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Phase Solubility Changes during Hydration of Monocalciumaluminate and Calcite—The Influence of Alkali Accumulation

机译:铝酸钙和方解石水合过程中的相溶解度变化—碱积累的影响

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摘要

The reaction of CA (monocalcium aluminate) with calcite was closely monitored with regard to phase development, pore water ion content and heat flow. Calcite acts as filler and reactant, finally leading to thermodynamically stable products after hydration at ambient conditions. For better understanding the mechanism taking place, a CA-cement and a commercial calcite mix were compared to a pure CA and pure calcite mix. Both reaction paths were compared. Thermodynamic modeling with PhreeqC gave insight about factors that can influence the course of the hydration reaction. Alkali ions in pore solution of the CA-cement relocate solubility curves of hydration products. Taking into account as many of the alkaline ions as possible, resulted in the closest representation of the measured phase content, confirming thermodynamic modeling. The high dynamics that develop during reaction could only be addressed if a concentration of alkalis in the pore solution at later points in time was respected, thus leading to a shift of solubility curves over time. This was not observed with the pure CA in absence of alkalis.
机译:关于相发展,孔隙水离子含量和热流,密切监测了CA(铝酸单钙)与方解石的反应。方解石充当填料和反应物,在环境条件下水合后最终产生热力学稳定的产物。为了更好地了解发生的机理,将CA水泥和商业方解石混合物与纯CA和纯方解石混合物进行了比较。比较了两种反应路径。用PhreeqC进行热力学建模可以深入了解影响水合反应过程的因素。 CA水泥孔隙溶液中的碱离子重定位水合产物的溶解度曲线。考虑到尽可能多的碱性离子,可以最精确地表示所测相含量,从而确定了热力学模型。如果考虑到稍后时间点的孔溶液中碱的浓度,则只能解决反应过程中产生的高动力学现象,从而导致溶解度曲线随时间推移而发生变化。在没有碱的情况下,纯CA则没有观察到这一点。

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