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Strength properties of ultra-soft kaolin

机译:超软高岭土的强度特性

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Geotechnical design considerations for offshore pipelines, foundations, and submarine slides involve assessment of the strength of fine-grained soils and the degradation of that strength with disturbance and remoulding. For offshore pipelines and slides, the relevant strength may be very low (a few kilopascals or lower), relating to near-surface soils and high levels of remoulding including the entrainment of additional water. It is commonly acknowledged that soils exhibit a loss of strength when disturbed, but it is not clear how the degradation properties vary with liquidity index. To address this uncertainty, this paper describes a series of centrifuge tests on kaolin samples consolidated from slurries with an initial voids ratio of 4.0. A total of 81 cyclic T-bar tests were conducted in samples with shear strengths ranging from 0.08 to 1.7 kPa (reflecting different stages of consolidation and in situ total stresses). Large-strain consolidation numerical analyses were used to assist the interpretation of the T-bar test results. The results demonstrate that the soil ductility (a parameter controlling the rate of strength degradation) can be linearly correlated to the liquidity index. The proposed ductility-liquidity index correlation is subsequently coupled with a previously published sensitivity-liquidity index relationship for natural clays to establish a model for the strain-softening behaviour observed in a T-bar test as a function of consolidation. In turn, because the sensitivity is a function of the liquidity index, the intact soil strength is linked to the remoulded strength obtained from laboratory (e.g., fall cone or miniature vane test) and simple index tests. These provide an improved basis to characterize softening effects for inclusion in simulations of submarine slide runout and models for soil-structure interactions that involve intense remoulding.
机译:海上管线,地基和海底滑坡的岩土工程设计考虑因素包括评估细粒土的强度以及该强度随扰动和重塑而降低的程度。对于近海管道和滑道,相关强度可能非常低(几千帕斯卡或更低),这与近地表土壤和大量重塑(包括夹带额外的水)有关。人们普遍认为,土壤在受到干扰时会表现出强度的损失,但尚不清楚降解特性如何随流动性指数而变化。为了解决这种不确定性,本文介绍了一系列对从初始空隙比为4.0的浆液固结的高岭土样品进行的离心测试。在抗剪强度范围从0.08到1.7 kPa(反映固结的不同阶段和现场总应力)的样品中进行了总共81次循环T型杆测试。大应变固结数值分析被用来帮助解释T型杆的测试结果。结果表明,土壤延性(控制强度下降速率的参数)可以与流动性指数线性相关。所提出的延展性-流动性指数相关性随后与先前发布的天然粘土的敏感性-流动性指数关系相结合,建立了在T型杆试验中观察到的作为固结函数的应变软化行为的模型。继而,由于灵敏度是流动性指数的函数,因此完整的土壤强度与实验室(例如跌落锥或微型叶片测试)和简单指数测试获得的重塑强度相关。这些为表征软化效果提供了改进的基础,可用于模拟海底滑坡跳动和涉及强烈重塑的土壤与结构相互作用的模型。

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