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首页> 外文期刊>Journal of geotechnical and geoenvironmental engineering >Piecewise-Linear Formulation of Coupled Large-Strain Consolidation and Unsaturated Flow. I: Model Development and Implementation
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Piecewise-Linear Formulation of Coupled Large-Strain Consolidation and Unsaturated Flow. I: Model Development and Implementation

机译:大应变固结与不饱和流耦合的分段线性公式。一:模型开发与实施

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A mass-conservative formulation of one-dimensional (1D) coupled large-strain consolidation and unsaturated flow using a piecewise-linear formulation is developed. The volume and water-content changes in the unsaturated zone are described using three-dimensional (3D) constitutive surfaces of void ratio and gravimetric water content as functions of net stress and matric suction, whereas the volume change in the saturated zone is described using a two-dimensional (2D) curve relating void ratio to Terzaghi effective stress. The hydraulic conductivity varies with both void ratio and suction in the unsaturated zone, and with void ratio only in the saturated zone. The associated nonlinearities are addressed by solving the flow-continuity equation for water mass conservation through a finite-difference scheme in a piecewise-linear manner. The unknowns are calculated from variables in the previous time step without requiring iteration. A novel algorithm is developed to smoothly model transition between the saturated and unsaturated zones. Four types of top boundary conditions are formulated to account for complex soil-atmosphere hydraulic interactions. The developed program is also capable of performing a quasi-unsaturated analysis, which uses the saturated soil's constitutive relationships in the unsaturated zone, similar to the approach of several models currently used in practice. The theoretical and numerical development of the model is described in this paper, and is followed by verifications of the program's implementation using a numerical example of saturated large-strain consolidation and an analytical solution to unsaturated flow. Validation of the quasi-unsaturated and unsaturated formulations is presented in the companion paper, using comparisons with numerical cases as well as laboratory and field data.
机译:开发了使用分段线性公式的一维(1D)耦合大应变固结和不饱和流的质量守恒公式。使用空隙率和重量含水量的三维(3D)本构面描述净应力和基质吸力的函数来描述非饱和区的体积和含水量变化,而使用零点描述了饱和区中的体积变化。将空隙率与Terzaghi有效应力相关的二维(2D)曲线。在非饱和区中,水力传导率随空隙率和吸力而变化,而仅在饱和区中,水力传导率随空隙率而变化。通过以分段线性方式通过有限差分方案求解节水的水流连续性方程,可以解决相关的非线性问题。未知数是根据上一个时间步长中的变量计算的,不需要迭代。开发了一种新颖的算法来平滑地模拟饱和区和非饱和区之间的过渡。制定了四种类型的顶部边界条件,以解释复杂的土壤-大气水力相互作用。所开发的程序还能够执行准不饱和分析,该分析使用不饱和区中饱和土的本构关系,类似于目前在实践中使用的几种模型的方法。本文描述了该模型的理论和数值发展,随后通过使用饱和大应变固结的数值示例和非饱和流的解析解验证了程序的实现。伴随文件中的数值不完整以及实验室和现场数据的比较,对准不饱和和不饱和配方的验证在随附的论文中进行了介绍。

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