Quantitative Field Observation on Frost Physical Weathering in the Great Wall Station Area

Field observing sites were set to measure frost weathering of bedrock in the Great Wall Station Area of Antarctica from 1988 to 1990. The result show that: (1), the weathering rate is higher in summer that in winter; (2), the weathering rate is greater at higher place that at lower place; (3), the w...

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Main Authors: Zhijiu, Cui, Heigang, Xiong
Format: Article in Journal/Newspaper
Language:English
Published: Polar Research Institute of China - PRIC 1992
Subjects:
Online Access:http://library.arcticportal.org/2050/
http://library.arcticportal.org/2050/1/A199202004.pdf
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spelling ftarcticportal:oai:generic.eprints.org:2050 2023-05-15T13:05:26+02:00 Quantitative Field Observation on Frost Physical Weathering in the Great Wall Station Area Zhijiu, Cui Heigang, Xiong 1992-12 application/pdf http://library.arcticportal.org/2050/ http://library.arcticportal.org/2050/1/A199202004.pdf en eng Polar Research Institute of China - PRIC http://library.arcticportal.org/2050/1/A199202004.pdf Zhijiu, Cui and Heigang, Xiong (1992) Quantitative Field Observation on Frost Physical Weathering in the Great Wall Station Area. Advances in Polar Science, 3 (2). pp. 32-37. Article PeerReviewed 1992 ftarcticportal 2023-04-05T22:52:04Z Field observing sites were set to measure frost weathering of bedrock in the Great Wall Station Area of Antarctica from 1988 to 1990. The result show that: (1), the weathering rate is higher in summer that in winter; (2), the weathering rate is greater at higher place that at lower place; (3), the weathering rate is higher in east and southeast slopes than in other slopes; (4), the weathering rate is greater in higher mean annual air temperature year than in lower year. Article in Journal/Newspaper Advances in Polar Science Antarc* Antarctica Polar Science Polar Science Arctic Portal Library Great Wall Station ENVELOPE(-58.970,-58.970,-62.217,-62.217)
institution Open Polar
collection Arctic Portal Library
op_collection_id ftarcticportal
language English
description Field observing sites were set to measure frost weathering of bedrock in the Great Wall Station Area of Antarctica from 1988 to 1990. The result show that: (1), the weathering rate is higher in summer that in winter; (2), the weathering rate is greater at higher place that at lower place; (3), the weathering rate is higher in east and southeast slopes than in other slopes; (4), the weathering rate is greater in higher mean annual air temperature year than in lower year.
format Article in Journal/Newspaper
author Zhijiu, Cui
Heigang, Xiong
spellingShingle Zhijiu, Cui
Heigang, Xiong
Quantitative Field Observation on Frost Physical Weathering in the Great Wall Station Area
author_facet Zhijiu, Cui
Heigang, Xiong
author_sort Zhijiu, Cui
title Quantitative Field Observation on Frost Physical Weathering in the Great Wall Station Area
title_short Quantitative Field Observation on Frost Physical Weathering in the Great Wall Station Area
title_full Quantitative Field Observation on Frost Physical Weathering in the Great Wall Station Area
title_fullStr Quantitative Field Observation on Frost Physical Weathering in the Great Wall Station Area
title_full_unstemmed Quantitative Field Observation on Frost Physical Weathering in the Great Wall Station Area
title_sort quantitative field observation on frost physical weathering in the great wall station area
publisher Polar Research Institute of China - PRIC
publishDate 1992
url http://library.arcticportal.org/2050/
http://library.arcticportal.org/2050/1/A199202004.pdf
long_lat ENVELOPE(-58.970,-58.970,-62.217,-62.217)
geographic Great Wall Station
geographic_facet Great Wall Station
genre Advances in Polar Science
Antarc*
Antarctica
Polar Science
Polar Science
genre_facet Advances in Polar Science
Antarc*
Antarctica
Polar Science
Polar Science
op_relation http://library.arcticportal.org/2050/1/A199202004.pdf
Zhijiu, Cui and Heigang, Xiong (1992) Quantitative Field Observation on Frost Physical Weathering in the Great Wall Station Area. Advances in Polar Science, 3 (2). pp. 32-37.
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