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The solubility of nantokite (CuCl(s)) and Cu speciation in low-density fluids near the critical isochore: An in-situ XAS study |
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| Authors: | Weihua Liu Joël Brugger Barbara Etschmann Denis Testemale Jean-Louis Hazemann |
| Institution: | a CSIRO Exploration and Mining, School of Geosciences, Monash University, Clayton, Vic. 3800, Australia b School of Earth and Environmental Sciences, The University of Adelaide, SA 5000, Australia c Division of Mineralogy, South Australian Museum, North Terrace, SA 5000, Australia d CODES Centre of Excellence, University of Tasmania, TAS 7001, Australia e SNBL, ESRF, Polygone Scientifique, 6 rue Jules Horowitz, 38043 Grenoble, France f Institut Néel, Département MCMF, 25 Avenue des Martyrs, BP166 38042 Grenoble Cedex 09, France |
| Abstract: | The solubility of nantokite (CuCl(s)) and the structure of the predominant copper species in supercritical water (290-400 bar at 420 °C; 350-450 °C at 290 bar; 500 °C at 350 bar; density = 0.14-0.65 g/cm3) were investigated concurrently using synchrotron X-ray absorption spectroscopy (XAS) techniques. These conditions were chosen as they represent single phase solutions near the critical isochore, where the fluid density is intermediate of typical values for vapour and brine and is highly sensitive to even small changes in pressure. X-ray absorption near edge spectroscopy (XANES) and extended X-ray absorption spectroscopy (EXAFS) analyses show that aqueous copper occurs in a slightly distorted linear coordination in the solutions studied, with an average of 1.35(±0.3) Cl and 0.65(±0.3) O neighbours. The solubility of CuCl(s) decreases exponentially with decreasing water density (i.e., decreasing pressure at constant temperature), in a manner similar to the solubility behaviour of salts such as NaCl in water vapour. Based on this similarity, an apparent equilibrium constant for the dissolution reaction of 0.5 ± 0.4 was calculated from a regression of the data at 420 °C, and it was determined that each Cu atom is solvated by approximately three water molecules. This indicates that under these conditions, copper solubility is controlled mainly by the structure of the second-shell hydration, which is essentially invisible to the XAS techniques used in this study.These results demonstrate that for a supercritical fluid near the critical isochore, decreasing pressure may initiate precipitation of copper even before boiling or phase separation. Such a process could be responsible for near-surface ore deposition in seafloor hydrothermal systems, where supercritical fluids experience rapid pressure changes during the transition between lithostatic and hydrostatic domains. |
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