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Tellurite And Fluorotellurite Glasses For Active And Passive

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5. Crystallisation studies; MDO 136<br />

the range of 1 to 10 Å (10 -10 to 10 -9 m) which corresponds to the wavelength of the X-ray<br />

part of the electromagnetic spectrum. When this X-ray radiation impinges on a material,<br />

two effects are observed: absorption and scattering [1]. Absorption results in excitation of<br />

inner orbital electrons of the atoms of the material which Auger electron spectroscopy<br />

(AES) and X-ray fluorescence (XRF) utilise for chemical analysis [1].<br />

When X-rays are scattered by a material their wavelength is either changed<br />

(incoherent scattering) or their wavelength remains unchanged (coherent scattering) [1].<br />

The coherent X-rays scattered from different electrons of the same atom lead to<br />

interference effects. These effects are more likely for X-rays coherently scattered by<br />

atoms of the same or adjacent planes [1]. This phenomena, known as X-ray diffraction, is<br />

analogous to the diffraction of light from an optical grating. The closely spaced lines of<br />

the grating are the two-dimensional equivalent of the atomic planes in a crystal. Once the<br />

diffraction pattern is obtained the atomic structure can be calculated [1].<br />

The scattering of X-rays was first treated by von Laue [2]. He considered a row of<br />

atoms periodically spaced, scattering a parallel set of rays, which are only observable if<br />

they are travelling in phase. This means the path difference between each of the scattered<br />

rays should be an integral multiple of the wavelength, λ (i.e. nλ, where n = an integer 1,<br />

2, 3 etc.).<br />

W.L. Bragg found that beams of diffracted X-rays can be treated in terms of<br />

‘reflections’ from the lattice planes of crystals [3]. Fig. (5.2) illustrates the diffraction of<br />

incident X-rays from parallel rows of atoms in a crystalline lattice, described below.

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