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Study on Black Carbon and Its Characterisation at an Urban Location, Hyderabad during 2010 to 2012

Received: 1 April 2014     Accepted: 18 April 2014     Published: 30 April 2014
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Abstract

A seven channel Aethalometer (AE31) was used to measure the black carbon (BC) mass concentrations at the premises of National Remote Sensing Centre (NRSC), Hyderabad during the period 2010-2012 to characterize BC temporal concentration and source identification. Diurnal variation of BC shows varied amplitude of BC mass concentration with peak during mornings and nights with minimum during afternoons of all the study periods (2010-2012). Highest absorption coefficient at 520 nm (babs = 38.79 Mm-1) was observed during post monsoon season of 2011 and lowest value observed (babs = 22.06 Mm-1) during winter season of 2010. Absorption Angstrom Exponents (AAE) were analysed in the lower (370 nm-520 nm) and higher wavelength (590 nm-950 nm) region to explain the BC origin. A few number of days with high contrasting AAE in lower and higher wavelengths, responsible for the bio fuel generated BC were found during the study period. Study revealed that majority of the study period, AAE values are around 1, attributed to mainly vehicular emission. Highest AAE of 1.57 (370 nm-950 nm) was observed on 4 January, 2012. Three representative days of pre-monsoon, post-monsoon and winter were considered for analyzing daily variations of AAE in conjunction with back trajectories from NOAA HYSPLIT model to confirm the source of BC as biomass burning origin.

Published in International Journal of Environmental Monitoring and Analysis (Volume 2, Issue 2)
DOI 10.11648/j.ijema.20140202.16
Page(s) 100-105
Creative Commons

This is an Open Access article, distributed under the terms of the Creative Commons Attribution 4.0 International License (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution and reproduction in any medium or format, provided the original work is properly cited.

