

请您输入您的关键词,以便更快的了解我们最新的新闻和产品信息
版权所有©重庆为讯科学仪器有限责任公司 2025 地址:重庆两江新区水土高新城云汉大道105号半导体产业园A5栋6F-8F
ICP备案/许可证号:渝ICP备2023002157号-1
技术支持:瑞秀科技
技术应用
Acta Geotechnica: An International journal for Geoengineering
Snehasis TripathyRamakrishna BagHywel R. Thomas
The Stern theory as applicable to interacting parallel clay platelet systems was used to study the compressibility behaviour of bentonites. For a constant surface electrical potential, the distribution of the total electrical charge among the Stern-layer and the Gouy-layer was found to have significant influence on the electrical potential at the midplane between clay platelets. Consideration of the Stern-layer was found to reduce the repulsive pressure or the swelling pressure between clay platelets at large platelet spacing, whereas the repulsive pressure increased significantly when the interacting Gouy-layers were pushed aside. A far greater repulsive pressure was noted for Ca-bentonite than that occurred for Na-bentonite at a platelet distance close to 1.0 nm. Similarly, strong interaction between clay platelets was noted due to suppressed Gouy-layers when the bulk fluid concentration was increased. The repulsive pressure generated due to the overlapping of the Sternlayers was found to be sensitive to changes in the specific adsorption potential, the dielectric constant of the pore fluid in the Stern-layer, and the surface electrical potential. Comparisons of the calculated pressure-void ratio relationships from the Stern theory and the Gouy-Chapman diffuse double layer theory with the experimental consolidation test results of Na- and divalent-rich bentonites showed that, in general, the Stern theory improved the predictions of pressure-void ratio relationships, particularly for pressures greater than 100 kPa; however, strong agreements were lacking in all the cases studied.