Water migration and ice segregation in the transition zone between thawed and frozen soil
Abstract Samples of silty clay were kept under constant boundary temperature conditions of +1°C (top) and −1°C (bottom) in a series of cold room laboratory experiments. Water migration and ice enrichment near the permafrost table were observed in all samples. Cryogenic layering was observed in soil...
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crwiley:10.1002/ppp.3430050307 2024-06-02T08:07:59+00:00 Water migration and ice segregation in the transition zone between thawed and frozen soil Solomatin, V. I. Xu, Xiaozu 1994 http://dx.doi.org/10.1002/ppp.3430050307 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fppp.3430050307 https://onlinelibrary.wiley.com/doi/pdf/10.1002/ppp.3430050307 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Permafrost and Periglacial Processes volume 5, issue 3, page 185-190 ISSN 1045-6740 1099-1530 journal-article 1994 crwiley https://doi.org/10.1002/ppp.3430050307 2024-05-03T11:19:25Z Abstract Samples of silty clay were kept under constant boundary temperature conditions of +1°C (top) and −1°C (bottom) in a series of cold room laboratory experiments. Water migration and ice enrichment near the permafrost table were observed in all samples. Cryogenic layering was observed in soil layers with boundary temperature conditions of −0.5 to −1.0°C. These results confirm earlier observations which explain the occurrence of an ice‐rich layer near the permafrost table, and they may be used to explain the influence of snow cover on isotopic composition of near‐surface ground water and ice. Article in Journal/Newspaper Ice permafrost Permafrost and Periglacial Processes Wiley Online Library Permafrost and Periglacial Processes 5 3 185 190 |
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Open Polar |
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Wiley Online Library |
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crwiley |
language |
English |
description |
Abstract Samples of silty clay were kept under constant boundary temperature conditions of +1°C (top) and −1°C (bottom) in a series of cold room laboratory experiments. Water migration and ice enrichment near the permafrost table were observed in all samples. Cryogenic layering was observed in soil layers with boundary temperature conditions of −0.5 to −1.0°C. These results confirm earlier observations which explain the occurrence of an ice‐rich layer near the permafrost table, and they may be used to explain the influence of snow cover on isotopic composition of near‐surface ground water and ice. |
format |
Article in Journal/Newspaper |
author |
Solomatin, V. I. Xu, Xiaozu |
spellingShingle |
Solomatin, V. I. Xu, Xiaozu Water migration and ice segregation in the transition zone between thawed and frozen soil |
author_facet |
Solomatin, V. I. Xu, Xiaozu |
author_sort |
Solomatin, V. I. |
title |
Water migration and ice segregation in the transition zone between thawed and frozen soil |
title_short |
Water migration and ice segregation in the transition zone between thawed and frozen soil |
title_full |
Water migration and ice segregation in the transition zone between thawed and frozen soil |
title_fullStr |
Water migration and ice segregation in the transition zone between thawed and frozen soil |
title_full_unstemmed |
Water migration and ice segregation in the transition zone between thawed and frozen soil |
title_sort |
water migration and ice segregation in the transition zone between thawed and frozen soil |
publisher |
Wiley |
publishDate |
1994 |
url |
http://dx.doi.org/10.1002/ppp.3430050307 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fppp.3430050307 https://onlinelibrary.wiley.com/doi/pdf/10.1002/ppp.3430050307 |
genre |
Ice permafrost Permafrost and Periglacial Processes |
genre_facet |
Ice permafrost Permafrost and Periglacial Processes |
op_source |
Permafrost and Periglacial Processes volume 5, issue 3, page 185-190 ISSN 1045-6740 1099-1530 |
op_rights |
http://onlinelibrary.wiley.com/termsAndConditions#vor |
op_doi |
https://doi.org/10.1002/ppp.3430050307 |
container_title |
Permafrost and Periglacial Processes |
container_volume |
5 |
container_issue |
3 |
container_start_page |
185 |
op_container_end_page |
190 |
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1800753128294842368 |