Reduction of Manganese Oxides: Thermodynamic, Kinetic and Mechanistic Considerations for One- Versus Two-Electron Transfer Steps

IF 1.7 4区 地球科学 Q3 GEOCHEMISTRY & GEOPHYSICS Aquatic Geochemistry Pub Date : 2018-07-28 DOI:10.1007/s10498-018-9342-1
George W. Luther III, Aubin Thibault de Chanvalon, Véronique E. Oldham, Emily R. Estes, Bradley M. Tebo, Andrew S. Madison
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引用次数: 25

Abstract

Manganese oxides, typically similar to δ-MnO2, form in the aquatic environment at near neutral pH via bacterially promoted oxidation of Mn(II) species by O2, as the reaction of [Mn(H2O)6]2+ with O2 alone is not thermodynamically favorable below pH of ~?9. As manganese oxide species are reduced by the triphenylmethane compound leucoberbelein blue (LBB) to form the colored oxidized form of LBB (λmax?=?623?nm), their concentration in the aquatic environment can be determined in aqueous environmental samples (e.g., across the oxic–anoxic interface of the Chesapeake Bay, the hemipelagic St. Lawrence Estuary and the Broadkill River estuary surrounded by salt marsh wetlands), and their reaction progress can be followed in kinetic studies. The LBB reaction with oxidized Mn solids can occur via a hydrogen atom transfer (HAT) reaction, which is a one-electron transfer process, but is unfavorable with oxidized Fe solids. HAT thermodynamics are also favorable for nitrite with LBB and MnO2 with ammonia (NH3). Reactions are unfavorable for NH4+ and sulfide with oxidized Fe and Mn solids, and NH3 with oxidized Fe solids. In laboratory studies and aquatic environments, the reduction of manganese oxides leads to the formation of Mn(III)-ligand complexes [Mn(III)L] at significant concentrations even when two-electron reductants react with MnO2. Key reductants are hydrogen sulfide, Fe(II) and organic ligands, including the siderophore desferioxamine-B. We present laboratory data on the reaction of colloidal MnO2 solutions (λmax?~?370?nm) with these reductants. In marine waters, colloidal forms of Mn oxides (<?0.2?μm) have not been detected as Mn oxides are quantitatively trapped on 0.2-μm filters. Thus, the reactivity of Mn oxides with reductants depends on surface reactions and possible surface defects. In the case of MnO2, Mn(IV) is an inert cation in octahedral coordination; thus, an inner-sphere process is likely for electrons to go into the empty e *g conduction band of its orbitals. Using frontier molecular orbital theory and band theory, we discuss aspects of these surface reactions and possible surface defects that may promote MnO2 reduction using laboratory and field data for the reaction of MnO2 with hydrogen sulfide and other reductants.

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锰氧化物的还原:一电子与二电子转移步骤的热力学、动力学和机理考虑
锰氧化物通常与δ-MnO2类似,在接近中性pH的水生环境中,通过细菌促进O2氧化Mn(II)种,因为[Mn(H2O)6]2+单独与O2的反应在热力学上不有利,pH低于~?9。氧化锰被三苯基甲烷化合物白蛋白蓝(LBB)还原形成有色氧化态LBB (λmax?=?623?nm),因此可以在水环境样品中测定其在水生环境中的浓度(例如,在切萨ake湾、半深海圣劳伦斯河口和盐沼湿地环绕的Broadkill河河口的氧-缺氧界面),并可以在动力学研究中跟踪其反应过程。与氧化Mn固体的LBB反应可以通过氢原子转移(HAT)反应进行,这是一个单电子转移过程,但与氧化Fe固体的LBB反应是不利的。HAT热力学也有利于亚硝酸盐与LBB和MnO2与氨(NH3)的反应。NH4+和硫化物与氧化的铁、锰固体以及NH3与氧化的铁固体的反应均不利。在实验室研究和水生环境中,即使双电子还原剂与MnO2反应,锰氧化物的还原也会导致形成显著浓度的Mn(III)-配体复合物[Mn(III)L]。关键还原剂是硫化氢、铁(II)和有机配体,包括铁载体去铁异胺- b。我们提供了MnO2胶体溶液(λmax ~ 370 nm)与这些还原剂反应的实验室数据。在海水中,未检测到Mn氧化物(0.2 μm)的胶体形式,因为Mn氧化物被定量捕获在0.2 μm过滤器上。因此,锰氧化物与还原剂的反应性取决于表面反应和可能的表面缺陷。在MnO2的情况下,Mn(IV)在八面体配位中是惰性阳离子;因此,一个内球过程很可能使电子进入其轨道的空e *g导带。利用前沿分子轨道理论和能带理论,我们利用MnO2与硫化氢和其他还原剂反应的实验室和现场数据,讨论了这些表面反应的各个方面以及可能促进MnO2还原的表面缺陷。
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来源期刊
Aquatic Geochemistry
Aquatic Geochemistry 地学-地球化学与地球物理
CiteScore
4.30
自引率
0.00%
发文量
6
审稿时长
1 months
期刊介绍: We publish original studies relating to the geochemistry of natural waters and their interactions with rocks and minerals under near Earth-surface conditions. Coverage includes theoretical, experimental, and modeling papers dealing with this subject area, as well as papers presenting observations of natural systems that stress major processes. The journal also presents `letter''-type papers for rapid publication and a limited number of review-type papers on topics of particularly broad interest or current major controversy.
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