Quantifying particle size effects on CO2 evolution at solid–liquid interfaces of calcium carbonate in acidic media

Yuki Z. Maeda , Hongyan Wu , Jing Liu
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Abstract

Environmental interfacial processes, from acid rain to acidic wastewaters, drive dissolution of carbonate-rich solids and CO2 release. In this study, we investigate particle size effects on CO2 emission kinetics in reaction between eggshell, a model porous bioceramic, with acetic acid (CH3COOH). Five particle size fractions of eggshells, including dimensions above and below the natural shell thickness, were tested. Time-resolved CH3COOH concentration measurements revealed that there are two regimes in dependence of CO2 emission rates on the particle sizes. Simply breaking the shells does not lead to a clear enhancement in the reaction rate. However, finer particles, particularly those approaching or smaller than the shell thickness, exhibited markedly higher initial rates due to exposure of internal pore networks upon fracture. For all particle sizes, the reaction rates decrease with acid depletion and reduced reactive surface availability with time. No noticeable difference was observed by the presence of CO2 bubbles on the reaction kinetics. These results highlight the role of particle size, morphology, and internal porosity in governing acid–carbonate interfacial reaction kinetics, with implications for porous carbonate dissolution in natural and engineered systems.
酸性介质中粒径对碳酸钙固液界面CO2演化的影响
环境界面过程,从酸雨到酸性废水,驱动富含碳酸盐的固体的溶解和二氧化碳的释放。在这项研究中,我们研究了粒径对多孔生物陶瓷蛋壳与醋酸(CH3COOH)反应CO2排放动力学的影响。测试了蛋壳的五种粒径分数,包括高于和低于自然蛋壳厚度的尺寸。时间分辨CH3COOH浓度测量表明,CO2排放率随粒径的变化存在两种机制。简单地打破壳层不会导致反应速率的明显提高。然而,更细的颗粒,特别是那些接近或小于壳厚的颗粒,由于破裂时内部孔隙网络的暴露,表现出明显更高的初始速率。对于所有粒径,反应速率随酸耗尽而降低,反应表面可用性随时间而降低。CO2气泡的存在对反应动力学没有明显的影响。这些结果强调了颗粒尺寸、形态和内部孔隙度在控制酸-碳酸盐界面反应动力学中的作用,对自然和工程系统中的多孔碳酸盐溶解具有重要意义。
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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