“…Probably owing to its pores' larger specific surface area and diameter, the hydrated lime showed larger SO 2 removal fractions than did the dolomitic limestone used by Pisani and Moraes [25] under all the conditions studied, a behavior that was congruent with the results of Al-Shawanekeh et al [7,19], obtained in thermobalances. The gas removal fraction increased with a decreasing slope as a function of temperature.…”