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首页> 外文期刊>Bulletin of engineering geology and the environment >Strength improvement in silty clay by microbial‑induced calcite precipitation
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Strength improvement in silty clay by microbial‑induced calcite precipitation

机译:微生物诱导的方解石沉淀的粉质粘土的力量改善

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摘要

The application of MICP (microbial-induced calcite precipitation) to clays has been restricted due to their low permeability and small pore size, which limit bacterial mobility. The authors proposed an injection method for introducing solutions into a silty clay for MICP in the pore space. Test results showed that injecting equal volumes of bacterial solution and cementation solution resulted in 200% soil strength. The soil strength was estimated using a miniature cone penetration test, which provided a continuous cone resistance profile. The strength profile of the improved samples clearly showed that the peak strength occurred at the top portion of the samples, which implied that bacteria and urease traveled through the soil and MICP occurred. After the injection, 70-90% of the soil volume was improved through MICP. An analysis of drainage solutions after a few days showed calcite precipitation, which indicated that the urease reaction was still active in the drainage. These results can conclude that MICP is applicable to silty clays with similar properties, such as low permeability, low pH, and small pore size.
机译:由于它们的低渗透性和小孔径,因此限制了MICP(微生物诱导的方解石沉淀)对粘土的应用,这限制了细菌迁移率。作者提出了一种注射方法,用于将溶液引入孔隙空间中MICP的粉冻粘土。测试结果表明,注射等体积的细菌溶液和胶结溶液导致200%的土壤强度。使用微型锥形渗透试验估计土壤强度,其提供连续的锥形电阻曲线。改进样品的强度剖面清楚地表明,样品的顶部发生的峰强度发生,这暗示细菌和释放通过土壤和麦克麦普发生的释放。注射后,通过MICP改善了70-90%的土壤体积。几天后排水溶液的分析显示方解石沉淀,表明脲酶反应仍然活跃在排水中。这些结果可以得出结论,MICP适用于具有相似性质的粉冻粘土,例如低渗透性,低pH和小孔径。

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