Oxidative Influence of the Presence of Dopant Atom on the Adsorption of Selenite Oxyanion on Manganese-Doped Hematite

IF 2.9 3区 化学 Q2 CHEMISTRY, MULTIDISCIPLINARY ACS Earth and Space Chemistry Pub Date : 2025-03-01 DOI:10.1021/acsearthspacechem.4c00278
Snigdha Srabanee, Ashutosh Srivastava, Sumit Kumar*, Vivekchandra G. Mishra, Sher Singh Meena, Raj B. Tokas, Jitendra Bahadur, Ankita Pathak and Sangita Dhara, 
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Abstract

Selenium could enter the environment through different anthropogenic sources, posing a potential health risk at higher concentrations. Although dopant atoms incorporated into the Fe(III) oxide lattice play a controlling role in the environmental speciation and fate of various contaminants, their role is poorly understood at the mechanistic level. The present study is an in situ investigation of the surface reactions of selenite oxyanion at the pristine/Mn-doped hematite (Mn-Ht)–water interface to delineate the role of the dopant in interfacial speciation and adsorption characteristics of the selenium oxyanion. Total and species-specific selenium ions present in the supernatant, estimated at the end of the equilibration of selenite ions with an aqueous suspension of the doped hematite, revealed the adsorption of selenite ions followed by their fast surface-induced oxidative transformation to selenate ions. This redox change of selenite ions was further characterized by using cyclic voltammetry and differential pulse voltammetry methods. Electrochemical evidence revealed an increased electron transfer (ET) rate constant (0.023–0.197 s–1) with Mn doping. The proposed mechanism is related to the suppression of electron–hole pair recombination with Mn doping in the hematite lattice. Due to the dopants, acceptor levels trap the photoelectrons produced in the Mn-Ht lattice; simultaneously, the photoholes collect in the valence band to execute the oxidative transformation of selenite anions to their oxidized species. As selenate exhibits weaker interactions with hematite than selenite ions, it is released into the supernatant phase. Our findings highlight the critical role that a dopant may play in mobilizing contaminants that otherwise will be strongly held by the pristine solid.

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掺杂原子的存在对亚硒酸盐氧阴离子在锰掺杂赤铁矿上吸附的氧化影响
硒可以通过不同的人为来源进入环境,在较高浓度下构成潜在的健康风险。虽然掺入Fe(III)氧化物晶格中的掺杂原子在各种污染物的环境形态和命运中起着控制作用,但它们在机制水平上的作用知之甚少。本研究对原生/ mn掺杂赤铁矿(Mn-Ht) -水界面上亚硒酸盐氧阴离子的表面反应进行了原位研究,以描述掺杂剂在界面形态和硒氧阴离子吸附特性中的作用。在亚硒酸盐离子与掺杂赤铁矿的水悬浮液平衡结束时,估计了上清中存在的总硒离子和种特异性硒离子,揭示了亚硒酸盐离子的吸附,然后是它们快速的表面诱导氧化转化为硒酸盐离子。利用循环伏安法和差分脉冲伏安法进一步表征亚硒酸盐离子的氧化还原变化。电化学证据表明,Mn掺杂增加了电子转移(ET)速率常数(0.023 ~ 0.197 s-1)。提出的机理与在赤铁矿晶格中掺杂锰抑制电子-空穴对复合有关。由于掺杂剂的存在,受体能级捕获了Mn-Ht晶格中产生的光电子;同时,光孔在价带中聚集,亚硒酸盐阴离子向其氧化态进行氧化转化。由于硒酸盐与赤铁矿的相互作用弱于亚硒酸盐离子,它被释放到上清相中。我们的研究结果强调了掺杂剂可能在动员污染物方面发挥的关键作用,否则这些污染物将被原始固体强烈持有。
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来源期刊
ACS Earth and Space Chemistry
ACS Earth and Space Chemistry Earth and Planetary Sciences-Geochemistry and Petrology
CiteScore
5.30
自引率
11.80%
发文量
249
期刊介绍: The scope of ACS Earth and Space Chemistry includes the application of analytical, experimental and theoretical chemistry to investigate research questions relevant to the Earth and Space. The journal encompasses the highly interdisciplinary nature of research in this area, while emphasizing chemistry and chemical research tools as the unifying theme. The journal publishes broadly in the domains of high- and low-temperature geochemistry, atmospheric chemistry, marine chemistry, planetary chemistry, astrochemistry, and analytical geochemistry. ACS Earth and Space Chemistry publishes Articles, Letters, Reviews, and Features to provide flexible formats to readily communicate all aspects of research in these fields.
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