化工学报 ›› 2018, Vol. 69 ›› Issue (10): 4353-4361.DOI: 10.11949/j.issn.0438-1157.20180639

• 能源和环境工程 • 上一篇    下一篇

循环流化床锅炉内石灰石同时煅烧/硫化反应模型研究

陈亮, 王春波   

  1. 华北电力大学能源动力与机械工程学院, 河北 保定 071003
  • 收稿日期:2018-06-09 修回日期:2018-07-09 出版日期:2018-10-05 发布日期:2018-10-05
  • 通讯作者: 陈亮
  • 基金资助:

    国家重点研发计划项目(2016YFB0600701);中央高校基本科研业务费重大项目(2018ZD03)。

Model of simultaneous calcination/sulfation reaction of limestone under CFB conditions

CHEN Liang, WANG Chunbo   

  1. School of Energy, Power and Mechanical Engineering, North China Electric Power University, Baoding 071003, Hebei, China
  • Received:2018-06-09 Revised:2018-07-09 Online:2018-10-05 Published:2018-10-05
  • Supported by:

    supported by the National Key R & D Program of China (2016YFB0600701) and the Fundamental Research Funds for the Central Universities (2018ZD03).

摘要:

循环流化床锅炉内石灰石分解、脱硫发生的是同时煅烧/硫化反应。建立了石灰石同时煅烧/硫化反应的随机孔模型,综合考虑石灰石的分解、烧结和硫化,且CaO硫化反应基于CaSO4产物层固态离子扩散模式。模型计算结果与实验测试结果吻合良好,并采用该模型研究了同时煅烧/硫化反应的特性。石灰石的同时煅烧/硫化反应包含连续的质量下降阶段和质量上升阶段,且质量最低点随着SO2浓度的增加而升高。石灰石颗粒的煅烧反应发生在颗粒的壳层内,煅烧反应更符合区域反应模型而不是均相反应或缩核反应模型。煅烧环境中的SO2与CaO层反应生成CaSO4,导致CaO层内孔径和孔隙率减小,CO2外扩散阻力增大,从而导致煅烧反应减慢。颗粒硫化反应速度随时间减慢,主要是颗粒内SO2耗尽导致的,颗粒外层不断积累的CaSO4减小了SO2扩散通道,增加了SO2孔内扩散阻力,使颗粒内SO2耗尽区不断增大,颗粒的硫化反应速度不断下降。

关键词: 石灰石, 反应动力学, 循环流化床, 煅烧, 硫化, 模型

Abstract:

Limestone decomposition and desulfurization in a circulating fluidized bed boiler occurs simultaneously with calcination/sulfidation. A random pore model, which considered the calcination of CaCO3, the sintering of CaO and the sulfation of CaO simultaneously, was established, and the sulfation model of CaO was based on the solid state ion diffusion in the CaSO4 product layer. The results of the model are well matched with the results from the TGA test, thus the model can be used to investigate the kinetics of the simultaneous calcination sulfation (SCS) reaction. The SCS reaction contains a mass loss stage and a mass gain stage, which were divided by the minimum mass point. The minimum mass point got higher with the increase of the SO2 concentration. The calcination reaction occurred in a layer of the particle, which is different from the homogeneous reaction model or the unreacted-core shrinking model. The SO2 in the calcination atmosphere can react with the CaO layer and form CaSO4, which can fill the pore of the CaO layer and narrow the pore width, increase the CO2 diffusion resistance and slow the calcination reaction. The sulfation of the calcined CaO got slower with the reaction time. For a particle with a radius of 200 μm sulfated in 0.4% SO2 atmosphere, the decrease of the sulfation rate in the part of the inner 150 μm was mainly caused by the lower SO2 concentration here. There was a zone where the SO2 exhausted. With the sulfation reaction proceeding, more CaSO4 accumulated in the outer layer of the particle, which increased the diffusion resistance of SO2 in the outer layer of the particle, caused the exhausting zone of SO2 being larger and the sulfation rate of the total particle being slower.

Key words: limestone, reaction kinetics, circulating fluidized bed, calcination, sulfation, model

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