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Observation of Injection and Pre-Acceleration Processes in the Slow Solar Wind

机译:慢风中注入和加速过程的观察

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Knowledge of injection and pre-acceleration mechanisms of ions is of fundamental importance for understanding particle acceleration that takes place in various astrophysical settings. The heliosphere offers the best chance to study these poorly understood processes experimentally. We examine ion injection and pre-acceleration using measurements of the bulk and suprathermal solar wind, and pickup ions. Our most puzzling observation is that high-velocity tails, extending to at least 60 keV/e-the upper limit of measurements -, are omnipresent in the slow, in-ecliptic solar wind; these tails exist even in the absence of any shocks. The cause of these tails is unknown. In the disturbed solar wind inside CIRs and downstream of shocks and waves these high-speed tails in the distributions of H~+, He~+ and He~(++) become more pronounced and more complex, but with the shapes of the tails showing the same dependence on ion speed for the different species. Pickup hydrogen and helium are found to be readily injected for subsequent acceleration to MeV energies, and thus are the dominant source of CIR-accelerated energetic ions. Competing sources of MeV ions heavier than He are: (1) heated suprathermal solar wind observed downstream of CIR shocks, (2) interstellar N, O and Ne, and (3) the newly discovered heavy pickup ions from an extended inner source inside 1 AU. Our main conclusion is that mechanisms other than the traditional first-order shock acceleration process produce most of the modestly accelerated ions seen in the slow solar wind.
机译:离子的注入和预加速机制的知识对于理解在各种天体环境中发生的粒子加速至关重要。日光层提供了最好的机会,以实验方式研究这些尚不为人所知的过程。我们使用对体热和超热太阳风以及拾取离子的测量来检查离子注入和预加速。我们最令人困惑的观察是,在黄道缓慢的日风中,高速尾巴无处不在,至少延伸到60 keV / e(测量的上限)。即使没有任何冲击,这些尾巴也存在。这些尾巴的原因尚不清楚。在CIR内部和冲击波的下游受扰动的太阳风中,这些高速尾巴在H〜+,He〜+和He〜(++)的分布中变得更加明显和复杂,但是尾巴的形状显示出不同物种对离子速度的相同依赖性。发现吸收的氢和氦很容易注入,随后加速到MeV能量,因此是CIR加速的高能离子的主要来源。比He重的MeV离子的竞争来源是:(1)在CIR冲击的下游观察到加热的超热太阳风;(2)星际N,O和Ne;(3)从内部1的扩展内部来源新发现的重质拾取离子AU。我们的主要结论是,除了传统的一阶冲击加速过程外,其他机制还产生了在缓慢的太阳风中观察到的大多数适度加速的离子。

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