Frequency domain elastic full waveform inversion using the new pseudo-Hessian matrix: elastic Marmousi-2 synthetic test

향상된 슈도-헤시안 행렬을 이용한 탄성파 완전 파형역산

  • Choi, Yun-Seok (School of Civil, Urban and Geosystem Engineering, Seoul Nation University) ;
  • Shin, Chang-Soo (School of Civil, Urban and Geosystem Engineering, Seoul Nation University) ;
  • Min, Dong-Joo (Korea Ocean Research and Development Institute)
  • 최윤석 (서울대학교 지구환경시스템공학부) ;
  • 신창수 (서울대학교 지구환경시스템공학부) ;
  • 민동주 (한국해양연구원)
  • Published : 2007.06.07

Abstract

For scaling of the gradient of misfit function, we develop a new pseudo-Hessian matrix constructed by combining amplitude field and pseudo-Hessian matrix. Since pseudo- Hessian matrix neglects the calculation of the zero-lag auto-correlation of impulse responses in the approximate Hessian matrix, the pseudo-Hessian matrix has a limitation to scale the gradient of misfit function compared to the approximate Hessian matrix. To validate the new pseudo- Hessian matrix, we perform frequency-domain elastic full waveform inversion using this Hessian matrix. By synthetic experiments, we show that the new pseudo-Hessian matrix can give better convergence to the true model than the old one does. Furthermore, since the amplitude fields are intrinsically obtained in forward modeling procedure, we do not have to pay any extra cost to compute the new pseudo-Hessian. We think that the new pseudo-Hessian matrix can be used as an alternative of the approximate Hessian matrix of the Gauss-Newton method.

Keywords