The Ground thermal regime with special reference to the occurrence of permafrost
This thesis deals with the ground thermal regime and specific reference is made to the occurrence of Permafrost. Consideration is given to the thermal characteristics of soils in that various methods for determining the specific heat and the thermal conductivity of soils are reviewed. The methods pr...
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1971
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ftcarletonuniv:oai:curve.carleton.ca:30513 2023-05-15T17:55:49+02:00 The Ground thermal regime with special reference to the occurrence of permafrost Gale, Charles Moore 1971 https://curve.carleton.ca/2b36883e-d132-4158-88dc-f3fe313cd961 http://catalogue.library.carleton.ca/record=b1960730 https://doi.org/10.22215/etd/1971-12803 unknown https://curve.carleton.ca/2b36883e-d132-4158-88dc-f3fe313cd961 http://catalogue.library.carleton.ca/record=b1960730 https://doi.org/10.22215/etd/1971-12803 Thesis/Dissertation 1971 ftcarletonuniv https://doi.org/10.22215/etd/1971-12803 2022-01-23T08:12:13Z This thesis deals with the ground thermal regime and specific reference is made to the occurrence of Permafrost. Consideration is given to the thermal characteristics of soils in that various methods for determining the specific heat and the thermal conductivity of soils are reviewed. The methods presented for determing these soil characteristics were chosen because they represent traditional, present, and future methods for determining the characteristics. An examination is then made of various factors which affect the ground thermal regime in Permafrost regions. Consideration is given to such items as air temperature, topography, water, vegetation, and climate. Some papers are reviewed which discuss these factors and an attempt is made to present general relationships between these factors and the ground thermal regime in Permafrost regions. Thesis permafrost CURVE - Carleton University Research Virtual Environment |
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Open Polar |
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CURVE - Carleton University Research Virtual Environment |
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ftcarletonuniv |
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unknown |
description |
This thesis deals with the ground thermal regime and specific reference is made to the occurrence of Permafrost. Consideration is given to the thermal characteristics of soils in that various methods for determining the specific heat and the thermal conductivity of soils are reviewed. The methods presented for determing these soil characteristics were chosen because they represent traditional, present, and future methods for determining the characteristics. An examination is then made of various factors which affect the ground thermal regime in Permafrost regions. Consideration is given to such items as air temperature, topography, water, vegetation, and climate. Some papers are reviewed which discuss these factors and an attempt is made to present general relationships between these factors and the ground thermal regime in Permafrost regions. |
format |
Thesis |
author |
Gale, Charles Moore |
spellingShingle |
Gale, Charles Moore The Ground thermal regime with special reference to the occurrence of permafrost |
author_facet |
Gale, Charles Moore |
author_sort |
Gale, Charles Moore |
title |
The Ground thermal regime with special reference to the occurrence of permafrost |
title_short |
The Ground thermal regime with special reference to the occurrence of permafrost |
title_full |
The Ground thermal regime with special reference to the occurrence of permafrost |
title_fullStr |
The Ground thermal regime with special reference to the occurrence of permafrost |
title_full_unstemmed |
The Ground thermal regime with special reference to the occurrence of permafrost |
title_sort |
ground thermal regime with special reference to the occurrence of permafrost |
publishDate |
1971 |
url |
https://curve.carleton.ca/2b36883e-d132-4158-88dc-f3fe313cd961 http://catalogue.library.carleton.ca/record=b1960730 https://doi.org/10.22215/etd/1971-12803 |
genre |
permafrost |
genre_facet |
permafrost |
op_relation |
https://curve.carleton.ca/2b36883e-d132-4158-88dc-f3fe313cd961 http://catalogue.library.carleton.ca/record=b1960730 https://doi.org/10.22215/etd/1971-12803 |
op_doi |
https://doi.org/10.22215/etd/1971-12803 |
_version_ |
1766163823442526208 |