Loss of Ag and Cl from Photochromic Glasses during Melting in Various Atmospheres

T. Maki, M. Tashiro
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引用次数: 4

Abstract

Batches of photochromic glasses (about 100g) containing various amounts of Ag and Cl (the nominal oxide compositions, SiO2 52.63, B2O3 20.09, Al2O3 6.89, Li2O 2.90, Na2O 1.80, BaO 8.18, PbO 4.81, ZrO2 2.10, Cu2O 0.014, Ag 0.44-5.80, Cl 0.15-2.18wt%) were melted at 1400° or 1450°C in the air or in the air saturated with AgCl, NaCl or BaCl2 vapor and amounts of Ag and Cl retained in the glasses after melting for various times were measured by X-ray fluorescence analysis.1) The glass batches containing large amounts of AgCl (more than about 3wt%), when melted in air, first separated into two liquid phases; a phase rich in AgCl and that rich in silicate. The latter remained as glass after cooling to room temperature. A great part of the AgCl added to the batches was thus lost almost instantaneously from the glass. After the phase separation, losses of the Ag and Cl from the glass melts continued probably by evaporation of chlorides such as AgCl and NaCl from the melts and also by oxidation of the chlorides in the melts by air: 4AgCl+O2→2Ag2O+2Cl2↑ In the latter mechanism only the Cl was considered to be lost because the Ag2O formed has high solubility in the glass melts. Loss rates of the Ag and Cl were both low but that of the Cl was a little higher than that of the Ag.2) The glass batch containing small amounts of AgCl (less than about 0.5wt%) showed no liquid phase separation but losses of the Ag and Cl occurred at slow rates as observed for the batches containing large amounts of AgCl.3) When the glasses were melted in the air saturated with AgCl vapor, the Ag contents increased rapidly, whereas the Cl contents were held constant. When the glasses were melted in the air saturated with NaCl vapor, the Ag contents decreased at slow rates, whereas the Cl contents were held constant. The loss rate of the Ag in the air saturated with NaCl vapor was a little higher than that in air. Effects of the air atmosphere saturated with BaCl2 vapor were intermediate between those in the air and the air saturated with the NaCl vapor.The above results were explained by supposing suppressing effects of the chloride vapors in the atmosphere on evaporation of the chlorides from the molten glasses and oxidation of the chloride vapors by air.4) Mechanical stirring of the molten glass did not give remarkable effects in accelerating evaporation of the chlorides from the molten glasses.
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光致变色玻璃在不同大气中熔化过程中银和氯的损失
在1400°或1450°C的空气中或在饱和AgCl的空气中熔化含有不同量的Ag和Cl(标称氧化物成分:SiO2 52.63, B2O3 20.09, Al2O3 6.89, Li2O 2.90, Na2O 1.80, BaO 8.18, PbO 4.81, ZrO2 2.10, Cu2O 0.014, Ag 0.44-5.80, Cl 0.15-2.18wt%)的成批光致变色玻璃(约100g)。用x射线荧光分析测定不同时间熔融后玻璃中保留的NaCl或BaCl2蒸气以及Ag和Cl的量。1)含有大量AgCl(约3wt%以上)的玻璃批,在空气中熔化时,首先分离成两个液相;一个是富含AgCl的相,另一个是富含硅酸盐的相。后者冷却到室温后仍保持玻璃状。因此,添加到批次中的AgCl的很大一部分几乎是瞬间从玻璃中丢失的。相分离后,损失的Ag)和Cl玻璃融化可能继续通过蒸发等氯化物AgCl和氯化钠的融化也被空气氧化的氯化物融化:4 AgCl + O2→2 Ag2O + 2氯↑在后一种机制只有Cl被认为是失去了,因为Ag2O玻璃融化形成的具有较高的溶解度。Ag)和Cl的损失率都低但Cl的有点高于Ag.2)包含少量的玻璃批AgCl(少于0.5 wt %)没有显示出液相分离但Ag)和Cl的损失发生在缓慢利率作为批次包含大量观察AgCl.3)眼镜与AgCl融化在空气中饱和蒸汽,Ag含量迅速增加,而Cl内容保持不变。当玻璃在NaCl蒸汽饱和的空气中熔化时,Ag的含量缓慢下降,而Cl的含量保持不变。NaCl蒸汽饱和空气中Ag的损失率略高于空气中。饱和BaCl2蒸汽的空气气氛的影响介于空气和饱和NaCl蒸汽的空气气氛之间。假设大气中的氯化物蒸气对玻璃熔液中氯化物的蒸发和氯化物蒸气被空气氧化的抑制作用,可以解释上述结果。4)机械搅拌玻璃熔液对加速玻璃熔液中氯化物的蒸发没有显著的作用。
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