Seismoacoustic measurements of the OSIRIS-REx re-entry with an off-grid Raspberry PiShake

B. Fernando, Constantinos Charalambous, Christelle Saliby, Eleanor Sansom, Carene Larmat, David Buttsworth, Daniel Hicks, Roy Johnson, Kevin Lewis, Meaghan McCleary, Giuseppe Petricca, Nick Schmerr, Fabian Zander, Jennifer Inman
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Abstract

Hypersonic re-entries of spacecraft are valuable analogues for the identification and tracking of natural meteoroids re-entering the Earth's atmosphere. We report on the detection of seismic and acoustic signals from the OSIRIS-REx landing sequence, acquired near the point of peak capsule heating and recorded using a fully off-grid Raspberry PiShake sensor. This simple setup is able to record all the salient features of both the seismic and acoustic wavefields; including the primary shockwave, later reverberations, and possible locally induced surface waves. Peak overpressures of 0.7~Pa and ground velocities of 2x10$^{-6}$~m/s yield lower bound on the air-to-ground coupling factor between 3 and 44~Hz of 1.4x10$^{-6}$m/s/Pa, comparable to results from other re-entries
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利用离网 Raspberry PiShake 对 OSIRIS-REx 再入大气层进行地震声学测量
对于识别和跟踪重返地球大气层的天然流星体来说,航天器的高超音速重返是一个宝贵的类比。我们报告了对来自 OSIRIS-REx 着陆序列的地震和声学信号的探测,这些信号是在太空舱加热峰值点附近采集的,并使用完全离网的 Raspberry PiShake 传感器进行记录。这种简单的设置能够记录地震波场和声波场的所有显著特征;包括初级冲击波、后期混响以及可能的局部诱导面波。0.7~Pa 的峰值超压和 2x10$^{-6}$~m/s 的地面速度使 3~44~Hz 之间的空地耦合系数下限达到 1.4x10$^{-6}$m/s/Pa,与其他再入大气层的结果相当。
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