Computer Science
Scientific paper
Mar 1987
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1987gecoa..51..683p&link_type=abstract
Geochimica et Cosmochimica Acta, vol. 51, Issue 3, pp.683-695
Computer Science
3
Scientific paper
Fractionation of the isotopes of H, O, and Cl during flow of aqueous solutions through semipermeable clay discs has been observed in the laboratory. The observed isotopic abundance trends of these elements in deep sedimentary basins have been attributed to similar phenomena. However, the mechanism responsible for such isotopic fractionation has not been identified. We propose that the fractionation of O and H isotopes in the water molecule results from increased activity of the heavy isotopic species in the membrane solution because high cation concentrations in the membrane pore fluid increase hydrationsphere fractionation effects. The heavy isotopic species thus diffuse away from the membrane and therefore are concentrated behind it. Predictions based on this theory satisfactorily model both laboratory and field observations. We propose that the fractionation of chlorine isotopes is a result of differences in the ionic mobility of 35 Cl - and 37 Cl - . Negative charges on the membrane repel the isotopic species at slightly different velocities against the uniform advective motion of the bulk water and thus the more mobile 35 Cl - is enriched behind the membrane. Predictions calculated from this theory compare well with laboratory and field data.
Bentley Harold W.
Phillips Fred M.
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