Following the previous report on the system of B
2O
3-GeO
2, we studied some properties of B
2O
3-Sb
2O
3 glasses, as a glass-forming system, with the interest of Sb
2O
3 glass. In the first the valence of Sb in those glasses was examined. Sb
2O
3 reacts with the oxygen in air to give Sb
2O
4 at the temperature range from 400° to 500°C, as shown in Fig. 1. The melting temperature of this glass-system is about 700°C, and this temperature is in the stable range of Sb
2O
4. By the chemical analysis of the glasses dissolved in HCl, it is concluded that the valency of Sb is almost trivalent (Table 1). It was difficult to prepare the glasses from Sb
2O
4, instead of Sb
2O
3, without a long melting process, and the resulting glasses contained a negligible amount of Sb
v (Table 2). Now it is assumed that the trivalent Sb ion is stable in B
2O
3-Sb
2O
3 glasses.
We then studied the expansion coefficient of these glasses. As the results are shown in Fig. 3, the curve of the thermal expansion has the minimum at 20mol% of Sb
2O
3. In Fig. 4 this curve is compared with those of B
2O
3-SiO
2 and B
2O
3-CeO
2 systems. The deviation of these experimental curves from the straight lines jointing both their ends, represents the structurl decrease in the thermal expansion. As the deviations in the above three systems are nearly same, we consider, the reason of the decrease in the B
2O
3-Sb
2O
3 system is the same as in other systems. Namely, 4-coordinated Sb, which may be formed by an additional coordination, interferes with the thermal vibrations of B
2O
3.
The temperature of the deformation, temperature of the transition, the density and the refractive index in this system are shown in Figs. 5, 7 and 8. It is noted that in the Sb
2O
3 rich range the increase of Sb
2O
3 lowers the transition temperature of glasses and on the contrary raises their liquidus temperature. Accordingly, it is assumed, the viscosity of Sb
2O
3 melt is low at the melting point and therefore the Sb
2O
3 glass may have a chain structure. The infrared spectra of the vitreous state and two crystalline states of Sb
2O
3 are shown in Fig. 9 and these spectra of B
2O
3-Sb
2O
3 glasses are shown in Fig. 10.
From the data of DTA and of the infrared spectra, it is considered that the structure of glassy Sb
2O
3 resembles the valentinite (see Fig. 2 b). In the DTA curves of Sb
2O
3 glasses containing B
2O
3 from 0 to 30mol%, shown in Fig. 11, the first endothermic peak A, the following exothermic peak B and the last endothermic peak E indicate the glass-transition, the crystalization and the melting, respectively.
The small endothermic peak D, which appears about the transition temperature of 570°C from the senarmontite to the valentinite, means this transition, because the same peak is found in the crystalline Sb
2O
3. The other small endothermic peak C seems to correspond to the reverse transition. It is confirmed by the change in the infrared spectra of Sb
2O
3 glass treated at 400°C (Fig. 12). Namely, the peak of the valentinite decrease with time and simultaneously the peak of the senarmontite increase progressively. We concluded that the glassy Sb
2O
3 devitrifies into the valentinite and then transforms into the senarmontite, the stable phase.
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