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On evolution of particle size distribution functions of incipient soot in premixed ethylene-oxygen-argon flames

机译:乙烯-氧-氩预混火焰中初生烟灰粒度分布函数的演变

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摘要

The evolution of the soot particle size distribution function (PSDF) and particle morphology are studied for premixed ethylene-oxygen-argon flat flames at equivalence ratio φ = 2.07 over the maximum flame temperature range of 1600-1900 K. Experiments were carried out using an in-situ probe sampling method in tandem with a scanning mobility particle sizer (SMPS), yielding the PSDF for various distances from the burner surface. The morphology of the particles was examined by transmission electron microscopy (TEM) and atomic force microscopy (AFM). Within the particle size range that can be detected, the PSDF transitions from an apparent unimodal PSDF for high temperature flames (T_f > ~1800 K) to a bimodal PSDF at lower temperatures (T_f < ~1800 K). The bimodal PSDF has a noticeable trough that separates the nucleation tail and log-normal mode. This mode-transition trough had been previously thought to occur at a fixed particle size, but these results show a continuous shift of the trough location towards smaller sizes with increasing flame temperature. TEM images show that the particles are spherical, even when the PSDF is bimodal, suggesting that the bimodality occurs as the primary particles undergoes mass and size growth, and is not a result of particle aggregation. Atomic force microscopy of substrate deposited particles shows that particles spread and form hill like structures upon impact with the substrate surface, indicating that the particles are liquid-like at the time of impact.
机译:研究了在1600-1900 K的最大火焰温度范围内当量比φ= 2.07时的预混乙烯-氧-氩扁平火焰的烟尘粒度分布函数(PSDF)的演变和粒子形态。与扫描迁移率粒度仪(SMPS)串联的原位探针采样方法,可在距燃烧器表面各种距离的位置产生PSDF。通过透射电子显微镜(TEM)和原子力显微镜(AFM)检查颗粒的形态。在可以检测到的粒径范围内,PSDF从高温火焰(T_f>〜1800 K)的表观单峰PSDF转变为较低温度(T_f <〜1800 K)的双峰PSDF。双峰PSDF有一个明显的槽,将成核尾部和对数正态模式分开。以前认为这种模式转变波谷发生在固定的颗粒尺寸上,但是这些结果表明,随着火焰温度的升高,波谷位置向较小尺寸的方向不断变化。 TEM图像显示,即使PSDF是双峰的,颗粒也是球形的,这表明双峰性是在初级颗粒经历质量和尺寸增长时发生的,而不是颗粒聚集的结果。基材沉积颗粒的原子力显微镜显示,颗粒在与基材表面碰撞时会散布并形成丘状结构,这表明在碰撞时颗粒呈液体状。

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