1999
DOI: 10.1051/aas:1999419
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Charge transfer in collisions of O+ with H and H+ with O

Abstract: Abstract. Cross sections and rate coefficients for total and fine-structure resolved charge transfer in collisions of O + with H and H + with O are presented for collision energies between 0.1 meV/u and 10 MeV/u and temperatures between 10 and 10 7 K. The results are obtained utilizing new quantal and semiclassical molecular-orbital closecoupling, classical trajectory Monte Carlo, and continuum distorted wave calculations in conjunction with previous experimental and theoretical data. Applications to various a… Show more

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Cited by 114 publications
(112 citation statements)
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“…The oxygen chemistry starts with the O( 3 P J ) + H + → O + ( 4 S) + H charge transfer process, where reaction rates are sensitive to the oxygen fine-structure level populations (Stancil et al 1999, and references therein). Indeed the charge transfer proceeds quickly when the O( 3 P 1 ) level (ΔE 12 /k = 228 K) is significantly populated, but it can be a slow proceess in cold gas where only the O( 3 P 2 ) ground-state level is populated (Spirko et al 2003).…”
Section: Pdr Modelsmentioning
confidence: 99%
“…The oxygen chemistry starts with the O( 3 P J ) + H + → O + ( 4 S) + H charge transfer process, where reaction rates are sensitive to the oxygen fine-structure level populations (Stancil et al 1999, and references therein). Indeed the charge transfer proceeds quickly when the O( 3 P 1 ) level (ΔE 12 /k = 228 K) is significantly populated, but it can be a slow proceess in cold gas where only the O( 3 P 2 ) ground-state level is populated (Spirko et al 2003).…”
Section: Pdr Modelsmentioning
confidence: 99%
“…For transitions for which data were not available, we incorporated the formulation of Seaton (1962). Charge exchange rates with protons were obtained from Stancil et al (1998aStancil et al ( , 1998b, Lin et al (2005), and Stancil et al (1999), for C, N, and O, respectively. Collisional excitation and ionization by neutral H was assumed according to Kaulakys (1985) formula for Rydberg levels and neglected for lower levels.…”
Section: The C and O Nlte Calculationsmentioning
confidence: 99%
“…6.3, it includes H 0 , whose contribution comes from the equilibrium condition O + /O 0 0.82 × (H + /H 0 ), valid for O 0 > O + , i.e. in the nebular regions affected by the O + + H 0 ← → O 0 + H + reaction (Williams 1973;Stancil et al 1999).…”
Section: Equatorial Moustachesmentioning
confidence: 99%