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Laser flash photolysis studies of some oxygen(D[1,2]) and OH(X(2)Pi) reactions of atmospheric interest.

机译:激光闪光光解法研究大气中一些氧(D [1,2])和OH(X(2)Pi)反应。

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摘要

A major focus of the research described in this dissertation is investigation of the gas phase atmospheric chemistry of hydrogen cyanide, HCN. The atmospheric chemistry of HCN was studied by investigating its reactions with the ground state OH radical, OH(X2Π), and with the electronically excited oxygen atom, O(1D2). In addition, a number of other O(1D2) reactions of atmospheric importance have also been studied.; A laser flash photolysis-laser induced fluorescence (LFP-LIF) technique was employed to study the kinetics and mechanism of the reaction of OH with HCN (RI) as a function of temperature and pressure over the ranges 268–371 K and 10–600 Torr, respectively. The LFP-LIF experiments involved time-resolved detection of OH by pulsed laser-induced fluorescence spectroscopy following laser flash photolysis of H2O2/HCN/N2, H 2O2/HCN/O2/N2, and H2O 2/HCN/O2 mixtures. The rate coefficient for R1 is found to be considerably slower than previously thought, a result that is consistent with the observed independence of the stratospheric HCN mixing ratio on altitude. The rate coefficient for R1 increases with increasing temperature and with increasing pressure. The values for the room temperature low pressure limiting rate coefficient (k0) and the high pressure limiting rate coefficient (k) are estimated to be 4.0 × 10−33 cm6molecule−2s−1 and 9.5 × 10−15 cm3 molecule −1s−1, respectively. The observed pressure dependence of R1 is typical of an addition reaction, while the observed temperature dependence suggests that addition is not a barrierless process.
机译:本文所研究的主要重点是对氰化氢HCN气相大气化学的研究。通过研究HCN与基态OH自由基OH(X 2 Π)和电子激发氧原子O( 1 的反应,研究了HCN的大气化学性质。 D 2 )。此外,还研究了其他许多具有大气重要性的O( 1 D 2 )反应。激光闪光光解-激光诱导荧光(LFP-LIF)技术用于研究OH与HCN(RI)反应的动力学和机理,温度和压力在268–371 K和10–600范围内分别为托。 LFP-LIF实验涉及在H 2 O 2 / HCN / N 2进行激光快速光解后,通过脉冲激光诱导荧光光谱法对OH的时间分辨检测,H 2 O 2 / HCN / O 2 / N 2 和H 2 O 2 / HCN / O 2 混合物。发现R1的速率系数比以前认为的要慢得多,这一结果与平流层HCN混合比在高度上的独立性一致。 R1的速率系数随温度升高和压力升高而增加。室温低压极限率系数(k 0 )和高压极限率系数(k )的值估计为4.0×10 −33 cm 6 分子 −2 s -1 和9.5×10 −15 cm < super> 3 分子 -1 s -1 。观察到的R1的压力依赖性是加成反应的典型特征,而观察到的温度依赖性则表明加成不是无​​障碍过程。

著录项

  • 作者单位

    Georgia Institute of Technology.;

  • 授予单位 Georgia Institute of Technology.;
  • 学科 Environmental Sciences.; Physics Atmospheric Science.
  • 学位 Ph.D.
  • 年度 2001
  • 页码 190 p.
  • 总页数 190
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 环境科学基础理论;大气科学(气象学);
  • 关键词

  • 入库时间 2022-08-17 11:46:56

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