Abstract
Velocity dispersion and attenuation in residual saturated porous media strongly depend on the properties of the discontinuous fluid phase. We present a multiscale model based on an oscillator rheology for the fluid blobs/clusters, taking into account their distinct dynamic properties on the pore scale.
Cite
CITATION STYLE
APA
Steeb, H., Kurzeja, P. S., Frehner, M., & Schmalholz, S. M. (2012). Phase Velocity Dispersion and Attenuation of Seismic Waves due to Trapped Fluids in Residual Saturated Porous Media. Vadose Zone Journal, 11(3), vzj2011.0121. https://doi.org/10.2136/vzj2011.0121
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