Physics
Scientific paper
Jul 1982
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1982gecoa..46.1183t&link_type=abstract
Geochimica et Cosmochimica Acta, vol. 46, Issue 7, pp.1183-1191
Physics
30
Scientific paper
Kinetic isotope fractionation of 13 C during precipitation of CaCO 3 under open system conditions has been investigated. The isotope enrichment factor HCO 3 - - CaCO 3 varies between -0.35 ± 0.23 and -3.37 ± 0.36%. at 25°C depending on the rate of precipitation and mineralogy, the enrichment of 13 C in the solid carbonate phase decreasing with increasing precipitation rate. An estimate of equilibrium HCO 3 - Calcite of between -1.83 ± 0.32 and -2.26 ± 0.31%. is calculated from slow precipitation runs. A surface diffusion crystal growth model is used to describe the combination of kinetic isotope effects on thermodynamic isotope fractionation during rapid diffusion controlled crystal growth. Under slow precipitation conditions Calcite - Aragonite was estimated as -1.4%.; however, during rapid precipitation this fractionation appears to diminish and aragonite becomes less enriched in 13 C.
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