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Computational studies on the gas phase reaction of methylenimine (CH(2)NH) with water molecules
In this work, we used quantum chemical methods and chemical kinetic models to answer the question of whether or not formaldehyde (CH(2)O) and ammonia (NH(3)) can be produced from gas phase hydration of methylenimine (CH(2)NH). The potential energy surfaces (PESs) of CH(2)NH + H(2)O → CH(2)O + NH(3)...
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Formato: | Online Artículo Texto |
Lenguaje: | English |
Publicado: |
Nature Publishing Group UK
2020
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Materias: | |
Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7335075/ https://www.ncbi.nlm.nih.gov/pubmed/32620911 http://dx.doi.org/10.1038/s41598-020-67515-3 |
Sumario: | In this work, we used quantum chemical methods and chemical kinetic models to answer the question of whether or not formaldehyde (CH(2)O) and ammonia (NH(3)) can be produced from gas phase hydration of methylenimine (CH(2)NH). The potential energy surfaces (PESs) of CH(2)NH + H(2)O → CH(2)O + NH(3) and CH(2)NH + 2H(2)O → CH(2)O + NH(3) + H(2)O reactions were computed using CCSD(T)/6–311++G(3d,3pd)//M06-2X/6–311++G(3d,3pd) level. The temperature-and pressure-dependent rate constants were calculated using variational transition state theory (VTST), microcanonical variational transition state theory [Formula: see text] and Rice–Ramsperger–Kassel–Marcus/master equation (RRKM/ME) simulations. The PES along the reaction path forming a weakly bound complex (CH(2)NH⋯H(2)O) was located using VTST and [Formula: see text] VTST, however, the PES along the tight transition state was characterized by VTST with small curvature tunneling (SCT) approach. The results show that the formation of CH(2)NH + H(2)O → CH(2)NH⋯H(2)O is pressure -and temperature-dependent. The calculated atmospheric lifetimes of CH(2)NH⋯H(2)O (~ 8 min) are too short to undergo secondary bimolecular reactions with other atmospheric species. Our results suggest that the formation of CH(2)O and NH(3) likely to occur in the combustion of biomass burning but the rate of formation CH(2)O and NH(3) is predicted to be negligible under atmospheric conditions. When a second water molecule is added to the reaction, the results suggest that the rates of formation of CH(2)O and NH(3) remain negligible. |
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