与方解石混合的铝酸钙水泥的温度依赖性后期水化——g因子定量电位结合gems预测相含量

J. Goergens, F. Goetz-Neunhoeffer
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引用次数: 7

摘要

作为早期水化研究的延续,本研究利用QXRD和热力学模型对不同温度下CAC和CaCO3的后期水化进行了评价。实验在5、23、40和60°C下进行,持续时间长达一年。如前所述,C2AHX在水化早期可能是单碳酸盐的前体,因此在低于20℃的温度下不形成或只形成少量的单碳酸盐。在5°C时,单碳酸酯在7天后开始沉淀,并与CAH10保持在一起。在所有其他研究温度下,单碳酸盐是主要的水合物相。在23°C下形成的CAH10在14天内是可见的,但随后相对于单一碳酸盐变得不稳定。在23°C和40°C时,在一年内达到热力学稳定的相组合。然而,在60°C时,所有样品中都检测到C3AH6的沉淀,这是由于膏体中碳酸盐- afm的w/CAC比不足,因为在这种条件下混合水不可避免地蒸发。然而,C3AH6可以在60°C下部分“再转化”,当样品随后储存在水中并且单碳酸盐再次稳定时。
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Temperature-dependent late hydration of calcium aluminate cement in a mix with calcite – Potential of G-factor quantification combined with GEMS-predicted phase content

In continuation of earlier work on early hydration, this study evaluates the late hydration of CAC and CaCO3 using QXRD and thermodynamic modelling at different temperatures. Experiments were performed at 5, 23, 40 and 60 °C for up to one year. As stated in the preceding study, C2AHX might act as a precursor for monocarbonate in early hydration, and thus no or only little monocarbonate should form at temperatures below 20 °C. At 5 °C, monocarbonate starts precipitating after 7 d and remains alongside CAH10. At all other investigated temperatures, monocarbonate is the dominant hydrate phase. Primarily formed CAH10 at 23 °C is visible up to 14 d but then becomes unstable with respect to monocarbonate. At 23 °C and 40 °C the thermodynamically stable phase assemblage is reached within one year. However, the precipitation of C3AH6 is detected in all samples at 60 °C, which results from an insufficient w/CAC ratio for carbonate-AFm in the paste due to the inevitable evaporation of mixing water for this condition. However, C3AH6 can partly be “re-converted” at 60 °C when the sample is subsequently stored under water and monocarbonate is stable again.

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