Xu Tingying, Roepke Elizabeth W, Flynn Elaine D, Rosenfeld Carla E, Balgooyen Sarah, Ginder-Vogel Matthew, Schuler Christopher J, Santelli Cara M
Department of Earth and Environmental Sciences, University of Minnesota - Twin Cities, Minneapolis, MN, 55455, USA; BioTechnology Institute, University of Minnesota - Twin Cities, Saint Paul, MN, 55108, USA.
Department of Earth and Environmental Sciences, University of Minnesota - Twin Cities, Minneapolis, MN, 55455, USA; BioTechnology Institute, University of Minnesota - Twin Cities, Saint Paul, MN, 55108, USA.
Chemosphere. 2023 Jun;327:138467. doi: 10.1016/j.chemosphere.2023.138467. Epub 2023 Mar 24.
Naturally occurring manganese (Mn) oxide minerals often form by microbial Mn(II) oxidation, resulting in nanocrystalline Mn(III/IV) oxide phases with high reactivity that can influence the uptake and release of many metals (e.g., Ni, Cu, Co, and Zn). During formation, the structure and composition of biogenic Mn oxides can be altered in the presence of other metals, which in turn affects the minerals' ability to bind these metals. These processes are further influenced by the chemistry of the aqueous environment and the type and physiology of microorganisms involved. Conditions extending to environments that typify mining and industrial wastewaters (e.g., increased salt content, low nutrient, and high metal concentrations) have not been well investigated thus limiting the understanding of metal interactions with biogenic Mn oxides. By integrating geochemistry, microscopic, and spectroscopic techniques, we examined the capacity of Mn oxides produced by the Mn(II)-oxidizing Ascomycete fungus Periconia sp. SMF1 isolated from the Minnesota Soudan Mine to remove the metal co-contaminant Co(II) from synthetic waters that are representative of mining wastewaters currently undergoing remediation efforts. We compared two different applied remediation strategies under the same conditions: coprecipitation of Co with mycogenic Mn oxides versus adsorption of Co with pre-formed fungal Mn oxides. Co(II) was effectively removed from solution by fungal Mn oxides through two different mechanisms: incorporation into, and adsorption onto, Mn oxides. These mechanisms were similar for both remediation strategies, indicating the general effectiveness of Co(II) removal by these oxides. The mycogenic Mn oxides were primarily a nanoparticulate, poorly-crystalline birnessite-like phases with slight differences depending on the chemical conditions during formation. The relatively fast and complete removal of aqueous Co(II) during biomineralization as well as the subsequent structural incorporation of Co into the Mn oxide structure illustrated a sustainable cycle capable of continuously remediating Co(II) from metal-polluted environments.
天然存在的锰(Mn)氧化物矿物通常通过微生物对Mn(II)的氧化作用形成,从而产生具有高反应活性的纳米晶态Mn(III/IV)氧化物相,这种相能够影响许多金属(如Ni、Cu、Co和Zn)的吸收和释放。在形成过程中,生物成因的锰氧化物的结构和组成会在其他金属存在的情况下发生改变,这反过来又会影响这些矿物结合这些金属的能力。这些过程还会受到水环境化学性质以及所涉及微生物的类型和生理特性的进一步影响。对于典型的采矿和工业废水环境(如盐含量增加、营养物质含量低和金属浓度高)的相关条件尚未得到充分研究,因此限制了我们对金属与生物成因的锰氧化物相互作用的理解。通过整合地球化学、显微镜和光谱技术,我们研究了从明尼苏达州苏达矿分离出的Mn(II)氧化子囊菌Periconia sp. SMF1产生的锰氧化物从模拟采矿废水的合成水中去除金属共污染物Co(II)的能力。在相同条件下,我们比较了两种不同的应用修复策略:Co与真菌生成的锰氧化物共沉淀,以及Co与预先形成的真菌锰氧化物的吸附。真菌锰氧化物通过两种不同机制有效地从溶液中去除Co(II):掺入锰氧化物和吸附在锰氧化物上。这两种修复策略的这些机制相似,表明这些氧化物去除Co(II)的总体有效性。真菌生成的锰氧化物主要是纳米颗粒状、结晶度差的水钠锰矿样相,根据形成过程中的化学条件略有差异。生物矿化过程中水溶液中Co(II)的相对快速和完全去除,以及随后Co在锰氧化物结构中的结构掺入,说明了一个能够持续从金属污染环境中修复Co(II)的可持续循环。