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Modelling Furrow Irrigation-Induced Erosion on a Sandy Loam Soil in Samaru, Northern Nigeria

机译:对尼日利亚北部萨马鲁的砂质壤土上沟灌引起的侵蚀进行建模

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Assessment of soil erosion and sediment yield in furrow irrigation is limited in Samaru-Zaria. Data was collected in 2009 and 2010 and was used to develop a dimensionless model for predicting furrow irrigation-induced erosion (FIIE) using the dimensional analyses approach considering stream size, furrow length, furrow width, soil infiltration rate, hydraulic shear stress, soil erodibility, and time flow of water in the furrows as the building components. One liter of water-sediment samples was collected from the furrows during irrigations from which sediment concentrations and soil erosion per furrow were calculated. Stream sizes (2.5, 1.5, and 0.5?l/s), furrow lengths (90 and 45?m), and furrow widths (0.75 and 0.9?m) constituted the experimental factors randomized in a split plot design with four replications. Water flow into and out of the furrows was measured using cutthroat flumes. The model produced reasonable predictions relative to field measurements with coefficient of determination in the neighborhood of 0.8, model prediction efficiency NSE (0.7000), high index of agreement (0.9408), and low coefficient of variability (0.4121). The model is most sensitive to water stream size. The variables in the model are easily measurable; this makes it better and easily adoptable.
机译:在萨马鲁-扎里亚(Samaru-Zaria),对沟灌中土壤侵蚀和沉积物产量的评估是有限的。收集了2009年和2010年的数据,并使用尺寸分析方法开发了无量纲模型来预测犁沟灌溉引起的侵蚀(FIIE),其中考虑了溪流大小,犁沟长度,犁沟宽度,土壤入渗率,水力剪切应力,土壤易蚀性,以及沟渠中水的时间流作为建筑的组成部分。灌溉期间从犁沟中收集到一升水沉积物样品,由此计算出每个犁沟的沉积物浓度和土壤侵蚀。溪流大小(2.5、1.5和0.5?l / s),犁沟长度(90和45?m)以及犁沟宽度(0.75和0.9?m)构成了在重复设计中随机重复四次的实验因素。使用割喉水槽测量流入和流出犁沟的水量。该模型相对于现场测量产生了合理的预测,确定系数在0.8附近,模型预测效率NSE(0.7000),一致性指数(0.9408)高,变异系数低(0.4121)。该模型对水流大小最敏感。模型中的变量很容易测量。这使其更容易被采用。

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