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AN EXPERIMENTAL INVESTIGATION OF A SEMI-ANALYTICAL INFILTRATION MODEL FOR ERRATIC RAINFALL

机译:不稳定降雨的半解析渗流模型的实验研究

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Careful laboratory observations were used to test the general model proposed by Corradini et al. ([1]) for local infiltration-redistribution-reinfiltration in a homogeneous soil. A laboratory slope in a nearly horizontal position was used. Infiltration into the loam soil was forced by a rainfall event characterized by two storms with intensity 22 mm h~(-1) separated by a rainfall hiatus of 18 h. Adopting an exponential function for the vertical profile of water content, θ, the model simulated very accurately the θ profiles, particularly during the infiltration and reinfiltration stages. Lastly, experimental and theoretical simulations indicated that the use of a compound profile after a redistribution period was a correct approximation of the actual profiles.
机译:仔细的实验​​室观察被用来测试Corradini等人提出的通用模型。 ([1])用于均质土壤中的局部渗透-重新分布-重新渗透。使用了接近水平位置的实验室坡度。降雨事件迫使渗透到壤土中,降雨事件的特征是两次风暴强度为22 mm h〜(-1),降雨间隔为18 h。该模型对水分的垂直剖面θ采用指数函数,因此可以非常精确地模拟θ剖面,尤其是在渗透和再渗透阶段。最后,实验和理论模拟表明,重新分布期后使用复合轮廓是实际轮廓的正确近似值。

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