diffraction, Fresnel class  To find the effect of interference of secondary  wavelets arising  out  of  an  wavefront of any shape falling on the screen kept at a finite distance, Fresnel observed that  the amplitude A, of the secondary wavelets arising out of a wavefront  should not be the same in all direction. It should be maximum in  the  forward  direction  and  zero  in  the backward direction.  For  the quantitative  variation  of amplitude with direction, he introduced a factor equal to (1 + cos q ), called the obliquity   factor,  where q  is  the  angle  with  the  forward direction.  The  amplitude  of  the  secondary  wavelets must be proportional to the area from where they originate (ds), and it should be   inversely  proportional  to  the distance  d,  between  the wavefront and the point on the screen.

A = constt. [ds/d]( 1 + cos q )

Now  imagine a plane wavefront for simplicity and consider a point  P  at a distance b in front of the wavefront (see fig.d7). Imagine  spheres  with radii, b + l /2, b + 2(l /2) , b + 3( l /2) ..... with P as center. These will cut circles on the wavefront. The central circle  is  called  the  first half period zone. Subsequent half period zones  are  annular areas between the circles. It can be easily  shown  that all the half period zones have the same area. The  significance  of these zones is that the secondary wavelets arising out of a particular zone are all of the same phase, while the adjoining  ones  are opposite in phase. The amplitude due to the hole wavefront is the sum of the series,

A = A1 - A2 + A3 - ............ + (-1)m-1 Am (1)

The successive amplitudes decrease gradually because of obliquity factor and distance. We may write

A2 = (A1 + A3 )/2; A4 =(A3 + A5)/2 and so on

With this approximation eq. (1) reduces to

A = A1 /2+ Am/2 for m odd,

and A = A1 /2- Am/2 for m even.

For m very large Am will be very small, and

A » A1/2

That is the amplitude due to the whole wavefront is only half the amplitude produced by the first half period zone.

The  diffraction  by  a  circular  aperture or by a circular obstacle  can  easily  be explained by the concept of half period zones.  Consider  a  circular aperture of  radius r in front of a screen. When the slit is illuminated concentric circular fringes are produced. If we gradually reduce the distance between the slit and screen,  the fringe  pattern will  shrink  and the center of the pattern  will  alternately  become bright and dark. This happens because  as  the  distance  is  reduced the number of half period zones  also  reduce. Since the alternate terms of the expression (1) are  of opposite sign the center will be alternately of high and  low  intensity. Ultimately only one half period zone remains, when  a bright spot is produced at the center. It is easy to see  that  for  circular obstacle the center of the fringe pattern will always be bright.

Fresnel  diffraction  with  straight  edge  and  cylindrical wavefront  :  The cylindrical wavefront generated by a parallel beam  and  rectangular slit, can also be divided into half period zones  as  done  in  plane wavefront. The half period zones will have  the  shape of strips. In this case however the areas of the half  period zones  are  not equal. The area of half period zones  decrease rapidly as we go from lower to higher half period zones.  If  we divide the strips further into equal parts, and construct  the  amplitude  diagram,  by placing the amplitudes of successive  strips,  as  shown  in  the  fig.d8,  the result is a spiral.  This  is because the successive strips have decreasing amplitude  and  the  phase also changes gradually. If the strips are made of infinitesimal width we get the smooth curve (fig.d9), which is called the Cornu's Spiral. Z and Z' are the eyes of the spiral.  A vector joining Z and Z' gives the resultant amplitude of the whole wavefront.

The  application  of  Cornu's  spiral can be demonstrated in case of diffraction due to straight edge as shown in fig.d10. We start  with  the point P, which is at the edge of the geometrical shadow.  At  this  point  the  amplitude is given by OZ (Fig.10), which is half of ZZ'. Therefore at P the intensity is one fourth of  the unobstructed wavefront. As we move upwards, the tail of the amplitude vector moves to the left along the spiral while its head  remains  fixed  at  the  eye  Z. The tail will go through maxima and minima alternately, till we are close to Z', where the amplitude  becomes  almost  constant.  If  we move down into the region  of  geometrical  shadow, the tail of the amplitude vector moves  up  and length  of the amplitude vector decrease steadily approaching  zero. The corresponding intensity curve is shown in fig. d11.

 

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