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从中国一个垃圾填埋场分离出的细菌的生物矿化性能。

Biomineralisation performance of bacteria isolated from a landfill in China.

作者信息

Rajasekar Adharsh, Wilkinson Stephen, Sekar Raju, Bridge Jonathan, Medina-Roldán Eduardo, Moy Charles K S

机构信息

a Department of Civil Engineering, Xi'an Jiaotong - Liverpool University, Suzhou 215123, Jiangsu, P.R. China.

b Department of Civil Engineering, University of Wolverhampton, Wolverhampton WV1 1LY, UK.

出版信息

Can J Microbiol. 2018 Dec;64(12):945-953. doi: 10.1139/cjm-2018-0254. Epub 2018 Aug 27.

Abstract

We report an investigation of microbially induced carbonate precipitation by seven indigenous bacteria isolated from a landfill in China. Bacterial strains were cultured in a medium supplemented with 25 mmol/L calcium chloride and 333 mmol/L urea. The experiments were carried out at 30 °C for 7 days with agitation by a shaking table at 130 r/min. Scanning electron microscopic and X-ray diffraction analyses showed variations in calcium carbonate polymorphs and mineral composition induced by all bacterial strains. The amount of carbonate precipitation was quantified by titration. The amount of carbonate precipitated in the medium varied among isolates, with the lowest being Bacillus aerius rawirorabr15 (LC092833) precipitating around 1.5 times more carbonate per unit volume than the abiotic (blank) solution. Pseudomonas nitroreducens szh_asesj15 (LC090854) was found to be the most efficient, precipitating 3.2 times more carbonate than the abiotic solution. Our results indicate that bacterial carbonate precipitation occurred through ureolysis and suggest that variations in carbonate crystal polymorphs and rates of precipitation were driven by strain-specific differences in urease expression and response to the alkaline environment. These results and the method applied provide benchmarking and screening data for assessing the bioremediation potential of indigenous bacteria for containment of contaminants in landfills.

摘要

我们报告了一项对从中国某垃圾填埋场分离出的7种本土细菌进行微生物诱导碳酸盐沉淀的研究。细菌菌株在添加了25 mmol/L氯化钙和333 mmol/L尿素的培养基中培养。实验在30°C下进行7天,通过摇床以130 r/min的转速搅拌。扫描电子显微镜和X射线衍射分析表明,所有细菌菌株诱导的碳酸钙多晶型和矿物成分存在差异。通过滴定法定量碳酸盐沉淀的量。培养基中沉淀的碳酸盐量在不同分离株之间有所不同,其中最低的是产气芽孢杆菌rawirorabr15(LC092833),其每单位体积沉淀的碳酸盐比非生物(空白)溶液多约1.5倍。发现硝基还原假单胞菌szh_asesj15(LC090854)效率最高,沉淀的碳酸盐比非生物溶液多3.2倍。我们的结果表明细菌碳酸盐沉淀是通过尿素分解发生的,并表明碳酸盐晶体多晶型和沉淀速率的变化是由脲酶表达和对碱性环境的反应中的菌株特异性差异驱动的。这些结果和所应用的方法为评估本土细菌对垃圾填埋场污染物的生物修复潜力提供了基准和筛选数据。

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