Prediction for swelling deformation of fractal-textured bentonite and its sand mixtures in salt solution

被引:5
|
作者
Xiang, Guo-sheng [1 ,2 ]
Yu, Feng [1 ]
Xu, Yong-fu [2 ]
Fang, Yuan [1 ]
Xie, Sheng-hua [1 ]
机构
[1] Anhui Univ Technol, Dept Civil Engn, Maanshan 243002, Anhui, Peoples R China
[2] Shanghai Jiao Tong Univ, Dept Civil Engn, Shanghai 200240, Peoples R China
关键词
bentonite-sand mixture; swelling; fractal; e(m)-p(e) relationship; effective stress; salt solution; OSMOTIC SUCTION; VOLUME CHANGE; BEHAVIOR; PRESSURES; CLAYS; COMPACTION; STRESS;
D O I
10.1180/clm.2019.24
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
Swelling deformation tests of Kunigel bentonite and its sand mixtures were performed in distilled water and NaCl solution. The salinity of NaCl solution has a significant impact on the swelling properties of bentonite, but not on its surface structure. The surface structure was characterized using the fractal dimension D-s. Based on the fractal dimension, a unique curve of the e(m)-p(e) relationship (e(m) is the void ratio of montmorillonite and p(e) is the effective stress) at full saturation was introduced to express the swelling deformation of bentonite-sand mixtures. In mixtures with a large bentonite content, the swelling deformation always followed the e(m)-p(e) relationship. In mixtures with a small bentonite content, when the effective stress reached a threshold, the void ratio of montmorillonite e(m) deviated from the unique e(m)-p(e) curve due to the appearance of a sand skeleton. The threshold of vertical pressure for mixtures in different solutions and the maximum swelling strains were estimated using the e(m)-p(e) relationship. The good agreement between estimates and experimental data suggest that the e(m)-p(e) relationship might be an alternative method for predicting the swelling deformation of bentonite-sand mixtures in salt solution.
引用
收藏
页码:161 / 167
页数:7
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