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Catalytic oxidation and adsorption of Cr(III) on iron-manganese nodules under oxic conditions.

机构信息

Key Laboratory of Arable Land Conservation (Middle and Lower Reaches of Yangtse River), Ministry of Agriculture and Rural Affairs of the People's Republic of China, Hubei Key Laboratory of Soil Environment and Pollution Remediation, College of Resources and Environment, Huazhong Agricultural University, Wuhan 430070, Hubei Province, China.

Key Laboratory of Arable Land Conservation (Middle and Lower Reaches of Yangtse River), Ministry of Agriculture and Rural Affairs of the People's Republic of China, Hubei Key Laboratory of Soil Environment and Pollution Remediation, College of Resources and Environment, Huazhong Agricultural University, Wuhan 430070, Hubei Province, China.

出版信息

J Hazard Mater. 2020 May 15;390:122166. doi: 10.1016/j.jhazmat.2020.122166. Epub 2020 Jan 22.

Abstract

The speciation, toxicity and mobility of chromium (Cr) are significantly affected by natural iron-manganese nodules due to the adsorption and redox reactions in soils. However, the redox processes in oxic environments have received little attention. In this work, the interaction mechanism between Cr(III) and natural iron-manganese nodules was studied under oxic conditions, and the effects of chemical composition, dissolved oxygen concentration, pH, ionic strength and coexisting ions were further investigated. The results showed that iron-manganese nodules could effectively oxidize dissolved Cr(III), and most of the newly formed Cr(VI) was adsorbed on the surface of nodules. In iron-manganese nodules, manganese oxides mainly contributed to Cr(III) oxidation, and iron oxides facilitated the adsorption and immobilization of Cr(VI). In addition, Cr(III) could be catalytically oxidized to Cr(VI) on the surface of manganese oxides through the generation of Mn(III) intermediate or Mn(IV) oxides from released Mn(II) under oxic conditions. The oxidation rate of Cr(III) by the nodules decreased with increasing pH from 2.0 to 8.0, and increased with increasing ionic strength. This work reveals the adsorption and catalytic oxidation mechanism of Cr(III) by iron-manganese nodules in a simulated open system, and improves the understanding of the geochemical behavior of chromium in soils.

摘要

铬(Cr)的形态、毒性和迁移性会受到自然铁锰结核的显著影响,这是由于土壤中的吸附和氧化还原反应。然而,氧化环境中的氧化过程却很少受到关注。在这项工作中,研究了在有氧条件下 Cr(III)与天然铁锰结核的相互作用机制,并进一步研究了化学成分、溶解氧浓度、pH 值、离子强度和共存离子的影响。结果表明,铁锰结核可以有效地氧化溶解的 Cr(III),并且大部分新形成的 Cr(VI)被吸附在结核表面上。在铁锰结核中,锰氧化物主要有助于 Cr(III)的氧化,而铁氧化物则有利于 Cr(VI)的吸附和固定。此外,在有氧条件下,通过释放的 Mn(II)生成 Mn(III)中间产物或 Mn(IV)氧化物,Cr(III)可以在锰氧化物表面上被催化氧化为 Cr(VI)。随着 pH 值从 2.0 增加到 8.0,结核对 Cr(III)的氧化速率降低,而随着离子强度的增加,氧化速率增加。这项工作揭示了铁锰结核在模拟开放系统中对 Cr(III)的吸附和催化氧化机制,提高了对土壤中铬地球化学行为的认识。

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