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Numerical Simulations of the Lunar Penetrating Radar and Investigations of the Geological Structures of the Lunar Regolith Layer at the Chang'E 3 Landing Site

机译:'娥三号着陆点月球穿透雷达的数值模拟和月球go石层的地质结构研究

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摘要

In the process of lunar exploration, and specifically when studying lunar surface structure and thickness, the established lunar regolith model is usually a uniform and ideal structural model, which is not well-suited to describe the real structure of the lunar regolith layer. The present study aims to explain the geological structural information contained in the channel 2 LPR (lunar penetrating radar) data. In this paper, the random medium theory and Apollo drilling core data are used to construct a modeling method based on discrete heterogeneous random media, and the simulation data are processed and collected by the electromagnetic numerical method FDTD (finite-difference time domain). When comparing the LPR data with the simulated data, the heterogeneous random medium model is more consistent with the actual distribution of the media in the lunar regolith layer. It is indicated that the interior structure of the lunar regolith layer at the landing site is not a pure lunar regolith medium but rather a regolith-rock mixture, with rocks of different sizes and shapes. Finally, several reasons are given to explain the formation of the geological structures of the lunar regolith layer at the Chang'E 3 landing site, as well as the possible geological stratification structure.
机译:在月球探测过程中,特别是在研究月球表面结构和厚度时,通常建立的月球白垩纪模型通常是一个统一的理想结构模型,不适合描述月球白垩纪层的真实结构。本研究旨在解释通道2 LPR(月球穿透雷达)数据中包含的地质结构信息。本文利用随机介质理论和阿波罗钻井岩心数据构建了基于离散异质随机介质的建模方法,并通过电磁数值方法FDTD(时差有限域)对模拟数据进行处理和收集。当将LPR数据与模拟数据进行比较时,异质随机介质模型与月球变质层中介质的实际分布更加一致。结果表明,登陆点月球re石层的内部结构不是纯粹的月球go石介质,而是具有不同大小和形状的岩石的re石-岩石混合物。最后,给出了解释reasons娥三号登陆点月球长石层地质结构的原因,以及可能的地质分层结构。

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  • 来源
    《International journal of antennas and propagation》 |2017年第2期|3013249.1-3013249.11|共11页
  • 作者单位

    Chinese Acad Sci, Key Lab Lunar & Deep Space Explorat, Beijing 100012, Peoples R China|Chinese Acad Sci, Natl Astron Observ, Beijing 100012, Peoples R China|Univ Chinese Acad Sci, Beijing 100049, Peoples R China;

    Chinese Acad Sci, Key Lab Lunar & Deep Space Explorat, Beijing 100012, Peoples R China|Chinese Acad Sci, Natl Astron Observ, Beijing 100012, Peoples R China;

    Chinese Acad Sci, Key Lab Lunar & Deep Space Explorat, Beijing 100012, Peoples R China|Chinese Acad Sci, Natl Astron Observ, Beijing 100012, Peoples R China;

    Chinese Acad Sci, Key Lab Lunar & Deep Space Explorat, Beijing 100012, Peoples R China|Chinese Acad Sci, Natl Astron Observ, Beijing 100012, Peoples R China;

    Chinese Acad Sci, Key Lab Lunar & Deep Space Explorat, Beijing 100012, Peoples R China|Chinese Acad Sci, Natl Astron Observ, Beijing 100012, Peoples R China|Univ Chinese Acad Sci, Beijing 100049, Peoples R China;

    Chinese Acad Sci, Key Lab Lunar & Deep Space Explorat, Beijing 100012, Peoples R China|Chinese Acad Sci, Natl Astron Observ, Beijing 100012, Peoples R China;

    Renmin Univ China, Beijing 100872, Peoples R China;

    Chinese Acad Sci, Key Lab Lunar & Deep Space Explorat, Beijing 100012, Peoples R China|Chinese Acad Sci, Natl Astron Observ, Beijing 100012, Peoples R China;

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