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首页> 外文期刊>Sustainable Water Resources Management >Prediction of suspended sediment yield by artificial neural network and traditional mathematical model in Mahanadi river basin, India
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Prediction of suspended sediment yield by artificial neural network and traditional mathematical model in Mahanadi river basin, India

机译:利用人工神经网络和传统数学模型预测印度马哈纳迪河流域的悬浮泥沙产量

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Estimation of sediment yield is essential towards understanding the mass balance between the ocean and land. Direct measurement of suspended sediment is difficult as it needs sufficient time and money. The suspended sediment yield depends on a number of variables, and their inter-relationships are highly non-linear and complex in nature. In this paper, soft computing-based sediment yield estimation algorithms are proposed for the Mahanadi river basin. A multilayer perceptron (MLP) artificial neural network (ANN) with an error back-propagation algorithm using historical monthly hydro-climatic data (temperature, water discharge and rainfall) was employed to predict the suspended sediment yield at the Tikarapara gauging station, which is the farthest downstream station in the Mahanadi river. The results demonstrated that water discharge and rainfall are significant controlling parameters of suspended sediment in the Mahanadi River. The comparative results show that the feed-forward back-propagation with Levenberg–Marquardt (FFBP–LM) is the best model for suspended sediment yield estimation, and provides more reasonable prediction for extremely high and low values. The performance of the sediment rating curve (SRC) model was below expectations as it produced the least accurate results for the peak sediment values, as well as overall model performance. It is also noticed that the multiple linear regressions (MLR) model predicted negative sediment yield at low values; which is completely unrealistic as suspended sediment yield cannot be negative in nature. It was also observed that suspended yield prediction by ANN was superior compared to that using MLR and SRC models. The proposed model will be beneficial for sediment prediction where estimates of suspended sediment values are unavailable.
机译:沉积物产量的估算对于理解海洋和陆地之间的质量平衡至关重要。直接测量悬浮沉淀物很困难,因为它需要足够的时间和金钱。悬浮沉积物的产量取决于许多变量,它们之间的相互关系是高度非线性的,而且本质上很复杂。本文提出了一种基于软计算的马哈纳迪河流域产沙量估算算法。运用错误背向传播算法的多层感知器(MLP)人工神经网络(ANN),该算法使用历史月度水文气候数据(温度,水流量和降雨量)进行反向传播,以预测Tikarapara测量站的悬浮泥沙产量,该方法为Mahanadi河中最远的下游站。结果表明,排水和降雨是马哈纳迪河悬沙的重要控制参数。比较结果表明,Levenberg-Marquardt(FFBP-LM)进行的前馈反向传播是悬浮泥沙产量估算的最佳模型,并为极高和极低的值提供了更合理的预测。泥沙等级曲线(SRC)模型的性能低于预期,因为它产生的泥沙峰值以及整体模型性能的准确性最差。还应注意的是,多元线性回归(MLR)模型预测的负沉积物产量较低。这是完全不现实的,因为悬浮沉积物的产量在本质上不能为负。还观察到,与使用MLR和SRC模型相比,通过ANN预测的悬浮产量要好。所提出的模型对于无法获得悬浮泥沙量估算值的泥沙预测将是有益的。

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