Pulverized coals have been tested under the conditions of industrial flames, with high heating rate and high temperatures. Coal particles were injected (5 g/h) into a flat, air-propane flame at 1400°C. The chars were collected after different pyrolysis times. The thermal history of the particles, as monitored by two color pyrometry, shows that particles undergo very large heating rates (6 × 10 6 K/s) and reach a peak temperature of 1100°C. For eight coals (volatile matter 1–57% d.a.f.), the devolatilized fraction of coal has been measured, as well as those of carbon, hydrogen and nitrogen. In every case, the devolatilized fraction of coal was greater than the predicted A.S.T.M. value, but proportional to it. The devolatilized fraction of hydrogen seems to be a more sensitive parameter than the coal's weight loss. During pyrolysis, the evolution of the texture of the grains has been studied by measurement of their microporous surface area, which undergoes a large increase, depending on coal rank. The composition of the volatiles, as deduced from the ultimate and proximate analysis of chars, showed high volatile bituminous coals to essentially produce tars with an aromatic structure. In that case, the surface area passed through a maximum at the beginning of devolatilization. The subsequent decrease could be due to recondensation of heavy molecular weight volatile matter at the char's surface. Low and medium volatile bituminous coals produced light hydrocarbons on devolatilization and the char's surface area continued increasing slowly during the whole of devolatilization, according to the slow increase of the fraction of hydrogen devolatilized. The char's reactivity with oxygen was followed by measurements of Active Surface Area (A.S.A.). It was shown that the A.S.A. continuously decreases during devolatilization. This may be due to the departure of prompt volatiles made of aliphatic groups, which are potential active sites for oxygen. Five models of devolatilization in the literature were tested and compared to the experimental results, assuming first-order reactions with respect to the remaining volatile matter. Badzioch's model correctly fitted the experimental results and values of the rate constant obtained by computer trial and error adjustment were higher for lower ranks of the four bituminous coals. Anthony's model also fits the measurements, provided an adjustment of the preexponential factor and activation energy ( k 0, E 0), for which it is shown that an infinite number of such pairs is suitable. If the model is run isothermally at the flame's peak temperature, it also correctly fits the experimental results.
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