Permeability, compressibility, and friction coefficient measurements under confining pressure and strain, Leg 190, Nankai Trough
Sylvain Bourlange, Laurence Jouniaux, Pierre Henry
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.
Create a lesson
Related papers
Quantifying the effects of nickel on Earth's inner-core nucleation
Jiahui Zhai, Liangrui Wei, Chen Gao et al.
Global Prevalence of Anti-similar Earthquakes at Intermediate Depth
Albert Leonardo Aguilar Suarez, Gregory Beroza, William Ellsworth et al.
Lab earthquakes confirm the theory of frictional slip pulses
Alina Shafir, Tom Gabrieli, Yuval Tal et al.
Continually learning neural-operator surrogate for three-dimensional airborne electromagnetic Bayesian inversion
Jaehong Chung, Andrew Lockwood, Jef Caers
GeoFormer: Geometry-Aware Transformer and its application to 5D First-Arrival Picking
Tianxiang Gao, Jianwei Ma
A 3D VTI factored eikonal solver using six-tetrahedron pyramidal stencil
Yuhang Wang, Yongming Lu, Jianming Zhang et al.