Cu K-edge X-ray absorption near edge structure (XANES) spectra were recorded from individual synthetic brine fluid inclusions as a function of temperature up to 500 °C. The inclusions serve as sample cells for high-temperature spectroscopic studies of aqueous Cu-Cl speciation. Cu + and Cu 2+ can both be identified from characteristic pre-edge features. Mixed oxidation states can be deconvoluted using linear combinations of Cu + and Cu 2+ spectra. This work illustrates how complex Cu XANES spectra can be interpreted successfully. Cu 2+ is the stable oxidation state in solution at room temperature and Cu + at high temperatures. The change in oxidation state with temperature was completely reversible. Cu + was found to occur exclusively as the linear species [CuCl 2 ] - in solutions containing KCl with Cu:Cl ratios up to 1:6. In the absence of K + , there is evidence for higher order coordination of Cu + , in particular the tetrahedral complex [CuCl 4 ] 3- . The importance of such complexes in natural ore-forming fluids is yet to be determined, but may explain the vapor-phase partitioning of Cu as a Cl complex from a Cl-rich brine.
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Berry et al. (2006) studied this question.
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