Sequestration of Cd(II) and Ni(II) ions on fungal manganese oxides associated with Mn(II) oxidase activity

Chang, Jianing; Tani, Yukinori; Naitou, Hirotaka; Miyata, Naoyuki; Seyama, Haruhiko

doi:10.1016/j.apgeochem.2014.06.007

Cited by 20 publications

(12 citation statements)

References 38 publications

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“…In other words, natural Mn oxides formed in Reocín incorporated higher amounts of trace metals (the case of Zn is outstanding) despite being precipitated from solutions with much lower metallic content. This represents more evidence of the extraordinary capacity of natural Mn oxides (likely, bio-oxides) to scavenge trace metals in the environment, which is in accordance with previous work [3,[8][9][10]43,44]. for Ni, and around 3 mg/L vs. 231-624 mg/L for Zn; Table 1).…”

Section: Trace Metal (Co Ni Zn) Partition Between Parent Solutions supporting

confidence: 92%

“…However, pH conditions of the IPB mine effluents a priori appear incompatible with the presence of Mn(II)-oxidizing microorganisms. This is an important limitation since Mn bio-oxides show adsorptive capacities, which are orders of magnitude higher than those of their abiotic counterparts [2,3,[8][9][10]45]. In the case of the circumneutral Reocín mine pit lake, geochemical conditions would a priori allow the presence of Mn(II)-oxidizing microorganisms that could be greatly catalyzing manganese oxidation.…”

Section: Factors Controlling Mn(ii) Oxidation and Mn Oxide Mineralogymentioning

confidence: 99%

“…The potential of manganese oxides to retain many different trace metals from natural and engineered environments is well known and has been recognized in very different settings [1][2][3][4]. Among over 30 different manganese oxide minerals with a MnO x -like formula, birnessite and todorokite are the most profusely studied by their high adsorbing capacity for trace metals like Ni, Co, or Zn [5][6][7][8][9][10][11][12][13][14][15][16][17][18]. the supposed absence of Mn(II)-oxidizing microbes (most of them known to be neutrophilic [28][29][30][31][32]), a priori that only allows chemical oxidation, and the sorptive capacity of the abiotic mineral products is usually much lower than the highly reactive Mn bio-oxides [8][9][10].…”

Section: Introductionmentioning

confidence: 99%

“…The results of our study could provide the basis for future remediation attempts in heavily contaminated mining districts aimed at removing the most soluble metal cations such as Mn(II), Co(II), Ni(II), or Zn(II) which, at present, can only be totally removed by hydroxide formation at very high pH (>9.5-10) in chemical treatment plants. products is usually much lower than the highly reactive Mn bio-oxides [8][9][10]. Thus, the first goal of this study was to investigate which Mn oxides are formed during the oxidation of Mn(II) in very concentrated mine waters.…”

Section: Introductionmentioning

confidence: 99%

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Coprecipitation of Co2+, Ni2+ and Zn2+ with Mn(III/IV) Oxides Formed in Metal-Rich Mine Waters

España

Yusta

2019

Minerals

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Manganese oxides are widespread in soils and natural waters, and their capacity to adsorb different trace metals such as Co, Ni, or Zn is well known. In this study, we aimed to compare the extent of trace metal coprecipitation in different Mn oxides formed during Mn(II) oxidation in highly concentrated, metal-rich mine waters. For this purpose, mine water samples collected from the deepest part of several acidic pit lakes in Spain (pH 2.7–4.2), with very high concentration of manganese (358–892 mg/L Mn) and trace metals (e.g., 795–10,394 µg/L Ni, 678–11,081 µg/L Co, 259–624 mg/L Zn), were neutralized to pH 8.0 in the laboratory and later used for Mn(II) oxidation experiments. These waters were subsequently allowed to oxidize at room temperature and pH = 8.5–9.0 over several weeks until Mn(II) was totally oxidized and a dense layer of manganese precipitates had been formed. These solids were characterized by different techniques for investigating the mineral phases formed and the amount of coprecipitated trace metals. All Mn oxides were fine-grained and poorly crystalline. Evidence from X-Ray Diffraction (XRD) and Scanning Electron Microscopy coupled to Energy Dispersive X-Ray Spectroscopy (SEM–EDX) suggests the formation of different manganese oxides with varying oxidation state ranging from Mn(III) (e.g., manganite) and Mn(III/IV) (e.g., birnessite, todorokite) to Mn(IV) (e.g., asbolane). Whole-precipitate analyses by Inductively Coupled Plasma-Mass Spectrometry (ICP-MS), Inductively Coupled Plasma-Atomic Emission Spectrometry (ICP-AES), and/or Atomic Absorption Spectrometry (AAS), provided important concentrations of trace metals in birnessite (e.g., up to 1424 ppm Co, 814 ppm Ni, and 2713 ppm Zn), while Co and Ni concentrations at weight percent units were detected in asbolane by SEM-EDX. This trace metal retention capacity is lower than that observed in natural Mn oxides (e.g., birnessite) formed in the water column in a circum-neutral pit lake (pH 7.0–8.0), or in desautelsite obtained in previous neutralization experiments (pH 9.0–10.0). However, given the very high amount of Mn sorbent material formed in the solutions (2.8–4.6 g/L Mn oxide), the formation of these Mn(III/IV) oxides invariably led to the virtually total removal of Co, Ni, and Zn from the aqueous phase. We evaluate these data in the context of mine water pollution treatment and recovery of critical metals.

