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A multi-rate iterative coupling scheme for simulating dynamic ruptures and seismic waves generation in the prestressed earth

机译:一种用于模拟预应力地球动态破裂和地震波生成的多速率迭代耦合方案

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We present a novel method to simulate the dynamic evolution of spontaneous ruptures governed by rate- and state-dependent friction laws and the interaction with seismic waves in a prestressed elastically deforming body. We propose a multi-rate iterative coupling scheme based on the variational form of the elastic-gravitational equations, and discretize employing a discontinuous Galerkin method, with nonlinear interior boundary conditions being weakly imposed across the fault surface as numerical fluxes. We introduce necessary interface jump penalty terms as well as an artificial viscous regularization, with the conditions for penalty and viscosity coefficients given based on an energy estimate and a convergence analysis. In the multi-rate scheme, an implicit-explicit Euler scheme in time is invoked, and the time step for the evolution of friction is chosen significantly finer than that for wave propagation and scattering. This is facilitated by the iterative scheme through the underlying decoupling where the linear, elastic wave equation plays the role of a Schur-complement to the friction model. A nonlinearly constrained optimization problem localized to each element on the rupture surface is then formulated and solved using the Gauss-Newton method. We test our algorithm on several benchmark examples and illustrate the generality of our method for realistic rupture simulations. (C) 2019 Elsevier Inc. All rights reserved.
机译:我们提出了一种新的方法来模拟通过速率和状态摩擦法治的自发性破裂的动态演变以及与预应力的弹性变形体中的地震波的相互作用。我们提出了一种基于弹性重力方程的变分形式的多速率迭代耦合方案,并采用不连续的Galerkin方法的离散化,非线性内部边界条件在故障表面上弱施加为数值势态。我们介绍必要的界面跳转术语以及人工粘性正则化,条件是基于能量估计和收敛分析给出的惩罚和粘度系数的条件。在多速率方案中,调用时间内隐式显式欧拉方案,并且选择摩擦演化的时间步骤明显比波传播和散射更精细。通过迭代方案通过线性的弹性波方程在摩擦模型中发挥作用的基础解耦的迭代方案促进了这一点。然后使用Gauss-Newton方法配制并解决了对破裂表面上的每个元件的非线性约束优化问题。我们在几个基准示例中测试我们的算法,并说明了我们实现现实破裂模拟方法的一般性。 (c)2019 Elsevier Inc.保留所有权利。

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