Toward The Simulation Of Attenuation: Oscillatory Flow In Porous Rock

Author(s)
Olson, John F.
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Massachusetts Institute of Technology. Earth Resources Laboratory
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Abstract
Fluid flow in porous rock due to an oscillatory pressure gradient is simulated. We observe distributions of density and velocity in the rock which point to viscous dissipation. We will use this method to seek a deeper understanding of the physics of attenuation.
Date issued
1998
URI
http://hdl.handle.net/1721.1/75390
Publisher
Massachusetts Institute of Technology. Earth Resources Laboratory
Series/Report no.
Earth Resources Laboratory Industry Consortia Annual Report;1998-13
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