{"title":"Permeability characteristics and empirical prediction of fine sandy soils stabilized by cement and metakaolin","authors":"Shengnian Wang, Haiyan Jiang, Wenjie Wang, Zhijian Wu, Leilei Gu, Xinqun Gao","doi":"10.1007/s10064-024-03959-5","DOIUrl":null,"url":null,"abstract":"<div><p>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.</p></div>","PeriodicalId":500,"journal":{"name":"Bulletin of Engineering Geology and the Environment","volume":"83 11","pages":""},"PeriodicalIF":3.7000,"publicationDate":"2024-10-29","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Bulletin of Engineering Geology and the Environment","FirstCategoryId":"5","ListUrlMain":"https://link.springer.com/article/10.1007/s10064-024-03959-5","RegionNum":2,"RegionCategory":"工程技术","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q3","JCRName":"ENGINEERING, ENVIRONMENTAL","Score":null,"Total":0}
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.
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.