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Investigation Artificial Neural Networks For Point Simulation Of Soil Water Retention Curve

机译:研究人工神经网络用于土壤水分保持曲线点模拟。

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In this research 35 soil samples with Loamy texture were gathered form region near Karaj-Alborz province-Iran. Different points of soil water retention curve (SWRC) in tensions points : 0, 10, 33, 100, and 1500 Kpa asdependent variables have been meseaured using pressure plate and presure membrane. Soil properties organiccarbon, bulk density, soil particles size distribution, Caco3, mean and Geometric standard deviation of particlediameter were measured as independent soil peroperties. Independents variables divided into 3 groups ofvariables. Statistical investigation of pedotransfer functions showed that regression pedotransfer functionestablished with soil particle size distribution, bulk density and organic carbon as dependent variable s resultedin best primary prediction also this pattern of input variables used as input variables of artificial neural networksmodels with Marquardt-levenburg training algorithm 3 layer procepteron structure with 6 neuron in hiddenlayer. R2 and RMSR ranged between 0.79- 0.82 and 2.53-1.21 for regression pedotransfer functions. In theother hand R2 and RMSr ranged between 0.85-0.94 and 0.88-1.30 for artificial neural networks. FinalInvestigation of result showed that artificial neural networks had more precious prediction.
机译:在这项研究中,从Karaj-Alborz省-伊朗附近地区收集了35个壤土质土壤样品。张力点:0、10、33、100和1500 Kpa的自变量是土壤保水曲线(SWRC)的不同点,已使用压板和压力膜进行了测量。测量土壤的有机碳,容重,土壤粒径分布,Caco3,粒径的平均值和几何标准偏差作为独立的土壤性能。独立变量分为3组变量。 pedotransfer函数的统计研究表明,以土壤粒径分布,堆积密度和有机碳为因变量建立的回归pedotransfer函数可产生最佳的初步预测,并且这种输入变量也用作Marquardt-levenburg训练算法的人工神经网络模型的输入变量3层procepteron结构,在隐藏层具有6个神经元。对于回归pedotransfer函数,R2和RMSR介于0.79-0.82和2.53-1.21之间。另一方面,对于人工神经网络,R2和RMSr介于0.85-0.94和0.88-1.30之间。对结果的最终调查表明,人工神经网络具有更有价值的预测。

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