NEES: The Shear Wave Velocity Profiles Database
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The author of this database is NEES @ UTexas. The database was published at NEEShub on January 10 2011 and has been reproduced here to preserve the data and ensure continued access.
Database
doi: 10.4231/D3JH3D27N
The SASW testing involves generating surface waves with a vertical excitation and then measuring the vertical surface motions. Receivers are arranged in a straight line which stretches outward from the source. The variation in phase shift with frequency for surface waves propagating between adjacent receivers is recorded for each receiver spacing. From each receiver pair, the phase velocity of the surface wave can be calculated. The phase velocity, VR, depends primarily on the material properties (shear wave velocity, mass density, and Poisson's ratio or compression wave velocity) over a depth of approximately one wavelength. From this calculation, a plot of phase velocity versus frequency, called a dispersion curve, is generated. This procedure is repeated for all source-receiver spacings used at the site and usually involves significant overlapping in the dispersion data between adjacent receiver sets.
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The individual dispersion curves from all receiver spacings are combined into a single composite dispersion curve called the experimental or field dispersion curve. A forward-modeling procedure is then used to match the field dispersion curve with a one-dimensional layered system of varying layer stiffnesses and thicknesses. The shear wave velocity profile that generates a dispersion curve that most closely matches the field dispersion curve is then presented as the shear wave velocity profile for the site.
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