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Stable element-free Galerkin solution procedures for the coupled soil-pore fluid problem

机译:耦合的土-孔流体问题的稳定无元素Galerkin解法

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摘要

It is always difficult to solve the coupled soil-pore fluid problem when the soil is saturated and impermeable, because this situation often results in intensive oscillations of the solutions. This topic has been discussed widely in the field of the finite element method but rarely by meshless methods. The Element-Free Galerkin (EFG) method has outstanding advantages of solving this problem, based on the fact that its interpolation function can be constructed flexibly by the nodes in the compact domain. In this study, an EFG numerical model together with a stabilization technique is proposed to obtain stable solutions, especially for the saturated and impermeable soil. Close agreement between computational results and analytical solutions for one-and two-dimensional examples shows that the proposed numerical model not only provides highly accurate solutions for the saturated soil with relatively high permeability, but also eliminates the oscillations of the solutions very effectively for the saturated and impermeable soil. Furthermore, the influences of the hydraulic anisotropy, a typical property of two-dimensional problems, on the proposed stabilization technique are discussed. It is suggested that the optimal distribution of the nodes of essential variables can be designed, according to the relative importance of the permeability in different directions.
机译:当土壤饱和且不可渗透时,总是很难解决耦合的土壤-孔隙流体问题,因为这种情况通常会导致溶液剧烈振荡。该主题在有限元方法领域中已被广泛讨论,但很少采用无网格方法。基于无元素Galerkin(EFG)方法可以通过紧凑域中的节点灵活地构造其插值功能,因此具有解决此问题的突出优势。在这项研究中,EFG数值模型与稳定技术一起被提出来获得稳定的解决方案,特别是对于饱和和不可渗透的土壤。一维和二维实例的计算结果与解析解之间的密切一致性表明,所提出的数值模型不仅为渗透率相对较高的饱和土提供了高精度的解,而且​​还非常有效地消除了饱和对解的振荡和不透水的土壤。此外,还讨论了二维各向异性的典型特性水力各向异性对所提出的稳定技术的影响。建议根据渗透率在不同方向上的相对重要性,设计基本变量节点的最佳分布。

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