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1)  model of water allocation
分水模型
2)  water regime model
水分模型
3)  distributed hydrologic model
分布式水文模型
1.
Discussion of theory and methods for building a distributed hydrologic model;
分布式水文模型构建理论与方法述评
2.
One arithmetic of the grids conflux order in the distributed hydrologic model based on Muskingum method
基于马斯京根法的分布式水文模型求解栅格汇流次序
3.
Studying the needed catchment information of model based on study of distributed hydrologic model,in order to obtain the needed parameter information for designing the procedure to extract the catchment information,giving a serial number for each drainage system according to the water chain and obtaining the subcatchement based on water chain,some programms were developed.
为得到分布式水文模型所需要的参数,开发了程序进行流域信息提取,对得到的水系按水链进行编号,进而得到以水链为基础的子流域坡面。
4)  initial water right allocation
水权分配模型
5)  distributed hydrology model
分布式水文模型
1.
However,after dividing vertical layers and horizontal grids to the watershed,a distributed hydrology model established based on the physical foundation and runoff producing theory could analyse the mutual effect and coupling simulation about surface water and ground water with considering hydraulic connection of different runoff components.
而分布式水文模型基于其精确的物理基础和产流机制,充分考虑到不同径流成分的水力联系,在对流域进行土壤垂直分层和水平网格划分后可进行地表水、地下水的交互作用分析与耦合模拟。
6)  moisture migrating force model
水分驱动力模型
1.
Based on the adsorption-film moisture migration mechanism and the changing in the volume content of the coupled deformations of the phase mediums in saturated frozen soils,the new unfrozen moisture migrating force model in the frozen soil with high confine pressure and the deformation corresponding equations of each phase medium are firstly got with the mass .
论文基于吸附薄膜理论,根据饱和冻土体内各相成分之间水、热、力耦合产生的变形在体积含量上的变化,利用质量守恒原理建立起各相成分的变形协调条件,推导出饱和冻土体的连续性方程,建立了高围压下的新的冻土的水分驱动力模型。
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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