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AN ITERATIVE STOCHASTIC INVERSE METHOD: CONDITIONAL EFFECTIVE TRANSMISSIVITY AND HYDRAULIC HEAD FIELDS

机译:迭代随机逆方法:条件有效透射率和水力头场

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摘要

An iterative stochastic approach is developed to estimate transmissivity and head distributionsudin heterogeneous aquifers. This approach is similar to the classical cokriging technique and it usesuda linear estimator that depends on the covariances of transmissivity and hydraulic head and theirudcross -covariance. The linear estimator is, however, improved successively by solving the governingudflow equation and by updating the covariances and cross -covariance function of transmissivity andudhydraulic head fields in an iterative manner. As a result, the nonlinear relationship betweenudtransmissivity and head is incorporated in the estimation and the estimated fields are approximateudconditional means. The ability of the iterative approach is tested with some deterministic andudstochastic inverse problems. The results show that the estimated transmissivity and hydraulic headudfields have smaller mean square errors than those obtained by classical cokriging even in the aquiferudwith variance of transmissivity up to 3.
机译:开发了一种迭代随机方法来估计透射率和水头分布 udin非均质含水层。这种方法类似于经典的cokriging技术,它使用线性估计器,该线性估计器取决于透射率和水头的协方差及其交叉协方差。但是,通过求解控制 udflow方程并以迭代方式更新透射率和水头场的协方差和互协方差函数,可以逐步改进线性估计器。结果,在透射率和水头之间的非线性关系被合并到估计中,并且被估计的场是近似的/无条件的手段。迭代方法的能力已通过一些确定性和非随机的逆问题进行了测试。结果表明,即使在透射率方差最大为3的含水层中,估计的透射率和水力头场的均方误差也比传统的克立格里夫方法具有的均方误差小。

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