The prominent emission feature near λ2145 Å in the ultraviolet spectrum of an aurora has been tentatively identified by Dick [1978] as the doublet lines, λ2139.68 Å and λ2143.55 Å, emitted by metastable N+(5S) ions, and dissociative excitation of N2 by electron impact with a cross section ≥2 × 10−18 cm² has been proposed as the source of this species. A detailed laboratory study of dissociative excitation is described in this letter which suggests two alternative viewpoints of this process: (1) If the calculated radiative lifetime for the N+(5S) state [4.4 µsec] is correct, then the N+(5S) dissociative excitation cross section is <3 × 10−21 cm². Thus, a new N+(5S) source mechanism would have to be found in order to account for the auroral data. (2) If dissociative excitation does form N+(5S) ions efficiently, then the laboratory and field observations imply a radiative lifetime for this state >10 msec, thus suggesting that there are major errors in the lifetime computation.
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Erdman et al. (1980) studied this question.
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