um
7 CAMERA TESTING BY THE USE OF SPECKLE PATTERNS
L H Tanner (Brighton Polytechnic) (11)
Just as the possibilities of the use of laser speckle
(Section 3) followed on the development of holographic
testing (Section 2), so one of the authors of the
work in the previous section has developed a visual
testing method based on the observation of speckle
generated at the surface of the film and observed in
the plane of the diaphragm (Figure 19).
LU ALL EU
I,
À à b:
P Ly
erem ~ 0.5m ss ed
7
Figure 19 Experimental apparatuse
The principle is that the focusing of the laser beam
on the film is judged by the absence of bodily
movement of the observed pattern when lens L, is
translated laterally. Under reasonable conditions
the focusing may be verified to about /20 of the
Rayleigh limit, and enables the aberration coefficients
to be derived from observations at various field angles
and positions within the camera aperture stop.
Separating out the aberrations provides information on
the focus—error term, and this is shown in Figure 20,
7
| 101
SF
se
5+ >,
e ó rm
“1.0 -0ls 0 0.5 1.0
— 5 ]-—t 1
o IS o
o
° -5+
e -104-
x ® Sagittal
e
o Astigmatism
asl
Focal position variation versus 6 for
x' = O, for the sagittal direction,
showing field curvature and film
position errore
Figure 20
94
and compared with the predicted parabolic form. This
result indicates the great power of the method to
relate the optical properties of the camera system and
its mechanical adjustments to the real condition of
focusing on the actual film.
Reference
11 Tanner L H, "Camera testing by the use of speckle
patterns" Applied Optics, 1974, 13, No 9,
pp 2026-2034.
8 FINE TOPOGRAPHIC STRUCTURE IN POLISHED GLASS
SURFACES
K Lindsey (Reference 12,13)
Surfaces for use as reflectors in the X-ray region must
have much smoother microstructure than is necessary
for visible light. The same applies to the reflecting
facets of diffraction gratings for X-ray use. The wave-
length of the X radiation is much shorter, and
undulations in the surface of very small height(&1 nm)
and small lateral extent (5-10 am) cause noticeable
variations in the convergence of the beam to its
intended focus, and show up as displaced subsidiary
images. Moreover, these surfaces are used near the
critical angle and variations of slope show up as the
reflectivity varies rapidly near the critical angle.
A method of mapping the variation of slope over
reflecting surfaces uses the latter principle. Well
collimated radiation of wavelength 0.15 nm is carefully
adjusted to be incident on the surface at the critical
angle, and the reflected beam is received on & photo-
graphic plate placed close to the reflecting surface.
Typical records are shown in Figure 21, and the
yariations in intensity may be related to the areas on
the reflector responsible.
Figure 21 Topographic maps of two surfaces produced
by the critical-angle X-ray reflection
method. (The horizontal lines are
instrumental artefacts).
Alternatively, the variations in focus mentioned first
will provide a means of testing the perfection of the
surface, as was suggested by Ehrenberg (Reference 13).
Examples of these secondary focal concentrations are
shown in Figure 22, where they are superimposed on a
slightly out of focus primary image. This method can
be more sensitive