Xin-Xin Dong, Yong-Gui Chen, Xiao-Hua Bao, Wei-Min Ye, Qiong Wang
{"title":"密实高庙子膨润土的界面自愈行为:物理和水力方面","authors":"Xin-Xin Dong, Yong-Gui Chen, Xiao-Hua Bao, Wei-Min Ye, Qiong Wang","doi":"10.1007/s10064-025-04091-8","DOIUrl":null,"url":null,"abstract":"<div><p>In deep geological repositories for disposing of high-level radioactive waste, various types of bentonite interfaces exist in the engineered barrier system. The hydromechanical resistances of the bentonite buffer rely on the sealing and healing of these interfaces, especially the assembled bentonite-bentonite interfaces that can heal spontaneously upon bentonite hydration (i.e., self-healing). This study explored the interfacial self-healing behavior of densely compacted Gaomiaozi bentonite via laboratory tests and evaluated the interfacial self-healing capacity in terms of the physical and hydraulic properties. In detail, the interfacial healing test results indicate that self-healing of the assembled bentonite interface initiated at low suction values (total suction <i>s</i> < 20 MPa) under confined conditions (when the assembled interface is compressed by the swelling pressure). The infiltration test results suggest an increased interfacial hydraulic resistance after long-time water infiltration and a slightly higher permeability than the saturated intact bentonite specimen with the same final dry density. The swelling pressure test results show that the bentonite assembly developed much lower swelling pressure than the intact bentonite specimen (for a given total suction) and achieved a rotated and slightly enhanced swelling pressure anisotropy compared with the saturated intact bentonite specimen with the same final dry density. The MIP test results reveal that the healed interfacial zone has similar pore structure as its adjacent intact zone. Thus, it is concluded that densely compacted Gaomiaozi bentonite has strong interfacial self-healing capacity in physical and hydraulic aspects.</p></div>","PeriodicalId":500,"journal":{"name":"Bulletin of Engineering Geology and the Environment","volume":"84 1","pages":""},"PeriodicalIF":3.7000,"publicationDate":"2025-01-13","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Interfacial self-healing behavior of densely compacted Gaomiaozi bentonite: physical and hydraulic aspects\",\"authors\":\"Xin-Xin Dong, Yong-Gui Chen, Xiao-Hua Bao, Wei-Min Ye, Qiong Wang\",\"doi\":\"10.1007/s10064-025-04091-8\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><p>In deep geological repositories for disposing of high-level radioactive waste, various types of bentonite interfaces exist in the engineered barrier system. The hydromechanical resistances of the bentonite buffer rely on the sealing and healing of these interfaces, especially the assembled bentonite-bentonite interfaces that can heal spontaneously upon bentonite hydration (i.e., self-healing). This study explored the interfacial self-healing behavior of densely compacted Gaomiaozi bentonite via laboratory tests and evaluated the interfacial self-healing capacity in terms of the physical and hydraulic properties. In detail, the interfacial healing test results indicate that self-healing of the assembled bentonite interface initiated at low suction values (total suction <i>s</i> < 20 MPa) under confined conditions (when the assembled interface is compressed by the swelling pressure). The infiltration test results suggest an increased interfacial hydraulic resistance after long-time water infiltration and a slightly higher permeability than the saturated intact bentonite specimen with the same final dry density. The swelling pressure test results show that the bentonite assembly developed much lower swelling pressure than the intact bentonite specimen (for a given total suction) and achieved a rotated and slightly enhanced swelling pressure anisotropy compared with the saturated intact bentonite specimen with the same final dry density. The MIP test results reveal that the healed interfacial zone has similar pore structure as its adjacent intact zone. Thus, it is concluded that densely compacted Gaomiaozi bentonite has strong interfacial self-healing capacity in physical and hydraulic aspects.</p></div>\",\"PeriodicalId\":500,\"journal\":{\"name\":\"Bulletin of Engineering Geology and the Environment\",\"volume\":\"84 1\",\"pages\":\"\"},\"PeriodicalIF\":3.7000,\"publicationDate\":\"2025-01-13\",\"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/s10064-025-04091-8\",\"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}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Bulletin of Engineering Geology and the Environment","FirstCategoryId":"5","ListUrlMain":"https://link.springer.com/article/10.1007/s10064-025-04091-8","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}
Interfacial self-healing behavior of densely compacted Gaomiaozi bentonite: physical and hydraulic aspects
In deep geological repositories for disposing of high-level radioactive waste, various types of bentonite interfaces exist in the engineered barrier system. The hydromechanical resistances of the bentonite buffer rely on the sealing and healing of these interfaces, especially the assembled bentonite-bentonite interfaces that can heal spontaneously upon bentonite hydration (i.e., self-healing). This study explored the interfacial self-healing behavior of densely compacted Gaomiaozi bentonite via laboratory tests and evaluated the interfacial self-healing capacity in terms of the physical and hydraulic properties. In detail, the interfacial healing test results indicate that self-healing of the assembled bentonite interface initiated at low suction values (total suction s < 20 MPa) under confined conditions (when the assembled interface is compressed by the swelling pressure). The infiltration test results suggest an increased interfacial hydraulic resistance after long-time water infiltration and a slightly higher permeability than the saturated intact bentonite specimen with the same final dry density. The swelling pressure test results show that the bentonite assembly developed much lower swelling pressure than the intact bentonite specimen (for a given total suction) and achieved a rotated and slightly enhanced swelling pressure anisotropy compared with the saturated intact bentonite specimen with the same final dry density. The MIP test results reveal that the healed interfacial zone has similar pore structure as its adjacent intact zone. Thus, it is concluded that densely compacted Gaomiaozi bentonite has strong interfacial self-healing capacity in physical and hydraulic aspects.
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.