Factors controlling near surface ground-ice characteristics in a region of warm permafrost, Beiluhe Basin, Qinghai-Tibet Plateau

Author:

Lin Zhanju,Gao Zeyong,Fan Xingwen,Niu Fujun,Luo Jing,Yin Guoan,Liu Minghao

Funder

National Natural Science Foundation of China

State Key Laboratory of Frozen Soil Engineering

Chinese Academy of Sciences

Publisher

Elsevier BV

Subject

Soil Science

Reference85 articles.

1. Ground ice in the sedimentary rocks and kimberlites of Yakutia, Russia;Alexeev;Permafrost Periglac. Process.,2002

2. Burn, C. R., Smith, M. W., 1985. On the origin of aggradational ice in permafrost. In: Anderson, D.M., Williams, P.J. (Eds.), Freezing and thawing of soil-water systems. Technical Council on Cold Regions Engineering Monograph, American Society of Civil Engineers, New York, PP. 77–84.

3. The development of near-surface ground ice during the Holocene at sites near Mayo, Yukon Territory, Canada;Burn;J. Quaternary Sci.,1988

4. Permafrost and climate change at Herschel Island (Qikitaruq), Yukon Territory, Canada;Burn;J. Geophys. Res-Earth,2009

5. Hydraulic conductivity in frozen soils;Burt;Earth Surf. Process.,1976

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