“…Many models have been proposed to incorporate the effect of various parameters on the rate of interface migration during ferrous phase transformations, as nicely summarized in a comprehensive review paper (Gouné et al, 2015). In such models, the phase transformation is modeled by reducing the actual interface to a mathematical surface characterized with multiple variables and parameters such as the interface thickness (Svoboda et al, 2011), trans-interface diffusivity (Gamsjäger & Rettenmayr, 2015), interface energy (Militzer et al, 2014) and crystallographic orientation relationship (OR) between two crystals in contact (Ecob & Ralph, 1981). Yet, all these models explicitly or implicitly assume that the local interface movement is the same for each interface and does not vary along a particular interface, except near triple lines and quadrupole points.…”