Effect of Ureolytic Bacteria on Compressibility of the Soils with Variable Gradation

IF 0.5 Q4 ENGINEERING, CIVIL
Mariola Wasil, Urszula Wydro, Elżbieta Wołejko
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引用次数: 0

Abstract

Abstract The aim of this study is to present the effect of treatment with ureolytic bacteria ( Sporosarcina pasteurii ) on the compressibility parameters of mineral and anthropogenic soils. In the presence of the urease enzyme, secreted by a strain of Sporosarcina pasteurii bacteria, urea hydrolysis occurs, allowing CaCO 3 to be precipitated. The literature suggests applying the Microbially Induced Calcite Precipitation (MICP) method to non-cohesive soils. In order to determine whether the biomineralization process occurs in other soil types, cohesive and anthropogenic soils were tested in the laboratory. Compressibility tests were carried out in the laboratory on MICP-treated and untreated soils as reference samples. The process of biocementation in the soil is made possible by the introduction of bacteria into the soil and subsequent activation by a cementation solution (consisting of urea and calcium ions Ca 2+ ). This paper presents the methodology for introducing bacteria into the soil, as well as the effect of the biomineralization process on the deformation parameters of the tested materials.
解尿菌对变级配土壤压缩性的影响
摘要本研究旨在探讨溶尿菌(Sporosarcina pasteurii)处理对矿物土壤和人为土壤压缩性参数的影响。在由巴氏孢芽孢杆菌菌株分泌的脲酶存在的情况下,尿素发生水解,使caco3沉淀。文献建议将微生物诱导方解石降水(MICP)方法应用于非粘性土壤。为了确定生物矿化过程是否发生在其他土壤类型中,在实验室中测试了粘性土壤和人为土壤。在实验室对micp处理和未处理的土壤作为参考样品进行了压缩性试验。土壤中的生物胶结过程是通过将细菌引入土壤并随后由胶结溶液(由尿素和钙离子ca2 +组成)激活而实现的。本文介绍了将细菌引入土壤的方法,以及生物矿化过程对被测材料变形参数的影响。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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