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Developing a Long Short-Term Memory (LSTM) based model for predicting water table depth in agricultural areas

机译:基于长期内存(LSTM)的模型,用于预测农业区水台深度

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Predicting water table depth over the long-term in agricultural areas presents great challenges because these areas have complex and heterogeneous hydrogeological characteristics, boundary conditions, and human activities; also, nonlinear interactions occur among these factors. Therefore, a new time series model based on Long Short-Term Memory (LSTM), was developed in this study as an alternative to computationally expensive physical models. The proposed model is composed of an LSTM layer with another fully connected layer on top of it, with a dropout method applied in the first LSTM layer. In this study, the proposed model was applied and evaluated in five sub-areas of Hetao Irrigation District in arid northwestern China using data of 14 years (2000-2013). The proposed model uses monthly water diversion, evaporation, precipitation, temperature, and time as input data to predict water table depth. A simple but effective standardization method was employed to pre-process data to ensure data on the same scale. 14 years of data are separated into two sets: training set (2000-2011) and validation set (2012-2013) in the experiment. As expected, the proposed model achieves higher R-2 scores (0.789-0.952) in water table depth prediction, when compared with the results of traditional feed-forward neural network (FFNN), which only reaches relatively low R-2 scores (0.004-0.495), proving that the proposed model can preserve and learn previous information well. Furthermore, the validity of the dropout method and the proposed model's architecture are discussed. Through experimentation, the results show that the dropout method can prevent overfitting significantly. In addition, comparisons between the R-2 scores of the proposed model and Double-LSTM model (R-2 scores range from 0.170 to 0.864), further prove that the proposed model's architecture is reasonable and can contribute to a strong learning ability on time series data. Thus, one can conclude that the proposed model can
机译:预测地下水位深度在农业领域呈现长期的,因为这些地区有复杂多样的水文地质特征,边界条件和人类活动的巨大挑战;还,这些因素之间发生非线性相互作用。因此,基于长短期记忆(LSTM)一个新的时间序列模型,在这项研究中开发,以替代昂贵的计算物理模型。该模型是由一个LSTM层与在它上面的另一完全连接层,与第一层LSTM施加的压差的方法。在这项研究中,提出的模型应用于使用14年(2000-2013)的数据在干旱中国西北河套灌区的五个子区域评估。所提出的模型采用每月引水,蒸发,沉淀,温度和时间作为输入数据来预测地下水位深度。采用了这样的简单而有效的方法标准化预先处理数据,以确保在同一比例的数据。在实验中训练集(2000年至2011年),并验证集(2012-2013):14年的数据被分成两个集合。如所预期的,所提出的模型实现了在地下水位深度预测更高R-2得分(0.789-0.952)中,当与传统的前馈神经网络的结果(FFNN),其仅达到相对低的R-2的分数进行比较(0.004 -0.495),证明该模型可以保存和学习以前的信息很好。此外,辍学方法和所提出的模型架构的有效性进行了讨论。通过实验,结果表明,辍学方法可以防止过度拟合显著。此外,所提出的模型和双LSTM模型(R-2得分范围从0.170至0.864)的R-2的分数之间的比较,进一步证实,该模型的结构是合理的,可以向在时间较强的学习能力系列数据。因此,可以得出结论,该模型能

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