首页> 外文期刊>Chemical geology >Ralstonia species mediate Fe-oxidation in circumneutral, metal-rich subsurface fluids of Henderson mine, CO
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Ralstonia species mediate Fe-oxidation in circumneutral, metal-rich subsurface fluids of Henderson mine, CO

机译:Ralstonia物种介导科罗拉多州亨德森矿的中性富金属地下流体中的铁氧化

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Deep subsurface oxic/anoxic interfaces within Henderson Mine, CO were investigated for the potential to support novel metal-oxidizing microorganisms. Ralstonia sp. were isolated from Fe-oxidizing enrichments inoculated with fracture fluids released through boreholes as well as Fe-oxides mineralizing around the mouths of the boreholes. 16S rRNA clone libraries of environmental DNA revealed that closely related Ralstonia sp. were numerically-dominant in metal-rich subsurface fluids. FeCO_3 gradient tubes were then utilized to demonstrate that isolate Ralstonia HM08-01 grows by oxidizing Fe(II) with O_2 at circumneutral pH. These results and the geochemical data from the borehole fluids implicate Fe-oxidation as a viable subsurface lifestyle. The differential development of Fe-oxide bands in biotic vs. abiotic gradient tubes suggests that Ralstonia HM08-01 exerts spatial control over Fe oxidation and precipitation. Geochemical profiles of Fe(II), Fe(III) and O_2 taken through the gradient tubes with voltammetric microelectrodes reveal that despite visual differences, similar total concentrations and distributions of aqueous Fe species were present in both systems. Extended X-ray Absorption Fine Structure (EXAFS) spectroscopy was used to characterize the mineralogy of the Fe-oxides produced in biotic vs. abiotic experiments. 2L-ferrihydrite dominated the mineral fits in both systems, and SEM revealed the ferrihydrite particles to be 50-100nm in diameter. This mineralogical identification combined with the detection of an abundant electroactive Fe(III) species are used to infer that 2L-ferrihydrite is a long-term stabilized colloidal species. The mechanism for stabilization of this phase is the presence of PO_4~(2-) and Si in growth experiments. In the Henderson fluids, PO_4~(2-) is below detection, but Si is at micromolar concentrations and likely influences the formation of potentially colloidal Fe-oxides in the environment.
机译:研究人员在科罗拉多州亨德森矿的深层地下有氧/缺氧界面中研究了支持新型金属氧化微生物的潜力。 Ralstonia sp。从通过钻孔释放的压裂液以及钻孔口周围矿化的铁氧化物中富集的铁氧化富集层中分离出来。环境DNA的16S rRNA克隆文库揭示了密切相关的Ralstonia sp。在富含金属的地下流体中以数字为主导。然后使用FeCO_3梯度管证明分离的Ralstonia HM08-01通过在环境pH值下用O_2氧化Fe(II)来生长。这些结果和来自井眼流体的地球化学数据表明,铁氧化是一种可行的地下生活方式。生物梯度管和非生物梯度管中Fe氧化带的差异发展表明,Ralstonia HM08-01对Fe的氧化和沉淀进行空间控制。 Fe(II),Fe(III)和O_2通过具有伏安法微电极的梯度管获得的地球化学分布图表明,尽管视觉上存在差异,但在两个系统中都存在相似的总浓度和分布的水性Fe物种。扩展的X射线吸收精细结构(EXAFS)光谱用于表征在生物与非生物实验中产生的铁氧化物的矿物学特征。 2L-水铁矿在两个体系中均占主导地位,而SEM显示该水铁矿颗粒的直径为50-100nm。这种矿物学特征与丰富的电活性Fe(III)物种的检测相结合,可以推断2L-水铁矿是一种长期稳定的胶体物种。该阶段稳定的机制是在生长实验中存在PO_4〜(2-)和Si。在亨德森流体中,PO_4〜(2-)低于检测范围,但Si的浓度为微摩尔浓度,可能会影响环境中潜在的胶体铁氧化物的形成。

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