Ambient noise interferometry using chirped-pulse DAS data for subsurface exploration

This study demonstrates the potential of Chirped-Pulse Distributed Acoustic Sensing (DAS) technology for subsurface imaging through the application of Ambient Noise Interferometry (ANI). By analyzing strain data, we successfully extracted geological insights without relying on active seismic sources. The low-intensity signals were isolated and enhanced using ANI techniques such as FK filtering, temporal normalization and spectral whitening. Using a custom ANI algorithm, velocity dispersion maps were generated from 24 hours of continuous DAS recordings. These maps revealed dispersion relationships corresponding to different terrain layers. The methodology employed, including Phase-Weighted Stacking and slant-stacking, proved effective for reducing noise and isolating surface wave propagation signals within the frequency range of 0.5–15 Hz. This versatile and cost-effective approach is well-suited for high-resolution, non-invasive subsurface imaging in diverse environments, from submarine cables to urban settings.

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Published
2025-05-22
DOI
https://doi.org/10.1117/12.3062853
Primary Topic
Seismic Waves and Analysis
Type
article
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article

Ambient noise interferometry using chirped-pulse DAS data for subsurface exploration

Pascual Sevillano, Hugo Fidalgo Martins, Jesús Subías, Miguel González‐Herráez et al.
Seismic Waves and Analysis
article

Ambient noise interferometry using chirped-pulse DAS data for subsurface exploration

Pascual Sevillano, Hugo Fidalgo Martins, Jesús Subías, Miguel González‐Herráez, Javier Preciado-Garbayo, Jorge Canudo, Beatriz Gaite-Castrillo, José Benito Bravo-Monge, Irene de María, Miguel Rodrigez-Plaza
article en

Abstract

This study demonstrates the potential of Chirped-Pulse Distributed Acoustic Sensing (DAS) technology for subsurface imaging through the application of Ambient Noise Interferometry (ANI). By analyzing strain data, we successfully extracted geological insights without relying on active seismic sources. The low-intensity signals were isolated and enhanced using ANI techniques such as FK filtering, temporal normalization and spectral whitening. Using a custom ANI algorithm, velocity dispersion maps were generated from 24 hours of continuous DAS recordings. These maps revealed dispersion relationships corresponding to different terrain layers. The methodology employed, including Phase-Weighted Stacking and slant-stacking, proved effective for reducing noise and isolating surface wave propagation signals within the frequency range of 0.5–15 Hz. This versatile and cost-effective approach is well-suited for high-resolution, non-invasive subsurface imaging in diverse environments, from submarine cables to urban settings.

Universidad de Alcalá (ES), Universidad de Zaragoza (ES), Servicio Aragonés de Salud (ES), Abertis Infraestructuras (Spain) (ES), Instituto Geográfico Nacional (ES)
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Seismic Waves and Analysis
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