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 irrigated 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...

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Bibliographic Details
Published inThe open hydrology journal Vol. 4; pp. 91 - 101
Main Authors Bouksila, Fethi, Persson, Magnus, Berndtsson, Ronny, Bahri, Akissa
Format Journal Article
LanguageEnglish
Published 01.12.2010
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Summary:Rapid and reliable observations of soil electrical conductivity are essential in order to maintain sustainable irrigated 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 input variables were chosen from the plot coordinates, groundwater table properties (depth, electrical conductivity, piezometric 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 performance 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[super]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[super]-1. Because of the complexity of the field soil salinity process and the spatial variability of the data, this clearly indicates the potential to use ANN models to predict ECe.
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ISSN:1874-3781
1874-3781
DOI:10.2174/1874378101003010091