针对扩张状态观测器对二阶及二阶以上系统的扰动观测值存在相位滞后的问题,提出了一种基于扰动频率自适应的自抗扰控制的新方法,并在直线型倒立摆装置中进行了实验验证。实验结果表明:本文方法解决了扩张状态观测器对二阶及二阶以上系...针对扩张状态观测器对二阶及二阶以上系统的扰动观测值存在相位滞后的问题,提出了一种基于扰动频率自适应的自抗扰控制的新方法,并在直线型倒立摆装置中进行了实验验证。实验结果表明:本文方法解决了扩张状态观测器对二阶及二阶以上系统的扰动观测值存在相位滞后的问题;在2 Hz以内随机扰动的作用下,对比传统状态反馈控制器,它将扰动隔离度至少提高了7.85 d B,同时,自抗扰控制器具有很强的鲁棒性,允许被控对象参数在15%的范围内浮动。展开更多
We used high-pass filtering and the Fourier transform to analyze tidal gravity data prior to five earthquakes from four superconducting gravity stations around the world. A stable gravitational perturbation signal is ...We used high-pass filtering and the Fourier transform to analyze tidal gravity data prior to five earthquakes from four superconducting gravity stations around the world. A stable gravitational perturbation signal is received within a few days before the earthquakes. The gravitational perturbation signal before the Wenchuan earthquake on May 12, 2008 has main frequency of 0.1–0.3 Hz, and the other four have frequency bands of 0.12-0.17 Hz and 0.06-0.085 Hz. For earthquakes in continental and oceanic plate fault zones, gravity anomalies often appear on the superconducting gravimeters away from the epicenter, whereas the stations near the epicenter record small or no anomalies. The results suggest that this kind of gravitational perturbation signals correlate with earthquake occurrence, making them potentially useful earthquake predictors. The far-field effect of the gravitational perturbation signals may reveal the interaction mechanisms of the Earth’s tectonic plates. However, owing to the uneven distribution of gravity tide stations, the results need to be further confirmed in the future.展开更多
文摘针对扩张状态观测器对二阶及二阶以上系统的扰动观测值存在相位滞后的问题,提出了一种基于扰动频率自适应的自抗扰控制的新方法,并在直线型倒立摆装置中进行了实验验证。实验结果表明:本文方法解决了扩张状态观测器对二阶及二阶以上系统的扰动观测值存在相位滞后的问题;在2 Hz以内随机扰动的作用下,对比传统状态反馈控制器,它将扰动隔离度至少提高了7.85 d B,同时,自抗扰控制器具有很强的鲁棒性,允许被控对象参数在15%的范围内浮动。
基金supported by the National Science Fund of China Project(Nos.41174104 and 41472301)the Project of Innovation-driven Plan in Central South University(No.2015CX008)
文摘We used high-pass filtering and the Fourier transform to analyze tidal gravity data prior to five earthquakes from four superconducting gravity stations around the world. A stable gravitational perturbation signal is received within a few days before the earthquakes. The gravitational perturbation signal before the Wenchuan earthquake on May 12, 2008 has main frequency of 0.1–0.3 Hz, and the other four have frequency bands of 0.12-0.17 Hz and 0.06-0.085 Hz. For earthquakes in continental and oceanic plate fault zones, gravity anomalies often appear on the superconducting gravimeters away from the epicenter, whereas the stations near the epicenter record small or no anomalies. The results suggest that this kind of gravitational perturbation signals correlate with earthquake occurrence, making them potentially useful earthquake predictors. The far-field effect of the gravitational perturbation signals may reveal the interaction mechanisms of the Earth’s tectonic plates. However, owing to the uneven distribution of gravity tide stations, the results need to be further confirmed in the future.
