Effect of thermal cycles on sand-concrete interface under constant shear stress

Mouadh Rafai, A. Tang, Thibault Badinier, Jean de Sauvage, Diana Salciarini
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Abstract

Energy geostructures provide a profitable solution for structural support as well as the heating and cooling of buildings. However, their activation can produce in structure and its surrounding soil thermally-induced stresses and strains with a crucial role played by the soil-structure interface which is the thin layer that transmits the thermal and mechanical loads. In the present work, the thermo-mechanical behaviour of the soil–structure interface is investigated using a temperature-controlled direct shear box. Tests were conducted on loose and dense sands in contact with a concrete plate representing the structure's surface. After applying the normal stress (25, 50, or 100 kPa), a shear stress was increased up to 45% of the shear strength. This stress state was then maintained while 20 cycles of temperature varying between 13 °C and 34 °C at the soil-concrete interface were applied. The obtained experimental results reveal that temperature cycles lead to irreversible cumulative displacements in both normal and shear directions. These displacements were found to be more significant in loose sand compared to dense sand. Additionally, under higher stress levels, greater displacements were observed for both soil densities.
热循环对恒定剪应力下砂-混凝土界面的影响
能源土工结构为结构支撑以及建筑物的供暖和制冷提供了一个有利的解决方案。然而,它们的激活会在结构及其周围土壤中产生热应力和应变,而土壤-结构界面是传递热负荷和机械负荷的薄层,起着至关重要的作用。在本研究中,使用温控直接剪切箱对土壤-结构界面的热机械性能进行了研究。试验在与代表结构表面的混凝土板接触的松散和致密砂土上进行。在施加法向应力(25、50 或 100 kPa)后,剪应力增加到剪切强度的 45%。然后保持这种应力状态,同时在土壤-混凝土界面上施加 20 个温度周期,温度在 13 °C 和 34 °C 之间变化。实验结果表明,温度循环会导致法向和剪切方向的不可逆累积位移。这些位移在松散砂土中比在致密砂土中更为显著。此外,在较高应力水平下,两种密度的土壤都出现了较大的位移。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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