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Soot formation, spray characteristics, and structure of jet spray flames under high pressure

机译:高压下的烟灰形成,喷雾特性和喷射喷雾火焰的结构

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摘要

Coaxial jet spray flames of kerosene and oxygen are experimentally studied over a pressure range of 0.1-1.0 MPa to determine the relationship between flame structure, droplet behavior, and soot formation region, which varies with changes in pressure. The direct images and chemiluminescence spectra show that the spray flames have three regions: the blue flame region, which has a peak of CH» and C_2* radical chemiluminescence, luminous flame region caused by soot emission, and blue emission region caused by CO_2 emission. With increase in ambient pressure, the flame length shortens drastically, the luminous flame region envelopes the blue flame region, and the blue emission becomes more intense. The result of phase-Doppler anemometry shows that a large number of small droplets evaporate and disappear near the burner, and the evaporation of large droplets also occurs rapidly under high pressure. The result of temperature measurements shows that high-temperature regions appear near the burner. The flame temperature drastically decreases along the central axis, and a minimum temperature point appears. This point moves upstream with increase in ambient pressure because evaporation of the droplets occurs further upstream. A laser-induced incandescence measurement shows that the soot volume fraction does not monotonously increase or decrease with increase in ambient pressure. The soot volume fraction at the central axis becomes low upstream and high downstream. As pressure increases, the vertical position at which the peak of soot volume fraction appears at the central axis moves upstream.
机译:在0.1-1.0 MPa的压力范围内对煤油和氧气的同轴喷射火焰进行了实验研究,以确定火焰结构,液滴行为和烟灰形成区域之间的关系,该关系随压力的变化而变化。直接图像和化学发光光谱表明,喷射火焰具有三个区域:蓝色火焰区域(具有CH»和C_2 *自由基化学发光的峰值),烟尘排放引起的发光火焰区域和CO_2排放引起的蓝色发光区域。随着环境压力的增加,火焰长度急剧缩短,发光火焰区域包围蓝色火焰区域,并且蓝色发射变得更加强烈。相多普勒风速测定的结果表明,大量的小液滴在燃烧器附近蒸发并消失,并且在高压下大液滴的蒸发也迅速发生。温度测量结果表明,燃烧器附近出现高温区域。火焰温度沿中心轴急剧降低,并且出现最低温度点。该点随着环境压力的增加而向上游移动,因为液滴的蒸发在更上游发生。激光诱导的白炽测量表明,烟灰体积分数不会随环境压力的增加而单调增加或减少。中心轴处的烟灰体积分数在上游变低而在下游变高。随着压力增加,烟灰体积分数峰值出现在中心轴的垂直位置向上游移动。

著录项

  • 来源
    《Combustion and Flame》 |2011年第8期|p.1615-1623|共9页
  • 作者单位

    Frontier Research Base for Global young Researchers, Osaka University, 2-1 Yamadaoka, Suita, Osaka 565-0871, Japan;

    Department of Mechanical Engineering, Osaka University, 2-1 Yamadaoka, Suita, Osaka 565-0871, Japan;

    Department of Mechanical Engineering, Osaka University, 2-1 Yamadaoka, Suita, Osaka 565-0871, Japan;

    Department of Mechanical Engineering, Osaka University, 2-1 Yamadaoka, Suita, Osaka 565-0871, Japan;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);美国《生物学医学文摘》(MEDLINE);
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Spray; Jet; Soot; Flame; Pressure;

    机译:喷雾;喷射;煤烟;火焰;压力;
  • 入库时间 2022-08-18 00:12:15

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