科研成果 by Type: 期刊论文

2010
Lu K, Zhang Y, Su H, Brauers T, Chou CC, Hofzumahaus A, Liu SC, Kita K, Kondo Y, Shao M, et al. Oxidant (O(3) + NO(2)) production processes and formation regimes in Beijing. Journal of Geophysical Research-AtmospheresJournal of Geophysical Research-Atmospheres. 2010;115.Abstract
For CareBeijing-2006, two sites were established in urban and suburban regions of Beijing in summer 2006. Observations of O(3) and its precursors together with meteorological parameters at both sites are presented. Gross ozone production rate P(O(3)) and sensitivity to nitric oxides (NO(x)) and volatile organic compounds (VOCs) were investigated using an observation-based photochemical box model (OBM). P(O(3)) varied from nearly zero to 120 and 50 ppb h(-1) for urban and suburban sites, respectively. These rates were greater than the accumulation rates of the observed oxidant (O(3) + NO(2)) concentrations. The O(3) episodes typically appeared under southerly wind conditions with high P(O(3)), especially at the urban site. Sensitivity studies with and without measured nitrous acid (HONO) as a model constraint suggested that the estimated P(O(3)) at both sites was strongly enhanced by radical production from HONO photolysis. Both NO(x)- and VOC-sensitive chemistries existed over time scales from hours to days at the two sites. The variation in O(3)-sensitive chemistry was relatively well explained by the ratio of the average daytime total VOC reactivity (k(TVOC)) to NO, with the transition chemistry corresponding to a k(TVOC)/NO value of 2-4 s(-1) ppb(-1). Pronounced diurnal variations in the O(3) production regime were found. In the morning, conditions were always strongly VOC-limited, while in the afternoon, conditions were variable for different days and different sites. The model-calculated results were tested by measurements of H(2)O(2), HNO(3), total OH reactivity, and HO(x) radicals. The OBM was generally capable of correctly simulating the levels of P(O(3)), although it might tend to overpredict the VOC-sensitive chemistry.
Lu K, YuanHang Z, Hang S, Min S, LiMin Z, LiuJu Z, YunRong X, Chung CC, Chou CCK, Wahner A. Regional ozone pollution and key controlling factors of photochemical ozone production in Pearl River Delta during summer time. Science China-ChemistryScience China-Chemistry. 2010;53:651-663.
Lou S, Holland F, Rohrer F, Lu K, Bohn B, Brauers T, Chang CC, Fuchs H, Haeseler R, Kita K, et al. Atmospheric OH reactivities in the Pearl River Delta - China in summer 2006: measurement and model results. Atmospheric Chemistry and PhysicsAtmospheric Chemistry and Physics. 2010;10:11243-11260.
2009
Xiao R, Takegawa N, Kondo Y, Miyazaki Y, Miyakawa T, Hu M, Shao M, Zeng LM, Hofzumahaus A, Holland F, et al. Formation of submicron sulfate and organic aerosols in the outflow from the urban region of the Pearl River Delta in China. Atmospheric EnvironmentAtmospheric Environment. 2009;43:3754-3763.
Hofzumahaus A, Rohrer F, Lu K, Bohn B, Brauers T, Chang C-C, Fuchs H, Holland F, Kita K, Kondo Y, et al. Amplified Trace Gas Removal in the Troposphere. ScienceScience. 2009;324:1702-1704.
2008
周维, 王雪松*, 张远航, 苏杭, 陆克定. 我国NOx污染状况与环境效应及综合控制策略. 北京大学学报(自然科学版). 2008;44(2):323-330.
Hua W, Chen ZM, Jie CY, Kondo Y, Hofzumahaus A, Takegawa N, Chang CC, Lu KD, Miyazaki Y, Kita K, et al. Atmospheric hydrogen peroxide and organic hydroperoxides during PRIDE-PRD'06, China: their concentration, formation mechanism and contribution to secondary aerosols. Atmospheric Chemistry and PhysicsAtmospheric Chemistry and Physics. 2008;8:6755-6773.

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