We apply ambient noise tomography to significant seismic data resources in a region including the northeastern Tibetan plateau, the Ordos block and the Sichuan basin. The seismic data come from about 160 stations of t...We apply ambient noise tomography to significant seismic data resources in a region including the northeastern Tibetan plateau, the Ordos block and the Sichuan basin. The seismic data come from about 160 stations of the provincial broadband digital seismograph networks of China. Ambient noise cross-correlations are performed on the data recorded between 2007 and 2009 and high quality inter-station Rayleigh phase velocity dispersion curves are obtained between periods of 6 s to 35 s. Resulting Rayleigh wave phase velocity maps possess a lateral resolution between 100 km and 200 kin. The phase velocities at short periods （〈20 s） are lower in the Sichuan basin, the northwest segment of the Ordos block and the Weihe graben, and outline sedimentary deposits. At intermediate and long periods （〉25 s）, strong high velocity anomalies are observed within the Ordos block and the Sichuan basin and low phase velocities are imaged in the northeastern Tibetan plateau, reflecting the variation of crustal thickness from the Tibetan plateau to the neighboring regions in the east. Crustal and uppermost mantle shear wave velocities vary strongly between the Tibetan plateau, the Sichuan basin and the Ordos block. The Ordos block and the Sichuan basin are dominated by high shear wave velocities in the crust and uppermost mantle. There is a triangle-shaped low velocity zone located in the northeastern Tibetan plateau, whose width narrows towards the eastern margin of the plateau. No low velocity zone is apparent beneath the Qinling orogen, suggesting that mass may not be able to flow eastward through the boundary between the Ordos block and the Sichuan basin in the crust and uppermost mantle.展开更多
电力电缆局部放电检测是诊断电缆绝缘状态的有效手段。针对传统时延估计局部放电定位方法中定位精度较低的问题,在互相关算法的基础上考虑电缆相速度的频变特性,利用电缆相速度对局放信号相位差进行修正。该方法不仅保留了互相关算法具...电力电缆局部放电检测是诊断电缆绝缘状态的有效手段。针对传统时延估计局部放电定位方法中定位精度较低的问题,在互相关算法的基础上考虑电缆相速度的频变特性,利用电缆相速度对局放信号相位差进行修正。该方法不仅保留了互相关算法具有的抗噪性能,而且通过对局放信号相位差进行修正后,定位精度明显提高。首先,通过MATLAB搭建电缆仿真模型对不同信噪比和不同位置下的局放源进行定位,然后在实验室一条长为498 m长的10 k V XLPE电缆上利用振荡波局部放电测试系统进行局部放电定位实验,对该方法的可行性进行了验证。仿真和实测结果表明,利用相速度对局放信号相位差进行修正后,定位精度明显提高,并且定位结果对不同位置的局放源具有较好的鲁棒性,同时该方法在较低信噪比（-5 dB）下也能达到较小的定位误差。展开更多
基金supported by Chinese Academy of Sciences grant kzcx2-yw-142 and Y009021002National Natural Science Foundation of China under grant No. 40974034+1 种基金NSF-EAR award 0944022NSF-OISE 0730154 at the University of Colorado at Boulder
文摘We apply ambient noise tomography to significant seismic data resources in a region including the northeastern Tibetan plateau, the Ordos block and the Sichuan basin. The seismic data come from about 160 stations of the provincial broadband digital seismograph networks of China. Ambient noise cross-correlations are performed on the data recorded between 2007 and 2009 and high quality inter-station Rayleigh phase velocity dispersion curves are obtained between periods of 6 s to 35 s. Resulting Rayleigh wave phase velocity maps possess a lateral resolution between 100 km and 200 kin. The phase velocities at short periods （〈20 s） are lower in the Sichuan basin, the northwest segment of the Ordos block and the Weihe graben, and outline sedimentary deposits. At intermediate and long periods （〉25 s）, strong high velocity anomalies are observed within the Ordos block and the Sichuan basin and low phase velocities are imaged in the northeastern Tibetan plateau, reflecting the variation of crustal thickness from the Tibetan plateau to the neighboring regions in the east. Crustal and uppermost mantle shear wave velocities vary strongly between the Tibetan plateau, the Sichuan basin and the Ordos block. The Ordos block and the Sichuan basin are dominated by high shear wave velocities in the crust and uppermost mantle. There is a triangle-shaped low velocity zone located in the northeastern Tibetan plateau, whose width narrows towards the eastern margin of the plateau. No low velocity zone is apparent beneath the Qinling orogen, suggesting that mass may not be able to flow eastward through the boundary between the Ordos block and the Sichuan basin in the crust and uppermost mantle.
文摘电力电缆局部放电检测是诊断电缆绝缘状态的有效手段。针对传统时延估计局部放电定位方法中定位精度较低的问题,在互相关算法的基础上考虑电缆相速度的频变特性,利用电缆相速度对局放信号相位差进行修正。该方法不仅保留了互相关算法具有的抗噪性能,而且通过对局放信号相位差进行修正后,定位精度明显提高。首先,通过MATLAB搭建电缆仿真模型对不同信噪比和不同位置下的局放源进行定位,然后在实验室一条长为498 m长的10 k V XLPE电缆上利用振荡波局部放电测试系统进行局部放电定位实验,对该方法的可行性进行了验证。仿真和实测结果表明,利用相速度对局放信号相位差进行修正后,定位精度明显提高,并且定位结果对不同位置的局放源具有较好的鲁棒性,同时该方法在较低信噪比（-5 dB）下也能达到较小的定位误差。
