“…For the graded layers with linear strain, our method allows us to compute parameters N, eo and A e, in contrast to the method of Fresnel's layers (Kolpakov & Punegov, 1988), if the rocking curve does not have clearly visible oscillations (Hill, Tanner, Halliwell & Lyons, 1985;Kolpakov & Punegov, 1985;Macrander, 1988;Macrander, Minami & Berreman, 1986) but only some broadening of the peak caused by diffraction from the epitaxic layer. This fact is illustrated in Fig.…”