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Temperature regime of tundra soils and underlying permafrost (Northeastern European Russia)
Kaverin D.A.; Pastukhov A.V.; Mazhitova G.G.
发表日期2014
ISSN15607496
卷号18期号:3
英文摘要Temperature regime has been studied in seven permafrost soils formed in mineral and peat soil-forming deposits in various landscapes of the southern tundra in Northeastern European Russia. Seasonal and long-term temperature dynamics has been revealed in both active layer and underlying permafrost. Soil temperature regime has been classified according to the Russian and American systems. The differentiation of permafrost soils has been shown according to the main temperature parameters.
英文关键词Active layer; Permafrost; Permafrost-affected soils; Temperature regime
学科领域active layer; permafrost; soil temperature; tundra soil; Russian Federation
语种英语
scopus关键词active layer; permafrost; soil temperature; tundra soil; Russian Federation
来源期刊Earth's Cryosphere
文献类型期刊论文
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/120219
作者单位Institute of Biology, Komi Scientific Center, UB RAS, Kommunisticheskya Str., 28, Syktyvkar, 167982, Russian Federation
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Kaverin D.A.,Pastukhov A.V.,Mazhitova G.G.. Temperature regime of tundra soils and underlying permafrost (Northeastern European Russia)[J],2014,18(3).
APA Kaverin D.A.,Pastukhov A.V.,&Mazhitova G.G..(2014).Temperature regime of tundra soils and underlying permafrost (Northeastern European Russia).Earth's Cryosphere,18(3).
MLA Kaverin D.A.,et al."Temperature regime of tundra soils and underlying permafrost (Northeastern European Russia)".Earth's Cryosphere 18.3(2014).
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