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The solubility of copper in high-temperature magmatic vapors: A quest for the significance of various chloride and sulfide complexes
Authors:Zoltán Zajacz  Jung Hun Seo  Philip M Piccoli
Institution:a Department of Geology, University of Maryland, College Park, MD, USA
b Institute of Geochemistry and Petrology, ETH Zürich, Zürich, Switzerland
c Department of Chemistry & Biochemistry, University of Maryland, College Park, MD, USA
Abstract:We conducted experiments to determine the effect of various chemical components (NaCl, KCl, HCl, FeCl2, H2S, SO2) on the solubility of Cu in single phase aqueous vapors at 1000 °C and 150 MPa. The experiments were conducted in Au97Cu3 alloy capsules buffering Cu activities at 0.01. The volatile phase was sampled at run conditions by the entrapment of synthetic fluid inclusions in quartz. To test if the volatile phase had reached equilibrium before the isolation of the inclusions by fracture healing, we trapped two inclusion generations, one in an initially prefractured chip and another in a quartz chip that was fractured in situ during the experiments. The synthetic fluid inclusions were subsequently analyzed by laser ablation inductively coupled plasma mass spectrometry. In pure water, the apparent solubility of Cu is below the limits of detection of 6 μg/g, showing the low stability of hydroxy Cu complexes at our experimental conditions. The presence of alkali chlorides supports modest Cu solubility likely in the form of NaCuCl2 and KCuCl2 complexes. In the H2O-H2S (+SiO2 and Au97Cu3) system at an fH2S of 10.4 MPa the apparent solubility of Cu is lower by a factor of ∼5 than that in a S-free 0.5 m NaCl solution, showing that copper hydrosulfide complexes are only moderately stable at these conditions. Addition of 4.7 mol% of sulfur to the H2O-NaCl system at an fO2 of 0.4 log units below the Ni-NiO buffer, yielding dominantly H2S species, results in only a moderate increase in apparent Cu solubility, which diminishes in the presence of HCl. The addition of KCl results in a strong increase of apparent Cu solubility in the presence of H2S. The solubility of Cu increases with the fugacity of oxygen in both the H2O-NaCl and the H2O-S-NaCl system following an approximately fourth root relationship as expected based on the stoichiometry of the involved redox reactions. Replacement of NaCl by FeCl2 exerted only a minor effect on the Cu solubility.Results of our experiments, combined with thermochemical data obtained by ab initio quantum chemical calculations, suggest dissolution of Cu dominantly as Na(/K)CuCl2, Na(/K)Cu(HS)2, H2SCuHS, and Na(/K)ClCuHS, the relative abundance of which are dictated by the H2S/total chloride and HCl/alkali chloride ratios.
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