Kelepertzis Efstratios, Matiatos Ioannis, Botsou Fotini, Antonopoulou Christina, Lappas Ioannis, Dotsika Elissavet, Chrastný Vladislav, Boeckx Pascal, Karavoltsos Sotirios, Komárek Michael
Department of Geology and Geoenvironment, National and Kapodistrian University of Athens, Panepistimiopolis, Zographou, 15784, Athens, Greece.
Hellenic Centre for Marine Research, 46.7 km of Athens-Sounio Ave., 19013 Anavissos Attikis, Greece.
Sci Total Environ. 2023 Feb 1;858(Pt 1):159763. doi: 10.1016/j.scitotenv.2022.159763. Epub 2022 Oct 26.
The Atalanti basin is an intensively cultivated area in central Greece, facing groundwater quality deterioration threats due to natural and anthropogenic-related contamination sources. A combination of statistical and hydrogeochemical techniques, and stable isotope compositions (δH-HO and δΟ-ΗΟ, δΝ-ΝΟ and δΟ-ΝΟ, δS-SO and δO-SO) were applied to elucidate the origin of salinity and nitrate contamination, and shed light on the potential associations between geogenic Cr(VI) and NO sources and transformations. Nitrate and Cr(VI) concentrations reached up to 337 mg L and 76.1 μg L, respectively, exceeding WHO threshold values in places. The cluster of samples with the high salinity was mostly influenced by irrigation return flow and marine aerosols, and less by seawater intrusion, as evidenced by the ionic ratios (e.g., Na/Cl) and the stable isotopes of oxygen and hydrogen in water, and sulphur and oxygen in sulphates. The δΝ-ΝΟ and δO-NO values ranged from +2.0 ‰ to +14.5 ‰ and + 0.3 ‰ to +11.0 ‰, respectively. We found that the dominant sources of NO in groundwater were fertilizers in the central part of the area and sewage waste in the northern part around the residential area of Livanates. The occurrence of denitrification was evident in the northern part of the basin, where the DO levels were lowest (≤ 2.2 mg L), whereas nitrification of NH-fertilizers prevailed in the central part. Elevated Cr(VI) values (≥ 20 μg/l) were associated with the lowest deviation of the measured from the theoretical nitrification δΟ-NO values, whereas the lowest Cr(VI) values were observed in the denitrified water samples. Our isotope findings revealed the strong influence of redox conditions on the biogeochemical transformations of N species and the mobilization of Cr(VI) that will help improve the understanding of the fate of these contaminants from the unsaturated zone to the groundwater in areas of agricultural and urban land use.
阿塔兰蒂盆地是希腊中部一个集约化种植区,由于自然和人为相关的污染源,面临着地下水质量恶化的威胁。运用统计和水文地球化学技术以及稳定同位素组成(δH-H₂O和δ¹⁸O-H₂O、δ¹⁵N-NO₃和δ¹⁸O-NO₃、δ³⁴S-SO₄和δ¹⁸O-SO₄)来阐明盐度和硝酸盐污染的来源,并揭示地质成因的Cr(VI)与NO₃来源及转化之间的潜在关联。硝酸盐和Cr(VI)浓度分别高达337 mg/L和76.1 μg/L,部分地区超过了世界卫生组织的阈值。高盐度样品组主要受灌溉回流和海洋气溶胶影响,受海水入侵影响较小,这由离子比率(如Na/Cl)以及水中氧和氢、硫酸盐中硫和氧的稳定同位素所证明。δ¹⁵N-NO₃和δ¹⁸O-NO₃值分别在+2.0‰至+14.5‰和+0.3‰至+11.0‰之间。我们发现,该区域中部地下水中NO₃的主要来源是化肥,而在利瓦纳特斯居民区北部,NO₃的主要来源是污水。反硝化作用在盆地北部明显存在,那里溶解氧水平最低(≤2.2 mg/L),而中部则以铵态氮肥的硝化作用为主。Cr(VI)值升高(≥20 μg/l)与实测硝化δ¹⁸O-NO₃值与理论值的最小偏差相关,而在反硝化水样中观察到最低的Cr(VI)值。我们的同位素研究结果揭示了氧化还原条件对氮物种生物地球化学转化和Cr(VI)迁移的强烈影响,这将有助于加深对农业和城市土地利用区域中这些污染物从不饱和带到地下水的归宿的理解。