首页> 外文会议>International Symposium on Water-Rock Interaction(WRI-11) vol.2; 20040627-0702; Saratoga Springs,NY(US) >In-situ structural characterization of biogenic manganese oxides produced by Bacillus sp., strain SG-1 in seawater
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In-situ structural characterization of biogenic manganese oxides produced by Bacillus sp., strain SG-1 in seawater

机译:芽孢杆菌属SG-1菌株在海水中产生的生物锰氧化物的原位结构表征

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Natural Mn oxide nanoparticles and grain coatings are ubiquitous in the environment and profoundly impact the quality of sediments via their ability to degrade and/or sequester contaminants. These oxides are believed to form dominantly via oxidation of Mn~(II) by marine and freshwater bacteria and have extremely high sorptive capacities for heavy metals. We have used XANES, EXAFS, and synchrotron (SR)-XRD techniques to study biogenic Mn oxides produced by spores of the marine Bacillus sp., strain SG-1 in sea water as a function of reaction time under fully in-situ conditions. The primary biogenic product is a nanocrystalline solid with an oxidation state and layered phyllomanganate local structure similar to that in δ-MnO_2. XRD data show the biooxides to have a phyllomanganate 10.0 A basal plane spacing, suggesting the interlayer is hydrated and contains Ca. Fits to EXAFS spectra suggest the octahedral layers of the biooxides to be relatively flat (out-of-plane bend < 10°) and to have relatively low octahedral layer Mn site vacancies (12 to 14%). These results suggest that aqueous Ca~(2+) is inserted into the biogenic oxide structure after completion of the enzymatic oxidation process. The biooxides observed in this study may be the most abundant Mn oxide phase suspended in the oxic and sub-oxic zones of the oceanic water column.
机译:天然氧化锰纳米颗粒和颗粒涂层在环境中无处不在,并通过其降解和/或隔离污染物的能力深刻影响沉积物的质量。据信这些氧化物主要是通过海洋和淡水细菌氧化Mn〜(II)形成的,对重金属具有极高的吸附能力。我们已经使用XANES,EXAFS和同步加速器(SR)-XRD技术研究了在完全原位条件下海洋芽孢杆菌(Bacillus sp。)菌株SG-1在海水中的孢子所产生的生物锰氧化物。主要的生物成因产物是具有类似于δ-MnO_2的氧化态和层状锰锰酸盐局部结构的纳米晶体固体。 XRD数据表明,生物氧化物的叶锰酸根基面间距为10.0 A,表明中间层已水合并含有Ca。与EXAFS光谱的拟合表明,生物氧化物的八面体层相对较平(平面外弯曲<10°),并且八面体层中的Mn位置空位相对较低(12%至14%)。这些结果表明,在酶促氧化过程完成后,Ca〜(2+)水溶液被插入到生物氧化物结构中。在这项研究中观察到的生物氧化物可能是悬浮在海洋水柱含氧和亚含氧区中的最丰富的Mn氧化物相。

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