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首页> 外文期刊>Nonlinear processes in geophysics >Ion motion in the current sheet with sheared magnetic field-Part 1: Quasi-adiabatic theory
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Ion motion in the current sheet with sheared magnetic field-Part 1: Quasi-adiabatic theory

机译:具有剪切磁场的电流板中的离子运动-第1部分:准绝热理论

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摘要

We present a theory of trapped ion motion in the magnetotail current sheet with a constant dawn-dusk component of the magnetic field. Particle trajectories are described analytically using the quasi-adiabatic invariant corresponding to averaging of fast oscillations around the tangential component of the magnetic field. We consider particle dynamics in the quasi-adiabatic approximation and demonstrate that the principal role is played by large (so called geometrical) jumps of the quasi-adiabatic invariant. These jumps appear due to the current sheet asymmetry related to the presence of the dawn-dusk magnetic field. The analytical description is compared with results of numerical integration. We show that there are four possible regimes of particle motion. Each regime is characterized by certain ranges of values of the dawn-dusk magnetic field and particle energy. We find the critical value of the dawn-dusk magnetic field, where jumps of the quasi-adiabatic invariant vanish.
机译:我们提出了具有恒定黎明黄昏分量磁场的磁尾电流板中被困离子运动的理论。使用准绝热不变量分析地描述了粒子轨迹,该准绝热不变量对应于磁场切向分量周围快速振荡的平均值。我们在准绝热近似中考虑了粒子动力学,并证明了主要作用是由准绝热不变量的大(所谓的几何)跃变引起的。这些跳变的出现是由于与黎明黄昏磁场的存在有关的当前薄片不对称性。将分析说明与数值积分结果进行比较。我们证明了粒子运动有四种可能的状态。每个状态的特征是黎明黄昏磁场和粒子能量的特定值范围。我们找到了黎明黄昏磁场的临界值,准绝热不变跃变消失了。

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