Physics – Geophysics
Scientific paper
Sep 2009
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2009georl..3617308l&link_type=abstract
Geophysical Research Letters, Volume 36, Issue 17, CiteID L17308
Physics
Geophysics
2
Marine Geology And Geophysics: Gas And Hydrate Systems, Marine Geology And Geophysics: Marine Hydrogeology, Marine Geology And Geophysics: Submarine Landslides
Scientific paper
During sea-level drop, water and gas pressures within oceanic hydrate systems can exceed the total vertical stress and this can drive slope failure and gas venting. We investigate this behavior with a multi-phase fluid and heat flow model. During sea-level drop, fluid pressures drop much less than the total stress due to both the high gas compressibility and hydrate dissociation. In permeable sediments, hydrate dissociation, water expulsion and gas mobility combine to induce underpressure and downward water flow from the seafloor. This study provides a causal mechanism for slope failure and fluid exchange that occur in hydrate systems during sea-level fall.
Flemings Peter
Liu Xiaoli
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