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Laboratory test study on the effect of freeze-thaw cycles on strength and hydraulic conductivity of high water content stabilized dredged sediments

机译:冻融循环对高含水量稳定疏ged沉积物强度和水力传导率影响的室内试验研究

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Dredged sediments with initial water contents between 200% and 400% were treated with single and composite binders. Samples were subjected to open and semi-closed freeze-thaw (f-t) cycles to investigate the impact of f-t cycling on hydraulic conductivity (HC) and unconfined compressive strength (UCS). A grace period (GP) for thaw consolidation is included to assess healing potential of the affected stabilized mass. Findings of this study show that the impact of f-t cycles depends on initially achieved UCS and HC values prior to the f-t cycling and time of testing after f-t cycles. The HC of specimens with an initial UCS value of 87 kPa increased with number of f-t cycles. The UCS values decreased in the range of 50%-80% when specimens were tested directly after the thaw period and values decreased in the range of 14%-60% when specimens were tested at the end of the GP. The HC of specimens with an initial UCS value of 299 kPa remained almost the same. These samples experienced permanent loss in the UCS values, irrespective of time of testing. Detrimental effects of the freezing action on the UCS were greater under semi-closed than open freezing conditions.
机译:初始含水量在200%至400%之间的疏sediment沉积物用单一和复合粘合剂处理。对样品进行开放和半封闭的冻融(f-t)循环,以研究f-t循环对水力传导率(HC)和无侧限抗压强度(UCS)的影响。包括融化合并的宽限期(GP),以评估受影响的稳定肿块的愈合潜力。这项研究的结果表明,f-t周期的影响取决于f-t周期之前最初获得的UCS和HC值以及f-t周期之后的测试时间。 UCS初始值为87 kPa的样品的HC随着f-t循环次数的增加而增加。在解冻期后立即对样品进行测试时,UCS值降低了50%-80%,而在GP结束时对样品进行测试时,UCS值降低了14%-60%。 UCS初始值为299 kPa的样品的HC几乎保持不变。无论测试时间长短,这些样品的UCS值都会永久丢失。在半封闭条件下,冷冻作用对UCS的不利影响要大于在开放条件下的冷冻作用。

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