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Drawdown in prolate spheroidal-spherical coordinates obtained via Green's function and perturbation methods

机译:通过格林函数和摄动方法获得的球状球面坐标的缩图

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When investigating aquifer behaviour it is important to note that there exists a close relationship between the geometrical properties of the aquifer and the behaviour of the solution. In this paper our concern is to solve the flow equation described by prolate spheroidal coordinates by means of perturbation and the Green's function method, where the spheroid is considered to be a perturbation of a sphere. We transformed the spheroidal coordinates to spherical polar coordinates in the limit, as the shape factor tends to zero. The new groundwater flow equation is solved via an asymptotic parameter expansion and the Green's function method. The approximate solution of the new equation is compared with experimental data from real world. To take into account the error committed while approximating, we estimate the error in the asymptotic expansion. The error functions obtained suggest that the error would be very small for the shape factor tending to zero if the first two terms of the expansion are taken as an approximation.
机译:在研究含水层的行为时,重要的是要注意,含水层的几何特性与溶液的行为之间存在密切的关系。在本文中,我们的关注点是通过扰动和格林函数方法来解决由椭球体坐标描述的流动方程,其中球体被认为是球体的扰动。由于形状因子趋于零,我们在极限条件下将球面坐标转换为球面极坐标。通过渐近参数展开和格林函数方法求解新的地下水流方程。将新方程的近似解与来自现实世界的实验数据进行比较。为了考虑近似时所犯的误差,我们估计渐近展开中的误差。所获得的误差函数表明,如果将展开的前两个项作为近似值,则对于趋于零的形状因数,误差将非常小。

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