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Effects of Microbial Induced Calcite Precipitation on Bentonite Cracking Remediation

机译:微生物诱导方解石沉淀对膨润土裂解修复的影响

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This paper describes a preliminary study of the effects of microbial induced calcite precipitation (MICP) on the desiccation cracking behaviors of bentonite. The drying shrinkage of bentonite mixed with bacteria and cementation medium is monitored in the petri dish under controlled temperature and relative humidity conditions. Three control groups are also monitored, in which bentonites are mixed with live bacteria + cementation medium without CaCl_2, dead bacteria + cementation medium, and dead bacteria + cementation medium without CaCl_2, in order to study the influence of MICP process and microbial activity on soil desiccation cracking. Scanning electron microscope images show bacteria survive on the surface of bentonite after dried. The MICP occurred at the early stage after mixing bentonite with cementation medium changes soil's property and leads to more intact cracking polygons while drying. Bentonite mixed with live bacteria tends to form larger cracking polygons due to the increase of soil's mechanical strength. It shows the MICP process as well as the microbial activity have a positive influence on bentonite's cracking potential remediation.
机译:本文描述了微生物诱导方解石沉淀(MICP)对膨润土干燥开裂行为的影响的初步研究。在受控温度和相对湿度条件下,在培养皿中监测混合有细菌和胶结介质的膨润土的干燥收缩率。还监测了三个对照组,其中将膨润土与活菌+不含CaCl_2的胶结介质,死菌+胶结介质以及死菌+不含CaCl_2的胶结介质混合,以研究MICP过程和微生物活性对土壤的影响。干燥裂纹。扫描电子显微镜图像显示细菌在干燥后在膨润土表面上存活。 MICP发生在膨润土与胶结介质混合后的早期,改变了土壤的性质并导致干燥时更多的完整的开裂多边形。由于土壤机械强度的提高,与活细菌混合的膨润土往往会形成较大的开裂多边形。它表明了MICP过程以及微生物活性对膨润土的裂化潜力修复具有积极的影响。

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