资源环境科技发展态势分析平台

Soil bulk density (rho(b)) variations influence soil hydraulic properties, such as the water retention curve (WRC), but they are usually ignored in soil water simulation models. We extend the van Genuchten WRC model parameters to account for rho(b) variations using a series of empirical expressions. WRC measurements made on eight soils with various rho(b), and textures are used to calibrate these rho(b)-related empirical equations. Accordingly, two approaches are developed to estimate WRCs of soils at various rho(b). Another eight soils with a wide range of rho(b) and textures are used to evaluate the accuracy of the new approaches. Approach 1 estimates WRCs for each soil at various rho(b) using a WRC measurement made at a reference rho(b) and the soil texture fractions. This approach gives reasonable WRC estimates for the eight validation soils, with an average root-mean-square error (RMSE) of 0.025 m(3)/ m(3) and an average determination coefficient (R-2) of 0.94. For Approach 2, a WRC measurement made at a reference rho(b) and one additional water content-matric potential value measured at a different rho(b) value are used, which produces WRC estimates with an average RMSE of 0.017 m(3)/ m(3) and an average R-2 of 0.97. The methodology used in Approach 2 is also applied to the Brooks and Corey WRC model to obtain accurate and precise WRC estimates. The proposed approaches have the potential to be incorporated into simulation models for estimating soil hydraulic properties that are affected by transient and variable rho(b).