Retrieving shallow shear-wave velocity profiles from 2D seismic-reflection data with severely aliased surface waves

• Published in: Journal of applied geophysics 2019-02, Vol.161, p.15-25
• Main Authors: Onnis, L.E., Osella, A., Carcione, J.M.
• Format: Article
• Language: English
• Subjects: MASW; Neighborhood algorithm; Shear-wave velocity; Spatial aliasing; Surface waves
• ISSN: 0926-9851; 1879-1859
• DOI: 10.1016/j.jappgeo.2018.11.014

The inversion of surface-wave phase-velocity dispersion curves provides a reliable method to derive near-surface shear-wave velocity profiles. In this work, we invert phase-velocity dispersion curves estimated from 2D seismic-reflection data. These data cannot be used to image the first 50 m with seismic-reflection processing techniques due to the presence of indistinct first breaks and significant NMO-stretching of the shallow reflections. A surface-wave analysis was proposed to derive information about the near surface in order to complement the seismic-reflection stacked sections, which are satisfactory for depths between 50 and 700 m. In order to perform the analysis, we had to overcome some problems, such as the short acquisition time and the large receiver spacing, which resulted in severe spatial aliasing. The analysis consists of spatial partitioning of each line in segments, picking of the phase-velocity dispersion curves for each segment in the f-k domain, and inversion of the picked curves using the neighborhood algorithm. The spatial aliasing is successfully circumvented by continuously tracking the surface-wave modal curves in the f-k domain. This enables us to sample the curves up to a frequency of 40 Hz, even though most components beyond 10 Hz are spatially aliased. The inverted 2D VS sections feature smooth horizontal layers, and a sensitivity analysis yields a penetration depth of 20–25 m. The results suggest that long profiles may be more efficiently surveyed by using a large receiver separation and dealing with the spatial aliasing in the described way, rather than ensuring that no spatially aliased surface waves are acquired. •Exploitation of seismic-reflection data with surface-wave methods•Dispersion curves are determined for the fundamental and 1st higher Rayleigh modes.•Components with less than half of the Nyquist wavelength are consistently sampled.•Best parameterizations have an increase of shear-wave velocity with depth.•Inverted sections show smooth horizontal layers up to a depth of 25 m.