2011
DOI: 10.1029/2010ja016103
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Laboratory studies of UV emissions from proton impact on N2: The Lyman-Birge-Hopfield band system for aurora analysis

Abstract: [1] We have measured the emission cross sections of the Lyman-Birge-Hopfield (LBH) a 1 P g − X 1 S g + band system and several atomic nitrogen (N I) multiplets (1200, 1243, 1493 Å) by H + (proton) impact on N 2 over an impact energy range of 1-7 keV. The peak proton-impact-induced emission cross section of the LBH band system (1260-2500 Å) was measured to be 5.05 ± 1.52 × 10 −17 cm 2 at 7 keV. To the best of our knowledge, the present LBH emission cross sections are reported for the first time in the far ultra… Show more

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Cited by 10 publications
(20 citation statements)
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“…(Ajello et al 2007;James et al 1990). For sufficiently energetic electron or proton collisions, a comparable amount of emission arises from the decay of excited atomic dissociation products (Ajello & Shemansky 1985;Ajello et al 1989Ajello et al , 2011aAjello et al , 2011b. Further electron-induced fluorescence occurs from the Lyman-Birge-Hopfield (LBH) series of bands originating from the a 1 Π g excited state.…”
Section: Introductionmentioning
confidence: 99%
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“…(Ajello et al 2007;James et al 1990). For sufficiently energetic electron or proton collisions, a comparable amount of emission arises from the decay of excited atomic dissociation products (Ajello & Shemansky 1985;Ajello et al 1989Ajello et al , 2011aAjello et al , 2011b. Further electron-induced fluorescence occurs from the Lyman-Birge-Hopfield (LBH) series of bands originating from the a 1 Π g excited state.…”
Section: Introductionmentioning
confidence: 99%
“…The UV emission studies of N 2 by electron-impact-induced fluorescence carried out over the past 30 years at the Jet Propulsion Laboratory (JPL) have been motivated by both astrophysical and theoretical interest (Ajello & Shemansky 1985;Ajello et al 1989Ajello et al , 1998Ajello et al , 2007Ajello et al , 2008Ajello et al , 2011aAjello et al , 2011bAjello et al , 2012James et al 1990;Mangina et al 2011;Young et al 2010). Intense atomic emissions in the dayglow from the atmospheres of N 2 -bearing solar system objects occur mainly from solar photodissociative ionization (PDI) and in the nightglow by collision with secondary electrons and other particles (e.g., magnetospheric protons and O + ; Ajello et al 2011aAjello et al , 2011bAjello et al , 2012Cravens et al 2008Cravens et al , 2010. The LBH molecular bands, the strongest band system in the far ultraviolet (FUV; 1200-2500 Å), excited by particle impact appear strongly in planetary atmospheres containing N 2 as a major species (Ajello et al 2011a).…”
Section: Introductionmentioning
confidence: 99%
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“…One of the important processes that take place in these events is charge transfer (CT), which leads to the ionization of the molecules and the possible production of fast neutrals. In this paper we concentrate on the study of proton collisions with nitrogen molecules, events that can occur in the polar regions of the Earth's atmosphere [8,9] due to the incoming flux of the solar wind, in which the typical energies of the protons are of the order of a few keV [10,11]. Proton collisions with N 2 may also be relevant in the edge of tokamak plasmas if N 2 is used as a scavenger, as suggested in Ref.…”
Section: Introductionmentioning
confidence: 99%