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Hydraulic Binder Stabilised Near-Surface Soils Exposed to Cold Curing Climate and Freeze-Thaw Cycles

机译:暴露于冷固化气候和冻融循环的水硬性粘合剂稳定的近地表土壤

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Fine-grained soils are normally not suitable as subbase in road, railway, and other largescale constructions due to their compressibility, low shear strength, and/or frost susceptibility. Common procedures to improve the subbase are soil replacement, lightweight fill, or insulation. The engineering properties of fine-grained soils can also be improved in situ by mixing them with hydraulic binders. A SWOT analysis based on literature study indicates that near-surface soil stabilisation has opportunities as a method. However, one major weakness of the method of near-surface soil stabilisation is the question of strength reduction as a consequence of freeze-thaw cycles. It is unclear how near zero curing temperature followed by freeze-thaw cycles, representing conditions in northern countries, might influence the curing as well as the ultimate strength of the stabilised soil. The impact of freeze-thaw cycles on the engineering properties of stabilised soils was investigated with focus on the reduction of strength. In these laboratory investigations, curing took place at temperatures of +4℃ with freeze-thaw cycles interrupting the curing period. Variations in the laboratory set up contained different soil types, binders, binder contents, and curing times before the freeze-thaw cycles. The results show, that the strength increases with curing time in spite of the near zero temperature; but for one binder, a strength-over-time development with decrease after 90 days has been observed in the cold curing conditions in the experiments. In general, the strength gained during curing was reduced by freeze-thaw cycles. However, strength was regained during curing afterwards, and reached a higher level of strength than the original soil before stabilisation.
机译:细粒土壤由于其可压缩性,低剪切强度和/或易受霜冻性影响,因此通常不适合用作公路,铁路和其他大型建筑的基层。改善路基的常用程序是土壤置换,轻质填充或保温。细粒土壤的工程性能也可以通过与水硬性粘结剂混合原位改善。基于文献研究的SWOT分析表明,近地表土壤稳定化是一种方法。然而,近地表土壤稳定方法的一个主要缺点是由于冻融循环而导致强度降低的问题。目前尚不清楚接近零的固化温度以及随后的冻融循环(代表北方国家的情况)如何影响固化以及稳定土的极限强度。研究了冻融循环对稳定土的工程特性的影响,重点是强度的降低。在这些实验室研究中,固化在+ 4℃的温度下进行,冻融循环中断了固化时间。实验室设置的变化包含不同的土壤类型,粘合剂,粘合剂含量和冻融循环之前的固化时间。结果表明,尽管温度接近零,但强度随固化时间的增加而增加。但是对于一种粘合剂,在冷固化条件下的实验中观察到强度随时间的发展在90天后降低。通常,通过冻融循环会降低固化过程中获得的强度。然而,强度在固化后恢复了,并且达到了比稳定前的原始土壤更高的强度水平。

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