251. Pedo-transfer functions for estimating the hydraulic properties of paddy soils in subtropical central China
- Author
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Yong Li, Jinshui Wu, De Li Liu, Yuyuan Li, Yi Wang, Ganghua Zou, and Xinliang Liu
- Subjects
chemistry.chemical_classification ,Hydrology ,geography ,geography.geographical_feature_category ,010504 meteorology & atmospheric sciences ,Water retention curve ,Soil physics ,Drainage basin ,Soil Science ,Soil science ,04 agricultural and veterinary sciences ,01 natural sciences ,Bulk density ,chemistry ,Hydraulic conductivity ,Soil water ,Vadose zone ,040103 agronomy & agriculture ,0401 agriculture, forestry, and fisheries ,Organic matter ,Agronomy and Crop Science ,Geology ,0105 earth and related environmental sciences - Abstract
Pedo-transfer functions (PTFs) have been widely used to estimate soil hydraulic properties in the simulation of catchment eco-hydrological processes. However, the accuracy of existing PTFs is usually inadequate for use. To develop PTFs for local use, soil columns were collected from a double rice-cropped agricultural catchment in subtropical central China. The PTFs for saturated soil hydraulic conductivity (Ks) and parameters (θs, α, and n) of the van Genuchten model for the soil water retention curve (SWRC) were obtained based on soil’s basic properties, and compared with models developed by Li et al. in 2007 and Wosten et al. in 1999, respectively. Our results indicated that Ks in the range of 0.04–1087 cm d−1 and θs in the range of 0.34–0.51 cm3 cm−3 were both well estimated with the R2adj of 0.72 and 0.87, respectively, but α (0.04–0.65 cm−1) and n (1.05–1.21) were relatively poorly predicted with the respective R2adj of 0.38 and 0.55, despite the use of more input parameters. Our local derive...
- Published
- 2015
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