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

Bones, D. L. ; Gerding, M. ; Höffner, J. ; [weitere]

American Geophysical Union (AGU) ; 2016

In: Geophysical Research Letters Vol. 43, No. 24 ( 2016-12-28)

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In: Geophysical Research Letters, American Geophysical Union (AGU), Vol. 43, No. 24 ( 2016-12-28)

Kurzfassung: The rate constant for the recombination of CaO + ions with electrons, which is important in the lower thermosphere, has been measured The eightfold larger ratio of Ca + /Fe + ions compared with Ca/Fe atoms between 90 and 100 km can now be explained Ca + ions in a descending sporadic E layer neutralize sufficiently rapidly to explain the sudden growth of sporadic neutral Ca layers

Materialart: Online-Ressource

ISSN: 0094-8276 , 1944-8007

URL: Issue

URL: Article

DOI: 10.1002/grl.v43.24

DOI: 10.1002/2016GL071755

Sprache: Englisch

Verlag: American Geophysical Union (AGU)

Publikationsdatum: 2016

ZDB Id: 2021599-X

ZDB Id: 7403-2

SSG: 16,13