Frost heave and dry density changes during cyclic freeze‐thaw of a silty clay
Abstract Open‐system frost heave tests were performed on a silty clay using a lower boundary condition of +2°C and unidirectional freezing at −10°C from the surface, or freezing and thawing with an upper boundary temperature that cycled from −10°C to +10°C or from −10°C to 0°C. The amount of frost h...
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Online Access: | http://dx.doi.org/10.1002/ppp.636 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fppp.636 https://onlinelibrary.wiley.com/doi/pdf/10.1002/ppp.636 |
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crwiley:10.1002/ppp.636 2024-06-02T08:13:10+00:00 Frost heave and dry density changes during cyclic freeze‐thaw of a silty clay Hui, Bing Ping, He 2009 http://dx.doi.org/10.1002/ppp.636 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fppp.636 https://onlinelibrary.wiley.com/doi/pdf/10.1002/ppp.636 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Permafrost and Periglacial Processes volume 20, issue 1, page 65-70 ISSN 1045-6740 1099-1530 journal-article 2009 crwiley https://doi.org/10.1002/ppp.636 2024-05-03T11:21:02Z Abstract Open‐system frost heave tests were performed on a silty clay using a lower boundary condition of +2°C and unidirectional freezing at −10°C from the surface, or freezing and thawing with an upper boundary temperature that cycled from −10°C to +10°C or from −10°C to 0°C. The amount of frost heave, the distribution of moisture at the end of the experiment and the final dry density profiles all differed for the three cases. The experiments demonstrate that freeze‐thaw history is important in assessing or predicting the frost heave of silty clays. Copyright © 2009 John Wiley & Sons, Ltd. Article in Journal/Newspaper Permafrost and Periglacial Processes Wiley Online Library Permafrost and Periglacial Processes 20 1 65 70 |
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Open Polar |
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Wiley Online Library |
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crwiley |
language |
English |
description |
Abstract Open‐system frost heave tests were performed on a silty clay using a lower boundary condition of +2°C and unidirectional freezing at −10°C from the surface, or freezing and thawing with an upper boundary temperature that cycled from −10°C to +10°C or from −10°C to 0°C. The amount of frost heave, the distribution of moisture at the end of the experiment and the final dry density profiles all differed for the three cases. The experiments demonstrate that freeze‐thaw history is important in assessing or predicting the frost heave of silty clays. Copyright © 2009 John Wiley & Sons, Ltd. |
format |
Article in Journal/Newspaper |
author |
Hui, Bing Ping, He |
spellingShingle |
Hui, Bing Ping, He Frost heave and dry density changes during cyclic freeze‐thaw of a silty clay |
author_facet |
Hui, Bing Ping, He |
author_sort |
Hui, Bing |
title |
Frost heave and dry density changes during cyclic freeze‐thaw of a silty clay |
title_short |
Frost heave and dry density changes during cyclic freeze‐thaw of a silty clay |
title_full |
Frost heave and dry density changes during cyclic freeze‐thaw of a silty clay |
title_fullStr |
Frost heave and dry density changes during cyclic freeze‐thaw of a silty clay |
title_full_unstemmed |
Frost heave and dry density changes during cyclic freeze‐thaw of a silty clay |
title_sort |
frost heave and dry density changes during cyclic freeze‐thaw of a silty clay |
publisher |
Wiley |
publishDate |
2009 |
url |
http://dx.doi.org/10.1002/ppp.636 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fppp.636 https://onlinelibrary.wiley.com/doi/pdf/10.1002/ppp.636 |
genre |
Permafrost and Periglacial Processes |
genre_facet |
Permafrost and Periglacial Processes |
op_source |
Permafrost and Periglacial Processes volume 20, issue 1, page 65-70 ISSN 1045-6740 1099-1530 |
op_rights |
http://onlinelibrary.wiley.com/termsAndConditions#vor |
op_doi |
https://doi.org/10.1002/ppp.636 |
container_title |
Permafrost and Periglacial Processes |
container_volume |
20 |
container_issue |
1 |
container_start_page |
65 |
op_container_end_page |
70 |
_version_ |
1800736563954450432 |