The gypsum-anhydrite equilibrium by solubility measurements

Details The gypsum-anhydrite equilibrium by solubility measurements The gypsum-anhydrite equilibrium by solubility measurements

Dec 1980

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1980gecoa..44.1931i&link_type=abstract

Geochimica et Cosmochimica Acta, vol. 44, Issue 12, pp.1931-1936

Physics

1

Scientific paper

Solubility measurements have been used to establish the gypsum-anhydrite
equilibrium in the CaSO 4 -H 2 O system at atmospheric pressure. The
saturation equilibrium has been approached both from undersaturated and
supersaturated solutions. The invariant point temperature has been found
to be 49.5 ± 2.5° C .

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