|本期目录/Table of Contents|

[1]刘刚,聂兆生,贾治革,等.高频GNSS地震监测中频率混叠现象的仿真实验研究*[J].地震研究,2017,40(02):186-192.
 LIU Gang,NIE Zhaosheng,JIA Zhige,et al.Simulation Experiment on the Aliasing of High Rate GNSS Used for Earthquake Monitoring[J].Journal of Seismological Research,2017,40(02):186-192.
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高频GNSS地震监测中频率混叠现象的仿真实验研究*(PDF/HTML)

《地震研究》[ISSN:1000-0666/CN:53-1062/P]

卷:
40
期数:
2017年02期
页码:
186-192
栏目:
出版日期:
2017-04-23

文章信息/Info

Title:
Simulation Experiment on the Aliasing of High Rate GNSS Used for Earthquake Monitoring
作者:
刘刚1聂兆生1贾治革1张锐2乔学军1
(1.中国地震局地震研究所 中国地震局地震大地测量重点实验室,湖北 武汉430071; 2.地壳运动监测工程研究中心,北京 100036)
Author(s):
LIU Gang1NIE Zhaosheng1JIA Zhige1ZHANG Rui2QIAO Xuejun1
(1. Key Laboratory of Earthquake Geodesy,Institute of Seismology,CEA,Wuhan 430071,Hubei,China)(2. National Earthquake Infrastructure Service,Beijing 100036,China)
关键词:
高频GNSS 采样率 频率混叠 振动台仿真实验
Keywords:
high rate GNSS sampling rate aliasing shake table simulation experiment
分类号:
P315.7
DOI:
-
摘要:
利用振动台实验,通过设置多个采样频率监测仿真的正弦波形及天然地震波形,研究高频GNSS出现的频率混叠现象及其时频特征,并讨论合理的规避混叠现象的采样率设置方法。结果表明:混叠效应在时域和频域中均有所体现,混叠频率的幅度若高于GNSS的误差水平,其导致的失真将不能忽略; 震级与震中距是导致混叠现象的主要因素,活动断裂的孕震能力与地震危险性及站点与断层面距离是决定高频GNSS监测站采样频率的重要依据。
Abstract:
High rate GNSS measuring the kinematic displacements caused by earthquake with discrete and equal interval sampling rate. According the Nyquist Law,if analog signals have resolve energy at the frequencies higher than the half of sampling rate,the higher frequency signals masquerading as the low frequency signal in the time and frequency domains will contaminate the sampled data. This effect is called aliasing. In this paper,we investigate the aliasing of high rate GNSS by using shake table tests. First we used the sinusoids as input signals to confirm the aliasing effects in the high rate GNSS. Then we used an acceleration record of real earthquake as the input signal to study the mechanism of aliasing effects in the high rate GNSS.The results show that the aliasing occurs both in time domain and frequency domain,and shows non-negligible effect if the masqueraded amplitude is greater than the uncertainty of GNSS positioning. The earthquake magnitude and epicenter distance of GNSS site are two major factors which determine the amplitude of the aliasing effect. Therefore, sampling rate of GNSS should be set according to the seismogenic ability of monitoring fault and the distances between the fault plane and GNSS sites.

参考文献/References:


方荣新,施闯,陈克杰,等.2011.GPS地震仪:PANDA软件测试结果与验证[J].武汉大学学报(信息科学版),36(4):453-456.
刘刚,聂兆生,方荣新,等.2014.高频GNSS形变波的震相识别:模拟实验与实例分析[J].地球物理学报,57(9):2813-2825,doi:10.6038/cjg20140908.
万永革.2007.数字信号处理的MATLAB实现[M].北京:科学出版社.
张培震,邓起东,张竹琪,等.2013.中国大陆的活动断裂、地震灾害及其动力过程[J].中国科学:地球科学,43(10):1607-1620.
BILICH A,CASSIDY J,LARSON K M.2008.GPS Seismology:Application to the 2002 MW7.9 Denali Fault Earthquake[J].Bull Seismol Soc Am,98(2):593-606.
BLEWITT G,HAMMOND W C,KREEMER C,et al.2009.GPS for real-time earthquake source determination and tsunami warning systems[J].Geod,83(3):335-343.
DAVIS J P,SMALLEY J R.2009.Love wave dispersion in central North America determined using absolute displacement seismograms from high-rate GPS[J].Geophys Res Lett,114(B11):292-310,doi:10.1029/2009JB006288.
DELOUIS B,NOCQUET J-M,VALLéE M.2010.Slip distribution of the February 27,2010 MW8.8 Maule Earthquake,central Chile,from static and high-rate GPS,InSAR and broadband teleseismic data[J].Geophys Res Lett,37(17),L17305,doi:10.1029/2010GL043899.
FANG R,SHI C,SONG W W,et al.2013.Determination of earthquake magnitude using GPS displacement waveforms from real-time precise point positioning[J].Geophys J Int,196(1):461-472,doi:10.1093/gji/ggt378.
GALETZKA J,MELGAR D,GENRICH J F,et al.2015.Slip pulse and resonance of the Kathmandu basin during the 2015 Gorkha earthquake,Nepal[J].Science,349(6252):1091-1095.
HUNG H K,RAU R J.2013.Surface waves of the 2011 Tohoku earthquake:Observations of Taiwan’s dense high-rate GPS network[J].J Geophys Res,118(1):332-345,doi:10.1029/2012JB009689.
LARSON KM,BODIN P,GOMBERG J.2003.Using 1-Hz GPS Data to Measure Deformations Caused by the Denali Fault Earthquake[J].Science,300(5624):1421,doi:10.1126/science.1084531.
LI H,WANG D,CAI Y J,et al.2012.Baseline Correction of Digital Strong-Motion Data-Examples from the 2008 Wenchuan,China,Earthquake[J].Adv Mater Res,378-379,247-250.
LOU Y,ZHANG W,SHI C,et al.2013.High-rate(1-Hz and 50-Hz)GPS Seismology:Application to the 2013 MW6.6 Lushan earthquake[J].Journal of Asian Earth Sciences,79:426-431,doi:http://dx.doi.rog/10.1016/j.jseases.2013.10.016.
MELGAR D,BOCK Y,CROWELL W B.2012.Real-time centroid moment tensor determination for large earthquakes from local and regional displacement records[J].Geophys Res Lett,188(2):703-718.
SMALLEY R.2009.High-rate GPS:How High do We Need to go?[J].Seismol Res Lett,80(6):1054-1061.
WRIGHT T J,HOULIé N,HILDYARD M,et al.2012.Real-time,reliable magnitudes for large earthquakes from 1Hz GPS precise point positioning:The 2011 Tohoku-Oki(Japan)earthquake[J].Geophys Res Lett,39(1),L12302,doi:10.1029/2012GL051894.
YANG S M,NIE Z S,JIAZ G,et al.2011.Co-seismic displacements of 2011 Japan MW9.0 earthquake recorded by far-field GPS stations[J].Geodesy and Geodynamics,2(3),12-15,doi:10.3724/SP.J.1246.2011.00012.
YUE H,LAY T.2011.Inversion of high-rate(1 sps)GPS data for rupture process of the 11 March 2011 Tohoku earthquake(MW9.1)[J].Geophys.Res Lett,38(7):752-767,doi:10.1029/2011GL048700.

备注/Memo

备注/Memo:
收稿日期:2016-10-28
基金项目:中国地震局地震研究所所长基金(IS201326127、IS201506204)和国家自然科学基金项目(41404016、41504011、41574017、41541029)联合资助.

更新日期/Last Update: 2017-06-10