Browse > Article
http://dx.doi.org/10.5572/KOSAE.2011.27.2.201

Inter-comparison of Two Aethalometers for Aerosol Black Carbon Measurements  

Jung, Jung-Hoon (Department of Environmental Engineering, Chonnam National University)
Park, Seung-Shik (Department of Environmental Engineering, Chonnam National University)
Yoon, Kwan-Hoon (APM Engineering Co., Ltd.)
Cho, Sung-Yong (Department of Environmental Engineering, Chonnam National University)
Kim, Seung-Jai (Department of Environmental Engineering, Chonnam National University)
Publication Information
Journal of Korean Society for Atmospheric Environment / v.27, no.2, 2011 , pp. 201-208 More about this Journal
Abstract
Recently, a real-time, pocket-sized aethalometer (microAeth$^{(R)}$ model AE51) has been developed by Magee Scientific Inc. for measuring the concentration of black carbon in the atmosphere. In this study, two aethalometers, models AE-16 and AE-51, which measure the optical absorption of carbon particles at infrared 880 nm, were operated at time interval of 5-min between January 9 and February 10, 2010 at an urban site of Gwangju, to compare the accuracy of black carbon (BC) concentrations reported from the AE-51 model and to investigate reasonable sampling time of filter media in the AE-51. The air samples in the AE-51 and AE-16 models are collected on T60 (Teflon coated glass fiber) filter media (filter spot area: 0.07 $cm^2$) and quartz fiber roll-tape filter (filter spot area: 1.67 $cm^2$), respectively. Real-time measurement results indicate that when the filters were clean, the AE-51 BC was greater than or similar to the AE-16 BC data. However as the filter spots become darker, the AE-16 BC concentrations were higher than the AE-51 BC data and the difference in the BC concentrations from two AE models becomes gradually increased. Relative error in the AE-51 and AE-16 BC concentrations showed significance difference depending on used time of the filter in the AE-51 model, weather pattern, levels of air pollution, etc, ranging from 11.5% (used time of the filter in AE-51: 1,595 min) to 52.5% (used time of the filter in AE-51: 2,085 min). When considering the used time of one filter ticket in the AE-51 model and difference (or relative error %) between AE-16 and AE-51 BC concentrations, it is recommended that the standard sampling time per one filter ticket within the AE-51 model be less than approximately 24 hr (1,440 min) under the normal weather conditions except for severe haze and mist events.
Keywords
Aethalometer; Pocket-sized aethalomter; Black carbon; Particle shadowing effect;
Citations & Related Records
Times Cited By KSCI : 2  (Citation Analysis)
연도 인용수 순위
1 Virkkula, A., T. Makela, R. Hillamo, T. Yli-Tuomi, A. Hirsikko, K. Hameri, and I.K. Koponen (2007) A simple procedure for correcting loading effects of aethalometer data, Journal of the Air and Wastement Management Association, 57, 1214-1222.   DOI
2 Weingartner, E., H. Saathoff, M. Schnaiter, N. Streit, B. Bitnar, and U. Baltensperger (2003) Absorption of light by soot particles: determination of the absorption coefficient by means of aethalometers, Journal of Aerosol Science, 34, 1445-1463.   DOI   ScienceOn
3 Gebhart, K., S.M. Kreidenweis, and W.C. Malm (2001) Backtrajectory analyses of fine particulate matter measured at Big Bend National Park in the historical database and the 1996 scoping study, The Science of the Total Environment, 276, 185-204.   DOI   ScienceOn
4 Hansen, A., H. Rosen, and T. Novakov (1984) The Aethalometer-an instrument for the real-time measurement of optical absorption by aerosol particles, The Science of the Total Environment, 36, 191-196.   DOI   ScienceOn
5 Hansen, J., M. Sato, R. Ruedy, A. Lacis, and V. Oinas (2000) Global warming in the twenty-first century: An alternative scenario, Proceedings of The National Academy of Sciences of The United States of America, 97(18), 9875-9880.   DOI   ScienceOn
6 Jung, J.H. and S.S. Park (2010) Characteristics of black carbon in PM2.5 observed in Gwangju for year 2008 and examination of filter loading effect, J. Korean Soc. Atmos. Environ., 26(4), 392-402. (in Korean with English abstract).   DOI   ScienceOn
7 Maynard, D., B.A. Coull, A. Gryparis, and J. Schwartz (2007) Mortality risk associated with short-term exposure to traffic particles and sulfates, Environmental Health Perspectives, 115(5), 751-755.   DOI   ScienceOn
8 Park, S.S., J.H. Jung, S.Y. Cho, and S.J. Kim (2009) Compensation of aethalometer black carbon data observed at a Gwangju site, J. Korean Soc. Atmos. Environ., 25(6), 571-578. (in Korean with English abstract)   과학기술학회마을   DOI   ScienceOn
9 Menon, S., J. Hansen, L. Nazarenko, and Y.F. Luo (2002) Climate effects of black carbon aerosols in China and India, Science, 297(5590), 2250-2253.   DOI   ScienceOn
10 Myhre, G., A. Myhre, and F. Stordal (2001) Historical evolution of radiative forcing of climate, Atmospheric Environment, 35, 2361-2373.   DOI   ScienceOn
11 Crutzen, P. and M. Andreae (1990) Biomass burning in the tropics: impact on atmospheric chemistry and biogeochemical cycles, Science, 250, 1669-1678.   DOI   ScienceOn
12 Adams, K., L. Davis, S. Japar, and D. Finley (1990) Realtime, in-situ measurements of atmospheric optical absorption in the visible via photo-acoustic spectroscopy: IV. Visibility degradation and aerosol optical properties in Los Angeles, Atmospheric Environment, 24, 605-610.   DOI   ScienceOn