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Estimation of soil pore-water pressure variations using a thin plate spline basis function

机译:薄板条状基函数估计土壤孔隙水压变化

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Information of soil pore-water pressure changes due to climatic effect is an integral part for studies associated with hill slope analysis. Soil pore-water pressure variations in a soil slope due to rainfall were predicted using Artificial Neural Network (ANN) technique with Thin Plate Spline (TPS) radial basis function. A radial basis function (RBF) neural network with network architecture of 8-36-1 (input-hidden-output) was selected to develop RBF model. Number of hidden neurons was selected using trial and error procedure whereas spread of the basis function was established using normalization method. Time series data of rainfall and pore-water pressure was used for training and testing the RBF model. The performance of the model was evaluated using root mean square error, coefficient of correlation and coefficient of efficiency. The results of the model prediction revealed that the model produced promising results indicating that TPS basis function is able to predict time series of pore-water pressure responses to rainfall. Comparison with other studies showed that the RBF model using TPS basis function can be used as alternate of Gaussian basis function for prediction of soil pore-water pressure variations.
机译:由于气候效果导致的土壤孔隙压力变化是与山坡坡分析相关的研究的一个组成部分。使用薄板花键(TPS)径向基函数的人工神经网络(ANN)技术来预测由于降雨导致的土壤坡度的土壤孔隙水压差。选择具有8-36-1(输入隐藏输出)的网络架构的径向基函数(RBF)神经网络以开发RBF模型。使用试验和错误程序选择隐性神经元数,而使用归一化方法建立基本功能的传播。时间序列降雨和孔隙压力的数据用于训练和测试RBF模型。使用根均方误差,相关系数和效率系数评估模型的性能。模型预测的结果显示,该模型产生了有希望的结果,表明TPS基函数能够预测降雨的时间序列的孔隙水压力响应。与其他研究的比较表明,使用TPS基函数的RBF模型可以用作高斯基础函数的替代,以预测土壤孔隙水压力变化。

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