http://arxiv.org/abs/2209.06559
A critical consideration in the design of next generation gravitational wave detectors is isolation from seismic vibrations that introduces various coherent and incoherent noises to the interferometers at different frequencies. We present the results of a detailed low frequency ambient seismic noise characterization (0.1–10~Hz) at Gingin High Optical Power Facility in Western Australia using a seismic array. The dominant noise sources below 1~Hz is microseism (0.06–1~Hz), strongly correlated with swell and sea heights measured by nearby buoy stations. Above 1~Hz, the seismic spectrum is dominated by wind induced seismic noise with a diurnal variation that prevents characterizing the background anthropogenic noise sources based on their daily power variations. We use f-k beamforming to distinguish between coherent and incoherent wind induced seismic noise. This allows the separation of some anthropogenic noise from wind induced noise based on the temporal variation of spatio-spectral properties. We show that the seismic coherency is reduced by wind induced seismic noise for wind speeds above 6~m/s. Furthermore, there are several spectral peaks between 4–9~Hz associated with the interaction of wind with a 40~m tall tower among which one at 4.2~Hz is strongest and coherent. By comparing our results with the properties of seismic noise at Virgo, we demonstrate that while the secondary microseism noise level is two orders of magnitude higher in Gingin (0.2~Hz), the anthropogenic noise level is three orders of magnitude lower between 2 and 4~Hz due to the absence of nearby road traffic. It is also at least one order of magnitude lower between 4 and 10~Hz due to the sparse population in Gingin.
H. Satari, C. Blair, L. Ju, et. al.
Thu, 15 Sep 22
32/67
Comments: The results have been presented at LVK conference, September 2022. 20 pages, 9 figures