Faulty of Geosciences and Environmental Engineering, Southwest Jiaotong University, Chengdu 610031, China.
Faulty of Geosciences and Environmental Engineering, Southwest Jiaotong University, Chengdu 610031, China.
Sci Total Environ. 2020 May 15;717:137134. doi: 10.1016/j.scitotenv.2020.137134. Epub 2020 Feb 4.
Nitrate (NO) contamination in groundwater is an environmental problem worldwide. Partitioning the pollution into its sources is the key for effective controls. In this study, NO dual isotopic compositions (δN-NO and δO-NO) were measured in groundwater samples from 28 wells in an area with multiple land-uses, followed by the application of an isotope mixing model (SIAR) to identify the main NO sources and their biogeochemical processes. The results showed that denitrification was unlikely occur at significant rates, while nitrification was an important nitrogen transformation processes. Spatial variation of groundwater NO and its isotopic compositions was associated with the land-use types. Agricultural areas were characterized by relatively high NO concentrations and low δN-NO values. In contrast, industrial areas were characterized by enriched δN-NO and δO-NO values. In crop field, vegetable field and poultry and livestock breading farm, the proportional contribution represented a similar pattern with highest contribution from chemical fertilizer followed by soil organic nitrogen, manure, atmospheric precipitation and sewage in order. Nitrate in groundwater in industrial areas has different pattern of the proportional contribution, in which groundwater NO is largely influenced by sewage discharge and atmospheric precipitation. We concluded that the combination of isotopic analysis together with land-use information and chemical analysis was an effective approach for assessing the source apportionment and the fate of nitrate in the aquifer in multiple land-use areas.
地下水硝酸盐(NO)污染是一个全球性的环境问题。将污染来源进行划分是有效控制的关键。本研究在一个具有多种土地利用类型的地区,对 28 口井的地下水样本进行了 NO 双重同位素组成(δN-NO 和 δO-NO)的测量,随后应用同位素混合模型(SIAR)来确定主要的 NO 来源及其生物地球化学过程。结果表明,反硝化作用不太可能以显著的速率发生,而硝化作用是一个重要的氮转化过程。地下水 NO 及其同位素组成的空间变化与土地利用类型有关。农业区的 NO 浓度相对较高,而 δN-NO 值较低。相比之下,工业地区的 δN-NO 和 δO-NO 值则较为富集。在农田、菜地、禽畜养殖场,化肥的贡献比例最高,其次是土壤有机氮、粪肥、大气降水和污水。工业地区地下水的硝酸盐的贡献比例则呈现不同的模式,其中地下水 NO 主要受到污水排放和大气降水的影响。我们得出结论,将同位素分析与土地利用信息和化学分析相结合,是评估含水层中硝酸盐来源分配和归宿的有效方法。