2019
DOI: 10.1186/s40323-019-0127-x
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Some comparisons and analyses of time or space discontinuous Galerkin methods applied to elastic wave propagation in anisotropic and heterogeneous media

Abstract: This research work presents some comparisons and analyses of the time discontinuous space-time Galerkin method and the space discontinuous Galerkin method applied to elastic wave propagation in anisotropic and heterogeneous media. Mechanism of both methods to ensure their stability using time or space discontinuities of unknown fields is analyzed and compared. The most general case of anisotropic and heterogeneous media with physical interfaces of discontinuous material properties is considered, especially for… Show more

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Cited by 3 publications
(4 citation statements)
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References 19 publications
(54 reference statements)
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“…At last, an explicit two-step second-order Runge-Kutta time-discretization is used to derive the discrete system. The reader interested in more details about formulation, implementation and stability of DG methods for anisotropic and piecewise homogeneous media should refer to references [30,40,43].…”
Section: Discretizationmentioning
confidence: 99%
“…At last, an explicit two-step second-order Runge-Kutta time-discretization is used to derive the discrete system. The reader interested in more details about formulation, implementation and stability of DG methods for anisotropic and piecewise homogeneous media should refer to references [30,40,43].…”
Section: Discretizationmentioning
confidence: 99%
“…All the three fluxes defined in Theorem 3.2 are identical. They are all equal to the Käser's flux (30) and can be written as follows:…”
Section: Upwind Numerical Fluxes For the 1st-order Velocity-stress Symentioning
confidence: 99%
“…(36a) is straightforward. The symmetric form of the numerical flux (36b) can be obtained by remarking that, in the case of continuous material properties, the following equations hold (see Appendix A2): (30) should be worse than the 1st-order flux (31), as it does not use the perturbed…”
Section: Upwind Numerical Fluxes For the 1st-order Velocity-stress Symentioning
confidence: 99%
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