Distributed acoustic sensing is shown to cancel seismometer noise with a residual factor near 0.11 at 20 Hz, comparable to geophone arrays, though the evaluation appears to use in-sample Wiener filtering.
Seismic gravity-gradient noise in interferometric gravitational-wave detectors
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Distributed Acoustic Sensing for Environmental Monitoring, and Newtonian Noise Mitigation:Comparable Sensitivity to Seismometers
Distributed acoustic sensing is shown to cancel seismometer noise with a residual factor near 0.11 at 20 Hz, comparable to geophone arrays, though the evaluation appears to use in-sample Wiener filtering.