Tracing nitrate pollution sources of karst groundwater in water resources using environmental isotopes

被引:0
作者
Yunfeng Zhang
Dalu Yu
Di Wu
Yuhui Zhao
Zhe Zhang
Bo Li
Baohui Huang
Mingguo Wang
Junru Gao
Yuxiao Kang
Rui Liu
机构
[1] 801 Institute of Hydrogeology and Engineering Geology,School of Resources and Environmental Engineering
[2] Shandong Provincial Bureau of Geology & Mineral Resources (Shandong Provincial Geo-Mineral Engineering Exploration Institute),undefined
[3] Shandong Engineering Research Center for Environmental Protection and Remediation on Groundwater,undefined
[4] Shandong Hydrogeology Engineering Geology and Environment Geology Corporation,undefined
[5] Shandong Geology and Mineral Resources Materials Corporation,undefined
[6] Shandong University of Technology,undefined
来源
Carbonates and Evaporites | 2023年 / 38卷
关键词
Karst groundwater; Nitrate pollution; Nitrogen isotopes; Water resource;
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学科分类号
摘要
The contamination of NO3− in groundwater is a global concern, requiring the identification of biogeochemical transformations and sources of nitrate (NO3−) to understand the different nitrogen (N) pathways. This is necessary for the regulation of dispersed pollution of groundwater caused by livestock and agricultural activities. Jinan, located in eastern China, serves as a suitable case study due to its reliance on karst groundwater as a water source and its significant population, industrial, and agricultural development, which pose a substantial risk of nitrogen pollutants in groundwater. Therefore, this study aims to investigate NO3− concentrations and isotopic compositions of N and oxygen in karst groundwater in Jinan City, Shandong province, eastern China, to determine the most significant sources and transformations of NO3−. Approximately 86% of the groundwater samples exceed the NO3−–N standard for drinking water proposed by the World Health Organization (WHO). Furthermore, chemical indicators (Cl−, HCO3−, and TDS) and the oxygen and nitrogen isotopic compositions of NO3− indicate that soil organic nitrogen, manure, and urban sewage are the main sources of NO3− in the groundwater. Isotopic analyses also suggest that various biogeochemical transformations, such as nitrification and volatilization, occur throughout the study area, with microbial nitrification being the dominant process in water resource areas with high NO3− concentrations. To reduce NO3− pollution in the Changqing–Xiaolipu water supply, several suggestions have been proposed.
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共 171 条
[1]  
Acevedo Peralta AI(2017)Política ambiental: uso y manejo del estiércol en la Comarca Lagunera Acta Universitaria 27 3-12
[2]  
Leos Rodríguez JA(1983)O FEBS Lett 164 236-240
[3]  
Figueroa Viramontes U(2013) and H Chemosphere 93 1009-1014
[4]  
Romo Lozano JL(1990)O are each the source of one O in NO− 2 produced from NH J Hydrol 114 413-424
[5]  
Andersson KK(2018) by Nitrosomonas: 15N-NMR evidence Chemosphere 210 1091-1098
[6]  
Hooper AB(2012)Evaluation of food chain transfer of the antibioticoxytetracycline and human risk assessment Nigeria 67 2383-2398
[7]  
Boonsaner M(2012)Using isotope fractionation of nitrate-nitrogen and nitrate-oxygen for evaluation of microbial denitrification in a sandy aquifer Environ Earth Sci 368 20130116-392
[8]  
Hawker DW(2013)Trace elements in atmospheric wet precipitation in the Detroit metropolitan area: levels and possible sources Philos Trans R Soc B 6 377-3078
[9]  
Böttcher J(2015)Spatial and temporal distribution of nitrate pollution in groundwater of Abuja Revista Mexicana De Ciencias Pecuarias 37 3070-2198
[10]  
Strebel O(2003)Nitrate source and fate at the catchment scale of the Vibrata River and aquifer (central Italy): an analysis by integrating component approaches and nitrogen isotopes Water Res 243 2191-226