Engineering Research Center for Groundwater Pollution Control, Remediation of Ministry of Education of China, College of Water Sciences, Beijing Normal University, Beijing 100875, China.
Engineering Research Center for Groundwater Pollution Control, Remediation of Ministry of Education of China, College of Water Sciences, Beijing Normal University, Beijing 100875, China.
Sci Total Environ. 2022 Feb 20;808:152162. doi: 10.1016/j.scitotenv.2021.152162. Epub 2021 Dec 5.
Anthropogenic pollutants (organic nitrogen and ammonia) can change the dynamic balances of hydrogeochemical components of groundwater, and this can affect the fates of the pollutants and groundwater quality. The aim of this paper is to assess the long-term impact of pollutants on groundwater component concentrations and species in three sites that has been polluted with illegal discharge wastewater containing organic nitrogen and ammonia, in order to reveal the interactions between nitrogen species and Mn. We analyzed semi-monthly groundwater data from three sites in northwestern China over a long period of time (2015-2020) by using statistical analyses, correlation analyses, and a correlation co-occurrence network method. The results showed that wastewater entering groundwater from surface changed the hydrogeochemical component concentrations and species significantly. The main form of inorganic nitrogen species changed from nitrate to ammonia. The Mn concentration increased from undetectable (<0.01 mg/L) to 1.64 mg/L (the maximum), which surpassed the guideline value suggested by China and WHO. The main mechanism for Mn increase is the reductive dissolution of Mn oxide caused by the oxidation of organic nitrogen. Mn‑nitrogen species interaction complicates the transformation of nitrogen components. Chemoautotrophic denitrification and dissimilatory nitrate reduction to ammonium (DNRA) mediated by Mn are the major mechanisms of nitrate attenuation when dissolved oxygen is greater than 2 mg/L. Mn oxides reductive dissolution and reoxidation of Mn by nitrate reduction cause Mn to circulate in groundwater. The results provide field evidence for interactions between nitrogen species transformation and Mn cycle in groundwater. This has important implications for pollution management and groundwater remediation, particularly monitored natural attenuation.
人为污染物(有机氮和氨)会改变地下水水文地球化学组分的动态平衡,从而影响污染物和地下水质量的归宿。本文的目的是评估受含有有机氮和氨的非法排放废水污染的三个地点的污染物对地下水组分浓度和形态的长期影响,以揭示氮形态与 Mn 的相互作用。我们通过统计分析、相关性分析和相关性共现网络方法,对中国西北地区三个地点在很长一段时间(2015-2020 年)的半月度地下水数据进行了分析。结果表明,废水从地表进入地下水会显著改变水文地球化学组分浓度和形态。无机氮形态的主要形式已由硝酸盐转变为氨。Mn 浓度从检测不到(<0.01 mg/L)增加到 1.64 mg/L(最大值),超过了中国和世界卫生组织建议的标准值。Mn 增加的主要机制是由于有机氮的氧化导致 Mn 氧化物的还原溶解。Mn-氮形态相互作用使氮组分的转化复杂化。当溶解氧大于 2 mg/L 时,Mn 介导的化能自养反硝化和异化硝酸盐还原为铵(DNRA)是硝酸盐衰减的主要机制。Mn 氧化物的还原溶解和硝酸盐还原引起的 Mn 再氧化导致 Mn 在地下水中循环。该研究结果为地下水氮形态转化与 Mn 循环之间的相互作用提供了现场证据。这对污染管理和地下水修复,特别是自然衰减监测具有重要意义。