首页> 外文期刊>Geochimica et Cosmochimica Acta: Journal of the Geochemical Society and the Meteoritical Society >Arsenite sequestration at the surface of nano-Fe(ОН)_2, ferrous-carbonate hydroxide, and green-rust after bioreduction of arsenic-sorbed lepidocrocite by Shewanella putrefaciens
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Arsenite sequestration at the surface of nano-Fe(ОН)_2, ferrous-carbonate hydroxide, and green-rust after bioreduction of arsenic-sorbed lepidocrocite by Shewanella putrefaciens

机译:腐烂的希瓦氏菌生物还原砷吸附的细铁云母后,纳米Fe(ОН)_2,氢氧化亚铁氢氧化物和绿锈表面的砷螯合

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X-ray Absorption Fine Structure (XAFS) spectroscopy was used in combination with high resolution transmission electron microscopy (HRTEM), electron energy loss spectroscopy (EELS), X-ray energy dispersive spectroscopy (XEDS), X-ray powder diffraction, and M_ssbauer spectroscopy to obtain detailed information on arsenic and iron speciation in the products of anaerobic reduction of pure and A_s(V)- or A_s(III)-adsorbed lepidocrocite ('y-FeOOH) by Shewanella putrefaciens ATCC 12099. We found that this strain of S. putrefaciens is capable of using Fe(III) in lepidocrocite and As(V) in solution or adsorbed on lepidocrocite surfaces as electron acceptors. Bioreduction of lepidocrocite in the absence of arsenic resulted in the formation of hydroxycarbonate green rust 1 [Fe~II_4F_eIII_2(OH)_(I2)СO_3: GRI(CO_3)], which completely converted into ferrous-carbonate hydroxide (Fе~II_2(ОН)_2CO_3: FCH) over nine months. This study thus provides the first evidence of bacterial reduction of stoichiometric GRI(CO_3) into FCH. Bioreduction of A_s(III)-adsorbed lepidocrocite also led to the formation of GRI(CO_3) prior to formation of FCH, but the presence of A_s(III) slows down this transformation, leading to the co-occurrence of both phases after 22-month of aging. At the end of this experiment, As(III) was found to be adsorbed on the surfaces of GRI(CO_3) and FCH. After five months, bioreduction of A_s(V)-bearing lepidocrocite led directly to the formation of FCH in association with nanometer-sized particles of a minor As-rich Fе(ОН)_2 phase, with no evidence for green rust formation. In this five-month experiment, A_s(V) was fully converted to A_s(III), which was dominantly sorbed at the surface of the Fе(ОН)2 nanoparticles as oligomers binding to the edges of F_е(ОН)_6 octahedra at the edges of the octahedral layers of F_е(ОН)_2. These multinuclear A_s(III) surface complexes are characterized by A_s_As pairs at a distance of 3.32 ± 0.02 A and by A_s_Fe pairs at a distance of 3.50 ± 0.02 A and represent a new type of A_s(III) surface complex. Chemical analyses show that the majority of A_s(III) produced in the experiments with As present is associated with iron-bearing hydroxycarbonate or hydroxide solids
机译:X射线吸收精细结构(XAFS)光谱与高分辨率透射电子显微镜(HRTEM),电子能量损失光谱(EELS),X射线能量色散光谱(XEDS),X射线粉末衍射和M_ssbauer结合使用光谱学以获取由Shewanella putrefaciens ATCC 12099厌氧还原纯和A_s(V)-或A_s(III)吸附的纤铁矿('y-FeOOH)的产物中砷和铁形态的详细信息。我们发现这种菌株腐臭链球菌能够使用纤铁矿中的Fe(III)和溶液中或吸附在纤铁矿表面上的As(V)作为电子受体。在不存在砷的情况下对锂铁辉石进行生物还原会导致形成羟基碳酸盐生铁锈1 [Fe〜II_4F_eIII_2(OH)_(I2)СO_3:GRI(CO_3)],它会完全转化为碳酸亚铁氢氧化物(Fе〜II_2(ОН )_2CO_3:FCH)超过9个月。因此,这项研究为细菌将化学计量的GRI(CO_3)还原为FCH提供了第一个证据。 A_s(III)吸附的纤铁矿的生物还原也导致在FCH形成之前GRI(CO_3)的形成,但是A_s(III)的存在减慢了这种转变,导致22-一个月的老化。在该实验结束时,发现As(III)吸附在GRI(CO_3)和FCH的表面上。五个月后,含A_s(V)的铁蒙脱石的生物还原直接导致了FCH的形成,与次要的富含As的Fе(ОН)_2相的纳米级颗粒相关,没有绿色锈蚀形成的证据。在这个为期五个月的实验中,A_s(V)完全转化为A_s(III),A_s(V)以低聚物的形式主要吸附在Fе(ОН)2纳米八面体的F_е(ОН)_6八面体的边缘。 F_е(ОН)_2八面体层的边缘。这些多核A_s(III)表面复合物的特征是距离为3.32±0.02 A的A_s_As对和距离为3.50±0.02 A的A_s_Fe对,代表了一种新型的A_s(III)表面复合物。化学分析表明,在实验中使用As生成的大多数A_s(III)与含铁的羟基碳酸盐或氢氧化物固体有关

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