Physics for Geologists, Second edition
Physics for Geologists, Second edition
Physics for Geologists, Second edition
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68 Electromagnetic radiation<br />
Source<br />
Figure 6.1 X-ray diffraction. The lower path is longer than the upper by<br />
2d sin 8.<br />
Figure 6.2 The Debye-Scherrer powder camera. The powder embedded in<br />
a non-crystalline medium is oriented at random to the X-ray path.<br />
(Courtesy Philips Nederland B.V.)<br />
X-ray diffraction analysis is based on the assumption that no two crystals<br />
of different composition have identical atomic spacing, and that mea-<br />
surement through all possible values of 0 will give a unique pattern of<br />
wavelengths. The Debye-Scherrer powder camera (Figure 6.2) can be used<br />
<strong>for</strong> simple solids that are fairly pure. The powder is embedded in a non-<br />
crystalline medium and it is assumed that random orientation of the particles<br />
will cover the full range of 0. Photographic film is in a circular holder. After<br />
exposure and development, the film has lines that are spaced according to 0,<br />
symmetrically arrayed around the point 0 = 0".<br />
X-ray fluorescence (XRF) or X-ray emission spectroscopy<br />
When metals and other massive samples with atomic numbers less than about<br />
20 are irradiated with high-energy X-rays, characteristic X-rays of lesser<br />
energy are excited. These wavelengths are analysed using XRD methods and<br />
a crystal grating of known spacing (an X-ray spectrometer, which is strictly<br />
Copyright 2002 by Richard E. Chapman