Zhitao Zhang, Enyue Ji, Zhongzhi Fu, Shengshui Chen
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引用次数: 0
Abstract
This study investigates the loading-wetting relationship of rockfill materials through oedometric and triaxial compression tests on two types of rockfill materials during the loading-wetting cycle. Despite significant differences in lithology, it was observed that the initial reloading phase following wetting in both oedometer and triaxial tests consistently involved a degree of plastic hardening, indicating a strong coupling effect between loading and wetting. The universality of this plastic hardening was further validated using a weakening model for rockfill materials. Notably, the hardening caused by the sliding, crushing and rearrangement of rock particles will always dominate, rather than the softening of rock particles. In terms of strength parameters, subsequent loading primarily influenced the cohesion of the material, while the internal friction angle remained largely unchanged. Finally, a conceptual model of the loading-wetting coupling was developed based on the elastic-plastic hardening theory. This model is straightforward and offers potential as a framework for expanding into a more comprehensive elastic-plastic constitutive model.
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.