“…Crelling et al (1993) concluded that variations both in lithotype and maceral composition gave rise to large variations in nitrogen content, char morphology and reactivity, i.e., that although the nitrogen content decreased in the order: vitrinite N semifusinite N inertinite, the conversion of the coal and char nitrogen to NO showed the reverse order: fusinite N semifusinite N vitrinite. Other authors also concluded that there could be other factors related to the structure and properties of the coal, in addition to the combustion conditions, such as rank and the degree of surface oxidation (Shimizu et al, 1992;Gavin and Dorrington, 1993;Pels et al, 1993), maceral composition (Gonzáles de Andrés and Wang et al, 1994), mineral matter (Zhao et al, 2003), char reactivity, and surface area (Kilpinen et al, 2002;Shen et al, 2003;Zhao et al, 2003).…”