地球上"缺失"的可能存在于地球核心
Nature
|May 9, 2001
概括
和在地球核心形成过程中表现相似. 这表明进入了核心与,否定了需要深地幔储存库.
科学领域:
- 地质化学 地质化学
- 行星科学 行星科学
- 地球科学 地球科学 地球科学
背景情况:
- 地球的核心形成涉及金属和酸盐相的分离.
- 温和的 siderophile 元素如在酸盐地幔中被耗尽,这表明核心进入.
- 耐火的光电元素 (如,稀土元素) 没有耗尽,表明它们仍然存在于酸盐部分.
研究的目的:
- 为了研究 (Nb) 在液体金属和液体酸盐之间的分区行为.
- 为了确定Nb在地和上层地幔的耗尽是否需要深层地幔储存.
- 为了比较Nb的分区与 (V) 的分区,这是一种已知的进入核心的元素.
主要方法:
- 高压实验模拟核心-地幔分化.
- 分析金属和酸盐之间的元素分区.
- 和分区系数的比较.
主要成果:
- 和在高压下在液态金属和液态酸盐之间表现出几乎相同的分离行为.
- Nb的分割与V的分割是一致的,V是一个中度的 siderophile 元素.
- 在地和上层地幔中观察到的Nb耗尽可以通过核心分割来解释,而不是隐藏的储存库.
结论:
- 可能在行星形成期间与一起进入地球核心.
- 深层地幔含丰富的水库的概念是不必要的,以解释观察到的耗尽.
- 这一发现完善了我们对地球早期化学差异化和元素分布的理解.
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