2019
DOI: 10.1039/c9cp01327j
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Impact of atmospheric water vapor on the thermal decomposition of calcium hydroxide: a universal kinetic approach to a physico-geometrical consecutive reaction in solid–gas systems under different partial pressures of product gas

Abstract: Impact of atmospheric water vapor pressure on the kinetics of the thermal decomposition of Ca(OH)2 can be described universally.

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Cited by 40 publications
(116 citation statements)
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“…The temperature difference between T eo and T p initially decreased in the lower p(H 2 O) region and subsequently increased with p(H 2 O) values, which was compensated by accompanying changes in the peak height at T p . The observed changes in the mass-loss behavior with p(H 2 O) are different from our previous results for the thermal decomposition of Ca(OH) 2 , 47 for which the non-isothermal mass-loss curves shifted to higher temperatures accompanied by a systematic increase in the DTG peak height with increasing p(H 2 O). A normal effect with respect to chemical equilibrium for the reversible reaction can explain the observed changes in the reaction behavior that depend on the p(H 2 O) value: Figure S2 shows the equilibrium water vapor pressure, P eq (T), at different temperatures, which was calculated using a thermodynamic database (MALT2, Kagaku Gijutsu-Sha), 60,61 together with the (T, p(H 2 O)) region applied to the TG−DTG measurements to obtain the kinePc data.…”
Section: Resultscontrasting
confidence: 99%
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“…The temperature difference between T eo and T p initially decreased in the lower p(H 2 O) region and subsequently increased with p(H 2 O) values, which was compensated by accompanying changes in the peak height at T p . The observed changes in the mass-loss behavior with p(H 2 O) are different from our previous results for the thermal decomposition of Ca(OH) 2 , 47 for which the non-isothermal mass-loss curves shifted to higher temperatures accompanied by a systematic increase in the DTG peak height with increasing p(H 2 O). A normal effect with respect to chemical equilibrium for the reversible reaction can explain the observed changes in the reaction behavior that depend on the p(H 2 O) value: Figure S2 shows the equilibrium water vapor pressure, P eq (T), at different temperatures, which was calculated using a thermodynamic database (MALT2, Kagaku Gijutsu-Sha), 60,61 together with the (T, p(H 2 O)) region applied to the TG−DTG measurements to obtain the kinePc data.…”
Section: Resultscontrasting
confidence: 99%
“…The slope of the Arrhenius plot decreased with increasing p(H 2 O) values, which was accompanied by a compensatory decrease in the intercept. Variations in the conventional Arrhenius plot, when applied to the IP process, indicate trends that are completely opposite of those previously reported for the IP process during the thermal decomposition of Ca(OH) 2 at various p(H 2 O) values, 47 in spite of the similar retardation effect that p(H 2 O) has on the IP processes. Table S1 lists the apparent Arrhenius parameters determined for the IP processes of the thermal decomposition of Cu(OH) 2 at each p(H 2 O) value.…”
Section: Kinetics Of the Inductioncontrasting
confidence: 92%
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“…A recent work suggests that the equilibrium pressure, P 0 (kPa), of the gaseous product has a significant influence on dα/dt and the effective E a for decomposition reactions under temperature swing cycling [46]. Various forms of the pressure dependence term (also known as the accommodation function) have been derived and used in solid-gas systems [47,48]. The following h(P) function is derived by considering the contribution of the reverse reaction (e.g.…”
Section: Introductionmentioning
confidence: 99%