在体石和陆地积累中的素
Patricia L Clay1, Ray Burgess1, Henner Busemann2
1School of Earth and Environmental Sciences, University of Manchester, Manchester M13 9PL, UK.
Nature
|December 1, 2017
概括
新的研究显示,石中的重素 (,,) 含量远低于此前的估计. 这些发现影响了我们对地球的理解.
科学领域:
- 地质化学
- 星球科学
- 宇宙化学
背景情况:
- 挥发性元素,包括重型素 (,,),对于理解地球的形成和分化至关重要.
- 重型素是积累过程的有价值的标记物,但通常含量较低.
- 贵气代理同位素为确定重素度提供了高灵敏度的方法.
研究的目的:
- 准确量化各种类型的石中的 (Cl), (Br) 和 (I) 的含量.
- 为了比较地球上的素库存与原始石中的库存.
- 在地球上研究控制素输送,储存和分布的过程.
主要方法:
- 使用贵族气体代理同位素对碳化,化,Rumuruti和普通化物中重型化物含量的分析.
- 在研究的石中确定Br/Cl和I/Cl的比率.
- 石素数据与大量酸盐地球的估计数据的比较.
主要成果:
- ,Br和I的含量分别低于以前公认的6x,9x和15-37x.
- 石中的Br/Cl和I/Cl比率与土壤中的大量酸盐比率一致.
- 地球地幔中的素耗尽反映了类似的挥发性质元素.
结论:
- 仅仅是晚期积累无法解释地球当前的素预算.
- 很大一部分 (80-90%) 沉重的素存在于地球表面的水库中.
- 在早期地球分化过程中,高效地提取富含素的液体,以及晚期积聚和地幔脱气,是解释表面素度的必要条件.
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