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arXiv 1712.04876math.NAcs.NAmath.APmath.PR
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椭圆偏微分方程中具有跳跃扩散系数的研究

A study of elliptic partial differential equations with jump diffusion coefficients

University of Stuttgart(斯图加特大学)

Andrea Barth, Andreas Stein

AI总结:

本文研究了具有跳跃扩散系数的椭圆偏微分方程,通过将随机系数分解为连续高斯随机场和不连续跳跃部分,结合多级蒙特卡洛方法估计解的矩。

摘要:

作为一种地下流体的简化模型,椭圆方程可能被用来。不足的测量或这些中的不确定性通常通过随机系数建模,然后代表给定介质的不确定渗透率。作为将此方法扩展到异质、裂隙或多孔介质流动的延伸,我们引入了扩散系数中的跳跃。这些不连续性然后代表介质中的转换。更准确地说,我们考虑一个二阶椭圆问题,其中随机系数由连续高斯随机场和不连续跳跃部分之和给出。为了估计由此产生的随机偏微分方程解的矩,我们使用路径上的数值近似结合多级蒙特卡洛采样。为了考虑不连续性并提高路径上的近似收敛性,空间域根据每个样本中的跳跃位置分解,导致路径依赖的网格。因此,无法为每个样本路径预先创建适合的嵌套网格序列。我们通过自适应多级算法解决这个问题,其中每个级别的离散化是样本依赖的,并满足给定的细化条件。

英文摘要:

As a simplified model for subsurface flows elliptic equations may be utilized. Insufficient measurements or uncertainty in those are commonly modeled by a random coefficient, which then accounts for the uncertain permeability of a given medium. As an extension of this methodology to flows in heterogeneous\fractured\porous media, we incorporate jumps in the diffusion coefficient. These discontinuities then represent transitions in the media. More precisely, we consider a second order elliptic problem where the random coefficient is given by the sum of a (continuous) Gaussian random field and a (discontinuous) jump part. To estimate moments of the solution to the resulting random partial differential equation, we use a pathwise numerical approximation combined with multilevel Monte Carlo sampling. In order to account for the discontinuities and improve the convergence of the pathwise approximation, the spatial domain is decomposed with respect to the jump positions in each sample, leading to pathdependent grids. Hence, it is not possible to create a nested sequence of grids which is suitable for each sample path a-priori. We address this issue by an adaptive multilevel algorithm, where the discretization on each level is sample-dependent and fulfills given refinement conditions.

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