Copyright

Copyright © The Author(s), 2014. Published by Science Publishing Group

Keywords

BC, Absorption Coefficient, AAE

References
[1] T.C. Bond, D.G. Streets , K.F. Yarber, S.M. Nelson., J.H. Woo, Z. Klimont, “A technology-based global inventory of black and organic carbon emissions from combustion,” J.Geophys. Res., 2004, 109, D14203, 2004.
[2] K.H. Kim, K. Sekiguchi, S. Kudo, and K. Sakamoto, “ Characte-risitics of Atmospheric Elemental Carbon (Char and Soot) in Ultrafine and Fine Particles in a Roadside Environ-mental, Japan,” Aerosol Air Qual. Res. 11: 1–12, 2011.
[3] J. Hansen, Mki. Sato, R. Ruedy, A. Lacis, and V. Oinas, “Global warming in the twenty-first cen-tury: An alternative scenario,” Proc. Natl. Acad. Sci., 97, 9875-9880, doi:10.1073/pnas.170278997, 2000.
[4] S. A. Twomey, M. Piepgrass, and T.L. Wolfe, “An assessment of the impact of pollution on global cloud albedo,” Tellus B. 36, 356–366, 1984.
[5] T.C. Bond, S.J. Doherty, D.W. Fahey, P.M. Forster, T. Berntsen, B.J. DeAngelo, M.G. Flanner, S. Ghan, B. Kärcher, D. Koch, S. Kinne, Y. Kondo, P. K. Quinn, M. C. Sarofim, M. G. Schultz, M. Schulz, C. Venkataraman, H. Zhang, S. Zhang, N. Bellouin, S. K. Guttikunda, P. K. Hopke, M. Z. Jacobson, J. W. Kaiser, Z. Klimont, U. Lohmann, J. P. Schwarz, D. Shindell, T. Storelvmo, S. G. Warren, C. S. Zender ,” Bounding the role of black carbon in the climate system: A scientific assessment,” J. Geophys. Res .DOI:10.1002/jgrd.50171, 2013.
[6] S. Menon, J.E. Hansen, L. Nazarenko, and Y. Luo, “Climate Effects of Black Carbon Aerosols in China and India,” Science 297: 2250–2253, 2002.
[7] C. Wang, “A modeling study on the climate impacts of black carbon aerosols,” J. Geophys. Res. 109, DO3 106. doi:10.1029/2003JD004084, 2004.
[8] V. Ramanathan, and G. Carmichael “Global and regional climate changes due to black carbon,” Nature Geosci., 1, 221–227, 2008.
[9] M.Z. Jacobson, “Short-term effects of controlling fossil-fuel soot, biofuel soot and gases, and methane on climate, arctic ice, and air pollution health,” J. Geophys. Res., 115, D14209, doi:10.1029/2009JD013795,2010.
[10] J.M. Lobert, and J. Warnatz, “Emission from the combustion process in vegetation,” Fire in the Environment: The Ecological, Atmospheric, and Climatic Importance of Vegetation Fires, edited by P.J. Crutzen and J.G. Glodhammer, pp.15-37, John Wiley, New York,1993.
[11] K.V.S. Badarinath, S.K. Kharol, A.R. Sharma, and V. Krishna Prasad, “Analysis of aerosol and carbon monoxide characteristics over Arabian Sea during crop residue burning period in the Indo-Gangetic Plains using multi-satellite remote sensing datasets,” J. Atmos. Solar-Terr. Phys., 71, 1267–1276, 2009a.
[12] K.V.S. Badarinath, S.K. Kharol, and A.R. Sharma, “Long-rangetransport of aerosols from agriculture crop residue burning inIndo-Gangetic Plains – A study using LIDAR, ground measurements and satellite data,” J. Atmos. Solar-Terr. Phys., 71, 112–120, 2009b.
[13] C. Venkataraman, G. Habib, A. Eiguren-Fernandez, A.H. Miguel, and S.K. Friedlander, “Residential biofuels in South Asia, Carbonaceous aerosol emissions and climate impacts,” Science, 307, 1454–1456, 2005.
[14] D. Ganguly, A. Jayaraman, T.A. Rajesh, and H. Gadhavi, “Wintertime aerosol properties during foggy and nonfoggy days over urban center Delhi and their im-plications for shortwave radiative forcing,” J. Geophys. Res., 111, D15217, doi: 10.1029/2005JD007029, 2006.
[15] K.M. Latha, and K.V.S. Badarinath, “Sea-sonal variations of black carbon aerosols and total aero-sol mass concentrations over urban environment in India,” Atmos. Environ., 39, 4129–4141, 2005.
[16] S.S. Babu, and K.K. Moorthy, “Aerosol black carbon over tropical coastal station in India,” Geophys. Res. Lett., 29, 2098, doi:10.1029/2002GL015662. 2002.
[17] Bergstrom, R. W., Russell, P. B., & Hignett, P. (2002). Wavelength dependence of the absorption of black carbon particles: Predictions and results from the TARFOX experiment and implications for the aerosol single scattering albedo. Journal of the Atmospheric Sciences, 59(3).
[18] Kirchstetter, T. W., Novakov, T., & Hobbs, P. V. (2004).Evidence that the spectral dependence of light absorption by aerosols is affected by organic carbon. Journal of Geophysical Research: Atmospheres (1984–2012), 109(D21).
[19] Bond, T. C., & Bergstrom, R. W. (2006). Light absorption by car-bonaceous particles: An investigative review. Aerosol Science and Technology, 40(1), 27-67.
[20] Smith, D. M., Keifer, J. R., Novicky, M., & Chughtai, A. R. (1989). An FT-IR Study of the Effect of Simulated Solar Radiation and Various Particulates on the Oxidation of SO< sub> 2. Applied spectroscopy, 43(1), 103-107.
[21] Kirchner, U., Scheer, V., & Vogt, R. (2000). FTIR spectroscopic investigation of the mechan-ism and kinetics of the heterogeneous reactions of NO2 and HNO3 with soot. The Journal of Physical Chemistry A, 104(39), 8908-8915.
[22] Fuller, K. A., Malm, W. C., & Kreidenweis, S. M. (1999). Effects of mixing on extinction by carbonaceous particles. Journal of Geophysical Research: Atmospheres (1984–2012), 104(D13), 15941-15954.
[23] A.D. A. Hansen, H. Rosen, and T. Novakov, “The Aethalometer: An instrument for the real-time measurements of optical absorption by aerosol particles,” Sci. Total Environ., 36, 191–196, 1984.
[24] Weingartner, E, H. Saathoff, M. Schnaiter, N. Streit, B. Bitnar, U. Baltensperger, Absorption of Light by Soot Particles: Determination of the Absorption Coefficient by Means of Aethalometer;” J. Aerosol Sci., 34, 1445-1463, 2003.
[25] K.K. Moorthy, S.S. Babu, S.K. Satheesh, “Temporal heterogeneity in aerosol characteristics and the resulting radiative impact at a trpical coastal station-Part 1: Microphysical and optical properties,” Ann. Geophys., 25, 2293-2308, 2007.
[26] L. Giglio, J. Descloitres, C.O. Justice, Y.J. Kaufman, “An enhanced contextual fire detection algorithm for MODIS,” Remote Sensing of Environment , 87 273-282, 2003.
[27] R.B. Stull, R. B. “An Introduction to Boundary Layer Meteorology,” Springer, New York, 1998.
[28] P. Yan,” Study on the Aerosol Optical Properties in the Background Regions in the East Part of China (in Chinese with English Abstract),” Ph. D. Thesis, Peking University, 2006.
[29] X.L. Pan, X.L. “Observation Study of Atmospheric Aerosol Scattering Characteristics as a Function of Relative Humidity (in Chinese with English Abstract),” Ph. D. Thesis, Chin. Acad. of Meteorol. Sci., Bejing, 2007.
[30] R.W. Bergstrom, P. Pilewskie, P.B. Russell, J. Redemann, T.C. Bond, P.K. Quinn, and B. Sierau, “Spectral absorption properties of atmospheric aerosols,” Atmos. Chem. Phys., 7, 5937–5943, doi:10.5194/acp-7-5937-2007, 2007.
[31] P. S. Praveen, T. Ahmed, A. Kar, I. H. Rehman, and V. Ramanathan, “Link between local scale BC emissions in the Indo-Gangetic Plains and large scale atmospheric solar absorption,” Atmos. Chem. Phys., 12, 1173–1187, 2012.
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    Subin Jose, Biswadip Gharai. (2014). Study on Black Carbon and Its Characterisation at an Urban Location, Hyderabad during 2010 to 2012. International Journal of Environmental Monitoring and Analysis, 2(2), 100-105. https://doi.org/10.11648/j.ijema.20140202.16

