| dc.contributor.author | Olson, John F. | |
| dc.contributor.other | Massachusetts Institute of Technology. Earth Resources Laboratory | en_US |
| dc.date.accessioned | 2012-12-11T16:57:38Z | |
| dc.date.available | 2012-12-11T16:57:38Z | |
| dc.date.issued | 1998 | |
| dc.identifier.uri | http://hdl.handle.net/1721.1/75390 | |
| dc.description.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. | en_US |
| dc.description.sponsorship | Massachusetts Institute of Technology. Earth Resources Laboratory (Founding Members Fellowship) | en_US |
| dc.publisher | Massachusetts Institute of Technology. Earth Resources Laboratory | en_US |
| dc.relation.ispartofseries | Earth Resources Laboratory Industry Consortia Annual Report;1998-13 | |
| dc.title | Toward The Simulation Of Attenuation: Oscillatory Flow In Porous Rock | en_US |
| dc.type | Technical Report | en_US |
| dc.contributor.mitauthor | Olson, John F. | |
| dspace.orderedauthors | Olson, John F. | en_US |
