Abstract

Knowledge of the groundwater potential, especially in an arid region, can play a major role in planning the sustainable management of groundwater resources. In this study, nine machine learning (ML) algorithms—namely, Artificial Neural Network (ANN), Decision Jungle (DJ), Averaged Perceptron (AP), Bayes Point Machine (BPM), Decision Forest (DF), Locally-Deep Support Vector Machine (LD-SVM), Boosted Decision Tree (BDT), Logistic Regression (LG), and Support Vector Machine (SVM)—were run on the Microsoft Azure cloud computing platform to model the groundwater potential. We investigated the relationship between 512 operating boreholes with a specified specific capacity and 14 groundwater-influencing occurrence factors. The unconfined aquifer in the Nineveh plain, Mosul Governorate, northern Iraq, was used as a case study. The groundwater-influencing factors used included elevation, slope, curvature, topographic wetness index, stream power index, soil, land use/land cover (LULC), geology, drainage density, aquifer saturated thickness, aquifer hydraulic conductivity, aquifer specific yield, depth to groundwater, distance to faults, and fault density. Analysis of the contribution of these factors in groundwater potential using information gain ratio indicated that aquifer saturated thickness, rainfall, hydraulic conductivity, depth to groundwater, specific yield, and elevation were the most important factors (average merit > 0.1), followed by geology, fault density, drainage density, soil, LULC, and distance to faults (average merit < 0.1). The average merits for the remaining factors were zero, and thus, these factors were removed from the analysis. When the selected ML classifiers were used to estimate groundwater potential in the Azure cloud computing environment, the DJ and BDT models performed the best in terms of all statistical error measures used (accuracy, precision, recall, F-score, and area under the receiver operating characteristics curve), followed by DF and LD-SVM. The probability of groundwater potential from these algorithms was mapped and visualized into five groundwater potential zones: very low, low, moderate, high, and very high, which correspond to the northern (very low to low), southern (moderate), and middle (high to very high) portions of the study area. Using a cloud computing service provides an improved platform for quickly and cheaply running and testing different algorithms for predicting groundwater potential.

Highlights

  • Groundwater is a vital resource for supplying drinking water for millions of people around the world, as well as for agriculture, industry, and preserving the natural environment

  • The Boosted Decision Tree (BDT) model showed the highest performance concerning the classification of high potential locations, having a recall index of 0.82, followed by Locally-Deep Support Vector Machine (LD-Support Vector Machine (SVM)) (0.81), Decision Jungle (DJ) (0.80), and Decision Forest (DF) (0.78)

  • The F-score was best for DJ (0.86), followed by BDT (0.85) and LD-SVM (0.83)

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Summary

Introduction

Groundwater is a vital resource for supplying drinking water for millions of people around the world, as well as for agriculture, industry, and preserving the natural environment. Traditional groundwater mapping requires a lot of effort and money, especially in remote areas or developing countries. This necessitates the development of new methods to make groundwater exploration and assessment as effective as possible. The term groundwater potential denotes the amount of groundwater available in an area, and it is a function of several hydrologic and hydrogeological factors [8] This definition, from our point of view, is too simple, as the groundwater potential in an area is the outcome of a complex process that is not influenced by hydrological and hydrogeological elements. Many other factors such as geology and structural setting, geomorphology, and topography can influence groundwater accumulation. The most accurate definition should be as follows: groundwater potential denotes the amount of groundwater available in an area, and it is a function of several surface and subsurface factors

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