Abstract
Iron oxide (Fe2O3) is catalytic to the sorption of SO2 by CaO in a chemical environment similar to that in fluidized-bed combustion of coal. Four percent by weight of Fe2O3 physically mixed with CaO approximately doubles the sorption (sulfation) rate. The kinetic mechanisms of the catalytic reaction are discussed based on the view that SO3 formation is the rate-limiting step. Coal ash also catalyzes the sulfation reaction, and Fe2O3 appears to be the active constituent in such catalytic effects. Other iron-containing compounds existent in coal and fluidized-bed combustion systems are oxidized rapidly in the combustion gases to form Fe2O3 and in turn catalyze the sulfation reaction.
| Original language | English |
|---|---|
| Pages (from-to) | 915-918 |
| Number of pages | 4 |
| Journal | Environmental Science and Technology |
| Volume | 12 |
| Issue number | 8 |
| DOIs | |
| State | Published - 1978 |
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