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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Bibliographic Details
Main Author: Penner, E.
Format: Article in Journal/Newspaper
Language:English
Published: 1970
Subjects:
ice
sol
Ice
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