Salo Vili-Taneli, Chen Jing, Runeberg Nino, Kjaergaard Henrik G, Kurtén Theo
Department of Chemistry, Faculty of Science, University of Helsinki, Helsinki FI-00014, Finland.
Department of Chemistry, University of Copenhagen, Copenhagen 2100, Denmark.
J Phys Chem A. 2024 Mar 14;128(10):1825-1836. doi: 10.1021/acs.jpca.3c08043. Epub 2024 Feb 28.
Peroxyl radicals (RO) are important intermediates in the atmospheric oxidation processes. The RO can react with other RO to form reactive intermediates known as tetroxides, ROR. The reaction mechanisms of ROR formation and its various decomposition channels have been investigated in multiple computational studies, but previous approaches have not been able to provide a unified methodology that is able to connect all relevant reactions together. An apparent difficulty in modeling the ROR formation and its decomposition is the involvement of open-shell singlet electronic states along the reaction pathway. Modeling such electronic states requires multireference (MR) methods, which we use in the present study to investigate in detail a model reaction of MeO + MeO → MeOMe, and its decomposition, MeOMe → MeO + O + MeO, as well as the two-body product complexes MeO···O + MeO and MeO···MeO + O. The used MR methods are benchmarked against relative energies of MeO + MeO, MeOMe, and MeO + MeO + O, calculated with CCSD(T)/CBS, W2X, and W3X-L methods. We found that the calculated relative energies of the overall MeO + MeO → MeOMe → MeO + O + MeO reaction are very sensitive to the chosen MR method and that the CASPT2(22e,14o)-IPEA method is able to reproduce the relative energies obtained by the various coupled-cluster methods. Furthermore, CASPT2(22e,14o)-IPEA and W3X-L results show that the MeO···O product complex + MeO is lower in energy than the MeO···MeO complex + O. The formation of MeOMe is exothermic, and its decomposition is endothermic, relative to the tetroxide. Both the formation and decomposition reactions appear to follow pathways with no saddle points. According to potential energy surface scans of the decomposition pathway, the concerted cleavage of both MeO···O bonds in MeOMe is energetically preferred over the corresponding sequential decomposition.
过氧自由基(RO)是大气氧化过程中的重要中间体。RO能与其他RO反应形成称为四氧化物(ROR)的反应中间体。在多项计算研究中已经对ROR形成及其各种分解途径的反应机理进行了研究,但先前的方法未能提供一种能够将所有相关反应联系在一起的统一方法。模拟ROR形成及其分解的一个明显困难是反应途径中涉及开壳单重态电子态。模拟此类电子态需要多参考(MR)方法,我们在本研究中使用该方法详细研究了MeO + MeO → MeOMe的模型反应及其分解反应MeOMe → MeO + O + MeO,以及二体产物复合物MeO···O + MeO和MeO···MeO + O。所使用的MR方法以用CCSD(T)/CBS、W2X和W3X-L方法计算得到的MeO + MeO、MeOMe和MeO + MeO + O的相对能量为基准进行了验证。我们发现,计算得到的整个MeO + MeO → MeOMe → MeO + O + MeO反应的相对能量对所选的MR方法非常敏感,并且CASPT2(22e,14o)-IPEA方法能够重现各种耦合簇方法获得的相对能量。此外,CASPT2(22e,14o)-IPEA和W3X-L的结果表明,MeO···O产物复合物 + MeO的能量低于MeO···MeO复合物 + O。相对于四氧化物,MeOMe的形成是放热的,其分解是吸热的。形成反应和分解反应似乎都遵循没有鞍点的途径。根据分解途径的势能面扫描,MeOMe中两个MeO···O键的协同断裂在能量上比相应的顺序分解更有利。