“…Consequently, it becomes possible to calculate a very wide range of physical properties, such as the structural, dynamical, thermodynamic, and transport properties of solids, liquids and vapors for a given interaction model. The application of atomistic simulation in minerals has achieved great success, in the fields of predicting the elastic constants of MgSiO 3 -perovskite [5], calculating the heat capacity and entropy of the major phase in the mantle [6], predicting the high pressure phase transition in simple oxides such as Al 2 O 3 at high pressure [7], and analyzing the diffusion mechanisms in a variety of oxides and silicates [8,9]. The important progresses in this field have been achieved with the development of first-principle methods [10][11][12][13].…”