TY - JOUR
T1 - Characteristics of carbonaceous aerosols in Beijing, China
AU - Duan, Fengkui
AU - He, Kebin
AU - Ma, Yongliang
AU - Jia, Yingtao
AU - Yang, Fumo
AU - Lei, Yu
AU - Tanaka, S.
AU - Okuta, T.
N1 - Funding Information:
This work was supported by the 3E Research Program project founded by Keio University, Japan. Beijing EPA ( http://www.bjepb.gov.cn ) is appreciated for providing us with ambient air quality data.
Copyright:
Copyright 2020 Elsevier B.V., All rights reserved.
PY - 2005/7
Y1 - 2005/7
N2 - Carbonaceous aerosols and PM10 were monitored from September 8 to November 30, 2002, in a semi-urban site (Tsinghua University) in Beijing. Daily concentrations of OC and EC ranged from 7.1 to 65.9 μg C m-3 and from 1.3 to 26.1 μg C m-3, with the overall average concentrations of 21.2 μg C m-3 and 7.3 μg C m-3, respectively. The diurnal variation of carbonaceous concentrations on 2 h basis presented two-peak trend, which was attributed to the cooperative effect of local meteorological conditions and anthropogenic sources such as traffic exhaust and human outdoor activities. Daily average OC/EC ratio varied between 1.5 and 5.3 with an average of 3.0. Strong correlation between OC and EC (R 2 = 0.8) indicated that their main sources were common. The frequency of OC/EC ratio presented Gaussian normal distribution trend in fall, of which the peak value appeared in the range of 2.8-5. In winter, it presented bi-peak mode, with the first peak near 1.4-1.6, and the second between 2.8 and 5. The high value (2.8-5) implied the SOC formation in both seasons, and the low one probably suggested the primary OC/EC ratio from coal burning in winter. Averagely, PM10 and carbonaceous species exhibited higher concentrations in Wednesday than in other weekdays, which could be ascribed to the low wind speed (1.6 m s-1) and high humidity (62.9%). OC was the abundant component accounting for 76% of TC. OC and EC contributed 15% and 5% to PM10, respectively. The estimation on a minimum OC/EC ratio (1.5) basis showed that SOC accounted more than 50% for the total organic carbon. Even in winter, the SOC contribution to OC was also significant, as high as 40%.
AB - Carbonaceous aerosols and PM10 were monitored from September 8 to November 30, 2002, in a semi-urban site (Tsinghua University) in Beijing. Daily concentrations of OC and EC ranged from 7.1 to 65.9 μg C m-3 and from 1.3 to 26.1 μg C m-3, with the overall average concentrations of 21.2 μg C m-3 and 7.3 μg C m-3, respectively. The diurnal variation of carbonaceous concentrations on 2 h basis presented two-peak trend, which was attributed to the cooperative effect of local meteorological conditions and anthropogenic sources such as traffic exhaust and human outdoor activities. Daily average OC/EC ratio varied between 1.5 and 5.3 with an average of 3.0. Strong correlation between OC and EC (R 2 = 0.8) indicated that their main sources were common. The frequency of OC/EC ratio presented Gaussian normal distribution trend in fall, of which the peak value appeared in the range of 2.8-5. In winter, it presented bi-peak mode, with the first peak near 1.4-1.6, and the second between 2.8 and 5. The high value (2.8-5) implied the SOC formation in both seasons, and the low one probably suggested the primary OC/EC ratio from coal burning in winter. Averagely, PM10 and carbonaceous species exhibited higher concentrations in Wednesday than in other weekdays, which could be ascribed to the low wind speed (1.6 m s-1) and high humidity (62.9%). OC was the abundant component accounting for 76% of TC. OC and EC contributed 15% and 5% to PM10, respectively. The estimation on a minimum OC/EC ratio (1.5) basis showed that SOC accounted more than 50% for the total organic carbon. Even in winter, the SOC contribution to OC was also significant, as high as 40%.
KW - Elemental carbon
KW - OC/EC ratio
KW - Organic carbon
KW - PM
KW - Secondary organic aerosol
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U2 - 10.1016/j.chemosphere.2004.12.035
DO - 10.1016/j.chemosphere.2004.12.035
M3 - Article
C2 - 15924954
AN - SCOPUS:19544380535
SN - 0045-6535
VL - 60
SP - 355
EP - 364
JO - Chemosphere
JF - Chemosphere
IS - 3
ER -