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EFFECT OF CURING CONDITIONS ON THE POROSITY CHARACTERISTICS OF METAKAOLIN-FLY ASH GEOPOLYMERS

机译:固化条件对偏高岭土粉煤灰聚合物孔隙率特性的影响

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The porosity characteristics of metakaolin (MK)- and fly ash (FA)-based geopolymers cured under ambient, thermal, and moist conditions were investigated using nitrogen adsorption porosimetry. In general, surface areas were higher for materials prepared from FA (29.0-59.2 m~2/g) than for MK (5.3-12.8 m~2/g). Total pore volumes ranged from 0.034-0.104 cc/g for MK-based materials and from 0.077-0.089 cc/g for FA-based materials. For MK-based geopolymers, curing under ambient conditions resulted in a single, broad pore size distribution (PSD) between 250-500 A. PSDs for MK-based geopolymers cured using thermal or moist methods were bimodal with broad peaks between approximately 60-250 A and 250-500 A. For FA-based geopolymers, a single, broad PSD was observed and ranged from 20-100 A for ambient temperature cured materials and 40-200 A for materials cured under thermal or moist conditions. The observed pore size distributions were accompanied by a shift to higher wavenumber in the position of the main geopolymer band in the ATR-FTIR spectra of geopolymer materials after thermal or moist curing, indicating a higher concentration of Si-O-Si bonds formed in the materials cured at elevated temperatures. These results suggest that the observed PSDs result from Si-O-Al and Si-O-Si bond formation during curing and are affected by the curing conditions.
机译:使用氮气吸附孔隙率法研究了在环境,热和潮湿条件下固化的偏高岭土(MK)和粉煤灰(FA)基地质聚合物的孔隙率特性。通常,用FA(29.0-59.2 m〜2 / g)制得的材料的表面积要比MK(5.3-12.8 m〜2 / g)高。对于MK基材料,总孔体积为0.034-0.104 cc / g,对于FA基材料,总孔体积为0.077-0.089 cc / g。对于基于MK的地质聚合物,在环境条件下固化会导致250-500 A之间的单个宽孔径分布(PSD)。使用热或湿法固化的基于MK的地质聚合物的PSD是双峰的,峰宽约为60-250 A和250-500A。对于基于FA的地质聚合物,观察到单个宽的PSD,对于环境温度固化的材料,其范围为20-100 A,对于在热或潮湿条件下固化的材料,范围为40-200A。在热或湿固化后,观察到的孔径分布伴随着地质聚合物材料的ATR-FTIR光谱中主要地质聚合物带的位置向更高波数的偏移,表明在高聚物中形成的Si-O-Si键浓度更高。材料在高温下固化。这些结果表明,观察到的PSD是由固化过程中Si-O-Al和Si-O-Si键的形成引起的,并且受固化条件的影响。

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