| 4th International Conference on Water Resource and Environment | |
| Physico-empirical methods for estimating soil water characteristic curve under different particle size | |
| 地球科学;生态环境科学 | |
| Zhao, Y.Q.^1,2,3 ; Wang, W.K.^1,2 ; Wang, Z.F.^1,2 ; Li, L Chen^1,2 | |
| School Environment Science and Engineering, Chang'An University, Xian | |
| 710054, China^1 | |
| Key Laboratory of Subsurface Hydrology and Ecological Effect, Xian | |
| 710054, China^2 | |
| Groundwater Monitoring Station, Xianyang | |
| 712000, China^3 | |
| 关键词: Coefficient of determination; Different particle sizes; Prediction precision; Root mean square errors; Soil particle size; Soil-water characteristic curve; Spherical particle; Water characteristics; | |
| Others : https://iopscience.iop.org/article/10.1088/1755-1315/191/1/012018/pdf DOI : 10.1088/1755-1315/191/1/012018 |
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| 学科分类:环境科学(综合) | |
| 来源: IOP | |
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【 摘 要 】
Soil water characteristic curve (SWCC) is an important property of soil, but directly measuring methods are costly and time-consuming. Many attempts have been made to predict the water characteristic curve indirectly from soil particle size distribution (PSD) and basic physical properties. In this study, the Arya-Paris (A-P) model and Non-similar midia concept (NSMC) model were applied to predict the SWCC indirectly with six soil samples in arid regions. The objective of this study was to compare the two physico-empirical methods and assess the applicability of them under different particle size of soil. The results showed that the A-P model was superior to NSMC model on prediction precision, and more suited to predict silty sand and silt, those soils with medium texture. While using Arya-Paris method, the scaling parameter, α (parameter used to scale pore lengths based on spherical particles to natural soil pore lengths), was estimated by non-linear fitting, linear fitting and as a constant. It was found that the A-P model with non-linear α that used improved logistic growth equation was the best method to estimate SWCC, which had a maximum coefficient of determination (R2) and minimum root mean square error (RMSE).
【 预 览 】
| Files | Size | Format | View |
|---|---|---|---|
| Physico-empirical methods for estimating soil water characteristic curve under different particle size | 1306KB |
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