Department of Civil and Environmental Engineering, The Hong Kong University of Science and Technology, Hong Kong; Department of Civil and Environmental Engineering, Shantou University, China.
Department of Civil and Environmental Engineering, The Hong Kong University of Science and Technology, Hong Kong; Illinois Sustainable Technology Centre, University of Illinois at Urbana Champaign, United States of America.
Sci Total Environ. 2022 Sep 10;838(Pt 3):156493. doi: 10.1016/j.scitotenv.2022.156493. Epub 2022 Jun 6.
Biochar amended clay layer has emerged as a sustainable hydraulic barrier for hazardous municipal waste containment system. The effects of pore fluid salinity on soil shrinkage and water retention characteristics of biochar amended clay are unknown. This study aims to investigate the behavior of soil shrinkage and water retention of biochar amended kaolin under different pore fluid salinity. A series of volumetric shrinkage and water retention tests were conducted on biochar amended kaolin in sodium chloride solution at initial concentrations of 1 %, 5 %, and 10 %. Biochar addition increased the shrinkage limit and minimum void ratio of kaolin by up to 17 % and 11 %, respectively. Air entry value of kaolin increased by 6-88 times with an increase in pore fluid salinity, caused by interparticle aggregation. Micrographs showed that biochar intrapore was filled by kaolin particles, partially hindering the interparticle aggregation of clay in the salt solution. Biochar addition lowered zeta potential on the surface of kaolin particles by 50-75 %, indicating that the immobilisation of excess sodium ions was achieved by biochar. Correspondingly, osmotic suction of pore fluid decreased by 21-64 % due to biochar's ion absorption. The findings highlighted that biochar addition to kaolin specimens minimises NaCl-induced soil shrinkage and reduces the pore fluid salinity. This study indicates that biochar could be potentially helpful for desalinisation and mitigating volumetric change issues for geo-environmental infrastructures.
生物炭改良黏土层作为一种可持续的水力屏障,用于危险城市废物封存系统。孔隙流体盐度对生物炭改良黏土的土壤收缩和保水特性的影响尚不清楚。本研究旨在研究不同孔隙流体盐度下生物炭改良高岭土的土壤收缩和保水特性。在初始浓度为 1%、5%和 10%的氯化钠溶液中,对生物炭改良高岭土进行了一系列体积收缩和保水试验。生物炭的添加使高岭土的收缩极限和最小空隙比分别增加了 17%和 11%。随着孔隙流体盐度的增加,空气进气值增加了 6-88 倍,这是由于颗粒间的聚集。显微照片显示,生物炭内部被高岭土颗粒填充,部分阻碍了盐溶液中粘土的颗粒间聚集。生物炭的添加使高岭土颗粒表面的动电电位降低了 50-75%,表明生物炭实现了过量钠离子的固定。相应地,由于生物炭的离子吸收,孔隙流体的渗透压降低了 21-64%。研究结果表明,生物炭的添加可以最小化 NaCl 引起的土壤收缩,并降低孔隙流体盐度。本研究表明,生物炭可能有助于脱盐和减轻地质环境基础设施的体积变化问题。