Phase separation in GeO–GeO2 glasses

John Philip de Neufville, D. Turnbull
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引用次数: 21

Abstract

A series of transparent homogeneous amorphous solids between GeO2 and GeO has been prepared by rapid quenching of liquids and by vapour deposition. Density and refractive index increase smoothly with increasing Ge/O ratio and provide a useful index of composition. Glasses in the range GeO–GeO1.85 undergo a rapid exothermic transformation when heated above 400°C accompanied by a pronounced blackening, an increase in refractive index, and slight decrease in density. Electron microscopy and diffraction results indicate that the transformation involves the precipitation on a 50–100 A scale of an amorphous tetrahedrally coordinated Ge-rich phase. The interconnected microstructure so produced is suggestive of spinodal decomposition. A transitional region near GeO1.9 is characterized by sluggish phase separation kinetics and a dispersed particle morphology suggestive of a nucleation and growth precipitation mechanism. Glasses in the range GeO1.9–GeO2 show no evidence for phase separation.
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GeO-GeO2玻璃的相分离
采用液相快速淬火和气相沉积法制备了一系列介于GeO2和GeO之间的透明均匀非晶固体。密度和折射率随Ge/O比的增加而平稳增加,并提供了一个有用的成分指标。当加热到400°C以上时,GeO-GeO1.85范围内的玻璃经历快速放热转变,伴随着明显的变黑、折射率增加和密度轻微下降。电镜和衍射结果表明,相变包括在50-100 a范围内析出非晶态的四面体配位富锗相。这样产生的相互连接的微观结构暗示了独立分解。靠近GeO1.9的过渡区具有缓慢的相分离动力学和分散的颗粒形态,提示成核和生长沉淀机制。在GeO1.9-GeO2范围内的玻璃没有显示出相分离的证据。
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