A Self Consistent Calculation of the Dissociation of Oxygen in the Upper Atmosph

Cover A Self Consistent Calculation of the Dissociation of Oxygen in the Upper Atmosph
A Self Consistent Calculation of the Dissociation of Oxygen in the Upper Atmosph
Harry E Moses
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It will be seen below that this is not true, at least with the cross sections used.
- 12 - V. Results of Numerical Calculations Three cases were calculated numerically. In all three cases ru at x=x was taken as 10 /cm . (If 2 is assumed to constitute l/5 of the atmosphere, x would correspond to 85 km. ) This choice is not special though it may seem so since n ? (x), nCx) depend only on the difference x-x . The three different cases correspond to different choices of the temperature function T =
... T +°

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