期刊文献+

Role of ammonia in forming secondary aerosols from gasoline vehicle exhaust 被引量:7

Role of ammonia in forming secondary aerosols from gasoline vehicle exhaust
原文传递
导出
摘要 Ammonia(NH3) plays vital roles in new particle formation and atmospheric chemistry. Although previous studies have revealed that it also influences the formation of secondary organic aerosols(SOA) from ozonolysis of biogenic and anthropogenic volatile organic compounds(VOCs), the influence of NH3 on particle formation from complex mixtures such as vehicle exhausts is still poorly understood. Here we directly introduced gasoline vehicles exhausts(GVE) into a smog chamber with NH3 absorbed by denuders to examine the role of NH3 in particle formation from GVE. We found that removing NH3 from GVE would greatly suppress the formation and growth of particles. Adding NH3 into the reactor after 3 h photo-oxidation of GVE, the particle number concentration and mass concentrations jumped explosively to much higher levels, indicating that the numbers and mass of particles might be enhanced when aged vehicle exhausts are transported to rural areas and mixed with NH3-rich plumes. We also found that the presence of NH3 had no significant influence on SOA formation from GVE. Very similar oxygen to carbon(O:C) and hydrogen to carbon(H:C) ratios resolved by aerosol mass spectrometer with and without NH3 indicated that the presence of NH3 also had no impact on the average carbon oxidation state of SOA from GVE. Ammonia(NH3) plays vital roles in new particle formation and atmospheric chemistry. Although previous studies have revealed that it also influences the formation of secondary organic aerosols(SOA) from ozonolysis of biogenic and anthropogenic volatile organic compounds(VOCs), the influence of NH3 on particle formation from complex mixtures such as vehicle exhausts is still poorly understood. Here we directly introduced gasoline vehicles exhausts(GVE) into a smog chamber with NH3 absorbed by denuders to examine the role of NH3 in particle formation from GVE. We found that removing NH3 from GVE would greatly suppress the formation and growth of particles. Adding NH3 into the reactor after 3 h photo-oxidation of GVE, the particle number concentration and mass concentrations jumped explosively to much higher levels, indicating that the numbers and mass of particles might be enhanced when aged vehicle exhausts are transported to rural areas and mixed with NH3-rich plumes. We also found that the presence of NH3 had no significant influence on SOA formation from GVE. Very similar oxygen to carbon(O:C) and hydrogen to carbon(H:C) ratios resolved by aerosol mass spectrometer with and without NH3 indicated that the presence of NH3 also had no impact on the average carbon oxidation state of SOA from GVE.
出处 《Science China Chemistry》 SCIE EI CAS CSCD 2015年第9期1377-1384,共8页 中国科学(化学英文版)
基金 supported by the Strategic Priority Research Program of the Chinese Academy of Sciences(XDB05010200) the National Natural Science Foundation of China(41025012/41121063) NSFC-Guangdong Joint Funds(U0833003) the Guangzhou Institute of Geochemistry(GIGCAS 135 Project Y234161001)
关键词 二次有机气溶胶 汽车尾气 汽油车 粒子数浓度 挥发性有机化合物 NH3 臭氧分解 ammonia,vehicle exhaust,secondary organic aerosols(SOA),smog chamber,fine particles,nitrogen oxides,volatile organic compounds
  • 相关文献

参考文献1

二级参考文献29

  • 1Andreae M O, Schmid O, Yang H, Chand D, Yu J Z, Zeng L M et al., 2008. Optical properties and chemical composition of the atmospheric aerosol in urban Guangzhou, China. Atmospheric Environment, 42(25): 6335-6350.
  • 2Bae M S, Schauer J J, Turner J R, 2006. Estimation of the monthly average ratios of organic mass to organic carbon for fine particulate matter at an urban site. Aerosol Science and Technology, 40(12): 1123-1139.
  • 3Bergin M H, Cass G R, Xu J, Fang C, Zeng L M, Yu T et al., 2001. Aerosol radiative, physical, and chemical properties in Beijing during June 1999. Journal Geophysical Research, 106(D16): 17969-17980.
  • 4Bi X H, Zhang G H, Li L, Wang X M, Li M, Sheng G Y et al., 2011. Mixing state of biomass burning particles by single particle aerosol mass spectrometer in the urban area of PRD, China. Atmospheric Environment, 45(20): 3447- 3453.
  • 5Cao J J, Lee S C, Ho K F, Zhang X Y, Zou S C, Fung K et al., 2003. Characteristics of carbonaceous aerosol in Pearl River Delta Region, China during 2001 winter period. Atmospheric Environment, 37(11): 1451-1460.
  • 6Cao J J, Lee S C, Ho K F, Zou S C, Fung K, Li Y et al., 2004. Spatial and seasonal variations of atmospheric organic carbon and elemental carbon in Pearl River Delta Region, China. Atmospheric Environment, 38(27): 4447- 4456.
  • 7Castro L M, Pio C A, Harrison R M, Smith D J T, 1999. Carbona- ceous aerosol in urban and rural European atmospheres: estimation of secondary organic carbon concentrations. Atmospheric Environment, 33(17): 2771-2781.
  • 8Chan C K, Yao X H, 2008. Air pollution in mega cities in China. Atmospheric Environment, 42(1): 1-42.
  • 9Chang D, Song Y, Liu B, 2009. Visibility trends in six megacities in China 1973-2007. Atmospheric Research, 94(2): 161- 167.
  • 10Che H Z, Zhang X Y, Li Y, Zhou Z J, Qu J J, 2007. Horizontal visibility trends in China 19812005. Geophysical Research Letters, 34: L24706. DOI: 10.1029/2007GL031450.

共引文献24

同被引文献84

引证文献7

二级引证文献46

相关作者

内容加载中请稍等...

相关机构

内容加载中请稍等...

相关主题

内容加载中请稍等...

浏览历史

内容加载中请稍等...
;
使用帮助 返回顶部