Thermodynamic studies of pyrrhotite pyrite equilibria in the Ag Fe S system by solid-state galvanic cell technique at 518 723 K and total pressure of 1 atm

Details Thermodynamic studies of pyrrhotite pyrite equilibria in the Ag Fe S system by solid-state galvanic cell technique at 518 723 K and total pressure of 1 atm Thermodynamic studies of pyrrhotite pyrite equilibria in the Ag Fe S system by solid-state galvanic cell technique at 518 723 K and total pressure of 1 atm

Nov 2006

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2006gecoa..70.5617o&link_type=abstract

Geochimica et Cosmochimica Acta, Volume 70, Issue 22, p. 5617-5633.

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The reaction FeS2(cr) + 2Ag(cr) = ‘FeS’(cr) + Ag2S(cr) was studied by measuring the temperature dependence of the electromotive force (EMF) of the all-solid-state galvanic cell with common gas space: (-)Pt|Ag|AgI|AgS,‘FeS’,FeS|Pt(+) The measurements were carried out in the flow of argon at atmospheric pressure to prevent oxidation. AgI was used as a solid electrolyte. From the measurements of EMF as a function of temperature, two linear (ΔrCp = 0) trends were obtained, which characterize the equilibrium hexagonal pyrrhotite + pyrite (po + py) and the β γ first-order phase transition in hexagonal pyrrhotite (ΔtrsHm(γ β) = (4020 ± 200) J mol-1) at (601 ± 2) K. The latter is presumably related to the γ-paramagnetic-β-antiferromagnetic Neel’s transition. For these measurements, the lower temperature limit (518 K) corresponds to the equilibrium sulfides + metallic silver (E = 0); and the upper temperature limit (723 K) is determined by the upper temperature at which the contribution of electron conductivity to AgI ion conductive properties may be significant. From experimental results of this study and literature data for Ag2S, the temperature dependence of the gaseous sulfur activity was determined in the following equilibria: pyrite + high-temperature hexagonal pyrrhotite (γ + py), pyrite + low-temperature pyrrhotite (β + py): logaS(γ+py)=(15.64±0.035)-(15455±23)·T,(601

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