首页 | 本学科首页   官方微博 | 高级检索  
     

高铁震源地震信号的稀疏化建模
引用本文:王晓凯, 陈建友, 陈文超, 蒋一然, 鲍铁钊, 宁杰远. 2019. 高铁震源地震信号的稀疏化建模. 地球物理学报, 62(6): 2336-2343, doi: 10.6038/cjg2019M0662
作者姓名:王晓凯  陈建友  陈文超  蒋一然  鲍铁钊  宁杰远
作者单位:1. 西安交通大学信息与通信工程学院, 西安 710049; 2. 中国酒泉卫星发射中心, 甘肃酒泉 732750; 3. 北京大学地球与空间科学学院, 北京 100871; 4. 高铁地震学联合研究组, 北京 100029
基金项目:国家重点研发计划(2017YFB0202902),国家自然科学基金(41774135,41504092),中央高等学校基本科研业务费(bgjs2018,xjj2016065)及中国博士后基金(2016T90925,2015M572566)联合资助.
摘    要:

我国每天有数千趟高铁列车运行在两万多公里的高铁线路上,不但会引起高铁路基的振动,还会激发出地震波.地震检波器所接收到的数据中不仅包含窄带分立谱特性的高铁震源地震信号,还包含宽频带特性的背景信号.如何实现从检波器所接收到的高铁震源地震数据中分离出高铁震源地震信号和宽频带背景信号是准确利用该类信号的关键.考虑到高铁震源地震信号与宽频带信号在频率域明显的形态特征差异,本文首次将形态成分分析这种信号分离手段引入到高铁震源地震信号处理中,实现高铁震源地震信号的稀疏化建模并进而实现从接收数据中分离出高铁震源地震信号以及宽频带背景信号.对北京大学在中国南方某高铁沿线采集到的大量高铁震源地震数据进行处理,结果表明:采用形态成分分析并结合分块坐标松弛算法,能够实现实际采集高铁震源地震数据中的高铁震源地震信号和宽频带信号的分离.



关 键 词:高铁震源地震信号   形态成分分析   分块坐标松弛
收稿时间:2018-11-27
修稿时间:2019-04-22

Sparse modeling of seismic signals produced by high-speed trains
WANG XiaoKai, CHEN JianYou, CHEN WenChao, JIANG YiRan, BAO TieZhao, NING JieYuan. 2019. Sparse modeling of seismic signals produced by high-speed trains. Chinese Journal of Geophysics (in Chinese), 62(6): 2336-2343, doi: 10.6038/cjg2019M0662
Authors:WANG XiaoKai  CHEN JianYou  CHEN WenChao  JIANG YiRan  BAO TieZhao  NING JieYuan
Affiliation:1. School of Information & Communication Engineering, Xi'an Jiaotong University, Xi'an 710049, China; 2. Jiuquan Satellite Launch Center, Jiuquan Gansu 732750, China; 3. School of Earth and Space Sciences, Peking University, Beijing 100871, China; 4. The Joint Research Group of High-Speed Rail Seismology, Beijing 100029, China
Abstract:In China, there are thousands of high-speed trains running on over twenty thousand kilometers railways every day. These running high-speed trains not only cause vibration of railway roadbed but also stimulate seismic waves. The data recorded by seismic receivers to these events contain multi-narrow-band waves by high-speed trains as well as wide-band background noise. Therefore, the key step to use these signals is to divide the complex data into the real high-speed train induced seismic signals and the background noise. Considering the morphological difference between the high-speed train induced seismic signals and the background noise, we firstly introduce the morphological component analysis to the processing of the high-speed train induced seismic signals, and realize the separation between these signals and the background noise by sparse modeling. We applied this approach to the dataset collected by Peking University in South China. The results show that the acquired dataset can be successfully divided to the multi-narrow-band high-speed train induced seismic signals and the wide-band background noise by using the morphological component analysis and block-coordinate relaxation.
Keywords:Seismic signal by high-speed train  Morphological component analysis  Block-coordinate relaxation  
本文献已被 CNKI 维普 等数据库收录!
点击此处可从《地球物理学报》浏览原始摘要信息
点击此处可从《地球物理学报》下载免费的PDF全文
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号