How to Measure Shear-Wave Velocity (Vs)

Vs can be measured through several different approaches:  surface-wave survey, refraction survey, down-hole survey, cross-hole survey, and
laboratory measurement (see illustrations below).  The first two are non-destructive in-situ methods, while the others require preparation of borehole(s)
and some additional pre-measurement procedures.  One formidable challenge common to all these methods, except for the surface-wave survey, is
dealing with a relatively low signal-to-noise ratio (S/N).  A high S/N is the most crucial factor in all types of wave-based techniques to ensure a high
accuracy in results.

On the other hand, the surface-wave method utilizes
Rayleigh-type surface waves as signal waves.    These are the strongest seismic waves, and until
about 15 years ago were considered to be most troublesome source-generated noise during the conventional seismic surveys for oil exploration.  
Because the surface wave method works on these Rayleigh waves as signal, it always achieves the highest S/N.  As a consequence, the field operation
to acquire data and subsequent data analysis procedures become extremely simple and effective in comparison to other methods, always ensuring the
most reliable results.  The
MASW method is the most advanced one among all types of surface-wave approaches historically developed.