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
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. Only above this altitude does dissociation be- come important. If we use the pressure vs. Altitude results of reference 'i, we find thst x is about 90 Km. The graphs of n- and n are given in I'l/mre 1. We h^vp also superposed the graph of n^ as it would be if no dissocl. Ition took piece - the vrlues ere obtained from the ordinary "baro- metric equation.
_ 1 _ It l8 seen that in the present model dissociation occurs at higher altitudes (about 5 Km. Higher) than in the model of reference 2. Th...is result is a consequence of the use in this paper of a greater •«ilue for the effective two-hody reconhination cross-section Cn„. Hence in the present model the oxygen atoms can recombine more readily than in the model of reference 2 and only at higher altitudes are dissociations numerous enough to ensure number balance. Another striking difference between the present results and those of reference 2 is the broadness of the region in which dissociation takes place - about 25 Km. , as opposed to less than 15 Km.
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To quickly assess the difficulty of the text, read a short excerpt:
. Only above this altitude does dissociation be- come important. If we use the pressure vs. Altitude results of reference 'i, we find thst x is about 90 Km. The graphs of n- and n are given in I'l/mre 1. We h^vp also superposed the graph of n^ as it would be if no dissocl. Ition took piece - the vrlues ere obtained from the ordinary "baro- metric equation.
_ 1 _ It l8 seen that in the present model dissociation occurs at higher altitudes (about 5 Km. Higher) than in the model of reference 2. Th...is result is a consequence of the use in this paper of a greater •«ilue for the effective two-hody reconhination cross-section Cn„. Hence in the present model the oxygen atoms can recombine more readily than in the model of reference 2 and only at higher altitudes are dissociations numerous enough to ensure number balance. Another striking difference between the present results and those of reference 2 is the broadness of the region in which dissociation takes place - about 25 Km. , as opposed to less than 15 Km.
What to read after A Self Consistent Calculation of the Dissociation of Oxygen in the Upper Atmosph?
You can find similar books in the "Read Also" column, or choose other free books by Harry Elecks Moses to read onlineMoreLess
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