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Space weathering on the Moon: Farside-nearside solar wind precipitation asymmetry

机译:月球上的空间风化:远-近太阳风降水不对称

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摘要

The lunar surface is continuously under the impact of solar wind plasma, which breaks the chemical bonds of the surface material resulting in weathering of the surface and a modified chemical composition. Ion impact also sputters the surface material, affecting the composition of the lunar exosphere, and it controls the electrical properties of both the lunar surface and the near surface space.We have studied the lunar farside-nearside (FN) hemispherical asymmetry of the solar wind proton impact on the lunar surface along the orbit of the Moon during fast solar wind conditions. The analysis is based on a 3D hybrid model where ions are accelerated by the macroscopic j x B and pressure gradient forces.The derived proton impact surface map shows that the highest cumulative solar wind proton addition on the lunar surface is located on the farside while the most energetic protons precipitate on the nearside. The total ion impact rate was found to be smallest when the Moon is deep in the magnetotail. The total ion impact rate on the lunar surface varies while the Moon orbits the Earth and these longitudinal variations are caused by the magnetosphere and lunar tidal locking.
机译:月球表面连续受到太阳风等离子体的影响,这会破坏表面材料的化学键,导致表面风化和化学成分改变。离子撞击还会溅射表面物质,影响月球外层的组成,并控制月球表面和近地表空间的电学特性。我们研究了太阳风的月球上半边不对称性在快速的太阳风条件下,质子沿月球轨道撞击月球表面。该分析基于3D混合模型,其中离子通过宏观jx B和压力梯度力加速。推导的质子撞击表面图显示,月球表面上最高的累积太阳风质子添加位于较远的地方,而最大的高能质子沉淀在附近。当月球深处在磁尾时,总离子撞击率最小。当月球绕地球运行时,对月球表面的总离子撞击率会发生变化,而这些纵向变化是由磁层和月球潮汐锁定引起的。

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  • 来源
    《Planetary and space science》 |2019年第2期|9-22|共14页
  • 作者单位

    Aalto Univ, Elect & Nanoengn, Sch Elect Engn, Espoo, Finland;

    Austrian Acad Sci, Space Res Inst, A-8042 Graz, Austria;

    Univ Bern, Phys Inst, Bern, Switzerland;

    Austrian Acad Sci, Space Res Inst, A-8042 Graz, Austria|Moscow MV Lomonosov State Univ, Skobeltsyn Inst Nucl Phys, Moscow, Russia;

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