在地球核心-地幔边界进行广泛的铁水交换可以解释地震异常
Katsutoshi Kawano1, Masayuki Nishi2,3, Hideharu Kuwahara4
1Department of Earth and Space Science, Osaka University, Toyonaka, 560-0043, Japan.
Nature communications
|October 15, 2024
概括
核心-地幔边界的富含水的化学反应解释了深层地幔的铁丰富,这表明水循环影响了超低速区 (ULVZ). 这解决了关于ULVZ起源的辩论.
科学领域:
- 地质物理学 地质物理学
- 矿物物理 矿物物理
- 地质化学 地质化学
背景情况:
- 地震观测揭示了核心-地幔界限 (CMB) 上方最下层地幔的化学异质性.
- 超低速度区域 (ULVZs) 呈现出神秘的地震波速度,核中的铁缩被认为是原因.
- 现有的原子扩散和铁透模型不能完全解释观察到的ULVZ铁缩.
研究的目的:
- 为了研究最下层地幔中铁丰富的机制.
- 确定水在核心-地幔相互作用和铁运输中的作用.
- 将CMB的化学过程与ULVZ的地震特征联系起来.
主要方法:
- 在不同的条件下,对酸桥和铁之间的化学反应进行实验研究.
- 对地震波速率的分析以及对地幔构成的影响.
- 模拟深水循环及其与核心-地幔边界的相互作用.
主要成果:
- 在水性条件下,酸桥和铁之间的化学反应会导致酸盐中铁的丰富程度显著.
- 无水条件不会产生相同程度的铁丰富.
- 当水存在时,在地幔底部的几公里内发生深度铁丰富.
结论:
- 核心和地幔之间的水性化学反应是深度铁丰富的关键机制.
- 水的存在促进了核心-地幔边界的深度铁丰富.
- ULVZ的地震特征可能表明整个地幔对流和地球历史上深水循环.
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