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Experimental Microbial Alteration and Fe Mobilization From Basaltic Rocks of the ICDP HSDP2 Drill Core Hilo Hawaii

机译:来自夏威夷希洛的ICDP HSDP2岩心的玄武岩中的实验微生物蚀变和铁动员

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摘要

The interaction of a single bacterial species (Burkholderia fungorum) with basaltic rocks from the ICDP HSDP2 drill core and synthetic basaltic glasses was investigated in batch laboratory experiments to better understand the role of microbial activity on rock alteration and Fe mobilization. Incubation experiments were performed with drill core basaltic rock samples to investigate differences in the solution chemistry during biotic and abiotic alteration. Additionally, colonization experiments with synthetic basaltic glasses of different Fe redox states and residual stresses were performed to evaluate their influence on microbial activity and surface attachment of cells. In biotic incubation experiments bacterial growth was observed and the release of Fe and other major elements from drill core basaltic rocks to solution exceeded that of abiotic controls only when the rock sample assay was nutrient depleted. The concentration of dissolved major elements in solution in biotic colonization experiments with synthetic basaltic glasses increased with increasing residual stress and Fe(II) content. Furthermore, the concentration of dissolved Fe and Al increased similarly in biotic colonization experiments indicating that their dissolution might be triggered by microbial activity. Surface morphology imaging by SEM revealed that cells on basaltic rocks in incubation experiments were most abundant on the glass and surfaces with high roughness and almost absent on minerals. In colonization experiments, basaltic glasses with residual stress and high Fe(II) content were intensely covered with a cellular biofilm. In contrast, glasses with high Fe(III) content and no residual stress were sparsely colonized. We therefore conclude that structurally bound Fe is most probably used by B. fungorum as a nutrient. Furthermore, we assume that microbial activity overall increased rock dissolution as soon as the environment becomes nutrient depleted. Our results show that besides compositional effects, other factors such as redox state and residual stress can control microbial alteration of basaltic glasses.
机译:在批处理实验室实验中研究了单一细菌物种(伯克霍尔德氏菌)与来自ICDP HSDP2钻芯的玄武岩和合成玄武岩玻璃的相互作用,以更好地了解微生物活性在岩石蚀变和铁动员中的作用。用钻芯玄武岩样品进行孵化实验,以研究生物和非生物蚀变过程中溶液化学的差异。此外,用不同Fe氧化还原态和残余应力的合成玄武岩玻璃进行定殖实验,以评估其对微生物活性和细胞表面附着的影响。在生物培养实验中,观察到细菌生长,仅当岩石样品测定营养物质耗尽时,铁和其他主要元素从钻芯玄武岩到溶液的释放才超过非生物对照。合成玄武岩玻璃在生物定殖实验中,溶液中溶解的主要元素的浓度随残余应力和Fe(II)含量的增加而增加。此外,在生物定殖实验中,溶解的铁和铝的浓度相似地增加,表明它们的溶解可能是由微生物活性触发的。 SEM的表面形态学成像表明,在孵化实验中,玄武岩上的细胞在玻璃和表面上最丰富,具有高粗糙度,而在矿物上几乎没有。在定植实验中,具有残余应力和高Fe(II)含量的玄武玻璃被细胞生物膜强烈覆盖。相反,稀疏地定植了具有高Fe(III)含量且没有残余应力的玻璃。因此,我们得出的结论是,结构结合的Fe最有可能被B. fungorum用作营养物。此外,我们假设一旦环境养分耗尽,微生物活动总体上就会增加岩石溶解。我们的结果表明,除了成分影响外,氧化还原状态和残余应力等其他因素也可以控制玄武玻璃的微生物变化。

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