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090			_aB-21094
245	1	0	_aControls of evaporative irrigation return flows in comparison to seawater intrusion in coastal karstic aquifers in northern Sri Lanka: evidence from solutes and stable isotopes
490	0		_vScience of the Total Environment, 548, p.421-428, 2016
520	3		_aGroundwater in Miocene karstic aquifers in the Jaffna Peninsula of Sri Lanka is an important resource since no other fresh water sources are available in the region. The subsurface is characterized by highly productive limestone aquifers that are used for drinking and agriculture purposes. A comprehensive hydrogeochemical study was carried out to reveal the processes affecting the groundwater quality in this region.Major and trace element composition and environmental isotope ratios of oxygen and hydrogen (?18OH2O and ?2HH2O)were determined in 35 groundwater samples for this investigation. The ion abundance of groundwater in the region was characterized by an anion sequence orderwith HCO3? N Cl? N SO4? N NO3?. For cations, average Na++K+ contents in groundwater exceeded those of Ca2++Mg2+ in most cases. Ionic relationships of major solutes indicated open system calcite dissolution while seawater intrusions are also evident but only close to the coast. The solute contents are enriched by agricultural irrigation returns and associated evaporation. This was confirmed by the stable isotope composition of groundwater that deviated fromthe localmeteoricwater line (LMWL)and formed its own regression line denoted as the local evaporation line (LEL). The latter can be described by ?2HH2O = 5.8 × ?18OH2O -- 2.9. Increased contents of nitrate-N (up to 5 mg/L), sulfate (up to 430 mg/L)and fluoride (up to 1.5 mg/L)provided evidences for anthropogenic inputs of solutes, most likely from agriculture activities. Among trace elements Ba, Sr, As and Se levels in the Jaffna groundwaterwere higher compared to that of the dry zone metamorphic aquifers in Sri Lanka. Solute geochemistry and stable isotope evidences from the región indicates that groundwater in the area is mainly derived from local modern precipitation but modified heavily by progressive evaporative concentration rather than seawater intrusion.
650	1	4	_aWATER STABLE ISOTOPES
650	1	4	_aCALCITE DISSOLUTION
650	1	4	_aCARBONATE AQUIFERS
650	1	4	_aIRRIGATION RETURN FLOWS
650	1	4	_aGROUNDWATER QUALITY
650	1	4	_aSELENIUM
700	1	2	_aChandrajith, R.
700	1	2	_aDiyabalanage, S.
700	1	2	_aPremathilake, K. M.
700	1	2	_aHanke, C.
700	1	2	_aVan Geldern, R.
700	1	2	_aBarth, J. A.
856	4	0	_uhttps://drive.google.com/open?id=1Dd5CSDxFXTTFg_8Oc0Q2hu-ivAhG61ZA&usp=drive_copy _zPara ver el documento ingresa a Google con tu cuenta: @cicy.edu.mx
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