Geochemical characteristics of deep groundwater from sandstone aquifer in Qianyingzi mine, northern Anhui province, China

• Published in: Water practice and technology 2014-03, Vol.9 (1), p.95-103
• Main Author: Gui, He Rong
• Format: Article
• Language: English
• Subjects: Anomalies; Aquifers; Detritus; Geochemistry; Groundwater; Isotopes; pH effects; Rare earth elements; Sandstone; Statistical analysis; Statistical methods; Total dissolved solids; Trace elements; Water analysis; Water sampling
• ISSN: 1751-231X; 1751-231X
• DOI: 10.2166/wpt.2014.011

Major ions, trace elements and isotope concentrations for eight groundwater samples were tested, which collected from sandstone aquifer in Qianyingzi mine, northern Anhui province, China. The Geochemical characteristic of groundwater samples were studied based on the conventional graphical and multivariate statistical approach, and the resulted showed: two types of groundwater could be identified through the Piper diagram, which have high concentrations total dissolved solids (1,164–5,165 mg/L), with alkaline environment (pH = 8.02–8.90) in nature; the rare earth element of groundwater samples are characterized by enrichment of HREEs compared to LREEs when normalized to PAAS, which presented from the NdSN/YbSN ratios ranging from 0.042 to 0.121, with an average 0.075; groundwater characterized by negative Ce anomalies and positive Eu anomalies, what could be caused by the Ph conditions and exchange reaction between Eu2+ and Sr2+, respectively; δ18O and δ2H of groundwater varied from −8.78 to −8.36‰ and −68.5 to −59.5‰, respectively. The detritus and the exchange reaction between groundwater and alkyl could be the reason of obviously drift of δ2H.