A study was performed to clarify the mechanisms of limestone dissolution in sulfuric and sulfurous acids, which is important in the wet method of flue gas desulfurization. The mass-transfer characteristics of a benzoic acid plate of fixed area were first tested in a dissolution vessel, and then the dissolution rates of limestone plates in sulfuric acid, sulfurous acid, and gypsum-saturated sulfuric acid were measured and correlated with various factors such as agitation speed in the vessel. The results obtained for sulfuric acid were as follows: the dissolution rate of limestone is controlled by the diffusion in the film formed on the solid surface, of which the diffused component is dissolved limestone in region I (
CH2SO4<2×10
-2 mol·m
-3), sulfuric acid in region II (2×10
-2<
CH2SO4 <5 mol·m
-3), and dissolved gypsum from the surface of deposited gypsum on the limestone surface in region III (5<
CH2SO4 <100 mol·m
-3). In the case of sulfurous acid, no deposit on the limestone surface that would affect the dissolution rate was observed, and the rate was found to be controlled by the diffusion of sulfurous acid. Finally, the dissolution rate in sulfuric acid saturated with gypsum was found to be controlled by the diffusion of sulfuric acid in region I and region II.
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