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Study on the Ground-Motion Acceleration Conversion Methods from the horizontal Strain-Rate Array Data of Distributed Acoustic Sensing

수평방향 분산진동센서 변형률 자료의 지반가속도 변환 방법에 대한 연구

  • Yun, Kwan-Hee (Safety Laboratory, Korea Electric Power Corporation (KEPCO) Research Institute) ;
  • Choi, Seunghun (Research Institute of Energy and Resources, Seoul National University) ;
  • Yoon, Byoungjoon (Geological Storage Research Center, Korea Institute of Geoscience and Mineral Resources)
  • 연관희 (한전전력공사 전력연구원 안전연구소 ) ;
  • 최승훈 (서울대학교 에너지자원신기술연구소) ;
  • 윤병준 (한국지질자원연구원 탄소저장연구센터)
  • Received : 2026.03.03
  • Accepted : 2026.04.10
  • Published : 2026.05.01

Abstract

This study evaluates ground-motion (GM) acceleration conversion methods by applying them to strain-rate data from a horizontal Distributed Acoustic Sensing (DAS) array under both idealized and real-world conditions. We test four conversion methods-1) slant-stacking, 2) Lior's method, 3) Lindsey's method, and 4) Curvelet transform-through numerical modeling and by applying them to a publicly available 9 km horizontal DAS array dataset. Numerical simulations reveal critical calculation factors specific to each method and show that numerically derived apparent ground velocity can deviate from theoretical values when multiple elastic waves arrive simultaneously. In real-world applications, the slant-stacking and Lior's methods are relatively insensitive to the measurement length of the straight DAS array. By contrast, the Curvelet method exhibits strong sensitivity to this factor, whereas Lindsey's method shows weaker dependence. Implementing Lior's method in the frequency-wavenumber domain also requires pre-determining water-levels by comparing adjacent seismograms. Additionally, we find that Lior's method generates excessively high spectral levels above 13 Hz, which may lead to underestimation of the high-frequency spectral attenuation parameter (κ0), a key parameter in GM simulation. Collectively, these findings provide a technical guideline for the use of horizontal DAS arrays in future observational earthquake seismology.

Keywords

References

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