This short contribution is meant to point out a basic mechanism for the oxi
dation of different carbons at high temperatures. The rate of carbon oxidat
ion. i.e. CO-formation, is proportional to a steady state oxygen activity w
hich is established on the carbon surface by the interplay of oxygen transf
er reactions and carbon oxidation. This was proven in detail for the reacti
on of electrode graphite. active charcoal and natural graphite in CO2-CO mi
xtures, where by isotope exchange studies the rate of oxygen transfer could
be measured separately [1, 2] but is also valid for other oxidizing atmosp
heres.