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首页> 外文期刊>Ground water >'Methods to Derive the Differen tial Equation of the Free Surface Boundary,' by Chongxi Chen,Xingxing Kuang,and Jiu Jimmy Jiao,May-June 2010,v.48,no.3:329-332.
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'Methods to Derive the Differen tial Equation of the Free Surface Boundary,' by Chongxi Chen,Xingxing Kuang,and Jiu Jimmy Jiao,May-June 2010,v.48,no.3:329-332.

机译:“推导自由表面边界的微分方程的方法”,陈重喜,匡兴星和焦九Jim,2010年5月6日,v.48,第3:329-332页。

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摘要

Recently Chen et al. (2010) (hereafter CKJ) challenged the classical dynamic boundary condition at the free surface in an unconfined aquifer as derived by Boul-ton (1954) and Bear (1972, 1978). However, we believe that the classical derivation is correct. In the CKJ derivation there is some confusion over the type of derivative applied at the free surface because we cannot take a simple partial derivative of the free-surface boundary condition. The fact that the particle is on the free surface allows us to take only the material derivative of the free-surface boundary condition as in the classical derivation. As a result, only the material derivative of the head, h, is known at the free surface, and we cannot calculate explicitly partial derivatives of h with respect to t (time) and z (vertical coordinate) from the dynamic boundary condition.
机译:最近,Chen等。 (2010)(以下称CKJ)挑战了由Boulton(1954)和Bear(1972,1978)推导的无约束含水层中自由表面的经典动态边界条件。但是,我们认为经典推导是正确的。在CKJ推导中,由于我们不能采用自由表面边界条件的简单偏导数,因此在自由表面上应用的导数类型存在一些混淆。粒子在自由表面上的事实使我们只能像经典推导中那样采用自由表面边界条件的材料导数。结果,只有头部的材料导数h在自由表面是已知的,并且我们不能根据动态边界条件明确地计算h相对于t(时间)和z(垂直坐标)的偏导数。

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