Journal
PHYSICAL CHEMISTRY CHEMICAL PHYSICS
Volume 9, Issue 31, Pages 4357-4369Publisher
ROYAL SOC CHEMISTRY
DOI: 10.1039/b704920j
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Funding
- Natural Environment Research Council [NE/B00015X/2] Funding Source: researchfish
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The reactions between Ca+(4(2)S(1/2)) and O-3, O-2, N-2, CO2 and H2O were studied using two techniques: the pulsed laser photo-dissociation at 193 nm of an organo-calcium vapour, followed 2 by time-resolved laser-induced fluorescence spectroscopy of Ca+ at 393.37 nm (Ca+(4(2)P(3/2)-4(2)S(1/2))); and the pulsed laser ablation at 532 nm of a calcite target in a fast flow tube, followed by mass spectrometric detection of Ca+. The rate coefficient for the reaction with 03 is essentially independent of temperature, k(189-312 K) = (3.9 +/- 1.2) x 10(-10) cm(3) molecule(-1)s(-1), and is about 35% of the Langevin capture frequency. One reason for this is that there is a lack of correlation between the reactant and product potential energy surfaces for near coplanar collisions. The recombination reactions of Ca+ with O-2, CO2 and H2O were found to be in the fall-off region over the experimental pressure range (1-80 Torr). The data were fitted by RRKM theory combined with quantum calculations on CaO2+, Ca+ . CO2 and Ca+ .H2O, yielding the following results with He as third body when extrapolated from 10(-3)-10(3) Torr and a temperature range of 100-1500 K. For Ca+ + O-2: log(10)(k(rec,0)/cm(6) molecule(-2) S-1) = -26.16 - 1.113log(10)T - 0.056log(10)(2) T, k(rec,infinity) = 1.4 x 10(-10) cm(3) molecule(-1)s(-1), F-c = 0.56. For Ca+ + CO2: log10(k(rec,0)/cm(6) molecule(-2) s(-1)) = -27.94 + 2.204log(10)T - 1.124log(10)(2) T, k(rec,infinity) = 3.5 x 10(-11) cm(3) molecule(-1)s(-1), F-c = 0.60. For Ca+ + H2O: log(10)(k(rec,0)/cm(6) molecule(-2)s(-1)) = -23.88-1.823log(10)T -0.063log(10)(2) T, k(rec,infinity) = 7.3 x 10(-11)exp(830 J mol(-1)/RT) cm(3) molecule(-1) s(-1), F = 0.50 (F-c is the broadening factor). A classical trajectory analysis of the Ca+ + CO2 reaction is then used to investigate the small high pressure limiting rate coefficient, which is significantly below the Langevin capture frequency. Finally, the implications of these results for calcium chemistry in the mesosphere are discussed.
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