“…This situation can be illustrated by the example of the simplest structure shown in Figure 2 . Using the concept of incident and reflected thermal waves and following the approach developed in [ 57 , 58 ], the alternative temperature components for three regions can be presented in the form of plane waves where x is the coordinate shown in Figure 2 , t is the time, l is the thickness of the second layer, q n were obtained from the heat equations for each layer and q n = (−1 + i ) ( ω /2 κ n ) 1/2 , ω is the cyclic frequency of thermal waves, κ n is the thermal diffusivity of the n th layer, a is the amplitude of the incident thermal wave, and r , b , c , τ are coefficients to be determined from boundary conditions.…”