New Method to Track Falling Space Debris Using Seismic Sensors
Scientists have recently discovered a groundbreaking way to monitor the uncontrolled reentry of falling space junk. This innovative technique involves utilizing seismic sensors to detect sonic booms created by chunks of space debris entering the Earth’s atmosphere.
Traditionally used to monitor seismic activity on Earth’s surface, these sensors have proven to be effective in tracking the reentry of space debris. Planetary scientist Benjamin Fernando from Johns Hopkins University and engineer Constantinos Charalambous from Imperial College London successfully tested this method during the 2024 reentry of the Shenzhou-15 orbital module.
The data collected by seismic sensors provided precise measurements of the reentry process, including speed, altitude range, size, descent angle, and fragmentation timing of the falling debris. This information offers valuable insights into debris disintegration dynamics, enhancing space situational awareness and debris hazard mitigation efforts.
Space debris poses a growing threat to Earth’s orbit, with approximately 1.2 million potentially hazardous pieces currently in circulation, a number expected to rise as more satellites reach the end of their operational lifespan. Monitoring the reentry of dead spacecraft is crucial as they can collide with other debris or pose risks to aviation and ground-based infrastructure.
The concept of sonic booms generated by falling objects exceeding the speed of sound in the atmosphere is key to this tracking method. As space debris enters Earth’s atmosphere at supersonic velocities, it creates a shock wave known as a Mach cone, which can be detected by seismic sensors originally designed to detect acoustic signals from the Earth’s interior.
During the reentry of the Shenzhou-15 orbital module over southern California, seismic sensors from the Southern California Seismic Network and Nevada Seismic Network captured the module’s passage. Analysis of the data revealed the object’s speed, fragmentation patterns, and final destruction, offering valuable insights into the atmospheric reentry process.
The researchers observed that the module reached speeds of Mach 25 to 30 during reentry, consistent with its pre-entry orbital velocity. The data also indicated a transition from a single large boom signal to multiple smaller boom signals, correlating with ground reports of the object’s fragmentation.
While the module ultimately burned up harmlessly in the atmosphere, this study demonstrates the effectiveness of using seismic sensors to track reentering space debris accurately. This method could prove invaluable in locating potential debris fields for objects that do not completely disintegrate during reentry.
By leveraging publicly available tools like seismic stations, scientists can improve their understanding of how space debris falls and disperses, aiding in hazard assessment and mitigation strategies. While uncontrolled reentries remain a challenge, this research offers a promising way to monitor and analyze these events more effectively.
The findings of this study have been published in the journal Science, highlighting the significance of using seismic sensors for tracking falling space debris.
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