概括
MgSiO(3) 矿在高压和高温下经历结构转变. 这一发现表明,当将其特性应用于地球下层地幔时,应谨慎,因为它支持整个地幔的对流.
科学领域:
- 矿物物理 矿物物理
- 地质化学 地质化学
- 高压地质物理学 高压地质物理学
背景情况:
- 了解酸矿 (MgSiO3) 的行为对于建模地球深层内部至关重要.
- 之前的研究依赖于Pbnm阶段的特性,可能误解了下层地幔条件.
研究的目的:
- 为了研究MgSiO3矿的高压,高温结构行为.
- 为了确定当前MgSiO3矿数据对地球下层地幔的适用性.
主要方法:
- 在现场进行了X射线衍射实验,使用的是DIA型立方天装置 (SAM 85).
- 测量是在7.3千兆帕斯卡的压力和超过600凯尔文的温度下进行的.
主要成果:
- 矿 MgSiO3 矿从正方体 Pbnm 对称性转化为另一种矿结构在 7.3 GPa 时在 600 K 以上.
- 在整个过渡期间,观察到0.7%的明显体积增加.
- 单元体积显示线性扩张,温度低于和高于过渡.
结论:
- Pbnm阶段的物理性质可能不适用于地球下层地幔.
- 密度分析表明,在下层地幔条件下,铁含量为10.4%的火石组成.
- 数据支持整个地幔的对流,并表明一个化学同质的地幔是合理的.
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