NaOH Activation of Raw Soils: Effect of NaOH Content on the Drying Kinetic and Its Modelling

Stevina Bouyila, R. Elenga, L. Ahouet, M. Ngoulou, Serge Konda
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Abstract

NaOH activation of soils is an affordable and promising way to improve mechanical properties of earthen bricks. If for well-activated geopolymers, the hard polymeric network limits the influence of water on mechanical properties, for the weakly activated one, as non-calcined raw clayey soils, the influence of water on these properties would be more critical. This work aims to determine the effect of sodium hydroxide concentration on the drying kinetics of bricks made with raw clayey soils, and to model this kinetics. The results show that the drying kinetics is governed by the diffusion of water due to the absence of free water. The drying duration increases linearly with the increasing of NaOH content, while the volumetric shrinkage decreases, probably thanks to the reduction of the material porosity during the formation of the zeolitic structures. Besides, the drying duration is strongly and negatively correlated with the initial drying rate (−0.97) and bricks did not show visible cracks. Among the five parametric models tested, the Khazaei’s model is the best in terms of all statistical criteria considered. For all models used, the coefficient of determination is ranged from 0.993 to 0.999, and the evolution of the models’ parameters is in accordance with that of the drying kinetics observed.
生土的NaOH活化:NaOH含量对干燥动力学的影响及其模型
NaOH活化土壤是一种经济实惠且有前景的改善土砖力学性能的方法。如果对于活性良好的地质聚合物,硬质聚合物网络限制了水对机械性能的影响,而对于活性较弱的地质聚合物(如未煅烧的原粘性土),水对这些性能的影响将更为关键。本工作旨在确定氢氧化钠浓度对用原始粘性土制成的砖的干燥动力学的影响,并对这种动力学进行建模。结果表明,干燥动力学是由水的扩散控制的,因为没有游离水。干燥持续时间随着NaOH含量的增加而线性增加,而体积收缩率降低,这可能是由于沸石结构形成过程中材料孔隙率的降低。此外,干燥持续时间与初始干燥速率(-0.97)呈强烈负相关,砖块没有出现明显的裂缝。在测试的五个参数模型中,Khazaei模型在所有考虑的统计标准方面都是最好的。对于所有使用的模型,确定系数在0.993至0.999之间,模型参数的演变与观察到的干燥动力学一致。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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