Atom–Molecule Kinetics Using ESR Detection. V. Results for O+OCS, O+CS2, O+NO2, and H+C2H4

Abstract
The wide‐temperature‐range, fast‐flow reactor with ESR detection used in previous papers of this series has been further improved so that rate coefficients of nearly 1013 cm3 mole−1·sec−1 can now be measured by the pseudo‐first‐order method. Results have been obtained over the temperature range 273°–808°K for the reaction O+OCS→CO+SO, over 227°–538°K for O+CS2→CS+SO, and over 297°–543°K for O+NO2→NO+O2 In Arrhenius form the rate coefficients are (cm3 mole−1·sec−1) k1 = 1.9 × 1013exp(− 4530 / RT); k2 = 1.2 × 1013exp(− 1050 / RT); k3 = 1.0 × 1013exp(− 580 / RT). The product SO in [1] and [2] was measured in its 3Σ ground state, and excited vibrational states could not be detected by ESR under our experimental conditions, although the SO must have been so excited initially. Stoichiometry and mechanisms are discussed. The H + C2H4 reaction was also measured in room‐temperature helium and argon, and in helium at 525°K. The data were obtained over a pressure range of about 0.5–2.5 mm, and the pressure dependence of the net rate coefficient kt for H‐atom decay was clearly measurable. Mass spectrometer analysis showed essentially all of the C2H4 to be converted to C2H6 and CH4. The mechanism is discussed. From the P−1 = 0 intercept of plots of kt−1 vs P−1 , the data were assumed to yield values of the rate coefficient k4 for the initial step H + C2H4→C2H5*, i.e., the production of vibrationally excited C2H5* in the Rabinovitch manner. At room temperature the helium data give k4 = 2.2 × 1011 and the argon data 1.4 × 1011cm3mole−1·sec−1 . From the slopes of the two plots the probability for transfer of vibrational energy from C2H5* to translation of argon is found to be about five times greater than for helium. The limited high‐temperature data imply very little temperature dependence for either k4 or its reverse.

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