Bhattacharya, S. K. ; Thiemens, Mark H. (1988) Isotopic fractionation in ozone decomposition Geophysical Research Letters, 15 (1). pp. 9-12. ISSN 0094-8276
Full text not available from this repository.
Official URL: http://europa.agu.org/?view=article&uri=/journals/...
Related URL: http://dx.doi.org/10.1029/GL015i001p00009
Abstract
The oxygen isotopic fractionation, which occurs during ozone decomposition, has been determined, complementing earlier studies on the fractionation during ozone formation. Oxygen produced in the decomposition is depleted in heavy isotopes in a mass-independent fashion. The mechanism for the mass-independent effect is unknown, though the fractionation magnitude information is required for modelling the steady-state isotopic composition of stratospheric ozone.
Item Type: | Article |
---|---|
Source: | Copyright of this article belongs to American Geophysical Union. |
ID Code: | 67069 |
Deposited On: | 28 Oct 2011 10:57 |
Last Modified: | 28 Oct 2011 10:57 |
Repository Staff Only: item control page