Elsevier

Atmospheric Research

Volume 92, Issue 4, June 2009, Pages 434-442
Atmospheric Research

Characteristics of organic and elemental carbon in PM2.5 samples in Shanghai, China

https://doi.org/10.1016/j.atmosres.2009.01.003Get rights and content

Abstract

Shanghai is the largest industrial and commercial city in China, and its air quality has been deteriorating for several decades. However, there are scarce researches on the level and seasonal variation of fine particle (PM2.5) as well as the carbonaceous fractions when compared with other cities in China and around the world. In the present paper, abundance and seasonal characteristics of PM2.5, organic carbon (OC) and elemental carbon (EC) were studied at urban and suburban sites in Shanghai during four season-representative months in 2005–2006 year. PM2.5 samples were collected with high-vol samplers and analyzed for OC and EC using thermal-optical transmittance (TOT) protocol. Results showed that the annual average PM2.5 concentrations were 90.3–95.5 μg/m3 at both sites, while OC and EC were 14.7–17.4 μg/m3 and 2.8–3.0 μg/m3, respectively, with the OC/EC ratios of 5.0–5.6. The carbonaceous levels ranked by the order of Beijing > Guangzhou > Shanghai > Hong Kong. The carbonaceous aerosol accounted for ∼ 30% of the PM2.5 mass. On seasonal average, the highest OC and EC levels occurred during fall, and they were higher than the values in summer by a factor of 2. Strong correlations (r = 0.79–0.93) between OC and EC were found in the four seasons. Average level of secondary organic carbon (SOC) was 5.7–7.2 μg/m3, accounting for ∼ 30% of the total OC. Strong seasonal variation was observed for SOC with the highest value during fall, which was about two times the annual average.

Introduction

Carbonaceous aerosol constitutes a significant fraction of fine particles (PM2.5), and it could account for up to 40% of PM2.5 mass in urban atmosphere (Seinfeld and Pandis, 1998). Carbonaceous species are usually classified into elemental carbon (EC) and organic carbon (OC). EC (sometimes called black carbon) derived from incomplete combustion of carbon-contained materials, while OC can be either released directly into the atmosphere (primary OC, POC) or produced from gas-to-particle reactions (secondary OC, SOC) (Pandis et al., 1992, Turpin and Huntzicker, 1995). EC has strong absorption of solar radiation and is one of the important drivers of global warming (Hansen et al., 2005). OC represents a mixture of hundreds of organic compounds, some of which are mutagenic and/or carcinogenic, such as polycyclic aromatic hydrocarbons (PAHs) and polychlorinated dibenzo-p-dioxins and dibenzofurans (PCDD/Fs) (Feng et al., 2006, Li et al., 2008).

Carbonaceous aerosol in China has drawn special attention in recent years due to its adverse effects on environment and human health and potential influence on climate change (Hamilton and Mansfield, 1991, Qiu and Yang, 2000, Jacobson, 2002). It has been estimated that China contributes roughly one-fifth of the global carbonaceous emissions (Bond et al., 2004). Jacobson (2002) suggested that emission reduction of fossil-fuel carbonaceous particles was possibly the most effective method of slowing global warming. The increased EC aerosols may be responsible for the significant variation of precipitation in eastern China over the past decades (Menon et al., 2002). EC also contributed to the marked degradation of optical depths and visibility in northern China (Qiu and Yang, 2000), and lowered the crop yields by reducing solar radiation that reaches the earth (Chameides et al., 1999).

There are several studies focusing on the field measurements of carbonaceous abundance in PM2.5 in China's industrialized areas, such as Guangzhou and Hong Kong in Pearl River Delta Region (Ho et al., 2002, Ho et al., 2003, Ho et al., 2006, Cao et al., 2003, Cao et al., 2004, Cao et al., 2005, Chow et al., 2005, Duan et al., 2007), Beijing (He et al., 2001, He et al., 2004a, Dan et al., 2004, Duan et al., 2006), and other cities (Guo et al., 2004, Cao et al., 2005, Yang et al., 2005b). However, there are only limited studies in Shanghai (Ye et al., 2003, Yang et al., 2005a, Feng et al., 2006), which is the largest commercial and industrial city in China and also one of the world's largest seaports. World Expositions will be held here in 2010. Furthermore, one-year carbonaceous measurements by Ye et al. (2003) and Yang et al. (2005a) were finished during 1999–2000 year, and since then the air pollution in Shanghai is ameliorating observably. For example, annual PM10 concentration in Shanghai was 100.5 μg/m3 in 2001 versus 86.2 μg/m3 in 2006 (http://www.envir.gov.cn/airnews/).

Ambient air quality in Shanghai began to deteriorate in the 1960s due to large consumption of low-quality coal for rapid industrial development. When coal smoke was somewhat controlled in the 1990s, vehicular population in Shanghai soared up to ∼ 2 million, and the type of air pollution in Shanghai evolved into the combination of coal smoke with vehicular exhaust (Chen, 2003). Great concern on the visibility reduction and public health has been drawn by the heavy PM pollution in Shanghai (Ye et al., 2000), and the primary carbonaceous emission in 2000 was about 16.3 Gg (gigagrams or ktons) for EC and 34.0 Gg for OC (Cao et al., 2006).

