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Method for Anisotropic Crystal-Orientation Fabrics Detection Using Radio-Wave Depolarization in Radar Sounding of Mars Polar Layered Deposits

机译:火星极地分层沉积物雷达探测中的无线电波去极化检测各向异性晶体取向织物的方法

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摘要

The polar layered deposits (PLDs) provide a wealth of information about the past climate evolution of Mars. Surface mass fluxes and ice flow mainly governed topography and layering of the PLD. China’s Mars probe including an orbiter and a landing rover will be launched by 2020. A new type satellite-borne Mars penetrating radar instrument has been selected to be a part of the payloads on the orbiter. Its main scientific objectives are to map the distribution of water, water–ice and to detect the soil characteristics at global scale on the Martian crust. Compared with Mars Advanced Radar for Subsurface and Ionospheric Sounding and Shallow Radar, the biggest difference is that the antenna system of this Mars penetrating radar consists of two dipole antennas mutually perpendicular. This special configuration enables the investigation of the ice flow of PLD by detecting and analyzing the features of anisotropic crystal-orientation fabric (COF). Thus, relying on the fact that the radio waves are depolarized while passing through an anisotropic COF layer, in this paper, a method for anisotropic COF detection based on this radar system is proposed. The radar echo formulation of anisotropic COF is derived and the ratio of the signals measured by the two perpendicular antennas is used to analyze the anisotropy of COF. We demonstrate that the ratio is an ideal criterion for the detection and analysis of COF, since it contains all parameters about the anisotropy feature of COF and it is independent of the attenuation in the propagation path and the reflection coefficient. In order to verify the validity of the derived analytical expression of the ratio for the detection of COF, finite-different time-domain simulations are carried out based on a simple model of the subsurface of PLD which contains an anisotropic COF layer. The advantages of this method, the potential application scenarios, and the effects of the Martian environment are also discussed.
机译:极地分层沉积物(PLD)提供了有关火星过去气候演变的大量信息。表面质量通量和冰流主要控制着PLD的地形和分层。中国的火星探测器将在2020年发射升空,包括一个轨道飞行器和一个着陆漫游器。一种新型的星载火星穿透雷达仪器已被选作轨道飞行器有效载荷的一部分。其主要科学目标是绘制水,冰冰的分布图,并在全球范围内探测火星地壳的土壤特征。与用于地下和电离层探测和浅层雷达的火星高级雷达相比,该火星穿透雷达的天线系统由两个互相垂直的偶极天线组成。这种特殊的配置可以通过检测和分析各向异性晶体取向织物(COF)的特性来研究PLD的冰流。因此,基于无线电波在穿过各向异性COF层时被去极化的事实,提出了一种基于该雷达系统的各向异性COF检测方法。推导了各向异性COF的雷达回波公式,并利用两个垂直天线测得的信号比值来分析COF的各向异性。我们证明,该比率是检测和分析COF的理想标准,因为它包含有关COF各向异性特征的所有参数,并且与传播路径中的衰减和反射系数无关。为了验证导出的用于COF检测的比率的解析表达式的有效性,基于包含各向异性COF层的PLD地下的简单模型,进行了有限差分时域模拟。还讨论了该方法的优点,潜在的应用场景以及火星环境的影响。

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  • 作者单位

    Chinese Academy of Sciences, Key Laboratory of Electromagnetic Radiation and Sensing Technology, Institute of Electronics, Beijing, China;

    Chinese Academy of Sciences, Key Laboratory of Electromagnetic Radiation and Sensing Technology, Institute of Electronics, Beijing, China;

    Chinese Academy of Sciences, Key Laboratory of Electromagnetic Radiation and Sensing Technology, Institute of Electronics, Beijing, China;

    Chinese Academy of Sciences, Key Laboratory of Electromagnetic Radiation and Sensing Technology, Institute of Electronics, Beijing, China;

    Chinese Academy of Sciences, Key Laboratory of Electromagnetic Radiation and Sensing Technology, Institute of Electronics, Beijing, China;

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  • 正文语种 eng
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  • 关键词

    Ice; Radar antennas; Anisotropic magnetoresistance; Mars; Spaceborne radar; Surface topography;

    机译:冰;雷达天线;各向异性磁阻;火星;星载雷达;表面形貌;

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