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1)  /hydrothermal coupling migration of soil
土壤水热耦合迁移
2)  simultaneous soil moisture and heat transfer
土壤水热迁移
3)  coupled moisture and heat transfer
水热耦合迁移
1.
By using the equation regularity of moisture movement and soil thermal conductive and adopting central scheme,the mathematical model for solving the problem of coupled moisture and heat transfer during soil freezing is established with some assumption,and the soil freeze-thaw depth in the source region of the Yellow River is simulated.
利用土壤水分迁移方程和热传导方程,采用中心差分格式并在一定假设前提下建立起冻土水热耦合迁移数学模型。
4)  coupled moisture and heat flow equation
土壤水热耦合
1.
Affected by precipita- tion,irrigation,wind speed,and so on,there exist complex material and energy exchanges on the interface of atmosphere and soil,which lead to very complex boundary conditions of coupled moisture and heat flow equation.
将二维有限元方法和遗传算法结合起来,求解土壤水热耦合方程,获取土壤含水量数据。
5)  thermo-hydro-mechanical-migratory coupling
热-水-应力-迁移耦合
6)  soil water movement
土壤水分迁移
补充资料:土壤水分运动基本方程(见土壤水运动)


土壤水分运动基本方程(见土壤水运动)


turang shuifen yundong iiben土壤水分运动基本方程fangeheng见土壤水运动。
说明:补充资料仅用于学习参考,请勿用于其它任何用途。
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