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Soil-Water Coupled Analyzer and Soil-Water Coupled Analysis Method

机译:土水耦合分析仪及土水耦合分析方法

摘要

The soil-water coupled analysis program of the invention computes a global L matrix and a modified global L matrix regarding a volume change rate of a soil skeleton over time, a global H matrix regarding a water permeability of soil, a global M matrix regarding a mass, and a global K matrix regarding a tangent stiffness of the soil skeleton, based on input settings of soils, such as clay, intermediate soil, and sand, to respective elements of a soil foundation, input settings of a solid soil model, and input settings of analysis conditions (steps S140 to S165). The soil-water coupled analysis program formulates a global tangent stiffness equation (simultaneous linear equations) using all these computed matrixes and determines an unknown ‘jerk field’ and a ‘pore water pressure field’ under given boundary conditions, for example, a given deformation condition and a given stress rate condition (step S170). This enables highly-accurate dynamic and static analyses in soil foundations of various soils from sand to intermediate soils and clay.
机译:本发明的土壤-水耦合分析程序计算关于土壤骨架随时间的体积变化率的整体L矩阵和修正的整体L矩阵,关于土壤的水渗透性的整体H矩阵,关于土壤的水渗透率的整体M矩阵。质量,以及关于土壤骨架的切线刚度的全局K矩阵,其基于土壤(例如粘土,中间土壤和沙子)对土壤基础各个元素的输入设置,实体土壤模型的输入设置和输入分析条件的设置(步骤S 140 至S 165 )。土水耦合分析程序使用所有这些计算出的矩阵来公式化整体切线刚度方程(同时线性方程式),并在给定的边界条件(例如给定的变形)下确定未知的“冲击场”和“孔隙水压力场”条件和给定的应力率条件(步骤S 170 )。这样就可以在从沙子到中间土壤和粘土的各种土壤的土壤基础中进行高精度的动态和静态分析。

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