Speciation and thermodynamic properties of zinc in sulfur-rich hydrothermal fluids: Insights from ab initio molecular dynamics simulations and X-ray absorption spectroscopy
Speciation and thermodynamic properties of zinc in sulfur-rich hydrothermal fluids: Insights from ab initio molecular dynamics simulations and X-ray absorption spectroscopy
复制标题
DOI:
10.1016/j.gca.2016.01.031
复制
发表时间:
2016-04
影响因子:
5
通讯作者:
Y. Mei;B. Etschmann;Weihua Liu;D. Sherman;D. Testemale;J. Brugger
中科院分区:
文献类型:
--
作者:
Y. Mei;B. Etschmann;Weihua Liu;D. Sherman;D. Testemale;J. Brugger
Chlorine and sulfur are the main elements involved in the complexing of metals in ore-forming fluids. The nature and thermodynamic properties of the Zn(II)–Cl complexes have been investigated by previous experimental and theoretical studies and are now well established up to high temperatures (600 °C). In contrast, the role of bisulfide complexes for zinc speciation in sulfur-bearing fluids remains poorly known, and a better understanding of Zn(II)–HS complexation is required for modeling zinc transport in magmatic and metamorphic fluids and for optimizing the hydrometallurgical processing of sulfide ores.We have conductedab initiomolecular dynamics (MD) simulations to calculate the speciation of Zn(II)–HS complexes from ambient to hydrothermal-magmatic conditions (25–600 °C, up to 2000 bar). These theoretical calculations were complemented by X-ray absorption spectroscopy (XAS) measurements of Zn(II) in HS−-rich solutions at 200–500 °C and 600–1000 bar. The speciation and geometrical properties predicted by theab initioMD simulations and thein situXAS data are in excellent agreement. Upon heating from room temperature to 250 °C, Zn(II) speciation in HS−-rich solutions shows a transition from the sixfold octahedral hexaaquo complex [Zn(H2O)6]2+to fourfold tetrahedral [Zn(HS)n(H2O)4−n]2−ncomplexes (n= 1–4).Ab initioMD simulations also show that at temperatures > 250 °C, the threefold trigonal-planar [Zn(HS)3]−complex becomes increasingly stable, and predominates in S-rich solutions; in contrast, chloro-complexes display a tetrahedral geometry at 25–500 °C, while trigonal planar ZnCl3−predominates at temperatures > 500 °C. The stability constants of Zn(II)–HS complexes were calculated by thermodynamic integration of constrainedab initioMD simulations at 200, 350 and 600 °C. The stability constants generated from this study predict that zinc can be transported by HS−at high temperature in reduced, neutral to alkaline solutions, while Zn chloride complexes dominate in acidic fluids.