Evaluation of the wave propagator

544 M. Romeo P t = ± 1 c L −1 p sLGs t, 25-a St = ±c L −1 1 √ sLGs t 25-b and Eq. 23 becomes ∂ x v + v − = − 1 c Q· 1 c Q· ∂ t v + v − 26 with Qt = L −1 1 √ sLGs t 27 and where the choice of the sign in 25 has been performed according to the meaning of v + and v − as forward and backward propagating disturbances. Explicit expressions for P t and Qt = Stc can be derived for the Maxwell model and the Maxwell–Kelvin model described in Section 2. With the help of a table of Laplace transforms Roberts and Kaufman, 1966, we have P t = δt exp−t2τ M + E t, 1 2τ M , Qt = δt exp−t2τ M + F t, 1 2τ M and P t = δt exp−t2τ 2 + E t, 1 2τ 2 + E t, 1 2 1 τ 1 + 1 τ K + E ·, 1 τ 2 · E ·, 1 2 1 τ 1 + 1 τ K t, Qt = δt exp−t2τ 2 + F t, 1 2τ 2 + F t, 1 2 1 τ 1 + 1 τ K + F ·, 1 τ 2 · F ·, 1 2 1 τ 1 + 1 τ K t respectively for the Maxwell model and the Maxwell–Kelvin model with t 0, where δt is the usual Dirac delta distribution and the functions E and F are given by Et, β = β I βt + I 1 βt exp−βt, F t, β = β I βt + I 1 βt exp−βt, where I and I 1 are modified Bessel functions.

4. Evaluation of the wave propagator

Equation 26 allows us to solve the problem of the one-dimensional transient propagation in a viscoelastic homogeneous medium in terms of the superposition of two independent modes v + and v − propagating in opposite directions. According to the present model, if a wave pulse is given at x = 0, the function v + 0, t can Wave splitting in linear viscoelasticity 545 be obtained by 20 and the evolution of the transient for x 0 can be determined by the equation ∂ x v + x, t = − 1 c Q· · ∂ · v + x, · t, 28 where ∂ · stands for derivative with respect to the argument involved in the convolution. A convenient form of the solution to Eq. 28 can be achieved in terms of a wave propagator P + x, t which is defined as v + x, t = P + x, · · v + 0, · t, 29 where v + x, t satisfies Eq. 28. A comprehensive treatment of wave propagators in the context of one- dimensional problems is given in Karlsson 1996 and applied to the more general case of inhomogeneous media. According to Eq. 29 the propagator P + x, t can be viewed as the solution to Eq. 28 corresponding to a δ-like pulse at x = 0, that is, under the boundary condition v + 0, t = δt. Substitution of 29 into 28 yields ∂ x P + x, · · v + 0, · t = − 1 c Q P + x, · · v + 0, · t − 1 c ∂ · Q· · P + x, · · v + 0, · t, where the condition 22 has been exploited. The use of Eq. 27 and the arbitrariness of v + 0, t yield the following equation for P + x, t ∂ x P + x, t = − 1 c L −1 s s LGs · · P + x, · t. 30 Equation 30 can be solved by means of the Laplace transform. Sine P + 0, t = δt, we have P + x, t = L −1 exp − x c s s LGs t. 31 In the case of the Maxwell model, Gs is given by 8 and an exact solution 31 is obtained in the form P + M x, t = exp−t2τ M δ t − x c + H t − x c x 2τ M c I 1 1 2τ M p t 2 − xc 2 p t 2 − xc 2 , 32 where H t is the Heaviside unit step function. Equation 32 corresponds to a superposition of a directly transmitted wave and a transient wave propagating with speed c and whose amplitude decays exponentially in time. In the case of a Maxwell–Kelvin model we are unable to work out the inverse transform in Eq. 31. However, a realistic approximation of the argument of the exponential in 31 allows us to bypass this difficulty. For the Maxwell–Kelvin model it results in s s LGs = s s s + 1 τ M s 1 + α τ K s s + 1 τ K s + 1 τ M . 33 546 M. Romeo Figure 1. Wave propagators for shear waves in a copper half-space for the Maxwell model P + M and the Maxwell–Kelvin model P + MK as functions of x for t = 100 s, τ M = 6 · 10 5 s, τ K = 2s, α = 130. As frequently occurs Caviglia and Morro, 1990, we have α ≪ 1 and τ M ≫ τ K . Then an approximated expression of the second root on the right-hand side of 33 holds for any s 0, such that s s LGs ≃ s s s + 1 τ M + α 2τ K s s + 1 τ K . 34 In view of 34 we can work out the inverse transform in 31 to obtain P + MK x, t ≃ exp − x c α 2τ K P + M x, t + Ax, · ∗ P + M x, · t , 35 where P + M is given by 32 and Ax, t = exp−tτ K 1 τ K √ t r αx 2c I 1 2 τ K s αx τ K t . In order to make a comparison between the two viscoelastic models, the solutions 32 and 35 are shown in figure 1 for a fixed time in correspondence to shear waves. A relevant difference between the two models appears at large distances from the boundary x = 0. Wave splitting in linear viscoelasticity 547

5. Exact solutions for the reflectivity