“…However, it can be assumed [12] that at each depth below the surface local equilibrium with respect to the local, lateral gross composition, the temperature, and the pressure is established, especially at the interfaces between the Fe-N-C solid-solution phases, i.e., the sublayer boundaries and the interface with the substrate. The phase constitution as a function of depth can be predicted using the concept of diffusion paths: [13][14][15][16] the evolution of the (laterally averaged) composition as a function of depth allows to plot these composition data in a phase diagram at the temperature (and pressure) concerned, which data together constitute the diffusion path. If local equilibrium at each point of the diffusion path and thus at each depth in the specimen separately prevails, the sequence of the phases developing within the compound layer and the diffusion path can be related with the corresponding phase diagram, [13][14][15] e.g., see Reference 12.…”