Touraj Sabzevari, Andrea Petroselli, Ali Torabi Haghighi, Hamidreza R. Babaali
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引用次数: 0
摘要
天然集水区的山坡具有复杂的几何形状。在复杂的山坡上,结合平面形状(收敛、平行和发散)和剖面曲率(凹、凸和直)的不同情况,会产生九种不同的几何形状。根据饱和超额径流机制预测集水区地表和地下径流时,必须首先分离山坡的饱和区和非饱和区。山坡的地下行程时间取决于饱和属性。本研究开发了一种名为 Gamma 的新饱和度模型,用于预测复杂山坡的饱和带长度和地下行程时间。在 Gamma 模型中引入了计算饱和带长度的解析公式。Gamma 模型的结果,即饱和带长度和地下行进时间,与另外两个复杂饱和模型 W 和 Sigma 的结果进行了比较。在不同剖面曲率类型的会聚和平行山坡上,三种模型的结果相对接近。不过,由于 Gamma 模型中存在估算饱和带长度的分析方程,因此推荐使用该模型。需要注意的是,对于直向发散和凸向发散山坡,Gamma 模型并不适用,应采用 Sigma 或 W 模型。
Comparison of saturation models in complex hillslopes
Hillslopes of natural catchment have a complex geometry. In complex hillslopes, combining different cases of plan shape (convergent, parallel and divergent) and profile curvature (concave, convex and straight) nine different geometries are created. In prediction of the surface and subsurface runoff of catchments based on saturation excess runoff mechanism, the saturated and unsaturated zones of hillslopes must be first separated. Subsurface travel time of hillslope is dependent on saturation attributes. In this research, a new saturation model, called Gamma, was developed to predict the saturated zone length and subsurface travel time in complex hillslopes. An analytical formula was introduced to calculate saturation zone length in Gamma model. Results of Gamma model, namely the saturation zone length and subsurface travel time, were compared with the results given by two other complex saturation models W and Sigma. The results of the three models were relatively close to each other in convergent and parallel hillslopes of different profile curvature type. However, due to the existence of an analytical equation for estimation of saturated zone length in the Gamma model, this model is recommended. It should be noted that for straight divergent and convex divergent hillslopes, the Gamma model is not suitable and Sigma or W model should be used.