Tellurite And Fluorotellurite Glasses For Active And Passive
Tellurite And Fluorotellurite Glasses For Active And Passive Tellurite And Fluorotellurite Glasses For Active And Passive
2. Literature review; MDO 15 2.2.2.3. Zachariasen’s random network theory Zachariasen did not agree with the crystallite theory proposed by Randall et al. [5] as assumptions in the theory 2 led to discrepancies between observed and calculated densities of silica glass. Diffraction patterns and thermal properties observed were also not in accordance [6]. Over large temperature ranges the mechanical properties of glasses are comparable (superior in some cases) to those of crystalline materials. Because of this Zachariasen proposed that the forces in glasses are essentially the same as those in a crystal, with atoms oscillating about definite equilibrium positions forming an extended three- dimensional network [6]. X-ray diffraction data had shown this network was not periodic and symmetrical, but not entirely random, as inter-nuclear distances do not fall below a minimum value. Therefore, all inter-nuclear distances are not equally probable which results in the diffraction patterns seen [6]. It can be said that the glass network is characterized by an infinitely large unit cell containing an infinite number of atoms. Due to a lack of periodicity, no two atoms are structurally equivalent [6]. The isotropic nature of glass is a direct consequence of this lack of symmetry, as the atomic arrangement is statistically equivalent in all dimensions. As all atoms are not structurally equivalent, the energy needed to detach an atom from the network will be different for each atom. This means with increasing temperature an increasing number of detached atoms would be expected, so the network breaks down continuously, as opposed to a crystalline material where the breakdown in an abrupt 2 These assumptions were: (i) the average linear dimensions of the cristobalite crystallites were of the order of 15Å, and (ii) lattice constants were 6.6% larger than in cristobalite crystals.
2. Literature review; MDO 16 phenomenon [6]. As a result of this the supercooled liquid ↔ glass transition occurs over a range of temperatures. Zachariasen outlined a set of ‘rules’ for glass formation from compounds such as SiO2, B2O3, P2O5, GeO2, As2S3, and BeF2 [2]: • The compound will tend to form a glass if it easily forms polyhedral units as the smallest structural units. • Polyhedra should not share more than one corner. • Anions (O 2- , S 2- , F - ) should not link more than two central cations of the polyhedra. • The number of corners of the polyhedra must be less than six. • At least three corners of the polyhedra must link with other polyhedra. Cations in the glass were the catagorised by Zachariasen according to their role in the glass network [2]. • Network-formers: Si 4+ , B 3+ , P 5+ , Ge 4+ , As 3+ , Be 2+ , with CN of 3 or 4. • Network-modifiers: Na + , K + , Ca 2+ , Ba 2+ , with CN ≥ 6. • Intermediates, which may reinforce (CN = 4) or loosen the network further (CN 6 to 8). The Zachariasen random network theory can be used to explain many properties of conventional glasses, such as viscosity-temperature behaviour, and electrical
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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.