Prospects for Observing Gravity-gradient Noise and Earthquake Gravity Signals with CHRONOS
使用CHRONOS观测重力梯度噪声和地震重力信号的前景
Mario Juvenal S. Onglao, Yuki Inoue, Daiki Tanabe
AI总结 研究提出使用低温亚赫兹扭摆探测器CHRONOS观测重力梯度噪声和地震瞬态重力信号,通过建模瑞利波、大气次声和地震质量重分布贡献,评估了其灵敏度及对5.2级地震信号的探测能力。
Comments 18 pages, 11 figures
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在亚赫兹频段运行的地基引力波探测器预计将受到环境重力梯度波动(通常称为牛顿噪声NN)的强烈限制。同时,该频段为探测与地震和大气过程相关的地球引力扰动提供了独特机会。本文研究了使用拟议的低温亚赫兹交叉扭摆探测器与量子非破坏速度计(CHRONOS)作为研究重力梯度噪声和探测地震瞬态引力信号的平台的可行性。我们模拟了来自瑞利波诱发地震场、大气次声波动以及地震期间瞬态质量重新分布的重力梯度贡献,并将这些投影到CHRONOS扭摆响应上。CHRONOS在约2 Hz附近达到约1e-18 Hz^(-1/2)的峰值应变灵敏度。发现瑞利波NN在约0.5 Hz以下为主导环境贡献,而大气NN在所考虑的整个频率范围内仍小几个数量级。我们进一步评估了地震瞬态引力信号的可探测性。对于一个代表性的Mw=5.2事件,约90公里内的震源可能产生可探测信号。在40公里距离处,我们在亚赫兹频段上积分得到的信噪比(SNR)约为3.62,相应的应变振幅在0.2至0.6 Hz附近达到CHRONOS灵敏度曲线。预计引力信号比地震P波到达早几秒,具体取决于假设的传播速度。这些结果展示了CHRONOS在亚赫兹频段探测重力梯度噪声和瞬态地球物理重力信号的潜力。
Ground-based gravitational-wave detectors operating in the sub-Hertz regime are expected to be strongly limited by environmental gravity-gradient fluctuations, commonly referred to as Newtonian Noise (NN). At the same time, this frequency band provides unique opportunities to probe terrestrial gravitational perturbations associated with seismic and atmospheric processes. In this work, we investigate the feasibility of using the proposed Cryogenic sub-Hz cROss torsion-bar detector with quantum NOn-demolition speed meter (CHRONOS) as a platform for studying gravity-gradient noise and detecting prompt gravitational signals from earthquakes. We model gravity-gradient contributions from Rayleigh-wave-induced seismic fields, atmospheric infrasound fluctuations, and transient mass redistribution during earthquakes, and project these onto the CHRONOS torsion-bar response. CHRONOS achieves a peak strain sensitivity of order ~1e-18 Hz^(-1/2) near ~2 Hz. Rayleigh-wave NN is found to be the dominant environmental contribution below approximately 0.5 Hz, while atmospheric NN remains several orders of magnitude smaller throughout the frequency range considered. We further assess the detectability of prompt gravitational signals from earthquakes. For a representative Mw = 5.2 event, sources within approximately 90 km may produce detectable signals. At 40 km distance, we obtain a signal-to-noise ratio (SNR) of approximately 3.62 integrated over the sub-Hz band, with a corresponding strain amplitude reaching the CHRONOS sensitivity curve around 0.2 to 0.6 Hz. The gravitational signal is expected to precede seismic P-wave arrival by several seconds, depending on the assumed propagation velocity. These results demonstrate the potential of CHRONOS to probe both gravity-gradient noise and transient geophysical gravity signals in the sub-Hertz regime.