Metastable O+ ions in Martian atmosphere

Authors

  • D. C. AGARWAL

DOI:

https://doi.org/10.54302/mausam.v21i3.5399

Abstract

. Production rates of atomic oxygen ions in the metastable states (2P and 2D) by photo-ionization have been calculated, Equilibrium distributions of these species have been calculated using recently measured rate-coefficients of ion-atom interchange and other ionic reactions.  Finally, the zenith intensity of the (7318.6- 733OA) multiple of O+in the dayglow has been calculated and found to be approximately in the range 4.5-8. OR.

 

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Published

01-07-1970

How to Cite

[1]
D. C. . AGARWAL, “Metastable O+ ions in Martian atmosphere”, MAUSAM, vol. 21, no. 3, pp. 391–397, Jul. 1970.

Issue

Vol. 21 No. 3 (1970): MAUSAM

Section

Research Papers

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