“…It is well known that upon heating in an inert atmosphere, the oxygen surface complexes of carbonaceous materials decompose, releasing CO 2 and CO [32]. CO 2 results from the decomposition of carboxyls, lactones and anhydrides, while CO comes from anhydrides, phenols, carbonyls, quinones and pyrones [20,32,33]. Figure 2 shows the profiles of evolved CO 2 and CO for samples GKOS and GKOSA50, in the course of heating at 15 ºC min -1 in 50 cm 3 min -1 of Ar.…”