“…The presence of carbon within the scale during the oxidation of transition metal carbides very often leads to the formation and stabilisation of oxides that would normally be unstable in this range of temperatures [21]. A similar situation has been observed in the present study, as the anatase phase, contained in the oxide scale, was observed up to 800 • C. According to recent data by Zhang et al [22], the polymorphic transition of the anatase to rutile phases begins at 500 • C and reaches about 95% at 700 • C. Another key observation is that the anatase phase, in contact with carbon, is more chemically stable; this is confirmed by noting that the carbothermic reduction of anatase starts at higher temperatures when compared with those for the rutile phase [23]. From the obtained experimental data, a convincing argument would be that, during the oxidation of TiC 1−x , the anatase-rutile phase transition is directly connected with the 'ridge' temperature, as the intensive polymorphic transformation is concurrent with deeper carbon burn-off in the scale.…”