Development of an empirical correlation for predicting shear wave velocity of Christchurch soils from cone penetration test data

Abstract Following the companion study of McGann et al. [1] , seismic piezocone (SCPTu) data compiled from sites in Christchurch, New Zealand area are used with multiple linear regression to develop a Christchurch-specific empirical correlation for use in predicting soil shear wave velocities, V s , from cone penetration test (CPT) data. An appropriate regression functional form is selected through an evaluation of the residuals for regression models developed with the Christchurch SCPTu database using functional forms adopted by previous empirical correlations between V s and CPT data. An examination of how the residuals for the chosen regression form vary with the predictor variables identifies the need for non-constant depth variance in the regression model. The performance of the model is assessed through comparisons of predicted and observed V s profiles and through forward predictions with synthetic CPT data. The new CPT– V s correlation provides a method to estimate V s from CPT data that is specific to the non-gravel soils of the Christchurch region in their current state (caution should be used for western portions of the Springston Formation where SCPTu data were sparse). The correlation also enables the utilization of the large, high-density database of CPT logs ( > 15 , 000 as of 1/1/2014) in the Christchurch region for the development of both site-specific and region-wide models of surficial V s for use in site characterization and site response analysis.