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Coprecipitation of Sr/sup 2 +/ with calcite at 25/sup 0/C and 1 atm

Journal Article · · Geochim. Cosmochim. Acta; (United States)

The incorporation of Sr/sup 2 +/ into calcite at earth surface aqueous conditions is affected by the absolute concentration of Sr/sup 2 +/, the presence of Ba/sup 2 +/ and NaCl in the solution, and the rate of precipitation. At solution ratios (molar) of Sr/sup 2 +/ to Ca/sup 2 +/ in the low 10/sup -3/ range, which yield calcites with several hundred ppm Sr/sup 2 +/, k/sub calcite//sup Sr/ typically assumes a value between 0.10 and 0.20. Above these concentrations the value of k/sub calcite//sup Sr/ drops to approximately 0.06. Furthermore, if minor amounts of Ba/sup 2 +/ or large amounts of Na/sup +/ (0.48 M) are added to a dilute Sr/sup 2 +/ solution, a value around 0.06 for k/sub calcite//sup Sr/ is found. This strontium concentration effect and the associated competitive cation effect suggest that small amounts of Sr/sup 2 +/ may be incorporated into a limited number of nonlattice sites in calcite. Incorporation of Sr/sup 2 +/ into these sites, presumably defects, noticeably affects k/sub calcite//sup Sr/ only at low Sr/sup 2 +/ concentrations and in the absence of competition from other large cations. An increase in k/sub calcite//sup Sr/ with rate of precipitation, qualitatively similar to that found in other studies, was observed only when precipitation times were decreased from days to hours. For many geologic settings a partition coefficient for Sr/sup 2 +/ into calcite of 0.06 appears appropriate, but there are situations - very low Sr/sup 2 +/ concentrations, the presence of Mg/sup 2 +/, and fast precipitation rates - in which a larger value might better approximate natural partitioning.

Research Organization:
Univ. of Texas, El Paso
OSTI ID:
6896643
Journal Information:
Geochim. Cosmochim. Acta; (United States), Journal Name: Geochim. Cosmochim. Acta; (United States) Vol. 50:10; ISSN GCACA
Country of Publication:
United States
Language:
English