Fractured rock stress‐permeability relationships from in situ data and effects of temperature and chemical‐mechanical couplings
Abstract
Abstract The purpose of this paper is to (i) review field data on stress‐induced permeability changes in fractured rock; (ii) describe estimation of fractured rock stress‐permeability relationships through model calibration against such field data; and (iii) discuss observations of temperature and chemically mediated fracture closure and its effect on fractured rock permeability. The field data that are reviewed include in situ block experiments, excavation‐induced changes in permeability around tunnels, borehole injection experiments, depth (and stress) dependent permeability, and permeability changes associated with a large‐scale rock‐mass heating experiment. Data show how the stress‐permeability relationship of fractured rock very much depends on local in situ conditions, such as fracture shear offset and fracture infilling by mineral precipitation. Field and laboratory experiments involving temperature have shown significant temperature‐driven fracture closure even under constant stress. Such temperature‐driven fracture closure has been described as thermal overclosure and relates to better fitting of opposing fracture surfaces at high temperatures, or is attributed to chemically mediated fracture closure related to pressure solution (and compaction) of stressed fracture surface asperities. Back‐calculated stress‐permeability relationships from field data may implicitly account for such effects, but the relative contribution of purely thermal‐mechanical and chemically mediated changes is difficult to isolate. Therefore,more »
- Authors:
-
- Lawrence Berkeley National Laboratory (LBNL) Berkeley CA USA
- Publication Date:
- Research Org.:
- Lawrence Berkeley National Laboratory (LBNL), Berkeley, CA (United States)
- Sponsoring Org.:
- USDOE
- OSTI Identifier:
- 1221699
- Alternate Identifier(s):
- OSTI ID: 1213470
- Grant/Contract Number:
- AC02-05CH11231
- Resource Type:
- Published Article
- Journal Name:
- Geofluids
- Additional Journal Information:
- Journal Name: Geofluids Journal Volume: 15 Journal Issue: 1-2; Journal ID: ISSN 1468-8115
- Publisher:
- Wiley-Blackwell
- Country of Publication:
- Canada
- Language:
- English
- Subject:
- 58 GEOSCIENCES; chemical and mechanical coupling; fractured rock; in situ experiments; permeabilty and stress; temperature
Citation Formats
Rutqvist, J. Fractured rock stress‐permeability relationships from in situ data and effects of temperature and chemical‐mechanical couplings. Canada: N. p., 2014.
Web. doi:10.1111/gfl.12089.
Rutqvist, J. Fractured rock stress‐permeability relationships from in situ data and effects of temperature and chemical‐mechanical couplings. Canada. https://doi.org/10.1111/gfl.12089
Rutqvist, J. Fri .
"Fractured rock stress‐permeability relationships from in situ data and effects of temperature and chemical‐mechanical couplings". Canada. https://doi.org/10.1111/gfl.12089.
@article{osti_1221699,
title = {Fractured rock stress‐permeability relationships from in situ data and effects of temperature and chemical‐mechanical couplings},
author = {Rutqvist, J.},
abstractNote = {Abstract The purpose of this paper is to (i) review field data on stress‐induced permeability changes in fractured rock; (ii) describe estimation of fractured rock stress‐permeability relationships through model calibration against such field data; and (iii) discuss observations of temperature and chemically mediated fracture closure and its effect on fractured rock permeability. The field data that are reviewed include in situ block experiments, excavation‐induced changes in permeability around tunnels, borehole injection experiments, depth (and stress) dependent permeability, and permeability changes associated with a large‐scale rock‐mass heating experiment. Data show how the stress‐permeability relationship of fractured rock very much depends on local in situ conditions, such as fracture shear offset and fracture infilling by mineral precipitation. Field and laboratory experiments involving temperature have shown significant temperature‐driven fracture closure even under constant stress. Such temperature‐driven fracture closure has been described as thermal overclosure and relates to better fitting of opposing fracture surfaces at high temperatures, or is attributed to chemically mediated fracture closure related to pressure solution (and compaction) of stressed fracture surface asperities. Back‐calculated stress‐permeability relationships from field data may implicitly account for such effects, but the relative contribution of purely thermal‐mechanical and chemically mediated changes is difficult to isolate. Therefore, it is concluded that further laboratory and in situ experiments are needed to increase the knowledge of the true mechanisms behind thermally driven fracture closure, and to further assess the importance of chemical‐mechanical coupling for the long‐term evolution of fractured rock permeability.},
doi = {10.1111/gfl.12089},
journal = {Geofluids},
number = 1-2,
volume = 15,
place = {Canada},
year = {Fri Sep 19 00:00:00 EDT 2014},
month = {Fri Sep 19 00:00:00 EDT 2014}
}
https://doi.org/10.1111/gfl.12089
Web of Science
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