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A study of the concomitant calcination and sulfation reactions of calcium carbonate and sulfur dioxide.

机译:碳酸钙和二氧化硫伴随的煅烧和硫酸化反应的研究。

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A structural pore propagation model has been developed to describe microscopic pore evolution from the thermal decomposition reaction of a single calcium carbonate sphere. This model depicts a uniform distribution of equal sized pores growing from the surface of the sphere toward its center while CO{dollar}sb2{dollar} is evolved from the pore bottom. The chemical reaction at the interface, as well as heat transfer from the surroundings to the decomposing sphere and transport of CO{dollar}sb2{dollar} from the pore bottom to the bulk gas, are included in the model.; The pore propagation model has been expanded for the concomitant calcination and sulfation reactions which occur when raw limestone particles are used in a dry flue gas desulfurization system. The model allows the sulfation reaction product to deposit along the pore wall during and after the course of the calcination reaction. The model takes into consideration the SO{dollar}sb2{dollar} transport from the bulk gas into the pore as well as the solid state diffusion through the product layer and the difference in the molar volume of the solid reactant and product.; The simulation of the calcination reaction confirms the experimental observations indicating slower calcination rates at higher background CO{dollar}sb2{dollar} pressures, mainly due to internal unsteady-state buildup of CO{dollar}sb2{dollar} in the pore. The effect of the background CO{dollar}sb2{dollar} pressure is significantly more prominent in the smaller particles.; The model shows the strong effect of the CO{dollar}sb2{dollar} accumulation in the pore during the calcination reaction on the extent of the sulfation reaction which depends on the SO{dollar}sb2{dollar} concentration in the pore space. This effect is more distinguished in larger particles and/or at lower reaction temperature where the calcination reaction is relatively slow compared to the sulfation reaction.
机译:已经开发出结构的孔隙传播模型,以描述由单个碳酸钙球的热分解反应引起的微观孔隙演化。该模型描绘了从球体表面向其中心生长的等大小孔隙的均匀分布,而CO {dollar} sb2 {dollar}从孔隙底部逸出。该模型包括界面处的化学反应,以及从周围环境到分解球体的热传递以及CO {dollar} sb2 {dollar}从孔底到大量气体的传输。孔扩展模型已经扩展,可用于在干烟气脱硫系统中使用原始石灰石颗粒时发生的伴随煅烧和硫酸化反应。该模型允许在煅烧反应的过程中和之后,硫酸化反应产物沿孔壁沉积。该模型考虑了从大量气体向孔隙中的SO {sbs sb 2 {dollar}传输,以及通过产物层的固态扩散以及固体反应物和产物的摩尔体积的差异。煅烧反应的模拟证实了实验观察结果,表明在较高背景CO {sb2 {dollar}压力下,煅烧速率较慢,这主要是由于孔隙中CO {sb2sb2 {dollar}的内部非稳态积累。在较小的颗粒中,本底CO {sb2 {dollar}压力的影响明显更大。该模型显示了煅烧反应期间孔中CO {sb2sb2 {dollar}的积累对硫酸化反应程度的强烈影响,硫酸化反应的程度取决于孔空间中SO {sb2sb2 {dollar}的浓度。在较大的颗粒中和/或在较低的反应温度下(与硫酸化反应相比,煅烧反应相对较慢),这种效果更为明显。

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