Permafrost and groundwater conditions, Huola river basin, northeast China
Abstract Permafrost and geohydrological investigations in a small basin in northeast China indicate that permafrost affects both the depth at which groundwater occurs and its artesian pressure. Artesian flow in the basin is common, and artesian head may be as much as 10 m above ground surface. The t...
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crwiley:10.1002/ppp.3430010106 2024-09-15T18:11:27+00:00 Permafrost and groundwater conditions, Huola river basin, northeast China Wang, Baolai 1990 http://dx.doi.org/10.1002/ppp.3430010106 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fppp.3430010106 https://onlinelibrary.wiley.com/doi/pdf/10.1002/ppp.3430010106 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Permafrost and Periglacial Processes volume 1, issue 1, page 45-52 ISSN 1045-6740 1099-1530 journal-article 1990 crwiley https://doi.org/10.1002/ppp.3430010106 2024-07-30T04:18:47Z Abstract Permafrost and geohydrological investigations in a small basin in northeast China indicate that permafrost affects both the depth at which groundwater occurs and its artesian pressure. Artesian flow in the basin is common, and artesian head may be as much as 10 m above ground surface. The thickness of permafrost bears a close relationship to groundwater discharge (i.e. artesian flow rate), since a number of boreholes indicate that the greater the discharge, the thinner the permafrost. Over time the average rate of artesian flow from the boreholes decreases. The duration of flow depends on the rate of artesian flow, and permafrost temperature and thickness. Long‐term observations in areas where the permafrost is 70 m thick and has a mean annual ground temperature of −2.5°C indicate that if flow rate is larger than 0.8 l/s, flow continues for an indefinite period of time, but that if flow is less than 0.6 l/s, flow stops shortly. The difference in permafrost thickness, caused by the differential development of fractures and associated artesian head, may be as great as 50 m. Massive ground ice, with a thickness of more than 20 m, occurs in some boreholes at depth and is probably intrusive in nature. Article in Journal/Newspaper Ice permafrost Permafrost and Periglacial Processes Wiley Online Library Permafrost and Periglacial Processes 1 1 45 52 |
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English |
description |
Abstract Permafrost and geohydrological investigations in a small basin in northeast China indicate that permafrost affects both the depth at which groundwater occurs and its artesian pressure. Artesian flow in the basin is common, and artesian head may be as much as 10 m above ground surface. The thickness of permafrost bears a close relationship to groundwater discharge (i.e. artesian flow rate), since a number of boreholes indicate that the greater the discharge, the thinner the permafrost. Over time the average rate of artesian flow from the boreholes decreases. The duration of flow depends on the rate of artesian flow, and permafrost temperature and thickness. Long‐term observations in areas where the permafrost is 70 m thick and has a mean annual ground temperature of −2.5°C indicate that if flow rate is larger than 0.8 l/s, flow continues for an indefinite period of time, but that if flow is less than 0.6 l/s, flow stops shortly. The difference in permafrost thickness, caused by the differential development of fractures and associated artesian head, may be as great as 50 m. Massive ground ice, with a thickness of more than 20 m, occurs in some boreholes at depth and is probably intrusive in nature. |
format |
Article in Journal/Newspaper |
author |
Wang, Baolai |
spellingShingle |
Wang, Baolai Permafrost and groundwater conditions, Huola river basin, northeast China |
author_facet |
Wang, Baolai |
author_sort |
Wang, Baolai |
title |
Permafrost and groundwater conditions, Huola river basin, northeast China |
title_short |
Permafrost and groundwater conditions, Huola river basin, northeast China |
title_full |
Permafrost and groundwater conditions, Huola river basin, northeast China |
title_fullStr |
Permafrost and groundwater conditions, Huola river basin, northeast China |
title_full_unstemmed |
Permafrost and groundwater conditions, Huola river basin, northeast China |
title_sort |
permafrost and groundwater conditions, huola river basin, northeast china |
publisher |
Wiley |
publishDate |
1990 |
url |
http://dx.doi.org/10.1002/ppp.3430010106 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fppp.3430010106 https://onlinelibrary.wiley.com/doi/pdf/10.1002/ppp.3430010106 |
genre |
Ice permafrost Permafrost and Periglacial Processes |
genre_facet |
Ice permafrost Permafrost and Periglacial Processes |
op_source |
Permafrost and Periglacial Processes volume 1, issue 1, page 45-52 ISSN 1045-6740 1099-1530 |
op_rights |
http://onlinelibrary.wiley.com/termsAndConditions#vor |
op_doi |
https://doi.org/10.1002/ppp.3430010106 |
container_title |
Permafrost and Periglacial Processes |
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1 |
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1 |
container_start_page |
45 |
op_container_end_page |
52 |
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1810449038349172736 |