“…Nature materials may have complicated layers, and in order to simplify the analysis, a model of three‐layered half‐space with h 1 : h 2 : r 0 = 3 : 5 : 5 is considered. The parameters of the media refer References , and four cases are chosen for comparison: case 1: κ 1 : κ 2 : κ 3 = κ 0 : κ 0 : 2 κ 0 , μ 1 : μ 2 : μ 3 = 0.3 : 0.3 : 0.25, and n j = 0.4; case 2: κ 1 : κ 2 : κ 3 = κ 0 : 3 κ 0 : 3 κ 0 , μ 1 : μ 2 : μ 3 = 0.3 : 0.3 : 0.25, and n j = 0.4; case 3: κ 1 : κ 2 : κ 3 = κ 0 : 3 κ 0 : 3 κ 0 , μ 1 : μ 2 : μ 3 = 0.3 : 0.25 : 0.25, and n j = 0.4; case 4: κ 1 : κ 2 : κ 3 = κ 0 : 3 κ 0 : 3 κ 0 , μ 1 : μ 2 : μ 3 = 0.3 : 0.25 : 0.25, and n j = 0.5, in which κ 0 = 1.1 × 10 − 6 m 2 /s and j = 1, 2, 3. Other parameters of the three‐layered porous thermoelastic half‐space satisfy the following relationship: G 1 : G 2 : G 3 = G 0 : 1.5 G 0 : 2 G 0 , , α j = 10 − 5 / o C , α wj = 2 × 10 − 4 / o C , C j = 600J/kg o C , ρ j = 2200 kg /m 3 , Q 0 = 100 k W, and r 0 = 5m, where G 0 = 6 × 10 4 kPa, and the other parameters and results are displayed in Figure .…”