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arXiv 2301.11642math.NAcs.NA
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一种基于近场动力学理论的 Richards 方程非局部形式的数值方法

A Numerical Method for a Nonlocal Form of Richards' Equation Based on Peridynamic Theory

M. Berardi, F. V. Difonzo, S. F. Pellegrino

AI总结:

针对含裂隙多孔介质中的非局部入渗问题,提出基于近场动力学理论、Chebyshev 变换与显式时间积分的谱数值格式,证明其在 Sobolev 空间中收敛于唯一解,并在多类土壤及根系吸水场景下验证。

摘要:

预测非均质多孔介质中的含水量动态在水文应用中具有重要意义;特别是,在存在裂缝和裂隙时处理入渗问题,可以借助近场动力学理论来完成,该理论能够对空间中的非局部性进行恰当建模。在此框架下,我们对方程的扩散分量采用 Chebyshev 变换,随后使用显式方法在时间上向前积分。我们证明,所提出的谱数值格式所给出的解在某个适当的 Sobolev 空间中收敛于唯一解。最后,我们在几种不同土壤上进行示例验证,同时考虑了表示根系吸水的汇项。

英文摘要:

Forecasting water content dynamics in heterogeneous porous media has significant interest in hydrological applications; in particular, the treatment of infiltration when in presence of cracks and fractures can be accomplished resorting to peridynamic theory, which allows a proper modeling of non localities in space. In this framework, we make use of Chebyshev transform on the diffusive component of the equation and then we integrate forward in time using an explicit method. We prove that the proposed spectral numerical scheme provides a solution converging to the unique solution in some appropriate Sobolev space. We finally exemplify on several different soils, also considering a sink term representing the root water uptake.

机构、总结、中文摘要均由AI分析而来,可能存在错误,请以论文正文为准。

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