Characterization of Fractured Reservoirs Using a Combination of Downhole Pressure and Self-Potential Transient Data

In order to appraise the utility of self-potential (SP) measurements to characterize fractured reservoirs, we carried out continuous SP monitoring using multi Ag-AgCl electrodes installed within two open holes at the Kamaishi Mine, Japan. The observed ratio of SP change to pressure change associated...

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Main Authors: Yuji Nishi, Tsuneo Ishido
Format: Article
Language:English
Published: Hindawi Limited 2012-01-01
Series:International Journal of Geophysics
Online Access:http://dx.doi.org/10.1155/2012/148919
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spelling doaj-9061e88c978f4b5da1eb0b559a7a1d4e2020-11-24T23:42:24ZengHindawi LimitedInternational Journal of Geophysics1687-885X1687-88682012-01-01201210.1155/2012/148919148919Characterization of Fractured Reservoirs Using a Combination of Downhole Pressure and Self-Potential Transient DataYuji Nishi0Tsuneo Ishido1GSJ, National Institute of Advanced Industrial Science and Technology (AIST), Tsukuba Central 7, Tsukuba, Ibaraki 305-8567, JapanGSJ, National Institute of Advanced Industrial Science and Technology (AIST), Tsukuba Central 7, Tsukuba, Ibaraki 305-8567, JapanIn order to appraise the utility of self-potential (SP) measurements to characterize fractured reservoirs, we carried out continuous SP monitoring using multi Ag-AgCl electrodes installed within two open holes at the Kamaishi Mine, Japan. The observed ratio of SP change to pressure change associated with fluid flow showed different behaviors between intact host rock and fractured rock regions. Characteristic behavior peculiar to fractured reservoirs, which is predicted from numerical simulations of electrokinetic phenomena in MINC (multiple interacting continua) double-porosity media, was observed near the fractures. Semilog plots of the ratio of SP change to pressure change observed in one of the two wells show obvious transition from intermediate time increasing to late time stable trends, which indicate that the time required for pressure equilibration between the fracture and matrix regions is about 800 seconds. Fracture spacing was estimated to be a few meters assuming several micro-darcies (10-18 m2) of the matrix region permeability, which is consistent with geological and hydrological observations.http://dx.doi.org/10.1155/2012/148919
collection DOAJ
language English
format Article
sources DOAJ
author Yuji Nishi
Tsuneo Ishido
spellingShingle Yuji Nishi
Tsuneo Ishido
Characterization of Fractured Reservoirs Using a Combination of Downhole Pressure and Self-Potential Transient Data
International Journal of Geophysics
author_facet Yuji Nishi
Tsuneo Ishido
author_sort Yuji Nishi
title Characterization of Fractured Reservoirs Using a Combination of Downhole Pressure and Self-Potential Transient Data
title_short Characterization of Fractured Reservoirs Using a Combination of Downhole Pressure and Self-Potential Transient Data
title_full Characterization of Fractured Reservoirs Using a Combination of Downhole Pressure and Self-Potential Transient Data
title_fullStr Characterization of Fractured Reservoirs Using a Combination of Downhole Pressure and Self-Potential Transient Data
title_full_unstemmed Characterization of Fractured Reservoirs Using a Combination of Downhole Pressure and Self-Potential Transient Data
title_sort characterization of fractured reservoirs using a combination of downhole pressure and self-potential transient data
publisher Hindawi Limited
series International Journal of Geophysics
issn 1687-885X
1687-8868
publishDate 2012-01-01
description In order to appraise the utility of self-potential (SP) measurements to characterize fractured reservoirs, we carried out continuous SP monitoring using multi Ag-AgCl electrodes installed within two open holes at the Kamaishi Mine, Japan. The observed ratio of SP change to pressure change associated with fluid flow showed different behaviors between intact host rock and fractured rock regions. Characteristic behavior peculiar to fractured reservoirs, which is predicted from numerical simulations of electrokinetic phenomena in MINC (multiple interacting continua) double-porosity media, was observed near the fractures. Semilog plots of the ratio of SP change to pressure change observed in one of the two wells show obvious transition from intermediate time increasing to late time stable trends, which indicate that the time required for pressure equilibration between the fracture and matrix regions is about 800 seconds. Fracture spacing was estimated to be a few meters assuming several micro-darcies (10-18 m2) of the matrix region permeability, which is consistent with geological and hydrological observations.
url http://dx.doi.org/10.1155/2012/148919
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AT tsuneoishido characterizationoffracturedreservoirsusingacombinationofdownholepressureandselfpotentialtransientdata
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