利用镭同位素和 227Ac 作为示踪剂调查印度洋西南脊地区的热液活动

Morgane Léon, P. van Beek, V. Sanial, Corentin Baudet, Matthew Charette, M. Souhaut, Frédéric Vivier, Elodie Kestenare, Catherine Jeandel, Helene Planquette
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引用次数: 0

摘要

热液喷口已被证明是各种化学元素进入海洋的重要载体。尤其是镭,它是一种天然放射性核素,在海洋中的浓度很低,但在热液中却明显富集。此外,镭只受清除或生物去除的轻微影响,这使它成为评估热液喷口释放的化学元素归宿的重要示踪剂。
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Investigation of hydrothermal activity in the South West Indian Ridge region using Ra isotopes and 227Ac as tracers
Hydrothermal vents have been shown to be important vectors for various chemical elements into the ocean. In particular, radium is a naturally occurring radionuclide present in low concentrations in the ocean but is significantly enriched in hydrothermal fluids. Additionally, radium is only slightly impacted by scavenging or biological removal, which makes it a valuable tracer to evaluate the fate of the chemical elements released by hydrothermal vents
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