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2. What is x-ray crystallography
and why is it important?
The shape of crystals in one form or
another has been known since early times. Observation over a
number of centuries had also confirmed the constancy of their
shape. An understanding of their underlying structure, however,
had to wait until the late eighteenth century when John Dalton
put forward the idea that atoms of different elements might
combine together in various proportions to make compound atoms
or molecules as we call them today. The various optical
properties of crystals were also of interest and many
observations were made with visible light about the ways in
which rays of light of various colours could be absorbed,
reflected and refracted in their passage through crystals.
The discovery by Wilhelm Konrad
von Roentgen in 1895 of x-rays, which unlike light could pass through
opaque objects, allowed the studies to be taken further and by 1912
Max von Leue and PP Ewald had deduced that x-rays must be capable of
being diffracted, like light. Shortly after the crystallographers Friedrich
and Knipping passed a beam of x-rays through a crystal of copper sulphate
on to a photographic plate. When the plate was developed, in addition
to the dark spot produced by the undeflected beam, they also found an
irregular pattern of black spots confirming the theory and encouraging
the idea that the pattern of diffraction (the scattering of the spots)
said something measurable about the molecular structure of the crystal.
Concerted work by a number of scientists including Sir William Bragg
and JD Bernal led both to the deduction of the molecular structure of
a number of crystals and deduction of equations to interpret their use.
In March 1929 the Royal Institution established three committees on
x-ray crystallography.
When
the technique of x-ray diffraction was used on protein molecules in
the 1930s, the growing possibility of the technique was recognised.
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