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首页> 外文期刊>Acta Geotechnica: An International journal for Geoengineering >Impact of bacteria and urease concentration on precipitation kinetics and crystal morphology of calcium carbonate
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Impact of bacteria and urease concentration on precipitation kinetics and crystal morphology of calcium carbonate

机译:细菌对碳酸钙沉淀动力学和晶体形态的影响

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摘要

Microbial/Enzyme-induced carbonate precipitation uses bacteria/urease to drive the biogeochemical reactions to generate CaCO3 precipitation. The goal of this study was to assess the impact of initial concentrations of urease and bacteria on precipitation kinetics and crystal morphology (crystal shape and chemical composition) of calcium carbonate precipitation. Experimental results showed that the CaCO3 precipitation kinetics were well-fitted by a modified exponential logistic model with a confidence value of 95%, and higher concentrations of bacteria and urease could increase the precipitation rate of CaCO3. The results of XRD, FTIR and SEM indicated that vaterite phase was the dominant form of CaCO3 crystals in bacteria-induced system, and calcite phase was the primary form of the CaCO3 crystals in urease-induced system. The results also showed that the effect of initial concentrations of bacteria and urease on the morphology of CaCO3 crystals was insignificant.
机译:微生物/酶诱导的碳酸碳酸盐沉淀使用细菌/脲酶来驱动生物地球化学反应,以产生CaCO 3沉淀。 本研究的目的是评估初始浓度对碳酸钙沉淀的沉淀动力学和晶体形态(晶体形态和化学成分)的影响。 实验结果表明,CaCO3沉淀动力学通过改进的指数逻辑模型良好装配,具有95%的置信度值,浓度较高的细菌和脲酶可以提高CaCO3的沉淀率。 XRD,FTIR和SEM的结果表明,Vaterite阶段是细菌诱导的系统中的CaCO 3晶体的主要形式,方解石相是脲酶诱导的系统中的CaCO 3晶体的主要形式。 结果还表明,初始浓度的细菌和释放释放液对CaCO 3晶体形态的影响是微不足道的。

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