Dual carbon isotope-based source apportionment and light absorption properties of water soluble organic carbon in PM 2.5 over China

2020 ◽  
Author(s):  
Yangzhi Mo ◽  
Jun Li ◽  
Zhineng Cheng ◽  
Guangcai Zhong ◽  
Sanyuan Zhu ◽  
...  
Keyword(s):  
Organic Carbon ◽  
Source Apportionment ◽  
Carbon Isotope ◽  
Light Absorption ◽  
Water Soluble ◽  
Absorption Properties ◽  
Pm 2.5 ◽  
Water Soluble Organic Carbon ◽  
Soluble Organic Carbon

A yearlong study of water-soluble organic carbon in Beijing II: Light absorption properties

2014 ◽  
Vol 89 ◽  
pp. 235-241 ◽  
Author(s):  
Zhenyu Du ◽  
Kebin He ◽  
Yuan Cheng ◽  
Fengkui Duan ◽  
Yongliang Ma ◽  
...  
Keyword(s):  
Organic Carbon ◽  
Light Absorption ◽  
Water Soluble ◽  
Absorption Properties ◽  
Water Soluble Organic Carbon ◽  
Soluble Organic Carbon

scholarly journals Water-soluble organic carbon aerosols during a full New Delhi winter: Isotope-based source apportionment and optical properties

2014 ◽  
Vol 119 (6) ◽  
pp. 3476-3485 ◽  
Author(s):  
Elena N. Kirillova ◽  
August Andersson ◽  
Suresh Tiwari ◽  
Atul Kumar Srivastava ◽  
Deewan Singh Bisht ◽  
...  
Keyword(s):  
Optical Properties ◽  
Organic Carbon ◽  
Source Apportionment ◽  
Water Soluble ◽  
New Delhi ◽  
Water Soluble Organic Carbon ◽  
Soluble Organic Carbon ◽  
Carbon Aerosols

scholarly journals Mass absorption efficiency of elemental carbon and water-soluble organic carbon in Beijing, China

2011 ◽  
Vol 11 (22) ◽  
pp. 11497-11510 ◽  
Author(s):  
Y. Cheng ◽  
K.-B. He ◽  
M. Zheng ◽  
F.-K. Duan ◽  
Z.-Y. Du ◽  
...  
Keyword(s):  
Organic Carbon ◽  
Biomass Burning ◽  
Light Absorption ◽  
Elemental Carbon ◽  
Organic Aerosol ◽  
Absorption Efficiency ◽  
Water Soluble ◽  
Water Soluble Organic Carbon ◽  
Soluble Organic Carbon ◽  
Mass Absorption Efficiency

Abstract. The mass absorption efficiency (MAE) of elemental carbon (EC) in Beijing was quantified using a thermal-optical carbon analyzer. The MAE measured at 632 nm was 8.45±1.71 and 9.41±1.92 m2 g−1 during winter and summer respectively. The daily variation of MAE was found to coincide with the abundance of organic carbon (OC), especially the OC to EC ratio, perhaps due to the enhancement by coating with organic aerosol (especially secondary organic aerosol, SOA) or the artifacts resulting from the redistribution of liquid-like organic particles during the filter-based absorption measurements. Using a converting approach that accounts for the discrepancy caused by measurements methods of both light absorption and EC concentration, previously published MAE values were converted to the equivalent-MAE, which is the estimated value if using the same measurement methods as used in this study. The equivalent-MAE was found to be much lower in the regions heavily impacted by biomass burning (e.g., below 2.7 m2 g−1 for two Indian cities). Results from source samples (including diesel exhaust samples and biomass smoke samples) also demonstrated that emissions from biomass burning would decrease the MAE of EC. Moreover, optical properties of water-soluble organic carbon (WSOC) in Beijing were presented. Light absorption by WSOC exhibited strong wavelength (λ) dependence such that absorption varied approximately as λ−7, which was characteristic of the brown carbon spectra. The MAE of WSOC (measured at 365 nm) was 1.79±0.24 and 0.71±0.20 m2 g−1 during winter and summer respectively. The large discrepancy between the MAE of WSOC during winter and summer was attributed to the difference in the precursors of SOA such that anthropogenic volatile organic compounds (AVOCs) should be more important as the precursors of SOA in winter. The MAE of WSOC in Beijing was much higher than results from the southeastern United States which were obtained using the same method as used in this study, perhaps due to the stronger emissions of biomass burning in China.

