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南极的星际 Fe-60。

Interstellar ^{60}Fe in Antarctica.

机构信息

Physik-Department, Technische Universität München, 85748 Garching, Germany.

Excellence Cluster Universe, 85748 Garching, Germany.

出版信息

Phys Rev Lett. 2019 Aug 16;123(7):072701. doi: 10.1103/PhysRevLett.123.072701.

DOI:10.1103/PhysRevLett.123.072701
PMID:31491090
Abstract

Earth is constantly bombarded with extraterrestrial dust containing invaluable information about extraterrestrial processes, such as structure formation by stellar explosions or nucleosynthesis, which could be traced back by long-lived radionuclides. Here, we report the very first detection of a recent ^{60}Fe influx onto Earth by analyzing 500 kg of snow from Antarctica by accelerator mass spectrometry. By the measurement of the cosmogenically produced radionuclide ^{53}Mn, an atomic ratio of ^{60}Fe/^{53}Mn=0.017 was found, significantly above cosmogenic production. After elimination of possible terrestrial sources, such as global fallout, the excess of ^{60}Fe could only be attributed to interstellar ^{60}Fe which might originate from the solar neighborhood.

摘要

地球不断受到含有宝贵外星过程信息的外星尘埃的轰炸,例如恒星爆炸或核合成引起的结构形成,可以通过长寿命放射性核素追踪到这些过程。在这里,我们通过加速器质谱分析 500 公斤来自南极洲的雪,首次报告了最近地球 ^{60}Fe 流入的情况。通过测量宇宙成因放射性核素 ^{53}Mn,发现 ^{60}Fe/^{53}Mn 的原子比为 0.017,明显高于宇宙成因产生的比例。在排除了可能的地球来源,如全球沉降物之后, ^{60}Fe 的过剩只能归因于星际 ^{60}Fe,它可能来自太阳系附近。

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