Article ID Journal Published Year Pages File Type
4706288 Geochimica et Cosmochimica Acta 2006 17 Pages PDF
Abstract
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|Ag2S,'FeS',FeS2|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):logaS2(γ+py)=(15.64±0.035)-(15455±23)·T-1,(601
Related Topics
Physical Sciences and Engineering Earth and Planetary Sciences Geochemistry and Petrology
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