School of Chemical Engineering, Zhengzhou University, Zhengzhou 450001, China.
School of Civil Engineering, Nanyang Institute of Technology, Nanyang 473004, China.
Int J Environ Res Public Health. 2021 Aug 16;18(16):8642. doi: 10.3390/ijerph18168642.
Nitrate (NO) contamination in water is an environmental problem of widespread concern. In this study, we combined the stable isotopes of NO (δN and δO) and water (δH and δO) with a Bayesian mixing model (SIAR) to identify the sources and transformation of NO in groundwater and rivers in the Ye River basin of North China. The results showed that the mean NO concentrations in groundwater were 133.5 and 111.7 mg/L in the dry and flood seasons, respectively, which exceeded the required Chinese drinking water standards for groundwater (88.6 mg/L) (GB14848-2017). This suggests that groundwater quality has been severely impacted by human activity. Land use significantly affected the concentration of NO in the Ye River basin ( < 0.05). However, the NO concentrations in groundwater and river water had no obvious temporal variation ( > 0.05). The principal mode of nitrogen transformation for both groundwater and river water was nitrification, whereas denitrification did not significantly affect the isotopic compositions of NO. The sources of NO mainly originated from sewage and manure, soil nitrogen, and NH in fertilizer for groundwater and from sewage and manure for the river water. According to the SIAR model, the primary sources of nitrate found in groundwater and river were sewage and manure in the Ye River basin. The proportional contributions of sewage and manure to nitrate contamination of groundwater and river were 58% and 48% in the dry season and 49% and 54% in the flood season, respectively. Based on these results, we suggest that the local government should enhance the sewage treatment infrastructure, construct an effective waste storage system to collect manure, and pursue a scientific fertilization strategy (such as soil formula fertilization) to increase the utilization rate of nitrogen fertilizer and prevent nitrate levels from increasing further.
硝酸盐(NO)污染是一个广泛关注的环境问题。本研究结合稳定同位素(δN 和 δO)和水同位素(δH 和 δO)与贝叶斯混合模型(SIAR),对中国华北冶河流域地下水和河水硝酸盐的来源和转化进行了研究。结果表明,枯水期和丰水期地下水硝酸盐平均浓度分别为 133.5 和 111.7mg/L,均超过中国地下水饮用水标准(GB14848-2017)(88.6mg/L),表明地下水水质受到人为活动的严重影响。土地利用对冶河流域硝酸盐浓度有显著影响(<0.05)。但地下水和河水中硝酸盐浓度无明显时间变化(>0.05)。地下水和河水中氮的主要转化方式为硝化作用,反硝化作用对硝酸盐的同位素组成没有明显影响。硝酸盐的主要来源为地下水的污水和粪肥、土壤氮和肥料中的 NH4+,河水的污水和粪肥。根据 SIAR 模型,冶河流域地下水和河水中硝酸盐的主要来源是污水和粪肥。枯水期和丰水期污水和粪肥对地下水和河水中硝酸盐污染的贡献率分别为 58%和 48%、49%和 54%。基于这些结果,建议当地政府加强污水处理基础设施建设,建立有效的粪便收集储存系统,推行科学施肥策略(如测土配方施肥),提高氮肥利用率,防止硝酸盐进一步增加。