The removal efficiency of SO
2 by the soils were studied and influence of relative humidity on the removal efficiency was also investigated. As typical soil samples, i. e. a Kanto-loam soil, soil mainly containing montmorillonite and soil containing volcanic ash were chosen. The removal efficiency of SO
2 for 50-270 mesh soils was measured at different relative humiditys. Four samples of them, except sta ndard sand, gave the maximum values at 50% relative humidity. The Kanto-loam (50-270 mesh) was divided in to three types of particle size (50-100, 150-170, 250-270 mesh). The removal efficiency of SO2 for each of the three samples was relatively higher than that for 50-270 mesh Kanto-loam, while the minimum value at 50% relative humidity was observed. The removal efficiency of SO
2 for the five samples increased with the increase in the specific surface areas at 50% relative humidity. For bentonite, Na-montmorillonite and kaolin, the removal efficiencies of SO
2 increased with the increase in relative humidity. Every clay mineral showed over 60% of removal efficiency of SO
2 at 95% relative humidity.
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