利用HYSPLIT模型研究珠三角地区VOCs时空分布特征

张涛, 王新明, 周炎, 岳玎利, 陈多宏, 区宇波

中国环境科学 ›› 2020, Vol. 40 ›› Issue (10) : 4216-4223.

PDF(917 KB)
PDF(917 KB)
中国环境科学 ›› 2020, Vol. 40 ›› Issue (10) : 4216-4223.
大气污染与控制

利用HYSPLIT模型研究珠三角地区VOCs时空分布特征

  • 张涛1,2,3, 王新明1, 周炎3, 岳玎利3, 陈多宏3, 区宇波3
作者信息 +

Spatial and temporal distribution characteristics of VOCs in the Pearl River Delta region using HYSPLIT model

  • ZHANG Tao1,2,3, WANG Xin-ming1, ZHOU Yan3, YUE Ding-li3, CHEN Duo-hong3, OU Yu-bo3
Author information +
文章历史 +

摘要

于2016年在中国广东大气超级监测站,开展4个季节的VOCs长时间观测,共获得2142组有效数据,并利用HYSPLIT模型分析珠三角地区VOCs时空分布特征.结果表明,各类VOCs混合比和化学反应活性具有明显的季节变化特点.观测期间,VOCs平均浓度为(18.523±20.978)×10-9,其中,低碳烯烃和苯系物二者混合比之和仅占46%,但贡献了85%的·OH消耗速率(LOH)、82%的臭氧生成潜势(OFP)和97%的二次气溶胶生成潜势(SOAFP).观测站点主要受来自北部内陆地区气团(1#)、西部内陆地区气团(2#)、台湾海峡南端气团(3#)以及南部海洋地区气团(4#)的影响.1#气团中炔烃和苯系物的混合比占比最高,分别达到10%、37%,而3#气团中低碳烷烃的浓度水平最高,达到(8.437±5.561)×10-9.通过估算气团中VOCs的化学反应活性,可以发现,1#气团的VOCs化学反应活性最强,其对O3和SOA的生成贡献最高.1#、2#、3#和4#气团中VOCs的化学反应活性主要由苯系物和低碳烯烃贡献.

Abstract

Based on the long time observation of VOCs at Guangdong Atmospheric Supersite (GAS) in the four seasons of 2016, 2142 sets of valid data were obtained. Using HYSPLIT model, the spatial and temporal distribution characteristics of VOCs in the Pearl River Delta region were analyzed. Mixing ratios and chemical reactivities of VOCs had obvious seasonal variation characteristics. The average concentration of VOCs was (18.523±20.978)×10-9 during the observation period. Though the mixing ratios of C2~C5 alkenes and BTEX accounted for only 46%, they contributed 85% of·OH loss rate (LOH)、82% of Ozone Formation Potential (OFP) and 97% of Secondary Oragnic Aerosol Formation Potential (SOAFP). The observation sites were mainly affected by the air masses from the northern inland areas (1#), the western inland areas (2#), the southern tip of the Taiwan Strait (3#) and the southern marine areas (4#). The mixing ratios of alkynes and BTEX of 1# air masses were both the highest, respectively, 10% and 37%, and the concentration of C2~C5 alkanes of 3# air masses was the highest, reaching (8.437±5.561)×10-9. By estimating the chemical reactivities of VOCs of air masses, it was found that the chemical reactivities of VOCs of 1# air masses were the strongest, and their contributions to O3 and SOA production were the highest. The chemical reactivities of VOCs of air masses of 1#, 2#, 3# and 4# were mainly contributed by BTEX and C2~C5 alkenes.

