相关实验视频
Updated: Jul 12, 2026

07:26
Synthesis and Microdiffraction at Extreme Pressures and Temperatures
Published on: October 7, 2013
概括
在高压下,矿物质高桑尼丁可逆地转化为三临床阶段. 这种结构变化是由压力,温度和性离子大小控制的,类似于高温转换.
科学领域:
- 矿物学和结晶学. 矿物学和结晶学.
- 地质化学和石油学.
背景情况:
- 高桑尼丁,地 (K,Na) AlSi(3) O(8) 的高温多态,在不同的条件下表现出结构变化.
- 高温转化为单矿是压力诱导相变的类比.
研究的目的:
- 在高压下研究高桑尼丁的可逆转化到高压下的三临床阶段.
- 阐明控制性地的这种相位过渡的结构控制.
主要方法:
- 在不同成分的性田上进行高压实验.
- 在过渡点对单元细胞尺寸和结构变化的分析.
主要成果:
- 在高压下,高桑尼丁可逆地转化为三临床阶段.
- 过渡时的单元细胞尺寸在不同的组成中非常相似 (a ≈ 8.30 Å,b ≈ 12.97 Å,c ≈ 7.14 Å,β ≈ 116.2°).
- 结构变化,包括四面体角,适应性离子大小 (Na+,K+) 的变化.
结论:
- 高桑尼丁到三临床相转换是结构控制的.
- 温度,压力和Na/K比率通过改变有效的酸盐大小和它们在地框架内的容纳来影响结构变化.
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