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Thermal conductivity of soils in the active layer of Eastern Siberia

Author

Listed:
  • Anatoli Brouchkov
  • Masami Fukuda
  • Go Iwahana
  • Yoshikazu Kobayashi
  • Pavel Konstantinov

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.

Suggested Citation

  • Anatoli Brouchkov & Masami Fukuda & Go Iwahana & Yoshikazu Kobayashi & Pavel Konstantinov, 2005. "Thermal conductivity of soils in the active layer of Eastern Siberia," Permafrost and Periglacial Processes, John Wiley & Sons, vol. 16(2), pages 217-222, April.
    • Handle: RePEc:wly:perpro:v:16:y:2005:i:2:p:217-222
    DOI: 10.1002/ppp.502
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