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    Subin Jose; Biswadip Gharai. Study on Black Carbon and Its Characterisation at an Urban Location, Hyderabad during 2010 to 2012. Int. J. Environ. Monit. Anal. 2014, 2(2), 100-105. doi: 10.11648/j.ijema.20140202.16

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    AMA Style

    Subin Jose, Biswadip Gharai. Study on Black Carbon and Its Characterisation at an Urban Location, Hyderabad during 2010 to 2012. Int J Environ Monit Anal. 2014;2(2):100-105. doi: 10.11648/j.ijema.20140202.16

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  • @article{10.11648/j.ijema.20140202.16,
      author = {Subin Jose and Biswadip Gharai},
      title = {Study on Black Carbon and Its Characterisation at an Urban Location, Hyderabad during 2010 to 2012},
      journal = {International Journal of Environmental Monitoring and Analysis},
      volume = {2},
      number = {2},
      pages = {100-105},
      doi = {10.11648/j.ijema.20140202.16},
      url = {https://doi.org/10.11648/j.ijema.20140202.16},
      eprint = {https://article.sciencepublishinggroup.com/pdf/10.11648.j.ijema.20140202.16},
      abstract = {A seven channel Aethalometer (AE31) was used to measure the black carbon (BC) mass concentrations at the premises of National Remote Sensing Centre (NRSC), Hyderabad during the period 2010-2012 to characterize BC temporal concentration and source identification. Diurnal variation of BC shows varied amplitude of BC mass concentration with peak during mornings and nights with minimum during afternoons of all the study periods (2010-2012). Highest absorption coefficient at 520 nm (babs = 38.79 Mm-1) was observed during post monsoon season of 2011 and lowest value observed (babs = 22.06 Mm-1) during winter season of 2010. Absorption Angstrom Exponents (AAE) were analysed in the lower (370 nm-520 nm) and higher wavelength (590 nm-950 nm) region to explain the BC origin. A few number of days with high contrasting AAE in lower and higher wavelengths, responsible for the bio fuel generated BC were found during the study period. Study revealed that majority of the study period, AAE values are around 1, attributed to mainly vehicular emission. Highest AAE of 1.57 (370 nm-950 nm) was observed on 4 January, 2012. Three representative days of pre-monsoon, post-monsoon and winter were considered for analyzing daily variations of AAE in conjunction with back trajectories from NOAA HYSPLIT model to confirm the source of BC as biomass burning origin.},
     year = {2014}
    }
    

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    AU  - Subin Jose
    AU  - Biswadip Gharai
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    T2  - International Journal of Environmental Monitoring and Analysis
    JF  - International Journal of Environmental Monitoring and Analysis
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    UR  - https://doi.org/10.11648/j.ijema.20140202.16
    AB  - A seven channel Aethalometer (AE31) was used to measure the black carbon (BC) mass concentrations at the premises of National Remote Sensing Centre (NRSC), Hyderabad during the period 2010-2012 to characterize BC temporal concentration and source identification. Diurnal variation of BC shows varied amplitude of BC mass concentration with peak during mornings and nights with minimum during afternoons of all the study periods (2010-2012). Highest absorption coefficient at 520 nm (babs = 38.79 Mm-1) was observed during post monsoon season of 2011 and lowest value observed (babs = 22.06 Mm-1) during winter season of 2010. Absorption Angstrom Exponents (AAE) were analysed in the lower (370 nm-520 nm) and higher wavelength (590 nm-950 nm) region to explain the BC origin. A few number of days with high contrasting AAE in lower and higher wavelengths, responsible for the bio fuel generated BC were found during the study period. Study revealed that majority of the study period, AAE values are around 1, attributed to mainly vehicular emission. Highest AAE of 1.57 (370 nm-950 nm) was observed on 4 January, 2012. Three representative days of pre-monsoon, post-monsoon and winter were considered for analyzing daily variations of AAE in conjunction with back trajectories from NOAA HYSPLIT model to confirm the source of BC as biomass burning origin.
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Author Information
  • Atmospheric & Climate Sciences Group, ECSA, NRSC, Dept. of Space-Govt. of India, Balanagar, Hyderabad, India

  • Atmospheric & Climate Sciences Group, ECSA, NRSC, Dept. of Space-Govt. of India, Balanagar, Hyderabad, India

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