铁在地球地幔中的分割:朝着深层下层地幔不连续性的方向
James Badro1, Guillaume Fiquet, François Guyot
1Laboratoire de Mine Université ralogie-Cristallographie de Paris, Université Paris VI, Université Paris 7, CNRS, IPGP, 4 place Jussieu, F-75252 Paris Cedex 05, France.
地球下层地幔中的铁经历了大约2000公里深处的高旋转到低旋转过渡. 这导致铁在ferropericlase中缩,可能在深层地幔中形成不同的层.
科学领域:
- 地质物理学 地质物理学
- 矿物物理 矿物物理
- 地球科学 地球科学 地球科学
背景情况:
- 地球的下层地幔主要由铁烯酸和酸盐矿组成.
- 了解铁在高压下的行为对于建模地球深层过程至关重要.
研究的目的:
- 为了研究与下层地幔相关的高压下铁烯酸中铁的旋转状态.
- 确定旋转过渡发生的压力及其对铁分区的影响.
主要方法:
- 在高压实验中对铁烯酶 ((Mg0.83Fe0.17) O) 进行了实验.
- 铁的自旋状态在60-70千兆帕斯卡尔的压力范围内被测量.
主要成果:
- 在ferropericlase中观察到铁的高旋转到低旋转过渡在60和70GPa之间.
- 这种压力范围对应于地球下层地幔中约2000公里的深度.
- 在ferropericlase和酸矿石之间,铁的分割系数可能会显著增加.
结论:
- 旋转过渡表明下层地幔的潜在分层成不同的富含铁和缺乏铁的层.
- 这种分层可能会对地球深层的热量和质量传输产生重大影响.
- 这些发现完善了下层地幔组成和动态的模型.
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