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Title: Changes in geophysical properties caused by fluid injection into porous rocks: analytical models: Geophysical changes in porous rocks

Abstract

Analytical models are provided that describe how the elastic compliance, electrical conductivity, and fluid-flow permeability of rocks depend on stress and fluid pressure. In order to explain published laboratory data on how seismic velocities and electrical conductivity vary in sandstones and granites, the models require a population of cracks to be present in a possibly porous host phase. The central objective is to obtain a consistent mean-field analytical model that shows how each modeled rock property depends on the nature of the crack population. We describe the crack populations by a crack density, a probability distribution for the crack apertures and radii, and the averaged orientation of the cracks. The possibly anisotropic nature of the elasticity, conductivity, and permeability tensors is allowed for; however, only the isotropic limit is used when comparing to laboratory data. For the transport properties of conductivity and permeability, the percolation effect of the crack population linking up to form a connected path across a sample is modeled. But, this effect is important only in crystalline rock where the host phase has very small conductivity and permeability. In general, the importance of the crack population to the transport properties increases as the host phase becomes lessmore » conductive and less permeable.« less

Authors:
 [1];  [1];  [1];  [1];  [1];  [1]
  1. Lawrence Berkeley National Lab. (LBNL), Berkeley, CA (United States). Energy Geosciences Division
Publication Date:
Research Org.:
Lawrence Berkeley National Lab. (LBNL), Berkeley, CA (United States)
Sponsoring Org.:
USDOE Office of Science (SC), Basic Energy Sciences (BES) (SC-22)
OSTI Identifier:
1379824
Alternate Identifier(s):
OSTI ID: 1401012
Grant/Contract Number:  
AC02-05CH11231
Resource Type:
Journal Article: Accepted Manuscript
Journal Name:
Geophysical Prospecting
Additional Journal Information:
Journal Volume: 65; Journal Issue: 3; Journal ID: ISSN 0016-8025
Publisher:
Wiley
Country of Publication:
United States
Language:
English
Subject:
58 GEOSCIENCES; seismic velocities; electrical conductivity; permeability; effective stress; fluid flow; anisotropy

Citation Formats

Pride, Steven R., Berryman, James G., Commer, Michael, Nakagawa, Seiji, Newman, Gregory A., and Vasco, Donald W.. Changes in geophysical properties caused by fluid injection into porous rocks: analytical models: Geophysical changes in porous rocks. United States: N. p., 2016. Web. doi:10.1111/1365-2478.12435.
Pride, Steven R., Berryman, James G., Commer, Michael, Nakagawa, Seiji, Newman, Gregory A., & Vasco, Donald W.. Changes in geophysical properties caused by fluid injection into porous rocks: analytical models: Geophysical changes in porous rocks. United States. doi:10.1111/1365-2478.12435.
Pride, Steven R., Berryman, James G., Commer, Michael, Nakagawa, Seiji, Newman, Gregory A., and Vasco, Donald W.. Tue . "Changes in geophysical properties caused by fluid injection into porous rocks: analytical models: Geophysical changes in porous rocks". United States. doi:10.1111/1365-2478.12435. https://www.osti.gov/servlets/purl/1379824.
@article{osti_1379824,
title = {Changes in geophysical properties caused by fluid injection into porous rocks: analytical models: Geophysical changes in porous rocks},
author = {Pride, Steven R. and Berryman, James G. and Commer, Michael and Nakagawa, Seiji and Newman, Gregory A. and Vasco, Donald W.},
abstractNote = {Analytical models are provided that describe how the elastic compliance, electrical conductivity, and fluid-flow permeability of rocks depend on stress and fluid pressure. In order to explain published laboratory data on how seismic velocities and electrical conductivity vary in sandstones and granites, the models require a population of cracks to be present in a possibly porous host phase. The central objective is to obtain a consistent mean-field analytical model that shows how each modeled rock property depends on the nature of the crack population. We describe the crack populations by a crack density, a probability distribution for the crack apertures and radii, and the averaged orientation of the cracks. The possibly anisotropic nature of the elasticity, conductivity, and permeability tensors is allowed for; however, only the isotropic limit is used when comparing to laboratory data. For the transport properties of conductivity and permeability, the percolation effect of the crack population linking up to form a connected path across a sample is modeled. But, this effect is important only in crystalline rock where the host phase has very small conductivity and permeability. In general, the importance of the crack population to the transport properties increases as the host phase becomes less conductive and less permeable.},
doi = {10.1111/1365-2478.12435},
journal = {Geophysical Prospecting},
number = 3,
volume = 65,
place = {United States},
year = {Tue Aug 30 00:00:00 EDT 2016},
month = {Tue Aug 30 00:00:00 EDT 2016}
}

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Cited by: 3 works
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Works referenced in this record:

Percolation and Conduction
journal, October 1973