Differential frost heave, load casting and convection: Converging mechanisms; a discussion of the origin of cryoturbations
Abstract This paper reviews and discusses the main mechanisms involved in cryoturbation processes and patterned ground. The arguments are based upon field, thermal, moisture and micromorphological data in relation to cryogenic fabric stability and local hydraulic conditions. Differential frost heavi...
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crwiley:10.1002/ppp.3430020207 2024-06-02T08:13:10+00:00 Differential frost heave, load casting and convection: Converging mechanisms; a discussion of the origin of cryoturbations Van Vliet‐Lanoë, Brigitte 1991 http://dx.doi.org/10.1002/ppp.3430020207 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fppp.3430020207 https://onlinelibrary.wiley.com/doi/pdf/10.1002/ppp.3430020207 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Permafrost and Periglacial Processes volume 2, issue 2, page 123-139 ISSN 1045-6740 1099-1530 journal-article 1991 crwiley https://doi.org/10.1002/ppp.3430020207 2024-05-03T11:57:22Z Abstract This paper reviews and discusses the main mechanisms involved in cryoturbation processes and patterned ground. The arguments are based upon field, thermal, moisture and micromorphological data in relation to cryogenic fabric stability and local hydraulic conditions. Differential frost heaving appears to be the main mechanism of cryoturbation, but its action can be helped by cryostatic pressures, by differential swelling and probably also by load casting in poorly drained sites. Differential frost heaving can be emphasized if organics are present. Frost‐susceptibility gradients provide an understanding of the geometry of deformations. Article in Journal/Newspaper Permafrost and Periglacial Processes Wiley Online Library Permafrost and Periglacial Processes 2 2 123 139 |
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Open Polar |
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Wiley Online Library |
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crwiley |
language |
English |
description |
Abstract This paper reviews and discusses the main mechanisms involved in cryoturbation processes and patterned ground. The arguments are based upon field, thermal, moisture and micromorphological data in relation to cryogenic fabric stability and local hydraulic conditions. Differential frost heaving appears to be the main mechanism of cryoturbation, but its action can be helped by cryostatic pressures, by differential swelling and probably also by load casting in poorly drained sites. Differential frost heaving can be emphasized if organics are present. Frost‐susceptibility gradients provide an understanding of the geometry of deformations. |
format |
Article in Journal/Newspaper |
author |
Van Vliet‐Lanoë, Brigitte |
spellingShingle |
Van Vliet‐Lanoë, Brigitte Differential frost heave, load casting and convection: Converging mechanisms; a discussion of the origin of cryoturbations |
author_facet |
Van Vliet‐Lanoë, Brigitte |
author_sort |
Van Vliet‐Lanoë, Brigitte |
title |
Differential frost heave, load casting and convection: Converging mechanisms; a discussion of the origin of cryoturbations |
title_short |
Differential frost heave, load casting and convection: Converging mechanisms; a discussion of the origin of cryoturbations |
title_full |
Differential frost heave, load casting and convection: Converging mechanisms; a discussion of the origin of cryoturbations |
title_fullStr |
Differential frost heave, load casting and convection: Converging mechanisms; a discussion of the origin of cryoturbations |
title_full_unstemmed |
Differential frost heave, load casting and convection: Converging mechanisms; a discussion of the origin of cryoturbations |
title_sort |
differential frost heave, load casting and convection: converging mechanisms; a discussion of the origin of cryoturbations |
publisher |
Wiley |
publishDate |
1991 |
url |
http://dx.doi.org/10.1002/ppp.3430020207 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fppp.3430020207 https://onlinelibrary.wiley.com/doi/pdf/10.1002/ppp.3430020207 |
genre |
Permafrost and Periglacial Processes |
genre_facet |
Permafrost and Periglacial Processes |
op_source |
Permafrost and Periglacial Processes volume 2, issue 2, page 123-139 ISSN 1045-6740 1099-1530 |
op_rights |
http://onlinelibrary.wiley.com/termsAndConditions#vor |
op_doi |
https://doi.org/10.1002/ppp.3430020207 |
container_title |
Permafrost and Periglacial Processes |
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2 |
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2 |
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123 |
op_container_end_page |
139 |
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1800736550837813248 |