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Relationship Between Microstructure and Properties of Limestone Calcined Rapidly at High Temperatures

机译:高温迅速煅烧石灰岩微观结构与性质的关系

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摘要

The relationship between microstructure and physicochemical properties of limestone including, porosity, bulk density, pore size distribution, specific surface area and activity were studied under the condition of rapid heating from room temperature to 1350-1550 degrees C. The results showed that complete decomposition of limestone (diameter 12.5-15 mm) at 1350 degrees C, 1450 degrees C and 1550 degrees C took 11.7 min, 9.2 min and 6.9 min, respectively. With the prolongation of calcination, lime porosity first increased and then decreased. The peak value of lime porosity was found roughly at the end of limestone decomposition. The variation of bulk density, however, was just the opposite compared to porosity. When calcination temperature increased, the pore size of lime became larger, and the number of micropores decreased correspondingly; furthermore, while calcination time increased, micropores disappeared fast, and macropores increased rapidly. The specific surface area of lime decreased with prolonged calcination time. The best activity of lime could be obtained with high porosity and high specific surface area at the same time. The maximum activity values of lime were 379 mL, 365 mL and 267 mL at the temperatures of 1350 degrees C, 1450 degrees C and 1550 degrees C, respectively.
机译:在从室温快速加热至1350-1550℃的情况下,研究了石灰岩和孔隙率,堆积密度,孔径分布,比表面积和活性的微观结构和物理化学性质的关系。结果表明,结果表明,完全分解了1350℃,1450℃和1550摄氏度的石灰石(直径为12.5-15毫米)分别为11.7分钟,9.2分钟和6.9分钟。随着煅烧的延长,石灰孔隙率首先增加,然后减少。在石灰石分解结束时大致发现石灰孔隙率的峰值。然而,与孔隙率相比,堆积密度的变化与孔隙相反。当煅烧温度增加时,石灰的孔径变大,微孔的数量相应地减少;此外,虽然煅烧时间增加,微孔快速消失,宏孔迅速增加。石灰的比表面积随着慢性煅烧时间而降低。可以在高孔隙率和高比表面积的同时获得最佳活性。石灰的最大活性值分别在1350℃,1450℃和1550℃的温度下为379mL,365mL和267mL。

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