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1. |
Salt fretting and chemical weathering in the Darwin mountains and the dry valleys, Victoria Land, Antarctica |
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Polar Geography and Geology,
Volume 7,
Issue 2,
1983,
Page 83-122
Franz‐Dieter Miotke,
Renate von Hodenberg,
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摘要:
The paper consists of two main parts. The more general first part deals with chemical weathering processes in Victoria Land, Antarctica, where salt occurrences and salt‐fretting were studied. The regional second part reports on similar research carried out in the Darwin Mountains (80°S) where microclimatic conditions of weathering processes during the antarctic summer were investigated. Temperatures in different rocks, in soils and in snow were recorded by thermistors, and the moisture content was determined. In summer, temperatures close to the surface of rocks and soils reach well above freezing point, ranging often from 10°C to a maximum above 30°C. Water infiltrates into the soil only where snow melts; here for a short period of time the water necessary for chemical weathering is available. The salts present in rocks and soils were mineralogically analyzed. Most of the salts collected consist of calcite, mirabilite, thenardite, and halite. On the basis of the measurements taken, the water circulation within the soils and the processes of salt migration as well as salt‐fretting are discussed in some detail. It is suggested that the so‐called “inner rock polygons”; described here for the first time result from thermal contraction during the winter months when temperatures drop to well below ‐50°C. These cracks are considered to be of major importance for salt‐fretting and frost shattering. Following a brief geomorphological description of the Darwin Mountains region, daily summer temperature curves from snow, rocks, and soil are presented and discussed. (Previous papers by the senior author on this general research area appeared inPolar Geography and GeologyApril‐June 1982.) (Translation by William Barr, University of Saskatchewan, Saskatoon.)
ISSN:0273-8457
DOI:10.1080/10889378309377191
出版商:Taylor & Francis Group
年代:1983
数据来源: Taylor
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2. |
Annual totals of the positive and negative mean daily air temperatures in the Arctic |
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Polar Geography and Geology,
Volume 7,
Issue 2,
1983,
Page 123-129
L. S. Petrov,
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摘要:
The author presents maps of the mean annual totals of positive and negative daily temperatures in the Arctic and analyzes their distribution and year‐to‐year variability. (The translation is by Elena Baranov, University of Kansas, Lawrence.)
ISSN:0273-8457
DOI:10.1080/10889378309377192
出版商:Taylor & Francis Group
年代:1983
数据来源: Taylor
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3. |
The climatic opposition in the Arctic |
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Polar Geography and Geology,
Volume 7,
Issue 2,
1983,
Page 130-137
A. I. Voskresenskiy,
A. N. Lyubarskiy,
L. S. Petrov,
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摘要:
The authors examine the peculiarities of localization of mean annual fluctuations of the temperature regime and ice conditions in the western and eastern sectors of the Soviet Arctic and analyze possible physical causes of the opposition that is revealed. (Paper read at a Soviet‐American symposium in Tbilisi, October 1979.) (The translation is by Elena Baranov, University of Kansas, Lawrence.)
ISSN:0273-8457
DOI:10.1080/10889378309377193
出版商:Taylor & Francis Group
年代:1983
数据来源: Taylor
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4. |
Latitudinal asymmetry of environmental factors during the glacial periods in the Northern Hemisphere |
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Polar Geography and Geology,
Volume 7,
Issue 2,
1983,
Page 138-158
A. A. Velichko,
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摘要:
The author describes the spatial patterns of glaciation, permafrost, vegetation and other features in both the Eastern and Western hemispheres during glacial periods. These patterns are compared to present‐day conditions. A model of atmospheric circulation is proposed to explain the distribution of these phenomena. (The translation is by Elena Baranov, University of Kansas, Lawrence.)
ISSN:0273-8457
DOI:10.1080/10889378309377194
出版商:Taylor & Francis Group
年代:1983
数据来源: Taylor
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5. |
The development of late ice age and early Holocene glaciation in the Arctic |
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Polar Geography and Geology,
Volume 7,
Issue 2,
1983,
Page 159-168
J.‐M. Punning,
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摘要:
Using the well known Camp Century oxygen‐isotope curve, the author examines the effect that changes in environmental conditions have had on δ18O values. The data from paleogeographical and geochronological studies are used to formulate a theoretical basis for the development of glaciation in the Arctic 13,000–7,000 years ago. Glacial events are then correlated with the observed variation of δ18O in ice core samples. The role of oxygen‐isotope curves in detecting regional climatic changes and in reconstructing past environments is also discussed. Finally, the problem of the stratigraphic classification of ice cores is considered in this article. (The translation is by Elena Baranov, University of Kansas, Lawrence.)
ISSN:0273-8457
DOI:10.1080/10889378309377195
出版商:Taylor & Francis Group
年代:1983
数据来源: Taylor
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6. |
News notes |
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Polar Geography and Geology,
Volume 7,
Issue 2,
1983,
Page 169-171
Theodore Shabad,
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ISSN:0273-8457
DOI:10.1080/10889378309377196
出版商:Taylor & Francis Group
年代:1983
数据来源: Taylor
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7. |
Editorial board |
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Polar Geography and Geology,
Volume 7,
Issue 2,
1983,
Page -
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PDF (66KB)
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ISSN:0273-8457
DOI:10.1080/10889378309377190
出版商:Taylor & Francis Group
年代:1983
数据来源: Taylor
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