Grup de Mineralogia Aplicada i Geoquímica de Fluids, Dept. de Mineralogia, Petrologia i Geologia Aplicada, Facultat de Ciències de la Terra, Universitat de Barcelona (UB), c/Martí i Franquès s/n, 08028 Barcelona, Spain.
Département des Sciences de la Terre et de l'Atmosphère, Geotop/UQAM, Montréal, Canada.
Sci Total Environ. 2017 Feb 15;580:518-532. doi: 10.1016/j.scitotenv.2016.11.206. Epub 2016 Dec 20.
Nitrate pollution is a widespread issue affecting global water resources with significant economic and health effects. Knowledge of both the corresponding pollution sources and of processes naturally attenuating them is thus of crucial importance in assessing water management policies and the impact of anthropogenic activities. In this study, an approach combining hydrodynamic, hydrochemical and multi-isotope systematics (8 isotopes) is used to characterize the sources of nitrate pollution and potential natural attenuation processes in a polluted basin of NE Spain. δH and δO isotopes were used to further characterize the sources of recharge of the aquifers. Results show that NO is not homogeneously distributed and presents a large range of concentrations, from no NO to up to 480mgL. δN and δO of dissolved NO identified manure as the main source of nitrate, although sewage and mineral fertilizers can also be isotopically detected using boron isotopes (δB) and δS and δO of dissolved sulphate, respectively. The multi-isotope approach proved that natural denitrification is occurring, especially in near-river environments or in areas hydrologically related to fault zones. δS and δO indicated that denitrification is not driven by pyrite oxidation but rather by the oxidation of organic matter. This could not be confirmed by the study of δC that was buffered by the entanglement of other processes and sources.
硝酸盐污染是一个全球性的水资源问题,对经济和健康都有重大影响。因此,了解硝酸盐污染的相应来源以及自然衰减过程对于评估水管理政策和人为活动的影响至关重要。在本研究中,采用了一种结合水动力、水化学和多同位素系统(8 种同位素)的方法,以表征西班牙东北部一个受污染流域的硝酸盐污染来源和潜在的自然衰减过程。δH 和 δO 同位素用于进一步表征含水层补给的来源。结果表明,NO 并不是均匀分布的,其浓度范围很大,从无 NO 到高达 480mg/L。溶解态 NO 的 δN 和 δO 表明,尽管使用硼同位素(δB)和溶解态硫酸盐的 δS 和 δO 也可以在同位素上检测到污水和矿物肥料,但粪肥是硝酸盐的主要来源。多同位素方法证明了自然反硝化作用的发生,特别是在近河环境或与断层带水力学相关的区域。δS 和 δO 表明,反硝化作用不是由黄铁矿氧化驱动的,而是由有机物的氧化驱动的。这一点无法通过研究被其他过程和来源纠缠的缓冲 δC 来证实。