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大气中过氧化氢的生成、污染特征及其影响因素
引用本文:陈炫,杨加赢,张安平,刘厚凤,孙建强,刘姣玉,孟凡.大气中过氧化氢的生成、污染特征及其影响因素[J].环境科学研究,2016,29(3):334-342.
作者姓名:陈炫  杨加赢  张安平  刘厚凤  孙建强  刘姣玉  孟凡
作者单位:1.中国环境科学研究院, 环境基准与风险评估国家重点实验室, 北京 100012
基金项目:中央级公益性科研院所基本科研业务专项(2010kyyw02);国家国际科技合作专项(2012DFG90290)
摘    要:过氧化氢(H2O2)是自由基的源和汇,是对流层大气中重要的氧化剂. 采用文献研究法对1990年以来H2O2的文献进行搜集整理,对其生成途径、污染特征及其影响因素进行了研究. 结果表明:H2O2在大气、云水和颗粒物中均有存在,大气中的H2O2主要通过O3和甲醛光解、VOC同OH·/O3等反应生成. 大气中φ(H2O2)一般在nd~8×10-9内波动,晴天φ(H2O2)呈早晚低、午后高的日变化特征;φ(H2O2)随φ(O3)、太阳辐射和气温的增加而升高,随φ(NOx)、φ(VOCs)和相对湿度的升高而降低;H2O2氧化SO2为SO42-是液相化学中最重要的反应,可以导致酸沉降以及二次气溶胶浓度的升高. 在气相光化学反应中,H2O2/HNO3(体积分数比)可以指示O3生成是VOCs控制还是NOx控制. 今后需对OH·浓度、NO2和O3的光解速率等影响H2O2关键因素开展监测研究,此外,还需对我国特殊大气环境下H2O2对SO42-生成的贡献、不同地区H2O2/HNO3指示O3生成对NOx或VOCs敏感性等方面开展更多的研究. 

关 键 词:过氧化氢    光化学反应    生成途径    污染特征    影响因素    大气化学行为
收稿时间:2015/10/1 0:00:00
修稿时间:2015/12/7 0:00:00

Pollution Characteristics and Chemical Behaviors of Atmospheric Hydrogen Peroxide
CHEN Xuan,YANG Jiaying,ZHANG Anping,LIU Houfeng,SUN Jianqiang,LIU Jiaoyu and MENG Fan.Pollution Characteristics and Chemical Behaviors of Atmospheric Hydrogen Peroxide[J].Research of Environmental Sciences,2016,29(3):334-342.
Authors:CHEN Xuan  YANG Jiaying  ZHANG Anping  LIU Houfeng  SUN Jianqiang  LIU Jiaoyu and MENG Fan
Institution:1.State Key Laboratory of Environmental Criteria and Risk Assessment, Chinese Research Academy of Environmental Sciences, Beijing 100012, China2.Zhejiang Huahai Pharmaceutical Co., Ltd., Taizhou 317000, China3.College of Environment,Zhejiang University of Technology, Hangzhou 310014, China4.College of Geography and Environment,Shandong Normal University, Jinan 250014, China5.College of Environmental & Resource Sciences of Zhejiang University, Hangzhou 310058, China
Abstract:Hydrogen peroxide (H2O2) is a reservoir and sink of free radicals, and also an important oxidant in the tropospheric atmosphere. Research into the literature was conducted to summarize publications about H2O2 since 1990s, including the formation route, pollution characteristics and the effect factors. The results showed that H2O2 exists in the atmosphere, cloud drops and particles. In the atmosphere, H2O2 is generated mainly through photolysis of O3 and formaldehyde, reactions of VOCs and OH·/O3, etc. Atmospheric concentrations of H2O2 range from nd to 8×10-9, with high concentrations around noon and low concentrations in the morning and in the evening on clear days. H2O2 concentrations increase with the increase of O3 concentration and the decrease of NOx and VOCs concentration. The increase of solar radiation and temperature or the decrease of relative humidity causes the increase of H2O2 concentration. The reaction in which H2O2 oxidizes sulfur dioxide to sulfuric acid is one of the most important reactions in aqueous-phase chemistry, leading to the formation of acid rain and the increase of secondary aerosol concentrations. In addition, the ratio of H2O2/HNO3 indicates the limitation of VOC or NOx in the O3 formation. In the future, more work on the measurement of key factors such as OH· concentration and photolysis rate of NO2 and O3 that influence H2O2 formation should be carried out. More studies on H2O2′s contribution to SO42- formation and on the ratio of H2O2/HNO3 as an indicator to ozone-NOx-VOCs sensitivity in different regions under the special atmospheric environment in China should be carried out as well. 
Keywords:hydrogen peroxide  photochemical reaction  formation route  pollution characteristics  effect factors  chemical behavior
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