Pore water salinity effect on the intrinsic compression behaviour of artificial soft soils

被引:31
作者
Deng, Yongfeng [1 ]
Zhang, Tongwei [1 ,2 ]
Cui, Yujun [3 ]
Chen, Yonggui [4 ]
Deng, Tingting [1 ]
Zhou, Xiaorong [5 ]
机构
[1] Southeast Univ, Transportat Coll, Inst Geotech Engn, SEU Ave 2, Nanjing 211189, Jiangsu, Peoples R China
[2] Lanzhou Univ, Coll Civil Engn & Mech, Key Lab Mech Disaster & Environm Western China, Lanzhou, Gansu, Peoples R China
[3] Ecole Ponts ParisTech, Lab Navier CERMES, Marne La Vallee, France
[4] Tongji Univ, Sch Civil Engn, Shanghai, Peoples R China
[5] Guangxi Univ, Coll Mech Engn, Nanning, Peoples R China
基金
中国国家自然科学基金;
关键词
Artificial soft clay; Pore water salinity effect; Intrinsic compression behaviour; Particle flocculation; COMPACTED GMZ01 BENTONITE; VOLUME CHANGE BEHAVIOR; FINE-GRAINED SOILS; HYDROMECHANICAL BEHAVIOR; HYDRAULIC CONDUCTIVITY; FLUID COMPOSITION; CLAY MINERALOGY; VERTICAL STRESS; FEBEX BENTONITE; COEFFICIENT;
D O I
10.1016/j.clay.2018.09.027
中图分类号
O64 [物理化学(理论化学)、化学物理学];
学科分类号
070304 ; 081704 ;
摘要
The framework of the intrinsic compression behaviour of normally consolidated soft clay proposed by Burland (1990) is widely adopted in engineering practices. However, further investigations should be conducted on its validity in the coastal and offshore environments to verify the effect of pore water salinity. In the present work, oedometer tests were performed on remoulded artificial soft clays (mixtures of kaolin and bentonite with 0%, 5%, 10%, and 20% of bentonite by mass). The artificial clays were salinized with sodium chloride solutions at concentrations 0 mol/L (distilled water), 0.17 mol/L, 0.51 mol/L, 0.86 mol/L, and 1.70 mol/L at water contents equal to 1.0-1.5 times of the liquid limits. The results showed that the 'intrinsic' properties of clays, including the compression index C-c*(100-1000 kPa), void ratio e(100)*, and compression line based on the void index I-v, changed with the pore water salinity. Following the empirical correlation proposed by previous researchers, the decrease in C-c* caused by pore water salinity could be generally characterised by the liquid limit and void ratio at the liquid limit (e(L)). The dispersed correlation between the predicted e(100)* and the experimental results in this study were caused by the significant changes in e(0)/e(L), controlled by pore water salinity. The relationships between void index I-v and vertical stress sigma(v)' deviated from the intrinsic compression line (ICL) under the saline environment. For the artificial clay rich in smectite, the slopes of I-v-log sigma(v)' before yielding increased with pore water salinity at the initial water content. Pore water salinity affected the intrinsic compression behaviour of soft clays primarily composed of kaolinite to a lesser extent.
引用
收藏
页码:299 / 306
页数:8
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