Simulation for ground penetrating radar (GPR) study of the subsurface structure of the Moon

被引:29
作者
Fa, Wenzhe [1 ]
机构
[1] Peking Univ, Inst Remote Sensing & Geog Informat Syst, Beijing 100871, Peoples R China
基金
中国国家自然科学基金; 国家高技术研究发展计划(863计划);
关键词
Modeling and simulation; Subsurface structure; GPR echo; Inversion; Moon; LASER ALTIMETER; LUNAR; THICKNESS; SOUNDER; MARIA;
D O I
10.1016/j.jappgeo.2013.08.002
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Ground penetrating radar (GPR) is currently within the scope of China's Chang-E 3 lunar mission, to study the shallow subsurface of the Moon. In this study, key factors that could affect a lunar GPR performance, such as frequency, range resolution, and antenna directivity, are discussed firstly. Geometrical optics and ray tracing techniques are used to model GPR echoes, considering the transmission, attenuation, reflection, geometrical spreading of radar waves, and the antenna directivity. The influence on A-scope GPR echoes and on the simulated radargrams for the Sinus Iridum region by surface and subsurface roughness, dielectric loss of the lunar regolith, radar frequency and bandwidth, and the distance between the transmit and receive antennas are discussed. Finally, potential scientific return about lunar subsurface properties from GPR echoes is also discussed. Simulation results suggest that subsurface structure from several to hundreds of meters can be studied from GPR echoes at P and VHF bands, and information about dielectric permittivity and thickness of subsurface layers can be estimated from GPR echoes in combination with regolith composition data. (C) 2013 Elsevier B.V. All rights reserved.
引用
收藏
页码:98 / 108
页数:11
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