Suppr超能文献

过去约50000年期间地球上未熔微陨石的特征、来源与通量

Characterisation, Sources and Flux of Unmelted Micrometeorites on Earth During the Last ~50,000 Years.

作者信息

Prasad M Shyam, Rudraswami N G, de Araujo Agnelo Alexandre, Khedekar V D

机构信息

Geological Oceanography Division CSIR-National Institute of Oceanography Dona Paula, Goa, 403004, India.

出版信息

Sci Rep. 2018 Jun 11;8(1):8887. doi: 10.1038/s41598-018-27158-x.

Abstract

Dust dominates extraterrestrial flux on the earth (30,000 tonnes/yr), however only ~5% of the cosmic dust survives atmospheric entry which is basically in two forms: melted and unmelted. Melted micrometeorites undergo transformational changes due to heating during atmospheric entry which obliterate evidences regarding their precursors. Unmelted micrometeorites (UMM) survive atmospheric entry with minimal alteration, they provide direct evidence for their parent bodies. Recent investigations unravelled a wide range of UMM, there are however no quantitative estimates of sources that contribute to the cosmic dust accreted by the Earth.

摘要

尘埃在地球的外星物质通量中占主导地位(每年30000吨),然而,只有约5%的宇宙尘埃在进入大气层后幸存下来,基本上有两种形式:熔融态和未熔融态。熔融的微陨石在进入大气层时由于加热而发生转变,这消除了有关其前身的证据。未熔融的微陨石(UMM)在进入大气层后幸存下来,变化极小,它们为其母体提供了直接证据。最近的研究揭示了各种各样的未熔融微陨石,然而,对于导致地球积累宇宙尘埃的来源,尚无定量估计。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/4465/5995856/146a4945e9f3/41598_2018_27158_Fig1_HTML.jpg

文献AI研究员

20分钟写一篇综述,助力文献阅读效率提升50倍。

立即体验

用中文搜PubMed

大模型驱动的PubMed中文搜索引擎

马上搜索

文档翻译

学术文献翻译模型,支持多种主流文档格式。

立即体验