尼日利亚北部不同矿区高岭土中铁还原菌的鉴定及其潜在的生物浸出活性

12 B.M, A. H. Kawo, S. Yahaya
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摘要

高岭土是一种天然存在的原料,可用于多种工业用途。此外,由于高岭土中含有氧化铁和氢氧化物等含铁杂质,使用高岭土的经济性受到一定限制。这对某些产品的白度和耐火度以及高纯陶瓷的生产都有负面影响。微生物浸出技术被认为比传统的浸出方法更便宜、更环保,因此本研究探讨了能够提供高效生物浸出的潜在铁还原细菌的分离。通过分子、形态学和生化分析,分离出了多种细菌,包括不动杆菌、气单胞菌、梭状芽胞菌、克雷伯氏菌、假单胞菌和Sporanaerobacter,其中气单胞菌和Sporanaerobacter与假单胞菌和地杆菌的亲缘关系较近,而假单胞菌和地杆菌是较好的铁还原菌。这可能提示了一种可能的候选菌株,可以提供有效的生物浸出活性。本地细菌分离鉴定前的高岭土x射线荧光光谱分析结果发现含有以下氧化物:Fe2O3、SiO2、A12O3、MgO、P2O5、SO3、TiO2、MnO和CaO,证实了所采集高岭土样品的身份。最高的氧化物被发现是SiO2。
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Identification of Iron Reducing Bacteria from Kaolin of Different Mining Sites in Northern Nigeria for Potential Bioleaching Activity
Kaolin is a naturally occurring raw material for several industrial applications. Moreover, the economy of using Kaolin has some restrictions due to presence of iron-bearing impurities in form of oxides and hydroxides. This has a negative effect on the whiteness and refractoriness of some products and the production of high purity ceramics. The application of microbial leaching has been regarded as cheap and bio-friendly than conventional methods, hence this study investigates the isolation of potential iron reducing bacteria capable of providing efficient bioleaching. Bacteria isolation was carried out using serial dilution and plating techniquesResult of molecular, morphological and biochemical analyses reveal the presence of many bacterial isolates that includes Acinobacter spp., Aeromonas spp., Clostridium spp., Klebsiella spp., Pseudomonas spp. and Sporanaerobacter spp. Aeromonas and Sporanaerobacter species were identified as more closely related to the Pseudomonas and Geobacter species that are reported to be good iron reducing bacteria. This may suggest a possible candidate strain that could provide efficient bioleaching activity. Result of X-ray Fluorescence spectrometry of Kaolin prior to isolation and identification of indigenous bacteria was found to contain the following oxides; Fe2O3, SiO2, A12O3, MgO, P2O5, SO3, TiO2, MnO and CaO which confirmed the identity of Kaolin samples collected. The highest oxide was found to be SiO2.
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