“…As shown in Table 2, the maximum ΔT was 56 °C, which was below the difference between the FT values tested by different AFT detectors under a reducing atmosphere (80 °C, ISO 540-2008; 23 85 °C, ASTM D1857-04 26 ) and also less than the reproducible critical difference for the FT measurement according to the Chinese standard (80 °C, GB/T219-2008). From thermodynamic calculations, the mineral crystals of high calcium and high iron ash [e.g., TC ash (CaO, 28.62%; Fe 2 O 3 , 18.95%)] are mainly in the forms of fayalite, hercynite, dicalcium silicate, feldspar, and melilite at 1100 °C.…”