Analysis of the microstructure of microbial solidified sand and engineering residue based on CT scanning

Minxia Zhang , Congrui Feng , Xiang He , Ping Xu
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引用次数: 0

Abstract

A close relationship exists between the pore network structure of microbial solidified soil and its macroscopic mechanical properties. The microbial solidified engineering residue and sand were scanned by computed tomography (CT), and a three-dimensional model of the sample was established by digital image processing. A spatial pore network ball-stick model of the representative elementary volume (REV) was established, and the REV parameters of the sample were calculated. The pore radius, throat radius, pore coordination number, and throat length were normally distributed. The soil particle size was larger after solidification. The calcium carbonate content of the microbial solidified engineering residue’s consolidated layer decreased with the soil depth, the porosity increased, the pore and throat network developed, and the ultimate structure was relatively stable. The calcium carbonate content of the microbial solidified sand’s consolidated layer decreased and increased with the soil depth. The content reached the maximum, the hardness of the consolidated layer was the highest, and the development of the pore and throat network was optimum at a depth of 10–15 mm.

基于 CT 扫描的微生物固化砂和工程渣土微观结构分析
微生物固化土的孔隙网络结构与其宏观力学性能之间存在密切关系。通过计算机断层扫描(CT)对微生物固化工程渣土和砂土进行扫描,并通过数字图像处理建立了样品的三维模型。建立了代表性基本体积(REV)的空间孔隙网络球棍模型,并计算了样品的 REV 参数。孔隙半径、喉管半径、孔隙配位数和喉管长度均呈正态分布。固化后土壤粒径变大。微生物固化工程渣土固结层的碳酸钙含量随土层深度的增加而降低,孔隙度增加,孔隙和喉道网络发达,最终结构相对稳定。微生物固化砂固结层的碳酸钙含量随土层深度的增加而减少,但含量达到最大值时,硬度增加。在土层深度为 10-15 mm 时,碳酸钙含量达到最大值,固结层的硬度最高,孔隙和喉网的发育达到最佳状态。
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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