摘要
根据冻结条件下非饱和土壤水分运动和热量迁移的基本方程,推求冻土水热耦合迁移的数学模型。采用Grank-Nicolson格式的有限差分法,计算结果表明土壤水分、温度的计算值与实验值吻合较好。
Based on the basic equations of simultaneous soil water and heat transfer during soil freezing, the coupled equation of moisture and heat was deduced. The equations were solved numerically by the finite difference method with Grank-Nicolson. As a result the simulated values of water content and temperature followed the measured values closely.
出处
《安徽农业科学》
CAS
北大核心
2007年第17期5216-5217,5282,共3页
Journal of Anhui Agricultural Sciences
基金
冻土工程国家重点实验室开放基金项目(SKLFSE200303)
辽宁省博士后基金
国家自然科学基金项目(40272102)资助
关键词
土壤冻结
水热迁移
水热耦合方程
Soil freezing
Soil moisture and heat transfer
coupled equation of moisture and heat