A XANES STUDY OF CU SPECIATION IN HIGH-TEMPERATURE BRINES USING SYNTHETIC FLUID INCLUSIONS

dc.contributor.authorBerry A.J.
dc.contributor.authorHack A.C.
dc.contributor.authorMavrogenes J.A.
dc.contributor.authorNewville M.
dc.contributor.authorSutton S.R.
dc.date.accessioned2024-09-22T02:54:21Z
dc.date.available2024-09-22T02:54:21Z
dc.date.issued2006
dc.description.abstractCu 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 Cu2+ can both be identified from characteristic pre-edge features. Mixed oxidation states can be deconvoluted using linear combinations of Cu+ and Cu2+ spectra. This work illustrates how complex Cu XANES spectra can be interpreted successfully. Cu2+ 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 [CuCl2]- 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 [CuCl4]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.
dc.identifierhttps://www.elibrary.ru/item.asp?id=14357167
dc.identifier.citationAmerican Mineralogist, 2006, 91, 11-12, 1773-1782
dc.identifier.doi10.2138/am.2006.1940
dc.identifier.issn0003-004X
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/45369
dc.subjectCU IN HIGH-TEMPERATURE BRINES
dc.subjectEXPERIMENTAL PETROLOGY
dc.subjectFLUID PHASE
dc.subjectHIGH-TEMPERATURE STUDIES
dc.subjectSYNTHETIC FLUID INCLUSIONS
dc.subjectXANES OF FLUID INCLUSIONS
dc.subjectXAS (XAFS, XANES)
dc.titleA XANES STUDY OF CU SPECIATION IN HIGH-TEMPERATURE BRINES USING SYNTHETIC FLUID INCLUSIONS
dc.typeСтатья

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