Review of Soil-Water Characteristic Curve Equations

TLDR

Practical applications of unsaturated soil mechanics lag because measuring the required parameters is time‑consuming, and although many equations for soil‑water characteristic curves exist, their success varies with soil type. The study evaluates popular soil‑water characteristic curve equations and demonstrates that they can all be derived from a single generic form. An equation that performs well across all soil types was identified, enabling easier establishment of unsaturated soil parameter databases for practical applications.

Abstract

Practical applications of unsaturated soil mechanics still lag behind the state-of-the-art knowledge. The main stumbling block is the time-consuming processes involved in the measurement of the unsaturated soil parameters required for the constitutive models. Recent research has shown that the soil-water characteristic curves of a soil can be used in the establishment of a number of the unsaturated soil parameters. In many applications it has become obvious that a satisfactory equation for describing the soil-water characteristic curve will simplify the determination of the soil parameters. Over the years a number of equations have been suggested. Most of these equations have limited success depending on soil types. This paper evaluates the more popular equations that have been suggested and shows that all the equations can be derived from a single generic form. One equation has been identified that performs very well for all soil types. If this equation is in common usage, useful databases on unsaturated soil parameters can be more easily established for practical applications of unsaturated soil mechanics.