相关实验视频
Updated: Jun 11, 2026

13:48
Design and Construction of an Urban Runoff Research Facility
Published on: August 8, 2014
概括
斯蒂索维特是一种高压二氧化矿物质,可以在地球地幔中储存大量的水. 它的含量与相关,表明潜水板中深水储存的可能性.
科学领域:
- 地质化学 地质化学
- 矿物学是什么?矿物学是什么?
- 石化学 石化学是一门学科.
背景情况:
- 斯蒂索维特是二氧化的高压多态,在地球地幔中具有潜在的意义.
- 了解地幔中的水存储对于地质过程至关重要.
研究的目的:
- 为了确定合成石中的含量.
- 为了研究含量和stishovite中的结合之间的关系.
主要方法:
- 史提索维特样品的合成.
- 福里埃变换红外光谱 (FTIR) 用于分析.
主要成果:
- 在stishovite中量化了的度.
- 含量取决于 (Al2O3) 的度.
- 最大含量达到了549个+/- 23个10个原子中的Si原子在1.51%的重量%Al2O3.
结论:
- 斯蒂索维特可以包含大量的.
- 这种矿物质可能会在深层潜水板中充当水库.
- 斯蒂索维特可以在热地幔区域储存水,那里的水性矿物是不稳定的.
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