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《Journal of Glaciology and Geocryology》 2004-05
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Study of Calculation of Soil Heat Conduction: Progress and Prospect

ZHANG Li-jie~(1,2),JIANG Hao~(1),LI Lei~(2,3) 730000, China; 2.Graduate School of the Chinese Academy of Sciences, Beijing 100039, China; 3.SLaboratory of Atmospheric Boundary Layer Physics and Atmospheric Chemistry, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China)  
The studies of the heat conduction in soil are of great importance both in the study on the thermal properties of soil for hydrometeorologists and in the study on land processes for micrometeorologists. The studies in this field are especially important in the study on the variation tendencies of permafrost in the Tibetan Plateau, which is directly related to the safety and stability of the Qinghai-Tibetan railway in construction. In this paper, the studies on the methods of calculating the heat flux conduction in soil are reviewed. The studies in this field are summarized into two categories, which are the methods of calculating soil heat flux and the methods of calculating soil thermal diffusivity, and both of these two categories can be divided into finer classes. At present, the methods of calculating the soil heat flux conduction can work well in the shallow layers of soil, but whether they can be well used in the deep layers of soil or not is still doubtful. Using porous media model and including the influences of water conduction in the soil into the methods of calculating soil heat flux conduction are the latest progress in the studies of the methods of calculating the soil thermal diffusivity in permafrost regions. With the more and more progress in this field, one of the important tasks in the future is to find a set of valid schemes of calculating the soil heat flux conduction, which can be used in the study of the permafrost variation tendencies along the Qinghai-Tibetan railway.
【Fund】: 中国科学院知识创新工程重大项目(KZCX 1 SW 04);; 国家自然科学基金项目(40471005)资助
【CateGory Index】: S152.8
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