关键词

·OH消耗速率 / 臭氧生成潜势 / 二次有机气溶胶 / 二次有机气溶胶生成潜势 / 轨迹聚类

Key words

·OH loss rate / ozone formation potential / secondary oragnic aerosol formation potential / secondary organic aerosol / trajectory clustering

引用本文

导出引用
张涛, 王新明, 周炎, 岳玎利, 陈多宏, 区宇波. 利用HYSPLIT模型研究珠三角地区VOCs时空分布特征[J]. 中国环境科学. 2020, 40(10): 4216-4223
ZHANG Tao, WANG Xin-ming, ZHOU Yan, YUE Ding-li, CHEN Duo-hong, OU Yu-bo. Spatial and temporal distribution characteristics of VOCs in the Pearl River Delta region using HYSPLIT model[J]. China Environmental Science. 2020, 40(10): 4216-4223
中图分类号: X513   

参考文献

[1] Zhang Y H, Hu M, Zhong L J, et al. Regional integrated experiments on air quality over Pearl River Delta 2004(PRIDE-PRD2004):Overview[J]. Atmospheric Environment, 2008,42(25):6157-6173.
[2] Wang T, Xue L K, Brimblecombe P, et al. Ozone pollution in China:A review of concentrations, meteorological influences, chemical precursors, and effects[J]. Science of the Total Environment, 2016, 575(JAN):1582-1596.
[3] Guo H, Jiang F, Cheng H R, et al. Concurrent observations of air pollutants at two sites in the Pearl River Delta and the implication of regional transport[J]. Atmospheric Chemistry & Physics, 2009,9(2):7343-7360.
[4] Wang T, Wei X L, Ding A J, et al. Increasing surface ozone concentrations in the background atmosphere of Southern China, 1994~2007[J]. Atmospheric Chemistry and Physics, 2009,9(2):6217-6227.
[5] Guangdong Provincial Environmental Monitoring Centre; Environmental Protection Department, Hong Kong SARG; Environmental Protection Bureau, Macao SARG; Meteorological and Geophysical Bureau, Macao SARG. Guangdong-Hong Kong-Macao Pearl River Delta regional air quality monitoring network:A report of monitoring Results in 2017[EB/OL].[2019-12-20]. http://gdee.gd.gov.cn/protect/P0201806/P020180620/P020180620631772750308.pdf.
[6] Seinfeld J H, Pandis S N. Atmospheric chemistry and physics, from air pollution to climate change[M]. 3rd ed. Hoboken, New Jersey:John Wily & Sons Incorporation. 2016:583-632.
[7] Taylor O C. Importance of Peroxyacetyl Nitrate (PAN) as a phytotoxic air pollutant[J]. Journal of the Air Pollution Control Association, 1969,19(5):347-351.
[8] Singh H B, Herlth D, O'Hara D, et al. Relationship of peroxyacetyl nitrate to active and total odd nitrogen at northern high latitudes:Influence of reservoir species on NOx and O3[J]. Journal of Geophysical Research, 1992,97(D15):16523-16530.
[9] Chung S H, Seinfeld, J H. Global distribution and climate forcing of carbonaceous aerosols[J]. Journal of Geophysical Research, 2002, 107(D19):4407-4440.
[10] Ramanathan V, Crutzen P J, Kiehl J T, et al. Atmosphere aerosols, climate, and the hydrological cycle[J]. Science, 2001,294(5549):2119-2124.
[11] Geron C D, Pierce T E, Guenther A B. Reassessment of biogenic volatile organic compound emissions in the Atlanta area[J]. Atmospheric Environment, 1995,29(94):1569-1571,1573-1578.
[12] Garzon J P, Huertas J I, Magana M, et al. Volatile organic compounds in the atmosphere of Mexico City[J]. Atmospheric Environment, 2015,119(OCT):415-429.
[13] Cai C J, Geng F H, Tie X X, et al. Characteristics and source apportionment of VOCs measured in Shanghai, China[J]. Atmospheric Environment, 2010,44(38):5005-5014.
[14] Louie K K, Ho W K, Tsang C W, et al. VOCs and OVOCs distribution and control policy implications in Pearl River Delta Region, China[J]. Atmospheric Environment, 2013,76(5):125-135.
[15] Zhang Z, Zhang Y L, Wang X M, et al. Spatiotemporal patterns and source implications of aromatic hydrocarbons at six rural sites across China's developed coastal regions[J]. Journal of Geophysical Research Atmospheres, 2016,121(11):6669-6687.
