“…Therefore, a three-dimensional MPBM, the corresponding three parameters, x, y, z, as shown in Figure 4, can be formed to simulate the morphological evolution of potash alum crystals. This complex inorganic hydrate compound, potash alum, was specially chosen in several PB studies [94][95][96]111], which displays no extensive attrition and without observed significant particle/particle agglomeration. By solving the morphological PB equation for a time interval of t, the growth of individual faces, {111}, {100} and{110}, can be obtained, and, hence, used to calculate the new locations of the corresponding crystal faces, with respect to their previous locations.…”