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Microbially-Mediated Precipitation of Calcium Carbonate Nanoparticles

机译:微生物介导的碳酸钙纳米粒子的沉淀

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摘要

The objective of this study was to investigate the biomineralization of carbonate minerals using microorganisms (Wu Do-1) enriched from rhodoliths. A 16S rRNA sequence analysis showed that Wu Do-1 mainly contained Proteus mirabilis. The pH decreased from 6.5 to 5.3 over the first 4 days of incubation due to microbial oxidation of organic acids, after which it increased to 7.8 over the remaining incubation period. XRD analysis showed that the precipitates were Mg-rich calcite (Mg Cal CO3), whereas no precipitates were formed without the addition of Wu Do-1 in D-1 medium. SEM-EDS analyses showed that the Mg-rich calcite had a rhombohedron shape and consisted of Ca, Si and Mg with an extracelluar polymeric substance (EPS). In addition, TEM-EDS analyses revealed they were hexagon in shape, 500-700 nm in size, and composed of Ca, Mg, C, and O. These results indicated that Wu Do-1 induced precipitation of Mg-rich calcite on the cell walls and EPS via the accumulation of Ca and/or Mg ions. Therefore, microbial precipitation of carbonate nanoparticles may play an important role in metal and carbon biogeochemistry, as well as in carbon sequestration in natural environments.
机译:本研究的目的是使用富含罗达尔斯富集的微生物(Wu Do-1)来研究碳酸盐矿物的生物键化。 16S RRNA序列分析表明,Wu Do-1主要含有Proteus mirabilis。由于微生物氧化有机酸的微生物氧化,pH从6.5降至5.3的pH从6.5降至5.3。 XRD分析表明,沉淀物是富含Mg的方解石(Mg Cal CO 3),而没有在D-1培养基中添加Wu Do-1的不添加沉淀物。 SEM-EDS分析表明,富含Mg的方解石具有菱形形状,并由具有细胞外聚合物物质(EPS)的Ca,Si和Mg组成。此外,TEM-EDS分析显示它们的形状六边形,大小为500-700nm,由Ca,Mg,C和O组成。这些结果表明,Wu Do-1诱导富含Mg的铌铁的沉淀通过Ca和/或Mg离子的积累,细胞壁和EPS。因此,碳酸酯纳米颗粒的微生物沉淀可能在金属和碳生物地球细胞以及自然环境中的碳封存中起重要作用。

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