“…At higher temperatures (>1200 K), the mass transfer to and away from the surface is the slowest step and, as a result, the erosion is only slightly temperature dependent [21,28,31,32]. For lower temperatures (<900 K) the chemical reaction between oxygen and carbon is the rate limiting process [27,28,33,34]. The transition temperatures between the different ranges depent on various parameters such as specimen porosity, microscopic structure, specimen shape and size, partial and total pressure, and the presence of water vapour [26,28].…”