Periodical changes of submarine fluid discharge from a deep seafloor, Suiyo Sea Mountain, Japan

Details Periodical changes of submarine fluid discharge from a deep seafloor, Suiyo Sea Mountain, Japan Periodical changes of submarine fluid discharge from a deep seafloor, Suiyo Sea Mountain, Japan

Sep 2003

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2003georl..30roce1t&link_type=abstract

Geophysical Research Letters, Volume 30, Issue 18, pp. OCE 1-1, CiteID 1917, DOI 10.1029/2003GL017924

Mathematics

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Marine Geology And Geophysics: Heat Flow (Benthic) And Hydrothermal Processes, Hydrology: Groundwater Hydrology, Oceanography: Biological And Chemical: Hydrothermal Systems, Oceanography: Physical: Surface Waves And Tides (1255)

Scientific paper

Semi-diurnal variations of the fluid discharge from the deep sea bottom were found at the water depth of 1360 m, Suiyo Sea Mountain, Ogasawara, Japan, by using newly developed automated seepage meters. A temperature depth profile of the pore water under the seabed also suggests heat is transported due to advection by the upward fluid flow. Upward fluid fluxes estimated from the type curve method using heat conduction-convection theory agreed well with the values obtained by automated seepage meter.

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