New insight into the spatiotemporal variability and source apportionments of C1-C4 alkyl nitrates in Hong Kong

被引:23
|
作者
Ling, Zhenhao [1 ,2 ]
Guo, Hai [2 ]
Simpson, Isobel Jane [3 ]
Saunders, Sandra Maria [4 ]
Lam, Sean Ho Man [4 ,5 ]
Lyu, Xiaopu [2 ]
Blake, Donald Ray [3 ]
机构
[1] Sun Yat Sen Univ, Sch Atmospher Sci, Guangzhou, Guangdong, Peoples R China
[2] Hong Kong Polytech Univ, Dept Civil & Environm Engn, Air Qual Studies, Hong Kong, Hong Kong, Peoples R China
[3] Univ Calif Irvine, Dept Chem, Irvine, CA 92717 USA
[4] Univ Western Australia, Sch Chem & Biochem, Perth, WA, Australia
[5] Pacific Environm Ltd, Perth, WA, Australia
基金
中国国家自然科学基金;
关键词
VOLATILE ORGANIC-COMPOUNDS; PEARL RIVER DELTA; MASTER CHEMICAL MECHANISM; TERM ATMOSPHERIC MEASUREMENTS; PHOTOCHEMICAL OZONE FORMATION; ABSORPTION CROSS-SECTIONS; MCM V3 PART; COMPOUNDS VOCS; TROPOSPHERIC DEGRADATION; TEMPORAL VARIABILITY;
D O I
10.5194/acp-16-8141-2016
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
C-1-C-4 alkyl nitrates (RONO2) were measured concurrently at a mountain site, Tai Mo Shan (TMS), and an urban site, Tsuen Wan (TW), at the base of the same mountain in Hong Kong from September to November 2010. Although the levels of parent hydrocarbons were much lower at TMS (p < 0.05), similar alkyl nitrate levels were found at both sites regardless of the elevation difference, suggesting various source contributions of alkyl nitrates at the two sites. Prior to using a positive matrix factorization (PMF) model, the data at TW were divided into "meso" and "non-meso" scenarios for the investigation of source apportionments with the influence of mesoscale circulation and regional transport, respectively. Secondary formation was the prominent contributor of alkyl nitrates in the meso scenario (60 +/- 2 %, 60.2 +/- 1.2 pptv), followed by biomass burning and oceanic emissions, while biomass burning and secondary formation made comparable contributions to alkyl nitrates in the non-meso scenario, highlighting the strong emissions of biomass burning in the inland Pearl River delta (PRD) region. In contrast to TW, the alkyl nitrate levels measured at TMS mainly resulted from the photooxidation of the parent hydrocarbons at TW during mesoscale circulation, i.e., valley breezes, corresponding to 52-86% of the alkyl nitrate levels at TMS. Furthermore, regional transport from the inland PRD region made significant contributions to the levels of alkyl nitrates (similar to 58-82 %) at TMS in the non-meso scenario, resulting in similar levels of alkyl nitrates observed at the two sites. The simulation of secondary formation pathways using a photochemical box model found that the reaction of alkyl peroxy radicals (RO2) with nitric oxide (NO) dominated the formation of RONO2 at both sites, and the formation of alkyl nitrates contributed negatively to O-3 production, with average reduction rates of 4.1 and 4.7 pptv pptv(-1) at TMS and TW, respectively.
引用
收藏
页码:8141 / 8156
页数:16
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