地震地磁观测与研究
地震地磁觀測與研究
지진지자관측여연구
Seismological and Geomagnetic Observation and Research
2015年
4期
19-25
,共7页
DEMETER卫星%ULF电场波形%典型干扰%标定信号%详查模式
DEMETER衛星%ULF電場波形%典型榦擾%標定信號%詳查模式
DEMETER위성%ULF전장파형%전형간우%표정신호%상사모식
DEMETER satellite%ultra low frequency (ULF) electric field waveform%typical interferences%calibration signals%Burst mode
分析由法国DEMETER卫星观测的ULF电场波形数据,发现两种典型干扰:由标定信号引起的脉冲式周期干扰及详查期间噪声水平增加.结果表明:①周期干扰特征表现为:在固定工作模式期间,干扰以约4 min周期出现;在详查和巡查模式开始时刻,干扰出现.结合VLF频段功率谱,可确认此干扰由625 Hz标定信号引起;②在详查模式期间噪声增加,获取ULF频段功率谱发现,此干扰并非来自单个频点或频段信号,对空间真实的ULF扰动分析影响不大.认识ULF电场波形数据的典型干扰特征,可为后续ULF电场扰动研究提供参考,为我国电磁监测试验卫星同类数据干扰分析提供借鉴.
分析由法國DEMETER衛星觀測的ULF電場波形數據,髮現兩種典型榦擾:由標定信號引起的脈遲式週期榦擾及詳查期間譟聲水平增加.結果錶明:①週期榦擾特徵錶現為:在固定工作模式期間,榦擾以約4 min週期齣現;在詳查和巡查模式開始時刻,榦擾齣現.結閤VLF頻段功率譜,可確認此榦擾由625 Hz標定信號引起;②在詳查模式期間譟聲增加,穫取ULF頻段功率譜髮現,此榦擾併非來自單箇頻點或頻段信號,對空間真實的ULF擾動分析影響不大.認識ULF電場波形數據的典型榦擾特徵,可為後續ULF電場擾動研究提供參攷,為我國電磁鑑測試驗衛星同類數據榦擾分析提供藉鑒.
분석유법국DEMETER위성관측적ULF전장파형수거,발현량충전형간우:유표정신호인기적맥충식주기간우급상사기간조성수평증가.결과표명:①주기간우특정표현위:재고정공작모식기간,간우이약4 min주기출현;재상사화순사모식개시시각,간우출현.결합VLF빈단공솔보,가학인차간우유625 Hz표정신호인기;②재상사모식기간조성증가,획취ULF빈단공솔보발현,차간우병비래자단개빈점혹빈단신호,대공간진실적ULF우동분석영향불대.인식ULF전장파형수거적전형간우특정,가위후속ULF전장우동연구제공삼고,위아국전자감측시험위성동류수거간우분석제공차감.
This paper analyzes typical interferences of ULF waveform records based on ULF electric field waveform data observed by French DEMETER satellite. There are two kinds of typical interferences, regularly impulsive interference induced by calibration sequences and increased noise level during Burst mode. The time features of regular interferences show that regular interferences are observed every 4 minutes inside a mode and at the beginning of each Burst and Survey modes. Combined with VLF power spectra, we can confirm that this kind of interferences is caused by 625 Hz calibration signals. By obtaining ULF power spectra,it is found that the increased noise level of ULF waveform records during Burst mode is not generated by signals of single frequency or band. This type of ULF interferences does not much affect the analysis of real ULF disturbances in space. Understanding typical interferences of ULF electric field waveform data can provide references for future studies on the earthquake-related ULF disturbances based on ULF waveform data observed by DEMETER satellite and the interferences analysis of similar data recorded by China Seismo-electromagnetic Satellite (CSES).