在半干旱的突尼斯估算浅层含盐地下水位的土壤盐度。

F. Bouksila, M. Persson, R. Berndtsson, A. Bahri, I. Hamba
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引用次数: 16

摘要

快速、可靠地观测土壤电导率对维持可持续灌溉农业至关重要。然而,直接测量饱和土膏体的电导率是一项繁琐且耗时的工作。因此,需要寻找有效的间接方法,从其他现成的观测数据中预测土壤盐度。本文探讨了多元线性回归(MLR)和人工神经网络(ANN)在半干旱突尼斯高度复杂和非均质野外条件下,从容易测量的土壤和地下水性质预测ECe变化的应用。我们比较了将数据集划分为训练子集和验证子集的两种方法;统计(SD)和随机数据集划分(RD),以及它们对模型性能的影响。输入变量选择自样地坐标、地下水位特性(深度、电导率、饼状水位)和5个深度的土壤粒度。人工神经网络和MLR的结果表明,需要考虑训练集和验证集数据的统计特性,以确保获得最优的模型性能。SD可以被认为是解决使用人工神经网络时模型过拟合问题的一种方法。对于SD,使用ANN模型时的决定系数(r2)在0.85 ~ 0.88之间,均方根误差在1.23 ~ 1.80 dS m -1之间。由于田间土壤盐分过程的复杂性和数据的空间变异性,这清楚地表明了使用人工神经网络模型预测土壤盐分的潜力。
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Estimating soil salinity over a shallow saline water table in semiarid Tunisia.
Rapid and reliable observations of soil electrical conductivity are essential in order to maintain sustainable irri- gated agriculture. Direct measurement of the electrical conductivity of saturated soil paste (ECe), however, is tedious and time consuming. Therefore, there are needs to find efficient indirect methods to predict the soil salinity from other readily available observations. In this paper we explore the application of multiple linear regression (MLR) and artificial neural networks (ANN) to predict ECe variation from easily measured soil and groundwater properties under highly complex and heterogeneous field conditions in semiarid Tunisia. We compare two methods for dividing the data set into training and validation sub-sets; a statistical (SD) and a random data set division (RD), and their effect on model performance. The in- put variables were chosen from the plot coordinates, groundwater table properties (depth, electrical conductivity, pie- zometric level), and soil particle size at 5 depths. The results obtained with ANN and MLR indicate that the statistical properties of data in the training and validation sets need to be taken into account to ensure that optimal model perform- ance is achieved. The SD can be considered as a solution to resolve the problem of over-fitting a model when using ANN. For the SD, the determination coefficient (R 2 ) when using an ANN model varied from 0.85 to 0.88 and the root mean square error from 1.23 to 1.80 dS m -1 . Because of the complexity of the field soil salinity process and the spatial variabil- ity of the data, this clearly indicates the potential to use ANN models to predict ECe.
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