Althorpe Stuart C
Department of Chemistry, University of Exeter, Stocker Road, Exeter EX4 4QD, United Kingdom.
J Chem Phys. 2004 Jul 15;121(3):1175-86. doi: 10.1063/1.1763833.
We recently interpreted several reactive scattering experiments using a plane wave packet (PWP) formulation of quantum scattering theory [see, e.g., S. C. Althorpe, F. Fernandez-Alonso, B. D. Bean, J. D. Ayers, A. E. Pomerantz, R. N. Zare, and E. Wrede, Nature (London) 416, 67 (2002)]. This paper presents the first derivation of this formulation for atom-plus-diatom reactive scattering, and explains its relation to conventional time-independent reactive scattering. We generalize recent results for spherical-particle scattering [S. C. Althorpe, Phys. Rev. A 69, 042702 (2004)] to atom-rigid-rotor scattering in the space-fixed frame, atom-rigid-rotor scattering in the body-fixed frame, and finally A+BC rearrangement scattering. The reactive scattering is initiated by a plane wave packet, describing the A+BC reagents in center-of-mass scattering coordinates, and is detected by projecting onto a series of AC+B (or AB+C) plane wave "probe" packets. The plane wave packets are localized at the closest distance from the scattering center at which the interaction potential can be neglected. The time evolution of the initial plane wave packet provides a clear visualization of the scattering into space of the reaction products. The projection onto the probe packets yields the time-independent, state-to-state scattering amplitude, and hence the differential cross section. We explain how best to implement the PWP approach in a numerical computation, and illustrate this with a detailed application to the H+D2 reaction.
我们最近使用量子散射理论的平面波包(PWP)公式解释了几个反应性散射实验[例如,参见S. C. Althorpe、F. Fernandez-Alonso、B. D. Bean、J. D. Ayers、A. E. Pomerantz、R. N. Zare和E. Wrede,《自然》(伦敦)416, 67 (2002)]。本文首次推导了这种用于原子加双原子反应性散射的公式,并解释了它与传统的与时间无关的反应性散射的关系。我们将球形粒子散射的最新结果[S. C. Althorpe,《物理评论A》69, 042702 (2004)]推广到空间固定坐标系中的原子-刚性转子散射、体固定坐标系中的原子-刚性转子散射,最后推广到A+BC重排散射。反应性散射由一个平面波包引发,该平面波包在质心散射坐标中描述A+BC反应物,并通过投影到一系列AC+B(或AB+C)平面波“探测”包上进行检测。平面波包定位在距散射中心最近的距离处,在该距离处相互作用势可以忽略不计。初始平面波包的时间演化清晰地展示了反应产物向空间的散射。投影到探测包上得到与时间无关的、态对态的散射振幅,从而得到微分截面。我们解释了如何在数值计算中最好地实施PWP方法,并通过对H+D2反应的详细应用来说明这一点。