GeoCongress 2012 2012
DOI: 10.1061/9780784412121.278
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Application of a Simplified Inversion Technique to Published Surface Wave Dispersion Data–Comparisons with Advanced Methods of Inversion

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Cited by 4 publications
(6 citation statements)
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“…[36] and then improved by Pelekis et al . [37]. There are two steps in the process of scaling the parameters in the SIM: (i) determining the equivalent depth Z eq from the wavelength value of the phase velocity L PH ; (ii) calculating the S-wave velocity V s from the phase velocity V ph .…”
Section: Methodsmentioning
confidence: 99%
“…[36] and then improved by Pelekis et al . [37]. There are two steps in the process of scaling the parameters in the SIM: (i) determining the equivalent depth Z eq from the wavelength value of the phase velocity L PH ; (ii) calculating the S-wave velocity V s from the phase velocity V ph .…”
Section: Methodsmentioning
confidence: 99%
“…The SIM method can handle both normally and inversely dispersive soil profiles without using the concept of the elastic Half Space. The critical parameter of the SIM is the wavelength to depth converter which is highly affected by the shape of the dispersion curve and the Poisson's ratio, (Pelekis and Athanasopoulos, 2012).…”
Section: Simplified Inversion Methods (Sim)mentioning
confidence: 99%
“…The model was developed by obtaining V s vs. depth profiles at a number of locations of the urban area, through surface wave measurements, and applying geostatistical interpolation to derive V s values for unsampled points. Surface Wave Methods (SWM), have evolved during the past decade, into a powerful and economic tool for establishing V s vs. depth profiles and they are being used with increasing frequency in soil dynamics and geotechnical earthquake engineering applications [38,39]. The Spectral Analysis of Surface Waves (SASW) method was used in the present study to obtain 1D V s vs. depth profiles at 19 locations in the urban area of Chania [1,8].…”
Section: Measurement and Interpetation Of V S Profilesmentioning
confidence: 99%
“…The recorded signals are processed to generate a dispersion curve (phase wave velocity, V R vs. frequency of vibration), which is, in turn, inverted i.e. transformed to a shear wave velocity profile (V s vs. depth) through the process of inversion [39,38]. The maximum depth of wave penetration depends on the lowest frequency contained in the recorded time histories of ground vibrations.…”
Section: Measurement and Interpetation Of V S Profilesmentioning
confidence: 99%
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