首页|期刊导航|东南大学学报(自然科学版)|基于低场核磁共振技术解析碱激发矿渣固化淤泥的水分演化及孔结构

基于低场核磁共振技术解析碱激发矿渣固化淤泥的水分演化及孔结构OA

Analysis of water evolution and pore structure of dredged sediment solidified with alkali-activated slag based on low-field nuclear magnetic resonance technology

中文摘要英文摘要

淤泥中过量的自由水对于固化体系的强度、耐久性和体积稳定性具有负面影响.本文基于低场核磁共振技术研究了淤泥含水率及固淤比对碱激发矿渣固化淤泥水化及孔结构的影响,提出了一种可定量表征水分水化及传输的新方法,从而深化了对水分在固化过程中作用机制的认识.结果表明,小尺寸孔隙能够通过毛细管力有效束缚水分,当淤泥含水率从50%增加至80%,毛细孔比例增加,基体孔隙网络的连通性增强.这导致水分传输效应增强,部分毛细孔内水分因湿度差异定向迁移至约160 nm的大孔中,并与未反应的矿渣发生二次水化反应.提高固淤比可使更多水分参与水化反应,不仅细化了孔隙结构,而且削弱了水分的传输作用.水化产物数量的增多改善了力学性能,高含水率对体系综合性能的不利影响减弱.

Excessive free water in dredged sediment(DS)has a negative impact on the strength,durability and volume stability of the solidification system.This paper investigated the effects of water content of DS and ratio of curing agent to DS on hydration and pore structure of DS solidified with alkali-activated slag(AAS)based on low-field nuclear magnetic resonance technology.A novel method for quantitatively characterizing water hydration and transport was proposed,thereby deepening the understanding of the mechanism of water action during the solidification process.The results show that small-sized pores could effectively trap moisture through capillary force.When the water content of DS increases from 50%to 80%,the proportion of capillary pores increases,and the connectivity of the matrix pore network is enhanced.It results in an enhanced water transport effect,and part of water in capillary pores migrates directionally to the large pores about 160 nm due to humidity differences,and participates in secondary hydration reactions with unreacted slag.Increasing the ratio of curing agent to DS allows more water to participate in the hydration reaction.This not only refines the pore structure,but also weakens the water transport effect.The increase of hydration products improves the mechanical properties,and mitigates the adverse impact of high water content on the comprehensive perfor-mance of the system.

陈振中;徐文沁;陈春;王伟;张亚梅

东南大学材料科学与工程学院,南京 211189东南大学材料科学与工程学院,南京 211189东南大学材料科学与工程学院,南京 211189东南大学材料科学与工程学院,南京 211189东南大学材料科学与工程学院,南京 211189

建筑与水利

碱激发矿渣淤泥固化水分演化孔结构低场核磁共振

alkali-activated slagdredged sediment solidificationwater evolutionpore structurelow-field nuclear magnetic resonance

《东南大学学报(自然科学版)》 2026 (8)

1168-1175,8

国家自然科学基金面上资助项目(51972057)中国施工企业管理协会科技研发资助项目(2024-C-134)常州地铁5号线建设弃置土资源化高效利用与应用技术研究资助项目(8512008673).

10.3969/j.issn.1001-0505.2026.08.008

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