Han Zhiguang, Xiao Jianzhang, Wei Yingqi
Department of Civil Engineering, Henan University, Kaifeng 475004, China.
State Key Laboratory of Simulation and Regulation of Water Cycle in River Basin, China Institute of Water Resources and Hydropower Research, Beijing 100048, China.
Materials (Basel). 2022 Sep 2;15(17):6102. doi: 10.3390/ma15176102.
Calcium carbonate induced by microorganisms can quickly fill and cement sand particles, thereby effectively reducing the potential for the liquefaction of sand. This process could represent a new green approach to the liquefaction treatment of saturated sand and has good prospects for application. However, owing to the diversity of microbial activities and the heterogenous spatiotemporal distribution of bacterial nutrient seepage in sandy soil foundations, the resultant complex distribution of calcium carbonate deposition in a sandy soil foundation can lead to differences in solidification strength and improvement effect. To understand the influence of earthquake action on the liquefaction resistance of saturated sand treated by microorganisms, and to evaluate the effect of microbial technology on sand liquefaction prevention under dynamic load, this study simulated the dynamic stress conditions of saturated sand under shear waves, using the world's first centrifuge shaking table (R500B), which realizes horizontal and vertical two-way vibration. On the basis of spatial heterogeneity of microbial mineralization after centrifuge shaking table tests, the effect of microbial strengthening on liquefied sand was analyzed, and the spatial distribution of calcium carbonate mineralization was examined. The results showed that the distribution of microorganisms in the solidified soil exhibited obvious spatial heterogeneity with a significant edge effect. Although microbial mineralization effectively improved the liquefaction resistance of saturated sand, a sudden change in the process of calcium carbonate deposition altered the cementation of the sand with depth. Moreover, the curing strength had obvious complexity and uncertainty that directly affected the shear stiffness of the soil under dynamic load, and this constitutes one of the reasons for the degradation of shear stiffness of sand during liquefaction. The derived conclusions could be used as a reference for engineering applications of microbial treatment of a liquefiable sandy soil foundation.
微生物诱导生成的碳酸钙能够迅速填充并胶结砂粒,从而有效降低砂土液化的可能性。这一过程可能代表了一种处理饱和砂土液化问题的新型绿色方法,具有良好的应用前景。然而,由于微生物活动的多样性以及细菌养分在砂土基础中渗流的时空分布不均,导致砂土基础中碳酸钙沉积物的复杂分布会造成固化强度和改良效果的差异。为了解地震作用对微生物处理后的饱和砂土抗液化性能的影响,并评估微生物技术在动荷载作用下对砂土液化防治的效果,本研究利用世界首台实现水平和垂直双向振动的离心机振动台(R500B),模拟了饱和砂土在剪切波作用下的动应力条件。基于离心机振动台试验后微生物矿化的空间异质性,分析了微生物强化对液化砂土的影响,并研究了碳酸钙矿化的空间分布。结果表明,固化土中微生物的分布呈现出明显的空间异质性和显著的边缘效应。尽管微生物矿化有效提高了饱和砂土的抗液化性能,但碳酸钙沉积过程中的突然变化改变了砂土随深度的胶结情况。此外,固化强度具有明显的复杂性和不确定性,直接影响了动荷载作用下土体的剪切刚度,这也是砂土液化过程中剪切刚度退化的原因之一。所得结论可为可液化砂土基础微生物处理的工程应用提供参考。