Ion-exchange fractionation of copper and zinc isotopes

Whether transition element isotopes can be fractionated at equilibrium in nature is still uncertain. Standard solutions of Cu and Zn were eluted on an anion-exchange resin, and the isotopic compositions of Cu (with respect to Zn) of the eluted fractions were measured by multiple-collector inductively coupled plasma mass spectrometry. It was found that for pure Cu solutions, the elution curves are consistent with a Cu-63/Cu-65 mass fractionation coefficient of 0.46%, in 7 mot/L HCl and 0.67parts per thousand in 3 mol/L HCl between the resin and the solution. Batch fractionation experiments confirm that equilibrium fractionation of Cu between resin and 7 mol/L HCl is similar to0.4parts per thousand and therefore indicates that there is no need to invoke kinetic fractionation during the elution, Zn isotope fractionation is an order of magnitude smaller, with a 66 Zn-66/Zn-68 fractionation factor of 0.02parts per thousand. in 12 mol/L HCl. Cu isotope fractionation results determined from a chalcopyrite solution in 7 mot/L HCl give a fractionation factor of 0.58parts per thousand, which indicates that Fe may interfere with Cu fractionation. Comparison of Cu and Zn results suggests that the extent of Cu isotopic fractionation may signal the presence of so far unidentified polynuclear complexes in solution. In contrast, we see no compelling reason to ascribe isotope fractionation to the coexistence of different oxidation states. We further suggest that published evidence for iron isotopic fractionation in nature and in laboratory experiments may indicate the distortion of low-spin Fe tetrahedral complexes. The isotope geochemistry of transition elements may shed new light on their coordination chemistry. Their isotopic fractionation in the natural environment may be interpreted using models of thermodynamic fractionation. Copyright (C) 2002 Elsevier Science Ltd.