A time domain system of equations is proposed to model elastic wave propaga-tion in an unbounded two-dimensional anisotropic solid using perfectly matched layer (PML). Starting from a system of first-order frequency domain stress-velocity equations and using complex coordinate stretching approach with a two-parameter stretch function, a second-order formulation is obtained. The final system, which consists of just two second order equations along with four aux-iliary equations, is smaller than existing formulations, thereby simplifying the problem and reducing the computational cost. The discrete stability of the so-lutions for a given mesh size is examined with the help of a plane-wave analysis of the corresponding continuous problem. It i...
The stability of the finite-difference approximation of elastic wave propagation in orthotropic homo...
Real sedimentary media can usually be characterized as transverse isotropy. To reveal wave propagati...
Abstract We transform the seismic wave equations in 2D inhomogeneous aniso-tropic media into a syste...
Perfectly matched layers (PML) are a well-developed method for simulating wave propagation in unboun...
The perfectly matched layer (PML) is a novel technique to simulate the absorption of waves in unboun...
AbstractWe consider the second order wave equation in an unbounded domain and propose an advanced pe...
International audienceThis review article revisits and outlines the perfectly matched layer (PML) me...
mms.sagepub.com Compact second-order time-domain perfectly matched layer formulation for elastic wav...
Many practical applications require the analysis of elastic wave propagation in a homogeneous isotro...
This brief article outlines a new and rather simple method for obtaining the finite element matrices...
One approach to the numerical solution of a wave equation on an unbounded domain uses a bounded doma...
International audiencePerfectly matched layers (PML) are a recent technique for simulating the absor...
We develop new numerical anisotropic perfectly matched layer (PML) boundaries for elastic waves in C...
This paper presents a framework for implementing a novel Perfectly Matching Layer and Infinite Eleme...
In recent years, the application of time-domain adjoint methods to improve large, complex undergroun...
The stability of the finite-difference approximation of elastic wave propagation in orthotropic homo...
Real sedimentary media can usually be characterized as transverse isotropy. To reveal wave propagati...
Abstract We transform the seismic wave equations in 2D inhomogeneous aniso-tropic media into a syste...
Perfectly matched layers (PML) are a well-developed method for simulating wave propagation in unboun...
The perfectly matched layer (PML) is a novel technique to simulate the absorption of waves in unboun...
AbstractWe consider the second order wave equation in an unbounded domain and propose an advanced pe...
International audienceThis review article revisits and outlines the perfectly matched layer (PML) me...
mms.sagepub.com Compact second-order time-domain perfectly matched layer formulation for elastic wav...
Many practical applications require the analysis of elastic wave propagation in a homogeneous isotro...
This brief article outlines a new and rather simple method for obtaining the finite element matrices...
One approach to the numerical solution of a wave equation on an unbounded domain uses a bounded doma...
International audiencePerfectly matched layers (PML) are a recent technique for simulating the absor...
We develop new numerical anisotropic perfectly matched layer (PML) boundaries for elastic waves in C...
This paper presents a framework for implementing a novel Perfectly Matching Layer and Infinite Eleme...
In recent years, the application of time-domain adjoint methods to improve large, complex undergroun...
The stability of the finite-difference approximation of elastic wave propagation in orthotropic homo...
Real sedimentary media can usually be characterized as transverse isotropy. To reveal wave propagati...
Abstract We transform the seismic wave equations in 2D inhomogeneous aniso-tropic media into a syste...