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Investigation of Infrasound Background Noise at Mátra Gravitational and Geophysical Laboratory (MGGL)

机译:Mátra引力和地球物理实验室对浅层背景噪声的调查(MGGL)

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Infrasound and seismic waves are supposed to be the main contributors to the gravity-gradient noise (Newtonian noise) of the third-generation subterranean gravitational wave detectors. This noise will limit the sensitivity of the instrument at frequencies below 20 Hz. Investigation of its origin and the possible methods of mitigation have top priority during the designing period of the detectors. Therefore, long-term site characterizing measurements are needed at several subterranean sites. However, at some sites, mining activities can occur. These activities can cause sudden changes (transients) in the measured signal, and increase the continuous background noise, too. We have developed an algorithm based on discrete Haar transform to find these transients in the infrasound signal. We found that eliminating the transients decreases the variation of the noise spectra, and therefore results a more accurate characterization of the continuous background noise. We carried out experiments for controlling the continuous noise. Machines operating at the mine were turned on and off systematically in order to see their effect on the noise spectra. These experiments showed that the main contributor of the continuous noise is the ventilation system of the mine. We also estimated the contribution of infrasound Newtonian noise at MGGL to the strain noise of a subterranean GW detector similar to Einstein Telescope.
机译:基础和地震波应该是第三代地区重力波检测器的重力梯度噪声(牛顿噪声)的主要贡献者。这种噪声将限制仪器在20 Hz以下频率下的灵敏度。调查其起源和可能的缓解方法在探测器的设计期间具有最优先权。因此,在几个地下站点需要长期站点表征测量。但是,在某些地点,可能发生采矿活动。这些活动可能导致测量信号中的突然变化(瞬态),也增加了连续的背景噪声。我们已经开发了一种基于离散哈尔变换的算法,以在InfraSound信号中找到这些瞬态。我们发现消除瞬变降低了噪声光谱的变化,因此导致更准确地表征连续背景噪声。我们对控制连续噪声进行了实验。在矿井操作的机器系统地打开和关闭,以便看到它们对噪声光谱的影响。这些实验表明,连续噪声的主要贡献者是矿井的通风系统。我们还估计了基于MGGL对MGGL噪声的贡献,以类似于爱因斯坦望远镜的地下GW探测器的应变噪声。

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