Abstract

The enthalpy of thermal decomposition of pyrite concentrate (PC) in an inert atmosphere was measured by differential thermal analysis (DTA) and differential scanning calorimetry (DSC). The decomposition is a two-stage process and the enthalpy values of the overall process determined by the two methods are very close to each other: DTA, Δ H = 72.2 kJ per mol FeS 2; DSC, Δ H = 70.1 kJ per mol FeS 2. These values are quite different from the calculated standard enthalpy of FeS 2 decomposition at 1000 K, Δ H = 154.0 kJ per mol FeS 2, and the enthalpy calculated from the Clausius—Clapeyron equation with dissociation pressure data for FeS 2, Δ H = 181.9 kJ per mol FeS 2.

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