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Accuracy of fully coupled and sequential approaches for modeling hydro- and geomechanical processes

机译:用于建模水电和地质力学过程的完全耦合和顺序方法的准确性

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摘要

Subsurface flow and geomechanics are often modeled with sequential approaches. This can be computationally beneficial compared with fully coupled schemes, while it requires usually compromises in numerical accuracy, at least when the sequential scheme is non-iterative. We discuss the influence of the choice of scheme on the numerical accuracy and the expected computational effort based on a comparison of a fully coupled scheme, a scheme employing a one-way coupling, and an iterative scheme using a fixed-stress split for two subsurface injection scenarios. All these schemes were implemented in the numerical simulator DuMu~x. This study identifies conditions of problem settings where differences due to the choice of the model approach are as important as differences in geologic features. It is shown that in particular transient and multiphase flow, effects can be causing significant deviations between non-iterative and iterative sequential schemes, which might be in the same order of magnitude as geologic uncertainty. An iterated fixed-stress split has the same numerical accuracy as a fully coupled scheme but only for a certain number of iterations which might use up the computational advantage of solving two smaller systems of equations rather than a big monolithical one.
机译:地下流量和地质力学通常以顺序方法为模拟。与完全耦合方案相比,这可以计算地有益,而通常需要以数值精度妥协,至少当顺序方案是非迭代的。我们讨论了基于完全耦合方案的比较,采用单向耦合的方案的比较来讨论方案选择的影响和预期计算工作,以及使用固定应力分裂的迭代方案进行两个地下注射方案。所有这些方案都在数值模拟器Dumu〜x中实现。本研究识别出问题设置的条件,其中由于模型方法选择的差异与地质特征的差异同样重要。结果表明,特别是瞬态和多相流,效果可能导致非迭代和迭代顺序方案之间的显着偏差,这可能与地质不确定性相同的数量级。迭代的固定应力分流具有与完全耦合方案相同的数值精度,而是仅用于一定数量的迭代,其可以利用求解两个较小的方程系统而不是大单片单片的计算优势。

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