A quantitative approach to determining sulfate balance for LC3

Oğulcan Canbek , Connor Szeto , Newell R. Washburn , Kimberly E. Kurtis
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引用次数: 2

Abstract

Achieving the correct sulfate balance in limestone calcined clay cements (LC3) to control aluminate hydration is critical for early hydration and property development, but the role of the calcined kaolin (metakaolin) fraction relative to other compositional variables has not been previously well-explored. In addition, little published research has investigated the influence of water-to-solid ratio (w/s) and superplasticizers in this context. This study assesses the influence and quantifies the relative significance of compositional predictors on the sulfate balance and cumulative heat evolved by 24 h for LC3 through a stepwise regression model. Sulfate balance was defined as the time difference between the sulfate depletion point and the time of maximum of alite peak obtained from a time derivative of data obtained through isothermal calorimetry. A methodology based on Kernel smoothing was used to precisely identify these events. The first 24 h of hydration of some LC3 pastes was also monitored via in-situ X-ray diffraction to develop linkages between LC3 composition and hydrated phase assemblage. The statistical analysis identified the metakaolin fraction as particularly significant for the sulfate balance. The results suggest that the metakaolin fraction influences the sulfate balance of LC3 both directly and through its interactions with other constituent materials such as limestone.

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测定LC3硫酸盐平衡的定量方法
在石灰石煅烧粘土水泥(LC3)中实现正确的硫酸盐平衡以控制铝酸盐水化对于早期水化和性能开发至关重要,但煅烧高岭土(偏高岭土)部分相对于其他组成变量的作用此前尚未得到很好的探索。此外,很少有发表的研究在这种情况下研究水固比(w/s)和超塑化剂的影响。本研究通过逐步回归模型评估了成分预测因子对LC3硫酸盐平衡和24小时累积热量的影响,并量化了其相对重要性。硫酸盐平衡被定义为硫酸盐贫化点和阿利特峰最大值时间之间的时间差,阿利特峰是通过等温量热法获得的数据的时间导数获得的。使用了一种基于内核平滑的方法来精确识别这些事件。还通过原位X射线衍射监测了一些LC3浆体的前24小时水合,以发展LC3组成和水合相组合之间的联系。统计分析表明偏高岭土部分对硫酸盐平衡特别重要。结果表明,偏高岭土组分直接影响LC3的硫酸盐平衡,并通过其与其他组成材料(如石灰石)的相互作用来影响。
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