Development of global correlation models between in situ stress-normalized shear wave velocity and soil unit weight for plastic soils

Abstract

© author(s) or their institution(s). Shear wave velocity (Vs) in geo-materials is strongly dependent on factors such as stress state, void ratio, and soil structure. Stress-dependency and void-ratio dependency can be represented by the equations V s = (Equation Found) and V s = (Equation Found) (where α and a are material constants; exponents β and b represent the sensitivity of stress and the void dependent effect, respectively(Equation Found) is effective confining stress; e is void ratio), respectively. To consider the effect of soil disturbance and stress relief in geomaterials, shear wave velocity is often required to be normalized by adopting the site-specific model parameters (β or b). Based on a special in situ database compiled from 156 well-documented test sites that include various geo-materials, this study presents (i) the apparent relationships of the model parameters α and β for all soil and rock materials as well as a and b for all soil materials, (ii) new global correlations between soil unit weight and two types of stress-normalized shear wave velocities (V s1 and V sn ), instead of the conventional V s -soil unit weight relationship for clays, and (iii) the best-fitted multi-regression models between soil unit weight and site-specifically normalized shear wave velocity as well as the plasticity index for plastic soils. Moreover, this study presents the importance of site-specific stress normalization (V sn ) in creating a better correlation model. The proposed relationships offer first-order assessments of soil unit weight within the ranges of available data, which are also approximately guided by a hyperbolic unit weight model with depth.