Ab'/> Water absorption measurement of fine porous aggregates using an evaporative method: Experimental results and physical analysis
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Water absorption measurement of fine porous aggregates using an evaporative method: Experimental results and physical analysis

机译:使用蒸发方法的细孔聚集体的吸水测量:实验结果和物理分析

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AbstractAssessment of the so-called “saturated-surface-dried” state shows a strong dependency on the test operator in the case of fine porous aggregates. This leads to low reliability and reproducibility of water absorption measurement for this family of particles. Evaporative methods for water absorption measurements seem to be a promising alternative. In this paper, we aim at evaluating the robustness and the limit of such methods while understanding the general underlying physical processes. We therefore measure the drying kinetics of non-porous and porous, real and model particles with various sizes and morphologies. We study specifically the unexpected effects of angularity and roughness of particles on drying rate changes over time. Our results suggest that this method is not suitable for all porous particles but shall apply well to crushed fine porous particles such as crushed sand and recycled sand.]]>
机译:<![cdata [ 抽象 所谓的“饱和表面干燥”状态的评估显示了对测试操作员的强大依赖细孔聚集体的情况。这导致该颗粒的吸水测量的可靠性和再现性。用于吸水测量的蒸发方法似乎是一个有希望的替代方案。在本文中,我们的目标是在理解一般底层物理过程的同时评估这些方法的鲁棒性和限制。因此,我们测量具有各种尺寸和形态的无孔和多孔,实体和模型颗粒的干燥动力学。我们专门研究了颗粒的角度和粗糙度对干燥速率随时间变化的意外影响。我们的研究结果表明,该方法不适合所有多孔颗粒,但应适用于压碎的细孔颗粒,例如碎砂和再循环砂。 ]]>

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