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Stable isotopes of water as a tool to study groundwater–seawater interactions in coastal south-eastern Sicily
Stable isotopes of hydrogen (δD) and oxygen (δ 18O) in groundwater, submarine springs and seawater collected in coastal south-eastern Sicily were investigated. While the spatial distribution of δ 18O in groundwater showed that most of the heavy-isotope-depleted samples (from −5.7‰ to −6.9‰) were loc...
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Published in: | Journal of hydrology (Amsterdam) 2009-01, Vol.364 (1), p.40-49 |
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Main Authors: | , , |
Format: | Article |
Language: | English |
Subjects: | |
Citations: | Items that this one cites Items that cite this one |
Online Access: | Get full text |
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Summary: | Stable isotopes of hydrogen (δD) and oxygen (δ
18O) in groundwater, submarine springs and seawater collected in coastal south-eastern Sicily were investigated. While the spatial distribution of δ
18O in groundwater showed that most of the heavy-isotope-depleted samples (from −5.7‰ to −6.9‰) were located in the higher portion of the Hyblean Mountains, more positive values (from −3.4‰ to −5.6‰) were found in the marginal areas. The isotope composition of submarine springs was characterized by significant variability (δ
18O between −5.6‰ and +1.0‰ and δD between −30‰ and +5.0‰) reflecting seasonal variations and different seawater contributions. The isotopic and chemical composition of coastal groundwater showed the presence of a surficial aquifer, while the composition of inland groundwater and beach springs characterizes a deeper limestone aquifer. The amount of NO
3 entering the sea from land-based sources was estimated to be >60
kg/day, which could be of potential environmental concern. Since the submarine groundwater manifestations are fed by coastal contaminated groundwater and re-circulated seawater, environmental implication on the freshwater resources management in the region is of particular interest, especially their protection against contaminants from land-based sources represented by growing agricultural activities in the region. |
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ISSN: | 0022-1694 1879-2707 |
DOI: | 10.1016/j.jhydrol.2008.10.005 |