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Microwave tomography for Lunar Penetrating Radar data processing in Chang'e 4 mission
Francesco Soldovieri1, Gianluca Gennarelli2, Yan Su3,4
1Institute for Electromagnetic Sensing of the Environment (IREA)-National Research Council of Italy (CNR), Naples, 80128, Italy. soldovieri.f@irea.cnr.it.
Scientific Reports
|February 12, 2025
Summary
Researchers used microwave tomography to analyze Lunar Penetrating Radar data from the Yutu-2 rover. This revealed interesting subsurface geological features on the Moon, consistent with prior studies.
Area of Science:
- Planetary Science
- Geophysics
- Radar Remote Sensing
Background:
- The Chang'e 4 mission's Yutu-2 rover utilizes the Lunar Penetrating Radar (LPR) to study the lunar subsurface.
- Interpreting LPR data requires advanced signal processing to overcome noise and computational challenges.
Purpose of the Study:
- To apply a microwave tomographic approach to LPR data for enhanced subsurface imaging.
- To compare two distinct tomographic methods for modeling signal propagation at the lunar air-soil interface.
Main Methods:
- A two-step signal processing pipeline was employed, including time-domain pre-processing for noise and clutter reduction.
- Microwave tomography was utilized to address computational issues associated with the large probing domain.
- Two tomographic approaches differing in air-soil interface propagation modeling were evaluated.
Main Results:
- Tomographic images were generated along a 1340 m traverse route.
- The images successfully identified significant subsurface geometrical features.
- These findings align with geological interpretations from previous research.
Conclusions:
- Microwave tomography is an effective technique for analyzing Lunar Penetrating Radar data.
- The study confirms the presence of complex subsurface structures on the Moon.
- The results support and enhance existing geological models of the Chang'e 4 landing site.

