Результаты исследований: Публикации в книгах, отчётах, сборниках, трудах конференций › статья в сборнике материалов конференции
Estimation of the P-wave velocity profile of elastic real data based on surface wave inversion. / Ponomarenko, A.V.; Kashtan, B.M.; Troyan, V.N.; Mulder, W.A.
Near Surface Geoscience 2013. 19th European Meeting of Environmental and Engineering Geophysics of the Near Surface Geoscience Division of EAGE, Near Surface Geoscience 2013; Bochum; Germany; 9 September 2013 through 11 September 2013;. 2013. стр. Code 104173.Результаты исследований: Публикации в книгах, отчётах, сборниках, трудах конференций › статья в сборнике материалов конференции
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TY - GEN
T1 - Estimation of the P-wave velocity profile of elastic real data based on surface wave inversion
AU - Ponomarenko, A.V.
AU - Kashtan, B.M.
AU - Troyan, V.N.
AU - Mulder, W.A.
PY - 2013
Y1 - 2013
N2 - Recently, we proposed an analytical approach to invert for a smoothly varying near-surface P-wave velocity profile that has a squared slowness linearly decreasing with depth. The exact solution for such a velocity profile in the acoustic approximation can be expressed in terms of Airy functions and leads to a dispersion equation. The method was successfully applied to synthetic elastic data with small Vs/Vp-ratio. Here, we apply the method to land data. The result agrees with that of multi-layered inversion, confirming its potential to provide an initial P-wave velocity model for acoustic full waveform inversion. Compared to multi-layered inversion, the method is simpler to use and produces a smooth model characterized by three parameters. In some cases, having a smooth rather than a blocky initial model for full waveform inversion is more appropriate.
AB - Recently, we proposed an analytical approach to invert for a smoothly varying near-surface P-wave velocity profile that has a squared slowness linearly decreasing with depth. The exact solution for such a velocity profile in the acoustic approximation can be expressed in terms of Airy functions and leads to a dispersion equation. The method was successfully applied to synthetic elastic data with small Vs/Vp-ratio. Here, we apply the method to land data. The result agrees with that of multi-layered inversion, confirming its potential to provide an initial P-wave velocity model for acoustic full waveform inversion. Compared to multi-layered inversion, the method is simpler to use and produces a smooth model characterized by three parameters. In some cases, having a smooth rather than a blocky initial model for full waveform inversion is more appropriate.
M3 - Conference contribution
SP - Code 104173
BT - Near Surface Geoscience 2013. 19th European Meeting of Environmental and Engineering Geophysics of the Near Surface Geoscience Division of EAGE, Near Surface Geoscience 2013; Bochum; Germany; 9 September 2013 through 11 September 2013;
ER -
ID: 7412267