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郑州市夏季大气VOCs污染特征及来源解析
摘要点击 2208  全文点击 1190  投稿时间:2022-03-09  修订日期:2022-05-25
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中文关键词  挥发性有机物(VOCs)  臭氧生成潜势(OFP)  比值分析  正定矩阵因子分解(PMF)模型  源解析(RA)  条件概率函数(CPF)模型  夏季
英文关键词  volatile organic compounds (VOCs)  ozone formation potential (OFP)  ratio analysis (RA)  positive matrix factorization (PMF) model  source apportionment  conditional probability function (CPF) model  summer
作者单位E-mail
齐一谨 河南天朗生态科技有限公司, 郑州 450000 yijinqi2017@163.com 
王玲玲 河南省环境监测中心, 河南省环境监测技术重点实验室, 郑州 450000  
倪经纬 河南天朗生态科技有限公司, 郑州 450000 nijingwei@hh12369.com 
何海洋 河南天朗生态科技有限公司, 郑州 450000  
赵东旭 河南天朗生态科技有限公司, 郑州 450000  
龚山陵 河南天朗生态科技有限公司, 郑州 450000
中国气象科学研究院, 北京 100081 
gongsl@cma.gov.cn 
中文摘要
      采用GC5000在线气相色谱仪,于2019年和2020年夏季6~8月分别对郑州市城区中大气环境挥发性有机化合物(VOCs)进行监测,探究了VOCs的污染特征,并重点利用比值分析,PMF受体模型和条件概率函数(CPF)模型对比研究了其来源贡献.结果表明,2019年和2020年夏季ρ(VOCs)平均值分别为65.7 μg·m-3和71.0μg·m-3.2019年烷烃占比逐月变化幅度不大,占比在55%左右,芳香烃整体呈上升趋势,烯烃呈下降趋势;前10物种占总VOCs的65.5%,主要物种依次为异戊烷、乙烷、丙烷、甲苯、正丁烷和间/对-二甲苯等.2020年烷烃和烯烃占比呈逐月升高趋势,芳香烃呈逐月降低趋势;前10物种占总VOCs的71.1%,主要物种依次为乙烷、乙烯、丙烷、异戊烷、正丁烷、甲苯和间/对-二甲苯等.2019年夏季OFP平均值为224.9 μg·m-3,其中芳香烃对OFP贡献率逐月升高,烯烃逐月降低;对OFP贡献的物种主要为间/对-二甲苯、异戊二烯、反式-2-丁烯、甲苯和乙烯等.2020年夏季OFP平均值为243.6 μg·m-3,其中芳香烃对OFP贡献逐月降低,烯烃逐月升高;对OFP贡献的物种主要为乙烯、间/对-二甲苯、异戊二烯、甲苯和间-乙基甲苯等.PMF和CPF模型解析表明,2019年对VOCs贡献较大的是溶剂使用源和油气挥发源,贡献率分别为36.7%和25.1%,其对OFP贡献也较大,分别为39.9%和23.3%,需重点关注西南部区域.2020年对VOCs贡献较大的仍为溶剂使用源和油气挥发源,贡献率分别为24.9%和22.5%;对OFP贡献较大的为溶剂使用源和机动车尾气排放源,贡献率分别为33.6%和22.9%,需重点关注北部和南部区域.因此,今后应重点关注溶剂使用、机动车尾气排放和油气挥发源的排放,尤其监测点位的西南部、北部和东南部区域污染源.
英文摘要
      The concentrations of volatile organic compounds (VOCs) in the atmospheric environment in the urban area of Zhengzhou were investigated by a GC5000 online gas chromatography in the summer of 2019 and 2020 from June to August, respectively, and the pollution characteristics, especially the source apportionment, were explored with the methods of ratio analysis (RA), positive matrix factorization (PMF) model, and conditional probability function (CPF) model. The results showed that the average VOCs concentrations in 2019 and 2020 summer were 65.7 μg·m-3 and 71.0 μg·m-3, respectively. In 2019, the proportion of alkanes was changed little, accounting for about 55%. The aromatic hydrocarbon showed an upward trend and olefin was decreased month by month. The top ten species were accounted for 65.5% of the total VOCs with the main species of isopentane, ethane, propane, toluene, n-butane, and m/p-xylene, etc. In 2020, the proportion of alkanes and olefins was increased, while the proportion of aromatic hydrocarbons was decreased month by month. The top ten species were accounted for 71.1% of the total VOCs with the main species of ethane, ethylene, propane, isopentane, n-butane, toluene and m/p-xylene, etc. The average ozone formation potential (OFP) concentration in summer 2019 was 224.9 μg·m-3. It was found that the contribution ratio of aromatic hydrocarbons to OFP was increased, while that of olefin was decreased month by month, and the main species contributing to OFP were m/p-xylene, isoprene, trans-2-butene, toluene, ethylene, etc. In 2020, The average OFP concentration in summer was 243.6 μg·m-3, the contribution of aromatic hydrocarbons to OFP was decreased, while the contribution of olefin was increased month by month, and the major species contributing to OFP were ethylene, m/p-xylene, isoprene, toluene, and m-ethyltoluene, etc. The RA, PMF and CPF model analysis showed that the major contributions in 2019 were the solvent usage and the oil/gas volatilization sources, accounted for 36.7% and 25.1% of VOCs, and their contributions to the OFP were accounted for 39.9% and 23.3% respectively, mainly from the southwest region of Zhengzhou. In 2020, the solvent usage and oil/gas volatilization sources were accounted for 24.9% and 22.5%, and solvent usage and motor vehicle exhaust were the major contribution to the OFP, accounting for 33.6% and 22.9%, respectively, mainly from the north and south regions. Therefore, more attention should be paid to the use of solvent, vehicle exhaust emissions, oil and gas volatilization sources emissions in the future, especially for the pollution sources in the southwest, north and southeast areas.

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