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磁尾中多尺度卫星(MMS)观测到的亚暴注入期间超热离子的电荷态相关能量化

Charge-State-Dependent Energization of Suprathermal Ions During Substorm Injections Observed by MMS in the Magnetotail.

作者信息

Bingham S T, Cohen I J, Mauk B H, Turner D L, Mitchell D G, Vines S K, Fuselier S A, Torbert R B, Burch J L

机构信息

The Johns Hopkins University Applied Physics Laboratory Laurel MD USA.

Southwest Research Institute San Antonio TX USA.

出版信息

J Geophys Res Space Phys. 2020 Oct;125(10):e2020JA028144. doi: 10.1029/2020JA028144. Epub 2020 Sep 29.

Abstract

Understanding the energization processes and constituent composition of the plasma and energetic particles injected into the near-Earth region from the tail is an important component of understanding magnetospheric dynamics. In this study, we present multiple case studies of the high-energy (≳40 keV) suprathermal ion populations during energetic particle enhancement events observed by the Energetic Ion Spectrometer (EIS) on NASA's Magnetospheric Multiscale (MMS) mission in the magnetotail. We present results from correlation analysis of the flux response between different energy channels of different ion species (hydrogen, helium, and oxygen) for multiple cases. We demonstrate that this technique can be used to infer the dominant charge state of the heavy ions, despite the fact that charge is not directly measured by EIS. Using this technique, we find that the energization and dispersion of suprathermal ions during energetic particle enhancements concurrent with (or near) fast plasma flows are ordered by energy per charge state (/) throughout the magnetotail regions examined (~7 to 25 Earth radii). The ions with the highest energies (≳300 keV) are helium and oxygen of solar wind origin, which obtain their greater energization due to their higher charge states. Additionally, the case studies show that during these injections the flux ratio of enhancement is also well ordered by /. These results expand on previous results which showed that high-energy total ion measurements in the magnetosphere are dominated by high-charge-state heavy ions and that protons are often not the dominant species above ~300 keV.

摘要

了解从磁尾注入近地区域的等离子体和高能粒子的加速过程及成分组成,是理解磁层动力学的重要组成部分。在本研究中,我们展示了美国国家航空航天局磁层多尺度(MMS)任务中,磁尾高能离子谱仪(EIS)观测到的高能粒子增强事件期间高能(≳40 keV)超热离子群体的多个案例研究。我们给出了多个案例中不同离子种类(氢、氦和氧)不同能量通道之间通量响应的相关分析结果。我们证明,尽管EIS不能直接测量电荷,但该技术可用于推断重离子的主导电荷态。使用该技术,我们发现在整个磁尾区域(约7至25个地球半径),与快速等离子体流同时发生(或接近)的高能粒子增强期间,超热离子的加速和扩散按每个电荷态的能量(/)排序。能量最高(≳300 keV)的离子是太阳风起源的氦和氧,由于它们较高的电荷态而获得更大的加速。此外,案例研究表明,在这些注入过程中,增强通量比也按/很好地排序。这些结果扩展了先前的结果,即磁层中的高能总离子测量主要由高电荷态重离子主导,并且质子通常不是高于约300 keV的主导物种。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/08dc/7583365/97aba4f2f564/JGRA-125-e2020JA028144-g001.jpg

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