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Journal of Environmental & Engineering Geophysics; June 2005; v. 10; issue. p. 219-228; DOI: 10.2113/JEEG10.2.219
© 2005 Environmental & Engineering Geophysical Society
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Propagation of Data Uncertainty in Surface Wave Inversion

Carlo G. Lai1, Sebastiano Foti2 and Glenn J. Rix3

European Centre for Training and Research in Earthquake Engineering, EUCENTRE, Via Ferrata, 1 Pavia, 27100, Italy Email: carlo.lai{at}eucentre.it
Politecnico di Torino, Department of Structural and Geotechnical Engineering, corso Duca degli Abruzzi, 24 Torino, TO 10129, Italy Email: sebastiano.foti{at}polito.it
Georgia Institute of Technology, School of Civil and Environmental Engineering, Atlanta, Georgia 30332 USA Email: glenn.rix{at}ce.gatech.edu

Although in recent years surface wave methods have undergone significant development that has greatly enhanced their capabilities, little effort has been spent to determine the uncertainty associated with surface wave measurements. The objective of this study is to determine how the uncertainty of the experimental data is mapped into the uncertainty of the shear wave velocity profile via the inversion algorithm. The methodology developed in this study for estimating the uncertainty of the shear wave velocity profile from surface wave measurements is based on the assumption that the experimental data are normally distributed. The validity of this hypothesis was experimentally verified using data gathered at two sites in Italy where surface wave tests were performed using linear arrays of multiple receivers. The experimental dispersion curve measured at the site was subsequently inverted to obtain the expected shear wave velocity profile together with an estimate of the associated standard deviation. The final results show that uncorrelated noise has a very little influence on multistation surface wave tests, confirming their robustness for applications in noisy environments.







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