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Sometimes at night one sees a diffuse disk of light around the moon if
it happens to be shining through a thin layer of cloud. This disk
consists of light diffracted by the water or ice particles in the
cloud. The diameter of the disk contains information about the size
of the cloud particles doing the diffraction. In particular, if the
particles have diameter
and the light has wavelength
,
then the diffraction half-angle shown in figure 18.2 is
approximately
This equation comes from the problem of passage of light through a
hole or slit of diameter or width
. This problem was treated in
the section on waves, and the above formula was concluded to hold in
that case. One can think of the diffraction of light by a particle to
be the linear superposition of a plane wave minus the diffraction of
light by a hole in a mask, as illustrated in figure 18.2.
The angular spread of the diffracted light is the same in both cases.
The interesting point about equation (18.1) is that the opening angle of the diffraction cone is inversely proportional to the diameter of the diffracting particles. Thus, for a given wavelength, smaller particles cause diffraction through a wider angle.
Note that when the wavelength exceeds the diameter of the particle by
a significant amount, equation (18.1) fails, since
scattering through an angle greater than
doesn't make physical
sense. In this case the diffracted photons tend to be isotropic,
i. e., they are scattered with equal probability into any direction.
If one wishes to measure the size of an object by observing the
diffraction of a wave around the object, the lesson is clear; the
wavelength of the wave must be less than or equal to the dimensions of
the object -- otherwise the scattering of the wave by the object is
largely isotropic and equation (18.1) yields no
information. Since wavelength is inversely related to momentum by the
de Broglie relationship, this condition implies that the momentum must
satisfy
| (19.2) |
David Raymond 2006-04-07