AI Article Synopsis

  • The study aims to identify and assess groundwater potential zones (GWPZs) using advanced machine learning techniques like Random Forest (RF) and Support Vector Machine (SVM).
  • GWPZs are determined by analyzing factors such as geology, drainage density, and land use, utilizing datasets that include both potential and non-potential sites.
  • The RF model outperformed the SVM model in accuracy (AUC of 0.91 vs. 0.88), highlighting that high GWPZs are found in water bodies and forests, while low GWPZs tend to be in shrubland and grassland, providing crucial insights for sustainable groundwater management.

Article Abstract

The main objective of this study is to map and evaluate groundwater potential zones (GWPZs) using advanced ensemble machine learning (ML) models, notably Random Forest (RF) and Support Vector Machine (SVM). GWPZs are identified by considering essential factors such as geology, drainage density, slope, land use/land cover (LULC), rainfall, soil, and lineament density. This is combined with datasets used for training and validating the RF and SVM models, which consisted of 75 potential sites (boreholes and springs), 22 non-potential sites (bare lands and settlement areas), and 20 potential sites (water bodies). Each dataset is randomly partitioned into two sets: training (70%) and validation (30%). The model's performance is evaluated using the area under the receiver operating characteristic curve (AUC-ROC). The AUC of the RF model is 0.91, compared to 0.88 for the SVM model. Both models classified GWPZs effectively, but the RF model performed slightly better. The classified GWPZ map shows that high GWPZs are typically located within water bodies, natural springs, low-lying regions, and forested areas. In contrast, low GWPZs are primarily found in shrubland and grassland areas. This study is vital for decision-makers as it promotes sustainable groundwater use and ensures water security in the studied area.

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Source
http://www.ncbi.nlm.nih.gov/pmc/articles/PMC11637779PMC
http://dx.doi.org/10.1002/gch2.202400137DOI Listing

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