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太原地区大气氮湿沉降变化特征
引用本文:梁亚宇,李丽君,宋志辉,白光洁,吕薇,刘平.太原地区大气氮湿沉降变化特征[J].地球与环境,2019,47(4):405-411.
作者姓名:梁亚宇  李丽君  宋志辉  白光洁  吕薇  刘平
作者单位:山西大学生物工程学院,太原,030006;山西省农业科学院农业环境与资源研究所山西省土壤环境与养分资源重点实验室,太原,030031;太原市环保局杏花岭分局监测站,太原,030009
基金项目:山西省财政支农项目(2015ZZCX-13);山西省财政支农项目(2016ZZX-13);山西省回国留学人员科研资助项目(2016-133)和山西省留学回国人员科技活动项目择优资助项目。
摘    要:为研究太原地区的大气氮湿沉降时空变化规律,于2016年1月~2017年12月采用雨量器对太原市市中、近郊和远郊三地大气氮湿沉降进行了为期2年的监测。得到市中、近郊、远郊的NO3--N平均浓度为12.9、18.4、1.3 mg/L,NH4+-N平均浓度分别为3.6、2.3、1.6 mg/L。季节变化上看,NH4+-N浓度值四季相对平均,春夏季稍高,而NO3--N浓度变化较大且冬春季浓度值较高。三个采样点大气氮湿沉降量(无机氮)年均沉降量分别为40.0、48.0、14.2 kg/hm2,以近郊的沉降量最高。市中、近郊、远郊的NH4+-N沉降量分别为9.0、5.0、8.2 kg/hm2,占总无机氮湿沉降量的比重分别为22%、11%、57%,NO3--N沉降量分别是31.0、43.0、6.0 kg/hm2,占总无机氮湿沉降量的比重分别为78%、89%、43%。从上可知城市降水中主要以NO3--N沉降为主,农村则以NH4+-N沉降为主。结合市中、近郊、远郊NH4+-N/NO3--N浓度比值分别为0.54、0.30、1.31,充分表明市中和近郊大气氮湿沉降主要来自工业和交通运输源,远郊则来自农业源。另外,市中、近郊月氮湿沉降量与降雨量差异不显著,远郊则达到极显著水平,说明影响市区两点氮湿沉降的因素较为复杂。由以上数据看出市中和近郊氮污染情况比较严重,应根据各自沉降特点予以控制。

关 键 词:市中  近郊  远郊  氮湿沉降  铵态氮和硝态氮  相关性
收稿时间:2018/10/11 0:00:00
修稿时间:2018/12/6 0:00:00

Characteristics of Atmospheric Nitrogen Wet Deposition Variations in the Taiyuan Area
LIANG Yayu,LI Lijun,SONG Zhihui,BAI Guangjie,LV Wei,LIU Ping.Characteristics of Atmospheric Nitrogen Wet Deposition Variations in the Taiyuan Area[J].Earth and Environment,2019,47(4):405-411.
Authors:LIANG Yayu  LI Lijun  SONG Zhihui  BAI Guangjie  LV Wei  LIU Ping
Institution:1. School of Biological Engineering, Shanxi University, Taiyuan 030006, China;2. Institute of Agricultural Environment and Resources, Shanxi Academy of Agricultural Sciences, Taiyuan 030031, China;3. Monitoring Station of Xinghualing Branch Bureau of Taiyuan Environmental Protection Bureau, Taiyuan 030009, China
Abstract:A research on temporal and spatial variation of atmospheric nitrogen wet deposition was conducted using the rain gauge method at the downtown, suburb and outer suburbs of the Taiyuan City from January 2016 to December 2017. The concentrations of NO3--N and NH4+-N averaged from1.3 mg/L to18.4 mg/L and from1.6 to 3.6 mg/L, respectively. The average concentrations of NH4+-N were stable in all seasons, but average concentrations of NO3--N were higher in winter and spring seasons. The annual averaged wet depositions of inorganic N(IN) were 40.0, 48.0, 14.2 kg/hm2, respectively, at three sampling sites (downtown, suburb and outer suburbs of Taiyuan). The wet deposition rates of NH4+-N were 9.0, 5.0, 8.2 kg/hm2 and accounted for 22%, 11%, 57% of the IN depositions, while wet deposition rates of NO3--N were 31.0, 43.0, 6.0 kg/hm2and accounted for 78%, 89%, 43% of IN depositions at three sampling sites, respectively. The average concentration ratios of NH4+-N/NO3--N were 0.54, 0.30 and 1.31, respectively, at three sites. In addition, the difference between nitrogen wet deposition and rainfall in the downtown and suburban areas was not significant but reached a very significant level at outer suburbs, indicating that affecting factors of wet deposition at urban areas are more complicated than at the outer suburbs. These results might suggest that atmospheric nitrogen wet depositions were affected mainly by industry or/and transportation at downtown and suburb, while by agriculture activities at outer suburbs. In summary, to prevent high wet depositions of N in the Taiyuan area, different strategies should be applied according to different sites.
Keywords:city center  near suburb  far suburb  wet N deposition  NH4+-N and NO3--N  correlation
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