Data report: permeability measurements under confining pressure, Expeditions 315 and 316, Nankai Trough.
Résumé
Permeability of six samples from sites C0001 and C0006 were measured in a triaxial cell under effective hydrostatic confining pressure from 1 to 30 MPa. Our results indicate that the initial permeability at 1 MPa of effective confining pressure ranges from 4.6e-18 to 1.8e-19 m2 depending on depth. Actually permeability decreases with increasing depth also corresponding to a decrease of porosity from 62 to 43%. The permeability vs. depth trend is similar for both sites. When the effective confining pressure is increased from 1 to 30 MPa, the permeability decreases for all samples, a decrease interpreted by microfracture closure. However this trend shows some variability indicating a finer microstructural control depending on the lithological origin of the sample.
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