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Efficient method for probabilistic estimation of spatially varied hydraulic properties in a soil slope based on field responses: A Bayesian approach

机译:基于场响应的概率估算土壤边坡中水力变化的有效方法:贝叶斯方法

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摘要

An efficient probabilistic back estimation method for characterization of spatial variability is proposed by integration of the Karhunen-Loeve (K-L) expansion method, the Polynomial Chaos Expansion (PCE) method and the Markov Chain Monte Carlo (MCMC) method. To reduce the dimension of back estimation, the spatially varied soil property is simulated using the K-L expansion method and the basic random variables of K-L terms are parameters to be estimated. To further reduce computation load, a PCE surrogate model is constructed to substitute the original model. The proposed method is applied on an example where a randomly heterogeneous soil slope is subject to surface infiltration. The pressure responses are used to estimate the spatial variability of the saturated coefficient permeability. The results show that the spatial variability can be satisfactorily estimated. The coefficient of variation of the estimation is less than 5%.
机译:通过结合Karhunen-Loeve(K-L)展开方法,多项式混沌展开(PCE)方法和Markov链蒙特卡洛(MCMC)方法,提出了一种用于表征空间变异性的高效概率反估计方法。为了减小反演的维数,使用K-L展开法对空间变化的土壤特性进行了模拟,而K-L项的基本随机变量是要估计的参数。为了进一步减少计算量,构建了PCE替代模型来替代原始模型。所提出的方法适用于随机异质土坡面渗入的例子。压力响应用于估计饱和系数渗透率的空间变异性。结果表明,空间变异性可以令人满意地估计。估计的变异系数小于5%。

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