Investigating the Martian soil at the InSight landing site

P. Delage, B. Caicedo, Matt Golombek, T. Spohn, C. Schmelzbach, N. Brinkman, E. Marteau, Naomi Murdoch, Nicholas Warner, V. Ansan, B. Banerdt, Juan-Pablo Castillo-Betancourt, P. Edme, Annabel Gomez, M. Grott, Ken Hurst, M. Lemmon, Philippe Lognonné, S. Piqueux, J. Robertsson, D. Sollberger, S. Stähler, N. Verdier, Christos Vrettos, Nathan Williams
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Abstract

The InSight mission is a geophysical mission aimed at better understanding the structure of Mars and of the other rocky planets of the solar system. To do so, a lander accommodating two cameras, a very sensitive seismometer, and a dynamic self-penetrating heat probe nicknamed the mole were placed on the Mars surface by the Instrument Deployment Arm (IDA). Besides geophysical data (which definitely enriched the existing knowledge on the structure of Mars), the InSight instruments significantly increased the knowledge of the geological and geotechnical characteristics of the surface material at the InSight site. Small strain (elastic) parameters were derived from wave velocity measurements during the hammering sessions between the self-penetrating probe and the seismometer. A detailed observation of the soil profile along a depth of 37 cm was made possible thanks to the photos taken by the cameras, and to a detailed analysis of the mole penetration process. Further information was provided by an intense campaign of scraping and piling conducted by the IDA on the surface sand/dust layer. It was shown that the soil profile was composed of a surface 1 cm thick sand/dust layer, overlaying an around 20 cm thick loose duricrust made up of a cohesive matrix containing some pebbles, located above a 12 cm layer of sand overlaying a gravel/sand deposit. It is believed that the geology and soil mechanics data provided by the InSight mission will help for further robotic exploration of Mars.
在InSight着陆点调查火星土壤
InSight任务是一项地球物理任务,旨在更好地了解火星和太阳系其他岩质行星的结构。为此,通过仪器部署臂(IDA)在火星表面放置了一个装有两台照相机的着陆器、一个非常灵敏的地震仪和一个绰号为 "鼹鼠 "的动态自穿透热探测器。除了地球物理数据(这些数据无疑丰富了现有的火星结构知识),InSight 仪器还大大增加了对 InSight 所在地表层材料的地质和岩土特性的了解。在自穿透探测器和地震仪之间的锤击过程中,通过波速测量得出了小应变(弹性)参数。通过照相机拍摄的照片和对鼹鼠穿透过程的详细分析,可以对 37 厘米深的土壤剖面进行详细观察。国际大地测量协会(IDA)对表层沙尘层进行的密集刮削和打桩活动提供了进一步的信息。结果表明,土壤剖面是由表面 1 厘米厚的沙尘层和约 20 厘米厚的松散硬壳层组成,硬壳层由含有一些卵石的粘性基质构成,上面是 12 厘米厚的沙层和砾石/沙沉积层。相信 "洞察 "号任务提供的地质和土壤力学数据将有助于机器人对火星的进一步探索。
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