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Tellurite And Fluorotellurite Glasses For Active And Passive

Tellurite And Fluorotellurite Glasses For Active And Passive

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7. Surface properties; MDO 311<br />

network. NaF is a stable compound, and fluorides of tellurium exist, but are not as stable<br />

as ZnF2 and NaF. TeF4 is a colorless, hygroscopic solid, which decomposes above 190°C,<br />

forming gaseous TeF6 (sublimes at -39°C), also hydrolysing completely after 1 day at<br />

room temperature [22]. A number of oxyfluorides of tellurium exist, but all are liquids at<br />

room temperature, and form from Te +6 , these include: Te2O2F8, Te2OF10, Te3O2F14, and<br />

Te6O5F26. However, the Te-F bond may be more stable in the solid state when contained<br />

within the glass network, but also may result in volatilisation of tellurium fluorides, as<br />

discussed in chapter 5. Asymmetry in the XPS peaks of tellurite and fluorotellurite<br />

glasses may be as a result of the high degree of asymmetry of the structural units in the<br />

glass. Unlike the [SiO4] unit which forms highly symmetric tetrahedra, the TeO2<br />

structural units are trigonal bipyramidal (tbp), [TeO4], and trigonal pyramidal (tp),<br />

[TeO3], in structure, with a lone pair of electrons from tellurium in the corner of the<br />

polyhedra not occupied by an oxygen atom [23]. This lone pair of electrons will<br />

inevitably affect the distribution of electrons (and as a consequence the bonding) of any<br />

atoms in close proximity, such as fluorine which is highly electronegative. The<br />

asymmetry could also be due to fluorine associated with ZnF2, and Zn(OH)F derived<br />

structural units in the bulk glass. This impurity (Zn(OH)F) would also shift the F1s peak<br />

in the glass away from the value for ZnF2.<br />

The O1s peak for this glass was also asymmetric, as shown by fig. (7.13), which<br />

shows the O1s peak deconvoluted into three main components, at 531.0 eV (81.2 % →<br />

BOs and NBOs), 532.1 eV (14.9 % → OH), and 535.7 eV (3.9 %). The peak at around<br />

535.7 eV could be due to C-O and / or C=O groups from hydrocarbons used in the<br />

vacuum system of the XPS; however this peak was not seen in the XPS spectra of the

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