Impact of sulfate and nitrate on black carbon aerosols at Nanjing in winter and summer
YANG Yi-fan1, TANG Li-li2,3, XU Xiao-feng1, JIANG Lei2, LIU Dan-tong4, ZHANG Yun-jiang5,6, HUA Yan2, DU Song-shan3, WANG Zhuang2, ZHOU Hong-cang2
1. School of Atmospheric Physics, Nanjing University of Information Science & Technology, Nanjing 210044, China;
2. Jiangsu Collaborative Innovation Center of Atmospheric Environment and Equipment Technology(CICAEET), School of Environmental Science and Engineering, Nanjing University of Information Science & Technology, Nanjing 210044, China;
3. Jiangsu Environmental Monitoring Center, Nanjing 210036, China;
4. Centre for Atmospheric Science, School of Earth, Atmospheric and Environmental Sciences, University of Manchester, Manchester M139 PL, UK;
5. Institut National de l'Environnement Industriel et des Risques, Verneuil-en-Halatte 60550, France;
6. Laboratoire des Sciences du Climat et l'Environment, CNRS-CEA-UVSQ, Gif sur Yvette 91191, France
The impact of nitrate and sulfate aerosols on the mixing state of black carbon (BC) particles was investigated by using on-line measurements of a single particles soot photometer (SP2) and a MARGA in urban Nanjing in winter and summer. Results showed that the mass concentration of BC was in the range of 1.01~14.5μg/m3 (0.20~3.81μg/m3), with an average value of (4.39±2.66)μg/m3[(1.67±0.76)μg/m3] inwinter (summer), respectively. The diurnal variations of BC particles presented two peaks relative to rush hours in morning and evening. The mixing state of BC-containing particles were evaluated as a ratio of Dp/Dc, the average ratio of which was 1.81±0.21 (1.24±0.08) and ranged from 1.39 to 2.34 (from 1.03 to 1.45) in winter (summer), respectively. Dp/Dcshowed an opposite diurnal trend as comparing with BC, where made more obvious variations for winter. Dp/Dccorrelated well with sulfate and nitrate, and showed higher correlation with nitrate (sulfate) in winter (summer), respectively. Local emissions were the major source contributing to BC, the mixing state of which was more significant influence of nitrate and sulfate during clean periods in winter. The correlation between Dp/Dcwith sulfate and nitrate in winter was lower during heavy pollution periods, resulting from the effects of both local emissions and regional transports on ambient BC particles.
杨一帆, 汤莉莉, 许潇锋, 蒋磊, 刘丹彤, 张运江, 花艳, 杜嵩山, 王壮, 周宏仓. 南京冬夏硫酸盐和硝酸盐对黑碳混合态的影响[J]. 中国环境科学, 2018, 38(4): 1221-1230.
YANG Yi-fan, TANG Li-li, XU Xiao-feng, JIANG Lei, LIU Dan-tong, ZHANG Yun-jiang, HUA Yan, DU Song-shan, WANG Zhuang, ZHOU Hong-cang. Impact of sulfate and nitrate on black carbon aerosols at Nanjing in winter and summer. CHINA ENVIRONMENTAL SCIENCECE, 2018, 38(4): 1221-1230.
Cooke W F, Liousse C, Cachier H, et al. Construction of a 1°×1° fossil fuel emission data set for carbonaceous aerosol and implementation and radiative impact in the ECHAM4model[J]. Journal of Geophysical Research Atmospheres, 1999,104(D18):22137-22162.
[2]
Irina M, Elissa W, Helen S, et al. Black Carbon Exposure, Oxidative Stress Genes, and Blood Pressure in a Repeated-Measures Study[J]. Environmental Health Perspectives, 2009, 117(11):1767-1772.
[3]
Jacobson M Z. Climate response of fossil fuel and biofuel soot, accounting for soot's feedback to snow and sea ice albedo and emissivity[J]. Journal of Geophysical Research Atmospheres, 2004,109(D21):D21201.
[4]
Jacobson M Z. Control of fossil-fuel particulate black carbon and organic matter, possibly the most effective method of slowing global warming[J]. Journal of Geophysical Research Atmospheres, 2002,107(D19):ACH 16-1-ACH 16-22.
[5]
Liu D, Flynn M, Gysel M, et al. Single particle characterization of black carbon aerosols at a tropospheric alpine site in Switzerland[J]. Atmospheric Chemistry & Physics Discussions, 2010, 10(2010):7389-7407.
