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Simulation of rainfall-underground outflow responses of a karstic watershed in Southwest China with an artificial neural network

机译:基于人工神经网络的西南喀斯特流域降雨-地下渗流响应模拟。

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In the karstic system, numerous karstic features influence hydrologic behavior. Underground stream discharges reflect the fluctuation of ground water level and variability of ground water storage in the watersheds. However, karstic aquifers in southwest China are largely located in the mountain areas and observation data of groundwater level are usually absent. Therefore, numerical groundwater models are inappropriate for simulation of groundwater flow and rainfall-underground outflow responses. In this study, an artificial neural network (ANN) model was developed to simulate underground stream flow discharges. ANN model was applied in the Houzhai subterranean drainage watershed in Guizhou Province of southwest China, a representative of karstic geomorphology in the humid areas of China. Correlation was used to determine the model inputs and time-lags between inputs and outputs. ANN model was trained using the error backpropagation algorithm and validated at three hydrological stations with different karstic features. Study results show that the ANN model performs well for the modeling of karstic aquifers, which are highly non-linear systems. The ANN model offers a promising tool for better understanding of karstic hydrological processes and thus estimation of groundwater resources in the karstic aquifer.
机译:在岩溶系统中,许多岩溶特征影响水文行为。地下流排放反映了地下水位的波动和流域中地下水存储量的变化。但是,中国西南地区的岩溶含水层主要位于山区,通常缺乏地下水位的观测数据。因此,数值地下水模型不适用于模拟地下水流量和降雨-地下流出响应。在这项研究中,开发了一个人工神经网络(ANN)模型来模拟地下流的流量。在中国西南贵州省后寨地下排水流域中应用了ANN模型,该模型是中国湿润地区岩溶地貌的代表。相关性用于确定模型输入以及输入和输出之间的时滞。使用误差反向传播算法训练了人工神经网络模型,并在三个具有不同岩溶特征的水文站进行了验证。研究结果表明,ANN模型在岩溶含水层的建模中表现良好,岩溶含水层是高度非线性的系统。人工神经网络模型为更好地了解岩溶水文过程,从而估算岩溶含水层中的地下水资源提供了有希望的工具。

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