Surface Runoff Essay

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For many years, it was believed that the occurrence of surface runoff was primarily controlled by the infiltration characteristics of the ground; whenever the rainfall rate exceeds or surpasses the soil's infiltration capacity, runoff is generated. Horton (1933, 1940) was responsible for some of the early foundational work for this concept and hence the process is referred to as Hortonian runoff. Horton (1943) also recognized that surface runoff rarely occurs on soils well protected by forest cover due to “somewhat unusual conditions”.
The term “unusual condition” can be referred to as the first concept applied for variable saturated areas in a watershed. Subsequently Hoover and Hursh (1943) and Hursh (1944) described a “dynamic form of subsurface flow” contributing to storm flow generation in forest lands while Roessel (1950) emphasized the importance of sub surface flow and groundwater changes in streamside outflow. Cappus (1960) provided clear field evidence of subsurface storm flow within the context of the variable source areaVSA concept. Based on the study of sandy soil dominated …show more content…

(2003) suggested that hillsides with mild slopes, concave topography, low-saturated hydraulic conductivity and high-shallow water table have high propensity for VSAs as compared to steep slope hillsides. Pilgrim et al. (1978); Jordan (1994); Perrin et al. (2001); Wetzel (2003); Godsey et al. (2004) reported that the spatial heterogeneity of the landscape may allow infiltration excess and saturation excess runoff generating mechanisms to be present simultaneously in a watershed. However Scherrer et al. (2007) suggested that depending on the hydrologic characteristics of a watershed, one or more of these mechanisms often dominates. Buda et al. 2009 demonstrated the influence of subsurface soil properties on surface runoff generation in agricultural watersheds with VSA hydrology which could be useful for improving the accuracy of existing VSA prediction

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