Bourlange, Sylvain et al. (2005): Permeability, compressibility, and friction coefficient measurements under confining pressure and strain, Leg 190, Nankai Trough

Leg/Site/Hole:
ODP 190
Identifier:
2005-060946
georefid

10.2973/odp.proc.sr.190196.215.2004
doi

Creator:
Bourlange, Sylvain
Ecole Normale Superieure, Laboratoire de Geologie, Paris, France
author

Jouniaux, Laurence
University of Tokyo, Japan
author

Henry, Pierre
author

Identification:
Permeability, compressibility, and friction coefficient measurements under confining pressure and strain, Leg 190, Nankai Trough
2005
In: Moore, Gregory F., Taira, Asahiko, Klaus, Adam, Becker, Keir, Becker, Luann, Boeckel, Babette, Cragg, Barry A., Dean, P. Allison, Fergusson, Christopher L., Henry, Pierre, Hirano, Satoshi, Hisamitsu, Toshio, Hunze, Sabine, Kastner, Miriam, Maltman, Alex J., Morgan, Julia K., Murakami, Yuki, Saffer, Demian M., Sanchez-Gomez, Mario, Screaton, Elizabeth J., Smith, David C., Spivack, Arthur J., Steurer, Joan F., Tobin, Harold J., Ujiie, Kohtaro, Underwood, Michael B., Wilson, Moyra E. J., Mikada, Hitoshi, Moore, J. Casey, Austin, Gary L., Bangs, Nathan L. B., Bourlange, Sylvain, Broilliard, Julien, Brueckmann, Warner, Corn, Ernest Ray, Davis, Earl E., Flemings, Peter B., Goldberg, David S., Gulick, Sean P. S., Hansen, Martin Bak, Hayward, Nathan, Hills, Denise J., Ienaga, Masanori, Ishiguro, Hiroyasu, Kinoshita, Masataka, Macdonald, Robert D., McNeill, Lisa, Obana, Shinichi, Hong, Ong Swee, Peacock, Sheila, Pettigrew, Thomas L., Saito, Saneatsu, Sawa, Takao, Thaiprasert, Nophawit, Tsurumi, Hikaru, Proceedings of the Ocean Drilling Program; scientific results; deformation and fluid flow processes in the Nankai Trough accretionary prism; coring, logging while drilling and advanced CORKs covering Legs 190 to 196 of the cruises of the drilling vessel JOIDES Resolution; Sydney, Australia, to Yokohama, Japan, Sites 1173-1178, 23 May-16 July 2000; and Keelung, Taiwan, to Kochi, Japan, Sites 808-1173, 2 May-1 July 2001
Texas A&M University, Ocean Drilling Program, College Station, TX, United States
190/196
Permeability measured on three samples in a triaxial cell under effective confining pressure from 0.2 to 2.5 MPa ranges from 10-18 to 10-19 m (super 2) . Overall, results indicate that permeability decreases with effective confining pressure up to 1.5 MPa; however, measurements at low effective 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 ( approximately 1-4 x 10-19 m (super 2) ). 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 approximately 1.5 MPa. Coefficients of friction on the fractures formed in the triaxial cell are approximately 0.4.
English
Coverage:Geographic coordinates:
North:32.4500
West:134.0000East: 135.1500
South:31.3000

Structural geology; compressibility; confining pressure; decollement; failures; fractures; friction; Leg 190; marine sediments; mathematical models; measurement; mechanical properties; Nankai Trough; North Pacific; Northwest Pacific; Ocean Drilling Program; Pacific Ocean; permeability; rock mechanics; sedimentary rocks; sediments; slickenlines; soil mechanics; structural analysis; triaxial tests; West Pacific;

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