Kinetics and Thermochemistry of Hydroxyacetonitrile (HOCH<sub>2</sub>CN) and Its Reaction with Hydroxyl Radical

The potential energy surface for OH + HOCH2CN was investigated computationally with B2PLYP-D3/cc-pVTZ density functional theory for geometries and frequencies, and coupled-cluster theory with double, triple and perturbative quadruple excitations approximately extrapolated to the complete basis set limit for energies. The results were employed with canonical variational transition state (TS) theory and an Eckart tunneling model to obtain rate coefficients, k, for three channels, (1) H abstraction from the C–H bonds, (2) H abstraction from the O–H bond and (3) addition to the nitrile C atom. Over 220–450 K, k1(T) = 2.07 × 10–13 (T/298 K)2.264 exp(+15 K/T) cm3 molecule–1 s–1 and is the dominant pathway, accounting for ca. 85% of total reactivity at 298 K and 1 atm. k2(T) = 5.16 × 10–15 (T/298 K)3.470 exp(+440 K/T) and the high-pressure limit for channel 3, k3,∞(T), was found to be temperature-independent with a value of 2.2 × 10–14 cm3 molecule–1 s–1. Consideration of the low-pressure limit and falloff indicates the high-pressure limit is the relevant quantity for atmospheric conditions. Intramolecular hydrogen bonding both stabilizes the TSs and makes them less flexible. The tropospheric lifetime of HOCH2CN with respect to reaction with OH is estimated to be ∼45 days. Its major degradation product is predicted to be HC(O)CN, with minor contributions from HOC(O)CN and other species. Thermochemistry for HOCH2CN and these two products was obtained.

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Publication Details

Journal
ACS Earth and Space Chemistry
Published
2024-08-20
DOI
https://doi.org/10.1021/acsearthspacechem.4c00176
Citations
3
Primary Topic
Atmospheric chemistry and aerosols
Type
article
Field-Weighted Citation Impact
1.13

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article

Kinetics and Thermochemistry of Hydroxyacetonitrile (HOCH2CN) and Its Reaction with Hydroxyl Radical

Paul Marshall, James B. Burkholder
3 citations
ACS Earth and Space Chemistry
Atmospheric chemistry and aerosols
1.13
article

Kinetics and Thermochemistry of Hydroxyacetonitrile (HOCH2CN) and Its Reaction with Hydroxyl Radical

Paul Marshall, James B. Burkholder
article en
3 citations

Abstract

The potential energy surface for OH + HOCH2CN was investigated computationally with B2PLYP-D3/cc-pVTZ density functional theory for geometries and frequencies, and coupled-cluster theory with double, triple and perturbative quadruple excitations approximately extrapolated to the complete basis set limit for energies. The results were employed with canonical variational transition state (TS) theory and an Eckart tunneling model to obtain rate coefficients, k, for three channels, (1) H abstraction from the C–H bonds, (2) H abstraction from the O–H bond and (3) addition to the nitrile C atom. Over 220–450 K, k1(T) = 2.07 × 10–13 (T/298 K)2.264 exp(+15 K/T) cm3 molecule–1 s–1 and is the dominant pathway, accounting for ca. 85% of total reactivity at 298 K and 1 atm. k2(T) = 5.16 × 10–15 (T/298 K)3.470 exp(+440 K/T) and the high-pressure limit for channel 3, k3,∞(T), was found to be temperature-independent with a value of 2.2 × 10–14 cm3 molecule–1 s–1. Consideration of the low-pressure limit and falloff indicates the high-pressure limit is the relevant quantity for atmospheric conditions. Intramolecular hydrogen bonding both stabilizes the TSs and makes them less flexible. The tropospheric lifetime of HOCH2CN with respect to reaction with OH is estimated to be ∼45 days. Its major degradation product is predicted to be HC(O)CN, with minor contributions from HOC(O)CN and other species. Thermochemistry for HOCH2CN and these two products was obtained.

ACS Earth and Space ChemistryVol. 8(9)
University of North Texas (US), National Oceanic and Atmospheric Administration (US), Cooperative Institute for Research in Environmental Sciences (US), University of Colorado Boulder (US)
National Aeronautics and Space Administration, National Oceanic and Atmospheric Administration, University of Colorado Boulder
Affordable and clean energy
Openalex Percentile: Top 25%
Atmospheric chemistry and aerosols
1.13
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