Sun Hou-Yun, Wei Xiao-Feng, Jia Feng-Chao, Li Duo-Jie, Li Jian, Li Xia, Yin Zhi-Qiang
School of Water Resources and Environment, China University of Geosciences(Beijing), Beijing 100083, China.
Beijing Institute of Geology for Mineral Resources, Beijing 100012, China.
Huan Jing Ke Xue. 2020 Nov 8;41(11):4936-4947. doi: 10.13227/j.hjkx.202004142.
The multi-environment media of water, surface soil and vadose zone soil samples were collected in the upstream of Miyun Reservoir, in the Luanping Basin of Chengde City, Hebei Province. The aim was to identify the pollution source, ratio, spatial distribution, migration, and transformation characteristics of nitrogen in groundwater. Hydrogeochemistry, soil total nitrogen, and dissolved nitrate nitrogen of vadose zone soil analysis and a multi isotope tracer technique of N-NO and O-NO, S-SO and O-SO, C, combined with land-use type analysis and geostatistics, were used in the study. The results showed that nitrate was the main form of nitrogen in the groundwater of the Luanping Basin. The NO concentration of groundwater was significantly correlated with the land-use types of residential land and cultivated land where the nitrate pollution of shallow groundwater was mainly distributed. Of the groundwater samples, 13.79% exceeded the National Standard Ⅲ for Groundwater (GB/T 14848-2017) of NO concentration value, while the excess multiple was 1.04-3.86, and 37.93% of the groundwater samples exceeded the World Health Organization NO concentration standard value. The excess multiple was 1.08-6.83. The spatial variation of groundwater NO concentration, soil total nitrogen and surface soil dissolved nitrate nitrogen of vadose zone was affected by the combination of natural structural factors and anthropogenic factors. The source of groundwater nitrate was mainly from livestock manure and domestic sewage, followed by chemical fertilizer leaching. The nitrogen cycle in the aeration zone-groundwater-dominated nitrogen circulation in the groundwater runoff area of the piedmont basin was nitrification. These findings are highly significant for the prevention and remediation of groundwater pollution when viewing the basin system as an independent unit, and for studying the sources and fate of nitrate pollution in the water environment.
在河北省承德市滦平盆地密云水库上游采集了水、表层土壤和包气带土壤样品的多环境介质。目的是确定地下水中氮的污染源、比例、空间分布、迁移及转化特征。本研究采用水文地球化学、土壤全氮和包气带土壤溶解态硝态氮分析以及N-NO和O-NO、S-SO和O-SO、C的多同位素示踪技术,并结合土地利用类型分析和地统计学方法。结果表明,硝酸盐是滦平盆地地下水中氮的主要形态。地下水中NO浓度与浅层地下水硝酸盐污染主要分布的居住用地和耕地等土地利用类型显著相关。在地下水样品中,13.79%超过了《地下水质量标准》(GB/T 14848—2017)Ⅲ类标准的NO浓度值,超标倍数为1.043.86,37.93%的地下水样品超过了世界卫生组织的NO浓度标准值,超标倍数为1.086.83。地下水NO浓度、土壤全氮和包气带表层土壤溶解态硝态氮的空间变异受自然构造因素和人为因素共同影响。地下水硝酸盐的来源主要是畜禽粪便和生活污水,其次是化肥淋溶。山前盆地地下水径流区以包气带-地下水为主的氮循环中的氮循环过程为硝化作用。当将盆地系统视为一个独立单元时,这些发现对于地下水污染的预防和修复以及研究水环境中硝酸盐污染的来源和归宿具有重要意义。