Effect of Freeze–Thaw and Wetting–Drying Cycles on the Hydraulic Conductivity of Modified Tailings

Longlong Meng, Liangxiong Xia, Min Xia, Shaokai Nie, Jiakai Chen, Wenyuan Wang, Aifang Du, Haowen Guo, Bate Bate
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Abstract

Mine tailings have shown viability as the fine–grained layer in a capillary barrier structure for controlling acid mine drainage in a circular economy. Their saturated hydraulic conductivities (ksat) under wetting–drying cycles and freeze–thaw cycles remain unexplored. In this study, modified tailings with a weight ratio of 95:5 (tailings/hydrodesulfurization (HDS) clay from waste–water treatment) and an initial water content of 12% were used. The ksat of specimens was measured after up to 15 wetting–drying cycles, each lasting 24 h, with a drying temperature of 105 °C. The ksat for wetting–drying cycles decreased from 3.9 × 10−6 m/s to 9.5 × 10−7 m/s in the first three cycles and then stabilized in the subsequent wetting–drying cycles (i.e., 5.7 × 10−7 m/s–6.3 × 10−7 m/s). Increased fine particles due to particle breakage are the primary mechanism for the ksat trend. In addition, the migration of fines and their preferential deposition near the pore throat area may also promote this decreasing trend through the shrinking and potentially clogging–up of pore throats. This could be explained by the movement of the meniscus, increased salinity, and, subsequently, the shrinkage of the electrical diffuse layer during the drying cycle. Similar specimens were tested to measure ksat under up to 15 freeze–thaw cycles with temperatures circling between −20 °C and 20 °C at 12 h intervals. Compared to the untreated specimen (i.e., 3.8 × 10−6 m/s), the ksat after three freeze–thaw cycles decreased by 77.6% (i.e., 8.5 × 10−7 m/s) and then remained almost unchanged (i.e., 5.6 × 10−7 m/s–8.9 × 10−7 m/s) in subsequent freeze–thaw cycles. The increased fine grain content (i.e., 3.1%) can be used to explain the decreased ksat trend. Moreover, the migration of fines toward the pore throat area, driven by the advancing and receding of ice lens fronts and subsequent deposition at the pore throat, may also contribute to this trend.
冻融循环和润湿-干燥循环对改良尾矿导水性的影响
矿山尾矿作为毛细管屏障结构中的细粒层,在循环经济中控制酸性矿山排水方面显示出可行性。但它们在湿润-干燥循环和冻融循环下的饱和导水性(ksat)仍有待探索。本研究使用了重量比为 95:5(尾矿/废水处理产生的脱硫粘土)、初始含水量为 12% 的改良尾矿。试样的 ksat 在湿润-干燥循环中最多测量 15 次,每次持续 24 小时,干燥温度为 105 °C。湿润-干燥循环的 ksat 在前三个循环中从 3.9 × 10-6 m/s 降至 9.5 × 10-7 m/s,然后在随后的湿润-干燥循环中趋于稳定(即 5.7 × 10-7 m/s-6.3 × 10-7 m/s)。颗粒破碎导致的细颗粒增加是造成 ksat 趋势的主要机制。此外,细颗粒的迁移及其优先沉积在孔隙喉部附近,也可能通过孔隙喉部的收缩和潜在堵塞而促进这种下降趋势。这可能是由于半月板的移动、盐度的增加以及随后在干燥周期中电扩散层的收缩造成的。对类似的试样进行了测试,以测量在 -20 °C 和 20 °C 之间以 12 小时为间隔进行多达 15 次冻融循环时的 ksat。与未经处理的试样(即 3.8 × 10-6 m/s)相比,经过三个冻融循环后的 ksat 下降了 77.6% (即 8.5 × 10-7 m/s),在随后的冻融循环中几乎保持不变(即 5.6 × 10-7 m/s-8.9 × 10-7 m/s)。细粒含量的增加(即 3.1%)可以用来解释 ksat 下降的趋势。此外,冰透镜前沿的前进和后退以及随后在孔隙喉部的沉积也可能导致细粒向孔隙喉部迁移。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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