Abstract
The conventional way of studying material reactivity—progression of the global reaction kinetics, preservation of their properties as a function of time and environmental condition does not fully give the complexity of the processes involved. Consequently conventional models developed often do no exactly represent the reaction processes in a medium. This article seeks to introduce nanoscience to the development of limestone decarbonization process chemistry model. The inclusion of atomistic computation into the conventional mathematical model could open a new perspective in the determination of parameters that influence global rate of CaCO3 decarbonization reaction. This is the focus of this presentation. Comparison of experimental results with computed values show appreciable agreement with correlation coefficient ranging from 0.77 to 1.