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HCl and SO_2 Simultaneous Absorption at 1023 K with Calcined Limestone

机译:HCl和SO_2在1023K与煅烧石灰石的同时吸收

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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_2 with calcined limestone was fundamentally investigated using a thermogravimetry at 1023 K. SO_2 absorption was interestingly accelerated in the presence of HCl and the level of conversion of calcined limestone reached almost 100percent even when particles with 710-1000 mum of diameter were used. The mechanisms of this increase in absorption capacity 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 limestone surface 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_4 and CaCl_2 mixture. It was considered that such amolten phase causeed the absorption capacity increase observed for simultaneous absorption of HCl and SO_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,并且通过在1023k的1023k的热量吡喃中使用热重试剂,在基本上研究了HCl和SO_2的同时吸收。SO_2吸收在HCl存在下有趣地加速。即使使用具有710-1000毫米的直径的颗粒,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散分析的结果来讨论这种吸收能力的增加。结果,得出结论是,在反应早期的初期在石灰石表面形成熔融相,并且这种相对于反应的进展延伸到体积中。熔点降至CA.通过形成CasO_4和CaCl_2混合物的共晶相的998K。认为这种氨水相阶段由于煅烧石灰石而同时吸收HCl和SO_2而观察到的吸收能力增加。

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