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Temperature effects on the in-situ mechanical response of clayey soils around an energy pile evaluated by CPTU

机译:CPTU评估的能量桩周围粘土土原位机械响应的温度效应

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Thermomechanical behaviour of clay has been widely investigated by well-controlled laboratory experiments, while in-situ test of thermal effects on soil is rare. The piezocone penetration test (CPTU) is first used in this study to directly evaluate the temperature effects under in-situ stress condition. A full-scale precast high strength concrete (PHC) pile was utilized as the heat source and a series of CPTU were conducted in adjacent layered clays after monotonic heating and thermal cycle. The results show that unprecedented temperature elevation leads to an apparent reduction of soil strength in all soil layers; this degradation was alleviated after the thermal cycle. After exposure to a higher temperature, the normally consolidated soil was improved even when tested at a lower elevated temperature; whereas, the overconsolidated soil could nearly recovered to the pre-heated value. The measured pore pressure (u(2)) also decreased after heating indicating a more overconsolidated or dilatant behaviour during shearing. By comprehensively considering the in-situ responses, the in-situ soils were believed to be unloaded by the thermally induced pore fluid pressurization and densified after cyclic thermal loading. Finally, a hypothesis is proposed to qualitatively explain the thermomechanical responses of in-situ soil in the framework of critical state soil mechanics theory.
机译:粘土的热机械行为已被受良好控制的实验室实验普遍研究,而原位试验对土壤的热效应是罕见的。首先在本研究中使用压区渗透试验(CPTU),直接评估原位应力条件下的温度效应。使用全刻度预制高强度混凝土(PHC)桩作为热源,在单调加热和热循环后,在相邻的分层粘土中进行一系列CPTU。结果表明,前所未有的温度升高导致所有土层中的土壤强度明显降低;在热循环之后减轻了这种降解。在暴露于较高温度后,即使在较低的温度下测试时,即使在较低的温度下测试也会改善通常固结的土壤;鉴于过度覆盖的土壤几乎可以回收到预热值。在加热后,测量的孔隙压力(U(2))也降低,表示在剪切期间更过于占用或稀释剂行为。通过全面考虑原位的反应,据信原地土壤被热诱导的孔隙流体加压卸载,并在环状热负荷后致密化。最后,提出了一个假设,以定性地解释临界状态土工程理论框架中原位土壤的热机械响应。

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