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Influence of tail-like magnetic field on O~+ ion distribution in the martian magnetosphere

机译:尾部磁场对火星磁层O〜+离子分布的影响

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摘要

Based on the comparison with the Earth, using the LB magnetic field model, the distribu- tion of O~+ ion originating from the ionosphere in the Martian magnetosphere is theoretically studied un- der different conditions of the tail-like magnetic field. The results show that the Tail-like magnetic field has influence on the O~+ ion flux in the Martian magnetic: (I) the O~+ ion flux in the martian tail will increase if the tail-like magnetic filed increases; when the tail-like magnetic field increases from 5 nt to 20 nT, the O~+ ion flux increases 3 times in the region of 2.8 R_m in the martian tail; and (II) the O~+ ion flux decreases with increasing intrinsic moment; when the intrinsic moment increases about 5 times, the flux decreases to one fourth in the region of 2.8 R_m in th emartian tail.
机译:在与地球的比较的基础上,使用LB磁场模型,在尾状磁场的不同条件下,从理论上研究了火星磁层中电离层中O〜+离子的分布。结果表明,尾状磁场对火星磁场中的O〜+离子通量有影响:(I)如果尾状磁场增加,火星尾部的O〜+离子通量会增加;当尾状磁场从5 nt增加到20 nT时,火星尾中O〜+离子通量在2.8 R_m的范围内增加3倍。 (II)O〜+离子通量随本征矩增加而减小;当本征矩增加约5倍时,通量在emartian尾部的2.8 R_m区域减小至四分之一。

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