Aeronautics and Astronautics, Purdue University, West Lafayette, Indiana 47907, USA.
J Chem Phys. 2017 Feb 21;146(7):074303. doi: 10.1063/1.4975770.
Quasi-classical trajectory (QCT) calculations are used in this work to calculate state-specific N(XΣ)+O(P)→2N(S)+O(P) dissociation and N(XΣ)+O(P)→NO(XΠ)+N(S) exchange cross sections and rates based on the 1A″ and 1A' ab initio potential energy surface by Gamallo et al. [J. Chem. Phys. 119, 2545-2556 (2003)]. The calculations consider translational energies up to 23 eV and temperatures between 1000 K and 20 000 K. Vibrational favoring is observed for dissociation reaction at the whole range of collision energies and for exchange reaction around the dissociation limit. For the same collision energy, cross sections for v = 30 are 4 to 6 times larger than those for the ground state. The exchange reaction has an effective activation energy that is dependent on the initial rovibrational level, which is different from dissociation reaction. In addition, the exchange cross sections have a maximum when the total collision energy (TCE) approaches dissociation energy. The calculations are used to generate compact QCT-derived state-specific dissociation (QCT-SSD) and QCT-derived state-specific exchange (QCT-SSE) models, which describe over 1 × 10 cross sections with about 150 model parameters. The models can be used directly within direct simulation Monte Carlo and computational fluid dynamics simulations. Rate constants predicted by the new models are compared to the experimental measurements, direct QCT calculations and predictions by other models that include: TCE model, Bose-Candler QCT-based exchange model, Macheret-Fridman dissociation model, Macheret's exchange model, and Park's two-temperature model. The new models match QCT-calculated and experimental rates within 30% under nonequilibrium conditions while other models under predict by over an order of magnitude under vibrationally-cold conditions.
本工作使用准经典轨线(QCT)计算基于 Gamallo 等人的 1A″ 和 1A' 从头算势能面[J. Chem. Phys. 119, 2545-2556 (2003)]计算基于态的 N(XΣ)+O(P)→2N(S)+O(P)离解和 N(XΣ)+O(P)→NO(XΠ)+N(S)交换截面和速率。计算考虑了高达 23 eV 的平移能和 1000 K 至 20000 K 之间的温度。在整个碰撞能范围内观察到离解反应和交换反应有利于振动,在离解极限附近有利于交换反应。对于相同的碰撞能,v = 30 的截面比基态大 4 到 6 倍。交换反应具有依赖于初始转动-振动能级的有效激活能,这与离解反应不同。此外,当总碰撞能(TCE)接近离解能时,交换截面有最大值。计算用于生成紧凑的 QCT 衍生态特异性离解(QCT-SSD)和 QCT 衍生态特异性交换(QCT-SSE)模型,这些模型用约 150 个模型参数描述了超过 1×10 个截面。这些模型可直接用于直接模拟蒙特卡罗和计算流体动力学模拟。新模型预测的速率常数与实验测量值、直接 QCT 计算值和其他模型的预测值进行了比较,这些模型包括:TCE 模型、基于 Bose-Candler QCT 的交换模型、Macheret-Fridman 离解模型、Macheret 的交换模型和 Park 的两温模型。在非平衡条件下,新模型与 QCT 计算和实验速率的匹配度在 30%以内,而其他模型在振动冷条件下的预测值低一个数量级以上。