1979
DOI: 10.1063/1.438813
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Nitrogen isotope exchange between nitric and nitrous acids

Abstract: The rate of nitrogen isotrope exchange between NO,;and NOi in aqueous solution has been measured, at low acidity, as a function of pH, [NO,;-], [NOi], and temperature. Exchange does not occur in the absence of NO, and during slow exchange processes NO and NOi remain closely similar in isotopic content. The exchange rate law is shown to be R = k[H+][HN0 2 ][N031, and the measured activation parameters are EA = 74.4±2.6kJ, AH! = 72.0±2.6kJ, AS! = -97.4±8.5JK-1 • It is concluded that there is no direct interactio… Show more

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Cited by 7 publications
(5 citation statements)
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“…This underscores the importance of accurately maintaining a constant temperature when studying this reaction. The activation energy of the reverse reaction was determined to be 76 ± 4 kJ mol –1 , in close agreement with the prior determination of 74 kJ mol –1 by Akhtar et al…”
Section: Resultssupporting
confidence: 88%
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“…This underscores the importance of accurately maintaining a constant temperature when studying this reaction. The activation energy of the reverse reaction was determined to be 76 ± 4 kJ mol –1 , in close agreement with the prior determination of 74 kJ mol –1 by Akhtar et al…”
Section: Resultssupporting
confidence: 88%
“…This underscores the importance of accurately maintaining a constant temperature when studying this reaction. The activation energy of the reverse reaction was determined to be 76 ± 4 kJ mol −1 , in close agreement with the prior determination of 74 kJ mol −1 by Akhtar et al 29 A quantum chemistry study was undertaken to determine the origin of the high activation energy associated with K 4 2 k 5 . The gas-phase free energies and enthalpies of reactions 6−9 were established using the average results of the CBS-QB3 and G3B3 methods.…”
Section: ■ Experimental Sectionsupporting
confidence: 79%
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“…The atmospheric cycling of N r (reactive nitrogen) is a focus of both scientific and policy concern, because of the importance of N r in controlling the formation of tropospheric ozone. Atmospheric N r also plays a role in the formation of particulate matter and its long-range transport modifies the global carbon cycle by providing nitrogen fertilization to remote ecosystems. , Measurements of stable nitrogen isotope ratios offer a means of discriminating sources of nitrogen and reactions involved in N r cycling via their specific isotopic signatures. The potential of using the stable nitrogen isotopic signatures of airborne particles to deepen our understanding of the sources, reactivity, transport, and removal of atmospheric nitrogen species has been recognized for a long time . Its application to real world samples, however, has suffered due to multiple analytical challenges.…”
mentioning
confidence: 99%