中国嫦娥三号月球车上的探月雷达初步结果

Yan Su, S. Xing, Jianqing Feng, S. Dai, Yuanzheng Xiao, Lei Zheng, Chunlai Li
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引用次数: 3

摘要

中国嫦娥三号于2013年12月2日发射,并成功登陆月球。月球车成功地从着陆器上部署,并于12月14日触及月球表面。嫦娥三号月球车上的有效载荷之一是月球探地雷达(LPR),旨在以60兆赫和500兆赫的频率通道观测月球地下地质。LPR工作了271分36秒,在60MHz下获得9960个航迹数据,在500MHz下获得19538个航迹数据,直到2014年1月1日1019 UTC。漫游车行走时间31分37秒,行走距离102.8m,雷达数据总量318MB。60MHz LPR初步结果显示,~208m和~328m深度有2层,可认为是海玄武岩沉积休止期积累的隐伏风化层。500MHz的结果显示,风化层约为4-6m,与我们的估计一致。
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The preliminary results of lunar penetrating radar on board the Chinese Chang'e-3 rover
Chinese Chang'e-3 was launched on 2nd December 2013, and it has successfully landed on the moon. The rover was successfully deployed from the lander, and touched the lunar surface on 14 December. One of the payloads on board the Chang'e-3 rover is the Lunar ground-Penetrating Radar (LPR), aimed at observing the lunar subsurface geology at frequency channels of 60MHz and 500MHz. The LPR has worked for 271minutes and 36 seconds to obtain 9960 track data at 60MHz and 19538 track data at 500MHz till 1019 on 1st Jan. 2014 UTC. The rover walking time was 31 minutes and 37 seconds with walking distance of 102.8m, and the total amount of the radar data is 318MB. The LPR preliminary results of 60MHz reveals two layers at the depths of ~208m and ~328m, which are considered as the buried regolith layers accumulated during depositional hiatus of mare basalts. The results of 500MHz displays the regolith is about 4-6m, which is consistent with our estimation.
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