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Devolatilization and Combustion of Coarse-Sized Coal Particles in Oxy-Fuel Conditions: Experimental and Modeling Studies

机译:含氧燃料条件下粗煤粉的脱挥发分和燃烧:实验和模型研究

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摘要

A generalized unsteady-state kinetic model, coupled with all modes of heat transfer, was developed to describe the combined coal devolatilization and the subsequent combustion of the residual char under oxy-fuel condition in both O-2-CO2 and O-2-N-2 environments. Experiments were conducted to validate the model, which was also found to predict the experimental data published in the literature well. The effect of coal particle diameter, temperature of the reactor, and oxygen concentration on devolatilization time was investigated. Peaks in devolatilization and char combustion rates and particle center temperature were studied, and the effect of different parameters assessed. Higher reaction time was observed in an O-2-CO2 environment compared to that in an O-2-N-2 environment due to lower particle temperatures resulting from endothermic gasification reaction and the difference in thermo-physical properties. Simulation studies were carried out to generate temperature, carbon, O-2, CO, and CO2 contours to understand the char combustion reaction mechanism. The reaction started at the external surface of the particle, following unreacted shrinking core model with two zones; the solid product layer and the unreacted shrinking core, separated by a thin reaction front. Gradually, the reaction front thickness increases, leading to the shrinking reactive core model, consisting of three zones: completely reacted ash layer, partially burnt reacting char called reaction zone, and unreacted zone or slightly reacted char core. At the outset, O-2 cannot penetrate into the particle and CO produced near the surface diffuses out to the boundary layer, forming a thin flame. Subsequently, O-2 diffuses through porous ash layer into the char, and CO burns within the pores, with hardly any CO detected in the boundary layer as the particle temperature increases.
机译:建立了一个广义的非稳态动力学模型,并结合了所有的传热模式,以描述组合的脱挥发分以及在氧气燃料条件下在O-2-CO2和O-2-N中残留煤焦的后续燃烧-2环境。进行了实验以验证模型,该模型还被发现可以很好地预测文献中发表的实验数据。研究了煤粒径,反应器温度和氧浓度对脱挥发分时间的影响。研究了脱挥发分,炭燃烧速率和颗粒中心温度的峰值,并评估了不同参数的影响。与O-2-N-2环境相比,在O-2-CO2环境中观察到了更长的反应时间,这是由于吸热气化反应产生的较低的颗粒温度以及热物理性质的差异。进行了模拟研究以生成温度,碳,O-2,CO和CO2等高线,以了解炭燃烧反应机理。按照未反应的具有两个区域的收缩核模型,反应从颗粒的外表面开始。固体产物层和未反应的收缩核,被薄的反应前沿隔开。反应前沿厚度逐渐增加,导致反应堆芯模型缩小,该模型由三个区域组成:完全反应的灰层,部分燃烧的反应炭(称为反应区)和未反应区或轻微反应的炭芯。首先,O-2不能渗透到颗粒中,并且在表面附近产生的CO扩散到边界层,形成稀薄的火焰。随后,O-2穿过多孔灰层扩散到炭中,CO在孔中燃烧,随着颗粒温度的升高,在边界层中几乎检测不到任何CO。

著录项

  • 来源
    《Energy & fuels》 |2018年第1期|839-854|共16页
  • 作者单位

    Natl Inst Technol, Dept Chem Engn, Durgapur 713209, W Bengal, India;

    Natl Inst Technol, Dept Chem Engn, Durgapur 713209, W Bengal, India;

    Natl Inst Technol, Dept Chem Engn, Durgapur 713209, W Bengal, India;

    Natl Inst Technol, Dept Chem Engn, Durgapur 713209, W Bengal, India;

    Natl Inst Technol, Dept Chem Engn, Durgapur 713209, W Bengal, India;

    Natl Inst Technol, Dept Chem Engn, Durgapur 713209, W Bengal, India;

  • 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

  • 入库时间 2022-08-18 00:39:06

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