Temperature Altitude gradient Latitude gradient Depth-density relationship Depth-load relationship Densification Stratigraphic analysis Facies relationship Climatological aspects 1960 meteorological observations Temperature Wind Barometric pressure Radiation Cloudiness Visibility Thermal studies Summary and conclusions References Appendix A Appendix B
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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-202-117
    In: Research report / Cold Regions Research and Engineering Laboratory, 117
    Description / Table of Contents: Summary: An experiment was designed to investigate operator-variance in the determination of the plastic limit of cohesive soils, independent of sample preparation and hydration time. A standard sample was prepared by dry-mixing commercial clay, "Grundite", with a pure silt. After the sample was hydrated for 3 weeks, five random samples were taken and five replicates performed on each sample. Analysis of variance (AOV) shows that there is no reason to doubt that the sample is homogeneous at the 0.05 level of significance. Random samples were then distributed to five zones of operators, where a zone is defined as a group of operators with similar backgrounds and engineering interests. Two operators from each group performed five replicates. The AOV model used in the analysis is mixed with the upper level fixed and the two lower levels random. The estimated "within" and "between" operator variances are 0. 45 and 4. 18 respectively. The estimated "between zones" contribution to the total sum of squares is negative. No correlation was found between an operator's internal variance and his deviation from the grand mean. On the basis of this experiment, no reason-exists to doubt that an "untrained" operator can obtain results comparable to those of professional operators. The major factor contributing to the total sample variance is the inconsistency between the individual operators who, although able to duplicate their own determinations, do not call the same end point. To minimize between operator variance, a readily prepared standard sample is suggested with which any operator can calibrate his plastic limit determinations against the expected national average.
    Type of Medium: Series available for loan
    Pages: iv, 8 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 117
    Language: English
    Note: CONTENTS Preface Summary ­Introduction Sample preparation Sample homogeneity Distribution of samples Analysis Conclusions and suggested standardization References
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    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
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    Call number: ZSP-202-118
    In: Research report / Cold Regions Research and Engineering Laboratory, 118
    Description / Table of Contents: Summary: The observation that newly frozen ice sheets, resulting from pools of -water freezing over,- support more than would be predicted by ordinary theory is assessed. A solution is presented for a circular plate on an elastic, sealed foundation. Graphical results are shown for supports at the circumference of the plate. Graphs to obtain moments in a circular plate on an elastic bearing surface, using a sealed or unsealed foundation, are compiled for fixed and simple supports. In reality the foundation may not be completely sealed, calling for discretion in selecting the actual moment. The ability of the refrozen ice sheet to support the extra load is explained by the fact that the water has been sealed between the surface and main sheet of ice and the volume occupied by the water cannot change.
    Type of Medium: Series available for loan
    Pages: iii, 14 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 118
    Language: English
    Location: AWI Archive
    Branch Library: AWI Library
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