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中国物理学会期刊

“嫦娥5号”登陆候选地Mons Rümker的光照与温度特征分析

CSTR: 32037.14.aps.69.20200114

Illumination and temperature analysis for CE-5 candidate landing site Mons Rümker

CSTR: 32037.14.aps.69.20200114
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  • 即将开展的“嫦娥5号”探月任务, 将使我国在月球上首次实现无人钻井取样. 考虑到实际探测活动与探测区域的光照和温度有关, 有必要对研究区域的光照和温度特征进行分析, 为此, 本文利用SPICE系统对“嫦娥5号”候选登陆区Mons Rümker高原的实时光照进行计算. 发现求解的相对光强度分布与日本SELENE卫星提供的早晨光照影像一致, 验证了光照算法及计算程序的合理性. 以此为基础, 利用1维热传导模型, 对候选登陆区风化层不同深度的温度进行仿真分析. 结果表明风化层温度在近表面区域受光照的影响较大, 随着深度的增加, 光照影响逐渐减弱. 到达0.57 m深度时, 风化层温度不再变化. 为确保钻井任务的开展, 实际钻井作业应考虑风化层内外温度差异引起的应力不均. 考虑“嫦娥5号”的实际钻井深度远大于0.57 m, 应能测量到常温层的热流值, 后续探月任务可考虑搭载热流探测设备, 以促进月球科学研究的发展.

     

    The forthcoming lunar exploration of Chang’e-5 (CE-5) mission will be the first sampling return project of China. The actual drilling needs the information about real-time illumination and corresponding temperature. To give a support for the project, in this paper the SPICE software system is first used to calculate the real-time illumination at the CE-5 candidate landing site Mons Rümker. It is found that our synthetic map of illumination is consistent with the morning map of illumination provided by the Japan’s SELENE satellite. This result verifies the rationality of our algorithm and the corresponding code. According to the calculated illumination and considering a one-dimensional heat conduction model, we study the temperature distribution over Mons Rümker. It is found that the regolith temperature near the surface is greatly related to the illumination, but varies a little with the depth increasing. It is also discovered that the regolith temperature beneath a depth of 0.57 m will not change any more. To give a support for the actual drilling program, it is recommended to consider the temperature difference between the outside and inside of the regolith, especially their stresses caused by such a temperature difference. Moreover, considering the drilling depth of CE-5 larger than 0.57 m, it is likely to measure the heat flow for the constant-temperature layer. We propose that for the next lunar exploration following CE-5 the measurement of heat flow is considered. This will promote the research of lunar science.

     

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