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Investigation of the intrusion of saltwater- freshwater interface along the eastern coast of Sri Lanka

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dc.contributor.author Fatheena, M. S. F.
dc.contributor.author Udagedara, D. T.
dc.contributor.author Adhikaram, A. M. N. M.
dc.contributor.author Karunarathne, S.
dc.date.accessioned 2025-08-28T04:03:04Z
dc.date.available 2025-08-28T04:03:04Z
dc.date.issued 2025-02-28
dc.identifier.citation Proceedings of the 41st Annual Technical Sessions “Innovations in Mineral Resource Optimization” 28th February 2025, Geological Society of Sri Lanka (GSSL) HQRS, Department of Geology, University of Peradeniya, Peradeniya. pp. 13. en_US
dc.identifier.issn 2362-0420
dc.identifier.uri http://www.gsslweb.org
dc.identifier.uri http://ir.lib.seu.ac.lk/handle/123456789/7623
dc.description.abstract Coastal aquifers are highly vulnerable to seawater intrusion due to natural and anthropogenic factors such as over-extraction, sea-level rise, and geological conditions. The shallow coastal aquifer along Sri Lanka’s eastern coast faces salinization risks due to overexploitation. This study focused on a 50 km stretch from Kallady to Karaitivu, where 47 groundwater samples were collected from deep tube wells (25) and dug wells (21) along ten transects spaced at 5 km intervals. Each transect included at least five wells, with samples taken 300–500 meters apart. Groundwater chemistry was analyzed using pH, electrical conductivity (EC), total dissolved solids (TDS), salinity, and major ion concentrations, alongside hydrochemical classification methods such as Piper diagrams and saltwater intrusion indicators. pH values ranged from 6.37 to 7.44, with most samples exhibiting mildly acidic to neutral conditions. EC values varied significantly, with 72.34% of the samples surpassing the freshwater threshold, indicating potential seawater intrusion. TDS levels further confirmed this, with some samples exceeding the WHO drinking water limit of 1,000 mg/l. The dominant ions detected were sodium (Na⁺), calcium (Ca²⁺), and bicarbonates (HCO₃⁻), reflecting geological influences and ion exchange processes. Piper diagram analysis classified 82.98% of the samples as Ca-Mg-HCO₃ type, characteristic of freshwater influenced by rock weathering and mineral dissolution. Saltwater intrusion indicators, including the chloride-bicarbonate ratio, sodium-chloride ratio, and base exchange indices (BEX), revealed that 91.49% of contamination was due to seawater intrusion, while 8.51% was linked to anthropogenic activities. BEX values showed that 87.23% of samples were undergoing a freshening process, although localized salinization persisted. Isolated saline intrusion zones were identified at 250 m, 300 m, and 500–600 m from the coastline in the highly populated areas of Koddaikallar South, Karaitivu, and Kalmunai respectively. The study underscores the need for continuous monitoring and groundwater management strategies to mitigate saltwater intrusion and ensure long-term water sustainability. en_US
dc.language.iso en_US en_US
dc.publisher Geological Society of Sri Lanka (GSSL), Department of Geology, University of Peradeniya, Peradeniya. en_US
dc.subject Groundwater en_US
dc.subject Seawater Intrusion en_US
dc.subject Hydrogeochemical Processes en_US
dc.subject Groundwater Quality en_US
dc.title Investigation of the intrusion of saltwater- freshwater interface along the eastern coast of Sri Lanka en_US
dc.type Article en_US


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