A new view on gold speciation in sulfur-bearing hydrothermal fluids from in situ X-ray absorption spectroscopy and quantum-chemical modeling

• Published in: Geochimica et cosmochimica acta Vol. 73; no. 18; pp. 5406 - 5427
• Main Authors: Pokrovski, Gleb S., Tagirov, Boris R., Schott, Jacques, Hazemann, Jean-Louis, Proux, Olivier
• Format: Journal Article
• Language: English
• Published: Elsevier Ltd 15.09.2009; Elsevier
• Subjects: Instrumentation and Detectors; Physics; gold; XAFS spectroscopy; quantum- 25 chemical modeling; hydrothermal fluid; sulfur; Au-S complexes; thermodynamic properties
• ISSN: 0016-7037; 1872-9533
• DOI: 10.1016/j.gca.2009.06.007

Despite the common belief that Au I complexes with hydrogen sulfide ligands (H 2S/HS −) are the major carriers of gold in natural hydrothermal fluids, their identity, structure and stability are still subjects of debate. Here we present the first in situ measurement, using X-ray absorption fine structure (XAFS) spectroscopy, of the stability and structure of aqueous Au I–S complexes at temperatures and pressures ( T–P) typical of natural sulfur-rich ore-forming fluids. The solubility of native gold and the local atomic structure around the dissolved metal in S–NaOH–Na 2SO 4–H 2SO 4 aqueous solutions were characterized at temperatures 200–450 °C and pressures 300–600 bar using an X-ray cell that allows simultaneous measurement of the absolute concentration of the absorbing atom (Au) and its local atomic environment in the fluid phase. Structural and solubility data obtained from XAFS spectra, combined with quantum-chemical calculations of species geometries, show that gold bis(hydrogensulfide) Au(HS) 2 − is the dominant Au species in neutral-to-basic solutions (5.5 ⩽ pH ⩽ 8.5; H 2O–S–NaOH) over a wide range of sulfur concentrations (0.2 < ΣS < 3.6 mol/kg), in agreement with previous solubility studies. Our results provide the first direct determination of this species structure, in which two sulfur atoms are in a linear geometry around Au I at an average distance of 2.29 ± 0.01 Å. At acidic conditions (1.5 ⩽ pH ⩽ 5.0; H 2O–S–Na 2SO 4–H 2SO 4), the Au atomic environment determined by XAFS is similar to that in neutral solutions. These findings, together with measured high Au solubilities, are inconsistent with the predominance of the gold hydrogensulfide Au(HS) 0 complex suggested by recent solubility studies. Our spectroscopic data and quantum-chemical calculations imply the formation of species composed of linear S–Au–S moieties, like the neutral [H 2S–Au–SH] complex. This species may account for the elevated Au solubilities in acidic fluids and vapors with H 2S concentrations higher than 0.1–0.2 mol/kg. However, because of the complex sulfur speciation in acidic solutions that involves sulfite, thiosulfate and polysulfide species, the formation of Au I complexes with these ligands (e.g., AuHS(SO 2) 0, Au(HS 2O 3) 2 −, Au(HS n ) 2 −) cannot be ruled out. The existence of such species may significantly enhance Au transport by high T–P acidic ore-forming fluids and vapors, responsible for the formation of a major part of the gold resources on Earth.