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      KCI등재 SCOPUS

      지진원 상대비율 측정법을 이용한 2017년 북한 핵실험의 실체파 규모 검증 = Validation on the Bodywave Magnitude Estimation of the 2017 DPRK’s Nuclear Test by Source Scaling

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      다국어 초록 (Multilingual Abstract)

      Democratic Peoples’ Republic of Korea (DPRK) conducted the 6th underground nuclear test at the Punggye-ri underground nuclear test site on September 27, 2017 12 hours 30 minutes of Korean local time. Comprehensive Nuclear-Test Ban Treaty Organization (CTBTO) under U.N. announced the body wave magnitude of the event was mb 6.1 while U.S. Geological Survey (USGS)’s calculation was mb 6.3. In this study, the differences of the magnitude estimates were investigated and verified. For this purpose, a source scaling between the 5th and 6th event, which’s epicenters are 200 meters apart, was performed using seismic data sets from 30 broadband stations. The relative amplitude variations of the 6th event compared to the 5th event in the frequency domain was analyzed through the scaling. The increased amount of the bodywave magnitude mb for the 6th event was calculated at 1 Hz, which was compared to those from USGS and CTBTO’s calculations.
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      Democratic Peoples’ Republic of Korea (DPRK) conducted the 6th underground nuclear test at the Punggye-ri underground nuclear test site on September 27, 2017 12 hours 30 minutes of Korean local time. Comprehensive Nuclear-Test Ban Treaty Organizatio...

      Democratic Peoples’ Republic of Korea (DPRK) conducted the 6th underground nuclear test at the Punggye-ri underground nuclear test site on September 27, 2017 12 hours 30 minutes of Korean local time. Comprehensive Nuclear-Test Ban Treaty Organization (CTBTO) under U.N. announced the body wave magnitude of the event was mb 6.1 while U.S. Geological Survey (USGS)’s calculation was mb 6.3. In this study, the differences of the magnitude estimates were investigated and verified. For this purpose, a source scaling between the 5th and 6th event, which’s epicenters are 200 meters apart, was performed using seismic data sets from 30 broadband stations. The relative amplitude variations of the 6th event compared to the 5th event in the frequency domain was analyzed through the scaling. The increased amount of the bodywave magnitude mb for the 6th event was calculated at 1 Hz, which was compared to those from USGS and CTBTO’s calculations.

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      참고문헌 (Reference)

      1 Gutenberg, "The energy of earthquakes" 112 : 1-14, 1956

      2 Park, J-H., "The analysis on the characteristics of North Korea 6th nuclear test, collapse and induced earthquakes" 2017

      3 CTBTO, "Technical Briefing 4 September 2017update"

      4 Murphy, J.R., "Revised Distance and Depth Corrections for Use in the Estimation of Short-Period P-Wave Magnitude" 93 (93): 1746-1764, 2003

      5 Kim, T., "Relative location of the North Korea’s third underground nuclear test" 2013

      6 Bormann, P., "New Manual of Seismological Observatory Practice 2(NMSOP2)" Deutsches GeoForschungs-Zentrum GFZ 1-259, 2013

      7 Veith, K.F., "Magnitude from short-period P-wave data" 62 : 435-452, 1972

      8 Gutenberg, B., "Magnitude determination of deepfocus earthquakes" 35 : 117-130, 1945

      9 US Geological Survey, "M 6.3 Explosion - 22km ENE of Sungjibaegam"

      10 Lee, D.S., "Geology of Korea" Kyohak-Sa Publishing Co. 313-315, 1988

      1 Gutenberg, "The energy of earthquakes" 112 : 1-14, 1956

      2 Park, J-H., "The analysis on the characteristics of North Korea 6th nuclear test, collapse and induced earthquakes" 2017

      3 CTBTO, "Technical Briefing 4 September 2017update"

      4 Murphy, J.R., "Revised Distance and Depth Corrections for Use in the Estimation of Short-Period P-Wave Magnitude" 93 (93): 1746-1764, 2003

      5 Kim, T., "Relative location of the North Korea’s third underground nuclear test" 2013

      6 Bormann, P., "New Manual of Seismological Observatory Practice 2(NMSOP2)" Deutsches GeoForschungs-Zentrum GFZ 1-259, 2013

      7 Veith, K.F., "Magnitude from short-period P-wave data" 62 : 435-452, 1972

      8 Gutenberg, B., "Magnitude determination of deepfocus earthquakes" 35 : 117-130, 1945

      9 US Geological Survey, "M 6.3 Explosion - 22km ENE of Sungjibaegam"

      10 Lee, D.S., "Geology of Korea" Kyohak-Sa Publishing Co. 313-315, 1988

      11 Patton, H. J., "Analysis of Lg Spectral Ratios from NTS Explosions: Implications for the Source Mechanism of Spall and the Generation of Lg Waves" 85 : 220-236, 1995

      12 Gutenberg, B., "Amplitude of surface waves and magnitudes of shallow earthquakes"

      13 Gutenberg, B., "Amplitude of P, PP, and S and magnitude of shallow earthquakes" 35 : 57-69, 1945

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      학술지 이력

      학술지 이력
      연월일 이력구분 이력상세 등재구분
      2023 평가예정 해외DB학술지평가 신청대상 (해외등재 학술지 평가)
      2020-01-01 평가 등재학술지 유지 (해외등재 학술지 평가) KCI등재
      2013-01-01 평가 등재 1차 FAIL (등재유지) KCI등재
      2010-01-01 평가 등재학술지 유지 (등재유지) KCI등재
      2008-01-01 평가 등재학술지 유지 (등재유지) KCI등재
      2006-01-01 평가 등재학술지 유지 (등재유지) KCI등재
      2004-01-01 평가 등재학술지 유지 (등재유지) KCI등재
      2001-07-01 평가 등재학술지 선정 (등재후보2차) KCI등재
      1999-01-01 평가 등재후보학술지 선정 (신규평가) KCI등재후보
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      학술지 인용정보

      학술지 인용정보
      기준연도 WOS-KCI 통합IF(2년) KCIF(2년) KCIF(3년)
      2016 0.35 0.35 0.34
      KCIF(4년) KCIF(5년) 중심성지수(3년) 즉시성지수
      0.29 0.27 0.625 0.19
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