富氧燃烧气氛下石灰石煅烧/硫化特性及模型模拟

利用自制恒温热重装置,模拟循环流化床富氧燃烧气氛,进行了石灰石同时煅烧/硫化实验,并通过对煅烧/硫化产物孔结构以及硫化产物电导率的测量,探讨了硫化反应机理。相比石灰石先煅烧成Ca O再硫化,吸收剂孔隙更容易堵塞且更早进入到产物层扩散控制阶段;产物层扩散控制阶段固态离子扩散率更高,可获得更快的硫化速率和更高的最终钙转化率。烧结会极大影响Ca O的钙转化率,尤其当温度高于950℃时;粒径效应显著,随石灰石颗粒粒径减小最终钙转化率明显提高;SO2浓度提高有助于最终钙利用率的提高。建立了晶粒-微晶粒模型,对不同温度、粒径、SO2浓度条件下石灰石同时煅烧/硫化特性进行了数学模拟,模拟结果与实验结果较为吻合。

Model of limestone calcination / sulfation under oxy-fuel fluidized bed combustion

The characteristics of the simultaneous calcination/ sulfation of limestone under oxy-fuel fluidized bed combustion were studied and compared with those of the sulfation of precalcined CaO. During the calcination stage, SO2 can react with product CaO and slow down the CaCO3 decomposition rate by the covering effect of the CaSO4 product. The sulfation rate of simultaneous calcinatiort/sulfation is slower than that of precalcined CaO, but with a long enough sulfation time, the calcium conversion of simultaneous calcination/sulfation is higher than that of the precalcined CaO. A grain-micrograin model is established to describe the simultaneous calcination, sintering and sulfation of limestone. The graln-micrograln model can reflect the true reaction process of the calcination and sulfation of limestone in oxy-fuel fluidized bed combustion.