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Estimating Soil Hydraulic and Solute Transport Parameters in Subsurface Drainage Systems Using an Inverse Modelling Approach

机译:逆建模方法估算地下排水系统中的土壤液压和溶质运输参数

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摘要

The aim of this study is to present an inverse modelling approach with a genetic algorithm for estimating soil hydraulic and solute transport parameters in two subsurface drainage systems in Iran. In this study, measured data were obtained from Amirkabir and Shoaybiyeh sugarcane fields equipped with subsurface drainage systems. The SWAP model was used for simulating the outputs of subsurface drainage systems. The accuracy of different objective functions which were based on the discrepancies between measured and simulated values of drainage discharge, groundwater depth and drainage water salinity was evaluated in the inverse modelling approach. Based on sensitivity analysis of the SWAP model in studied areas, n shape parameter, lateral hydraulic conductivity, depth to impermeable layer, saturated water content and shape parameter were selected in the inverse modelling approach. By applying the objective function which is based on drainage discharge and salinity in the Amirkabir study area, the Nash-Sutcliffe Efficiency (NSE) values for predicting drainage discharge and salinity were 0.63 and 0.79, respectively. In the Shoaybiyeh study area, the objective function which includes drainage discharge, groundwater depth and drainage water salinity resulted in NSE values of 0.83, 0.95 and 0.89 for predicting drainage discharge, groundwater depth and drainage water salinity, respectively. Copyright (c) 2017 John Wiley & Sons, Ltd.
机译:本研究的目的是提出一种反向建模方法,其具有遗传算法,用于估算伊朗两种地下排水系统中的土壤液压和溶质运输参数。在本研究中,从配备有地下排水系统的Amirkabir和Shoaybiyeh甘蔗领域获得测量数据。 SWAP模型用于模拟地下排水系统的输出。根据逆建模方法评估了基于测量和模拟的排出排放,地下水深度和排水水盐度之间测量和模拟值之间的差异的不同目标功能的准确性。基于研究领域的交换模型的灵敏度分析,N形参数,横向液压导电性,深度对不透水层,饱和含水量和形状参数,以逆建模方法选择。通过应用基于Amirkabir研究区域的排水排出和盐度的目标函数,预测排水排出和盐度的纳什苏克利夫效率(NSE)值分别为0.63和0.79。在Shoaybiyeh研究区,包括引流放电,地下水深度和排水水的目标函数导致NSE值为0.83,0.95和0.89,分别用于预测排水排出,地下水深度和排水盐度。版权所有(C)2017 John Wiley&Sons,Ltd。

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