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首页> 外文期刊>Journal of Geophysical Research, A. Space Physics: JGR >Kinetic simulations of electric field structure within magnetic island during magnetic reconnection and their applications to the satellite observations
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Kinetic simulations of electric field structure within magnetic island during magnetic reconnection and their applications to the satellite observations

机译:磁重连接期间磁岛内电场结构的动力学模拟及其在卫星观测中的应用

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摘要

Magnetic islands are considered to play a crucial role in collisionless magnetic reconnection. We use particle-in-cell simulations to investigate electric field E_z structure in the magnetic islands (including primary and secondary islands) with and without a guide field during magnetic reconnection. It is found that the electric field has multilayers in the primary island and a large bipolar structure in the secondary island in the absence of guide field. The electric field is provided by the Hall term (J × B)_z (mainly), the divergence of electron pressure tensor, and the convective term (V_i × B)_z in the outer and the inner region of primary island, while the electric field is much smaller (~0) in the middle and the core region of primary island due to the cancelation of the three terms. The single bipolar electric field is primarily provided by the Hall term in the secondary island. In the presence of a guide field, the electric field has multiple layers in the primary island (similar to zero guide field case) and the secondary island. However, there still exists one single large sharp bipolar structure of electric field in the central region of the secondary island. The differences of electric field in the primary and secondary islands are essentially due to the variations of the current J_y. These features can be used as the observational criteria to identify different types of magnetic islands in the magnetosphere using the data of future mission, such as the Magnetospheric Multiscale mission.
机译:磁岛被认为在无碰撞磁重新连接中起着至关重要的作用。我们使用质点模拟来研究在磁重连接过程中有无引导磁场的磁岛(包括主岛和次级岛)中的电场E_z结构。发现在没有引导场的情况下,电场在初级岛中具有多层,并且在次级岛中具有大的双极结构。电场由霍尔项(J×B)_z(主要),电子压力张量的散度和对流项(V_i×B)_z在主岛的外部和内部区域提供,而电场由由于三个项的取消,在主岛的中部和核心区域的磁场小得多(〜0)。单双极电场主要由次级岛中的霍尔项提供。在存在引导场的情况下,电场在主岛(类似于零引导场的情况)和次岛中具有多层。然而,在次级岛的中心区域中仍然存在一个单一的大的尖锐双极电场结构。初级和次级岛中的电场差异主要归因于电流J_y的变化。这些特征可以用作观测标准,使用未来任务(如“磁层多尺度”任务)的数据来识别磁层中不同类型的磁岛。

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