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曾召田, 付慧丽, 吕海波, 梁珍, 于海浩. 水泥胶结钙质砂热传导特性及微观机制[J]. 岩土工程学报, 2021, 43(12): 2330-2338. DOI: 10.11779/CJGE202112021
引用本文: 曾召田, 付慧丽, 吕海波, 梁珍, 于海浩. 水泥胶结钙质砂热传导特性及微观机制[J]. 岩土工程学报, 2021, 43(12): 2330-2338. DOI: 10.11779/CJGE202112021
ZENG Zhao-tian, FU Hui-li, LÜ Hai-bo, LIANG Zhen, YU Hai-hao. Thermal conduction characteristics and microcosmic mechanism of cement-cemented calcareous sand[J]. Chinese Journal of Geotechnical Engineering, 2021, 43(12): 2330-2338. DOI: 10.11779/CJGE202112021
Citation: ZENG Zhao-tian, FU Hui-li, LÜ Hai-bo, LIANG Zhen, YU Hai-hao. Thermal conduction characteristics and microcosmic mechanism of cement-cemented calcareous sand[J]. Chinese Journal of Geotechnical Engineering, 2021, 43(12): 2330-2338. DOI: 10.11779/CJGE202112021

水泥胶结钙质砂热传导特性及微观机制

Thermal conduction characteristics and microcosmic mechanism of cement-cemented calcareous sand

  • 摘要: 南海岛礁建设中,钙质砂地基面临的高温环境问题需要全面掌握钙质砂热传导性能的演变规律。基于热探针法测定了不同试验条件下水泥胶结钙质砂的导热系数λ,探讨了水灰比W/C、养护时间t、胶结程度(水泥掺量Ps)、含水率w等因素对其产生的影响规律,发现水泥胶结钙质砂的导热系数λ随养护龄期t的增加呈现出先急剧增大而后缓慢减小的变化规律,随水泥掺量Ps、含水率w的增加而递增,随水灰比W/C的增加反而递减;在此基础上,利用电镜扫描和压汞试验从微观角度解释了水泥胶结钙质砂导热系数随胶结程度的变化趋势:水泥胶结钙质砂内微孔隙大小、数量的变化从本质上决定了其宏观热传导特性,凝胶状水化产物连续填充其内部孔隙,引起其孔隙率降低,改善砂样内部传热,宏观表现为其导热系数λ随着胶结程度的增加而递增。

     

    Abstract: In the construction of islands and reefs in the South China Sea, the high-temperature environment problem of calcareous sand foundation requires a comprehensive understanding of the evolution laws of calcareous sand thermal conductivity. Based on the thermal probe method, the thermal conductivity of cement-cemented calcareous sand under different test conditions is determined, and the variation laws of the influence factors such as water-cement ratio, curing period, cementing degree (cement content) and moisture content on the thermal conductivity are discussed. It is found that the thermal conductivity of the cement-cemented calcareous sand increases sharply firstly and then decreases slowly with the increasing curing period. At the same time, the thermal conductivity increases with the increase of the cement content and moisture content, and decreases with the increase of the water cement ratio. On this basis, the trend of thermal conductivity of the cement-cemented calcareous sand with the degree of cementation is explained by the scanning electron microscope and mercury intrusion porosimetry tests. The result shows that the macroscopic thermal conduction characteristics of the cement-cemented sand are determined by the variation of size and quantity of its micro-pores. The gelatinous hydration products continuously fill the internal pores of cemented sand, causing a reduction in porosity and improving the internal heat transfer of the sand sample. At the macro level, the thermal conductivity increases with the degree of cementation.

     

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