| 基于野外原位抽注试验和同位素技术的含水层反硝化速率研究 |
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| 引用本文： | 郇环,刘兵,朱岗辉,刘梦娇,刘伟江,姜永海.基于野外原位抽注试验和同位素技术的含水层反硝化速率研究[J].环境科学研究,2020,33(9):1991-2000. |
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| 作者姓名： | 郇环 刘兵 朱岗辉 刘梦娇 刘伟江 姜永海 |
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| 作者单位： | 1.生态环境部土壤与农业农村生态环境监管技术中心, 北京 100012 |
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| 基金项目： | 国家自然科学基金项目（No.41602260）；国家水体污染控制与治理科技重大专项（No.2017ZX07107-005， 2018ZX07109-003） |
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| 摘 要： | 反硝化作用是地下水硝酸盐污染去除最重要的过程.由于水文地质条件和水文地球化学环境的复杂性和不确定性，精准测定含水层反硝化速率是反硝化过程的研究难点.选取潮白河冲洪积扇中部中国环境科学研究院地下水创新野外基地作为研究区，基于野外原位试验和15N同位素示踪法提出一种含水层反硝化速率的测定方法.该方法综合体现了研究区实际水文地质条件和水文地球化学环境对反硝化作用的影响，并充分考虑了硝酸盐在含水层中稀释弥散作用对计算结果的影响.结果表明:①潮白河冲洪积扇中部某地地下26~28 m处于还原环境，含水介质以粉细砂为主，ρ（NO3-N）平均值为2.77 mg/L.②地下26~28 m反硝化速率在349.52~562.99 μg/（kg·d）（以N计，下同）之间，平均值为450.31 μg/（kg·d）.通过与研究区含水介质、采样深度和硝酸盐背景值相似的国内外案例对比研究，初步评估结果处于合理区间.③测试结果具有一定不确定性，主要来自忽略中间产物NO2-和NO的计算方法、扰动采样方法、N2O的操作规范程度及采样频率等方面.研究方法为测定含水层硝酸盐速率研究提供了新的思路，研究结果可为地下水中硝酸盐转化过程机理研究、地下水硝酸盐污染修复及风险管控提供关键的理论支撑数据.
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| 关 键 词： | 地下水 反硝化速率 硝酸盐污染 同位素技术 原位抽注试验 |
| 收稿时间： | 2019/12/31 0:00:00 |
| 修稿时间： | 2020/7/7 0:00:00 |
Denitrification Rate in Aquifer Based on In-Situ Pumping/Injecting Test and Isotope Technique |
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| HUAN Huan,LIU Bing,ZHU Ganghui,LIU Mengjiao,LIU Weijiang,JIANG Yonghai.Denitrification Rate in Aquifer Based on In-Situ Pumping/Injecting Test and Isotope Technique[J].Research of Environmental Sciences,2020,33(9):1991-2000. |
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| Authors: | HUAN Huan LIU Bing ZHU Ganghui LIU Mengjiao LIU Weijiang JIANG Yonghai |
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| Affiliation: | 1.Technical Centre for Soil, Agricultural and Rural Ecology and Environment, Ministry of Ecology and Environment, Beijing 100012, China2.State Environmental Protection Key Laboratory of Simulation and Control of Groundwater Pollution, Chinese Research Academy of Environmental Sciences, Beijing 100012, China3.Institute of Disaster Prevention Technology, Sanhe 065201, China |
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| Abstract: | Denitrification process of nitrate in aquifers is vital because it can dissipate groundwater nitrate pollution. It is very difficult to acquire the accurate denitrification rate in the aquifer due to the complicated hydrogeological conditions and hydrogeochemical environment in the field. A method was proposed for determining the denitrification rate in the aquifer based on in-situ pumping/injecting test and isotope technique. The method was applied in the groundwater innovation field base of Chinese Research Academy of Environmental Sciences, in the middle of the Chaobai River alluvial-proluvial fan. The method integrated the effect of actual hydrogeological conditions and hydrogeochemical environment on the denitrification process, as well as the effect of dilution and dispersion of nitrate in the aquifer. The results showed that the shallow aquifer, which was composed by sandy loam, was in the reducing environments at the depth of 26-28 m in the study area. The average nitrate concentration was 2.77 mg/L. The denitrification rates ranged between 349.52 and 562.99 μg/(kg·d) with the average value of 450.31 μg/(kg·d). The values were preliminarily verified to be reasonable by comparative study of domestic and foreign cases in the study area. The method of ignoring the intermediate products of NO2- and NO, perturbation sampling method, operation specification degree of N2O and sampling frequency can result in the uncertainty of the denitrification rates. The method can objectively and quantitatively determine the denitrification intensity in the aquifer as a new idea. The research results can provide key data for studying the mechanism of nitrate fate and transport in the aquifer, and remediation and risk control of groundwater nitrate pollution. |
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| Keywords: | groundwater denitrification rate nitrate pollution isotope technique in-situ pumping/injecting test |
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