Journal
APPLIED SCIENCES-BASEL
Volume 11, Issue 16, Pages -Publisher
MDPI
DOI: 10.3390/app11167595
Keywords
self-organizing maps; hydrogeochemical statistical data analysis; groundwater body conceptualization; coastal aquifer
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The hydrogeochemical characteristics of a significant subterranean water body in Italy were evaluated using multivariate statistical analysis methods, revealing that major ions had a significant influence over groundwater chemistry. Three clusters were identified based on the chemical characteristics of the water samples: low salinity/mixed waters, high salinity waters, and low salinity/fresh waters. Temporal changes in cluster assignment were observed in only two wells, indicating the impact of hydrodynamic conditions on groundwater chemistry. The results were also displayed using the classical hydrochemical approach of the Piper plot, showing the effectiveness of this method in quickly analyzing large datasets and identifying spatiotemporal patterns.
The hydrogeochemical characteristics of the significant subterranean water body between Cecina River and San Vincenzo (Italy) was evaluated using multivariate statistical analysis methods, like principal component analysis and self-organizing maps (SOMs), with the objective to study the spatiotemporal relationships of the aquifer. The dataset used consisted of the chemical composition of groundwater samples collected between 2010 and 2018 at 16 wells distributed across the whole aquifer. For these wells, all major ions were determined. A self-organizing map of 4 x 8 was constructed to evaluate spatiotemporal changes in the water body. After SOM clustering, we obtained three clusters that successfully grouped all data with similar chemical characteristics. These clusters can be viewed to reflect the presence of three water types: (i) Cluster 1: low salinity/mixed waters; (ii) Cluster 2: high salinity waters; and (iii) Cluster 3: low salinity/fresh waters. Results showed that the major ions had the greater influence over the groundwater chemistry, and the difference in their concentrations allowed the definition of three clusters among the obtained SOM. Temporal changes in cluster assignment were only observed in two wells, located in areas more susceptible to changes in the water table levels, and therefore, hydrodynamic conditions. The result of the SOM clustering was also displayed using the classical hydrochemical approach of the Piper plot. It was observed that these changes were not as easily identified when the raw data were used. The spatial display of the clustering results, allowed the evaluation in a hydrogeological context in a quick and cost-effective way. Thus, our approach can be used to quickly analyze large datasets, suggest recharge areas, and recognize spatiotemporal patterns.
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