在地观测H2O冰的高压阶段
1I. Chou, 955 National Center, U.S. Geological Survey, Reston, VA 20192, USA. J. G. Blank, A. F. Goncharov, H. Mao, R. J. Hemley, Geophysical Laboratory and Center for High Pressure Research, Carnegie Institution of Washington, 5251 Broad.
概括
科学家们发现了一种新的固态水 (H2O) 阶段,具有独特的晶体结构和融化行为. 这一发现扩大了我们对水的理解.
科学领域:
- 固态化学 固态化学
- 材料科学是一种材料科学.
- 地质物理学 地质物理学
背景情况:
- 水 (H2O) 在不同的压力-温度条件下存在于许多固体相 (冰).
- 了解这些阶段对于行星科学和高压物理学至关重要.
- 以前的研究已经确定了许多冰的多态,但完整的相位图仍然不完整.
研究的目的:
- 识别和描述以前未知的水的固态相.
- 研究压力-温度融关系和这些相的结构性质.
主要方法:
- 直接观察冰晶的生长和融化,使用水热钻石细胞.
- 分析H2O散装密度在1203~1257kg/m3之间.
- 在-10°C至50°C之间的温度下进行的测量.
- 使用振动拉曼光谱学的表征.
主要成果:
- 识别了一种新的,以前未知的H2O固态相.
- 对新阶段观察到明显的生长模式和压力-温度融关系.
- 新冰期呈现出一个无序的异构结构,与冰VI相似.
- 在实验条件下,观察到四种冰形式 (V,VI,IV和新阶段冰) 在实验条件下融化.
结论:
- 通过实验证实了水的新固态阶段.
- 新阶段具有独特的结构和热力学特性.
- 这一发现有助于更全面地了解H2O相位图.
相关概念视频
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