The purpose of this paper is to present updated knowledge on abundance and seasonal characteristics of PM2.5-associated EC and OC in Shanghai, which is helpful to investigate of their sources and PM control strategies.

Section snippets

Sampling sites description

Shanghai is located at the east end of the Yangtze River Delta Region and faces the East China Sea (Fig. 1), and possesses a population of over 15 million and a land area of about 6340 km2. Shanghai belongs to the northern subtropical monsoon climate, and northwest wind prevails in wintertime whereas southeast wind in summertime. Annual average of temperature in Shanghai is 15.8 °C, with the lowest in January (3.6 °C) and the highest in July (27.8 °C).

In this study, two sites were selected for

Levels of PM2.5, OC and EC in Shanghai

The statistics for PM2.5 mass, OC and EC at both sampling sites in Shanghai are presented in Table 1. Firstly, it can be seen that the levels of PM2.5 and carbonaceous fractions at suburban site (JD) (95.5 ± 41.8 μg/m3) are a little higher than that at urban site (ZB) (90.3 ± 54.9 μg/m3), suggesting that fine particle pollution occurred not only in the urban, but also in the suburban area of Shanghai. Similar situation was observed by Feng et al. (2006) that there was no clear difference of

Conclusions

Abundance and seasonal characteristics of PM2.5 and carbonaceous species were investigated at two sites at Shanghai, China. On annual average, PM2.5 concentration was 90.3 μg/m3 at ZB Site and 95.5 μg/m3 at JD, indicating the serious situation of fine particle pollution in Shanghai. The concentrations for OC and EC were 14.7 and 2.8 μg/m3 at ZB whereas 17.4 and 3.0 μg/m3 at JD, respectively, following the order of Beijing > Guangzhou > Shanghai > Hong Kong. Carbonaceous aerosol (TCA) accounted

Acknowledgements

This project was financially supported by the Department of Science and Technology of Shandong Province (2006GG2205033, 2007GG2QT06018), National Natural Scientific Foundation of China (40605033, 40503012), and Shanghai Leading Academic Disciplines (S30109). The authors would like to thank Jia-ding Environmental Monitoring Station in Shanghai for the assistant of sampling at the station, Dr. Xiyong Hou from YIC, CAS and Ms. Paromita Chakraborty from GIG, CAS for their helps in this manuscript.

References (54)

  • FangG.-C. et al.

    Organic carbon and elemental carbon in Asia: a review from 1996 to 2006

    Journal of Hazardous Materials

    (2008)
  • FengJ. et al.

    Characteristics of organic matter in PM2.5 in Shanghai

    Chemosphere

    (2006)
  • GuoZ.G. et al.

    The elemental and organic characteristics of PM2.5 in Asian dust episodes in Qingdao, China, 2002

    Atmospheric Environment

    (2004)
  • HamiltonR.S. et al.

    Airborne particulate elemental carbon: Its sources, transport and contribution to dark smoke and soiling

    Atmospheric Environment

    (1991)
  • HeK.B. et al.

    The characteristics of PM2.5 in Beijing, China

    Atmospheric Environment

    (2001)
  • HeZ. et al.

    Carbonaceous aerosol characteristics of PM2.5 particles in Northeastern Asia in summer 2002

    Atmospheric Environment

    (2004)
  • HeL.-Y. et al.

    Measurement of emissions of fine particulate organic matter from Chinese cooking

    Atmospheric Environment

    (2004)
  • HoK.F. et al.

    Carbonaceous characteristics of atmospheric particulate matter in Hong Kong

    The Science of The Total Environment

    (2002)
  • HoK.F. et al.

    Characterization of chemical species in PM2.5 and PM10 aerosols in Hong Kong

    Atmospheric Environment

    (2003)
  • LiH. et al.

    The PCDD/F and PBDD/F pollution in the ambient atmosphere of Shanghai, China

    Chemosphere

    (2008)
  • LonatiG. et al.

    Primary and secondary carbonaceous species in PM2. 5 samples in Milan (Italy)

    Atmospheric Environment

    (2007)
  • NaK. et al.

    Primary and secondary carbonaceous species in the atmosphere of Western Riverside County, California

    Atmospheric Environment

    (2004)
  • PandisS.N. et al.

    Secondary organic aerosol formation and transport

    Atmospheric Environment (Part A)

    (1992)
  • SalmaI. et al.

    Elemental and organic carbon in urban canyon and background environments in Budapest, Hungary

    Atmospheric Environment

    (2004)
  • TurpinB.J. et al.

    Identification of secondary organic aerosol episodes and quantitation of primary and secondary organic aerosol concentrations during SCAQS

    Atmospheric Environment

    (1995)
  • VianaM. et al.

    Comparative analysis of organic and elemental carbon concentrations in carbonaceous aerosols in three European cities

    Atmospheric Environment

    (2007)
  • ViidanojaJ. et al.

    Organic and black carbon in PM2.5 and PM10: 1 year of data from an urban site in Helsinki, Finland

    Atmospheric Environment

    (2002)
  • Cited by (249)

    View all citing articles on Scopus
    View full text