IEECAS OpenIR  > 黄土与第四纪地质国家重点实验室(2010~)
Wintertime organic and inorganic aerosols in Lanzhou, China:sources, processes, and comparison with the results during summer
Xu,JZ(Xu,Jianzhong)[1]; Shi,JS(Shi,Jinsen)[2]; Zhang,Q(Zhang,Qi)[3]; Ge,XL(Ge,Xinlei)[4]; Canonaco,F(Canonaco,Francesco)[5]; Prévôt,A S.H.(Prévôt,André S. H.)[5,6]; Vonwiller,M(Vonwiller,Matthias)[7]; Szidat,S(Szidat,Sönke)[7]; Ge,JM(Ge,Jinming)[2]; Ma,JM(Ma,Jianmin)[8]; An,YQ(An,Yanqing)[1]; Kang,SC(Kang,Shichang)[1]; Qin,DH(Qin,Dahe)[1]

Lanzhou, which is located in a steep alpine valley in western China, is one of the most polluted cities in China during the wintertime. In this study, an Aerodyne high-resolution time-of-flight aerosol mass spectrometer (HR-ToF-AMS), a seven-wavelength aethalometer, and a scanning mobility particle sizer (SMPS) were deployed during 10 January to 4 February 2014 to study the mass concentrations, chemical processes, and sources of submicrometer particulate matter (PM1/. The average PM1 concentration during this study was 57.3 µg m−3 (ranging from 2.1 to 229.7 µg m−3 for hourly averages), with organic aerosol (OA) accounting for 51.2 %, followed by nitrate (16.5 %), sulfate (12.5 %), ammonium (10.3 %), black carbon (BC, 6.4 %), and chloride (3.0 %). The mass concentration of PM1 during winter was more than twice the average value observed at the same site in summer 2012 (24.5 µg m−3/, but the mass fraction of OA was similar in the two seasons. Nitrate contributed a significantly higher fraction to the PM1 mass in winter than summer (16.5 % vs. 10 %), largely due to more favored partitioning to the particle phase at low air temperature. The mass fractions of both OA and nitrate increased by ∼ 5 % (47 to 52 for OA and 13 to 18 % for nitrate) with the increase of the total PM1 mass loading, while the average sulfate fraction decreased by 6 % (17 to 11 %), indicating the importance of OA and nitrate for the heavy air pollution events in Lanzhou. The size distributions of OA, nitrate, sulfate, ammonium, and chloride all peaked at ∼ 500 nm, with OA being slightly broader, suggesting that aerosol particles were internally mixed during winter, likely due to frequently calm and stagnant air conditions during wintertime in Lanzhou (average wind speed: 0.82 m s−1/. The average mass spectrum of OA showed a medium oxidation degree (average O = C ratio of 0.28), which was lower than that during summer 2012 (O = C D 0.33). This is consistent with weaker photochemical processing during winter. Positive matrix factorization (PMF) with the multi-linear engine (ME-2) solver identified six OA sources, i.e., a hydrocarbon-like OA (HOA), a biomass burning OA (BBOA), a cooking-emitted OA (COA), a coal combustion OA (CCOA), and two oxygenated OA (OOA) factors. One of the OOAs was less oxidized (LO-OOA), and the other one more oxidized (MO-OOA). LO-OOA was the most abundant OA component (22.3 % of OA mass), followed by CCOA (22.0 %), COA (20.2 %), MO-OOA (14.9 %), BBOA (10.8 %), and HOA (9.8 %). The mass fraction of primary OA (D HOA C BBOA C COA C CCOA) increased during high PM pollution periods, indicating that local primary emissions were a main reason for the formation of air pollution events in Lanzhou during winter. Radiocarbon (14C) measurement was conducted on four PM2:5 filter samples from this study, which allowed for a quantitative source apportionment of organic carbon (OC). The non-fossil sources on average accounted for 55 ± 3 % of OC, which could be mainly from biomass burning and cooking activities, suggesting the importance of non-fossil sources for the PM pollution in Lanzhou. Together with the PMF results, we also found that a large fraction (66 ± 10 %) of the secondary OC was from non-fossil OC.

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Document Type期刊论文
Affiliation1.State Key Laboratory of Cryospheric Sciences, Cold and Arid Regions Environmental and EngineeringResearch Institute, CAS, Lanzhou 730000, China;
2.Key Laboratory for Semi-Arid Climate Change of the Ministry of Education, College of Atmospheric Sciences,Lanzhou University, Lanzhou 730000, China;
3.Department of Environmental Toxicology, University of California, Davis, CA 95616, USA;
4.Jiangsu Key Laboratory of Atmospheric Environment Monitoring and Pollution Control (AEMPC), School ofEnvironmental Science and Engineering, Nanjing University of Information Science & Technology, Nanjing 210044, China;
5.Laboratory of Atmospheric Chemistry, Paul Scherrer Institute (PSI), Villigen 5232, Switzerland;
6.State Key Laboratory of Loess and Quaternary Geology and Key Laboratory of Aerosol Chemistry and Physics, Institute ofEarth Environment, Chinese Academy of Sciences, Xi’an 710075 , China;
7.Department of Chemistry and Biochemistry & Oeschger Centre for Climate Change Research, University of Bern,3012 Bern, Switzerland;
8.College of Earth Environmental Science, Lanzhou University, Lanzhou 730000, China
Recommended Citation
GB/T 7714
Xu,JZ,Shi,JS,Zhang,Q,et al. Wintertime organic and inorganic aerosols in Lanzhou, China:sources, processes, and comparison with the results during summer[J]. ATMOSPHERIC CHEMISTRY AND PHYSICS,2016,16:14937-14957.
APA Xu,JZ.,Shi,JS.,Zhang,Q.,Ge,XL.,Canonaco,F.,...&Qin,DH.(2016).Wintertime organic and inorganic aerosols in Lanzhou, China:sources, processes, and comparison with the results during summer.ATMOSPHERIC CHEMISTRY AND PHYSICS,16,14937-14957.
MLA Xu,JZ,et al."Wintertime organic and inorganic aerosols in Lanzhou, China:sources, processes, and comparison with the results during summer".ATMOSPHERIC CHEMISTRY AND PHYSICS 16(2016):14937-14957.
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