Chemical modeling of groundwater in the Banat Plain, southwestern Romania, with elevated As content and co-occurring species by combining diagrams and unsupervised multivariate statistical approaches Sinziana Butaciu a , Marin Senila b , Costel Sarbu a , Michaela Ponta a , Claudiu Tanaselia b , Oana Cadar b , Marius Roman b , Emil Radu c , Mihaela Sima d , Tiberiu Frentiu a, * a Babes-Bolyai University, Faculty of Chemistry and Chemical Engineering, Arany Janos 11, 400028, Cluj-Napoca, Romania b National Institute for Research and Development of Optoelectronics Bucharest, Research Institute for Analytical Instrumentation, Donath 67, 400293, Cluj- Napoca, Romania c National Institute of Hydrology and Water Management, Bucuresti-Ploiesti 97, 013686, Bucharest, Romania d Romanian Academy, Institute of Geography, Dimitrie Racovita 12, 023993, Bucharest, Romania highlights Groundwater naturally enriched with inorganic arsenic species. Classication of groundwater sources using Fuzzy Hierarchical Cross-Clustering. PO 4 3 eAsO 4 3 ion exchange and water-rocks interactions as sources of As. Na þ eF epH cluster as marker for As naturally enriched groundwater. Co-occurrence of As species and F under the inuence of HCO 3 and alkaline pH. article info Article history: Received 15 July 2016 Received in revised form 21 December 2016 Accepted 26 December 2016 Available online 29 December 2016 Handling Editor: X. Cao Keywords: Groundwater Arsenic speciation Cluster analysis Principal component analysis Fuzzy hierarchical cross-clustering abstract The study proposes a combined model based on diagrams (Gibbs, Piper, Stuyfzand Hydrogeochemical Classication System) and unsupervised statistical approaches (Cluster Analysis, Principal Component Analysis, Fuzzy Principal Component Analysis, Fuzzy Hierarchical Cross-Clustering) to describe natural enrichment of inorganic arsenic and co-occurring species in groundwater in the Banat Plain, south- western Romania. Speciation of inorganic As (arsenite, arsenate), ion concentrations (Na þ ,K þ , Ca 2þ , Mg 2þ , HCO 3 , Cl ,F , SO 4 2 , PO 4 3 , NO 3 ), pH, redox potential, conductivity and total dissolved substances were performed. Classical diagrams provided the hydrochemical characterization, while statistical ap- proaches were helpful to establish (i) the mechanism of naturally occurring of As and F species and the anthropogenic one for NO 3 , SO 4 2 , PO 4 3 and K þ and (ii) classication of groundwater based on content of arsenic species. The HCO 3 type of local groundwater and alkaline pH (8.31e8.49) were found to be responsible for the enrichment of arsenic species and occurrence of F but by different paths. The PO 4 3- eAsO 4 3- ion exchange, water-rock interaction (silicates hydrolysis and desorption from clay) were asso- ciated to arsenate enrichment in the oxidizing aquifer. Fuzzy Hierarchical Cross-Clustering was the strongest tool for the rapid simultaneous classication of groundwaters as a function of arsenic content and hydrogeochemical characteristics. The approach indicated the Na þ eF - epH cluster as marker for groundwater with naturally elevated As and highlighted which parameters need to be monitored. A chemical conceptual model illustrating the natural and anthropogenic paths and enrichment of As and co-occurring species in the local groundwater supported by mineralogical analysis of rocks was established. © 2016 Elsevier Ltd. All rights reserved. * Corresponding author. E-mail address: ftibi@chem.ubbcluj.ro (T. Frentiu). Contents lists available at ScienceDirect Chemosphere journal homepage: www.elsevier.com/locate/chemosphere http://dx.doi.org/10.1016/j.chemosphere.2016.12.130 0045-6535/© 2016 Elsevier Ltd. All rights reserved. Chemosphere 172 (2017) 127e137