Thermal gradients and rock weathering at low temperatures: Some simulation data
Abstract The heating of rock by insolation during subzero air temperatures may cause thermal stresses within that rock. The values of Δt may be such that fracturing due to thermal shock may occur. The uneven heating of a rock body may cause buttressing of the heated faces such that thermal stresses...
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crwiley:10.1002/ppp.3430020205 2024-09-15T18:30:16+00:00 Thermal gradients and rock weathering at low temperatures: Some simulation data Hall, Kevin Hall, Alida 1991 http://dx.doi.org/10.1002/ppp.3430020205 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fppp.3430020205 https://onlinelibrary.wiley.com/doi/pdf/10.1002/ppp.3430020205 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Permafrost and Periglacial Processes volume 2, issue 2, page 103-112 ISSN 1045-6740 1099-1530 journal-article 1991 crwiley https://doi.org/10.1002/ppp.3430020205 2024-06-25T04:13:50Z Abstract The heating of rock by insolation during subzero air temperatures may cause thermal stresses within that rock. The values of Δt may be such that fracturing due to thermal shock may occur. The uneven heating of a rock body may cause buttressing of the heated faces such that thermal stresses are accentuated. Upon removal of the heat source, rapid cooling may occur and values of Δt may be sufficient to cause thermal shock. Replications of these thermal stresses may lead to fatigue and failure. The zone within which these stresses may occur is also one within which freeze‐thaw can take place if water is present. It is suggested that thermally induced fracturing of rock in cold environments may be a significant but underrated process. Thermal results of laboratory simulation experiments are presented during which values of Δt = >500ºC/h occurred for short periods. Article in Journal/Newspaper Permafrost and Periglacial Processes Wiley Online Library Permafrost and Periglacial Processes 2 2 103 112 |
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English |
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Abstract The heating of rock by insolation during subzero air temperatures may cause thermal stresses within that rock. The values of Δt may be such that fracturing due to thermal shock may occur. The uneven heating of a rock body may cause buttressing of the heated faces such that thermal stresses are accentuated. Upon removal of the heat source, rapid cooling may occur and values of Δt may be sufficient to cause thermal shock. Replications of these thermal stresses may lead to fatigue and failure. The zone within which these stresses may occur is also one within which freeze‐thaw can take place if water is present. It is suggested that thermally induced fracturing of rock in cold environments may be a significant but underrated process. Thermal results of laboratory simulation experiments are presented during which values of Δt = >500ºC/h occurred for short periods. |
format |
Article in Journal/Newspaper |
author |
Hall, Kevin Hall, Alida |
spellingShingle |
Hall, Kevin Hall, Alida Thermal gradients and rock weathering at low temperatures: Some simulation data |
author_facet |
Hall, Kevin Hall, Alida |
author_sort |
Hall, Kevin |
title |
Thermal gradients and rock weathering at low temperatures: Some simulation data |
title_short |
Thermal gradients and rock weathering at low temperatures: Some simulation data |
title_full |
Thermal gradients and rock weathering at low temperatures: Some simulation data |
title_fullStr |
Thermal gradients and rock weathering at low temperatures: Some simulation data |
title_full_unstemmed |
Thermal gradients and rock weathering at low temperatures: Some simulation data |
title_sort |
thermal gradients and rock weathering at low temperatures: some simulation data |
publisher |
Wiley |
publishDate |
1991 |
url |
http://dx.doi.org/10.1002/ppp.3430020205 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fppp.3430020205 https://onlinelibrary.wiley.com/doi/pdf/10.1002/ppp.3430020205 |
genre |
Permafrost and Periglacial Processes |
genre_facet |
Permafrost and Periglacial Processes |
op_source |
Permafrost and Periglacial Processes volume 2, issue 2, page 103-112 ISSN 1045-6740 1099-1530 |
op_rights |
http://onlinelibrary.wiley.com/termsAndConditions#vor |
op_doi |
https://doi.org/10.1002/ppp.3430020205 |
container_title |
Permafrost and Periglacial Processes |
container_volume |
2 |
container_issue |
2 |
container_start_page |
103 |
op_container_end_page |
112 |
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1810471749768183808 |