Chapter
Apr 26, 2012
Estimation of Shear-Wave Velocity Profiles: Inversion of Spatial Autocorrelation Coefficients
Publication: GeoFlorida 2010: Advances in Analysis, Modeling & Design
Abstract
Microtremors are measured and analized by spatial autocorrelation method (SPAC) for determination of shear-wave velocity (Vs) models. In SPAC method, estimating Vs profiles is a two-stage process. Conventionally, Rayleigh wave phase velocity dispersion data, which are obtained from SPAC coefficients, are inverted for the shear-wave velocity models. In this study, a more practical (one-stage) scheme is utilized where the SPAC coefficients are directly inverted for unknown shear-wave velocities. The method is based on a weighted damped-least squares solution. Stability of inversion is achieved by using differential smoothing approach that provides Vs models in which the velocity differences between adjacent layers are minimized.
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© 2010 American Society of Civil Engineers.
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Published online: Apr 26, 2012
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Istanbul Technical University, Faculty of Mines, Department of Geophysical Engineering, Maslak, Istanbul, Turkey, P. O. Box 34469. E-mail: [email protected]
Istanbul Technical University, Faculty of Mines, Department of Geophysical Engineering, Maslak, Istanbul, Turkey, P. O. Box 34469. E-mail: [email protected]
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