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Precipitation of Phosphate Minerals by Microorganisms Isolated from a Fixed-Biofilm Reactor Used for the Treatment of Domestic Wastewater

机译:从固定生物膜反应器中分离的用于处理生活污水的微生物对磷酸盐矿物的沉淀

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摘要

The ability of bacteria isolated from a fixed-film bioreactor to precipitate phosphate crystals for the treatment of domestic wastewater in both artificial and natural media was studied. When this was demonstrated in artificial solid media for crystal formation, precipitation took place rapidly, and crystal formation began 3 days after inoculation. The percentage of phosphate-forming bacteria was slightly higher than 75%. Twelve major colonies with phosphate precipitation capacity were the dominant heterotrophic platable bacteria growing aerobically in artificial media. According to their taxonomic affiliations (based on partial sequencing of the 16S rRNA), the 12 strains belonged to the following genera of Gram-negative bacteria: Rhodobacter, Pseudoxanthobacter, Escherichia, Alcaligenes, Roseobacter, Ochrobactrum, Agromyce, Sphingomonas and Paracoccus. The phylogenetic tree shows that most of the identified populations were evolutionarily related to the Alphaproteobacteria (91.66% of sequences). The minerals formed were studied by X-ray diffraction, scanning electron microscopy (SEM), and energy dispersive X-ray microanalysis (EDX). All of these strains formed phosphate crystals and precipitated struvite (MgNH4PO4·6H2O), bobierrite [Mg3(PO4)2·8H2O] and baricite [(MgFe)3(PO4)2·8H2O]. The results obtained in this study show that struvite and spherulite crystals did not show any cell marks. Moreover, phosphate precipitation was observed in the bacterial mass but also near the colonies. Our results suggest that the microbial population contributed to phosphate precipitation by changing the media as a consequence of their metabolic activity. Moreover, the results of this research suggest that bacteria play an active role in the mineral precipitation of soluble phosphate from urban wastewater in submerged fixed-film bioreactors.
机译:研究了从固定膜生物反应器中分离出的细菌沉淀磷酸盐晶体以在人造和天然介质中处理生活污水的能力。当在人造固体介质中证明形成晶体时,沉淀迅速发生,并且接种后3天开始形成晶体。磷酸盐形成细菌的百分比略高于75%。十二个具有磷酸盐沉淀能力的主要菌落是在人工培养基中有氧生长的主要异养平板细菌。根据它们的分类学隶属关系(基于16S rRNA的部分测序),这12个菌株分别属于革兰氏阴性细菌的以下属:红细菌,假黄杆菌,大肠埃希氏菌,产碱菌,迷迭香属,O骨细菌,土壤杆菌,鞘氨醇单胞菌和副球菌。系统进化树表明,大多数已鉴定的种群在进化上与α-变形杆菌有关(91.66%的序列)。通过X射线衍射,扫描电子显微镜(SEM)和能量色散X射线显微分析(EDX)研究形成的矿物。所有这些菌株均形成磷酸盐晶体,并沉淀出鸟粪石(MgNH4PO4·6H2O),硼铁矿[Mg3(PO4)2·8H2O]和重晶石[(MgFe)3(PO4)2·8H2O]。在这项研究中获得的结果表明鸟粪石和球晶晶体没有显示任何细胞痕迹。此外,在细菌团中以及在菌落附近也观察到磷酸盐沉淀。我们的结果表明,微生物种群由于其代谢活性而通过改变培养基来促进磷酸盐沉淀。此外,这项研究的结果表明,细菌在固定膜生物反应器中城市污水中可溶性磷酸盐的矿物沉淀中起着积极作用。

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