The connection between soil shrinkage and pore water distribution of compacted clays using the nuclear magnetic resonance technique
文献类型:期刊论文
作者 | Jia, Shengao2; Chen, Pan1,2; Wei, Changfu1,2; Tian, Huihui1,2; Yi, Panpan2 |
刊名 | ACTA GEOTECHNICA
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出版日期 | 2024-03-09 |
页码 | 16 |
关键词 | Atterberg limits Compacted clay Nuclear magnetic resonance Soil shrinkage Water content |
ISSN号 | 1861-1125 |
DOI | 10.1007/s11440-024-02291-2 |
英文摘要 | The shrinkage behavior of compacted clays is crucial for evaluating deformation and failure potentials in subgrade and earth dam engineering. A series of soil shrinkage and nuclear magnetic resonance tests were performed on the same specimen for a wide range of compacted clays under drying condition. The correlation between soil shrinkage on the macroscale and pore water evolution on the microscale was thoroughly investigated. The experimental results show that structural shrinkage depends on the initial structure of compacted clay, while the impact of compaction density on basic and residual shrinkages is relatively minimal. The distribution of the transverse relaxation time T2 in a saturated specimen effectively indicates the transitional water content from the structural to basic shrinkage using the NMR technique. Furthermore, a nearly identical maximum T2 could serve as the characteristic time for identifying the other transitional water content between basic and residual shrinkage stages in compacted clays. Two transitional water contents in the shrinkage curve and Atterberg limits are highly correlated, indicating a potential method for estimating the soil shrinkage curve of compacted clays using fundamental soil properties. |
资助项目 | Program of the Youth Innovation Promotion Association, Chinese Academy of Sciences[2020326] ; National Natural Science Foundation of China[51939011] ; National Natural Science Foundation of China[41877269] ; National Natural Science Foundation of China[12002243] |
WOS研究方向 | Engineering |
语种 | 英语 |
WOS记录号 | WOS:001178219600003 |
出版者 | SPRINGER HEIDELBERG |
源URL | [http://119.78.100.198/handle/2S6PX9GI/40893] ![]() |
专题 | 中科院武汉岩土力学所 |
通讯作者 | Chen, Pan |
作者单位 | 1.Univ Chinese Acad Sci, Beijing 100049, Peoples R China 2.Chinese Acad Sci, Inst Rock & Soil Mech, State Key Lab Geomech & Geotech Engn, Wuhan 430071, Hubei, Peoples R China |
推荐引用方式 GB/T 7714 | Jia, Shengao,Chen, Pan,Wei, Changfu,et al. The connection between soil shrinkage and pore water distribution of compacted clays using the nuclear magnetic resonance technique[J]. ACTA GEOTECHNICA,2024:16. |
APA | Jia, Shengao,Chen, Pan,Wei, Changfu,Tian, Huihui,&Yi, Panpan.(2024).The connection between soil shrinkage and pore water distribution of compacted clays using the nuclear magnetic resonance technique.ACTA GEOTECHNICA,16. |
MLA | Jia, Shengao,et al."The connection between soil shrinkage and pore water distribution of compacted clays using the nuclear magnetic resonance technique".ACTA GEOTECHNICA (2024):16. |
入库方式: OAI收割
来源:武汉岩土力学研究所
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