Ionic composition of a humid air plasma under ionizing radiation
- Authors: Filippov A.V.1, Derbenev I.N.1,2, Dyatko N.A.1, Kurkin S.A.1,3, Lopantseva G.B.1, Pal’ A.F.1,4, Starostin A.N.1
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Affiliations:
- Troitsk Institute for Innovation and Fusion Research
- School of Chemistry
- Moscow Institute of Physics and Technology (State University)
- Skobel’tsyn Research Institute of Nuclear Physics
- Issue: Vol 125, No 2 (2017)
- Pages: 246-267
- Section: Atoms, Molecules, Optics
- URL: https://journals.rcsi.science/1063-7761/article/view/192444
- DOI: https://doi.org/10.1134/S1063776117070020
- ID: 192444
Cite item
Abstract
A kinetic model is proposed for ion–molecular processes involving charged particles of a humid air plasma produced by a fast electron beam. The model includes more than 600 processes involving electrons and 41 positive and 14 negative ions, including hydrated ions H3O+ (H2O)n and O2−(H2O)n with n = 1, 2, …, 12. The energy costs of production of electron–ion pairs and electronic and vibrational (for water molecules, also rotational) excitation of molecules are calculated in nitrogen, oxygen, water vapor, air, and humid air. A method is proposed for calculating the energy costs in mixtures by the calculation data in pure gases. The evolution of the plasma composition is studied by the numerical solution of a system of 56 time-dependent balance equations for the number of charged particles of plasma by the fourth-order Runge–Kutta method. The steady-state composition of plasma is determined by solving nonlinear steady-state balance equations for the ionization rates of humid air from 10 to 1016 cm–3/s and the fraction of water molecules from 10–3% to 1.5%. It is established that, for water vapor content (the ratio of the number density of water molecules to the total number density of air molecules) of 0.015–1.5% in air at atmospheric pressure and room temperature, the main ion species are two types of positive ions H3O+ (H2O)n with the number of water molecules n = 5, 6 and three species of negative ions O2−(H2O)n with n = 5, 8, 9.
About the authors
A. V. Filippov
Troitsk Institute for Innovation and Fusion Research
Author for correspondence.
Email: fav@triniti.ru
Russian Federation, Troitsk, Moscow, 108840
I. N. Derbenev
Troitsk Institute for Innovation and Fusion Research; School of Chemistry
Email: fav@triniti.ru
Russian Federation, Troitsk, Moscow, 108840; University Park, Nottingham NG&.2RD
N. A. Dyatko
Troitsk Institute for Innovation and Fusion Research
Email: fav@triniti.ru
Russian Federation, Troitsk, Moscow, 108840
S. A. Kurkin
Troitsk Institute for Innovation and Fusion Research; Moscow Institute of Physics and Technology (State University)
Email: fav@triniti.ru
Russian Federation, Troitsk, Moscow, 108840; Dolgoprudnyi, Moscow oblast, 141701
G. B. Lopantseva
Troitsk Institute for Innovation and Fusion Research
Email: fav@triniti.ru
Russian Federation, Troitsk, Moscow, 108840
A. F. Pal’
Troitsk Institute for Innovation and Fusion Research; Skobel’tsyn Research Institute of Nuclear Physics
Email: fav@triniti.ru
Russian Federation, Troitsk, Moscow, 108840; Moscow, 119991
A. N. Starostin
Troitsk Institute for Innovation and Fusion Research
Email: fav@triniti.ru
Russian Federation, Troitsk, Moscow, 108840
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