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Experimental study and kinetic modeling of pulverized coal devolatilization under air and oxycombustion conditions at a high heating rate

机译:空气和氧气燃烧条件下高升温速率下煤粉脱挥发分的实验研究和动力学模型

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This work aims to study the devolatilization of pulverized coal particles under air and oxycombustion conditions. To do so, a newly developed experimental test bench has been used to stabilize coal jet flames with fuel heating rates similar to those found in industrial cbmbustors. The thermal history of coal particles has been experimentally monitored by coupling pyrometric and particle image velocimetry (PIV) measurements. Char samples have been collected at different residence times to obtain devolatilization profiles that have been compared with data issued from 4 empirical models. New sets of kinetic parameters have been proposed to simulate coal devolatilization under high heating rate (>10~6 K/s) with N2- and CO2-based atmospheres. The composition of the burnt gases has also been characterized at various heights above the burner (HAB). The analysis of the obtained results confirmed that an oxygen enrichment of the combustion atmosphere enhances the devolatilization process by favoring an increase of the coal particle temperature. From the comparison between measured and modeled data, it has been observed that apparent devolatilization rates and kinetics were influenced only by the thermal history of the fuel particles with no char-CO2 gasification or CO2-cross linking reaction at the surface of the char in the conditions investigated here. CO releases were found to depend on the devolatilization rates and on the temperatures of the flames. An increase of the SO2 emissions has been strongly correlated to the oxygen concentration in the medium for a given devolatilization yield. NO emissions were not significantly reduced during experiments conducted under oxycombustion conditions compared to those performed under air which is due to the fact that NO emissions have been mainly related to the formation of fuel-NO in this work.
机译:这项工作旨在研究粉煤颗粒在空气和氧气燃烧条件下的脱挥发分。为此,已经使用了新开发的实验测试台来稳定燃煤火焰,其燃料加热速率与工业用燃烧室中的燃料加热速率相似。煤颗粒的热历史已通过高温和颗粒图像测速(PIV)测量的耦合进行了实验监测。已在不同的停留时间收集了炭样品,以获得脱挥发分曲线,并将其与4种经验模型发布的数据进行了比较。提出了新的动力学参数集,以模拟在基于N2和CO2的气氛下高加热速率(> 10〜6 K / s)下的煤挥发。还已在燃烧器(HAB)上方的各种高度对燃烧气体的成分进行了表征。对获得的结果的分析证实,通过促进煤颗粒温度的升高,燃烧气氛中的氧气富集增强了脱挥发分过程。通过对实测数据和模型数据的比较,可以发现,明显的脱挥发分速率和动力学仅受燃料颗粒的热历史影响,而燃料中的焦炭表面未发生焦炭-CO2气化或CO2-交联反应。在这里调查条件。发现CO释放取决于脱挥发分速率和火焰温度。对于给定的脱挥发分产量,SO2排放的增加与培养基中的氧气浓度密切相关。与在空气中进行的实验相比,在氧燃烧条件下进行的实验中NO的排放没有显着减少,这是因为在这项工作中NO的排放主要与燃料NO的形成有关。

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