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Large-scale stochastic linear inversion using hierarchical matrices

机译:使用分层矩阵的大规模随机线性反演

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Stochastic inverse modeling deals with the estimation of functions from sparse data, which is a problem with a nonunique solution, with the objective to evaluate best estimates, measures of uncertainty, and sets of solutions that are consistent with the data. As finer resolutions become desirable, the computational requirements increase dramatically when using conventional solvers. A method is developed in this paper to solve large-scale stochastic linear inverse problems, based on the hierarchical matrix (or H~2 matrix) approach. The proposed approach can also exploit the sparsity of the underlying measurement operator, which relates observations to unknowns. Conventional direct algorithms for solving large-scale linear inverse problems, using stochastic linear inversion techniques, typically scale as O(n~2m+nm~2). where n is the number of measurements and m is the number of unknowns. We typically have n 《 m. In contrast, the algorithm presented here scales as O(n~2m). i.e., it scales linearly with the larger problem dimension m. The algorithm also allows quantification of uncertainty in the solution at a computational cost that also grows only linearly in the number of unknowns. The speedup gained is significant since the number of unknowns m is often large. The effectiveness of the algorithm is demonstrated by solving a realistic crosswell tomography problem by formulating it as a stochastic linear inverse problem. In the case of the crosswell tomography problem, the sparsity of the measurement operator allows us to further reduce the cost of our proposed algorithm from O(n~2m) to O(n~2m~(1/2) + nm). The computational speedup gained by using the new algorithm makes it easier, among other things, to optimize the location of sources and receivers, by minimizing the mean square error of the estimation. Without this fast algorithm, this optimization would be computationally impractical using conventional methods.
机译:随机逆建模处理来自稀疏数据的函数估计,这是非唯一解的一个问题,目的是评估最佳估计,不确定性度量以及与数据一致的解集。随着更精细的分辨率变得越来越理想,使用传统的求解器时,计算需求将急剧增加。本文提出了一种基于层次矩阵(或H〜2矩阵)的方法来解决大规模随机线性逆问题。所提出的方法还可以利用基础测量算子的稀疏性,该稀疏性将观测值与未知数相关联。使用随机线性反演技术解决大规模线性反问题的常规直接算法通常标度为O(n〜2m + nm〜2)。其中,n是测量次数,m是未知数。我们通常有n《 m。相反,此处提出的算法的缩放比例为O(n〜2m)。即,它以较大的问题维度m线性缩放。该算法还允许以计算成本来量化解决方案中的不确定性,而未知数的数量也仅线性增长。由于未知数m常常很大,因此获得的加速效果显着。通过将现实的井间层析成像问题公式化为随机线性反问题,证明了该算法的有效性。在井间层析成像问题的情况下,测量算子的稀疏性使我们可以将拟议算法的成本从O(n〜2m)进一步降低到O(n〜2m〜(1/2)+ nm)。通过使用新算法获得的计算速度加快,尤其是通过最小化估计的均方误差,更容易优化源和接收器的位置。如果没有这种快速算法,则使用常规方法进行此优化在计算上将是不切实际的。

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