Corrigendum to “Re-examination of C1–C5 alkyl nitrates in Hong Kong using an observation-based model” [Atmos. Environ. 120 28–37]

2016 ◽  
Vol 129 ◽  
pp. 133
Author(s):  
X.P. Lyu ◽  
Z.H. Ling ◽  
H. Guo ◽  
S.M. Saunders ◽  
S.H.M. Lam ◽  
...  
2021 ◽  
Vol 270 ◽  
pp. 116285
Author(s):  
Lewei Zeng ◽  
Hai Guo ◽  
Xiaopu Lyu ◽  
Beining Zhou ◽  
Zhenhao Ling ◽  
...  

2016 ◽  
Vol 16 (13) ◽  
pp. 8141-8156 ◽  
Author(s):  
Zhenhao Ling ◽  
Hai Guo ◽  
Isobel Jane Simpson ◽  
Sandra Maria Saunders ◽  
Sean Ho Man Lam ◽  
...  

Abstract. C1–C4 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 (∼  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 O3 production, with average reduction rates of 4.1 and 4.7 pptv pptv−1 at TMS and TW, respectively.


2015 ◽  
Vol 120 ◽  
pp. 28-37 ◽  
Author(s):  
X.P. Lyu ◽  
Z.H. Ling ◽  
H. Guo ◽  
S.M. Saunders ◽  
S.H.M. Lam ◽  
...  
Keyword(s):  

2018 ◽  
Vol 52 (10) ◽  
pp. 5581-5589 ◽  
Author(s):  
Lewei Zeng ◽  
Xiaopu Lyu ◽  
Hai Guo ◽  
Shichun Zou ◽  
Zhenhao Ling

2015 ◽  
Vol 15 (16) ◽  
pp. 22597-22636
Author(s):  
Z. H. Ling ◽  
H. Guo ◽  
I. J. Simpson ◽  
S. M. Saunders ◽  
S. H. M. Lam ◽  
...  

Abstract. Alkyl nitrates (RONO2) were measured concurrently at a mountain site (TMS) and an urban site (TW) at the foot of the same mountain in Hong Kong from September to November 2010, when high O3 mixing ratios were frequently observed. The abundance and temporal patterns of five C1–C4 RONO2 and their parent hydrocarbons (RH), the RONO2/RH ratios and photochemical age of air masses at TMS differed from those at TW, reflecting different contributions of direct emissions and secondary formation of RONO2 at the two sites. Relative to 2-BuONO2/n-butane, the measured ratios of C1–C2 RONO2/RH at the two sites exhibited significant positive deviations from pure photochemical (PP) curves and background initial ratio (BIR) curves obtained from laboratory kinetic data, suggesting that background mixing ratios had a significant influence on the RONO2 and RH distributions. In contrast to the C1–C2 RONO2/RH ratios, the evolution for the measured ratios of C3 RONO2/RH to 2-BuONO2/n-butane agreed well with the ratio distributions in the PP and BIR curves at the two sites. Furthermore, the ratios of 1-/2-PrONO2 and yields of 1- and 2-PrONO2 suggested that the C3 RONO2 were mainly from secondary formation at TMS, whereas secondary formation and other additional sources had a significant influence on C3 RONO2 mixing ratios at TW. The source apportionment results confirmed that secondary formation was the dominant contributor to all the RONO2 at TMS, while most of the RONO2 at TW were from secondary formation and biomass burning. The findings of the source apportionments and photochemical evolution of RONO2 are helpful to evaluate photochemical processing in Hong Kong using RONO2 as an indicator.


Chemosphere ◽  
2018 ◽  
Vol 194 ◽  
pp. 275-284 ◽  
Author(s):  
Junwei Song ◽  
Yingyi Zhang ◽  
Yu Huang ◽  
Kin Fai Ho ◽  
Zibing Yuan ◽  
...  

1998 ◽  
Vol 13 (11-s4) ◽  
pp. S289-S293 ◽  
Author(s):  
SSY WONG ◽  
WC YAM ◽  
PHM LEUNG ◽  
PCY WOO ◽  
KY YUEN

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