全部 标题 作者
关键词 摘要

OALib Journal期刊
ISSN: 2333-9721
费用:99美元

查看量下载量

相关文章

更多...

Atmospheric Volatile Organic Compounds and Ozone Creation Potential in an Urban Center of Southern Nigeria

DOI: 10.1155/2014/764948

Full-Text   Cite this paper   Add to My Lib

Abstract:

The relative contribution of individual volatile organic compounds (VOC) species to photochemical ozone formation depends on their atmospheric concentrations and their oxidation mechanism. In an attempt to evaluate the ozone creation potential of ambient VOCs captured in an urban settlement of Benin City, Nigeria, the VOCs concentrations data collected in field studies at nine measurement sites of different air quality in the city and a background site were analysed. Air samples were collected at human breathing height of 1.5 meters from ground level at each site. Active sampling method using the low volume sampling pump (Acuro, Drager, Lubeck, Germany) was used to drawn the air into the tube; the absorbent was Chromosorb 106. The sampling periods were between May 2010 and June 2011; the period covered both dry and wet seasons. The adsorbed gases were desorbed using solvent extraction method with carbon disulphide as solvent. The extracted solutions were analyzed with gas chromatography and mass spectrometer. The observed concentrations of individual VOCs were determined and maximum incremental reactivity (MIR) coefficient along with rate constants of VOC-OH reactions were applied to assess the ozone formation potential of individual VOC in the ambient atmosphere. Sixteen VOC species were observed at various sites with mixing height in decreasing order: toluene (5.82), mp-xylene (3.58), ethylbenzene (3.46), benzene (2.29), and n-butane (0.84). The ozone formation potential study revealed that, ranking by propyl-equivalent, the alkanes included in this study account for 58% of the total propyl-equivalent concentration. The total ozone creation potential in the atmosphere of the Benin City was calculated to be 281.1?μg/m3. A comparison of total ozone formation potential (OFP) in our study with results obtained from other cities of the world revealed that the total concentration of ozone production in our study is threefold lower than the values reported in China city of Foshan. It is suggested that the sources of this pollutant need to be monitored in the area as a way of curtailing the impact of ozone in this city. 1. Introduction Monitoring of volatile organic compounds (VOCs) is a key piece in understanding photochemical air quality in urban atmosphere. VOCs degradation in the atmosphere contributes significantly to the generation of secondary air pollutants, such as aldehydes and peroxyacetyl nitrate (PAN) secondary aerosol [1]. Anthropogenic sources such as incomplete combustion of organic substances, the use of petrochemical solvents, and

