Electron production through the associative detachment reaction of nitrogen molecules with the negative ion of atomic oxygen revisited in the context of initiation of sprite streamers
Abstract
Although molecular oxygen, O2, is an attaching gas, current growth measurements in air demonstrate negligible electron attachment [e.g., Moruzzi and Price, J. Phys. D: Appl. Phys., 7, 1434, 1974]. This observation is interpreted in terms of an electron detachment mechanism involving O- ions and excited molecular nitrogen, N2, since detachment of electrons from O- ions by collision with unexcited O2 and N2 molecules practically does not occur at low gas temperatures [e.g., Fehsenfeld et al., J. Chem. Phys., 45, 1844, 1966; Moruzzi et al., J. Chem. Phys., 48(7), 3070, 1968; Kossyi et al., PSST, 1, 207, 1992]. It has been demonstrated that for the associative detachment reaction to proceed, N2 must be excited to at least the first vibrational level [Hopper et al., J. Chem. Phys., 65, 5474, 1976]. Contrary to studies above and based on a unique flow-drift tube setup, Rayment et al. [Int. J. Mass Spectrom. Ion Phys., 26, 321, 1978] argued that ground state N2 is in fact responsible for the associative detachment reaction. We note that Doussot et al. [J. Phys. D: Appl. Phys., 15, 2451, 1982] also arrive at the same conclusion with rates in qualitative agreement with those presented in [Rayment et al., 1978], though the O2/N2 ratio is significantly different in the two works. Also, it is not obvious how excited species are identified or removed from the drift region to limit the study to O- reacting with ground state N2. Here, we review the unique flow-drift tube setup in [Rayment et al., 1978] as it's the only work which provides values for the detachment rate coefficient in a considerable range of reduced electric fields, and is the basis of recent studies devoted to initiation of sprite streamers [e.g., Luque et al., Nat. Geosci., 5, 22, 2012]. In particular, we (i) demonstrate that excited N2 species in fact do contaminate the experimental setup of [Rayment et al., 1978], (ii) model the experimental setup of [Rayment et al., 1978] using a Green's function method and provide corrections to the approach outlined in that work, and (iii) underscore that reaction rates in majority of flow-drift tube setups mentioned above are obtained under steady state conditions which are not reflective of the transient nature of gas discharge dynamics [e.g., da Silva and Pasko, JGR, 118, 13561, 2013].
- Publication:
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AGU Fall Meeting Abstracts
- Pub Date:
- December 2020
- Bibcode:
- 2020AGUFMAE0120005J
- Keywords:
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- 3304 Atmospheric electricity;
- ATMOSPHERIC PROCESSES;
- 3324 Lightning;
- ATMOSPHERIC PROCESSES;
- 3394 Instruments and techniques;
- ATMOSPHERIC PROCESSES