Open AccessWindowed f ‐ k spectra of a three‐dimensional wavefield excited by a point source in a two‐dimensional multilayered elastic medium
Author(s) -
Fujiwara Hiroyuki
Publication year - 1997
Publication title -
geophysical journal international
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.302
H-Index - 168
eISSN - 1365-246X
pISSN - 0956-540X
DOI - 10.1111/j.1365-246x.1997.tb05319.x
Subject(s) - spectral line , point source , rayleigh wave , wavelength , computation , wavenumber , phase velocity , excited state , point (geometry) , boundary element method , phase (matter) , geometry , geology , surface wave , physics , computational physics , optics , finite element method , mathematics , atomic physics , algorithm , astronomy , quantum mechanics , thermodynamics
SUMMARY When full 3‐D modelling is too costly or cumbersome, computations of 3‐D elastic wave propagation in laterally heterogeneous, multilayered 2‐D geological structures may enhance considerably our ability to predict strong ground motion for seismological and engineering purposes. Towards this goal, we extend the method based on the combination of the thin‐layer finite‐element and boundary‐element methods (TLFE‐BEM) and calculate windowend f ‐ k spectra of the 3‐D wavefield. The windowed f ‐ k spectra are spatially localized spectra from which the local properties of the wavefield can be extracted. The TLFE‐BEM is particularly suited for calculating the complete wavefield where surface waves are dominant in multilayered media. The computations are performed in the frequency domain, providing the f ‐ k spectra directly. From the results for the 3‐D wavefield excited by a point source in a 2‐D multilayered, sloped structure, it can be said that the phase velocity of the fundamental‐mode Rayleigh wave in a laterally heterogeneous multilayered medium, estimated from the windowed f ‐ k spectra, varies with the location of the point source. For the model calculated in this article, the phase velocity varies between the value for the flat layered structure of the thick‐layer side and that for the structure just under the centre of the window. The exact subsurface structure just under the centre of an array in a laterally heterogeneous medium cannot be obtained if we use the f ‐ k spectral analysis assuming a flat layered structure.