阶段转换对地球地幔压缩波速度的影响
1Mineral Physics Institute Department of Geosciences, Stony Brook University, Stony Brook, New York 11794, USA. lilli@ic.sunysb.edu
Nature
|August 23, 2008
概括
地球上的地震波速度.
科学领域:
- 地质物理学 地质物理学
- 矿物物理 矿物物理
- 地震学 地震学
背景情况:
- 地震波的速度取决于矿物质对压力和压力的反应.
- 减少体积的相位转换显著降低了散装模量.
- 在地球深处的条件下,很难获得实验数据.
研究的目的:
- 实验性地研究在相位过渡期间的地震波速度变化.
- 评估相变动力学对波浪传播的影响.
- 为了确定相位过渡是否影响地球地幔中的地震速度.
主要方法:
- 进行了基于同步射线的X射线衍射实验.
- 研究了橄 - 环木石相变的过程.
- 在100秒的时间尺度上测量了散装模块软化.
主要成果:
- 在橄-环木二相循环中观察到散装模量软化.
- 在地球的410,520和660公里不连续处,压缩波速度可能较低.
- 结果被调整为预期的地球压力和颗粒大小.
结论:
- 阶段过渡动力学显著影响地震波速度.
- 这些发现表明,上层地幔中存在大量的速度扰动.
- 类似的效应可能发生在其他相位过渡中,影响地幔结构模型.
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Phase Diagram
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