首页> 外文OA文献 >Early evolution of coal nitrogen in opposed flow combustion configurations.
【2h】

Early evolution of coal nitrogen in opposed flow combustion configurations.

机译:逆流燃烧配置中煤氮的早期释放。

代理获取
本网站仅为用户提供外文OA文献查询和代理获取服务,本网站没有原文。下单后我们将采用程序或人工为您竭诚获取高质量的原文,但由于OA文献来源多样且变更频繁,仍可能出现获取不到、文献不完整或与标题不符等情况,如果获取不到我们将提供退款服务。请知悉。

摘要

A laminar opposed flow, pulverized coal combustion configuration was used to explore the early evolution of light gaseous nitrogenous and hydrocarbon species into the bulk gas phase. Two coals of different ranks were considered. Effects of pyrolysis environment, particle size and heating rates were investigated. Concentration profiles of HCN, NH₃, NO, CH₄, C₂H₂, C₂H₄ and C₂H₆ were measured, under both oxidizing and reducing environments, for three particle sizes, and at high heating rates provided by the hot flue gases of a CO/O₂/Ar flame. Net rates of formation into the bulk gas phase were calculated from the experimental data after correcting for diffusion and convection effects, and were then related to particle time-temperature histories. Experimental data show that HCN precedes NH₃ and NO for both coals. It is the first light gaseous product of coal nitrogen evolution entering into the bulk gas phase. For low rank coals, either only a small amount of tar nitrogen is released or its subsequent oxidation to light gaseous products is slow. For high rank coals secondary reactions of tars are rapid and lead to substantial levels of nitrogenous species. Nature of nitrogenous species evolving into the bulk gas phase was found to be independent of particle size. Lower heating rates favor increased yields of ammonia. Evolution of hydrocarbon species from high rank coals occurs via low molecular weight species, whereas low rank coals yield high molecular weight species. Evolution of hydrocarbon species was found to be independent of particle size and heating rates. Evolution of hydrogen occurs during late stages of devolatilization indicating that it is a product of secondary pyrolysis reactions. A simple kinetic model is proposed to relate rates of formation of nitrogenous species to coal devolatilization kinetics. The latter are similar for three experiments, with fine particles, involving two coals and can be described by a single rate constant given by 63.8 exp (-5220/RT). Bituminous coal (fines), under oxidizing conditions, shows substantially higher rates, possibly due to energy feedback mechanisms in the vicinity of the particles. Literature values, which originated from solid phase measurements, underpredict the quantities of total XN entering the post flame zone by substantial amounts. Our value, which was derived from gas phase species measurements, yields a better prediction of total nitrogenous species entering the post flame zone, and can be incorporated in engineering models aiming at optimizing of pollutant emissions.
机译:层流对流粉煤燃烧结构用于探索轻质气态氮和烃类物质向大量气相的早期演化。考虑了两种不同等级的煤。研究了热解环境,粒度和加热速率的影响。在氧化和还原环境下,测量三种粒径的HCN,NH 3,NO,CH 3,C 2 H 2,C 2 H 3和C 2 H 3的浓度分布,并通过CO / O 2 / Ar火焰的热烟道气提供的高加热速率进行测量。 。校正扩散和对流效应后,根据实验数据计算出进入本体气相的净形成速率,然后将其与颗粒时间-温度历史记录相关联。实验数据表明,两种煤的HCN都先于NH 3和NO。它是进入本体气相的煤氮放出的第一种轻质气态产物。对于低级煤,要么仅释放少量的焦油氮,要么随后氧化为轻质气态产物的速度很慢。对于高级煤,焦油的二次反应迅速,并导致大量的含氮物质。发现演变成整体气相的含氮物质的性质与粒径无关。较低的加热速率有利于提高氨的产率。高等级煤从低分子量物种中析出碳氢化合物,而低等级煤则产生高分子量物种。发现碳氢化合物种类的释放与粒度和加热速率无关。氢的挥发发生在脱挥发分的后期,表明它是二次热解反应的产物。提出了一个简单的动力学模型,将含氮物质的形成速率与煤的脱挥发分动力学联系起来。后者对于三个实验非常相似,涉及两个煤的细颗粒,可以用63.8 exp(-5220 / RT)给出的单个速率常数来描述。烟煤(粉)在氧化条件下表现出明显更高的速率,这可能是由于颗粒附近的能量反馈机制所致。源自固相测量的文献值低估了进入后火焰区的总XN量。我们的值来自气相物种测量,可更好地预测进入火焰后区的总含氮物种,并可将其纳入旨在优化污染物排放的工程模型中。

著录项

  • 作者

    Ghani Muhammad Usman.;

  • 作者单位
  • 年度 1990
  • 总页数
  • 原文格式 PDF
  • 正文语种 en
  • 中图分类

相似文献

  • 外文文献
  • 中文文献
  • 专利

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号