The influence of lithology on permeability reduction process by MICP technology in fracture: comparative study between limestone and granite
摘要
In this study, the microbial-induced calcium carbonate precipitation (MICP) technology was used to grout and reduce the permeability of the fissures in limestone and granite. The effectiveness of the MICP under different conditions in permeability reduction in different lithologies were comprehensively investigated through lab tests. Three influential factors of interests include the grouting flow rate, the concentration of the cementing solution, and the concentration of the bacterial solution (OD600). The indications of the effectiveness of the permeability reduction investigated in this study include the amount of CaCO3 generated, the area proportion of the generated CaCO3, and the thickness of the generated CaCO3, the accumulation density in the fissures and the filling rate. It was found that the effect of lithology on the permeability reduction effectiveness is more significant under lower grouting flow rates, lower cementing solution concentrations, and higher bacterial solution concentrations. The better compatibility between the limestone fissures and the CaCO3 particles leads to a faster CaCO3 deposition rate compared with that in the granite, resulting in more CaCO3 accumulation, the permeability in limestone fractures is lower than that in granite fractures. And the lithology difference makes the planar and spatial accumulation forms of the generated CaCO3 in the two fissures different, which is reflected in the proportion of the coverage area, the accumulation thickness and the accumulation density. In addition, a fitting and comparative analysis was carried out on the generated CaCO3 in the fissures of limestone and granite, and it was found that the proportion of the CaCO3 coverage area has a significant impact on the permeability reduction effect in the limestone fissures; while the mass of CaCO3 has a significant impact on the permeability reduction effect in the granite fissures.