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观察单核钴氮氧自由基中的铁磁交换、自旋交叉、还原诱导氧化和场诱导慢磁弛豫。

Observation of ferromagnetic exchange, spin crossover, reductively induced oxidation, and field-induced slow magnetic relaxation in monomeric cobalt nitroxides.

机构信息

School of Chemistry, Monash University, Clayton, Victoria 3800, Australia.

出版信息

Inorg Chem. 2013 Jul 1;52(13):7557-72. doi: 10.1021/ic400565h. Epub 2013 Jun 18.

Abstract

The reaction of [Co(II)(NO3)2]·6H2O with the nitroxide radical, 4-dimethyl-2,2-di(2-pyridyl) oxazolidine-N-oxide (L(•)), produces the mononuclear transition-metal complex Co(II)(L(•))22 (1), which has been investigated using temperature-dependent magnetic susceptibility, electron paramagnetic resonance (EPR) spectroscopy, electrochemistry, density functional theory (DFT) calculations, and variable-temperature X-ray structure analysis. Magnetic susceptibility measurements and X-ray diffraction (XRD) analysis reveal a central low-spin octahedral Co(2+) ion with both ligands in the neutral radical form (L(•)) forming a linear L(•)···Co(II)···L(•) arrangement. This shows a host of interesting magnetic properties including strong cobalt-radical and radical-radical intramolecular ferromagnetic interactions stabilizing a S = (3)/2 ground state, a thermally induced spin crossover transition above 200 K and field-induced slow magnetic relaxation. This is supported by variable-temperature EPR spectra, which suggest that 1 has a positive D value and nonzero E values, suggesting the possibility of a field-induced transverse anisotropy barrier. DFT calculations support the parallel alignment of the two radical π*NO orbitals with a small orbital overlap leading to radical-radical ferromagnetic interactions while the cobalt-radical interaction is computed to be strong and ferromagnetic. In the high-spin (HS) case, the DFT calculations predict a weak antiferromagnetic cobalt-radical interaction, whereas the radical-radical interaction is computed to be large and ferromagnetic. The monocationic complex Co(III)(L(-))2 (2) is formed by a rare, reductively induced oxidation of the Co center and has been fully characterized by X-ray structure analysis and magnetic measurements revealing a diamagnetic ground state. Electrochemical studies on 1 and 2 revealed common Co-redox intermediates and the proposed mechanism is compared and contrasted with that of the Fe analogues.

摘要

[Co(II)(NO3)2]·6H2O 与氮氧化物自由基,4-二甲基-2,2-二(2-吡啶基)恶唑啉-N-氧化物(L(•))反应,生成单核过渡金属配合物Co(II)(L(•))22(1),该配合物已通过温度依赖的磁化率、电子顺磁共振(EPR)光谱、电化学、密度泛函理论(DFT)计算和变温 X 射线结构分析进行了研究。磁化率测量和 X 射线衍射(XRD)分析表明,中心低自旋八面体 Co(2+)离子与两个配体均处于中性自由基形式(L(•)),形成线性 L(•)···Co(II)···L(•)排列。这显示了一系列有趣的磁性性质,包括强钴自由基和自由基自由基分子内铁磁相互作用,稳定 S = (3)/2 基态,在 200 K 以上的热诱导自旋交叉跃迁以及场诱导缓慢磁弛豫。这得到了变温 EPR 光谱的支持,表明 1 具有正 D 值和非零 E 值,表明存在场诱导横向各向异性势垒的可能性。DFT 计算支持两个自由基 π*NO 轨道的平行排列,具有较小的轨道重叠,导致自由基自由基铁磁相互作用,而钴自由基相互作用被计算为强且铁磁。在高自旋(HS)情况下,DFT 计算预测钴自由基相互作用较弱反铁磁,而自由基自由基相互作用被计算为大且铁磁。通过钴中心的罕见还原诱导氧化形成单阳离子配合物Co(III)(L(-))2(2),并通过 X 射线结构分析和磁性测量对其进行了全面表征,揭示了抗磁性基态。对 1 和 2 的电化学研究揭示了常见的 Co 氧化还原中间体,并比较和对比了该机制与 Fe 类似物的机制。

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