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雷达对火星次表层的探测与研究现状

Overview of the Martian Subsurface Exploration and Research Using Radar

  • 摘要: 大量火星地貌及表面物质成分的研究表明火星上曾经存在地表水,而目前已探测到的火星上的水广泛存在于极区冰盖和次表层中。近十二年来,欧洲火星快车上搭载的火星次表层和电离层探测先进雷达和美国的火星勘测轨道器上搭载的浅表雷达已经开展了对火星次表层的探测和研究,并取得了一系列科学成果。火星次表层记录着火星形成与演化的重要历史信息。对火星次表层的探测和研究,可以为了解火星的物理特性和构造组成,探寻火星生命,研究火星的地质演化历史提供科学依据。综述目前利用雷达对火星次表层进行的探测和研究,介绍了雷达探测的原理与方法,总结了已取得的科学成果,并展望未来的火星探测雷达。

     

    Abstract: The surface morphology and mineral composition of Mars attest to the past presence of fluid water. Recent research reveals the existence of large amount of water in Mars Polar Caps and subsurface. In the past 12 years, the Martian subsurface has been probed by orbital radar sounders, the Mars Advanced Radar for Subsurface and Ionosphere Sounding (MARSIS) on ESA's Mars Express, and the Shallow Subsurface Radar (SHARAD) on NASA's Mars Reconnaissance Obiter. Both have been successful and obtained a series of scientific achievements. Martian subsurface is believed to have recorded the important massage about the history of Mars. Probing and studying the Martian subsurface could help revealing the formation and revolution of Mars and searching for Martian life. We described the research status about Martian subsurface in this overview, introduced the operation principle of the space-based penetrating radar, and presented the key findings of MARSIS and SHARAD, which have provided a new insight into many aspects of the history and environment of the planet. We also introduced several future Martian subsurface radars in this paper.

     

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