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The effect of microbial calcite precipitation on the retention properties of unsaturated fine-grained soils: discussion of the governing factors

机译:微生物方解石沉淀对不饱和细粒土壤保留性质的影响:探讨控制因素

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In recent years, biogeotechnology has been introduced as a novel and environmentally friendly technique for soil improvement. The need to address global warming and the adverse environmental effects of the chemical additives have led to the emergence and development of the techniques which use calcite producing microorganisms in order to improve soil mechanical properties. While the effects of microbial induced calcite precipitation (MICP) on the hydraulics and mechanics of saturated coarse-grained soils have been well examined and studied, there is not yet much information on the effects these microorganisms would have on the unsaturated soil mechanical behaviour. The first step, in this regard, is to understand the effect of the processes involved in the MICP on the soil retention properties. Soil water suction is a key factor controlling soil hydraulic and mechanical behaviour. In this study, the influence of MICP on the soil total suction in an unsaturated fine-grained soil sample has been explored using filter paper experiment. The results of this study revealed that by increasing the amount of bacterial solution, the soil saturation-total suction curves are significantly affected. The soil water retention changes are attributed to the change in double layer thickness as well as the precipitation of calcite crystals.
机译:近年来,已引入生物质技术作为土壤改善的新颖和环保技术。解决全球变暖和化学添加剂的不利环境影响的需要导致了使用方解石生产微生物的技术的出现和发展,以改善土壤机械性能。虽然微生物诱导的方解石沉淀(MICP)对饱和粗粒土壤的液压和力学的影响已经很好地检查和研究,但这些微生物对不饱和土机械行为的影响没有太多信息。在这方面,第一步是了解在土壤保留性质上涉及所涉及的过程的效果。土壤吸水是控制土壤液压和力学行为的关键因素。在这项研究中,使用滤纸实验探索了麦克风对不饱和细粒土壤样品中的土壤总吸气物的影响。该研究的结果表明,通过增加细菌溶液的量,土壤饱​​和 - 总吸力曲线受到显着影响。土壤水保留变化归因于双层厚度的变化以及方解石晶体的沉淀。

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