论文标题
随机重力波背景永久存在,并证明了时间域不对称
The stochastic gravitational-wave background exists permanently and demonstrates time-domain asymmetry
论文作者
论文摘要
分析晚期Ligo和处女座重力观测站的记录,我们发现仅固有的永久时间域不对称性仅固有其重力探测器的信号。具有不同周期性信号,高斯和非高斯噪音的实验,可以得出结论,重力探测器的噪声是信号的异常混合物。我们还开发了一个专门的皮尔森相关分析仪来检测引力波(GW)事件。事实证明,LIGO和处女座检测器的输出信号包含一个重要的(-6dB)组件,证明了已确认已解决的GW事件的记录的特性。它使我们可以争辩说,重力背景很大程度上是由于恒星质量合并的过程。由于特定信号是由检测器连续注册的,因此我们可以考虑发现的sub-kilohertz带重力背景场。我们的分析方法还使我们能够估计重力背景成分对总信号能量的贡献。在它的帮助下,不仅有可能提供重力干扰大小的射频估计,而且还可以获得GW背景天图。
Analyzing the records of Advanced LIGO and Virgo gravitational observatories, we found a permanent time-domain asymmetry inherent only to the signals of their gravitational detectors. Experiments with different periodic signals, Gaussian and non-Gaussian noises, made it possible to conclude that the noise of gravitational detectors is an unusual mixture of signals. We also developed a specialized Pearson correlation analyzer to detect gravitational-wave (GW) events. It turned out that the LIGO and Virgo detectors' output signals contain a significant (-6dB) component demonstrating the properties of records of confirmed resolved GW events. It allows us to argue that the gravitational background is largely due to the processes of stellar masses merging. Since the specific signal is registered by the detectors continuously, we can consider the sub-kilohertz band gravitational background field as discovered. Our analysis method also allows us to estimate the contribution of the gravitational background component to the total signal energy. With its help, it will be possible not only to provide the radio-frequency estimation of the magnitude of gravitational disturbances but also to obtain the GW background sky map.