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Data assimilation and parameter estimation via ensemble Kalman filter coupled with stochastic moment equations of transient groundwater flow

机译:集成卡尔曼滤波与瞬时地下水渗流随机矩方程相结合的数据同化和参数估计

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摘要

The ensemble Kalman filter (EnKF) is a powerful tool for assimilating data in earth system models. The approach allows real time Bayesian updating of system states and parameters as new data become available. This paper focuses on EnKF data assimilation in models of groundwater flow through complex geologic media. It has become common to treat the hydraulic conductivity of such media as correlated random fields conditioned on measured conductivity (medium property) and/or hydraulic head (system state) values. This renders the conductivity nonstationary and the corresponding conditional flow equations stochastic. Solving these equations and coupling them with EnKF generally entails computationally intensive Monte Carlo (MC) simulation. We propose to circumvent the need for MC through a direct solution of approximate nonlocal (integrodifferential) equations that govern the space-time evolution of conditional ensemble means (statistical expectations) and covariances of hydraulic heads and fluxes. We illustrate and explore our approach on synthetic two-dimensional examples in which a well pumps water from a randomly heterogeneous aquifer subject to prescribed head and flux boundary conditions. Embedding the solution in EnKF provides sequential updates of conductivity and head estimates throughout the space-time domain of interest. We demonstrate the computational feasibility and accuracy of our methodology, showing that hydraulic conductivity estimates are more sensitive to early than to later head values and improve with increasing assimilation frequency at early time.
机译:集合卡尔曼滤波器(EnKF)是用于吸收地球系统模型中数据的强大工具。该方法允许在新数据可用时实时对系统状态和参数进行贝叶斯更新。本文重点研究复杂地质介质中地下水流模型中的EnKF数据同化。将这样的介质的水力传导率视作以测得的传导率(介质特性)和/或水压头(系统状态)值为条件的相关随机场已成为普遍现象。这使得电导率不稳定,并且相应的条件流动方程是随机的。解决这些方程并将其与EnKF耦合通常需要计算量大的蒙特卡洛(MC)仿真。我们建议通过直接求解近似的非局部(积分微分)方程来解决对MC的需求,该方程控制条件集合均值(统计期望)的时空演化以及水头和流量的协方差。我们在合成二维示例中说明和探索了我们的方法,在该示例中,一口井从随机的非均质含水层中抽水,并使其受到规定的水头和通量边界条件的影响。将解决方案嵌入EnKF可在整个感兴趣的时空范围内提供电导率和水头估算的顺序更新。我们证明了该方法的计算可行性和准确性,表明水力传导率估算值对早期的敏感度高于对后期的水头值,并且随着早期同化频率的增加而提高。

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