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脲酶和碳酸酐酶产生菌的特性及其在方解石沉淀中的作用。

Characterization of urease and carbonic anhydrase producing bacteria and their role in calcite precipitation.

机构信息

Laboratory of Environmental Pollution and Bioremediation, Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences, 830011, Urumqi, People's Republic of China.

出版信息

Curr Microbiol. 2011 Mar;62(3):894-902. doi: 10.1007/s00284-010-9801-4. Epub 2010 Nov 4.

Abstract

Urease and carbonic anhydrase (CA) are key enzymes in the chemical reaction of living organisms and have been found to be associated with calcification in a number of microorganisms and invertebrates. Three bacterial strains designated as AP4, AP6, and AP9 were isolated from highly alkaline soil samples using the enrichment culture technique. On the basis of various physiological tests and 16S rRNA sequence analysis, these three bacteria were identified as Bacillus sp., B. megaterium, and B. simplex. Further, these Bacillus species have been characterized for the production of urease and CA in the process of biocalcification. One of the isolates, AP6 produced 553 U/ml of urease and 5.61 EU/ml CA. All the strains were able to produce significant amount of exopolymeric substances and biofilm. Further, efficacy of these strains was tested for calcite production ability and results were correlated with urease and CA. Isolate AP6 precipitated 2.26 mg calcite/cell dry mass (mg). Our observations strongly suggest that it is not only urease but CA also plays an important role in microbially induced calcium carbonate precipitation process. The current work demonstrates that urease and CA producing microbes can be utilized in biocalcification as a sealing agent for filling the gaps or cracks and fissures in constructed facilities and natural formations alike.

摘要

脲酶和碳酸酐酶(CA)是生物体化学反应中的关键酶,已在许多微生物和无脊椎动物的钙化中发现与它们有关。使用富集培养技术从高碱性土壤样品中分离出三株细菌,分别命名为 AP4、AP6 和 AP9。基于各种生理测试和 16S rRNA 序列分析,这三种细菌被鉴定为芽孢杆菌属、巨大芽孢杆菌和简单芽孢杆菌。此外,这些芽孢杆菌的特征在于在生物钙化过程中产生脲酶和 CA。其中一个分离物 AP6 产生 553 U/ml 的脲酶和 5.61 EU/ml 的 CA。所有菌株都能够产生大量的胞外聚合物和生物膜。此外,还测试了这些菌株生产方解石的能力,并将结果与脲酶和 CA 进行了相关性分析。分离物 AP6 沉淀了 2.26 mg 方解石/细胞干质量(mg)。我们的观察结果强烈表明,在微生物诱导碳酸钙沉淀过程中,不仅是脲酶,CA 也起着重要作用。目前的工作表明,产脲酶和 CA 的微生物可用作生物钙化中的密封剂,用于填充人工设施和天然地层中的间隙、裂缝和裂隙。

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