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dc.contributor.authorReppert, Philip M.
dc.contributor.authorMorgan, F. Dale
dc.contributor.otherMassachusetts Institute of Technology. Earth Resources Laboratoryen_US
dc.date.accessioned2012-12-11T16:51:13Z
dc.date.available2012-12-11T16:51:13Z
dc.date.issued1998
dc.identifier.urihttp://hdl.handle.net/1721.1/75387
dc.description.abstractFrequency dependent streaming potentials were measured on a glass capillary, porous filter, and a sample of Boise sandstone. The pore diameters for these three samples range from 1 millimeter to 34 micrometers. The frequencies used in these experiments range from 0-600 Hz with the critical frequencies being 6.8 Hz, 90 Hz, and 400 Hz for the three specimens. The fluid was moved relative to the sample with the pressure measured by hydrophones and the streaming potential measured using silver silverchloride electrodes. Both Packard's (1953) and Pride's (1994) models satisfactorily predict the streaming potential behavior for these frequencies, and the measured critical frequencies are directly related to the sample pore diameters.en_US
dc.description.sponsorshipUnited States. Air Force Office of Scientific Research (Grant F49620-95-1-0224)en_US
dc.description.sponsorshipMassachusetts Institute of Technology. Borehole Acoustics and Logging Consortiumen_US
dc.description.sponsorshipMassachusetts Institute of Technology. Earth Resources Laboratory. Reservoir Delineation Consortiumen_US
dc.publisherMassachusetts Institute of Technology. Earth Resources Laboratoryen_US
dc.relation.ispartofseriesEarth Resources Laboratory Industry Consortia Annual Report;1998-11
dc.titleLaboratory Study Of Frequency Dependent Streaming Potentialsen_US
dc.typeTechnical Reporten_US
dc.contributor.mitauthorReppert, Philip M.
dc.contributor.mitauthorMorgan, F. Dale
dspace.orderedauthorsReppert, Philip M.; Morgan, F. Daleen_US


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