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Estimating groundwater levels using system identification models in Nzhelele and Luvuvhu areas, Limpopo Province, South Africa

机译:南非利普勒省利尔勒和吕维湖地区系统识别模型估算地下水位

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This study was focused on testing the ability of a coupled linear and non-linear system identification model in estimating groundwater levels. System identification provides an alternative approach for estimating groundwater levels in areas that lack data required by physically-based models. It also overcomes the limitations of physically-based models due to approximations, assumptions and simplifications. Daily groundwater levels for 4 boreholes, rainfall and evaporation data covering the period 2005-2014 were used in the study. Seventy and thirty percent of the data were used to calibrate and validate the model, respectively. Correlation coefficient (R), coefficient of determination (R-2), root mean square error (RMSE), percent bias (PBIAS), Nash Sutcliffe coefficient of efficiency (NSE) and graphical fits were used to evaluate the model performance. Values for R, R2, RMSE, PBIAS and NSE ranged from 0.8 to 0.99, 0.63 to 0.99, 0.01-2.06 m, -7.18 to 1.16 and 0.68 to 0.99, respectively. Comparisons of observed and simulated groundwater levels for calibration and validation runs showed close agreements. The model performance mostly varied from satisfactory, good, very good and excellent. Thus, the model is able to estimate groundwater levels. The calibrated models can reasonably capture description between input and output variables and can, thus be used to estimate long term groundwater levels. (C) 2017 The Authors. Published by Elsevier Ltd.
机译:该研究专注于测试耦合线性和非线性系统识别模型在估计地下水位的能力。系统识别提供了一种替代方法,用于估计基于物理模型所需的数据的区域中的地下水位。它还克服了由于近似,假设和简化而导致物理基础的局限性。在研究中使用了4个钻孔,降雨和蒸发数据的日常地下水位,覆盖了2005-2014期的蒸发数据。 70%和30%的数据分别用于校准并验证模型。相关系数(R),确定系数(R-2),均均方误差(RMSE),百分比偏置(PBIAS),NASH SUTCLIFFE效率系数(NSE)和图形配合用于评估模型性能。 R,R2,RMSE,PBIA和NSE的值范围为0.8至0.99,0.63至0.99,0.01-2.06 m,-7.18至1.16和0.68至0.99。校准和验证运行的观察和模拟地下水位的比较显示了密切的协议。模型性能主要从令人满意,良好,非常好,非常好的变化。因此,该模型能够估计地下水位。校准的模型可以合理地捕获输入和输出变量之间的描述,并且可以使用,从而用于估计长期地下水位。 (c)2017作者。 elsevier有限公司出版

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