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Hydrology and Earth System Sciences An interactive open-access journal of the European Geosciences Union
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Volume 19, issue 3
Hydrol. Earth Syst. Sci., 19, 1353–1370, 2015
https://doi.org/10.5194/hess-19-1353-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.

Special issue: Groundwater resources and their ecosystem services: new methods...

Hydrol. Earth Syst. Sci., 19, 1353–1370, 2015
https://doi.org/10.5194/hess-19-1353-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 12 Mar 2015

Research article | 12 Mar 2015

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

S. Luoma1, J. Okkonen2, K. Korkka-Niemi3, N. Hendriksson1, and B. Backman1 S. Luoma et al.
  • 1Geological Survey of Finland, P.O. Box 96, 02151 Espoo, Finland
  • 2Geological Survey of Finland, P.O. Box 97, 67101 Kokkola, Finland
  • 3Department of Geosciences and Geography, University of Helsinki, P.O. Box 64, 00014 Helsinki, Finland

Abstract. 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.

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