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낙뢰에 의해 방사된 전계와 자계 파형의 파라미터

Waveform Parameters of the Electric and Magnetic Fields Radiated Form Lightning Return Strokes

  • 이복희 (인하대학교 전자전기공학부) ;
  • 백영환 (인하대 대학원 전기공학과) ;
  • 이우철 (인하대 대학원 전기공학과)
  • 발행 : 2006.06.30

초록

본 논문은 낙뢰에 의해서 방사된 전계와 자계 파형의 물리적 특성과 파라미터분석에 대한 것으로 낙뢰에 의한 전계와 자계 파형은 각각 평판형 전계센서와 루프형 자계센서로 검출되고, 측정된 신호는 12 비트의 해상도, 10[MS/s] 샘플링, 10[ms]의 기록시간을 가지는 데이터취득시스템으로 기록하였다. 낙뢰에 의해 발생한 전계와 자계 파형의 극성의존성은 거의 없었으며, 상승시간은 $13[{\mu}s]$이내이고 정 부극성의 평균값은 각각 $4.1[{\mu}s],\;4.2[{\mu}s]$이었다. 정 부각성의 영점교차시간은 각각 $65.2[{\mu}s],\;67.0[{\mu}s]$이고, 반전딥의 깊이는 38.0[%], 40.3[%]이었다.

This paper deals with the physical properties and statistical analysis of waveform parameters of electric and magnetic folds radiated from lightning return strokes. The lightning electric and magnetic fields were detected by an plate-type electric field sensor and a loop-type magnetic field sensor respectively, and they were recorded by a data acquisition system having a resolution of 12bits, a sampling rate of 10[MS/s] and recording length of 10[ms]. As a result, a little difference between the parameters of electric and magnetic fields for positive and negative polarities was observed. The rise times of electric and magnetic fields were within the range of less than $13[{\mu}s]$ and the average values for positive and negative polarities were $4.1[{\mu}s]\;and\;4.2[{\mu}s]$, respectively. The average values of the zero-to zero crossing times were $65.2[{\mu}s]\;and\;67.0[{\mu}s]$, and the average depths of the dip to opposite polarity were 38.0[%] and 40.3[%], for positive and negative polarities, respectively.

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참고문헌

  1. C. D. Weidman, E. P. Krider, 'The Fine Structure of Lightning Retum St개ke Waveforms', J. Goo. Res., Vol.83, No.C12, pp. 6239-6247, 1978 https://doi.org/10.1029/JC083iC12p06239
  2. W. Beasley, M. A. Uman and P. L. Rustan, 'Electric Fields Processing Cloud-to-Ground Lightning Flashes', J. Coe., Res., Vol.87, No.C7, pp. 4883-4902, 1982
  3. C. Leteinturier, J. Hamelin and C. Weidman, 'Correlation of Lightning Current and Electric Field Derivative', 8th International Zurich Symposiurn and Technical Exhibition on Electromagnetic Compatibilitv, pp. 405-410, 1989
  4. Y. T. Lin, M. A. Uman and R. B. Standler, 'Lightning Return Stroke Models', J. Geo. Res., Vol.85, No.C3, pp. 1571-1583, 1980.3 https://doi.org/10.1029/JC085iC03p01571
  5. M, lshii and J. Hojo, 'Statics on Fine Structure of Cloud-to-Grourd Lightning Field Waveforms', J. Geo. Res., Vo1.94, No.D11, pp. 267-274, 1989
  6. V. Coorav and S. Lundquist, 'Characteristics of the Radiation Fields from Lightning in Sri Lanka in the tropics', J. Geo. Res., Vol.90, No.D4, pp. 6099-6109, 1985 https://doi.org/10.1029/JD090iD04p06099
  7. 이복희, 이우철, '운방전에 의해서 발생한 전계와 자계파형의 파라미터 분석', 조명전기설비학회 논문지, Vol.20, in press
  8. M. A. Uman and E. P. Krider, 'A Review of Natural Lightning : Experimental Data and Modeling', IEEE Trans., Vol.EMC-24, No.2, pp. 78-105, 1982
  9. 石井 勝 外, '落雷に伴う電磁界變化波形の特性と評價法', 日本電氣學會論文誌B, Vol.108, No.4, pp. 28-35, 1988
  10. Bok-Hee Lee, Ju-Hong Eom, Sung-Man Kang, Seung-Kwon Paek and Tatsuo Kawamura, 'Characteristics of the Radiation Field Waveforms Produced by Lightning Return Strokes', Japanses Journal of Applied Physics, Vol.43, No.7A, pp.4379-4385, 2004 https://doi.org/10.1143/JJAP.43.4379