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Open Access

Subsurface target recognition in Utopia Planitia of Mars by Tianwen-1 FP-SPR simulation

Ying WANGXuan FENG( )Wenjing LIANGXiaotian LICewen XUE
College of Geo-Exploration Science and Technology, Jilin University, Changchun 130026, China
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Abstract

As a cold and dry planet, Mars contains water resources in the form of water ice, so that the electromagnetic waves can be transmitted to the deep underground to get the information of the topography and subsurface geological structure. Subsurface penetrating radar(SPR) can be widely used in deep space exploration for a long time because of its non-destructive detection mode and its working characteristics not limited by visible light. It is an important type of equipment for detecting the subsurface structure of planets. Orbiter radar is mainly used in Mars exploration. However, because of its low resolution, it is difficult to describe the near surface structure, so there is a lack of radar data which can reflect the shallow information. In this paper, a three-dimensional near surface model of Utopia Planitia on Mars is established. In order to make the simulation results more reasonable, the key factors such as topographic relief, subsurface rocks and water ice, and the variation of dielectric constant in different layers are taken into account. Then the full polarization forward modeling is carried out by using the three-dimensional finite-difference time-domain method. The acquired full polarimetric subsurface penetrating radar(FP-SPR) data with noise is preprocessed and further processed by Pauli decomposition. The underground reflection can be picked up more clearly from the Pauli decomposition results. This work is helpful to identify more details of subsurface structures and provides a reference for the measured data in the future.

References

 

Bandfield J L, Hamilton V E, Christensen P R. 2000. A global view of Martian surface compositions from MGS-TES. Science, 287: 1626-1630.

 

Campbell B A, Shepard M K. 2003. Coherent and incoherent components in near-nadir radar scattering: Applications to radar sounding of Mars. Journal of Geophysical Research (Planets), 108(E12): 5132-5139.

 

Clifford S M, Hillel D. 1983. The stability of ground ice in the equatorial region of Mars. Journal of Geophysical Research (Solid Earth), 88(B3): 2456-2474.

 

Feng X, Yu Y, Liu C, et al. 2015. Subsurface polarimetric migration imaging for full polarimetric ground-penetrating radar. Geophysical journal international, 202(2): 1324-1338.

 

Feng X, Zou L L, Liu C, et al. 2011. Forward modeling for full-polarimetric ground penetrating radar. Chinese Journal of Geophysics Chinese Edition, 54(2): 349-357. (in Chinese with English abstract)

 

Jin Y Q, Fa W Z, Xu F. 2008. Overview of the advance for Mars exploration using microwave remote sensing. Chinese Journal of Space Science, 28(3): 264-272. (in Chinese with English abstract)

 

Leuschen C, Clifford S, Gogineni P. 2003. Simulation of a surface-penetrating radar for Mars exploration. Journal of Geophysical Research (Planets), 108(E4): 8035-8048.

 

Liu C, Ye H X, Jin Y Q. 2014. Simulation of radar echoes from Mars' surface/subsurface and inversion of surface media parameters. Radio Science. 49(7): 473-484.

 

Michael M T, Jakosky B M. 1995. The distribution and behavior of Martian ground ice during past and present epochs. Journal of Geophysical Research (Planets), 100(E6): 11781-11799.

 

Picardi G, Plaut J J, Biccari D, et al. 2005. Radar soundings of the subsurface of Mars. Science, 310: 1925-1928.

 

Piqueux S, Buz J, Edwards C S, et al. 2019. Widespread shallow water ice on Mars at high latitudes and midlatitudes. Geophysical Research Letters. 46: 14290-14298.

 

Plaut J J, Picardi G, Safaeinili A, et al. 2007. Subsurface radar sounding of the south polar layered deposits of Mars. Science, 316: 92-95.

 

Plaut J J, Safaeinili A, Holt J W, et al. 2009. Radar evidence for ice in lobate debris aprons in the mid-northern latitudes of Mars. Geophysical Research Letters, 36(2): 1-4. doi:10.1029/2008GL036379.

 

Seu R, Phillips R J, Alberti G, et al. 2007. Accumulation and erosion of Mars' south polar layered deposits. Science, 317: 1715-1718.

 

Zhang L, Zeng Z F, Li J, et al. 2018. Simulation of the lunar regolith and lunar-penetrating radar data processing. IEEE Journal of Selected Topics in Applied Earth Observations and Remote Sensing, 11(2): 655-663.

 
Zhou B, Shen S X, Ji Y C, et al. 2016. The subsurface penetrating radar on the rover of China's Mars 2020 mission//2016 16th International Conference on Ground Penetrating Radar (GPR), 1-4.
Global Geology
Pages 169-176
Cite this article:
WANG Y, FENG X, LIANG W, et al. Subsurface target recognition in Utopia Planitia of Mars by Tianwen-1 FP-SPR simulation. Global Geology, 2021, 24(3): 169-176. https://doi.org/10.3969/j.issn.1673-9736.2021.03.05

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Received: 20 December 2020
Accepted: 15 January 2021
Published: 25 August 2021
© 2021 GLOBAL GEOLOGY
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