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Numerical Simulation of the Consolidation in the Presence of Sand Lenses with Time-Dependent Drainage Boundaries

机译:含时变排水边界的沙粒存在下固结的数值模拟

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摘要

Sand lenses in clay layers may have various shapes and sizes. In many geotechnical studies, their effects are not considered carefully since detection of their positions and characteristics is difficult. In the simulation of the consolidation in clay layers with imbedded sand lenses, the problem can hardly be taken as a one-dimensional problem, and the phenomenon should be considered as a two- or three-dimensional problem. In the present study, the effect of the existence of sand lenses is investigated in terms of their positions and drainage characteristics in two-dimensional space. All drainage boundary conditions, including the boundary of lenses, are considered to be time dependent due to their variable thicknesses and permeability coefficients. A least squares based mesh free technique is used to solve the governing equations. In this method, radial basis functions are applied in function approximation. The results show the significant effect of the lenses and their characteristics in the process of dissipation of excess pore water pressure.
机译:粘土层中的沙透镜可能具有各种形状和大小。在许多岩土研究中,由于很难检测其位置和特性,因此并未仔细考虑其影响。在用嵌入的沙粒透镜模拟粘土层的固结过程中,几乎不能将问题视为一维问题,而应将该现象视为二维或三维问题。在本研究中,从沙透镜的存在和排水特性在二维空间方面研究了沙透镜的存在的影响。由于所有排水边界条件(包括透镜边界),都具有可变的厚度和渗透系数,因此被认为是时间依赖性的。基于最小二乘的无网格技术用于求解控制方程。在这种方法中,将径向基函数应用于函数逼近。结果表明,在多余的孔隙水压力消散过程中,镜片及其特性具有明显的作用。

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