Laboratory Study Of Frequency Dependent Streaming Potentials

Frequency 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 freque...

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Main Authors: Reppert, Philip M., Morgan, F. Dale
Other Authors: Massachusetts Institute of Technology. Earth Resources Laboratory
Format: Technical Report
Published: Massachusetts Institute of Technology. Earth Resources Laboratory 2012
Online Access:http://hdl.handle.net/1721.1/75387
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author Reppert, Philip M.
Morgan, F. Dale
author2 Massachusetts Institute of Technology. Earth Resources Laboratory
author_facet Massachusetts Institute of Technology. Earth Resources Laboratory
Reppert, Philip M.
Morgan, F. Dale
author_sort Reppert, Philip M.
collection MIT
description Frequency 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.
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spelling mit-1721.1/753872019-04-12T20:32:23Z Laboratory Study Of Frequency Dependent Streaming Potentials Reppert, Philip M. Morgan, F. Dale Massachusetts Institute of Technology. Earth Resources Laboratory Reppert, Philip M. Morgan, F. Dale Frequency 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. United States. Air Force Office of Scientific Research (Grant F49620-95-1-0224) Massachusetts Institute of Technology. Borehole Acoustics and Logging Consortium Massachusetts Institute of Technology. Earth Resources Laboratory. Reservoir Delineation Consortium 2012-12-11T16:51:13Z 2012-12-11T16:51:13Z 1998 Technical Report http://hdl.handle.net/1721.1/75387 Earth Resources Laboratory Industry Consortia Annual Report;1998-11 application/pdf Massachusetts Institute of Technology. Earth Resources Laboratory
spellingShingle Reppert, Philip M.
Morgan, F. Dale
Laboratory Study Of Frequency Dependent Streaming Potentials
title Laboratory Study Of Frequency Dependent Streaming Potentials
title_full Laboratory Study Of Frequency Dependent Streaming Potentials
title_fullStr Laboratory Study Of Frequency Dependent Streaming Potentials
title_full_unstemmed Laboratory Study Of Frequency Dependent Streaming Potentials
title_short Laboratory Study Of Frequency Dependent Streaming Potentials
title_sort laboratory study of frequency dependent streaming potentials
url http://hdl.handle.net/1721.1/75387
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