A Theoretical Model of Altitudinal Distribution of Sodium Atom

Details A Theoretical Model of Altitudinal Distribution of Sodium Atom A Theoretical Model of Altitudinal Distribution of Sodium Atom

Nov 1995

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1995em%26p...71..147j&link_type=abstract

Earth, Moon, and Planets, Volume 71, Issue 1-2, pp. 147-152

Physics

2

Scientific paper

It has been well accepted that sodium is a minor constituent in the upper atmosphere. The possible formation and destruction processes of sodium has been considered and the following results are obtained: (i) An empirical equation has been established for calculation of the concentration of sodium for different altitude and time. (ii) It is confirmed that the rate constant for the reaction NaO + O2 → Na + O3 is temperature dependent. The activation energy for this reaction is 70.88 Kcals/mole.

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