共查询到19条相似文献,搜索用时 109 毫秒
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煤粉燃烧产物的辐射特性 总被引:7,自引:1,他引:6
以Edwards指数宽谱带模型为基冷比较了几种常见的二氧化碳、水蒸汽混合物的吸收系数计算公式。在粒子为光滑、均质假设的基础上,利用Lorentz-Mie理论计算了煤粉粒子、焦炭粒子及碳黑粒子的辐射特怀。经比较,发现国产动力煤煤粉料屯煤灰粒子的辐射特性与原茵联的差别很大。针对国产动力煤,给出了适用于炉内过程数值计算使用的煤粉燃烧产物辐射特性的计算方法。 相似文献
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燃用神华类易结焦煤种的电厂在持续高负荷运行时,其炉膛出口受热面易发生结焦问题,以往以控制炉膛出口烟温作为防止结焦的措施。根据工程实践情况并从煤灰颗粒与烟气的辐射传热特性不同出发,提出了烟温与煤灰颗粒温度的区别,并指出实际运行中炉膛出口受热面发生结焦问题的主要原因在于煤灰颗粒在到达炉膛出口处时其温度仍高于软化温度(ST)。基于此,以单个煤粉颗粒为研究对象,重点计算分析了燃烧速率对炉膛出口处煤灰颗粒温度的影响。结果表明,提高煤粉燃烧速率可以有效地降低炉膛出口处的煤灰颗粒温度,从而极大地改善结焦问题。介绍了上海外高桥第三发电厂首创的广义回热技术,对比分析可知,此技术对防治锅炉结焦更为经济、有效。 相似文献
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国产动力煤煤粉粒子系的辐射特性 总被引:4,自引:1,他引:3
基于均质光滑球形粒子散射的Lorentz-Mie电磁理论,利用实验测得的煤粉粒子的复折射率,在假定粒径符合Rozin-Rammler分布的基础上,计算了国产20种动力煤煤粉粒子系的辐射特性参数。计算结果表明,Planck平均衰减系数、散射系数、吸收系数与粒径分布参数(R90,p)、辐射源温度T、粒子系体积份额fv有关,并可拟合成如下函数形式:K=apbR90c(T+273.15)dfv。在温度(300~1700℃)范围内,拟合误差小于±15%。图4表1参5 相似文献
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选用高硫长广煤为试验煤种、分析纯 CaO 和 MgO 为添加剂,按照设定的配料方案配制为混合煤粉.依据 GB/T 219-1996煤灰熔融特性测试方法,使用 SE-AF 智能灰熔点测试仪对混合煤粉的灰熔点进行了测量.结果表明:随混合煤粉中 CaO 添加质量分数的逐渐增加,混合煤粉灰熔融特性温度呈现 V 型变化规律;按照联产 Q 相水泥熟料配料方案配制的混合煤粉煤灰的结渣趋势程度属于轻微,较长广煤的结渣趋势程度有所降低.对软化温度下混合煤粉煤灰的矿物组成进行了 XRD 分析,并利用 CaO-Al2O3一SiO2 三元系统相图,进一步分析了混合煤粉熔融特性温度变化机理.结果表明:随着混合煤粉中 CaO 添加质量分数的变化,煤灰矿物组成中不同程度地出现低温共融体是煤灰熔融特性温度变化的原因. 相似文献
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炉内煤粉燃烧一维数学模型及其仿真 总被引:4,自引:0,他引:4
为了准确计算炉内煤粉的燃尽率,从研究煤粉粒子的燃烧机理入手,以炉膛内最复杂的燃烧器区域的煤粉燃烧过程为研究对象,通过合理简化煤粉中挥发分和焦炭的燃烧过程,建立了炉内煤粉燃烧沿高度方向上的一维宏观模型,在模型中考虑了煤粉燃烧过程中氧含量的变化,以单个煤粉颗粒燃烧的等密度模型为基础,通过多种煤粉粒径的燃烧过程反映煤粉燃烧的整体过程,推导出计算炉内煤粉燃尽率的显示公式,满足了实时仿真计算的要求。计算结果与实测数据和现有的文献相符,并对结果进行了分析。 相似文献
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本文数值模拟了煤粉旋流火焰燃烧过程,燃烧数值计算包括理论物理模型建立,数值方法两个大部分,计算模型处理了气相湍流与燃烧、气固两相流动、煤颗粒燃烧过程和辐射传热等物理化学过程,以k-ε模型模拟湍流流动;PDF法模拟气相扩散火焰燃烧;颗粒运动计算颗粒运动少颗粒湍流浓度方程模拟颗粒湍流扩散;通量法计算火焰辐射传热,煤粉颗粒复杂燃烧模型计算了颗粒尺寸、形状变化和颗粒孔隙内部燃烧、表面平度对整个颗粒的燃烧过程影响。计算获得了气相速度分布场、气相k和ε分布场、气相温度场、气相组份场和颗粒浓度场及运动过程,揭示了煤粉复合旋流燃烧特性。 相似文献
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本文提出了轴流式燃气透平中煤灰粒径分布对粒子动态特性和叶片磨蚀方面影响的研究结果。在透平叶片流道内应用三元流分析法求解粒子动态特性及其对叶片的冲击。用由实验测量导出的经验公式来描述粒子的回弹情况和叶片材料的磨蚀特性。对典型的煤灰粒径分布所做的研究结果表明,煤灰粒径分布对叶片磨蚀的程度和图样有着显著的影响。 相似文献
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Distribution of mineral matter in pulverized coal 总被引:1,自引:0,他引:1
Mineral transformations, and therefore fly ash evolution, during pulverized coal combustion, depend on the amount, composition and spatial distribution of the inorganic matter within individual pulverized coal particles. Thus, it is necessary to have information on the mineral composition of individual particles, as well as that of the raw pulverized coal. A model is proposed based on the assumption that mineral inclusions of size and composition determined using a CCSEM are distributed randomly in the coal. From this distribution it is possible to generate distributions of mineral content for any particle size and density fraction of coal. The model has been checked by comparing computed results with data on the compositional variations of narrowly and density classified fractions of an Upper Freeport bituminous coal. The results of individual coal particle compositions are used to generate information on the variability of the composition of the fly ash generated during combustion. 相似文献
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Siqi LIU Yanqing NIU Liping WEN Yang LIANG Bokang YAN Denghui WANG Shi en HUI 《Frontiers in Energy》2021,15(1):91
