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The First 20 Hours of Geopolymerization: An in Situ WAXS Study of Flyash-Based Geopolymers

机译:地质聚合的前20小时:基于粉煤灰的地质聚合物的原位WAXS研究

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摘要

This study followed the first 20 h of flyash geopolymerization at 70 °C using time resolved Wide Angle X-ray Scattering (WAXS). The extent of dissolution of the amorphous phase of the flyash was determined to range from 29% to 54% for the different formulations trialed. The dissolution rate of the flyash significantly reduced after the first 5 h for all samples. During the formation stage of the geopolymer there were significant temporal variations in the chemistry of the dissolved solution due to the rate of flyash dissolution, with a relative standard deviation of 20%, 57% and 24% for the Si/Al, Na/Al and H/Si ratios, respectively. Utilizing the Power Law, scattering in the low angle region of the WAXS pattern combined with the geopolymer peak area yielded a measure which correlated with the compressive strength—providing a new method to measure the flyash dissolution and geopolymer formation processes independently. The evolution of several zeolite-like phases was followed, noting there are different formation mechanisms involved even within the same sample. Four samples were examined with compressive strengths ranging from 14(2)–50(9) MPa, each was synthesized with flyash from Collie Power Station (Western Australia) activated with sodium silicate solution of varying concentrations.
机译:这项研究是采用时间分辨广角X射线散射(WAXS)在70°C进行的粉煤灰地质聚合的前20小时。对于所试验的不同制剂,粉煤灰无定形相的溶解程度确定为29%至54%。所有样品在开始5小时后,粉煤灰的溶解速率均显着降低。在地质聚合物的形成阶段,由于粉煤灰的溶解速率,溶解溶液的化学成分存在明显的时间变化,Si / Al,Na / Al的相对标准偏差为20%,57%和24%和H / Si比。利用幂定律,在WAXS模式的低角度区域中的散射与地质聚合物的峰面积相结合,得出了一种与抗压强度相关的量度,从而提供了一种独立测量飞灰溶解和地质聚合物形成过程的新方法。跟踪了几个类似沸石的相的演化过程,注意到即使在同一样品中也存在不同的形成机理。检查了四个样品,其抗压强度在14(2)–50(9)MPa范围内,每个样品均由来自Collie Power Station(西澳大利亚州)的粉煤灰合成,并用不同浓度的硅酸钠溶液活化。

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