Seawater intrusion mapping using electrical resistivity tomography and hydrochemical data. An application in the coastal area of eastern Thermaikos Gulf, Greece
Autor: | G. Soulios, Konstantinos Voudouris, A. Pavlou, George Vargemezis, F. Pliakas, Nerantzis Kazakis, G. Tsokas |
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Rok vydání: | 2015 |
Předmět: |
Wet season
Hydrology geography Environmental Engineering Soil salinity geography.geographical_feature_category Seawater intrusion 0208 environmental biotechnology Borehole Aquifer 02 engineering and technology 010501 environmental sciences 01 natural sciences Pollution 020801 environmental engineering Environmental Chemistry Seawater Electrical resistivity tomography Waste Management and Disposal Groundwater Geology 0105 earth and related environmental sciences |
Zdroj: | The Science of the total environment. 543 |
ISSN: | 1879-1026 |
Popis: | The aim of this study was to determine the extent and geometrical characteristics of seawater intrusion in the coastal aquifer of the eastern Thermaikos Gulf, Greece. Hydrochemical data and geoelectrical measurements were combined and supplemented to determine the hydrochemical regime of the study site in regard to seawater phenomena. Chemical analysis of groundwater was performed in 126 boreholes and fifteen electrical resistivity tomographies (ERT) were measured, whereas in two sites the ERT measurements were repeated following the wet season. The Cl(-) concentrations recorded reached 2240 mg/L indicating seawater intrusion which was also verified by ionic ratios. The ionic ratios were overlapped and a seawater intrusion map (SWIM) was produced. A significant part of the coastal aquifer (up to 150 km(2)) is influenced by seawater intrusion. The areas with the most intensive salinization are located between Nea Kallikratia-Epanomi and Aggelochori-Peraia. According to the ERTs, in the influenced areas the salinization of the aquifer exceeds 1 km toward the mainland and its depth reaches 200 m. In the area surrounding Thessaloniki airport, the ERTs revealed salinization of the upper aquifer to depths of up to 40 m, whereas the lower aquifer is uninfluenced. This abnormal distribution of seawater intrusion demonstrates the value of geoelectrical methods in the study of seawater intrusion especially in areas with limited available hydrochemical data. |
Databáze: | OpenAIRE |
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