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Effect of Ambipolar Diffusion on the Flow of a Two-Component Plasma Gas Model in the Earth’s Planetary Ionosphere

Received: 23 December 2016    Accepted: 5 January 2017    Published: 22 August 2017
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Abstract

The paper presents analytical study on the effect of ambipolar diffusion on the flow of a two-component plasma gas in the Earth’s Planetary Ionosphere as a model to examine the ions-neutral and electrons-neutral atom interactions. The problem which consists of a set of partial non-linear differential equations was addressed using a plane wave and perturbation method of solutions. The result indicates that plasma frequency and electron-density in the Ionosphere increase with increase in magnetic field strength as well as with radiation and free convection parameters. It is observed that for; the plasma interactive state becomes more stable, otherwise some bit of oscillation is noticed. The stability is seen to depend on the magnetic (M2) and thermal convection (Gr) parameters. Under this condition the signal propagation becomes less diffuse when the frequency of the signal is far greater than the plasma frequency, that is, ω >> p. The study aids our understanding of the effect of coupling frequency on the propagation of satellite signals through the ionosphere.

Published in International Journal of Astrophysics and Space Science (Volume 5, Issue 3)
DOI 10.11648/j.ijass.20170503.12
Page(s) 47-54
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), 2024. Published by Science Publishing Group

Keywords

Ambipolar Diffusion, Two-Component Plasma Flow, Planetary Ionosphere

References
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Cite This Article
  • APA Style

    B. S. Tuduo, T. M. Abbey. (2017). Effect of Ambipolar Diffusion on the Flow of a Two-Component Plasma Gas Model in the Earth’s Planetary Ionosphere. International Journal of Astrophysics and Space Science, 5(3), 47-54. https://doi.org/10.11648/j.ijass.20170503.12

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    ACS Style

    B. S. Tuduo; T. M. Abbey. Effect of Ambipolar Diffusion on the Flow of a Two-Component Plasma Gas Model in the Earth’s Planetary Ionosphere. Int. J. Astrophys. Space Sci. 2017, 5(3), 47-54. doi: 10.11648/j.ijass.20170503.12

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    AMA Style

    B. S. Tuduo, T. M. Abbey. Effect of Ambipolar Diffusion on the Flow of a Two-Component Plasma Gas Model in the Earth’s Planetary Ionosphere. Int J Astrophys Space Sci. 2017;5(3):47-54. doi: 10.11648/j.ijass.20170503.12

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  • @article{10.11648/j.ijass.20170503.12,
      author = {B. S. Tuduo and T. M. Abbey},
      title = {Effect of Ambipolar Diffusion on the Flow of a Two-Component Plasma Gas Model in the Earth’s Planetary Ionosphere},
      journal = {International Journal of Astrophysics and Space Science},
      volume = {5},
      number = {3},
      pages = {47-54},
      doi = {10.11648/j.ijass.20170503.12},
      url = {https://doi.org/10.11648/j.ijass.20170503.12},
      eprint = {https://article.sciencepublishinggroup.com/pdf/10.11648.j.ijass.20170503.12},
      abstract = {The paper presents analytical study on the effect of ambipolar diffusion on the flow of a two-component plasma gas in the Earth’s Planetary Ionosphere as a model to examine the ions-neutral and electrons-neutral atom interactions. The problem which consists of a set of partial non-linear differential equations was addressed using a plane wave and perturbation method of solutions. The result indicates that plasma frequency and electron-density in the Ionosphere increase with increase in magnetic field strength as well as with radiation and free convection parameters. It is observed that for;  the plasma interactive state becomes more stable, otherwise some bit of oscillation is noticed. The stability is seen to depend on the magnetic (M2) and thermal convection (Gr) parameters. Under this condition the signal propagation becomes less diffuse when the frequency of the signal is far greater than the plasma frequency, that is, ω >> p. The study aids our understanding of the effect of coupling frequency on the propagation of satellite signals through the ionosphere.},
     year = {2017}
    }
    

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  • TY  - JOUR
    T1  - Effect of Ambipolar Diffusion on the Flow of a Two-Component Plasma Gas Model in the Earth’s Planetary Ionosphere
    AU  - B. S. Tuduo
    AU  - T. M. Abbey
    Y1  - 2017/08/22
    PY  - 2017
    N1  - https://doi.org/10.11648/j.ijass.20170503.12
    DO  - 10.11648/j.ijass.20170503.12
    T2  - International Journal of Astrophysics and Space Science
    JF  - International Journal of Astrophysics and Space Science
    JO  - International Journal of Astrophysics and Space Science
    SP  - 47
    EP  - 54
    PB  - Science Publishing Group
    SN  - 2376-7022
    UR  - https://doi.org/10.11648/j.ijass.20170503.12
    AB  - The paper presents analytical study on the effect of ambipolar diffusion on the flow of a two-component plasma gas in the Earth’s Planetary Ionosphere as a model to examine the ions-neutral and electrons-neutral atom interactions. The problem which consists of a set of partial non-linear differential equations was addressed using a plane wave and perturbation method of solutions. The result indicates that plasma frequency and electron-density in the Ionosphere increase with increase in magnetic field strength as well as with radiation and free convection parameters. It is observed that for;  the plasma interactive state becomes more stable, otherwise some bit of oscillation is noticed. The stability is seen to depend on the magnetic (M2) and thermal convection (Gr) parameters. Under this condition the signal propagation becomes less diffuse when the frequency of the signal is far greater than the plasma frequency, that is, ω >> p. The study aids our understanding of the effect of coupling frequency on the propagation of satellite signals through the ionosphere.
    VL  - 5
    IS  - 3
    ER  - 

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Author Information
  • Applied Mathematics and Theoretical Physics Group, Department of Physics, University of Port Harcourt, Port Harcourt, Nigeria

  • Applied Mathematics and Theoretical Physics Group, Department of Physics, University of Port Harcourt, Port Harcourt, Nigeria

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