Executive SummaryA project was undertaken to characterize the oxidation of iron pyrite to the non-slagging species magnetite during pulverized coal combustion. The work was aimed at defining the pyrite transformations responsible for the higher slagging propensity of staged, low-NO x pulverized coal combustor burners. With such burners, coal is injected into a reducing environment. Consequently, the products of pyrite combustion become shifted from non-depositing, oxidized species such as Fe 3 O 4 to highly-depositing, reduced species such as FeO and Fe 1-x S, where x ranges from 0 to 0.125. The propensity for slagging can be minimized by the judicious redistribution of furnace air to maximize the oxide formation rate. This must be accomplished with minimal degradation of other aspects of boiler performance. To effect this, an understanding of the rate-limiting mechanisms of pyrite oxidation is required.The overall objectives of this project were to characterize the various mechanisms that control overall pyrite combustion rates and to synthesize the mechanisms into a pyrite combustion model. These objectives were achieved. The model produced has the capability of being incorporated into numerical codes developed to predict phenomena occurring in coal-fired boilers and furnaces. Such comprehensive codes can be used to formulate and test strategies for enhancing pyrite transformation rates that involve the minor adjustment of firing conditions. Ultimately, the benefit of this research project is intended to be an increase in the range of coals compatible with staged, low-NO x combustor retrofits. Project activities were aimed at identifying the mechanisms of pyrite combustion and quantifying their effects on the overall oxidation rate in order to formulate a model for pyrite conversion during coal combustion. Chemical and physical processes requiring characterization included pyrite intraparticle kinetics and mass transfer, gas-phase kinetics and mass transfer, and carbon matrix kinetics and mass transfer.In our efforts, time-resolved phase identifications of extraneous pyrite combustion products were used to determine a pyrite oxidation pathway. Combustion tests indicated that pyrite oxidizes through the following reaction sequence:Pyrite (FeS 2 ) is transformed to troilite (FeS), which is oxidized to wusite (FeO). The troilite-towusite transformation involves oxidation of an oxysulfide melt (Fe-S-O) melt to an iron-oxide melt (Fe-O) melt . Magnetite (Fe 3 O 4 , really, FeO·Fe 2 O 3 ) crystallizes from the oxide melt after complete melt oxidation. At high oxygen levels, crystallized magnetite is oxidized to hematite (Fe 2 O 3 ). Pyrrhotite (Fe 1-x S) is a product of FeS 2 decomposition that rapidly oxidizes as part of the 3 oxysulfide melt. Based on the above reaction sequence, a detailed chemical reaction mechanism for pyrite oxidation was developed. The mechanism was employed in models developed for the oxidation of extraneous pyrite particles and pyrite inclusions in coal.A key feature of the experimental app...