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Tellurite And Fluorotellurite Glasses For Active And Passive

Tellurite And Fluorotellurite Glasses For Active And Passive

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2. Literature review; MDO 15<br />

2.2.2.3. Zachariasen’s random network theory<br />

Zachariasen did not agree with the crystallite theory proposed by Randall et al. [5] as<br />

assumptions in the theory 2 led to discrepancies between observed and calculated densities<br />

of silica glass. Diffraction patterns and thermal properties observed were also not in<br />

accordance [6].<br />

Over large temperature ranges the mechanical properties of glasses are comparable<br />

(superior in some cases) to those of crystalline materials. Because of this Zachariasen<br />

proposed that the forces in glasses are essentially the same as those in a crystal, with<br />

atoms oscillating about definite equilibrium positions forming an extended three-<br />

dimensional network [6]. X-ray diffraction data had shown this network was not periodic<br />

and symmetrical, but not entirely random, as inter-nuclear distances do not fall below a<br />

minimum value. Therefore, all inter-nuclear distances are not equally probable which<br />

results in the diffraction patterns seen [6].<br />

It can be said that the glass network is characterized by an infinitely large unit cell<br />

containing an infinite number of atoms. Due to a lack of periodicity, no two atoms are<br />

structurally equivalent [6]. The isotropic nature of glass is a direct consequence of this<br />

lack of symmetry, as the atomic arrangement is statistically equivalent in all dimensions.<br />

As all atoms are not structurally equivalent, the energy needed to detach an atom from the<br />

network will be different for each atom. This means with increasing temperature an<br />

increasing number of detached atoms would be expected, so the network breaks down<br />

continuously, as opposed to a crystalline material where the breakdown in an abrupt<br />

2 These assumptions were: (i) the average linear dimensions of the cristobalite crystallites were of the order<br />

of 15Å, and (ii) lattice constants were 6.6% larger than in cristobalite crystals.

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