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Updating Markov chain models using the ensemble Kalman filter

机译:使用集成卡尔曼滤波器更新马尔可夫链模型

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The problem we address is how to condition discrete variables with a prior described by a Markov chain model to a set of continuous, nonlocal observations. This is motivated by the need for improved approaches to condition geological facies descriptions of a reservoir to production data. In this study, we assume that the spatial arrangement of facies can be modeled by a Markov chain model. The conditioning to nonlocal observations consists of two primary steps. First, the ensemble Kalman filter is used to assimilate data without regard for the discrete nature of the variables, or the probability of transition from one state to another. Second, the updated realizations are projected onto the discrete state space using an algorithm for finding the sequence of states with maximum probability. The method, which is based on the Viterbi algorithm, is not iterative and is capable of assimilating nonlocal data such as production data with some limitations. We demonstrate the application of the method first with an example in which the data are nonlocal but linear. The second example is a nonlinear fluid flow example in which data are assimilated sequentially. For the linear problem, the distribution of conditional realizations from the approximate algorithm was found to be indistinguishable from the distribution of realizations from an exact sampling algorithm (McMC). Finally, we discuss how to generalize the methodology from the ID example presented here to more general cases.
机译:我们要解决的问题是如何使用Markov链模型描述的先验条件对离散变量进行条件化,以处理一组连续的非局部观测值。这是由于需要改进的方法来调节储层的地质相描述来生产数据。在这项研究中,我们假设可以通过马尔可夫链模型来模拟相的空间排列。非本地观测的条件包括两个主要步骤。首先,集成卡尔曼滤波器用于吸收数据,而无需考虑变量的离散性质或从一种状态转换到另一种状态的可能性。其次,使用一种算法以最大的概率找到状态序列,将更新的实现投影到离散状态空间上。该方法基于Viterbi算法,不是迭代的,并且能够吸收非本地数据(例如生产数据),但有一些限制。我们首先以数据为非局部但线性的示例演示该方法的应用。第二个示例是非线性流体流动示例,其中数据被顺序吸收。对于线性问题,发现近似算法的条件实现分布与精确采样算法(McMC)的实现分布是无法区分的。最后,我们讨论如何从此处介绍的ID示例到更一般的情况来概括该方法。

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