在地球下层地幔的旋转过渡区
Jung-Fu Lin1, György Vankó, Steven D Jacobsen
1Lawrence Livermore National Laboratory (LLNL), 7000 East Avenue, Livermore, CA 94550, USA.
概括
铁铁铁是什么意思 铁铁铁
科学领域:
- 地质物理学 地质物理学
- 矿物物理 矿物物理
背景情况:
- 地球下层地幔中的矿物质特性受到铁的电子状态的影响.
- 之前的研究还没有探测到代表性的压力和温度.
- 铁烯酸是下层地幔的一个关键矿物.
研究的目的:
- 在高压和高温下测量铁在低地幔铁烯酸中铁的自旋状态.
- 了解下层地幔中铁旋转过渡的地震影响.
主要方法:
- 使用X射线发射光谱测量铁的自旋状态.
- 实验是在激光加热的钻石天细胞中进行的.
- 达到了高达95千兆帕斯卡的压力和高达2000凯尔文的温度.
主要成果:
- 观察到铁烯酸酶中铁的逐渐旋转过渡.
- 这种过渡发生在与中至下地幔相对应的压力-温度范围内.
- 低旋转铁烯酸盐比高旋转铁烯酸盐密度更高,音速也更快.
结论:
- 在中低地幔条件下观察到的低旋转铁烯酶的增加将产生一个旋转过渡区.
- 这个区域的特点是比正常密度更的密度梯度.
- 这一发现对解释来自地球深层内部的地震数据具有重大意义.
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