Chemical osmosis, reverse chemical osmosis, and the origin of subsurface brines (reply to a comment by F. M. Phillips)

Details Chemical osmosis, reverse chemical osmosis, and the origin of subsurface brines (reply to a comment by F. M. Phillips) Chemical osmosis, reverse chemical osmosis, and the origin of subsurface brines (reply to a comment by F. M. Phillips)

Jul 1983

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1983gecoa..47.1333g&link_type=abstract

Geochimica et Cosmochimica Acta, vol. 47, Issue 7, p.1333

Physics

1

Scientific paper

The osmotic inefficiency of shales makes it possible for the aquathermal pressuring below shale insulators in thick sedimentary sequences to drive reverse chemical osmosis. Topographic relief will also be effective in many localities. The latter mechanism is helpful in explaining the observed substitution for marine water molecules of fresh-water ones in the pore fluids of marine sedimentary sequences.

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