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Shock tube measurements of methyl radical+molecular oxygen kinetics and the heat of formation of the hydroxyl radical.

机译:冲击管测量的是甲基自由基+分子氧动力学和羟基自由基的形成热。

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摘要

The reaction of methyl radicals (CH3) with molecular oxygen (O2), a rate-controlling process in the ignition of natural gas under radical-poor conditions, has been investigated in high-temperature shock tube experiments. The overall rate coefficient, k1 = k1a + k1b, and individual rate coefficients for the two high-temperature product channels, (1a) producing CH3O+O and (1b) producing CH 2O+OH, were determined using ultra-lean mixtures of CH3I and O2 in Ar/He. Narrow-linewidth UV laser absorption at 306.7 nm was used to measure OH concentrations, for which the normalized rise time is sensitive to the overall rate coefficient k1 but relatively insensitive to the branching ratio and to secondary reactions. Atomic resonance absorption spectroscopy measurements of O-atoms were used for a direct measurement of channel (1a). Through the combination of two different diagnostics, rate coefficient expressions for both channels were determined. Over the temperature range 1590 to 2430 K, k1a = 6.08 x 107T 1.54exp(-14005/T) cm3mol-1s -1 and k1b = 68.6 T2.86exp(-4916/T) cm3mol-1s-1. The overall rate coefficient is in close agreement with a recent ab initio calculation and one other shock tube study, while comparison of k1a and k1b to these and other experimental studies yields mixed results.The standard heat of formation of OH at 298 K, Deltaf H°298(OH), a fundamental thermochemical parameter influencing the equilibrium constants of many combustion and atmospheric chemical reactions, has been determined from shock tube measurements spanning the temperature range 1964 to 2718 K and at pressures of 1 to 2.4 atm. Low-concentration, lean and stoichiometric mixtures of H2 and O2 in Ar produced well-controlled levels of OH in a "partial equilibrium" state, in which the OH concentration was dependent only on the thermochemical parameters of the reacting species. Laser absorption was used to measure OH concentrations with sufficient accuracy (2--4%) to clearly determine the value of the heat of formation. Over the range of experimental conditions, the average determination is DeltafH° 298(OH) = 8.92 +/- 0.16 kcal/mol with a standard deviation sigma = 0.04 kcal/mol. This value is 0.40 to 0.48 kcal/mol below the previously accepted values, and agrees with recent theoretical calculations, experimental studies using the positive-ion cycle, and calculations using thermochemical cycles.
机译:在高温激波管实验中,已经研究了甲基自由基(CH3)与分子氧(O2)的反应,这是自由基引发条件下天然气点火过程中的速率控制过程。使用CH3I的超稀混合物确定了两个高温产物通道(1a)生成CH3O + O和(1b)生成CH 2O + OH的总速率系数k1 = k1a + k1b,以及各个速率系数。和氧气在Ar / He中。窄线宽紫外激光在306.7 nm处的吸收用于测量OH浓度,其归一化的上升时间对总速率系数k1敏感,但对支化比和次级反应相对不敏感。 O原子的原子共振吸收光谱测量用于直接测量通道(1a)。通过两种不同的诊断程序的组合,可以确定两个通道的速率系数表达式。在1590至2430 K的温度范围内,k1a = 6.08 x 107T 1.54exp(-14005 / T)cm3mol-1s -1和k1b = 68.6 T2.86exp(-4916 / T)cm3mol-1s-1。总速率系数与最近的从头算和其他激波管研究非常吻合,而将k1a和k1b与这些实验研究和其他实验研究进行比较则得出不同的结果.OH在298 K时的标准生成热,Deltaf H&deg298 (OH)是影响许多燃烧和大气化学反应平衡常数的基本热化学参数,已通过在1964至2718 K的温度范围和1至2.4 atm的压力下进行的冲击管测量确定。 H2和O2在Ar中的低浓度,稀薄和化学计量的混合物在“部分平衡”状态下产生了受控水平的OH,其中OH的浓度仅取决于反应物种的热化学参数。使用激光吸收以足够的精度(2--4%)测量OH浓度,以清楚地确定地层热的值。在实验条件范围内,平均测定值为DeltafH&deg 298(OH)= 8.92 +/- 0.16 kcal / mol,标准偏差sigma = 0.04 kcal / mol。该值比先前接受的值低0.40至0.48 kcal / mol,并且与最近的理论计算,使用正离子循环的实验研究以及使用热化学循环的计算一致。

著录项

  • 作者

    Herbon, John Thomas.;

  • 作者单位

    Stanford University.;

  • 授予单位 Stanford University.;
  • 学科 Chemistry Physical.Engineering Mechanical.
  • 学位 Ph.D.
  • 年度 2004
  • 页码 172 p.
  • 总页数 172
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

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