水和在地球地幔中是不可混合的
Enikő Bali1, Andreas Audétat, Hans Keppler
1Bayerisches Geoinstitut, Universität Bayreuth, 95440 Bayreuth, Germany. enikoe.bali@geo.uni-goettingen.de
Nature
|March 15, 2013
概括
水和分子 (H2) 可以在地球深层地幔中形成两个独立的,不混合的相. 这一发现挑战了先前的假设,并可能解释了核心形成后的超缩地幔领域和上层地幔氧化.
科学领域:
- 地质化学 地质化学
- 矿物物理 矿物物理
- 地球深层的过程.
背景情况:
- 深地地幔液体含有分子 (H2).
- 之前的热力学模型假定H2和水的混合性是完全的.
- 神秘的超缩薄膜领域表明了异常的流体行为.
研究的目的:
- 在深层地幔条件下实验性地研究水和分子 (H2) 的混合性.
- 探索H2-水不可混合性对地幔地化学和演化的影响.
主要方法:
- 高压,高温实验装置. 高压,高温实验装置.
- 在现场观察流体相态度.
- 实验数据的热力学分析.
主要成果:
- 实验证据表明,水和分子 (H2) 可以作为两个不混合的相存在.
- 这种不混合性挑战了长期以来在地幔流体模型中完全混合性的假设.
- 这些发现表明,超缩地幔领域形成的新机制.
结论:
- 在某些深层地幔条件下,水和分子 (H2) 是不可混合的.
- 地幔流体不混合性可能解释了莫桑石 (SiC) 在超缩小领域的存在.
- 这种不混合性可能是上层地幔核心形成后快速氧化的关键因素.
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