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Comparative Study on Sulfur Capture Mechanisms of Shell and Limestone

机译:壳和石灰石硫捕获机制的比较研究

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Three types of shells and two types of limestones are used as sorbent material in this research. The experiments were conducted in a muffle furnace and a fluidized-bed reactor at 800~950°C, at atmosphere and analog flue-gas respectively. The pore shape and the crystal structure of samples were observed by SEM and sulfation property was analyzed by mercury injection apparatus and thermo-gravimetric analyzer. SEM photos show that CaO of calcined shells is composed of a size distribution of cylindrical and connective pores, the hole-wall of which is relative smooth; the large pores can be observed in the sulfated shells. The experimental data show that porosity of original shells varies from 2.45% to 7.23%, but that of the limestone is about 0.10%. According previous research that the calcined shells have a better pore size distribution and connectivity of the pore structure than the calcined limestone, the sulfur capture capability of shells greatly exceeds that of the limestone, which can not be explained well based only on pore structure. Based on gas diffusion theory and solid-state ions diffusion theory, a conclusion has been drawn that the pore structure of shells allows for greater product layer expansion, which aids the penetration of the reaction gases and improves the utility of the intraparticle surface area; the calcined shells have a higher lattice defects concentration than the calcined limestone, which makes the shells have a higher ions diffusion through the product layer at the later stage of sulfation reaction.
机译:在本研究中使用了三种类型的壳和两种类型的石灰石作为吸附剂材料。该实验分别在800〜950℃下在800〜950℃下在大气和模拟烟道气中进行。通过SEM和硫化性能观察样品的孔形和晶体结构,并通过汞注射装置和热重分析仪分析。 SEM照片显示煅烧壳的CAO由圆柱形和连接孔的尺寸分布组成,其孔壁相对光滑;可以在硫酸化壳中观察大孔。实验数据表明,原始壳的孔隙率从2.45%变化至7.23%,但石灰石的孔隙率约为0.10%。根据先前的研究,煅烧壳具有比煅烧的石灰石更好的孔径分布和孔结构的连接,壳的硫捕获能力大大超过石灰石的捕获能力,这对于孔结构仅基于孔结构而无法解释。基于气体扩散理论和固态离子扩散理论,已经绘制了结论,即壳的孔结构允许更大的产品层膨胀,这有助于反应气体的渗透并改善椎间内表面区域的效用;煅烧的壳具有比煅烧的石灰石更高的晶格缺陷浓度,这使得壳体在硫化反应的后期通过产物层具有较高的离子扩散。

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