Temporal variations of the abundance and optical properties of water soluble Humic-Like Substances (HULIS) in PM2.5 at Guangzhou, China

被引:78
作者
Fan, Xingjun [1 ,2 ]
Song, Jianzhong [1 ]
Peng, Ping'an [1 ]
机构
[1] Chinese Acad Sci, Guangzhou Inst Geochem, State Key Lab Organ Geochem, Guangzhou 510640, Guangdong, Peoples R China
[2] Anhui Sci & Technol Univ, Coll Resource & Environm, Hefei 233100, Anhui, Peoples R China
关键词
HULIS; Abundance; Special UV absorbance; Biomass burning; Secondary atmospheric formation; PEARL RIVER DELTA; ORGANIC-CARBON; CHEMICAL CHARACTERISTICS; AEROSOL-PARTICLES; SIZE DISTRIBUTION; AMBIENT AEROSOLS; MOLECULAR-WEIGHT; URBAN; MATTER; REGION;
D O I
10.1016/j.atmosres.2015.12.024
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
Humic-Like Substances (HULIS) are important macromolecular compounds that are present in PM2.5 and play significant roles in the atmospheric environment. In this study, 48 PM2.5 samples were collected from February 2010 to January 2011 at an urban site in Guangzhou, southern China. The water soluble HULIS fractions in PM2.5 were analyzed to explore the temporal variation of abundance and optical properties and to identify their possible sources. The HULIS concentrations were in the range of 0.4 to 8.2 mu g C m(-3), with a mean of 2.4 mu g C m(-3). HULIS are important components in organic aerosols, accounting for 17 +/- 5% of the organic carbon (OC), and 49 +/- 6 and 68 +/- 5% of water soluble organic carbon (WSOC) as determined with a total organic carbon (TOC) analyzer and UV absorbance at 250 nm, respectively. The special UV absorbance (SUVA) at 254 nm and 280 nm and the E-250/E-365 ratio of HULIS were 3.2 +/- 0.5 L (m mg C)(-1), 2.2 +/- 0.4 L (m mg C)(-1), and 5.9 +/- 0.9, respectively. The HULLS fractions had higher concentrations, slightly higher SUVA values, and lower E-250/E-365 ratios from November to January, indicating the important contribution of aromatic compounds to HULIS in the dry season. The concentrations of HULIS were positively correlated with water soluble K+, secondary organic carbon (SOC), and secondary inorganic ions (NH4+, NO3-, and SO42-). These results suggest that biomass burning and secondary photochemical formation are both sources of HULLS in our study area. In addition, the SUVA(280) of HULIS was strongly correlated with k(+) and SOC, suggesting that HULIS properties were also influenced by their primary source of biomass burning and secondary atmospheric formation. (C) 2016 Elsevier B.V. All rights reserved.
引用
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页码:8 / 15
页数:8
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