首页> 外文学位 >The origin of the suprathermal seed population for Fermi acceleration of ions at the Earth's bow shock.
【24h】

The origin of the suprathermal seed population for Fermi acceleration of ions at the Earth's bow shock.

机译:在地球弓激波中费米加速离子加速的超热种子种群的起源。

获取原文
获取原文并翻译 | 示例

摘要

The Fermi mechanism for the acceleration of ions to energies of hundreds of keV at the Earth's bow shock is generally accepted, but the origin of the necessary suprathermal seed particle population is not known. The two current hypotheses are leakage from the magnetosheath, and acceleration directly out of the solar wind at the shock surface. Observations of 3D ion distributions close to the shock are presented from the 3D Plasma and Energetic Particle experiment on the WIND spacecraft. A model is developed to trace the trajectories of these particles back to the shock using plasma and magnetic field observations to reconstruct the shock geometry and magnetic turbulence encountered by the particle.; We use this model to interpret the observations. We follow the trajectories of ions in the observed distribution just downstream of the shock, and show that the phase space density that leaks through the shock is too low to explain the observed upstream ions.; We then use the model to predict the evolution of observed solar wind ion distributions as they encounter the shock. The model predicts a fraction of the solar wind will reflect off the shock. We find that turbulence increases the fraction that reflects, and the predicted reflecting phase space density agrees with the observed upstream distribution. The simulations correctly predict the velocity and pitch angle of the observed upstream ions, and also the evolution of gyrophase with time. A comparison between the simulations and observations shows that the reflected ions have a broader distribution in gyrophase than predicted. We show that this is not due to interactions with the upstream medium, and present an argument that it is caused by local variations in the shock normal direction caused by magnetic turbulence convecting into the shock.; The model also predicts that, under certain conditions, ions can undergo multiple encounters with the shock, gaining energy as they grad-B drift in the convective electric field. We present observations in agreement with these predictions, showing that ions can be accelerated up to at least {dollar}sim{dollar}7 keV at the shock surface, directly out of the solar wind.
机译:人们普遍接受费米机理,即在地球的弓激波中将离子加速到几百keV的能量,但是尚不清楚必需的超热种子粒子的起源。当前的两个假设是磁石表面的泄漏,以及在冲击表面直接从太阳风中加速出来的现象。 WIND航天器上的3D等离子体和高能粒子实验提供了接近冲击的3D离子分布的观察结果。建立了一个模型,利用等离子和磁场观测来追踪这些粒子的轨迹回到激波,以重建粒子遇到的激波几何形状和磁湍流。我们使用此模型来解释观察结果。我们遵循在冲击下游观察到的分布中离子的轨迹,并表明通过冲击泄漏的相空间密度太低,无法解释观察到的上游离子。然后,我们使用该模型预测观察到的太阳风离子在遇到冲击时的演变。该模型预测,太阳风的一部分会从冲击中反射出来。我们发现湍流增加了反射的比例,并且预测的反射相空间密度与观察到的上游分布一致。该模拟正确地预测了所观察到的上游离子的速度和俯仰角,以及旋流相随时间的演变。模拟和观察结果之间的比较表明,反射离子在旋相中的分布比预测的要宽。我们证明这不是由于与上游介质的相互作用所引起的,并且提出了一个论点,认为这是由于在对流中对流的磁湍流引起的在冲击法线方向上的局部变化引起的。该模型还预测,在某些条件下,离子可能会经受多次冲击,因为它们在对流电场中的grad-B漂移会获得能量。我们提出的观测结果与这些预测相符,表明离子可以在冲击表面上直接从太阳风中加速至至少7 keV。

著录项

  • 作者

    Ashford, Stephen Martin.;

  • 作者单位

    University of California, Berkeley.;

  • 授予单位 University of California, Berkeley.;
  • 学科 Physics Astronomy and Astrophysics.; Physics Fluid and Plasma.
  • 学位 Ph.D.
  • 年度 1998
  • 页码 166 p.
  • 总页数 166
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 天文学;等离子体物理学;
  • 关键词

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号