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Kinetics of calcite precipitation by ureolytic bacteria under aerobic and anaerobic conditions

机译:有氧和厌氧条件下Ureolytic细菌的方解石降水的动力学

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摘要

The kinetics of urea hydrolysis (ureolysis) and induced calcium carbonate(CaCO3) precipitation for engineering use in the subsurface wasinvestigated under aerobic conditions using Sporosarcina pasteurii(ATCC strain 11859) as well as Bacillus sphaericus strains 21776and 21787. All bacterial strains showed ureolytic activity inducingCaCO3 precipitation aerobically. Rate constants not normalized tobiomass demonstrated slightly higher-rate coefficients for both ureolysis(kurea) and CaCO3 precipitation (kprecip)for B. sphaericus 21776 (kurea=0.10±0.03 h−1, kprecip=0.60±0.34 h−1) compared toS. pasteurii (kurea=0.07±0.02 h−1,kprecip=0.25±0.02 h−1), though these differences werenot statistically significantly different. B. sphaericus 21787showed little ureolytic activity but was still capable of inducing someCaCO3 precipitation. Cell growth appeared to be inhibited duringthe period of CaCO3 precipitation. Transmission electron microscopy (TEM) images suggest this is dueto the encasement of cells and was reflected in lower kureavalues observed in the presence of dissolved Ca. However, biomass regrowthcould be observed after CaCO3 precipitation ceased, which suggeststhat ureolysis-induced CaCO3 precipitation is not necessarilylethal for the entire population. The kinetics of ureolysis andCaCO3 precipitation with S. pasteurii was furtheranalyzed under anaerobic conditions. Rate coefficients obtained in anaerobicenvironments were comparable to those under aerobic conditions; however, nocell growth was observed under anaerobic conditions with NO3-,SO42- or Fe3+ as potential terminal electronacceptors. These data suggest that the initial rates of ureolysis andureolysis-induced CaCO3 precipitation are not significantlyaffected by the absence of oxygen but that long-term ureolytic activity mightrequire the addition of suitable electron acceptors. Variations in theureolytic capabilities and associated rates of CaCO3 precipitationbetween strains must be fully considered in subsurface engineering strategiesthat utilize microbial amendments.
机译:尿素水解(尿素水解)和用于在地下工程使用诱导碳酸钙(CaCO 3)沉淀动力学使用Sporosarcina巴氏(ATCC菌株11859),以及球形芽孢杆菌菌株21776and 21787.所有细菌菌株显示尿素分解活性inducingCaCO3需氧条件下wasinvestigated沉淀有氧。速率常数不是球形芽孢杆菌21776标准化tobiomass两个尿素水解(kurea)和CaCO 3沉淀(kprecip)证明稍高速率系数(kurea = 0.10±0.03 H-1,kprecip = 0.60±0.34 H-1)相比,TOS。巴氏(kurea = 0.07±0.02 H-1,kprecip = 0.25±0.02 H-1),尽管这些差异都不在统计学上不同显著。球形芽孢杆菌21787showed小尿素分解活性,但仍能够诱导someCaCO3沉淀。细胞生长似乎被抑制碳酸钙沉淀的duringthe周期。透射电子显微镜(TEM)图像表明这是dueto细胞的包套,并反映在溶解Ca的存在下观察到较低kureavalues然而,在碳酸钙沉淀停止,这suggeststhat尿素水解诱导的碳酸钙沉淀是不necessarilylethal整个人口的生物质regrowthcould被观察到。尿素水解andCaCO3沉淀与S.巴斯德的动力学厌氧条件下furtheranalyzed。在anaerobicenvironments获得的速率系数比得上那些在有氧条件下;然而,用NO3-,SO42-或Fe3 +的厌氧条件如电势端子electronacceptors下观察nocell增长。这些数据表明,尿素水解的初始速率andureolysis诱导的碳酸钙沉淀不是由氧不存在下但长期尿素分解活性significantlyaffected mightrequire加入合适的电子受体的。在theureolytic能力的变化和CaCO3 precipitationbetween株的相关率必须在地下工程strategiesthat利用微生物修正案予以充分考虑。

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