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Sputtering of lunar regolith simulant by protons and singly and multicharged Ar ions at solar wind energies

机译:质子和单电荷和多电荷Ar离子在太阳风能下溅射月球重石模拟物

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We report preliminary results on sputtering of a lunar regolith simulant at room temperature by singly and multiply charged solar wind ions using quadrupole and time-of-flight (TOF) mass spectrometry approaches. Sputtering of the lunar regolith by solar-wind heavy ions may be an important particle source that contributes to the composition of the lunar exosphere, and is a possible mechanism for lunar surface ageing and compositional modification. The measurements were performed in order to assess the relative sputtering efficiency of protons, which are the dominant constituent of the solar wind, and less abundant heavier multicharged solar wind constituents, which have higher physical sputtering yields than same-velocity protons, and whose sputtering yields may be further enhanced due to potential sputtering. Two different target preparation approaches using JSC-1A AGGL lunar regolith simulant are described and compared using SEM and XPS surface analysis.
机译:我们通过使用四极杆和飞行时间(TOF)质谱方法,通过单个和乘以带电的太阳风离子,报告了在室温下溅射月go石模拟物的初步结果。太阳风重离子对月球重石的溅射可能是重要的粒子源,它有助于月球外层的组成,并且是月球表面老化和成分改变的可能机制。进行测量是为了评估质子的相对溅射效率,质子是太阳风的主要成分,质子的相对溅射效率较低,较重的多电荷太阳风成分,质子的溅射率要高于等速质子,并且溅射率较高。由于潜在的溅射,可以进一步增强。描述了两种不同的使用JSC-1A AGGL月球重生石模拟物的目标制备方法,并使用SEM和XPS表面分析进行了比较。

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