[16] Zhang Y L, Wang X M, Zhang Z, et al. Sources of C2-C4alkenes, the most important ozone nonmethane hydrocarbon precursors in the Pearl River Delta region[J]. Science of the Total Environment, 2015, 502(JAN):236-245.
[17] Wang M, Shao M, Chen W T, et al. A temporally and spatially resolved validation of emission inventories by measurements of ambient volatile organic compounds in Beijing, China[J]. Atmospheric Chemistry & Physics, 2014,14(12):5871-5891.
[18] Shan W P, Yin Y Q, Lu H X, et al. A meteorological analysis of ozone episodes using HYSPLIT model and surface data[J]. Atmospheric Research, 2009,93(4):767-776.
[19] Yue D L, Zhong L J, Zhang T, et al. Pollution properties of water-soluble secondary inorganic ions in atmospheric PM2.5 in the Pearl River Delta Region[J]. Aerosol & Air Quality Research, 2015,15(5):1737-1747.
[20] Wang M, Zeng L M, Lu S H, et al. Development and validation of a cryogen-free automatic gas chromatograph system (GC-MS/FID) for online measurements of volatile organic compounds[J]. Analytical Methods, 2014,6(23):9424-9434.
[21] Atkinson R, Baulch D L, Cox R A, et al. Evaluated kinetic and photo-chemical data for atmospheric chemistry:Supplement VIII, halogen species evaluation for atmospheric chemistry[J]. Journal of Physical and Chemical Reference Data, 2000,29(2):167-266.
[22] Atkinson R, Baulch D L, Cox R A, et al. Evaluated kinetic and photo-chemical data for atmospheric chemistry, organic species:Supplement VII[J]. Atmospheric Environment. part A. general Topics, 2010,26(7):1187-1230.
[23] Carter W P L. Development of ozone reactivity scales for volatile organic compounds[J]. Journal of Air and Waste Management Association, 1994,44(7):881-899.
[24] Grosjean D, Seinfeld J H. Parameterization of the formation potential of secondary organic aerosols[J]. Atmospheric Environment, 1989, 23(8):1733-1747.
[25] Grosjean D. In situ organic aerosol format ion during a smog episode estimated production and chemical functionality[J]. Atmospheric Environment, 1992,26(6):953-963.
[26] 王倩,陈长虹,王红丽,等.上海市秋季大气VOCs对二次有机气溶胶的生成贡献及来源研究[J]. 环境科学, 2013,34(2):424-433. Wang Q, Chen C H, Wang H L, et al. Forming Potential of Secondary Organic Aerosols and Sources Apportionment of VOCs in Autumn of Shanghai, China[J]. Environmental Science, 2013,34(2):424-433.
[27] 王扶潘,朱乔,冯凝,等.深圳大气中VOCs的二次有机气溶胶生成潜势[J]. 中国环境科学, 2014, 34(10):2449-2457. Wang F P, Zhu Q, Feng N, et al. The generation potential of secondary organic aerosol of atmospheric VOCs in Shenzhen[J]. China Environmental Science, 2014,34(10):2449-2457.
[28] 邓雪娇,王新明,赵春生,等.珠江三角洲典型过程VOCs的平均浓度与化学反应活性[J]. 中国环境科学, 2010,30(9):1153-1161. Deng X J, Wang X M, Zhao C S, et al. The mean concentration and chemical reactivity of VOCs of typical processes over Pearl River Delta Region[J]. China Environmental Science, 2010,30(9):1153-1161.
[29] 周炎,钟流举,岳玎利,等.典型污染时段鹤山大气VOCs的臭氧生成潜势及来源解析[J]. 环境监控与预警, 2014,6(4):1-16. Zhou Y, Zhong L J, Yue D L, et al. Potential ozone formation and emission sources of atmospheric VOCs in Heshan during typical pollution episode[J]. Environmental Monitoring and Forewarning, 2014,6(4):1-16.
[30] 虞小芳,程鹏,古颖纲,等.广州市夏季VOCs对臭氧及SOA生成潜势的研究[J]. 中国环境科学, 2018,38(3):830-837. Yu X F, Cheng P, Gu Y G, et al. Formation potential of ozone and secondary organic aerosol from VOCs oxidation in summer in Guangzhou, China[J]. China Environmental Science, 2018,38(3):830-837.

基金

国家重点研发计划(2018YFC0213903);国家自然科学基金资助项目(91743109);广州珠江科技新星专项(201506010079)

PDF(917 KB)

Accesses

Citation

Detail

段落导航
相关文章

/