[6]
Laborde M, Crippa M, Tritscher T, et al. Black carbon physical properties and mixing state in the European megacity Paris[J]. Atmospheric Chemistry & Physics, 2013,13(11):5831-5856.
[7]
Wentzel M, Gorzawski H, Naumann K H, et al. Transmission electron microscopical and aerosol dynamical characterization of soot aerosols[J]. Journal of Aerosol Science, 2003,34(10):1347-1370.
[8]
Saathoff H, Naumann K H, Schnaiter M, et al. Coating of soot and (NH4)2SO4 particles by ozonolysis products of a-pinene[J]. Journal of Aerosol Science, 2003,34(10):1297-1321.
[9]
Schwarz J P, Spackman J R, Fahey D W, et al. Coatings and their enhancement of black carbon light absorption in the tropical atmosphere[J]. Journal of Geophysical Research Atmospheres, 2007,113(D3):D03203.
[10]
Shiraiwa M, Kondo Y, Moteki N, et al. Evolution of mixing state of black carbon in polluted air from Tokyo[J]. Geophysical Research Letters, 2007,34(16):L16803.
[11]
Lewis K A, Arnott W P, Moosmüller H, et al. Reduction in biomass burning aerosol light absorption upon humidification:roles of inorganically-induced hygroscopicity, particle collapse, and photoacoustic heat and mass transfer[J]. Atmospheric Chemistry & Physics, 2009,9(22):8949-8966.
[12]
Liu D, Allan J, Whitehead J, et al. Ambient black carbon particle hygroscopic properties controlled by mixing state and composition[J]. Atmospheric Chemistry & Physics, 2013,13(4):2015-2029.
[13]
Bond T C, Habib G, Bergstrom R W. Limitations in the enhancement of visible light absorption due to mixing state[J]. Journal of Geophysical Research Atmospheres, 2006,111(D20):D20211.
Huang X F, Sun T L, Zeng L W, et al. Black carbon aerosol characterization in a coastal city in South China using a single particle soot photometer[J]. Atmospheric Environment, 2012, 51(5):21-28.
Baumgardner D, Kok G, Raga G. Warming of the Arctic lower stratosphere by light absorbing particles[J]. Geophysical Research Letters, 2004,310(6):337-357.
[28]
Schwarz J P, Gao R S, Fahey D W, et al. Single-particle measurements of midlatitude black carbon and light-scattering aerosols from the boundary layer to the lower stratosphere[J]. Journal of Geophysical Research Atmospheres, 2006,111(2006):D16207.
[29]
Liu D, Allan J D, Young D E, et al. Size distribution, mixing state and source apportionment of black carbon aerosol in London during wintertime[J]. Atmospheric Chemistry & Physics, 2014, 14(18):10061-10084.
Zhang Y, Tang L, Yu H, et al. Chemical composition, sources and evolution processes of aerosol at an urban site in Yangtze River Delta, China during winter time[J]. Atmospheric Environment, 2015,123:339-349.
Allen G A, Lawrence J, Koutrakis P. Field validation of a semi-continuous method for aerosol black carbon (aethalometer) and temporal patterns of summertime hourly black carbon measurements in southwestern PA[J]. Atmospheric Environment, 1999,33(5):817-823.
[48]
Hyvärinen A P, Kolmonen P, Kerminen V M, et al. Aerosol black carbon at five background measurement sites over Finland, a gateway to the Arctic[J]. Atmospheric Environment, 2011,45(24):4042-4050.
[49]
Laborde M, Crippa M, Tritscher T, et al. Black carbon physical properties and mixing state in the European megacity Paris[J]. Atmospheric Chemistry & Physics, 2013,13(11):5831-5856.
[50]
Schwarz J P, Gao R S, Spackman J R, et al. Measurement of the mixing state, mass, and optical size of individual black carbon particles in urban and biomass burning emissions[J]. Geophysical Research Letters, 2008,35(13):L13810.
[51]
唐孝炎,张远航,邵敏.大气环境化学[M]. 北京:高等教育出版社, 2006:63-70.
[52]
Riemer N, Vogel H, Vogel B. Soot aging time scales in polluted regions during day and night[J]. Atmospheric Chemistry & Physics & Discussions, 2004,4(7):1885-1893.
[53]
Yue D L, Hu M, Zhang R Y, et al. The roles of sulfuric acid in new particle formation and growth in the mega-city of Beijing[J]. Atmospheric Chemistry & Physics Discussions, 2010,10(2):4953-4960.