The kinetics of the thermal decomposition
of CaCO3 is
significantly influenced by atmospheric and self-generated CO2 due to the reversibility of the reaction. More detailed understanding
of this well-known phenomenon is desired for establishing an effective
Ca-looping in the CaO–CaCO3 system for energy storage
and CO2 capture. This article shows the universal kinetics
of the thermal decomposition of CaCO3 over different temperatures
and partial pressures of CO2 (p(CO2)) with the aid of an accommodation function (AF) composed
of p(CO2) and equilibrium pressure. An
analytical form of AF with exponents (a, b) was derived based on the kinetic considerations for the
consecutive elementary steps of the surface nucleation and interfacial
reaction. The overall kinetics of the thermal decomposition of CaCO3 were described universally over different temperatures and p(CO2) values by introducing the AF, in views
of the isoconversional and isothermal kinetic relationships using
the extended Friedman and experimental master plots, respectively.
The universal kinetic description was extended to the kinetic modeling
based on the physico-geometrical consecutive process comprising an
induction period (IP), a surface reaction (SR), and a phase boundary-controlled
reaction (PBR). The proposed kinetic approach enables parameterizing
the CO2 effect via the optimized (a, b) and tracking changes in the CO2 effect as
the physico-geometrical reaction step advanced from IP to PBR via
SR. Furthermore, using the established universal kinetic description
across different temperatures and p(CO2) values, a challenge was set to quantify the contributions of atmospheric
and self-generated CO2 on the kinetics.