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Section: Trace Metal (Co Ni Zn) Partition Between Parent Solutions supporting

confidence: 92%

Section: Factors Controlling Mn(ii) Oxidation and Mn Oxide Mineralogymentioning

confidence: 99%

Section: Introductionmentioning

confidence: 99%

Section: Introductionmentioning

confidence: 99%

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Coprecipitation of Co2+, Ni2+ and Zn2+ with Mn(III/IV) Oxides Formed in Metal-Rich Mine Waters

España

Yusta

2019

Minerals

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“…In contrast to very low oxidation efficiency, the cumulative C T seq concentration was high at 1.18 mM (0.43 ± 0.01, 0.46 ± 0.01, and 0.14 ± 0.00 mM for the 1st, 2nd, and 3rd treatments, respectively), corresponding to 83% ± 1% of the cumulative Cr III Int (Figure 7 and Table S2). The molar ratio of C T seq relative to solid Mn was abnormally high (~120 mol%), implying a sequestration mechanism specific to Cr other than the simple sorption process of common divalent heavy metal ions, Zn 2+ and Cd 2+ (their maximum sorption relative to solid Mn was 20-25 mol%; [39,41]) or trivalent La 3+ ions (~30 mol% [45]). Heated BMOs possessed similar Cr sequestration capacity ( Figure S3) even under aerobic conditions with the domination of Cr(III) in the solid phase, which was revealed by X-ray Absorption Near-Edge Structure (XANES) (Figure 8).…”

Section: Anaerobic Sequestration Of Cr(iii) By Bmosmentioning

confidence: 99%

Sequestration and Oxidation of Cr(III) by Fungal Mn Oxides with Mn(II) Oxidizing Activity

et al. 2019

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Biogenic manganese oxides (BMOs) have gained increasing attention for environmental application because of their sequestration and oxidizing abilities for various elements. Oxidation and sequestration of Cr(III) by BMOs, however, still remain unknown. We prepared BMOs in liquid cultures of Acremonium strictum strain KR21-2, and subsequently conducted single or repeated treatment experiments in Cr(NO3)3 at pH 6.0. Under aerobic conditions, newly formed BMOs exhibited a rapid production of Cr(VI) without a significant release of Mn(II), demonstrating that newly formed BMO mediates a catalytic oxidation of Cr(III) with a self-regeneration step of reduced Mn. In anaerobic solution, newly formed BMOs showed a cessation of Cr(III) oxidation in the early stage of the reaction, and subsequently had a much smaller Cr(VI) production with significant release of reduced Mn(II). Extraordinary sequestration of Cr(III) was observed during the repeated treatments under anaerobic conditions. Anaerobically sequestered Cr(III) was readily converted to Cr(VI) when the conditions became aerobic, which suggests that the surface passivation is responsible for the anaerobic cessation of Cr(III) oxidation. The results presented herein increase our understanding of the roles of BMO in Cr(III) oxidation and sequestration processes in potential application of BMOs towards the remediation of Cr(III)/Cr(VI) in contaminated sites.

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The important role of the interaction between manganese minerals and metals in environmental remediation: a review

Chen

Qiu

et al. 2023

Environ Sci Pollut Res

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With illegal discharge of wastewater containing inorganic and organic pollutants, combined pollution is common and need urgent attention. Understanding the migration and transformation laws of pollutants in the environment has important guiding signi cance for environmental remediation. Due to the characteristics of adsorption, oxidation and catalysis, manganese minerals play important role in the environment fate of pollutants. This review summarizes the forms of interaction between manganese minerals and metals, the environmental importance of the interaction between manganese minerals and metals, and the contribution of this interaction in improving performance of Mn-based composite for environmental remediation. The literatures have indicated that the interactions between manganese minerals and metals involve in surface adsorption, lattice replacement and formation of association minerals. The synergistic or antagonistic effect resulted from the interaction in uence the puri cation of heavy metal and organism pollutant. The synergistic effect bene ted from the coordination of adsorption and oxidation, convenient electron transfer, abundant oxygen vacancies and fast migration of lattice oxygen. Based on the synergy, Mn-based composites have been widely used for environmental remediation. This review is helpful to fully understand the migration and transformation process of pollutants in the environment, expand the resource utilization of manganese minerals for environmental remediation.

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Sequestration of Cd(II) and Ni(II) ions on fungal manganese oxides associated with Mn(II) oxidase activity

Cited by 20 publications

References 38 publications

Coprecipitation of Co2+, Ni2+ and Zn2+ with Mn(III/IV) Oxides Formed in Metal-Rich Mine Waters

Coprecipitation of Co2+, Ni2+ and Zn2+ with Mn(III/IV) Oxides Formed in Metal-Rich Mine Waters

Sequestration and Oxidation of Cr(III) by Fungal Mn Oxides with Mn(II) Oxidizing Activity

The important role of the interaction between manganese minerals and metals in environmental remediation: a review

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