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6 - Fluid Effects on Wave Propagation

Published online by Cambridge University Press:  05 March 2020

Gary Mavko ,
Tapan Mukerji  and
Jack Dvorkin
Gary Mavko
Affiliation:
Stanford University, California
Tapan Mukerji
Affiliation:
Stanford University, California
Jack Dvorkin
Affiliation:
Stanford University, California
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Summary

Biot (1956) derived theoretical formulas for predicting the frequency-dependent seismic velocities of saturated rocks in terms of the dry-rock properties. His formulation incorporates some, but not all, of the mechanisms of viscous and inertial interaction between the pore fluid and the mineral matrix of the rock.

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The Rock Physics Handbook , pp. 367 - 473
Publisher: Cambridge University Press
Print publication year: 2020

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