1978
DOI: 10.1016/0040-6031(78)80074-4
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A thermogravimetric study of the effect of pore volume-pore size distribution on the sulfation of calcined limestone

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Cited by 46 publications
(21 citation statements)
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“…This might be because of the more limited extent of sintering to which the sorbent is exposed in the first case. Sintering results in an enlargement of the average particle pore size (Gullett and Bruce, 1987), and ultimately in an increase of the maximum degree of sulfation (Ulerich et al, 1978). This mechanism would also be consistent with the stronger sensitivity of the sulfation rate on particle size (related to stronger intraparticle diffusional resistances) observed under differential reaction conditions (Figure 10) compared to integral reaction conditions ( Figure 6).…”
Section: Apparent Kinetics Of Calcination and Sulfationsupporting
confidence: 71%
“…This might be because of the more limited extent of sintering to which the sorbent is exposed in the first case. Sintering results in an enlargement of the average particle pore size (Gullett and Bruce, 1987), and ultimately in an increase of the maximum degree of sulfation (Ulerich et al, 1978). This mechanism would also be consistent with the stronger sensitivity of the sulfation rate on particle size (related to stronger intraparticle diffusional resistances) observed under differential reaction conditions (Figure 10) compared to integral reaction conditions ( Figure 6).…”
Section: Apparent Kinetics Of Calcination and Sulfationsupporting
confidence: 71%
“…By integrating over the pore size distribution, the macroscopic properties necessary to obtain the pseudo-steady state concentration profile in the pellet were obtained. Figure 11 shows the predictions of the model as compared to experimental data taken by Ulerich et al [51]. During the initial reaction period, the model closely fits the experimental data; however, at later times, the model is seen to overestimate solid conversion, …”
Section: E Lime Sulfation Modelsmentioning
confidence: 70%
“…[51] found that calcination in an atmosphere containing COg produced calcines with pores of larger diameters than those of calcines prepared in nitrogen. The overall porosity and surface area of the calcines prepared in the presence of COg were less than those produced in nitrogen as a result of the shift from finer to wider mouthed pores in the former.…”
Section: Evaluation Of Model Parametersmentioning
confidence: 99%
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