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针铁矿表面上 Mn(II)吸附和催化氧化的动力学。

Kinetics of Mn(II) adsorption and catalytic oxidation on the surface of ferrihydrite.

机构信息

Key Laboratory of Poyang Lake Basin Agricultural Resource and Ecology of Jiangxi Province, College of Land Resource and Environment, Jiangxi Agricultural University, Nanchang 330045, China.

Key Laboratory of Arable Land Conservation (Middle and Lower Reaches of Yangtze River), Ministry of Agriculture, College of Resources and Environment, Huazhong Agricultural University, Wuhan 430070, China; State Environmental Protection Key Laboratory of Soil Health and Green Remediation, Wuhan 430070, China.

出版信息

Sci Total Environ. 2021 Oct 15;791:148225. doi: 10.1016/j.scitotenv.2021.148225. Epub 2021 Jun 4.

Abstract

Mn(II) adsorption-oxidation on iron (Fe) oxides (e.g., ferrihydrite) occurs in various soils and sediments, significantly affecting the toxicities and bioavailabilities of Mn and other associated elements. However, the detailed processes of Mn(II) adsorption-oxidation on ferrihydrite remain elusive. In this study, the Mn(II) (2 mM) adsorption-oxidation kinetics on different masses of ferrihydrite (0.25, 0.50, 1.00, and 1.25 g) at pH 7 were determined using batch kinetic studies combined with X-ray diffraction, transmission electron microscopy, and wet chemistry analyses. The results indicated that the low-concentration Mn(II) adsorption-oxidation on ferrihydrite occurred in two steps. First, Mn(II) was adsorbed onto ferrihydrite, where it was partially oxidized by the catalytic effect of ferrihydrite, within 0-60 min; subsequently, the remaining Mn(II) underwent autocatalytic oxidation on the previously generated Mn (oxyhydr)oxides. The initial adsorption-oxidation behaviors of Mn(II) on the ferrihydrite surface determined the kinetics of Mn(II) removal and oxidation, and therefore the amounts and types of Mn (oxyhydr)oxides formed. Furthermore, the specific characteristics of Mn(II) adsorption-oxidation on ferrihydrite showed a strong dependence on the Fe/Mn molar ratio. When this ratio was below 16.35, the initial process was dominated by Mn(II) adsorption onto ferrihydrite, with slight oxidation generating hausmannite (0-60 min), followed by the catalytic oxidation of Mn(II) on the formed hausmannite, generating manganite or groutite. Conversely, when the Fe/Mn molar ratio was above 32.7, the reactions primarily involved Mn(II) adsorption onto ferrihydrite with minor oxidation to form Mn(III/IV) (oxyhydr)oxides (~0-60 min), followed by the autocatalytic oxidation of Mn(II) on the freshly-generated Mn(III/IV) (oxyhydr)oxides, forming Mn(III) (oxyhydr)oxides, i.e., feitknechtite. These results provide further insight into the interaction between Fe and Mn, Mn(II) removal, and Mn (oxyhydr)oxide formation in the environment.

摘要

Mn(II)在铁(Fe)氧化物(例如水铁矿)上的吸附-氧化作用发生在各种土壤和沉积物中,显著影响 Mn 和其他相关元素的毒性和生物可利用性。然而,Mn(II)在水铁矿上的吸附-氧化的详细过程仍然难以捉摸。在这项研究中,通过使用批处理动力学研究结合 X 射线衍射、透射电子显微镜和湿化学分析,确定了在 pH 7 下不同质量的水铁矿(0.25、0.50、1.00 和 1.25 g)上的 Mn(II)(2 mM)吸附-氧化动力学。结果表明,低浓度 Mn(II)在水铁矿上的吸附-氧化分两步进行。首先,Mn(II)被吸附到水铁矿上,在 0-60 分钟内,被水铁矿的催化作用部分氧化;随后,剩余的 Mn(II)在先前生成的 Mn(氧氢)氧化物上进行自催化氧化。Mn(II)在水铁矿表面的初始吸附-氧化行为决定了 Mn(II)去除和氧化的动力学,因此决定了形成的 Mn(氧氢)氧化物的数量和类型。此外,Mn(II)在水铁矿上的吸附-氧化的特定特征表现出强烈依赖于 Fe/Mn 摩尔比。当该比值低于 16.35 时,初始过程主要由 Mn(II)吸附到水铁矿上,轻微氧化生成黑锌锰矿(0-60 分钟),然后是形成的黑锌锰矿上的 Mn(II)催化氧化,生成锰矿或硬锰矿。相反,当 Fe/Mn 摩尔比高于 32.7 时,反应主要涉及 Mn(II)吸附到水铁矿上,轻微氧化形成 Mn(III/IV)(氧氢)氧化物(0-60 分钟),然后是新生成的 Mn(III/IV)(氧氢)氧化物上的 Mn(II)的自催化氧化,形成 Mn(III)(氧氢)氧化物,即针铁矿。这些结果为进一步了解 Fe 和 Mn 之间的相互作用、Mn(II)去除和 Mn(氧氢)氧化物在环境中的形成提供了新的认识。

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