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中国物理学会期刊

高压下NaAlSi2O6体系中硬玉-玻璃双向相变起始边界的非对称压力响应

Asymmetric pressure response of the onset boundaries of bidirectional phase transformations between jadeite and glass in the NaAlSi2O6 system under high pressure

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  • 翡翠被誉为“玉中之王”, 其主要组成矿物为硬玉(NaAlSi2O6). 在高压条件下, 人工合成翡翠与天然翡翠改性过程均涉及硬玉与同成分玻璃之间的双向相变. 因此, 明确NaAlSi2O6体系在高压升温条件下硬玉向玻璃转变及玻璃向硬玉晶化转变的起始边界, 对于认识该体系的相变规律以及优化相关合成与改性工艺均具有重要意义. 本研究采用高压原位差热分析技术, 并结合X射线衍射、拉曼光谱和扫描电子显微镜表征, 系统研究了0—5 GPa范围内NaAlSi2O6体系在连续升温条件下上述两种转变的起始边界, 并分析了其压力响应特征. 结果表明: 硬玉向玻璃转变起始温度随压力升高显著上移; 而在约2.2 GPa条件下未明确观察到玻璃晶化, 在3.0—5.0 GPa范围内晶化起始温度稳定于1000—1050 ℃, 呈现较弱的压力依赖性. 上述结果表明, 该体系硬玉-玻璃双向相变起始边界具有明显的非对称压力响应特征, 为翡翠高压合成与热处理工艺温压窗口的选择提供参考.

     

    Jadeite, the principal mineral constituent of jadeite jade, is widely regarded as the “king of jade”. Under high-pressure conditions, both artificial jadeite-jade synthesis and the modification of natural jadeite jade involve transformations between crystalline jadeite and a glass with the same composition. Therefore, clarifying the onset boundaries of the jadeite-to-glass transformation and the glass-to-jadeite crystallization in the NaAlSi2O6 system under high-pressure heating conditions is important for understanding the phase transformation behavior of this system and for optimizing related synthesis and modification processes. In this work, the bidirectional transformation behavior between jadeite and glass in the NaAlSi2O6 system was systematically investigated over the pressure range of 0–5 GPa under continuous heating. High-pressure in situ differential thermal analysis was used to determine the thermal anomalies and onset temperatures of the transformations, and the phase and microstructural characteristics of the quenched samples were examined by X-ray diffraction, Raman spectroscopy, and scanning electron microscopy. The results show that the onset temperature of the jadeite-to-glass transformation increases markedly with increasing pressure. It increases from approximately 1116 ℃ at 1.3 GPa to approximately 1750–1850 ℃ at 5.0 GPa, indicating that high pressure significantly enhances the thermal stability of crystalline jadeite. In contrast, no clear crystallization of NaAlSi2O6 glass was observed at approximately 2.2 GPa under the present heating path and holding conditions. When the pressure increases to 3.0–5.0 GPa, glass-to-jadeite crystallization occurs, but its onset temperature remains nearly constant at 1000–1050 ℃, showing only weak pressure dependence. This behavior suggests that the crystallization process is more strongly constrained by kinetic factors such as nucleation, crystal growth, and atomic diffusion. The comparison of the two opposite transformation processes reveals a pronounced asymmetric pressure response of the onset boundaries between jadeite and glass in the NaAlSi2O6 system. The main contribution of this work is to establish, within a unified experimental framework, the onset boundaries of the jadeite-to-glass and glass-to-jadeite transformations under continuous high-pressure heating, rather than only discussing equilibrium phase relations or individual crystallization conditions. These results provide an experimental reference for understanding the actual transformation behavior of the NaAlSi2O6 system under non-equilibrium heating paths and for selecting pressure-temperature windows in high-pressure jadeite synthesis and heat-treatment processes.

     

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