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Fe(III) Reduction and U(VI) Immobilization by Paenibacillus sp. Strain 300A, Isolated from Hanford 300A Subsurface Sediments

机译:Paenibacillus sp。的Fe(III)还原和U(VI)固定化。与汉福德300A地下沉积物隔离的应变300A

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A facultative iron-reducing [Fe(III)-reducing] Paenibacillus sp. strain was isolated from Hanford 300A subsurface sediment biofilms that was capable of reducing soluble Fe(III) complexes [Fe(III)-nitrilotriacetic acid and Fe(III)-citrate] but unable to reduce poorly crystalline ferrihydrite (Fh). However, Paenibacillus sp. 300A was capable of reducing Fh in the presence of low concentrations (2 μM) of either of the electron transfer mediators (ETMs) flavin mononucleotide (FMN) or anthraquinone-2,6-disulfonate (AQDS). Maximum initial Fh reduction rates were observed at catalytic concentrations (<10 μM) of either FMN or AQDS. Higher FMN concentrations inhibited Fh reduction, while increased AQDS concentrations did not. We also found that Paenibacillus sp. 300A could reduce Fh in the presence of natural ETMs from Hanford 300A subsurface sediments. In the absence of ETMs, Paenibacillus sp. 300A was capable of immobilizing U(VI) through both reduction and adsorption. The relative contributions of adsorption and microbial reduction to U(VI) removal from the aqueous phase were ~7:3 in PIPES [piperazine- N , N ′ - bis(2-ethanesulfonic acid)] and ~1:4 in bicarbonate buffer. Our study demonstrated that Paenibacillus sp. 300A catalyzes Fe(III) reduction and U(VI) immobilization and that these reactions benefit from externally added or naturally existing ETMs in 300A subsurface sediments.
机译:兼性铁还原[Fe(III)还原] Paenibacillus sp.。从汉福德(Hanford)300A地下沉积物生物膜中分离出了可还原可溶性Fe(III)络合物[Fe(III)-亚硝酸三乙酸和柠檬酸Fe(III)]但无法还原结晶性较差的亚铁水合物(Fh)的菌株。但是,Paenibacillus sp。 300A能够在低浓度(2μM)的电子转移介质(ETM)黄素单核苷酸(FMN)或蒽醌-2,6-二磺酸盐(AQDS)的存在下降低Fh。在FMN或AQDS的催化浓度(<10μM)下观察到最大的初始Fh还原速率。较高的FMN浓度抑制Fh降低,而增加的AQDS浓度则不抑制。我们还发现了Paenibacillus sp.。如果存在来自汉福德300A地下沉积物的天然ETM,则300A可以降低Fh。在没有ETM的情况下,Paenibacillus sp。 300A能够通过还原和吸附固定化U(VI)。在PIPES [哌嗪-N,N'-双(2-乙磺酸)]中,吸附和微生物还原对水相中U(VI)去除的相对贡献为〜7:3,在碳酸氢盐缓冲液中为〜1:4。我们的研究表明,Paenibacillus sp。 300A催化Fe(III)还原和U(VI)固定化,这些反应得益于300A地下沉积物中外部添加的或天然存在的ETM。

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