References

[1]  A. Srivastava, A. E. Joseph, A. More, and S. Patil, “Emissions of VOCs at urban petrol retail distribution centres in India (Delhi and Mumbai),” Environmental Monitoring and Assessment, vol. 109, no. 1–3, pp. 227–242, 2005.
[2]  S. Sillman, “The use of NOX, H2O2, and HNO3 as indicators for ozone-NOx- hydrocarbon sensitivity in urban locations,” Journal of Geophysical Research, vol. 100, no. 7, pp. 14175–14188, 1995.
[3]  S. C. Lee, M. Y. Chiu, K. F. Ho, S. C. Zou, and X. Wang, “Volatile organic compounds (VOCs) in urban atmosphere of Hong Kong,” Chemosphere, vol. 48, no. 3, pp. 375–382, 2002.
[4]  B. Barletta, S. Meinordi, S. F. Rowland, et al., “VOCs in 43 Chinese Cities,” Atmospheric Environment, vol. 39, pp. 5979–5990, 2005.
[5]  A. Srivastava, “Source apportionment of ambient VOCS in Mumbai city,” Atmospheric Environment, vol. 38, no. 39, pp. 6829–6843, 2004.
[6]  K. Na, Y. P. Kim, K.-C. Moon, I. Moon, and K. Fung, “Concentrations of volatile organic compounds in an industrial area of Korea,” Atmospheric Environment, vol. 35, no. 15, pp. 2747–2756, 2001.
[7]  K. Na, Y. P. Kim, and K. C. Moon, “Diurnal characteristics of volatile organic compounds in the Seoul atmosphere,” Atmospheric Environment, vol. 37, no. 6, pp. 733–742, 2003.
[8]  C. Chang, U. Sree, Y. Lin, and J. Lo, “An examination of 7:00–9:00 PM ambient air volatile organics in different seasons of Kaohsiung city, southern Taiwan,” Atmospheric Environment, vol. 39, no. 5, pp. 867–884, 2005.
[9]  H. Cheng, H. Guo, X. Wang et al., “On the relationship between ozone and its precursors in the Pearl River Delta: application of an observation-based model (OBM),” Environmental Science and Pollution Research, vol. 17, no. 3, pp. 547–560, 2010.
[10]  S. Saito, I. Nagao, and H. Kanzawa, “Characteristics of ambient C2-C11 non-methane hydrocarbons in metropolitan Nagoya, Japan,” Atmospheric Environment, vol. 43, no. 29, pp. 4384–4395, 2009.
[11]  R. Atkinson, Kinetics and Mechanisms of the Gasphase Reactions of the Hydroxyl Radical with Organic Compounds, American Institute of Physics, New York, NY, USA, 1989.
[12]  W. P. L. Carter, “Development of ozone reactivity scales for volatile organic compounds,” Journal of the Air and Waste Management Association, vol. 44, no. 7, pp. 881–899, 1994.
[13]  D. R. Blake, D. F. Hurst, J. T. W. Smith et al., “Summertime measurements of selected nonmethane hydrocarbons in the Arctic and Subarctic during the 1988 Arctic Boundary Layer Expedition (ABLE 3A),” Journal of Geophysical Research: Atmospheres, vol. 97, no. 15, pp. 16559–16588, 1992.
[14]  Y. H. Zhang, H. Su, L. J. Zhong et al., “Regional ozone pollution and observation-based approach for analyzing ozone-precursor relationship during the PRIDE-PRD2004 campaign,” Atmospheric Environment, vol. 42, no. 25, pp. 6203–6218, 2008.
[15]  M. Wang, H. Cheng, G. Ding et al., “Study on the composition of NMHCs and the variation of concentration at Linan and Shangdianzi atmospheric background station,” Acta Meteorologica Sinica, vol. 64, pp. 658–665, 2006.
[16]  M. Wang, H. Cheng, G. Ding, et al., “The primary study of measured result of ambient VOCs in Beijing areas,” Journal of Applied Meteorological Science, vol. 16, no. 5, pp. 600–607, 2005.
[17]  J. H. Tang, L. Y. Chan, C. Y. Chan et al., “Characteristics and diurnal variations of NMHCs at urban, suburban, and rural sites in the Pearl River Delta and a remote site in South China,” Atmospheric Environment, vol. 41, no. 38, pp. 8620–8632, 2007.
[18]  M. Shao, Y. Zhang, L. Zeng et al., “Ground-level ozone in the Pearl River Delta and the roles of VOC and NOx in its production,” Journal of Environmental Management, vol. 90, no. 1, pp. 512–518, 2009.
[19]  E. G. Olumayede and J. M. Okuo, “Ambient air pollution and assessment of ozone creation potential for reactive Volatile Organic Compounds in atmosphere of Southwestern, Nigeria,” Nigeria African Journal of Environmental Science and Technology, vol. 7, no. 8, pp. 815–823, 2013.
[20]  E. G. Olumayede and J. M. Okuo, “Variation characteristics of volatile organic compounds in an urban atmosphere in Nigeria,” Polish Journal of Environmental Studies, vol. 21, no. 1, pp. 177–186, 2012.
[21]  E. G. Olumayede and J. M. Okuo, “Baseline levels of volatile organic compounds in atmosphere of two Urban Centres of Southwestern, Nigeria Intern,” Journal of Chemical Science, vol. 4, no. 1, pp. 42–55, 2011.
[22]  J. M. Okuo, C. C. Ojiodu, and E. G. Olumayede, “Ambient air pollution by Volatile Organic Compounds (VOCs) in Ikeja industrial areas of Lagos State, Southwestern Nigeria,” Nigerian Journal of Applied Science, vol. 30, pp. 138–149, 2012.
[23]  NMA, “Nigerian Meteorological Agency,” Weather Report Bulletin, 2009.
[24]  ASTM, “Method D3686-84: standard practice for sampling atmospheres to collect organic compound vapours,” in Annual Book of ASTM Standards, vol. 11, 03, pp. 234–240, 1988.
[25]  “National Population Commission (NPC) Nigeria 2006 census Final Results,” Official Gazette, Federal Republic of Nigeria, vol. 96, no. 2, 2009.
[26]  P. A. O. Odjugo, “Regional evidence of climate change in Nigeria,” Journal of Geography and Regional Planning, vol. 3, no. 6, pp. 142–150, 2010.
[27]  W. L. Chameides, F. Fehsenfeld, M. O. Rodgers, et al., “Ozone precursor relationships in the ambient atmosphere,” Journal of Geophysical Research, vol. 97, no. 5, pp. 6037–6055, 1992.
[28]  E. A. Woolforenden, “Use of diffusive sampler with thermal desorption- capillary GC analysis for monitoring volatile organic compounds in ambient air. Summary of reported data and practices,” Technical Support Document, Mark International, Bradford, UK.
[29]  H. U. Pferffer, L. Brever, and K. Ellermann, “Validation of hydrocarbon diffusive tubes for ambient air monitoring,” LUA Report 46, 1998.
[30]  W. P. L. Carter and R. Atkinson, “Computer modeling study of incremental hydrocarbon reactivity,” Environmental Science & Technology, vol. 23, no. 7, pp. 864–880, 1989.
[31]  E. E. Ukpebor, J. E. Ukpebor, F. Eromomene, J. I. Odiase, and D. Okoro, “Spatial and diurnal variations of Carbon monoxide (CO) pollution from motor vehicles in an Urban centre,” Polish Journal of Environmental Studies, vol. 19, no. 4, pp. 817–823, 2010.
[32]  J. H. Seinfeld and S. N. Pandis, Atmospheric Chemistry and Physics: From Air Pollution to Climate Change, Wiley, New York, NY, USA, 1998.
[33]  J. H. Tan, S. J. Guo, Y. L. Ma et al., “Non-methane hydrocarbons and their Ozone formation potentials in Foshan,” Aerosol and Air Quality Research, vol. 12, pp. 387–398, 2012.
[34]  H. Guo, K. L. So, I. J. Simpson, B. Barletta, S. Meinardi, and D. R. Blake, “C1-C8 volatile organic compounds in the atmosphere of Hong Kong: overview of atmospheric processing and source apportionment,” Atmospheric Environment, vol. 41, no. 7, pp. 1456–1472, 2007.
[35]  H. Singh and P. B. BZimmermon, Wiley Services on Advance in Environment Science and Technology, vol. 24, 1992, edited by O. Nriagu.

Full-Text

Contact Us

service@oalib.com

QQ:3279437679

WhatsApp +8615387084133