冻融环境下晶须-纤维泡沫混凝土抗压强度与孔隙结构特征

Compressive strength and pore structure characteristics of whisker-fiber foamed concrete in freeze-thaw environment

  • 摘要: 为研究冻融环境下碳酸钙晶须和玄武岩纤维泡沫混凝土的抗压强度及孔隙结构特征。对冻融环境下密度为600 kg/m3的晶须-纤维泡沫混凝土试件开展了X-CT测试与单轴压缩试验,借助Avizo软件对泡沫混凝土孔隙模型进行三维重构,基于泡沫混凝土实测孔隙率、孔径分布、孔隙分形维数等特征参数定量分析了冻融环境下泡沫混凝土孔隙结构特征参数演变规律,采用灰色关联理论分析方法探究抗压强度与孔隙结构特征参数的关联度。结果表明:随着冻融循环次数的增加,泡沫混凝土孔隙率和平均孔径不断增大,孔隙球形度逐渐降低,孔径分布更加离散,孔隙壁厚度也逐渐增大,引起抗压强度的下降;碳酸钙晶须和玄武岩纤维的加入有效抑制冻融循环的影响,减少了泡沫混凝土孔隙率和孔隙直径,对孔隙球形度有良好的改善效果,促进了孔隙结构完整性,显著提高其抗压强度;孔隙分形维数与抗压强度灰色关联度最高,处于0.831~0.854之间,说明孔隙结构的复杂程度对抗压强度有较大影响。

     

    Abstract: To investigate the compressive strength and pore structure characteristics of calcium carbonate whisker and basalt fiber foamed concrete under freeze-thaw environment. X-CT testing and uniaxial compression tests were performed on 600 kg/m3 density whisker-fiber foamed concrete specimens subjected to freeze-thaw cycles. Three-dimensional reconstruction of the pore structure in foamed concrete was achieved using Avizo software. Quantitative analysis of pore structure evolution under freeze-thaw cycles was conducted based on measured porosity, pore size distribution, pore fractal dimension, and other characteristic parameters. Grey correlation theory was employed to explore the correlation between compressive strength and pore structure parameters. The results show that with the increase of freeze-thaw cycles, the porosity and average pore size of foamed concrete increase, the sphericity of pores decreases, the pore size distribution becomes more discrete, and the thickness of pore wall increases, which leads to the decrease of compressive strength. The addition of calcium carbonate whisker and basalt fiber can effectively restrain the influence of freeze-thaw cycle, reduce the porosity and pore diameter of foamed concrete, improve the sphericity of pores, promote the integrity of pore structure and significantly improve its compressive strength; The grey correlation between pore fractal dimension and compressive strength is the highest, ranging from 0.831 to 0.854, indicating that the complexity of pore structure is right.

     

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