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Title: The solubility of sphalerite and galena in 1-5 m NaCl solutions to 300 degree C

Journal Article · · Geochimica et Cosmochimica Acta; (USA)
 [1];  [2]
  1. McGill Univ., Montreal, Quebec (Canada)
  2. Univ. of Toronto, Ontario (Canada)

Sphalerite and galena solubilities have been experimentally determined under H{sub 2}S-saturated conditions over the 3-5 molal (=m) NaCl range and for temperatures up to 95{degree}C. Using recent literature values for the stability constants of the chloride complexes of Zn and Pb up to 300{degree}C, the authors have calculated ZnS and PbS solubilities over the 25-300{degree}C and 1-5 m NaCl range. Field data from various geothermal systems have been used to calculate equilibrium solubilities of sphalerite and galena in these systems. High-salinity brines appear to range from supersaturated (Salton Sea, high-temperature) to strongly supersaturated (Red Sea, low temperature) with respect to these sulfides. By contrast, high-temperature seawater-salinity solutions at sediment-free spreading axes are grossly undersaturated in sphalerite and galena. The latter situation is of interest in that massive sulfide deposits are nevertheless forming from such solutions. On the other hand, vent fluids depositing sulfides at the sediment-covered axis in the Guaymas Basin appear to be near saturation in sphalerite and galena. This is probably related to the higher pH of these fluids, and the higher metal contents of the underlying sediments relative to basalts. Calculated solubilities for on-land geothermal systems yield values in reasonable agreement (<0.2 log units) in two of three cases.

OSTI ID:
5327375
Journal Information:
Geochimica et Cosmochimica Acta; (USA), Vol. 52:4; ISSN 0016-7037
Country of Publication:
United States
Language:
English