Thermal regime of permafrost active layer has a great significance on revealing hydrological processes and ecological changes in Alpine regions.The equivalent-apparent heat capacity was an important method to study this issue.By introducing a parameter describing the saturation of the active layer,the equivalent-apparent heat capacity method was modified to be capable of unsaturated zone.On the premise of ignoring soil moisture convection and the source(sink) of heat,this paper utilized COMSOL Multiphysics ...
| 
推荐 
点击下列相关研究机构和相关文献作者，可以直接查到这些机构和作者被《中国知识资源总库》收录的其它文献，使您全面了解该机构和该作者的研究动态和历史。
