Modeling Surface Runoff on a Semi-Arid Watershed Using a Physically Based Model
Publication: World Environmental and Water Resources Congress 2008: Ahupua'A
Abstract
Physically based hydrologic models can represent spatial variability of soil hydraulic properties. In this study, a two-dimensional distributed rainfall-runoff model is used to examine runoff on a small (4.4 ha) basin (Lucky Hills 104) in the Walnut Gulch Experimental Watershed, near Tombstone, Arizona. Soil samples were collected across the basin and analyzed for texture. Soil hydraulic parameters were derived using a pedotransfer function. Parameter fields were then generated using a geostatistical approach. The numerical model was run for four rainfall events that generated measured runoff from on-site flumes. The results showed that the geostatistical approach generated parameter fields with significant spatial patterns. Simulated runoff depths were closely correlated to measured depths (relative error ranged from 3–31.9%). Results showed that the Green-Ampt infiltration model underestimated infiltration for multi-peak events. A more realistic infiltration model and more detailed use of spatial variability of hydraulic properties are needed to improve the prediction accuracy.
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Copyright
© 2008 American Society of Civil Engineers.
History
Published online: Apr 26, 2012
ASCE Technical Topics:
- Arid lands
- Engineering fundamentals
- Hydraulic engineering
- Hydraulic models
- Hydraulic properties
- Hydrologic engineering
- Hydrologic models
- Hydrology
- Irrigation engineering
- Mathematics
- Models (by type)
- Parameters (statistics)
- River engineering
- River systems
- Runoff
- Statistics
- Surface properties
- Water and water resources
- Watersheds
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