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Soot formation and temperature field structurein co-flow laminar methane–air diffusion flamesat pressures from 10 to 60 atm

机译:烟灰形成和温度场族结构杂交层流 - 空气扩散火焰从10到60atm的压力

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The effects of pressure on soot formation and the structure of the temperature field were studied in coflow methane–air laminar diffusion flames over a wide pressure range, from 10 to 60 atm in a high-pressure combustion chamber. The selected fuel mass flow rate provided diffusion flames in which the soot was completely oxidized within the visible flame envelope and the flame was stable at all pressures considered. The spatially resolved soot volume fraction and soot temperature were measured by spectral soot emission as a function of pressure. The visible (luminous) flame height remained almost unchanged from 10 to 100 atm. Peak soot concentrations showed a strong dependence on pressure at relatively lower pressures; but this dependence got weaker as the pressure is increased. The maximum conversion of the fuel’s carbon to soot, 12.6%, was observed at 60 atm at approximately the mid-height of the flame. Radial temperature gradients within the flame increased with pressure and decreased with flame height above the burner rim. Higher radial temperature gradients near the burner exit at higher pressures mean that the thermal diffusion from the hot regions of the flame towards the flame centerline is enhanced. This leads to higher fuel pyrolysis rates causing accelerated soot nucleation and growth as the pressure increases.
机译:在高压范围内的COFLOW甲烷 - 空气层状扩散火焰中研究了在高压燃烧室中的10至60atm中的COFLOW甲烷 - 空气层状扩散火焰中对烟灰形成和温度场的结构的影响。所选择的燃料质量流量提供了扩散火焰,其中烟雾在可见的火焰封套内完全氧化,并且在考虑的所有压力下燃烧稳定。通过作为压力的函数,通过光谱烟灰发射测量空间分辨的烟灰体积分数和烟灰温度。可见(发光)火焰高度仍然与10到100瓦上的几乎保持不变。峰值浓度在相对较低的压力下对压力的强烈依赖性表现出强烈的依赖性​​;但随着压力的增加,这种依赖性变得越来越弱。在大约火焰中高度的60atm下观察到燃料碳对烟灰的最大转化为12.6%。火焰内的径向温度梯度随压力而增加并随着燃烧器边缘上方的火焰高度而降低。较高压力燃烧器出口附近的较高径向温度梯度意味着从火焰的热区域朝向火焰中心线的热扩散得到增强。这导致较高的燃料热解率,导致加速烟灰成核和生长随着压力的增加而产生。

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