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398    MEMS-IDT MICROSENSORS

   is  possible  to create  a wireless  MEMS-IDT  microsensor  in a  manner similar to that was
   shown as possible to make a wireless IDT microsensor  in Chapter  13 (Subramanian et  al.
   1997).


   14.2  PRINCIPLES     OF A  MEMS-IDT      ACCELEROMETER

   The  Rayleigh  wave  is  a  surface  wave  in  which  the  wave  energy  is  almost  completely
   confined  within a distance  of one wavelength above the substrate (Ballantine et al.  1997).
  There  are  basically  two  types  of  boundary  conditions  applicable  with the  surface  of  the
  piezoelectric  being mechanically free.  In one form, the surface has a thin conductive layer.
  This  layer  does  not  alter  the  mechanical  boundary  conditions  but  causes  the  surface  to
  be  equipotential  and  the  propagating  potential  to  be  zero  at  the  surface of  the  substrate.
  The  other  case is the  one  in which the surface is electrically  free  and  the potential above
  the  surface  follows  Laplace's  equation.  The  potential  vanishes  as the distance above  the
                          1
  substrate  approaches  infinity .
     In  a  MEMS-IDT  accelerometer,  a  conductive  seismic  mass  is  placed  close  to  the
  substrate  (at  a  distance  of  less  than  one  acoustic  wavelength). This  serves  to  alter  the
  electrical  boundary condition  discussed  earlier.  The  seismic  mass  can  be fabricated  from
  polysilicon  and incorporates reflectors  and flexible beams (Figure  14.1).
     The  MEMS  device  functions  as  follows:  An  incoming  electromagnetic  wave  at  the
  IDT creates  a radio frequency  electrical field between the transducer fingers. Owing to the
  piezoelectric  effect,  mechanical  deformations  follow  the  signal  and  propagate  along the
  surface  of  the  piezoelectric  substrate. The  array of reflectors  sends  back this wave to  the
  IDT.  The  phase  of  the  reflected  wave  is  dependent  on  the  position  of  the  reflectors.  If
  the  position  of  the  reflectors is  altered,  the  phase  of  the  reflected wave also  changes.  As
  can be  seen  from  the  figure,  the reflectors are part of the  seismic  mass.  In response  to an
  acceleration,  the  beam  flexes, causing the  reflectors to  move. This  can  be  measured  as a
  phase  shift  of  the reflected wave. By calibrating the  phase shift  measured with  respect  to






















               Figure  14.1  Basic arrangement of a MEMS-IDT accelerometer

  1
    Readers are referred to Chapters 9 and  10 for a basic introduction to surface acoustic waves and SAW devices.
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