A temperature gradient test system for investigating thermo-mechanical responses of containment materials of underground storage facilities

Wei Wu , Dazhao Lu , Alessandro Romagnoli
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引用次数: 1

Abstract

Underground energy storage is a promising option for the global ambition of moving towards carbon neutrality. To achieve safe and reliable energy storage in underground caverns, it is essential to understand the contributions of thermal and mechanical loads to the deformation of containment materials (e.g., concrete and geomaterials) and to forecast potential risks related to unexpected failure of these materials. A temperature gradient test system is developed to investigate the thermo-mechanical responses of containment materials under simulated temperature gradient and earth pressure conditions. The test system has advantages of establishing a temperature gradient of over 400 ​°C/m across a large-scale specimen and examining the resulting strain based on the digital image correlation analysis. This study sheds light on 3 typical applications of the test system to examine the thermal and mechanical responses of intact limestone, flawed limestone, and fractured concrete. The results demonstrate that the mechanical load mainly controls the strain evolution of the intact limestone, while the thermal load strongly affects the strain evolution around the circular hole. The failure pattern of concrete primarily influences the mechanically induced strain, and the thermally induced strain is insensitive to the concrete failure. This test system can be modified and upgraded to study various research topics related to underground energy storage.

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用于研究地下储存设施安全壳材料热机械响应的温度梯度测试系统
地下储能是实现碳中和全球目标的一个很有前途的选择。为了在地下洞室中实现安全可靠的储能,必须了解热负荷和机械负荷对安全壳材料(如混凝土和岩土材料)变形的影响,并预测与这些材料意外失效相关的潜在风险。开发了一个温度梯度测试系统来研究安全壳材料在模拟温度梯度和土压力条件下的热机械响应。该测试系统具有建立超过400的温度梯度的优点​°C/m,并基于数字图像相关性分析检查产生的应变。本研究揭示了测试系统的3个典型应用,以检查完整石灰石、有缺陷石灰石和断裂混凝土的热响应和力学响应。结果表明,机械载荷主要控制完整石灰石的应变演化,而热载荷强烈影响圆孔周围的应变演化。混凝土的破坏模式主要影响机械应变,而热应变对混凝土的破坏不敏感。该测试系统可以进行修改和升级,以研究与地下储能相关的各种研究课题。
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CiteScore
2.40
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