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...

Ausführliche Beschreibung

Gespeichert in:
Bibliographische Detailangaben
Veröffentlicht in:Proceedings of the Ocean Drilling Program. Scientific results 2004, Vol.190/196
Hauptverfasser: Bourlange, Sylvain, Jouniaux, Laurence, Henry, Pierre
Format: Artikel
Sprache:eng
Schlagworte:
Online-Zugang:Volltext
Tags: Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
container_end_page
container_issue
container_start_page
container_title Proceedings of the Ocean Drilling Program. Scientific results
container_volume 190/196
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.
format Article
fullrecord <record><control><sourceid>hal</sourceid><recordid>TN_cdi_hal_primary_oai_HAL_hal_00108311v1</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><sourcerecordid>oai_HAL_hal_00108311v1</sourcerecordid><originalsourceid>FETCH-hal_primary_oai_HAL_hal_00108311v13</originalsourceid><addsrcrecordid>eNqVjLFuwkAQRK9IJEjCP2wbyUh3cgy4jCIiCoQo6K3F3rM3sddoz0aiy6fnQMkHUM1o3sw8mKmz-WK-fMvcxDyF8GVtmq3yfGp-9qQd4ZFbHi4JlH13UgqB_wOUCrxyOXAvkZL3XDLJAHEURqUu-gCjVKQRi2dhqeH2EeltHgZFlgS2VIPLbQI7lG9kOGg_1s2LefTYBpr96bN5_VwfPjbzBtvipNyhXooeudi8b4trZq2zq9S5s0vv6f4C3MVT-w</addsrcrecordid><sourcetype>Open Access Repository</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype></control><display><type>article</type><title>Permeability, compressibility, and friction coefficient measurements under confining pressure and strain, Leg 190, Nankai Trough</title><source>U.S. Government Documents</source><source>Alma/SFX Local Collection</source><creator>Bourlange, Sylvain ; Jouniaux, Laurence ; Henry, Pierre</creator><creatorcontrib>Bourlange, Sylvain ; Jouniaux, Laurence ; Henry, Pierre</creatorcontrib><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><identifier>ISSN: 1096-7451</identifier><language>eng</language><publisher>Ocean Drilling Program</publisher><subject>Earth Sciences ; Environmental Sciences ; Geophysics ; Global Changes ; Physics ; Sciences of the Universe ; Tectonics</subject><ispartof>Proceedings of the Ocean Drilling Program. Scientific results, 2004, Vol.190/196</ispartof><rights>Distributed under a Creative Commons Attribution 4.0 International License</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><orcidid>0000-0002-2288-6805 ; 0000-0002-8047-0680 ; 0000-0002-6391-5836 ; 0000-0002-6391-5836 ; 0000-0002-2288-6805 ; 0000-0002-8047-0680</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>230,314,778,782,883,4012</link.rule.ids><backlink>$$Uhttps://hal.science/hal-00108311$$DView record in HAL$$Hfree_for_read</backlink></links><search><creatorcontrib>Bourlange, Sylvain</creatorcontrib><creatorcontrib>Jouniaux, Laurence</creatorcontrib><creatorcontrib>Henry, Pierre</creatorcontrib><title>Permeability, compressibility, and friction coefficient measurements under confining pressure and strain, Leg 190, Nankai Trough</title><title>Proceedings of the Ocean Drilling Program. 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. 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.</abstract><pub>Ocean Drilling Program</pub><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><oa>free_for_read</oa></addata></record>
fulltext fulltext
identifier ISSN: 1096-7451
ispartof Proceedings of the Ocean Drilling Program. Scientific results, 2004, Vol.190/196
issn 1096-7451
language eng
recordid cdi_hal_primary_oai_HAL_hal_00108311v1
source U.S. Government Documents; Alma/SFX Local Collection
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
url https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-01-16T22%3A53%3A23IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-hal&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Permeability,%20compressibility,%20and%20friction%20coefficient%20measurements%20under%20confining%20pressure%20and%20strain,%20Leg%20190,%20Nankai%20Trough&rft.jtitle=Proceedings%20of%20the%20Ocean%20Drilling%20Program.%20Scientific%20results&rft.au=Bourlange,%20Sylvain&rft.date=2004&rft.volume=190/196&rft.issn=1096-7451&rft_id=info:doi/&rft_dat=%3Chal%3Eoai_HAL_hal_00108311v1%3C/hal%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_id=info:pmid/&rfr_iscdi=true