Distributed Acoustic Sensing for Environmental Monitoring, and Newtonian Noise Mitigation:Comparable Sensitivity to Seismometers

TL;DR

Distributed acoustic sensing can effectively replace traditional seismometers for Newtonian noise monitoring and mitigation in gravitational wave detectors, offering comparable sensitivity and scalability for environmental noise suppression.

Contribution

This study demonstrates that distributed acoustic sensing provides a scalable, high-performance alternative to seismometers for Newtonian noise cancellation in gravitational wave observatories.

Findings

Distributed acoustic sensing correlates strongly (>0.8) with seismometers in 3-20 Hz range.

DAS accurately predicts geophone signals with correlation above 0.7.

Both DAS and geophones achieve a residual noise factor of 0.11 at 20 Hz in noise cancellation.

Abstract

Newtonian noise limits the low-frequency sensitivity of ground-based gravitational wave detectors. While seismometers and geophones are commonly employed to monitor ground motion for Newtonian noise cancellation, their limited spatial coverage and high deployment costs hinder scalability. In this study, we demonstrate that distributed acoustic sensing offers a viable and scalable alternative, providing performance comparable to that of conventional seismic instruments. Using data from acoustic sensing and colocated seismometers during both natural and controlled events, we observe a strong correlation, exceeding 0.8, between the two sensor types in the 3 to 20 Hz frequency band relevant for Newtonian noise. Moreover, when distributed acoustic sensing data are used to predict geophone signals, the correlation remains high, above 0.7, indicating that distributed acoustic sensing accurately captures both the spatial and spectral features of ground motion. As a case study, we apply distributed acoustic sensing data to cancel noise recorded by the vertical component of a seismometer and compare the results with those obtained using geophone data for the same task. Both distributed acoustic sensing and geophone-based cancellations yield a residual noise factor of 0.11 at 20 Hz. These findings confirm the feasibility of using distributed acoustic sensing for Newtonian noise mitigation and highlight its potential, in combination with traditional seismic sensors, to improve environmental monitoring and noise suppression in current and next-generation gravitational wave observatories.