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模拟微波驱动的沸石的弛豫动力学。

Simulating the relaxation dynamics of microwave-driven zeolites.

作者信息

Combariza Aldo F, Sullivan Ethan, Auerbach Scott M, Blanco Cristian

机构信息

Department of Chemistry and Department of Chemical Engineering, University of Massachusetts, Amherst, Massachusetts 01003, USA.

出版信息

J Phys Chem B. 2005 Oct 6;109(39):18439-44. doi: 10.1021/jp0524680.

DOI:10.1021/jp0524680
PMID:16853374
Abstract

We have performed equilibrium and nonequilibrium molecular dynamics simulations to study how microwave (MW)-heated zeolite systems relax to thermal equilibrium. We have simulated the relaxation of both ionic and dipolar phases in FAU-type zeolites, finding biexponential relaxation in all cases studied. Fast-decay times were uniformly below 1 ps, while slow-decay times were found to be as long as 14 ps. Fast-decay times increase with an increase in the initial temperature difference between MW-heated ions/dipoles and the equilibrium system. Slow-decay times were found to be relatively insensitive to the details of the MW-heated nonequilibrium state. Velocity, force, and orientational correlation functions, calculated at equilibrium to explore the natural dynamics of energy transfer, decay well before 1 ps and show little evidence of biexponential decay. In contrast, kinetic energy correlation functions show strong biexponential behavior with slow-decay times as long as 14 ps. We suggest a two-step mechanism involving initial, efficient energy transfer mediated by strongly anharmonic zeolite-guest forces, followed by a slower process mediated by weakly anharmonic couplings among normal modes of the zeolite framework. In addition to elucidating relaxation from MW-heated states, we expect that these studies will shed light on energy transfer in other contexts, such as adsorption and reaction in zeolites, which often involve significant heat release.

摘要

我们进行了平衡和非平衡分子动力学模拟,以研究微波(MW)加热的沸石系统如何弛豫至热平衡。我们模拟了FAU型沸石中离子相和偶极相的弛豫过程,发现在所有研究案例中均存在双指数弛豫。快速衰减时间均低于1皮秒,而慢速衰减时间长达14皮秒。快速衰减时间随着MW加热的离子/偶极与平衡系统之间初始温差的增加而增加。发现慢速衰减时间对MW加热的非平衡态细节相对不敏感。在平衡状态下计算的速度、力和取向相关函数,用于探索能量转移的自然动力学,在1皮秒之前就衰减良好,几乎没有双指数衰减的迹象。相比之下,动能相关函数显示出强烈的双指数行为,慢速衰减时间长达14皮秒。我们提出了一种两步机制,包括由强非谐沸石-客体力介导的初始高效能量转移,随后是由沸石骨架正常模式之间弱非谐耦合介导的较慢过程。除了阐明从MW加热状态的弛豫过程外,我们预计这些研究将为其他情况下的能量转移提供启示,例如沸石中的吸附和反应,这些过程通常涉及大量的热释放。

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