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dc.contributor.authorHierl, Peter M.
dc.contributor.authorDotan, I.
dc.contributor.authorSeeley, John V.
dc.contributor.authorDoren, Jane M. Van
dc.contributor.authorMorris, Robert A.
dc.contributor.authorViggiano, A. A.
dc.date.accessioned2014-12-15T15:29:39Z
dc.date.available2014-12-15T15:29:39Z
dc.date.issued1997-01-01
dc.identifier.citationHierl, Peter M. et al. (1997). "Rate constants for the reactions of O+ with N2 and O2 as a function of temperature (300–1800 K)." Journal of Chemical Physics, 106:3540-3544. http://dx.doi.org/10.1063/1.473450.
dc.identifier.issn0021-9606
dc.identifier.urihttp://hdl.handle.net/1808/16089
dc.descriptionThis is the publisher's version, also available electronically from http://scitation.aip.org/content/aip/journal/jcp/106/9/10.1063/1.473450.
dc.description.abstractWe have studied the rate constants for the reaction of O+ with N2 over the temperature range 300–1600 K and the reaction of O+ with O2 over the range 300 to 1800 K. The results are in good agreement with previous measurements made up to 900 K. The rate constant for the O+reaction with N2 shows a minimum in the temperature range 1100–1300 K. The increase above this temperature is due to N2 v=2 becoming populated. The rate constant for O++O2 shows a minimum in the 800–1100 K range. Comparing to previous drift tube measurements allows the rate constant for O2 (v>0) to be derived. The v>0 rate constant is approximately five times larger than the v=0 rate constant.
dc.publisherAmerican Institute of Physics
dc.titleRate constants for the reactions of O+ with N2 and O2 as a function of temperature (300–1800 K)
dc.typeArticle
kusw.kuauthorHierl, Peter M.
kusw.kudepartmentChemistry
dc.identifier.doi10.1063/1.473450
kusw.oaversionScholarly/refereed, publisher version
kusw.oapolicyThis item does not meet KU Open Access policy criteria.
dc.rights.accessrightsopenAccess


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