Temperature-programmed pyrolysis (TPP) experiments are conducted on two high-sulfur South Australian low-rank coals, Bowmans and Lochiel coals, and several acid-washed and ion-exchanged Bowmans coal samples to study sulfur retention, changes in sulfur forms, and the influence of inorganic matter on sulfur transformations during pyrolysis. Changes in sulfur forms between 200 and 900 °C are monitored by Australian Standards wet chemical analysis and confirmed by scanning electron microcscopy (SEM) combined with energy dispersive X-ray analysis (EDX). The TPP results show retention of sulfur at low pyrolysis temperatures (400-800 °C) due to the decomposition of sulfate sulfur and its solid-state transformation to organic sulfur in the char. The retention is enhanced for higher sulfate contents and lower sulfate volatilities and suppressed by a greater proportion and decomposition of organic sulfur species between 300 and 600 °C. For acid-washed and ion-exchanged coal samples, organic sulfur decomposition above 600 °C is suppressed by the addition of organically bound sodium and calcium ions, as well as calcium carbonate constituents in the coal. The presence of organically bound calcium facilitates reactions with organic sulfur to form sulfide sulfur in the char. Organically bound sodium and discrete carbonate materials do not appear to form sulfides to any substantial degree. Hence, their effect on total sulfur retention requires further investigation. Substantial discrepancies exist between sulfide formation in Bowmans and Lochiel coals, despite similar inorganic matter.
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