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首页> 外文期刊>Soil Science Society of America Journal >Kinetics of Competitive Reduction of Nitrate and Iron Oxides by Aeromonas hydrophila HS01
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Kinetics of Competitive Reduction of Nitrate and Iron Oxides by Aeromonas hydrophila HS01

机译:嗜水气单胞菌HS01竞争性还原硝酸盐和氧化铁的动力学

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摘要

While the interaction between NO3- and Fe reduction is well reported, it still lacks a detailed quantitative analysis of the properties and reactions responsible for the competitive reduction. In this study, the kinetics of the reduction of NO3- and Fe oxides by Aeromonas hydrophila HS01 were investigated in an artificial groundwater medium. The presence of Fe oxides showed an inhibitory effect on NO3- reduction to a varying extent, and vice versa, which was also evidenced by cyclic voltammetry analysis of Fe(II)/Fe(III). Higher Fe(III) availability and increased Fe oxide surface areas were more favorable for Fe reduction but resulted in a stronger inhibitory effect on NO3- reduction. The inhibitory effect also decreased with increased hematite crystallinity. Based on the kinetics and the elementary reactions, we established a kinetic model suggesting that direct biotic NO3- reduction by HS01 is the leading contribution, while the cell-associated Fe(II) produced by HS01 also reduced NO3- but with a limited contribution because the reaction rates of NO3 reduction by cell-associated Fe(II) are lower than that of NO3 reduction by HS01. This detailed kinetics and modeling study provides useful information for understanding the interaction between NO3- and Fe reduction in various subsurface environments.
机译:虽然NO3-和Fe还原之间的相互作用已得到很好的报道,但仍缺乏对引起竞争性还原的性质和反应进行详细的定量分析。在这项研究中,研究了在人工地下水介质中嗜水气单胞菌HS01还原NO3-和Fe氧化物的动力学。 Fe氧化物的存在在不同程度上显示出对NO3-还原的抑制作用,反之亦然,Fe(II)/ Fe(III)的循环伏安分析也证明了这一点。较高的Fe(III)利用率和增加的Fe氧化物表面积更有利于Fe还原,但对NO3-还原的抑制作用更强。随着赤铁矿结晶度的增加,抑制作用也降低。基于动力学和基本反应,我们建立了一个动力学模型,表明HS01直接还原生物NO3-是主要贡献,而HS01产生的与细胞相关的Fe(II)也还原NO3-,但贡献有限,因为与细胞相关的Fe(II)还原NO3的反应速率低于HS01还原NO3的反应速率。这项详细的动力学和模型研究为了解各种地下环境中NO3-和Fe还原之间的相互作用提供了有用的信息。

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