Light absorption by water-soluble organic carbon in atmospheric fine particles in the central Tibetan Plateau

2017 ◽  
Vol 24 (26) ◽  
pp. 21386-21397 ◽  
Author(s):  
YanGe Zhang ◽  
JianZhong Xu ◽  
JinSen Shi ◽  
CongHui Xie ◽  
XinLei Ge ◽  
...  
Keyword(s):  
Tibetan Plateau ◽  
Organic Carbon ◽  
Light Absorption ◽  
Fine Particles ◽  
Water Soluble ◽  
Central Tibetan Plateau ◽  
Water Soluble Organic Carbon ◽  
Soluble Organic Carbon

scholarly journals Sources and light absorption of water-soluble organic carbon aerosols in the outflow from northern China

2014 ◽  
Vol 14 (3) ◽  
pp. 1413-1422 ◽  
Author(s):  
E. N. Kirillova ◽  
A. Andersson ◽  
J. Han ◽  
M. Lee ◽  
Ö. Gustafsson
Keyword(s):  
Organic Carbon ◽  
Light Absorption ◽  
Radiative Forcing ◽  
Large Fraction ◽  
Northern China ◽  
Water Soluble ◽  
Cloud Formation ◽  
Carbonaceous Aerosols ◽  
Water Soluble Organic Carbon ◽  
Soluble Organic Carbon

Abstract. High loadings of anthropogenic carbonaceous aerosols in Chinese air influence the air quality for over one billion people and impact the regional climate. A large fraction (17–80%) of this aerosol carbon is water-soluble, promoting cloud formation and thus climate cooling. Recent findings, however, suggest that water-soluble carbonaceous aerosols also absorb sunlight, bringing additional direct and indirect climate warming effects, yet the extent and nature of light absorption by this water-soluble "brown carbon" and its relation to sources is poorly understood. Here, we combine source estimates constrained by dual carbon isotopes with light-absorption measurements of water-soluble organic carbon (WSOC) for a March 2011 campaign at the Korea Climate Observatory at Gosan (KCOG), a receptor station in SE Yellow Sea for the outflow from northern China. The mass absorption cross section at 365 nm (MAC365) of WSOC for air masses from N. China were in general higher (0.8–1.1 m2 g−1), than from other source regions (0.3–0.8 m2 g−1). However, this effect corresponds to only 2–10% of the radiative forcing caused by light absorption by elemental carbon. Radiocarbon constraints show that the WSOC in Chinese outflow had significantly higher fraction fossil sources (30–50%) compared to previous findings in S. Asia, N. America and Europe. Stable carbon (δ13C) measurements were consistent with aging during long-range air mass transport for this large fraction of carbonaceous aerosols.

scholarly journals Water-soluble organic carbon over the Pearl River Delta region during fall–winter: spatial variations and source apportionment

2013 ◽  
Vol 13 (5) ◽  
pp. 13773-13798 ◽  
Author(s):  
X. Ding ◽  
X.-M. Wang ◽  
Q.-F. He ◽  
X.-X. Fu ◽  
B. Gao
Keyword(s):  
Organic Carbon ◽  
Source Apportionment ◽  
Pearl River Delta ◽  
Water Soluble ◽  
Pearl River ◽  
The Pearl River Delta ◽  
Water Soluble Organic Carbon ◽  
Soluble Organic Carbon ◽  
Rural Sites ◽  
The Pearl River

Abstract. Water-soluble organic carbon (WSOC) is a major component of carbonaceous aerosols. However, the detailed information of WSOC origins is still unclear. In the current study, fine particles (PM2.5) were collected at one sub-urban and two rural sites in the Pearl River Delta (PRD) region, south China during fall–winter 2008 to measure WSOC and organic tracers of biomass burning (BB) and secondary organic aerosols (SOA) from isoprene, monoterpenes, β-caryophyllene, aromatics and 2-ring polycyclic aromatic hydrocarbons (PAHs). WSOC concentrations ranged from 7.63 to 11.5 μg C m−3 and accounted for 38.8–57.9% of organic carbon (OC). Both WSOC and water-insoluble organic carbon (WIOC) exhibited higher levels at the sub-urban site than the rural sites. Subtracting BB-derived WSOC (WSOCBB) from measured WSOC, secondary OC (SOC) and primary OC (POC) were estimated that POC exhibited dominance over SOC and contributed 68–79% to OC. Significant correlation between WSOC and EC was observed, suggesting that BB could have important contributions to ambient WSOC in the PRD region during fall–winter. Organic tracers were applied to do source apportionment of WSOC, which further confirmed that BB was the dominant contributor, accounting for 42–47% of measured WSOC. SOC estimated by SOA tracers totally contributed 22–40% of WSOC, among which anthropogenic SOC (sum of aromatics and 2-ring PAHs, 18–25%) exhibited dominance over biogenic SOC (sum of isoprene, monoterpenes and β-caryophyllene, 4–15%). The unexplained WSOC (18–31%) showed a positive correlation with POC, indicating that this portion might be associated with POC aging.

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