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HCl and SO{sub}2 simultaneous absorption at 1023 K with calcined limestone

机译:HCl等{亚} 2在1023 k下的同时吸收煅烧石灰石

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In order to understand sorbent performance for co-combustion of coal and wastes such as refused derived fuel, simultaneous absorption of HCl and SO{sub}2 with calcined limestone was fundamentally investigated using a thermogravimetry at 1023 KSO{sub}2 absorption was interestingly accelerated in the presence of HCl and the level of conversion of calcined limestone reached almost 100% even when particles with 710-1000μm of diameter were used. The mechanisms of this increase in absorptioncapacity were discussed mainly based on the results of scanning electron microscopic and energy dispersive analysis of X-ray observations, and differential scanning calorimetry. As a result, it was concluded that a molten phase was formed on limestonesurface in the early stage of reaction and this phase spreaded into the bulk with the progress of reaction. Melting point was lowered to ca. 998 K by formation of an eutectic phase of CaSO{sub}4 and CaCl{sub}2 mixture. It was considered that such a molten phase caused the absorption capacity increase observed for simultaneous absorption of HCl and SO{sub}2 with calcined limestone.
机译:为了了解煤和废物的共燃烧的吸附剂性能,例如拒绝衍生的燃料,HCl的同时吸收与煅烧石灰石的{Sub} 2在1023kso {sub} 2吸收下使用热重试剂在基本上进行了研究,有趣的是加速在HCl存在下,即使使用具有710-1000μm的直径的颗粒,煅烧石灰石的转化水平达到了几乎100%。主要基于X射线观测结果的扫描电子显微镜和能量分散分析和差示扫描量热法的扫描电子显微镜和能量分析的结果来讨论这种增加的吸收能力的机制。结果,得出结论是,在反应早期阶段的石灰质表面上形成熔融相,并且该阶段随着反应的进展而延伸到体积中。熔点降至CA. 998K通过形成Caso {Sub} 4和CaCl {} 2混合物的共晶相。认为这种熔融相使观察到的吸收能力增加,以同时吸收HCl等{Sub} 2与煅烧的石灰石。

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