Anisotropic dispersion and attenuation due to wave-induced fluid flow: Quasi-static finite element modeling in poroelastic solids

Heterogeneous porous media such as hydrocarbon reservoir rocks are effectively described as anisotropic viscoelastic solids. They show characteristic velocity dispersion and attenuation of seismic waves within a broad frequency band, and an explanation for this observation is the mechanism of wave‐i...

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Veröffentlicht in:	Journal of Geophysical Research: Solid Earth Jg. 115; H. B7
Hauptverfasser:	Wenzlau, F., Altmann, J. B., Müller, T. M.
Format:	Journal Article
Sprache:	Englisch
Veröffentlicht:	Washington, DC Blackwell Publishing Ltd 01.07.2010 American Geophysical Union
Schlagworte:	anisotropy Attenuation Computational fluid dynamics Dispersions Earth sciences Earth, ocean, space Exact sciences and technology finite element simulation Fluid flow Fluids Geology Geophysics Heterogeneity High performance computing Mathematical analysis Mathematical models Media Physical properties Porous media Rocks seismic attenuation Seismic waves reservoir rocks Frequency dependence layered media simulation pore fluid S-waves Modeling frequency Relaxation fluid pressure seismic waves models hydrocarbons P-waves finite element analysis stiffness tensor Velocity dispersion incidence angle heterogeneity Flow(fluid) porous media inclusions theory wave attenuation
ISSN:	0148-0227, 2169-9313, 2156-2202, 2169-9356
Online-Zugang:	Volltext
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