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首页> 外文期刊>Advances in Cement Research >Depth evolution of mechanical properties of fugitive dust cemented by microbe cement based on carbon dioxide capture and utilisation
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Depth evolution of mechanical properties of fugitive dust cemented by microbe cement based on carbon dioxide capture and utilisation

机译:基于二氧化碳捕获和利用的微骨水泥粘合粘粘械机械性能深度演变

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摘要

Fugitive dust, which was cemented with microbe cement based on carbon dioxide capture and utilisation, was prepared and the evolution of mechanical properties over the sample depth was investigated. The microstructure of samples at different depths was analysed by X-ray diffraction, Fourier transform infrared spectroscopy and scanning electron microscopy. The calcite content and hardness of samples at different depths were also verified. Three-dimensional (3D) reconstruction evolution and cross-section evolution of porosity at different depths were demonstrated by X-ray computed tomography. The experimental results indicate that calcite could be formed at different depths with the use of microbe cement. Compared with the structure of the lower region of the sample, fugitive dust particles cemented with microbe cement in the upper region were found to be more dense, of lower porosity and with more calcite formed. The calcite content and hardness significantly decreased with an increase in sample depth: at 0, 5, 10, 15 and 20 mm, the respective calcite content was 10.51%, 8.32%, 4.93% and 1.70% and the hardness was 18.2 GPa, 17.1 GPa, 10.9 GPa and 3.6 GPa. 3D reconstructions and cross-section evolutions of porosity at different depths indicate that the inner structure of the sample was not uniform, with the structure of the upper region better than that of the sample bottom. With an increase in sample depth, pores and cracks in the cross-section significantly increased.
机译:制备了基于二氧化碳捕获和利用的微细水泥粘合的疲惫粉尘,并研究了样品深度上的机械性能的演化。通过X射线衍射,傅里叶变换红外光谱和扫描电子显微镜分析不同深度时的样品的微观结构。还验证了不同深度在不同深度的方解石含量和硬度。通过X射线计算断层扫描证明了不同深度孔隙率的三维(3D)重建演化和横截面演变。实验结果表明,通过使用微泥浆可以在不同深度形成方解石。与样品下部区域的结构相比,发现粘附在上部区域中的微骨水泥粘合的逃逸粉末颗粒更致密,孔隙率低,形成更多的方解石。通过样品深度的增加,方解石含量和硬度显着降低:在0,5,10,15和20mm,相应的方解石含量为10.51%,8.32%,4.93%和1.70%,硬度为18.2GPa,17.1 GPA,10.9 GPA和3.6 GPA。不同深度的三维重建和孔隙率的横截面演化表明样品的内部结构不均匀,上部区域的结构比样品底部更好。随着样品深度的增加,横截面中的孔隙和裂缝显着增加。

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