Subsurface imaging with a voice-coil portable active seismic source and a single geophone: From field validation to lunar application

• Voice-coil portable active seismic source (PASS) for lunar subsurface imaging. • PASS enables continuous signals, enhancing S/N for both body and surface waves. • 2D/3D S-wave velocity profiles (∼7m depth) derived from surface-wave analysis. • P-wave tomography and reflection imaging resolve subsurface structures to ∼80 m. • Space-qualified PASS supports astronaut and rover deployment in future missions. To image and characterize the lunar subsurface, we have developed an active seismic exploration system that combines a single ultra-compact seismic source with a single geophone. The seismic source employs a voice-coil actuator, a type of linear electromagnetic motor, which minimizes the source mass while maintaining a nearly constant force of ∼10 N over a wide frequency range. Despite its compact size of less than 800 g, the source can emit seismic signals repeatedly. Stacking the repeated signals enhances the signal-to-noise ratio, allowing both body-wave and surface-wave propagation over source–receiver distances exceeding 60 m, as demonstrated in field tests at Mount Fuji. When the seismic source is operated at multiple locations around a fixed geophone, astronauts or rovers can acquire multichannel-equivalent seismic datasets. This configuration enables retrieval of 2D or 3D S-wave velocity profiles to depths of ∼7 m through surface-wave analysis. In contrast, when both the seismic source and the geophone are mounted on separate rovers and moved independently, the system allows flexible multi-shot and multi-receiver acquisition geometries. This configuration enables body-wave-based seismic refraction and reflection surveys, allowing refraction tomography to derive 2D P-wave velocity models and reflection analysis to image subsurface structures to depths of ∼80 m. Finally, we optimized these systems and adapted them for space applications, enabling deployment by astronauts and integration with rovers in future space missions.

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Publication Details

Journal
Advances in Space Research
Published
2026-02-16
DOI
https://doi.org/10.1016/j.asr.2026.02.037
Primary Topic
Planetary Science and Exploration
Type
article
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article

Subsurface imaging with a voice-coil portable active seismic source and a single geophone: From field validation to lunar application

Arata Kioka, Hitoshi Tsukahara, Tarek Imam, Kimiaki Ochi et al.
Advances in Space Research
Planetary Science and Exploration
article

Subsurface imaging with a voice-coil portable active seismic source and a single geophone: From field validation to lunar application

Arata Kioka, Hitoshi Tsukahara, Tarek Imam, Kimiaki Ochi, Fumitoshi Murakami, Kazutoshi Sakamoto, Yuya Takenaka, Satoshi Tanaka, Susumu Abe, Taichi Kawamura, Takeshi Tsuji
article en

Abstract

• Voice-coil portable active seismic source (PASS) for lunar subsurface imaging. • PASS enables continuous signals, enhancing S/N for both body and surface waves. • 2D/3D S-wave velocity profiles (∼7m depth) derived from surface-wave analysis. • P-wave tomography and reflection imaging resolve subsurface structures to ∼80 m. • Space-qualified PASS supports astronaut and rover deployment in future missions. To image and characterize the lunar subsurface, we have developed an active seismic exploration system that combines a single ultra-compact seismic source with a single geophone. The seismic source employs a voice-coil actuator, a type of linear electromagnetic motor, which minimizes the source mass while maintaining a nearly constant force of ∼10 N over a wide frequency range. Despite its compact size of less than 800 g, the source can emit seismic signals repeatedly. Stacking the repeated signals enhances the signal-to-noise ratio, allowing both body-wave and surface-wave propagation over source–receiver distances exceeding 60 m, as demonstrated in field tests at Mount Fuji. When the seismic source is operated at multiple locations around a fixed geophone, astronauts or rovers can acquire multichannel-equivalent seismic datasets. This configuration enables retrieval of 2D or 3D S-wave velocity profiles to depths of ∼7 m through surface-wave analysis. In contrast, when both the seismic source and the geophone are mounted on separate rovers and moved independently, the system allows flexible multi-shot and multi-receiver acquisition geometries. This configuration enables body-wave-based seismic refraction and reflection surveys, allowing refraction tomography to derive 2D P-wave velocity models and reflection analysis to image subsurface structures to depths of ∼80 m. Finally, we optimized these systems and adapted them for space applications, enabling deployment by astronauts and integration with rovers in future space missions.

Advances in Space ResearchVol. 77(7)
Institut de physique du globe de Paris (FR), Japan Aerospace Exploration Agency (JP), Institute of Space and Astronautical Science (JP), The University of Tokyo (JP)
Openalex Percentile: Top 53%
Planetary Science and Exploration
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