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248 The Elastic Solid






         5.10 Reflection of Plane Elastic Waves.

            In Fig. 5.5, the plane #2 = 0 is the free boundary of an elastic medium, occupying the lower
         half-space X2 ^0. We wish to study how an incident plane wave is reflected by the boundary.
         Consider an incident transverse wave of wavelength /j, polarized in the plane of incidence with
         an incident angle a j, (see Fig. 5.5). Since*2 = 0 is a free boundary, the surface traction on the
         plane is zero at all times. Thus, the boundary will generate reflection waves in such a way that
         when they are superposed on the incident wave, the stress vector on the boundary vanishes at
         all times.
            Let us superpose on the incident transverse wave two reflection waves (see Fig. 5.5), one
         transverse, the other longitudinal, both oscillating in the plane of incidence. The reason for
         superposing not only a reflected transverse wave but also a longitudinal one is that if only one
         is superposed, the stress-free condition on the boundary in general cannot be met, as will
         become obvious in the following derivation.















                                              Fig. 5.5


            Let «,• denote the displacement components of the superposition of the three waves, then
         from the results of Example 5.9.4, we have







         where
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