Relatively large spheres of non-porous graphite (diam. 2–12 mm) have been burned in electrically heated beds of sand, fluidized by air. The rate of reaction of the carbon was derived from measurements of the concentrations of CO and CO 2 in the gases leaving the bed. The carbon particle's temperature was monitored continuously during its combustion using a very fine thermocouple inserted in the graphite sphere. The temperature of the burning particle rose whilst its diameter shrank. The observations can be interpreted in terms of CO being the only product of oxidation for graphite particles burning between 1000 and 1400 K in such a fluidized bed. The oxidation of CO is inhibited by the proximity of sand, which provides a large surface area for radicals (e.g. OH and HO 2) to recombine. Nevertheless, CO does burn to CO 2 close to the carbon at the higher temperatures studied (1400 K), but at ∼ 1100 K it mainly diffuses away before burning in say a rising air bubble. In this case less heat is fed back to the burning carbon. The use of tiny sand particles can give small air velocities over the carbon particle, so that convection of CO away from the carbon is reduced and the full enthalpy of combustion of carbon to CO 2 is donated to the carbon. It seems likely that, just as radicals are important in oxidising CO to CO 2, they are also involved in burning solid carbon to CO.
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