期刊
HYDROLOGICAL PROCESSES
卷 32, 期 9, 页码 1173-1187出版社
WILEY
DOI: 10.1002/hyp.11458
关键词
debris flows; hydraulic conductivity; infiltration capacity; run-off; wildfire
资金
- U.S. Geological Survey (USGS) Landslide Hazards Program
Soils in post-wildfire environments are often characterized by a low infiltration capacity with a high degree of spatial heterogeneity relative to unburned areas. Debris flows are frequently initiated by run-off in recently burned steeplands, making it critical to develop and test methods for incorporating spatial variability in infiltration capacity into hydrologic models. We use Monte Carlo simulations of run-off generation over a soil with a spatially heterogenous saturated hydraulic conductivity (Ks) to derive an expression for an aerially averaged saturated hydraulic conductivity (K e) that depends on the rainfall rate, the statistical properties of Ks, and the spatial correlation length scale associated with Ks. The proposed method for determining K e is tested by simulating run-off on synthetic topography over a wide range of spatial scales. Results provide a simplified expression for an effective saturated hydraulic conductivity that can be used to relate a distribution of small-scale Ks measurements to infiltration and runoff generation over larger spatial scales. Finally, we use a hydrologic model based on K e to simulate run-off and debris flow initiation at a recently burned catchment in the Santa Ana Mountains, CA, USA, and compare results to those obtained using an infiltration model based on the Soil Conservation Service Curve Number.
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