A simple model for squirt-flow dispersion and attenuation in fluid-saturated granular rocks.

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A simple model for squirt-flow dispersion and attenuation in fluid-saturated granular rocks.

A major cause of seismic attenuation in fluid-saturated rocks is the flow of the pore fluid induced by the passing wave. At sonic and ultrasonic frequencies, attenuation appears to be dominated by the local (pore-scale) flow between pores of different shapes and orientations. A simple squirt flow mo...

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Bibliographic Details
Main Authors:	Gurevich, Boris, Makarynska, Dina, De Paula, Osni, Pervukhina, M.
Format:	Journal Article
Published:	Society of Exploration Geophysics 2010
Online Access:	http://hdl.handle.net/20.500.11937/15049

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