首页> 外文期刊>Journal of Geophysical Research, A. Space Physics: JGR >Model investigation of the influence of the crustal magnetic fieldon the oxygen ion distribution in the near Martian tail
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Model investigation of the influence of the crustal magnetic fieldon the oxygen ion distribution in the near Martian tail

机译:地壳磁场对火星尾附近氧离子分布影响的模型研究

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摘要

To investigate the influence of the Martian crustal magnetic field on the accelerationand escape of the planetary ions in the near tail region, the distributions of planetary oxygenions are studied by means of test particle simulation in an electromagnetic environmentcreated by a recent multispecies Magnetohydrodynamics (MHD) simulation of the solar windinteraction with Mars, with crustal field included or excluded. Results under differentcrustal field conditions are compared to determine the effects of crustal field. It is found thatwhen crustal field is present, draped magnetic field lines are replaced by closed field linesin the near tail region and the electric field is also intensified because of the Hall effect. As aresult, the oxygen ion distribution reveals distinct stream structures in the tail region whencrustal field is included, with one hot stream at the central tail and two cold streams at the flankof the tail. Some energetic ions inside the hot stream are accelerated toward the planet,instead of escaping downstream.
机译:为了研究火星地​​壳磁场对近尾区域行星离子的加速和逸出的影响,在最近的多物种磁流体动力学(MHD)模拟创建的电磁环境中,通过测试粒子模拟研究了行星含氧离子的分布。与火星的太阳风相互作用,包括或不包括地壳。比较不同地壳条件下的结果,以确定地壳的影响。结果发现,当存在地壳磁场时,在近尾巴区域,垂线磁场线被闭合的场线代替,并且由于霍尔效应,电场也被增强。结果,当包含地壳时,氧离子分布在尾部区域显示出不同的流结构,其中一个热流在中央尾部,而两个冷流在尾部侧面。热流内部的一些高能离子会向行星加速,而不是向下游逸出。

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