Permeability characteristics and empirical prediction of fine sandy soils stabilized by cement and metakaolin

IF 3.7 2区 工程技术 Q3 ENGINEERING, ENVIRONMENTAL
Shengnian Wang, Haiyan Jiang, Wenjie Wang, Zhijian Wu, Leilei Gu, Xinqun Gao
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引用次数: 0

Abstract

The permeability of cementitious soils is substantially controlled by the permeability of the soil itself, the dosage of binder, the water-to-binder ratio, and other factors. This study employed metakaolin as the additive to enhance underground engineering construction's economic benefit since it could improve the impermeability of cement-stabilized soils and replace cement partly. A series of indoor permeability tests on cement- and metakaolin-stabilized fine sandy soils (CMSFSSs) with different cement-to-metakaolin ratios, water-to-binder (the mixture of cement and metakaolin) ratios, total binder contents, and curing times were conducted. The influences of these factors on the impermeability of CMSFSSs were investigated. Their impermeability improvement mechanism at the microscale was explored by Scanning Electron Microscopy and Mercury Injection Porosimeter tests. The empirical permeability coefficient prediction formulas about these influence factors, compressive strength, and porosity were discussed. The results showed that the best impermeability of CMSFSSs was achieved when the cement-to-metakaolin ratio was 5:1, saving 1/6 cement consumption. This ratio did not vary with the total binder content. The permeability coefficient of CMSFSSs increased nonlinearly with the water-to-binder ratio but decreased rapidly at first and then slowly with the increase of total binder content and curing time. The optional water-to-binder ratio should be less than 0.6 if both their liquidity and impermeability requirements were met together. The total binder content for fine sandy soil stabilization should be less than 15% since it was not more reliable to improve the impermeability of fine sandy soils by using excessive binder in terms of economic benefits. The hydrated gels in CMSFSSs formed rapidly at the early curing time. The calcium hydroxide formed by cement hydration disappeared over the curing time. The internal pore volume and sizes in CMSFSSs decreased over the curing time, resulting in worse and worse connectivity. All of them proved the contribution of metakaolin to cement-stabilized soil's impermeability improvement. Six empirical formulas for the permeability coefficient of binder-stabilized soils were summarized regarding the water-to-binder ratio, total binder content, curing time, unconfined compressive strength, and porosity. The results of this study provide theoretical and technical references for improving the impermeability of binder-stabilized soils.

用水泥和偏高岭土加固的细砂土的渗透性特征和经验预测
水泥稳定土的渗透性主要受土壤本身的渗透性、粘结剂的用量、水与粘结剂的比例等因素的控制。本研究采用偏高岭土作为添加剂,以提高地下工程施工的经济效益,因为它可以改善水泥稳定土的抗渗性,并部分取代水泥。研究人员对不同水泥与偏高岭土比例、水与粘结剂(水泥与偏高岭土的混合物)比例、粘结剂总含量和固化时间的水泥和偏高岭土稳定细砂土(CMSFSS)进行了一系列室内渗透性试验。研究了这些因素对 CMSFSS 抗渗性的影响。通过扫描电子显微镜和汞注射孔隙度测试,探讨了微观尺度上的抗渗性改善机制。讨论了有关这些影响因素、抗压强度和孔隙率的经验渗透系数预测公式。结果表明,当水泥与高岭土的比例为 5:1 时,CMSFSS 的抗渗性最好,可节省 1/6 的水泥用量。该比例不随粘结剂总含量的变化而变化。CMSFSS 的渗透系数随水与粘结剂比率的增加而非线性增加,但随着总粘结剂含量和固化时间的增加,渗透系数最初迅速下降,然后缓慢下降。如果同时满足流动性和抗渗性要求,可选的水胶比应小于 0.6。用于稳定细砂土的粘结剂总含量应小于 15%,因为从经济效益角度考虑,使用过量粘结剂来提高细砂土的抗渗性并不可靠。CMSFSS 中的水化凝胶在固化初期迅速形成。水泥水化形成的氢氧化钙在固化过程中逐渐消失。随着固化时间的推移,CMSFSS 的内部孔隙体积和大小逐渐减小,导致连通性越来越差。所有这些都证明了偏高岭土对水泥稳定土防渗性能改善的贡献。研究总结了六种关于粘结剂稳定土渗透系数的经验公式,分别涉及水与粘结剂的比例、粘结剂总含量、固化时间、无侧限抗压强度和孔隙率。研究结果为改善粘结剂稳定土的抗渗性提供了理论和技术参考。
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来源期刊
Bulletin of Engineering Geology and the Environment
Bulletin of Engineering Geology and the Environment 工程技术-地球科学综合
CiteScore
7.10
自引率
11.90%
发文量
445
审稿时长
4.1 months
期刊介绍: Engineering geology is defined in the statutes of the IAEG as the science devoted to the investigation, study and solution of engineering and environmental problems which may arise as the result of the interaction between geology and the works or activities of man, as well as of the prediction of and development of measures for the prevention or remediation of geological hazards. Engineering geology embraces: • the applications/implications of the geomorphology, structural geology, and hydrogeological conditions of geological formations; • the characterisation of the mineralogical, physico-geomechanical, chemical and hydraulic properties of all earth materials involved in construction, resource recovery and environmental change; • the assessment of the mechanical and hydrological behaviour of soil and rock masses; • the prediction of changes to the above properties with time; • the determination of the parameters to be considered in the stability analysis of engineering works and earth masses.
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