首页 | 本学科首页   官方微博 | 高级检索  
     

基于水化学及氮氧同位素技术的硝酸盐来源解析——以鄱阳湖湿地为例
引用本文:李智滔,肖红伟,伍作亭,马艳,肖扬宁,陈振平,陶继华. 基于水化学及氮氧同位素技术的硝酸盐来源解析——以鄱阳湖湿地为例[J]. 中国环境科学, 2022, 42(9): 4315-4322
作者姓名:李智滔  肖红伟  伍作亭  马艳  肖扬宁  陈振平  陶继华
作者单位:1. 东华理工大学, 江西省大气污染成因与控制重点实验室, 江西 南昌 330013;2. 东华理工大学水资源与环境工程学院, 江西 南昌 330013;3. 上海交通大学环境科学与工程学院, 上海 200240;4. 东华理工大学地球科学学院, 江西 南昌 330013
基金项目:国家自然科学基金资助项目(42063001,41663003);江西省科技计划项目(2017BCD40010)
摘    要:为了识别鄱阳湖湿地水体中硝酸盐污染的来源,转化特征和各污染来源的贡献比例,选取枯水期这一典型时期,于2019年1月份对鄱阳湖中的蚌湖湿地,沙湖山湿地和庐山湿地的地表水进行取样,并测定了水样中的离子组成和硝酸盐氮氧同位素值.研究结果显示, NO3-/Cl-物质的量浓度比值与Cl-浓度的关系表明3处湿地中硝酸盐来源可能受到农业活动和降雨的影响.蚌湖,沙湖山和庐山湿地水体中δ15N-NO3-和δ18O-NO3-值的范围分别为-6.19‰~4.67‰和3.41‰~39.95‰,-4.14‰~1.45‰和31.54‰~68.30‰,-6.98‰~3.83‰和2.80‰~30.43‰,硝酸盐氮氧同位素值表明3处湿地硝酸盐来源可能受到降水NO3-,硝酸盐氮肥,氨态氮肥和土壤有机氮的影响.利用硝酸盐氮氧同位素之间的关系,并结合NO3-与Cl-比值关系判断湿地中无明显反硝化作用的发生.SIAR模型结果显示:蚌湖湿地,沙湖山湿地,庐山湿地硝酸盐来源中降水NO3-贡献占比最大,其次是化肥,土壤有机氮,粪便和生活污水贡献占比最小.

关 键 词:鄱阳湖  硝酸盐  来源  氮氧同位素  反硝化作用  SIAR模型
收稿时间:2022-02-15

Hydrochemistry,nitrogen and oxygen isotope composition of nitrate to trace its source in Poyang Lake wetland
LI Zhi-tao,XIAO Hong-wei,WU Zuo-ting,MA Yan,XIAO Yang-ning,CHEN Zhen-ping,TAO Ji-hua. Hydrochemistry,nitrogen and oxygen isotope composition of nitrate to trace its source in Poyang Lake wetland[J]. China Environmental Science, 2022, 42(9): 4315-4322
Authors:LI Zhi-tao  XIAO Hong-wei  WU Zuo-ting  MA Yan  XIAO Yang-ning  CHEN Zhen-ping  TAO Ji-hua
Affiliation:1. Jiangxi Province Key Laboratory of the Causes and Control of Atmospheric Pollution, East China University of Technology, Nanchang 330013, China;2. School of Water Resources and Environmental Engineering, East China University of Technology, Nanchang 330013, China;3. School of Environmental Science and Engineering, Shanghai Jiao Tong University, Shanghai 200240, China;4. School of Earth Sciences, East China University of Technology, Nanchang 330013, China
Abstract:In order to identify the sources, transformation and source apportionment of nitrate in Poyang lake wetland, surface water samples were collected in Poyang lake wetland, including Bang lake wetland, Shahushan wetland and Lushan wetland, in January 2019, a typical dry season. The ion composition, and nitrogen and oxygen isotope values of nitrate in the water samples were determined. Results showed that the relationship between the molar ratio of NO3- to Cl- and Cl- concentration indicated the source of nitrate mainly from agricultural activities and rainfall in the three wetlands. The range of δ15N-NO3- and δ18O-NO3- values in the three wetlands were -6.19‰~4.67‰ and 3.41‰~39.95‰, -4.14‰~1.45‰ and 31.54‰~68.30‰, -6.98‰~3.83‰ and 2.80‰~ 30.43‰, respectively. Nitrogen and oxygen isotope values of nitrate showed that the nitrate sources may be influenced by precipitation NO3-, nitrate nitrogen fertilizer, ammonia nitrogen fertilizer and soil organic nitrogen in the three wetlands. The relationship between nitrogen and oxygen isotopes of nitrate and the ratio relationship between NO3- and Cl- suggested that there was no obvious denitrification in these wetlands. The results of SIAR model showed that the contribution of precipitation NO3- to nitrate sources was the largest, then followed by fertilizer and soil organic nitrogen, feces and domestic sewage was the least in three wetlands.
Keywords:Poyang Lake  nitrate  source  nitrogen and oxygen isotopes  denitrification  SIAR model  
点击此处可从《中国环境科学》浏览原始摘要信息
点击此处可从《中国环境科学》下载全文
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号