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Simulation of Soil Water Retention Curve using Artificial Neural Networks with Pseudocontinuous Pedotransfer Functions

机译:利用伪连续Pedo传递函数的人工神经网络模拟土壤保水曲线

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摘要

Artificial neural networks for estimating the soil water retention curve have been developed considering measured data and require a large quantity of soil samples because only retention curve data obtained for the same set of matric potentials can be used. In order to preclude this drawback, we present two ANN models which tested the performance of ANNs trained with fitted water contents data. These models were compared to a recent new ANN approach for predicting water retention curve, the pseudocontinuous pedotransfer functions (PTFs), which is also an attempt to deal with limited data. Additionally, a sensitivity analysis was carried out to verify the influence of each input parameter on each output. Results showed that fitted ANNs provided similar statistical indexes in predicting water contents to those obtained by the pseudocontinuous method. Sensitivity analysis revealed that bulk density and porosity are the most important parameters for predicting water contents in wet regime, whereas sand and clay contents are more significant in drier conditions. The sensitivity analysis for the pseudocontinuous method demonstrated that the natural logarithm of the matric potential became the most important parameter, and the influences of all other inputs were reduced to be not relevant, except the bulk density.
机译:考虑到测量数据,已经开发了用于估计土壤保水曲线的人工神经网络,并且需要大量的土壤样品,因为只能使用针对同一组基质势获得的保水曲线数据。为了避免这一缺点,我们提出了两个神经网络模型,用于测试用拟合水含量数据训练的人工神经网络的性能。这些模型与最近的一种新的ANN方法(用于预测保水曲线)进行了比较,该方法是伪连续的pedotransfer函数(PTF),这也是尝试处理有限的数据。此外,进行了敏感性分析,以验证每个输入参数对每个输出的影响。结果表明,拟合的人工神经网络在预测含水量方面提供了与拟连续方法相似的统计指标。敏感性分析表明,堆积密度和孔隙率是预测湿态含水量的最重要参数,而在干燥条件下,沙子和粘土的含量更为重要。伪连续法的灵敏度分析表明,矩阵势的自然对数成为最重要的参数,除堆积密度外,所有其他输入的影响均减小。

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