Zhao Zhang, Yong He, Zhi-peng Yu, Hao Wang, Kao-fei Zhu, He Wei, Mayoulou Raud Eucaristia, Ke-neng Zhang, Wei-min Ye
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引用次数: 0
Abstract
Field investigations reveal that shallow clayey soils in heavy metal-contaminated sites often remain in a long-term unsaturated state, experiencing coupled chemo-hydro-mechanical effects. In this study, a series of suction-controlled oedometer tests and microstructural analyses were respectively performed on Cr(VI)-contaminated red clay collected from an abandoned chromite slag disposal site, in order to systematically study the mechanical behaviours of unsaturated contaminated soils. Results indicated that the volumetric behaviour of red clay was synergistically governed by Cr(VI) concentration and suction, with suction variations exerting more pronounced effects on soil compression and swelling/shrinkage deformations than chemical contaminants. Microstructural characterization revealed a dual-porosity system dominated by micropores in the unsaturated red clay. The volume change mechanism induced by heavy metal infiltration was further elucidated through clay particle fabric analysis. Notably, chemical softening phenomena were identified in contaminated specimens. A yield surface equation incorporating chemical softening effects was developed to characterize the mechanical response of unsaturated contaminated red clay under chemo-hydro-mechanical coupling. Validation demonstrated that the proposed model was able to effectively capture the yield characteristics of red clay in the p0 ~ s ~ c plane.
现场调查表明,重金属污染场地的浅层粘土长期处于非饱和状态,受到化学-水-力学耦合效应的影响。为了系统地研究非饱和污染土壤的力学行为,对某废弃铬铁矿渣处置场的Cr(VI)污染红粘土分别进行了一系列吸控测湿试验和微观结构分析。结果表明,Cr(VI)浓度和吸力对红粘土的体积行为有协同作用,吸力变化对土壤压缩和胀缩变形的影响比化学污染物更显著。微观结构表征表明,非饱和红粘土具有以微孔为主的双重孔隙系统。通过对粘土颗粒结构的分析,进一步阐明了重金属入渗引起土壤体积变化的机理。值得注意的是,污染试样中发现了化学软化现象。建立了考虑化学软化效应的屈服面方程,以表征化学-水-力耦合作用下非饱和污染红粘土的力学响应。验证表明,该模型能够有效地捕捉到红粘土在p0 ~ s ~ c平面上的屈服特性。
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.