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首页> 外文期刊>Advances in space research >Plasma electron temperature variability in lunar surface potential and in electric field under average solar wind conditions
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Plasma electron temperature variability in lunar surface potential and in electric field under average solar wind conditions

机译:平均太阳风条件下月球表面电势和电场中的等离子体电子温度变化

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The Moon is immersed in plasma environment. The most interesting challenge of the lunar plasma- field environment is that it is alternatively dominated by the extended but variable outer atmosphere of the Earth - the magnetosphere - and by the extended but highly variable solar atmosphere - the solar wind. Understanding the plasma environment and its interaction with the lunar surface will be beneficial to both manned and robotic surface exploration activities and to scientific investigations. Presented is a preliminary map of variations of lunar surface electric potential over the day side and night side using probe equations and a discussion on dust dynamics in this E-field structure using the data from Electron Reflectometer in Lunar Prospector spacecraft during 1998-1999. On the day side, potential is around 5 V and on the night side it reaches up to —82 V. On the night side region, only highly energetic electrons can overcome this large negative potential. The variation at electron temperature (T_e) strongly reflects in the surface potential. The potential reaches to a value of —82 V for T_e = 58 eV. Surface charging causes the electrostatic transport of charged dust grains. Dust grain size of 0.1 um shows a levitation height of 4.92 m on lunar day side, 748 m on terminator region and 3.7 km on the night side. The radius of maximum sized grain to be lofted, R_(max) peaks at the terminator region (R_(max) = 0.83 μm). At the transition region dust levitation is almost absent. This region is most suited for exploration activities as the region is free from hazards caused by lunar dust.
机译:月球浸没在等离子体环境中。月球等离子场环境最有趣的挑战是,它交替地受到地球扩展但可变的外部大气(磁层)和扩展但变化很大的太阳大气(太阳风)的控制。了解等离子体环境及其与月球表面的相互作用将有利于载人和机器人表面探测活动以及科学调查。呈现的是利用探测器方程式计算的白天和夜晚的月球表面电势变化的初步图,并使用1998-1999年月球探测器的电子反射仪的数据,对该电子场结构中的尘埃动力学进行了讨论。在白天,电势约为5 V,在夜间,电势达到–82V。在夜间,只有高能电子才能克服这一大的负电势。电子温度(T_e)的变化强烈反映在表面电势中。对于T_e = 58 eV,电势达到-82 V的值。表面带电会导致带电尘埃颗粒的静电传输。 0.1 um的尘埃粒径在月球日一侧的悬浮高度为4.92 m,在终结者区域为748 m,在夜间则为3.7 km。要放样的最大尺寸晶粒的半径R_(max)在终止区域(R_(max)= 0.83μm)达到峰值。在过渡区几乎没有尘埃悬浮。该地区没有月尘造成的危害,因此最适合勘探活动。

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