Thermal conductivity of soils in the active layer of Eastern Siberia | Zendy

Brouchkov Anatoli | Zendy; Fukuda Masami | Zendy; Iwahana Go | Zendy; Kobayashi Yoshikazu | Zendy; Konstantinov Pavel | Zendy

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Thermal conductivity of soils in the active layer of Eastern Siberia

Author(s) -

Brouchkov Anatoli,

Fukuda Masami,

Iwahana Go,

Kobayashi Yoshikazu,

Konstantinov Pavel

Publication year - 2005

Publication title -

permafrost and periglacial processes

Language(s) - English

Resource type - Journals

SCImago Journal Rank - 0.867

H-Index - 76

eISSN - 1099-1530

pISSN - 1045-6740

DOI - 10.1002/ppp.502

Subject(s) - permafrost , active layer , soil water , geology , thermal conductivity , soil science , thermal , layer (electronics) , earth science , geomorphology , materials science , composite material , meteorology , geography , oceanography , thin film transistor

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.

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