Quantitative estimation of the thermal conductivity of saturated frozen soils

被引：0
|
作者：
Gavriliev, RI [1 ]
机构：
[1] Russian Acad Sci, Melnikov Permafrost Inst, Yakutsk, Russia
来源：
PERMAFROST, VOLS 1 AND 2 | 2003年
关键词：
D O I：
暂无
中图分类号：
P [天文学、地球科学];
学科分类号：
07 ;
摘要：
A method is suggested for the theoretical calculation of the thermal conductivity coefficient of soils using parameters of a clear ground of horizon C as the parent rock of soils, as well as organic (humus) concentration. The soil is modeled by assuming concentric shells of soil components - mineral, colloidal aggregate, bound (unfrozen) water and free water (ice).
引用
收藏
页码：283 / 285
页数：3
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