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A SOOT MAP FOR METHANE-OXYGEN COUNTERFLOW DIFFUSION FLAMES

机译:甲烷-氧气逆流扩散火焰的烟尘图

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We report on the development of a soot map that separates non-sooting from sooting regions of laminar, eounterflow, methane-oxygen-nitrogen diffusion flames at almospherie pressure. Soot formation is studied at a constant global strain rate of 20 s~(-1) as a function of the amounts of methane (0―100%) in the fuel stream and of oxygen (0―100%) in the oxidizer stream. Visual evidence for incipient soot formation is obtained by increasing the mole fraction of oxygen in the oxidizer stream for a given mole fraction of methane in the fuel stream. As the percent methane in the fuel stream increases, less percent oxygen in the oxidizer stream is required for soot inception. A detailed soot model duplicates the experimentally observed soot map and suggests that soot formation under our conditions is associated with a peak flame temperature near 2550 K and a peak soot volume fraction around 1 ppm. Similarly, peak soot inception can be correlated with a temperature of ~1750 K anywhere along the soot limit curve.
机译:我们报告了烟灰图的发展情况,该烟灰图将非烟火与层流,气流,甲烷-氧-氮-氮扩散火焰的烟ing区域分开,在大气压力下。研究了在20 s〜(-1)的恒定全局应变率下烟灰的形成与燃料流中甲烷(0-100%)和氧化剂流中氧气(0-100%)的关系。对于燃料流中给定的甲烷摩尔分数,通过增加氧化剂流中氧气的摩尔分数,可获得初生烟灰形成的视觉证据。随着燃料流中甲烷的百分比增加,烟灰引入所需的氧化剂流中的氧气百分比将减少。详细的烟灰模型复制了实验观察到的烟灰图,并表明在我们的条件下烟灰的形成与峰值火焰温度接近2550 K和峰值烟灰体积分数约1 ppm有关。同样,在烟灰极限曲线上的任何地方,烟灰峰值的开始都可能与〜1750 K的温度相关。

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