首先介绍了中压电力线信道噪声通用模型,对现场采集的噪声进行互相关系数计算,并采用对称分量法进行相关性分析,得出三相电力系统相间噪声具有一定相关性的结论。改变单相传输模式,根据两相噪声的一致性特点,提出基于自适应最小均方误差...首先介绍了中压电力线信道噪声通用模型,对现场采集的噪声进行互相关系数计算,并采用对称分量法进行相关性分析,得出三相电力系统相间噪声具有一定相关性的结论。改变单相传输模式,根据两相噪声的一致性特点,提出基于自适应最小均方误差(least-mean-square error,LMS)算法实现中压电力线通信(medium voltage power line communication,MV-PLC)的噪声对消。自适应LMS算法虽然收敛速度较慢,但是计算量小,易于实现。仿真结果表明,噪声对消方法的采用有效改善了10kV中压电力线的信噪比,为10kV配网自动化系统采用载波通信技术提供了新的实现途径。展开更多
The Haicheng earthquake （Ms 7.3） occurred in Liaoning Province （39°N-43°N, 120°E-126°E ）, China on February 4, 1975. The mortality rate was only 0.02% owing to the first timely and accurate pre...The Haicheng earthquake （Ms 7.3） occurred in Liaoning Province （39°N-43°N, 120°E-126°E ）, China on February 4, 1975. The mortality rate was only 0.02% owing to the first timely and accurate prediction, although the area affected by the earthquake was 9200 km^2 and covered cities with a population density of 1000 p/km^2. In this study, the double- difference （DD） tomography method was used to obtain high-resolution three-dimensional （3D） P- and S-wave velocity （Vp and Vs） structures and Vp/Vs as well as the earthquake locations. Tomography results suggest that velocity structure at shallow depth coincides well with topography and sediment thickness. The earthquake locations form a northwest-striking zone associated with the Jinzhou（JZ） Fault and a northeast-striking zone associated with the Haichenghe-Dayanghe （HD） Fault, and suggest that the JZ Fault consists of three faults and the Ms 7.3 Haicheng earthquake originated at the intersection of the JZ and the Faults. Low- velocity zones （LVZs） with low Vp/Vs are observed at 15-20 km depth beneath the Haicheng （HC） region. We interpret the LVZs in the middle crust as regions of fluids, suggesting rock dehydration at high temperatures. The LVZs and low Vp/Vs in the upper crust are attributed to groundwater-filled cracks and pores. We believe that large crustal earthquakes in this area are caused by the combination of faulting and fluid movement in the middle crust.展开更多
由于受到台站分布不理想、速度结构研究不准确以及震相拾取误差等因素的影响，常规地震定位结果精度较低。因此，研究收集了辽宁省地震台网的地震目录及震相数据，采用双差地震定位方法，对海城及其附近地区（39°N —43°N，12...由于受到台站分布不理想、速度结构研究不准确以及震相拾取误差等因素的影响，常规地震定位结果精度较低。因此，研究收集了辽宁省地震台网的地震目录及震相数据，采用双差地震定位方法，对海城及其附近地区（39°N —43°N，120°E— 126°E）20 a 的1400多次地震进行重新定位。与原始定位结果相比，双差定位结果表明：1）震中更加呈条带状集中，尤其在40．5°N —41．0°N，122．0°E—123．0°E 区间，与该地区的海城河大洋河断裂带走向相一致；2）该地区地震多发生于地下5～20 km，与该区中地壳存在的低速高导层相对应；3）深度剖面图显示，大部分地震沿垂直向下柱状分布，原因是该处有粉碎性破裂带，从地下25 km 处延伸到近地表。双差定位算法使得定位后均方根残差的平均值由0．74 s 下降到0．26 s。辽宁地区的地震震级与发生地震数量有关，地震数量陡然增多，大地震发生概率增大。展开更多
文摘首先介绍了中压电力线信道噪声通用模型,对现场采集的噪声进行互相关系数计算,并采用对称分量法进行相关性分析,得出三相电力系统相间噪声具有一定相关性的结论。改变单相传输模式,根据两相噪声的一致性特点,提出基于自适应最小均方误差(least-mean-square error,LMS)算法实现中压电力线通信(medium voltage power line communication,MV-PLC)的噪声对消。自适应LMS算法虽然收敛速度较慢,但是计算量小,易于实现。仿真结果表明,噪声对消方法的采用有效改善了10kV中压电力线的信噪比,为10kV配网自动化系统采用载波通信技术提供了新的实现途径。
基金supported by the National Natural Science Foundation of China(Grants Nos.41430322 and 41474030)the National Key Research and Development Project of China(Grants No.2016YFC0600301)
文摘The Haicheng earthquake （Ms 7.3） occurred in Liaoning Province （39°N-43°N, 120°E-126°E ）, China on February 4, 1975. The mortality rate was only 0.02% owing to the first timely and accurate prediction, although the area affected by the earthquake was 9200 km^2 and covered cities with a population density of 1000 p/km^2. In this study, the double- difference （DD） tomography method was used to obtain high-resolution three-dimensional （3D） P- and S-wave velocity （Vp and Vs） structures and Vp/Vs as well as the earthquake locations. Tomography results suggest that velocity structure at shallow depth coincides well with topography and sediment thickness. The earthquake locations form a northwest-striking zone associated with the Jinzhou（JZ） Fault and a northeast-striking zone associated with the Haichenghe-Dayanghe （HD） Fault, and suggest that the JZ Fault consists of three faults and the Ms 7.3 Haicheng earthquake originated at the intersection of the JZ and the Faults. Low- velocity zones （LVZs） with low Vp/Vs are observed at 15-20 km depth beneath the Haicheng （HC） region. We interpret the LVZs in the middle crust as regions of fluids, suggesting rock dehydration at high temperatures. The LVZs and low Vp/Vs in the upper crust are attributed to groundwater-filled cracks and pores. We believe that large crustal earthquakes in this area are caused by the combination of faulting and fluid movement in the middle crust.
文摘由于受到台站分布不理想、速度结构研究不准确以及震相拾取误差等因素的影响，常规地震定位结果精度较低。因此，研究收集了辽宁省地震台网的地震目录及震相数据，采用双差地震定位方法，对海城及其附近地区（39°N —43°N，120°E— 126°E）20 a 的1400多次地震进行重新定位。与原始定位结果相比，双差定位结果表明：1）震中更加呈条带状集中，尤其在40．5°N —41．0°N，122．0°E—123．0°E 区间，与该地区的海城河大洋河断裂带走向相一致；2）该地区地震多发生于地下5～20 km，与该区中地壳存在的低速高导层相对应；3）深度剖面图显示，大部分地震沿垂直向下柱状分布，原因是该处有粉碎性破裂带，从地下25 km 处延伸到近地表。双差定位算法使得定位后均方根残差的平均值由0．74 s 下降到0．26 s。辽宁地区的地震震级与发生地震数量有关，地震数量陡然增多，大地震发生概率增大。
