State-to-state quantum dynamics of O + O2 isotope exchange reactions reveals nonstatistical behavior at atmospheric conditions

被引:66
|
作者
Sun, Zhigang [2 ,3 ]
Liu, Lan [2 ,3 ]
Lin, Shi Ying [1 ]
Schinke, Reinhard [4 ]
Guo, Hua [1 ]
Zhang, Dong H. [2 ,3 ]
机构
[1] Univ New Mexico, Dept Chem & Chem Biol, Albuquerque, NM 87131 USA
[2] Chinese Acad Sci, State Key Lab Mol React Dynam, Dalian 116023, Peoples R China
[3] Chinese Acad Sci, Ctr Theoret & Computat Chem, Dalian Inst Chem Phys, Dalian 116023, Peoples R China
[4] Max Planck Inst Dynam & Selbstorg, D-37073 Gottingen, Germany
基金
中国国家自然科学基金;
关键词
complex-forming reactions; isotope effects; ozone; reactive scattering; POTENTIAL-ENERGY SURFACE; O+O-2 EXCHANGE-REACTION; DEPENDENT WAVE-PACKET; REACTIVE SCATTERING; METASTABLE STATES; STATISTICAL-MODEL; RATE COEFFICIENTS; OZONE FORMATION; ISOTOPE; RESONANCES;
D O I
10.1073/pnas.0911356107
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
The O + O-2 exchange reaction is a prerequisite for the formation of ozone in Earth's atmosphere. We report here state-to-state differential and integral cross sections for several O + O-2 isotope-exchange reactions obtained by dynamically exact quantum scattering calculations at collision energies relevant to atmospheric conditions. These reactions are shown to be highly nonstatistical, evidenced by dominant forward scattering and deviation of the integral cross section from the statistical limit. Mechanistic analyses revealed that the nonstatistical channel is facilitated by short-lived osculating resonances. The theoretical results provided an in-depth interpretation of a recent molecular beam experiment of the exchange reaction and shed light on the initial step of ozone recombination.
引用
收藏
页码:555 / 558
页数:4
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