In pulverized coal particle combustion, part of the ash forms the ash film and exerts an inhibitory influence on combustion by impeding the diffusion of oxygen to the encapsulated char core, while part of the ash diffuses toward the char core. Despite the considerable ash effects on combustion, the fraction of ash film still remains unclear. However, the research of the properties of cenospheres can be an appropriate choice for the fraction determination, being aware that the formation of cenospheres is based on the model of coal particles with the visco-plastic ash film and a solid core. The fraction of ash film X is the ratio of the measuring mass of ash film and the total ash in coal particle. In this paper, the Huangling bituminous coal with different sizes was burnt in a drop-tube furnace at 1273, 1473, and 1673 K with air as oxidizer. A scanning electron microscope (SEM) and cross-section analysis have been used to study the geometry of the collected cenospheres and the effects of combustion parameters on the fraction of ash film. The results show that the ash film fraction increases with increasing temperature and carbon conversion ratio but decreases with larger sizes of coal particles. The high fraction of ash film provides a reasonable explanation for the extinction event at the late burnout stage. The varied values of ash film fractions under different conditions during the dynamic combustion process are necessary for further development of kinetic models. 相似文献
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Fly ash from pulverized coal combustion contains residual carbon that can adsorb the air-entraining admixtures (AEAs) added to control the air entrainment in concrete. This is a problem that has increased by the implementation of low-NOx combustion technologies. In this work, pulverized fuel has been combusted in an entrained flow reactor to test the impact of changes in operating conditions and fuel type on the AEA adsorption of ash and NOx formation.Increased oxidizing conditions, obtained by improved fuel-air mixing or higher excess air, decreased the AEA requirements of the produced ash by up to a factor of 25. This was due to a lower carbon content in the ash and a lower specific AEA adsorptivity of the carbon. The latter was suggested to be caused by changes in the adsorption properties of the unburned char and a decreased formation of soot, which was found to have a large AEA adsorption capacity based on measurements on a carbon black. The NOx formation increased by up to three times with more oxidizing conditions and thus, there was a trade-off between the AEA requirements of the ash and NOx formation. The type of fuel had high impact on the AEA adsorption behavior of the ash. Ashes produced from a Columbian and a Polish coal showed similar AEA requirements, but the specific AEA adsorptivity of the carbon in the Columbian coal ash was up to six times higher. The AEA requirements of a South African coal ash was unaffected by the applied operating conditions and showed up to 12 times higher AEA adsorption compared to the two other coal ashes. This may be caused by larger particles formed by agglomeration of the primary coal particles in the feeding phase or during the combustion process, which gave rise to increased formation of soot. 相似文献
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