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Updated: Aug 7, 2026

Retropinacol/Cross-pinacol Coupling Reactions - A Catalytic Access to 1,2-Unsymmetrical Diols
Published on: April 4, 2014
Unravelling the reaction kinetics of ethyl propiolate with OH radicals
1Department of Chemistry, School of Advanced Sciences, VIT-AP University, Beside AP Secretariat Amaravati 522241 Andhra Pradesh India manas.iitm@gmail.com manasranjan.dash@vitap.ac.in.
Abstract:
Ethyl propiolate (EP) is released into the atmosphere primarily due to anthropogenic activities, particularly through its widespread use in laboratory and industrial syntheses of organic compounds. In this study, the kinetics of the gas-phase reaction between EP and OH radicals were investigated experimentally at 298 K and 700 mbar of N2 using a relative rate technique. The measured rate constant was determined to be (2.34 ± 0.54) × 10-13 cm3 per molecule per s. Theoretical calculations were performed to explore the temperature-dependent kinetics over the range of 200-800 K by employing the variational transition state theory (VTST) with high-level single-point energies (SPE). All possible addition and abstraction pathways were explored for two lowest-energy conformers, syn-gauche (R1) and syn-anti (R2). Quantum mechanical tunneling effects were accounted for using both Wigner and Eckart corrections. The computed rate constants exhibited a positive temperature dependence and were fitted to three-parameter Arrhenius expressions (cm3 per molecule per s): k VTST/Wig = 4.1 × 10-28 T 5.2 exp[1230/T] and k VTST/Eck = 1.3 × 10-27 T 5.0 exp[1020/T]. Kinetic analysis indicated that hydrogen abstraction from the secondary carbon (-CH2-) dominated at lower temperatures, while at higher temperatures, OH addition to the terminal carbon and abstraction from the primary carbon (-CH3) became competitive. Potential energy surface and thermochemical analyses supported these findings. Atmospheric assessment showed that OH-initiated oxidation was the primary global loss pathway for EP. The calculated global warming potentials (GWPs) indicated a stronger climate impact at shorter time horizons, which decreased at longer times due to the short atmospheric lifetime of EP.
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