Abstract

The deposition rate of α-Al 2 O 3 was measured at 0.1 and 1 bar and variable partial pressures of AlCl 3 , CO 2 , H 2 and HC by means of thermobalance. HCl additions proved to have a retarding effect on the deposition. From the temperature and the total pressure dependence of the deposition rate it was concluded that the process was determined by chemical reactions rather than gas diffusion. The rate increased with AlCl 3 , CO 2 and H 2 partial pressures, decreased with rising HCl contents, and was independent of the CO pressure. The partial pressure dependences did not lead to simple reaction orders indicating the overlap of at least two parallel reactions. Two rate equations were deduced front the measurements to describe two parallel reaction paths, one equation being based on an assumed reaction mechanism involving the homogeneous watergas shift reaction and the subsequent heterogeneous formation of AlOCl(ad) as rate-determining intermediate. The second equation is purely empirical. Results of the numerical simulation based on these equations and heat and mass transport calculations are compared with the experimental observation.

Full Text
Published version (Free)

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call