Numerical Simulation in Applied Geophysics pp 269-281 | Cite as
Wave propagation in partially frozen porous media
Abstract
The propagation of waves in a fluid-saturated poroelastic medium which matrix is composed of two weakly coupled solids is simulated using an iterative finite element domain decomposition algorithm. The equations of motion are formulated in the space-frequency domain including dissipation in the solid matrix and frequency correction factors in the mass and viscous coupling coefficients. First order absorbing boundary conditions are employed at the artificial boundaries of the computational domain. The algorithm is applied to simulate wave propagation in a sample of partially frozen Berea sandstone at ultrasonic frequencies.
Keywords
Side Length Domain Decomposition Viscous Coupling Ultrasonic Range Simulate Wave PropagationPreview
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