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Examining the Liquefaction Resistance of Lightly Cemented Sands Using Microbially Induced Calcite Precipitation (MICP)

机译:用微生物诱导方解石沉淀法(MICP)检查轻质水泥砂的抗液化性

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Microbially induced calcite precipitation (MICP), or bio-cementation, is a bio-mediated, environmentally-conscious soil improvement technology that can improve the engineering properties of granular soils through the precipitation of calcium carbonate (CaCO_3) on soil particle surfaces and contacts. While past studies have shown the potential of bio-cementation to improve the resistance of granular soils to earthquake-induced soil liquefaction, the spectrum of behaviors during the transition from the uncemented to lightly cemented conditions has remained poorly characterized. In this study, a series of direct simple shear tests were performed to improve our understanding of the effect of CaCO_3 bio-cementation on the liquefaction triggering and post-triggering strain accumulation behavior of loose sands. A poorly-graded Ottawa F-65 sand material was treated to varying degrees of very light bio-cementation and subjected to undrained cyclic shearing events. All specimens were cemented and sheared under a vertical effective stress of 100 kPa and subjected to cyclic stress ratios (CSR) of 0.1 and 0.2. During these tests, shear wave velocity (V_s) measurements were completed to non-destructively monitor cementation progression and degradation during shearing. Results suggest that even very light levels of bio-cementation (△V_S ≈ 0 to 100 m/s) can significantly increase the number of cycles needed to trigger soil liquefaction (3% single amplitude shear strain), e.g., a 10-fold increase in the number of cycles needed to trigger liquefaction was observed when V_s values were increased by only 25 m/s. Despite this significant improvement in small-strain pre-triggering behavior, little improvement was observed with respect to strain accumulation before and after initial triggering. While additional testing is needed, results from this study can improve our understanding of the behavior of lightly bio-cemented and naturally-cemented soils subjected to earthquake-induced undrained cyclic loading.
机译:微生物诱导的方解石沉淀(MICP)或生物胶结是一种生物介导的,具有环境意识的土壤改良技术,可以通过在土壤颗粒表面和接触面上沉淀碳酸钙(CaCO_3)来改善粒状土壤的工程特性。尽管过去的研究表明,生物固结有可能改善粒状土壤对地震引起的土壤液化的抵抗能力,但从未固结到轻固结条件过渡期间的行为谱仍然没有得到很好的描述。在这项研究中,进行了一系列直接的简单剪切试验,以增进我们对CaCO_3生物胶结对松散砂土液化触发和触发后应变累积行为的影响的理解。对等级不佳的渥太华F-65砂料进行了不同程度的轻质生物固结处理,并进行了不排水的循环剪切事件。在100 kPa的垂直有效应力下,将所有试样固结并剪切,并承受0.1和0.2的循环应力比(CSR)。在这些测试中,完成了剪切波速度(V_s)的测量,以非破坏性地监测剪切过程中的胶结过程和降解。结果表明,即使是非常轻量的生物固结(△V_S≈0至100 m / s)也可以显着增加触发土壤液化所需的循环次数(单振幅剪切应变为3%),例如增加10倍。当V_s值仅增加25 m / s时,观察到了触发液化所需的循环次数。尽管小应变的预触发行为有了显着的改善,但是在初始触发之前和之后,应变累积方面几乎没有改善。尽管还需要进行额外的测试,但这项研究的结果可以增进我们对遭受地震诱发的不排水循环荷载的轻质生物胶结和天然胶结土壤的行为的了解。

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