Abstract

The drinking and irrigation water scarcity is a major global issue, particularly in arid and semi-arid zones. In rural areas, groundwater could be used as an alternative and additional water supply source in order to reduce human suffering in terms of water scarcity. In this context, the purpose of the present study is to facilitate groundwater potentiality mapping via spatial-modelling techniques, individual and ensemble machine-learning models. Random forest (RF), logistic regression (LR), decision tree (DT) and artificial neural networks (ANNs) are the main algorithms used in this study. The preparation of groundwater potentiality maps was assembled into 11 ensembles of models. Overall, about 374 groundwater springs was identified and inventoried in the mountain area. The spring inventory data was randomly divided into training (75%) and testing (25%) datasets. Twenty-four groundwater influencing factors (GIFs) were selected based on a multicollinearity test and the information gain calculation. The results of the groundwater potentiality mapping were validated using statistical measures and the receiver operating characteristic curve (ROC) method. Finally, a ranking of the 15 models was achieved with the prioritization rank method using the compound factor (CF) method. The ensembles of models are the most stable and suitable for groundwater potentiality mapping in mountainous aquifers compared to individual models based on success and prediction rate. The most efficient model using the area under the curve validation method is the RF-LR-DT-ANN ensemble of models. Moreover, the results of the prioritization rank indicate that the best models are the RF-DT and RF-LR-DT ensembles of models.

Highlights

  • Mountainous areas cover more than 20% of the Earth’s land surface where 25% of the global population lives [1]

  • Two methods were applied for the factors selection which contribute to springs emergence (IG) and variance inflation factor (VIF). (2) A frequency ratio method was applied to determine the spatial relationships between spring occurrence and its predisposing factors

  • (3) Random forest (RF), logistic regression (LR), decision tree (DT) and artificial neural networks (ANNs) models were applied for mapping groundwater potential; different ensemble of models were tested in order to find the best rate of prediction, in addition to the production of various groundwater potentiality maps

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Summary

Introduction

Mountainous areas cover more than 20% of the Earth’s land surface where 25% of the global population lives [1]. The mountains areas are well known to provide 50% of freshwater [2] compared to the other critical resources (i.e., food and wood). These areas constitute the main recharge areas of several porous and continuous aquifers in downstream lowland regions [3,4,5]. The groundwater potential in mountainous aquifers is governed by several parameters (i.e., lithology, geomorphology, topography, secondary porosity, geological structures, fracture density, permeability, drainage pattern and density, groundwater recharge, piezometric level, slope, land use/cover and climatic conditions, and their interrelationships) [7]

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