Confronting the vicinity of the surface water and sea shore in a shallow glaciogenic aquifer in southern Finland

• Main Authors: S. Luoma, J. Okkonen, K. Korkka-Niemi, N. Hendriksson, B. Backman
• Format: Article
• Language: English
• Published: Copernicus Publications 2015-03-01
• Series: Hydrology and Earth System Sciences
• Online Access: http://www.hydrol-earth-syst-sci.net/19/1353/2015/hess-19-1353-2015.pdf
• ISSN: 1027-5606; 1607-7938

The groundwater in a shallow, unconfined, low-lying coastal aquifer in Santala, southern Finland, was chemically characterised by integrating multivariate statistical approaches, principal component analysis (PCA) and hierarchical cluster analysis (HCA), based on the stable isotopes δ²H and δ¹⁸O, hydrogeochemistry and field monitoring data. PCA and HCA yielded similar results and classified groundwater samples into six distinct groups that revealed the factors controlling temporal and spatial variations in the groundwater geochemistry, such as the geology, anthropogenic sources from human activities, climate and surface water. High temporal variation in groundwater chemistry directly corresponded to precipitation. With an increase in precipitation, KMnO₄ consumption, EC, alkalinity and Ca concentrations also increased in most wells, while Fe, Al, Mn and SO₄ were occasionally increased during spring after the snowmelt under specific geological conditions. The continued increase in NO₃ and metal concentrations in groundwater indicates the potential contamination risk to the aquifer. Stable isotopes of δ¹⁸O and δ²H indicate groundwater recharge directly from meteoric water, with an insignificant contribution from lake water, and no seawater intrusion into the aquifer. Groundwater geochemistry suggests that local seawater intrusion is temporarily able to take place in the sulfate reduction zone along the freshwater and seawater mixed zone in the low-lying coastal area, but the contribution of seawater was found to be very low. The influence of lake water could be observed from higher levels of KMnO₄ consumption in wells near the lake. The integration of PCA and HCA with conventional classification of groundwater types, as well as with the hydrogeochemical data, provided useful tools to identify the vulnerable groundwater areas representing the impacts of both natural and human activities on water quality and the understanding of complex groundwater flow system for the aquifer vulnerability assessment and groundwater management in the future.