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      KCI등재

      하모닉 웨이브릿 변환을 이용한 표면파 시험을 위한 향상된 데이터 해석기법의 개발 = Development of Advanced Data Analysis Method Using Harmonic Wavelet Transform for Surface Wave Method

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      https://www.riss.kr/link?id=A104618917

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      다국어 초록 (Multilingual Abstract)

      The dispersive phase velocity of a wave propagating through multilayered systems such as a soil site is an important parameter and carries valuable information in non-destructive site characterization tests. The dispersive phase velocity of a wave can be determined using the phase spectrum, which is easily evaluated through the cross power spectrum. However, the phase spectrum determined using the cross power spectrum is easily distorted by background noise which always exists in the field. This causes distortion of measured signal and difficulties in the determination of the dispersive phase velocities. In this paper, a new method to evaluate the phase spectrum using the harmonic wavelet transform is proposed and the phase spectrum by the proposed method is applied to the determination of dispersion curve. The proposed method can successfully remove background noise effects. To evaluate the validity of the proposed method, numerical simulations of multi-layered systems were performed. Phase spectrums and dispersion curves determined by the proposed method were found to be in good agreement with the actual phase spectrums and dispersion curves biased by heavy background noise. The comparison manifests the proposed method to be a very useful tool to overcome noise effects.
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      The dispersive phase velocity of a wave propagating through multilayered systems such as a soil site is an important parameter and carries valuable information in non-destructive site characterization tests. The dispersive phase velocity of a wave can...

      The dispersive phase velocity of a wave propagating through multilayered systems such as a soil site is an important parameter and carries valuable information in non-destructive site characterization tests. The dispersive phase velocity of a wave can be determined using the phase spectrum, which is easily evaluated through the cross power spectrum. However, the phase spectrum determined using the cross power spectrum is easily distorted by background noise which always exists in the field. This causes distortion of measured signal and difficulties in the determination of the dispersive phase velocities. In this paper, a new method to evaluate the phase spectrum using the harmonic wavelet transform is proposed and the phase spectrum by the proposed method is applied to the determination of dispersion curve. The proposed method can successfully remove background noise effects. To evaluate the validity of the proposed method, numerical simulations of multi-layered systems were performed. Phase spectrums and dispersion curves determined by the proposed method were found to be in good agreement with the actual phase spectrums and dispersion curves biased by heavy background noise. The comparison manifests the proposed method to be a very useful tool to overcome noise effects.

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      참고문헌 (Reference)

      1 Nazarian S, Stokoe KH, "situ shear wave velocities from spectral analysis of surface wave" 31-38, 1984

      2 Newland DE., "Time-frequency and time-scale signal analysis by harmonic wavelets (Chap 1 of the book Signal Analysis and Prediction)" Birkhauser 1998

      3 Kausel E, Roesset JM, "Stiffness matrices for layered soils" 71 : 1743-1761, 1981

      4 Bendat JS, "RANDOM DATA : Analysis and Measurement Procedures" John Wiley & Sons 1991

      5 Park HC, "Evaluation of the Dispersive Phase and Group Velocities using Harmonic Wavelet Transform" 34 : 457-467, 2001

      6 Kausel E, Peek R., "Dynamic loads in the interior of a layered stratum: An explicit solution" 72 (72): 1459-1481, 1982

      7 Stokoe KH, "Characterization of geotechnical sites by SASW method (Geotechnical characterization of sites)" 15-26. 15-26, 1994

      8 Joh SH., "Advanced in Interpretation and Analysis Techniques for Spectral-Analysis-of-Surface-Waves(SASW) Measurements" The Unversity of Texas at Austin. 1996

      1 Nazarian S, Stokoe KH, "situ shear wave velocities from spectral analysis of surface wave" 31-38, 1984

      2 Newland DE., "Time-frequency and time-scale signal analysis by harmonic wavelets (Chap 1 of the book Signal Analysis and Prediction)" Birkhauser 1998

      3 Kausel E, Roesset JM, "Stiffness matrices for layered soils" 71 : 1743-1761, 1981

      4 Bendat JS, "RANDOM DATA : Analysis and Measurement Procedures" John Wiley & Sons 1991

      5 Park HC, "Evaluation of the Dispersive Phase and Group Velocities using Harmonic Wavelet Transform" 34 : 457-467, 2001

      6 Kausel E, Peek R., "Dynamic loads in the interior of a layered stratum: An explicit solution" 72 (72): 1459-1481, 1982

      7 Stokoe KH, "Characterization of geotechnical sites by SASW method (Geotechnical characterization of sites)" 15-26. 15-26, 1994

      8 Joh SH., "Advanced in Interpretation and Analysis Techniques for Spectral-Analysis-of-Surface-Waves(SASW) Measurements" The Unversity of Texas at Austin. 1996

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      학술지 이력

      학술지 이력
      연월일 이력구분 이력상세 등재구분
      2026 평가예정 재인증평가 신청대상 (재인증)
      2020-01-01 평가 등재학술지 유지 (재인증) KCI등재
      2017-01-01 평가 등재학술지 유지 (계속평가) 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
      2001-01-01 평가 등재학술지 선정 (등재후보2차) KCI등재
      1998-07-01 평가 등재후보학술지 선정 (신규평가) KCI등재후보
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      학술지 인용정보

      학술지 인용정보
      기준연도 WOS-KCI 통합IF(2년) KCIF(2년) KCIF(3년)
      2016 0.31 0.31 0.28
      KCIF(4년) KCIF(5년) 중심성지수(3년) 즉시성지수
      0.29 0.28 0.564 0.12
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