Aqueous sulphates from the Stripa groundwater system

Details Aqueous sulphates from the Stripa groundwater system Aqueous sulphates from the Stripa groundwater system

Aug 1989

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1989gecoa..53.1783f&link_type=abstract

Geochimica et Cosmochimica Acta, vol. 53, Issue 8, pp.1783-1789

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Scientific paper

The isotopic composition of aqueous sulphate in the groundwater in the Stripa pluton reflects the geochemical history of the groundwater as well as the origin of the sulphur or sulphate. In shallow, modern groundwater, sulphate originates from fallout and the oxidation of pyrite or other reduced forms of sulphur. At intermediate depths, sulphate of surface origin is lost through bacterial reduction. The origin of sulphate of the deep and more saline water is not clearly defined but could be derived from a sedimentary brine which was subject to substantial modification through rock-water interaction. Bacterial sulphate reduction also occurs locally at depths below about 800 m.

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