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Preparation and Properties of an MnIV–Hydroxide Complex: Proton and Electron Transfer at a Mononuclear Manganese Site and its Relationship to the Oxygen Evolving Complex within Photosystem II

机译:MnIV-氢氧化物配合物的制备和性质:在单核锰位点的质子和电子转移及其与光系统II中放氧配合物的关系

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摘要

Photosynthetic water oxidation is catalyzed by a Mn4O5Ca cluster with an unprecedented arrangement of metal ions in which a single manganese center is bonded to a distorted Mn3O4Ca cubane-like structure. Several mechanistic proposals describe the unique manganese center as a site for water binding and subsequent formation of a high valent Mn–oxo center that reacts with a M–OH unit (M = Mn or CaII) to form the O–O bond. The conversion of low valent Mn–OHn (n = 1,2) to a Mn–oxo species requires that a single manganese site be able to accommodate several oxidation states as the water ligand is deprotonated. To study these processes, the preparation and characterization of a new monomeric MnIV–OH complex is described. The MnIV–OH complex completes a series of well characterized Mn–OH and Mn–oxo complexes containing the same primary and secondary coordination spheres; this work thus demonstrates that a single ligand can support mononuclear Mn complexes spanning four different oxidation states (II through V) with oxo and hydroxo ligands that are derived from water. Moreover, we have completed a thermodynamic analysis based on this series of manganese complexes to predict the formation of high valent Mn–oxo species; we demonstrated that the conversion of a MnIV–OH species to a MnV–oxo complex would likely occur via a stepwise proton transfer-electron transfer mechanism. The large dissociation energy for the MnIVO–H bond (~95 kcal/mol) diminished the likelihood that other pathways are operative within a biological context. Furthermore, these studies showed that reactions between Mn–OH and Mn–oxo complexes lead to non-productive, one-electron processes suggesting that initial O–O bond formation with the OEC does not involve an Mn–OH unit.
机译:Mn4O5Ca团簇以前所未有的金属离子排列催化光合水的氧化,其中单个锰中心键合到扭曲的Mn3O4Ca古巴样结构上。一些机制性建议将独特的锰中心描述为与水结合的位点,随后形成了高价的Mn-氧中心,该中心与M-OH单元(M = Mn或Ca II )反应形成O-O键。低价Mn-OHn(n = 1,2)转变为Mn-oxo物种要求在水配体去质子化时,一个锰位点能够容纳多个氧化态。为了研究这些过程,描述了一种新型的单体Mn IV -OH配合物的制备和表征。 Mn IV -OH配合物完成了一系列特征明确的Mn-OH和Mn-oxo配合物,它们包含相同的一级和二级配位球。因此,这项工作证明了单个配体可以支持跨越四个不同氧化态(II到V)的单核Mn配合物,这些配体具有衍生自水的氧代和羟基配体。此外,我们已经基于这一系列的锰配合物完成了热力学分析,以预测高价Mn-oxo物种的形成。我们证明了Mn IV -OH物种向Mn V -oxo配合物的转化很可能是通过逐步质子转移-电子转移机制发生的。 Mn IV O–H键的大解离能(〜95 kcal / mol)降低了其他途径在生物学环境中起作用的可能性。此外,这些研究表明,Mn-OH和Mn-oxo配合物之间的反应导致非生产性单电子过程,这表明与OEC形成的初始O-O键不涉及Mn-OH单元。

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