Abstract

AbstractDF‐CL studies using NO2 chemiluminescence detection of O yielded a rate constant k1 for O + SiH4 of (2.6 ± 0.5)×10−13 cm3 s−1 at 295 K, where the 95% confidence interval reflects accuracy. FP‐RF studies using flash photolysis of SO2 followed by time‐resolved vuv fluorescence detection of O at 295 K yielded k1 = (3.0 ± 0.5) ×10−13 cm3 s−1. These results are in good accord with most previous measurements and lead to a combined best estimate of k1 = (3.2 ± 0.4) × 10−13 cm3 s−1. The DF‐CL and FP‐RF methods appear to have little unrecognized systematic error. © 1993 John Wiley & Sons, Inc.

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