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一种基于VG模型的非饱和土渗流参数反演方法
引用本文:张华,周小超.一种基于VG模型的非饱和土渗流参数反演方法[J].三峡大学学报(自然科学版),2012,34(3):64-68.
作者姓名:张华  周小超
作者单位:三峡大学三峡库区地质灾害防治教育部重点实验室,湖北宜昌,443002
基金项目:国家自然科学基金资助项目
摘    要:针对非饱和土渗流分析中土水特征曲线和渗透性函数难以获取的问题,本文提出一种基于van Genuchten(VG)模型的非饱和土渗流参数反演方法,非饱和渗流控制方程采用Richards方程,通过计算数值模拟值与实测各观测点不同时刻孔隙水压力或重量(体积)含水量之误差平方和,寻求最优VG模型参数组合使得误差平方和最小.编制了二维非饱和渗流参数反演程序(BAKSEEP),并通过算例展示了该程序良好的适用性和稳定性.

关 键 词:反演  饱和-非饱和  暂态渗流  有限元

A Back Analysis Method for VG Model Parameters in Unsaturated Seepage Simulation
Zhang Hua , Zhou Xiaochao.A Back Analysis Method for VG Model Parameters in Unsaturated Seepage Simulation[J].Journal of China Three Gorges University(Natural Sciences),2012,34(3):64-68.
Authors:Zhang Hua  Zhou Xiaochao
Institution:Zhang Hua Zhou Xiaochao (Key Laboratory of Geological Hazards in Three Gorges Reservoir Area, Ministry of Education, China Three Gorges Univ. , Yichang 443002, China)
Abstract:In unsaturated seepage numerical simulation, the soil-water characteristic curve and hydraulic conductivity function for unsaturated soils are difficult to be obtained. To solve this problem, a back analysis method for VG model parameters in unsaturated seepage simulation is presented. The Richards equation is used as governing equation for unsaturated seepage. The VG model is adopted for soil-water characteristic curve and hydraulic conductivity function. The summation of squared error between simulated pore water pressure or gravitational (volumetric) water content and measured value is calculated. A set of local optimized VG model parameters can be found with minimized the summation of squared errors. A two dimensional back analysis program for unsaturated seepage (BAKSEEP) is compiled. The results of a benchmark case show that the back analysis method for unsaturated seepage is robust and practical.
Keywords:back analysis  saturated-unsaturated  transient seepage  finite element
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