非框架迁移和不可逆转的压力诱导的化在一个地石
Yongjae Lee1, Thomas Vogt, Joseph A Hriljac
1Physics Department, Brookhaven National Laboratory, Upton, New York 11973, USA.
Nature
|December 6, 2002
概括
对石的液压压力影响还没有得到充分的研究. 这项研究表明,非框架金属离子显著影响压力下的甲酸盐纳托利特中不可逆转的水分.
科学领域:
- 材料科学 材料科学 材料科学
- 晶体学 晶体学是指结晶学.
- 地质化学 地质化学
背景情况:
- 石是微孔晶体固体,具有多样化的3D结构.
- 框架包含/四面体,带有电荷平衡和孔中的水.
- 水静压对热带石结构的影响比温度效应更难理解.
研究的目的:
- 调查水静压对热带石结构和性质的影响.
- 比较压力诱导的酸和酸加酸纳托利特的水分行为.
- 阐明非框架金属离子在压力诱导的结构变化中的作用.
主要方法:
- 使用可变温度和X射线衍射的高压研究.
- 高压回收相的结构分析.
- 合成和天然石类型的比较分析.
主要成果:
- 氨基酸盐纳托莱特显示了可逆的压力诱导水合.
- 气酸盐纳特洛伊特在释放压力时表现出不可逆转的水合.
- 不可逆转的水合与非框架金属离子的显著重新排列有关.
结论:
- 非框架金属离子在水立压下调解石特性方面发挥着至关重要的作用.
- 阴离子的类型会影响天然石结构中压力诱导的水合的可逆性.
- 了解这些依赖压力的行为是极端环境中热石应用的关键.
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