“…MgO is mostly derived from the thermal decomposition of dolomite (CaMg(CO 3 ) 2 ) and this variability is evidently due to the variation in dolomite admixture in raw OS, depending on the geological section used for mining. The separation of S along the boiler gas pass in PF ashes shows a gradual enrichment in finer ash fractions, whereas in CFBC boilers, as expected, the S proportion is the highest in the ash removed in the INTREX preheater [37,39].…”