“…When coal is combusted in pulverized-fuel (pf) boilers to produce electricity, mineral matter in the coal is transformed at elevated temperatures to produce ash and related materials (e.g., slagging and fouling deposits) of varying chemical composition, mineralogy, and physical characteristics (size, shape, viscosity, and density). − While some minerals, such as quartz, may be essentially nonreactive at the temperatures and exposure times associated with combustion, the clay minerals (e.g., kaolinite, illite, and montmorillonite) are reactive phases and usually start to lose water of hydration at temperatures below 500 °C . Carbonates such as calcite, dolomite, and siderite are also reactive, decomposing at temperatures typically between 400 and 1000 °C to liberate CO 2 and produce metal oxide residues (e.g., CaO, MgO, and FeO) .…”