Permeability, compressibility, and friction coefficient measurements under confining pressure and strain, Leg 190, Nankai Trough
Permeability measured on three samples in a triaxial cell under effective confining pressure from 0.2 to 2.5 MPa ranges from 10E-18 to 10E-19m2. Overall, results indicate that permeability decreases with effective confining pressure up to 1.5 MPa; however, measurements at low effec-tive pressure are...
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Veröffentlicht in: | Proceedings of the Ocean Drilling Program. Scientific results 2004, Vol.190/196 |
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container_title | Proceedings of the Ocean Drilling Program. Scientific results |
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creator | Bourlange, Sylvain Jouniaux, Laurence Henry, Pierre |
description | Permeability measured on three samples in a triaxial cell under effective confining pressure from 0.2 to 2.5 MPa ranges from 10E-18 to 10E-19m2. Overall, results indicate that permeability decreases with effective confining pressure up to 1.5 MPa; however, measurements at low effec-tive pressure are too dispersed to yield a precise general relationship between permeability and pressure. When the effective pressure is increased from 1.5 to 2.5 MPa, permeability is roughly constant (~1-4 x 10E-19 m2). Samples deformed in the triaxial cell developed slickenlined fractures, and permeability measurements were performed before and after failure. A permeability increase is observed when the sample fails under low effective confining pressure (0.2 MPa), but not under effective pressure corresponding to the overburden stress. Under isotropic stress conditions, permeability decrease related to fracture closure occurs at a relatively high effective pressure of ~1.5 MPa. Coefficients of friction on the fractures formed in the triaxial cell are ~0.4. |
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Overall, results indicate that permeability decreases with effective confining pressure up to 1.5 MPa; however, measurements at low effec-tive pressure are too dispersed to yield a precise general relationship between permeability and pressure. When the effective pressure is increased from 1.5 to 2.5 MPa, permeability is roughly constant (~1-4 x 10E-19 m2). Samples deformed in the triaxial cell developed slickenlined fractures, and permeability measurements were performed before and after failure. A permeability increase is observed when the sample fails under low effective confining pressure (0.2 MPa), but not under effective pressure corresponding to the overburden stress. Under isotropic stress conditions, permeability decrease related to fracture closure occurs at a relatively high effective pressure of ~1.5 MPa. 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Scientific results</title><description>Permeability measured on three samples in a triaxial cell under effective confining pressure from 0.2 to 2.5 MPa ranges from 10E-18 to 10E-19m2. Overall, results indicate that permeability decreases with effective confining pressure up to 1.5 MPa; however, measurements at low effec-tive pressure are too dispersed to yield a precise general relationship between permeability and pressure. When the effective pressure is increased from 1.5 to 2.5 MPa, permeability is roughly constant (~1-4 x 10E-19 m2). Samples deformed in the triaxial cell developed slickenlined fractures, and permeability measurements were performed before and after failure. A permeability increase is observed when the sample fails under low effective confining pressure (0.2 MPa), but not under effective pressure corresponding to the overburden stress. Under isotropic stress conditions, permeability decrease related to fracture closure occurs at a relatively high effective pressure of ~1.5 MPa. Coefficients of friction on the fractures formed in the triaxial cell are ~0.4.</description><subject>Earth Sciences</subject><subject>Environmental Sciences</subject><subject>Geophysics</subject><subject>Global Changes</subject><subject>Physics</subject><subject>Sciences of the Universe</subject><subject>Tectonics</subject><issn>1096-7451</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2004</creationdate><recordtype>article</recordtype><recordid>eNqVjLFuwkAQRK9IJEjCP2wbyUh3cgy4jCIiCoQo6K3F3rM3sddoz0aiy6fnQMkHUM1o3sw8mKmz-WK-fMvcxDyF8GVtmq3yfGp-9qQd4ZFbHi4JlH13UgqB_wOUCrxyOXAvkZL3XDLJAHEURqUu-gCjVKQRi2dhqeH2EeltHgZFlgS2VIPLbQI7lG9kOGg_1s2LefTYBpr96bN5_VwfPjbzBtvipNyhXooeudi8b4trZq2zq9S5s0vv6f4C3MVT-w</recordid><startdate>2004</startdate><enddate>2004</enddate><creator>Bourlange, Sylvain</creator><creator>Jouniaux, Laurence</creator><creator>Henry, Pierre</creator><general>Ocean Drilling Program</general><scope>1XC</scope><scope>VOOES</scope><orcidid>https://orcid.org/0000-0002-2288-6805</orcidid><orcidid>https://orcid.org/0000-0002-8047-0680</orcidid><orcidid>https://orcid.org/0000-0002-6391-5836</orcidid><orcidid>https://orcid.org/0000-0002-6391-5836</orcidid><orcidid>https://orcid.org/0000-0002-2288-6805</orcidid><orcidid>https://orcid.org/0000-0002-8047-0680</orcidid></search><sort><creationdate>2004</creationdate><title>Permeability, compressibility, and friction coefficient measurements under confining pressure and strain, Leg 190, Nankai Trough</title><author>Bourlange, Sylvain ; Jouniaux, Laurence ; Henry, Pierre</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-hal_primary_oai_HAL_hal_00108311v13</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2004</creationdate><topic>Earth Sciences</topic><topic>Environmental Sciences</topic><topic>Geophysics</topic><topic>Global Changes</topic><topic>Physics</topic><topic>Sciences of the Universe</topic><topic>Tectonics</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Bourlange, Sylvain</creatorcontrib><creatorcontrib>Jouniaux, Laurence</creatorcontrib><creatorcontrib>Henry, Pierre</creatorcontrib><collection>Hyper Article en Ligne (HAL)</collection><collection>Hyper Article en Ligne (HAL) (Open Access)</collection><jtitle>Proceedings of the Ocean Drilling Program. Scientific results</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Bourlange, Sylvain</au><au>Jouniaux, Laurence</au><au>Henry, Pierre</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Permeability, compressibility, and friction coefficient measurements under confining pressure and strain, Leg 190, Nankai Trough</atitle><jtitle>Proceedings of the Ocean Drilling Program. Scientific results</jtitle><date>2004</date><risdate>2004</risdate><volume>190/196</volume><issn>1096-7451</issn><abstract>Permeability measured on three samples in a triaxial cell under effective confining pressure from 0.2 to 2.5 MPa ranges from 10E-18 to 10E-19m2. Overall, results indicate that permeability decreases with effective confining pressure up to 1.5 MPa; however, measurements at low effec-tive pressure are too dispersed to yield a precise general relationship between permeability and pressure. 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subjects | Earth Sciences Environmental Sciences Geophysics Global Changes Physics Sciences of the Universe Tectonics |
title | Permeability, compressibility, and friction coefficient measurements under confining pressure and strain, Leg 190, Nankai Trough |
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