Menéndez Marta, Veselinova Anzhela, Zanchet Alexandre, Jambrina Pablo G, Aoiz F Javier
Departamento de Química Física, Unidad Asociada CSIC, Universidad Complutense de Madrid, 28040 Madrid, Spain.
Departamento de Química Física, Universidad de Salamanca, 37008 Salamanca, Spain.
Phys Chem Chem Phys. 2024 Aug 7;26(31):20947-20961. doi: 10.1039/d4cp01711k.
We present here extensive calculations of the O(P) + H and O(P) + D reaction dynamics spanning the temperature range from 200 K to 2500 K. The calculations have been carried out using fully converged time-independent quantum mechanics (TI QM), quasiclassical trajectories (QCT) and ring polymer molecular dynamics (RPMD) on the two lowest lying adiabatic potential energy surfaces (PESs), 1A' and 1A'', calculated by Zanchet [, 2019, , 094307]. TI QM rate coefficients were determined using the cumulative reaction probability formalism on each PES including all of the total angular momenta and the Coriolis coupling and can be considered to be essentially exact within the Born-Oppenheimer approximation. The agreement between the rate coefficients calculated by using QM and RPMD is excellent for the reaction with D in almost the whole temperature range. For the reaction with H, although the agreement is very good above 500 K, the deviations are significant at lower temperatures. In contrast, the QCT calculations largely underestimate the rate coefficients for the two isotopic variants due to their inability to account for tunelling. The differences found in the disagreements between RPMD and QM rate coefficients for the reactions for both the isotopologues are indicative of the ability of the RPMD method to accurately describe systems where tunelling plays a relevant role. Considering that both reactions are dominated by tunelling below 500 K, the present results show that RPMD is a very powerful tool for determining rate coefficients. The present QM rate coefficients calculated on adiabatic PESs slightly underestimate the best global fits of the experimental measurements, which we attribute to the intersystem crossing with the singlet 1A' PES.
我们在此展示了对O(P) + H和O(P) + D反应动力学在200 K至2500 K温度范围内的广泛计算。这些计算是在由赞切特[2019, , 094307]计算得到的两个最低绝热势能面(PESs)1A'和1A''上,使用完全收敛的与时间无关的量子力学(TI QM)、准经典轨迹(QCT)和环聚合物分子动力学(RPMD)进行的。TI QM速率系数是在每个PES上使用累积反应概率形式确定的,包括所有的总角动量和科里奥利耦合,并且在玻恩 - 奥本海默近似内可被认为基本精确。对于与D的反应,在几乎整个温度范围内,使用QM和RPMD计算的速率系数之间的一致性非常好。对于与H的反应,虽然在500 K以上一致性非常好,但在较低温度下偏差显著。相比之下,由于QCT计算无法考虑隧穿,它们在很大程度上低估了这两种同位素变体的速率系数。对于这两种同位素异构体反应,RPMD和QM速率系数之间分歧中发现的差异表明RPMD方法能够准确描述隧穿起相关作用的系统。考虑到这两个反应在500 K以下都以隧穿为主,目前的结果表明RPMD是确定速率系数的非常强大的工具。在绝热PES上计算的当前QM速率系数略微低估了实验测量的最佳全局拟合值,我们将其归因于与单重态1A' PES的系间窜越。