English (United Kingdom)

https://curated-unify.zendy.io/wp-json/zendy-region/v1/featured_content/oa?rat=en

https://curated-unify.zendy.io/wp-json/zendy-region/v1/highlighted_journal/

Global: Zendy Plus annual

Presents the access of premium content as premium feature

Premium Content

Presents the keyphrase highlighting as premium feature

Keyphrase Highlighting

Presents the summarisation as premium feature

Summarisation

Insights

Presents the pdf analysis as premium feature

PDF Analysis

Presents the zaia usage as premium feature

ZAIA

Global: Zendy Tools annual

Global: Zendy Free Plan

Global: Zendy Tools monthly

Global: Zendy Plus monthly

International audiencePermeability 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

Data report: permeability measurements under confining pressure, Expeditions 315 and 316, Nankai Trough