Civil Engineering Reference
In-Depth Information
the system X,Y,Z . The coefficients N j must be chosen for the boundary conditions to
be satisfied. In a first step, the displacement components a i and b i are predicted in the
system X ,Y ,Z for each wave. Let ψ be the angle between the axes X and X (see
Figure 10.7). The angle ψ is defined by
cos ψ = q x /q P
sin ψ
(10.103)
=
q y /q P
The displacement components in the system X ,Y ,Z and the system X ,Y ,Z are
related by
a 1 = a 1 cos ψ a 2 sin ψ
a 2 =
a 1 sin ψ
a 2 cos ψ
a 3 =
+
(10.104)
a 3
The same relations are satisfied by the components b i and b i . The stress components
can be evaluated in the system X ,Y ,Z from the displacement components a i ,b i and
the slowness vector components with Equations (10.21) - (10.27). In a last step, the con-
tribution a i and b i of each wave to the total velocity are evaluated with the relations
a 1 cos ϕ
a 3 sin ϕ
a 1 =
+
a 2
a 3 =−
a 2 =
(10.105)
a 1 sin ϕ
a 3 cos ϕ
+
The same relations hold for the b i and the b i . For each wave the total stress compo-
nents in the system X,Y,Z and in the system X ,Y ,Z are related by
σ zz =
σ x x sin 2 ϕ
2 σ x z sin ϕ cos ϕ
σ z z cos 2 ϕ,
+
(10.106)
σ zx =−
σ x x sin ϕ cos ϕ
σ z x ( cos 2 ϕ
sin 2 ϕ)
+
(10.107)
σ z z sin ϕ cos ϕ,
+
σ zy =− σ x z sin ϕ + σ x y cos ϕ
(10.108)
q y y)) applied on the frame at the free
surface of the layer creates a plane wave in air with a spatial dependence exp[
The unit stress field τ zz =
exp (
jω(q x x
+
j(ωq x x
+
ωq y y
k 0 z cos θ) ]wherecos θ is given by
(k 0 /ω) 2
q x q y
k 0
cos θ
(10.109)
The choice in the physical Riemann sheet corresponds to Im cos θ
0. The pressure
p e and the velocity component v z are related by
p e
v z Z 0 / cos θ
=−
(10.110)
where Z 0 is the characteristic impedance in the free air. If the predictions are restricted
to the case of a semi-infinite layer, there are no upward waves and only the contribu-
tions in the porous medium of the four other waves must be taken into account. Let
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