It is possible that 111 plane for austenite γ-Fe was overlapped by Cr 110 and CrN 200 peaks when increasing total thickness and reducing bilayer period i.e. with a greater number of interfaces.
Es probable que el plano 111 de la austenita γ-Fe sea traslapado por el Cr 110 y el CrN 200 a medida que se incrementa el espesor y se reduce el período, es decir, con el mayor número de interfaces.