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《Journal of Glaciology and Geocryology》 2003-03
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Relationship Between Frozen Soil Together with Its Water-Heat Process and Ecological Environment in the Tibetan Plateau

WU Qing-bai 1, 2 ,\ SHEN Yong-ping 2 ,\ SHI Bin 1 (1.AECI, Department of Earth Science, Nanjing University, Nanjing Jiangsu 210093, China; 2.State Key Laboratory of Frozen Soil Engineering, CAREERI, CAS, Lanzhou Gansu 730000, China)  
The relationship between frozen soil together with its water-heat process and vegetation-growing environment is discussed according to the monitored data of active layers in the Tibetan Plateau. The water-heat process in seasonal frozen soil is compared with that in permafrost. Freezing and thawing process changing with meadow ecology is discussed. Analysis result shows that vegetation ecology in cold region has an interactive relationship with frozen soil and its water-heat process. Frozen soil and its water-heat process not only control the change of surface state, but also affect the vegetation-growing extent. They have an extensive relationship of interaction. If the surface condition and the balance between vegetation growth and water-heat in frozen soil are destroyed, there present desertification.
【Fund】: 中国科学院知识创新重大项目(KZCX1 SW 0 4);; 国家自然科学基金重大项目(90 10 2 0 0 6);; 中国科学院寒区旱区环境与工程研究所知识创新工程项目(CACX2 10 0 47);; 南京大学博士后基金项目资助
【CateGory Index】: P642.14
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