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Wiley, Permafrost and Periglacial Processes, 2(16), p. 217-222, 2005

DOI: 10.1002/ppp.502

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Thermal conductivity of soils in the active layer of Eastern Siberia

Journal article published in 2005 by Anatoli Brouchkov, Masami Fukuda, Go Iwahana ORCID, Yoshikazu Kobayashi, Pavel Konstantinov
This paper was not found in any repository, but could be made available legally by the author.
This paper was not found in any repository, but could be made available legally by the author.

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Abstract

Landscape changes accompanied by changes in soil properties occur in Central Siberia as a result of forest fire, surface processes and human impact. A non-steady-state technique tested the thermal properties of Siberian soils. Thermal conductivity of thawed soil increases in the active layer at depths of 5 and 30 cm after fire, especially in the organic layer due to an increase in density. Copyright # 2005 John Wiley & Sons, Ltd.