Direct evidence of helium rain in Jupiter and Saturn
编号:243 访问权限:仅限参会人 更新:2024-04-25 23:08:48 浏览:136次 张贴报告

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摘要
The immiscibility of hydrogen-helium mixture under the temperature and pressure conditions of planetary interiors is crucial for understanding the structures of gas giant planets (e.g., Jupiter and Saturn). While the experimental probe at such extreme conditions is challenging, theoretical simulation is heavily relied in an effort to unravel the mixing behavior of hydrogen and helium. Here we develop a method via a machine learning accelerated molecular dynamics simulation to quantify the physical separation of hydrogen and helium under the conditions of planetary interiors. The immiscibility line achieved with the developed method yields substantially higher demixing temperatures at pressure above 1.5 Mbar than earlier theoretical data, but matches better to the experimental estimate. Our results revise the structures of Jupiter and Saturn where H-He demixing takes place in a large fraction of the interior radii, i.e., 27.5% in Jupiter and 48.3% in Saturn. This direct evidence of an H-He immiscible layer supports the formation of helium rain and explains the helium reduction in atmosphere of Jupiter and Saturn.
 
关键词
hydrogen-helium mixture,machine learning,planetary interiors
报告人
Xiaoju Chang
National University of Defense Technology

稿件作者
Xiaoju Chang National University of Defense Technology
Bo Chen National University of Defense Technology
Jiayu Dai National University of Defense Technology
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重要日期
  • 会议日期

    05月13日

    2024

    05月17日

    2024

  • 03月31日 2024

    注册截止日期

  • 04月15日 2024

    摘要截稿日期

主办单位
冲击波物理与爆轰物理全国重点实验室
浙江大学物理学院
中国核学会脉冲功率技术及其应用分会
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