Thermal conductivity of frozen soils
Thermal conductivity measurements of two frozen soils, Leda clay and Sudbury silty clay, taken at temperatures between 0 and -22 degrees C by means of a thermal probe and a transient heat flow technique, compare favorably with estimates of thermal conductivity calculated by the DeVries method. Both...
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Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
1970
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Online Access: | https://nrc-publications.canada.ca/eng/view/ft/?id=01a20e33-74a4-4d5d-a2af-78257128e068 https://nrc-publications.canada.ca/eng/view/object/?id=01a20e33-74a4-4d5d-a2af-78257128e068 https://nrc-publications.canada.ca/fra/voir/objet/?id=01a20e33-74a4-4d5d-a2af-78257128e068 |