Thermal conductivity of soils in the active layer of Eastern Siberia

Anatoli Brouchkov, Masami Fukuda, Go Iwahana, Yoshikazu Kobayashi and Pavel Konstantinov

Permafrost and Periglacial Processes, 2005, vol. 16, issue 2, 217-222

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.

Date: 2005
References: Add references at CitEc
Citations:

Downloads: (external link)
https://doi.org/10.1002/ppp.502

Related works:
This item may be available elsewhere in EconPapers: Search for items with the same title.

Export reference: BibTeX RIS (EndNote, ProCite, RefMan) HTML/Text

Persistent link: https://EconPapers.repec.org/RePEc:wly:perpro:v:16:y:2005:i:2:p:217-222

Access Statistics for this article

More articles in Permafrost and Periglacial Processes from John Wiley & Sons
Bibliographic data for series maintained by Wiley Content Delivery ().