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Study on eliminating noises in short-period data of geomagnetic intensity by using nu-merical multichannel predictive filtering 被引量:1

Study on eliminating noises in short-period data of geomagnetic intensity by using nu- merical multichannel predictive filtering
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摘要 The effectiveness of eliminating the noises in short-period data of geomagnetic intensity recorded in a little seismo-geomagnetic array by using numerical multichannel predictive filtering has been studied. The result shows that this technique is effective to fit external magnetic disturbance to inner electromagnetic induced difference field and reduce the noise level of difference data successfully. The filter quality factor Q of two examples in this work are 0. 86 and 0.68 respectively. The spectral analysis shows that during geomagnetic-calm days the fourfold-frequency harmonics of S q in difference data are main components. The length of the optimum filter depends on not only the frequency of predicable energy in difference data but also maybe the phase difference between input and expected output data. It is difficult to obtain the filter fitting both the data during magnetic-disturbed days and calm days. The result shows that the conductivity in Yanqing-Huailai basin west to Beijing may be much non-uniform. The effectiveness of eliminating the noises in short-period data of geomagnetic intensity recorded in a little seismo-geomagnetic array by using numerical multichannel predictive filtering has been studied. The result shows that this technique is effective to fit external magnetic disturbance to inner electromagnetic induced difference field and reduce the noise level of difference data successfully. The filter quality factor Q of two examples in this work are 0. 86 and 0.68 respectively. The spectral analysis shows that during geomagnetic-calm days the fourfold-frequency harmonics of S q in difference data are main components. The length of the optimum filter depends on not only the frequency of predicable energy in difference data but also maybe the phase difference between input and expected output data. It is difficult to obtain the filter fitting both the data during magnetic-disturbed days and calm days. The result shows that the conductivity in Yanqing-Huailai basin west to Beijing may be much non-uniform.
出处 《Acta Seismologica Sinica(English Edition)》 EI CSCD 1998年第5期66-71,共6页
关键词 intensity differences multichannel predictive filtering seismo-magnetic effect electromagnetic induction external magnetic disturbance intensity differences multichannel predictive filtering seismo-magnetic effect electromagnetic induction external magnetic disturbance
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同被引文献2

  • 1Xi-Xian Ren,Yu-Min Zhang,Zhi-Jia Zhan,Jin-Tian Gao.Study on terrestiral noise in data of geomagnetic total field in North China[J].Acta Seismologica Sinica.1993(4)
  • 2Frank D. Stacey.The seismomagnetic effect[J].Pure and Applied Geophysics PAGEOPH.1964(1)

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