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A study of the dissociative recombination of CaO+ with electrons: Implications for Ca chemistry in the upper atmosphere.


ABSTRACT: The dissociative recombination of CaO+ ions with electrons has been studied in a flowing afterglow reactor. CaO+ was generated by the pulsed laser ablation of a Ca target, followed by entrainment in an Ar+ ion/electron plasma. A kinetic model describing the gas-phase chemistry and diffusion to the reactor walls was fitted to the experimental data, yielding a rate coefficient of (3.0?±?1.0)?×?10-7?cm3?molecule-1?s-1 at 295?K. This result has two atmospheric implications. First, the surprising observation that the Ca+/Fe+ ratio is ~8 times larger than Ca/Fe between 90 and 100?km in the atmosphere can now be explained quantitatively by the known ion-molecule chemistry of these two metals. Second, the rate of neutralization of Ca+ ions in a descending sporadic E layer is fast enough to explain the often explosive growth of sporadic neutral Ca layers.

SUBMITTER: Bones DL 

PROVIDER: S-EPMC5302016 | biostudies-literature | 2016 Dec

REPOSITORIES: biostudies-literature

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A study of the dissociative recombination of CaO<sup>+</sup> with electrons: Implications for Ca chemistry in the upper atmosphere.

Bones D L DL   Gerding M M   Höffner J J   Martín Juan Carlos Gómez JC   Plane J M C JM  

Geophysical research letters 20161229 24


The dissociative recombination of CaO<sup>+</sup> ions with electrons has been studied in a flowing afterglow reactor. CaO<sup>+</sup> was generated by the pulsed laser ablation of a Ca target, followed by entrainment in an Ar<sup>+</sup> ion/electron plasma. A kinetic model describing the gas-phase chemistry and diffusion to the reactor walls was fitted to the experimental data, yielding a rate coefficient of (3.0 ± 1.0) × 10<sup>-7</sup> cm<sup>3</sup> molecule<sup>-1</sup> s<sup>-1</sup> at 2  ...[more]

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