受激发射泵浦(SEP)1高振动激发氧中能量传递的研究

J. A. Mack, J. Price, A. Wodtke
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摘要

最近的研究结果表明,基态臭氧的紫外光解作用形成了大量的高振动激发O2。要了解上层大气中臭氧的平衡,一个重要的问题是这些高度振动激发的分子的寿命,这些分子被认为是奇氧原子的光解源。本文报道了O2(v”=0)对O2(v”=18-25)制备的SEP在295和395 K下的碰撞失活速率常数。实验类似于Yang等人在NO.3上进行的“泵”、“转储”和“探针”研究,利用脉冲可调谐氟化氩激光器通过众所周知的Schumann-Runge波段,将O2从x3 Σ u -基电子态“泵”到b3 Σ g -激发态的特定旋转振动能级。然后,氙-氯化物泵浦可调谐染料激光系统刺激或“DUMPS”O2回到基电子状态的特定激发旋转振动水平。第二个可调谐染料激光系统然后通过激光诱导荧光“探测”振动激发的O2族。通过改变DUMP和PROBE激光器之间的时间延迟,可以监测制备的振动能级的时间依赖性占用。然后根据寿命的压力依赖性确定给定振动水平下的碰撞淬火速率常数。讨论了测量速率对大气化学反应的影响。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Stimulated Emission Pumping (SEP)1 Studies of Energy Transfer in Highly Vibratonally Excited Oxygen
Recent results have shown that highly vibrationally excited O2 is formed in significant quantities from the ultraviolet photolyis of ground state ozone. An important question for understanding the balance of O3 in the upper atmosphere is the lifetime of these highly vibrationally excited molecules which are proposed2 to be a photolytic source of odd oxygen atoms. In this work we report the rate constants for the collisional deactivation of SEP prepared O2(v"=18-25) by O2(v"=0), at temperatures of 295 and 395 K. The experiments are analogous to the "Pump", "Dump" and "Probe" studies carried out by Yang et al on NO.3 A pulsed tunable Argon Fluoride laser is used to "PUMP" O2 from X 3 Σ u − ground electronic state to a specific rovibrational level of the B 3 Σ g − excited electronic state via the well known Schumann-Runge bands4. A Xenon-Chloride pumped tunable dye laser system then stimulates, or "DUMPS" the O2 back to a specific excited rovibrational level of the ground electronic state. A second tunable dye laser system then "PROBES" the vibrationally excited O2 population by Laser Induced Fluorescence. By varying the time delay between the DUMP and PROBE lasers, the time dependant occupation of the prepared vibrational level is monitored. The collisional quenching rate constant for a given vibrational level is then determined from the pressure dependance of the lifetime. Implications of the measured rates for atmospheric chemical reactions are discussed.
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