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Cyclic Freeze-thaw To Enhance The Stability Of Coal Tailings

机译:循环冻融提高尾矿的稳定性

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Laboratory freezing experiments were conducted to evaluate the feasibility of using cyclic freeze-thaw to enhance the surface stability of coal mine fine tailings. Undrained shear strength increased from non-measurable to 10 kPa after five cycles of freeze-thaw in tailings samples with initial moisture contents of 84% and 102%. Cyclic freeze-thaw also significantly dewatered the tailings samples. Decanting the melt water after each thaw reduced the water content of each sample by approximately 50%. A large scale one dimensional freezing test was also conducted to determine the advance of frost within the fine tailings and to understand how moisture migrates as the tailings freeze. Water was attracted to the freezing front from tailings ahead of the advancing front, decreasing the moisture content within the still unfrozen tailings. As the freezing front passed, the tailings were dewatered further at temperatures below 0 ℃. Unfrozen microscale water from within the frozen tailings was attracted to a three dimensional network of ice lenses surrounding the frozen soil peds. The laboratory experiments suggest freeze-thaw may be a technically feasible method to increase the strength and surface stability of fine tailings.
机译:进行了实验室冷冻实验,以评估使用循环冻融技术提高煤矿细尾矿表面稳定性的可行性。在初始含水量为84%和102%的尾矿样品中经过5次冻融循环后,不排水的剪切强度从不可测量的增加到10 kPa。循环冻融也使尾矿样品明显脱水。每次融化后将融化水倒掉会使每个样品的含水量减少约50%。还进行了大规模的一维冻结测试,以确定细尾矿中的霜冻进展并了解水分如何随着尾矿冻结而迁移。水从前进的前部的尾矿被吸引到冰冻的前部,从而降低了仍未冻结的尾矿中的水分含量。随着冰冻锋面的过去,尾矿在低于0℃的温度下进一步脱水。来自冷冻尾矿的未冷冻的微尺度水被吸引到围绕冷冻土壤小脚的冰晶的三维网络。实验室实验表明,冻融可能是提高细尾矿强度和表面稳定性的技术上可行的方法。

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