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Analytical Solution of Time Dependent Diffusion Equation in Stable Case

Received: 27 May 2018     Accepted: 8 June 2018     Published: 9 August 2018
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Abstract

The normalized integrated concentration of pollutant has been obtained after solving temporaly diffusion equation using the method of separation variable considering the eddy diffusivities which measuring at night or at any time in high inversion layer in the stable condition. The dataset is observed from the “Project prairie Grass” (Barad 1958) which is measured using wind speed at 1.5m and downwind distance during the experiment at 50, 200 and 800 m in stable case for runs from 1 to 10. Comparison between the estimated and observed normalized integrated concentration at a different downwind distance for all runs at t = 30 minutes is calculated.

Published in American Journal of Environmental Science and Engineering (Volume 2, Issue 2)
DOI 10.11648/j.ajese.20180202.12
Page(s) 32-36
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), 2018. Published by Science Publishing Group

Keywords

Project Prairie Grass, Laplace Transform, Normalized Concentration, Diffusion Equation, Stable Condition

References
[1] Akula Venkatram (2004): On estimating emissions through horizontal fluxes. Atmospheric Environment38, 1337-1344.
[2] Barad M. L. (Ed) (1958). Project prairie Grass, A field program in diffusion, vol. 1. Geophysics Research Paper no. 59, Geophysics Research Directorate, Air Force Cambridge Research Center.
[3] Doran J. C., and Horst T. W. (1985). ”An evaluation of Gaussian plume-depletion models with dual-tracer field measurement”. Atmos. Environ., 19, 939-951.
[4] Eckman, R. M., (1994). “Ro-examination of empirically derived formulas for horizontal diffusion from surface sources”. Atmospheric Environment: 28, 265-272.
[5] Hanna Steven R. Gary A. Briggs and Rayford P. hosker Jr. (1982). “Handbook on Atmospheric Diffusion”. Technical Information Center, U. S. Department of Energy.
[6] Hanna, S. R., 1989, “confidence limit for air quality models as estimated by bootstrap and Jacknife resembling methods”, Atom. Environ. 23, 1385-1395.
[7] Hazewinkel, Michiel, ed. (2001), “Delta-function”, Encyclopedia of Mathematics, Springer, ISBN 978-1-55608-010-4.
[8] John E. Till, Helen A. Grogan (2008). “Radiological risk assessment and environmental analysis”.
[9] Khaled S. M. Essa, Sawsan E. M. Elsaid and Fawzia Mubarak (2015).” Time dependent Advection-Diffusion Equation in Two Dimensions” Journal of Atmosphere, vol. 1, issue1, pages 8-16.
[10] Michael R. K. Thambynayagam, R. K. M (2011). The Diffusion Handbook: Applied Solutions for Engineers. McGraw-Hill.
[11] Palazzi, E., De Faveri, M., Fumarola, G., Ferraiolla, G., (1982), Diffusion from a steady source of short duration, Atmospheric Environment 16, 2785–2790.
[12] Panofsky, H. A., H. Tennekes, D. H. Lenschow, and J. C. Wyngaard, (1977).”The characteristics of turbulent velocity components in the surface layer under convective conditions, boundary layer meteorology. 11:355-361.
Cite This Article
  • APA Style

    Khaled Sadek Mohamed Essa, Sawsan Ibrahim Mohamed El Saied, Ayman Marrouf. (2018). Analytical Solution of Time Dependent Diffusion Equation in Stable Case. American Journal of Environmental Science and Engineering, 2(2), 32-36. https://doi.org/10.11648/j.ajese.20180202.12

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    ACS Style

    Khaled Sadek Mohamed Essa; Sawsan Ibrahim Mohamed El Saied; Ayman Marrouf. Analytical Solution of Time Dependent Diffusion Equation in Stable Case. Am. J. Environ. Sci. Eng. 2018, 2(2), 32-36. doi: 10.11648/j.ajese.20180202.12

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    AMA Style

    Khaled Sadek Mohamed Essa, Sawsan Ibrahim Mohamed El Saied, Ayman Marrouf. Analytical Solution of Time Dependent Diffusion Equation in Stable Case. Am J Environ Sci Eng. 2018;2(2):32-36. doi: 10.11648/j.ajese.20180202.12

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  • @article{10.11648/j.ajese.20180202.12,
      author = {Khaled Sadek Mohamed Essa and Sawsan Ibrahim Mohamed El Saied and Ayman Marrouf},
      title = {Analytical Solution of Time Dependent Diffusion Equation in Stable Case},
      journal = {American Journal of Environmental Science and Engineering},
      volume = {2},
      number = {2},
      pages = {32-36},
      doi = {10.11648/j.ajese.20180202.12},
      url = {https://doi.org/10.11648/j.ajese.20180202.12},
      eprint = {https://article.sciencepublishinggroup.com/pdf/10.11648.j.ajese.20180202.12},
      abstract = {The normalized integrated concentration of pollutant has been obtained after solving temporaly diffusion equation using the method of separation variable considering the eddy diffusivities which measuring at night or at any time in high inversion layer in the stable condition. The dataset is observed from the “Project prairie Grass” (Barad 1958) which is measured using wind speed at 1.5m and downwind distance during the experiment at 50, 200 and 800 m in stable case for runs from 1 to 10. Comparison between the estimated and observed normalized integrated concentration at a different downwind distance for all runs at t = 30 minutes is calculated.},
     year = {2018}
    }
    

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    T1  - Analytical Solution of Time Dependent Diffusion Equation in Stable Case
    AU  - Khaled Sadek Mohamed Essa
    AU  - Sawsan Ibrahim Mohamed El Saied
    AU  - Ayman Marrouf
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    T2  - American Journal of Environmental Science and Engineering
    JF  - American Journal of Environmental Science and Engineering
    JO  - American Journal of Environmental Science and Engineering
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    EP  - 36
    PB  - Science Publishing Group
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    UR  - https://doi.org/10.11648/j.ajese.20180202.12
    AB  - The normalized integrated concentration of pollutant has been obtained after solving temporaly diffusion equation using the method of separation variable considering the eddy diffusivities which measuring at night or at any time in high inversion layer in the stable condition. The dataset is observed from the “Project prairie Grass” (Barad 1958) which is measured using wind speed at 1.5m and downwind distance during the experiment at 50, 200 and 800 m in stable case for runs from 1 to 10. Comparison between the estimated and observed normalized integrated concentration at a different downwind distance for all runs at t = 30 minutes is calculated.
    VL  - 2
    IS  - 2
    ER  - 

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Author Information
  • Department of Mathematics and Theoretical Physics, NRC, Atomic Energy Authority, Cairo, Egypt

  • Department of Mathematics and Theoretical Physics, NRC, Atomic Energy Authority, Cairo, Egypt

  • Department of Mathematics and Theoretical Physics, NRC, Atomic Energy Authority, Cairo, Egypt

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