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Investigation and in situ visualisation of interfacial interactions of thermophilic microbial with metal-sulfides in a simulated heap environment

机译:模拟堆环境中硫酸金属硫化物邻近嗜热微生物界面相互作用的研究及其研究

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This study sought to provide a better understanding of the dynamics of microbial-metal sulfide interfacial processes relevant to heap bioleaching. Attachment and subsequent biofilm formation by Metallosphaera hakonensis (M. hakonensis) on the surface of massive chalcopyrite and pyrite samples, as well as a low-grade chalcopyritic whole ore were investigated. The method made use of a biofilm reactor in which thin sections of mineral ore were mounted. Operating conditions in the reactor simulated those of a bioheap in terms of fluid-flow and mineralogy, where the low-grade chalcopyrite ore sections were used. Pure cultures of M. hakonensis were used to inoculate the reactors and the attachment and subsequent biofilm development visualised in situ after 2, 4 and 8 days using a combination of atomic force and epifluorescent microscopy (AFM-EFM) as well as confocal scanning laser microscopy (CSLM) and revealed insights into biofilm structure and architecture: The effect of varying temperature on the extent of attachment and biofilm development was also assessed after 4 days using three temperature regimes: room temperature (20 ± 1°C), 45°C and 65°C. The density of the attached micro-colonies increased with an increase in time, indicative of an actively growing biofilm. The extent of surface coverage and proliferation of the biofilm was dependent on the temperature, with surface coverage being more extensive at 65 °C, near the optimal temperature for growth. Preferential attachment and biofilm formation to sulfide minerals was observed, with increased surface coverage of pyrite mineral surfaces relative to chalcopyrite and low-grade ore. The AFM-EFM technique enhanced the level of detail at which site specific associations of microorganisms with mineral surfaces could be assessed. Spatial orientation and density of attached micro-colonies were noted.
机译:该研究寻求更好地了解与堆生物浸出相关的微生物 - 金属硫化物界面过程的动态。研究了大量黄铜矿和黄铁矿样品表面的Metallosphaera Hakonensis(M.Hakonensis)的附着和随后的生物膜形成,以及低级硫代吡喃全矿石。该方法使用了生物膜反应器,其中安装了矿物矿石的薄部分。反应器中的操作条件模拟了流体流动和矿物的BioHeap的条件,其中使用了低级黄铜矿矿石部分。使用M. hakonensis的纯培养物用于在2,4和8天后用原子力和eFM-EFM)以及共聚焦扫描激光显微镜(AFM-EFM)在2,4和8天后地接种反应器和附件和随后的生物膜显现。 (CSLM)并揭示了生物膜结构和架构的见解:在使用三个温度制度的4天后,还评估了不同温度对附着和生物膜发育程度的影响:室温(20±1°C),45°C和65°C。随着时间的推移,附着的微菌落的密度增加,指示活跃的生物膜。生物膜的表面覆盖范围和增殖依赖于温度,表面覆盖在65℃下更广泛,靠近增长的最佳温度。观察到硫化物矿物的优先附着和生物膜形成,随着硫代铜矿和低级矿石的硫铁矿矿物表面的表面覆盖率增加。 AFM-EFM技术提高了可以评估与矿物表面的微生物特异性关联的细节水平。注意到附着的微菌落的空间取向和密度。

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