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328   SURFACE ACOUSTIC WAVES  IN SOLIDS















                Unstressed                      Rayleigh wave

         Figure  10.5  Particle displacement on  the  sagittal plane for the Rayleigh wave


     These  displacements  are  as  shown  in  Figure  10.5.  It  is  seen  that  as  u$  is  in  phase
  quadrature  with  MI, the  motion  of  each  particle  is  an  ellipse.  Because  of  the  change
  in  sign  in  u 1  at  a  depth  of  about  0.2  wavelengths,  the  ellipse  is  described  in  different
  directions  above  and  below  this point. At  the  surface, the  motion  is  retrograde,  whereas
  lower  down  it  is  prograde.

       u 1 = [A 1 exp(-£i.*3) + A 2exp(-b 2*3)]exp[jk:(.xi  -  x 1)]

       "3 =  (-                                               -  ct)]  (10.29)
                                          2
                                            2 1 / 2
                     2
                   2
  where b 1 = k(1 -  c /v )1/2  and b 2 = k(1 -  c /v )
    The  longitudinal and transverse  velocities,  v 1  and  v,,  are given by



  where  the Lames'  constants  G is given by E m /2(l  +  v)  and A is given by vE m/[(l  +  v)
  (1  — 2v)] with  v  being  Poisson's ratio  and  E m  being  Young's modulus.


  10.5.2  Shear  Horizontal  or Acoustic  Plate  Modes

  Acoustic plate modes (APW) or shear horizontal (SH) waves in a half-space  utilise single-
  crystal  quartz  substrates.  These  act  as  an  acoustic  waveguide  by  confining  the  acoustic
  energy  between  the  upper  and  lower  surfaces of  the  plate.  Such a  mechanism  is  used  to
  confine  waves  traveling  between  an  input  and  output  IDT.  SH  modes  may  be thought
  of  as  those  waves with a  superposition  of  SH  plane  waves, which  are  multiply reflected
  at  some  angle  between  the  upper  and  lower  surfaces  of  the  quartz  plate.  These  upper
  and  lower faces  impose  a transverse  resonance  condition, which results in each  SH  mode
  having  the  displacement  maxima  at  the  surfaces,  with  sinusoidal  variation  between  the
  surfaces.
    The  solution  is  simply  a plane  shear wave  propagating  parallel to the surface,  with its
  amplitude  independent  of  X3, within the  material.  The  phase  velocity  is  equal  to  v,.  The
  particle  displacement  associated  with  the  nth  order  SH  plate  mode  (propagating  in  the
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