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碱土金属(镁、钙、锶、钡)在石墨插层化合物中的可逆M-M键合

Reversible M-M Bonding by Alkaline Earth Metals (Mg, Ca, Sr, Ba) in Graphite Intercalation Compounds.

作者信息

Xu Wei, Kozma Karoly, Sha Tianxiang, Wu Yi-Jen, Nyman May, Lerner Michael M

机构信息

Department of Chemistry, Oregon State University, Corvallis, Oregon, 97331-4003, United States.

出版信息

Chemistry. 2020 Jun 26;26(36):8101-8104. doi: 10.1002/chem.202000504. Epub 2020 Jun 2.

Abstract

The alkaline earth metals (M=Mg, Ca, Sr, and Ba) exhibit a +2 oxidation state in nearly all known stable compounds, but M dimeric complexes with M-M bonding, [M (en) ] , (en=ethylenediamine) of all these metals can be stabilized within the galleries of donor-type graphite intercalation compounds (GICs). These metals can also form GICs with more conventional metal (II) ion complexes, [M(en) ] . Here, the facile interconversion between dimeric-M and monomeric-M intercalates upon the addition/removal of en are reported. Thermogravimetry, powder X-ray diffraction, and pair distribution function analysis of total scattering data support the presence of either [M (en) ] or [M(en) ] guests. This phase conversion requires coupling graphene and metal redox centers, with associated reversible M-M bond formation within graphene galleries. This chemistry allows the facile isolation of unusual oxidation states, reveals M →M reaction pathways, and present new opportunities in the design of hybrid conversion/intercalation materials for applications such as charge storage.

摘要

碱土金属(M = Mg、Ca、Sr和Ba)在几乎所有已知的稳定化合物中都呈现 +2 氧化态,但所有这些金属的具有M - M键的M二聚体配合物[M(en)₂]₂(en = 乙二胺)可以在供体型石墨插层化合物(GICs)的层间稳定存在。这些金属还可以与更传统的金属(II)离子配合物[M(en)₂]形成GICs。在此,报道了在添加/去除乙二胺时二聚体 - M和单体 - M插层物之间的 facile 相互转化。热重分析、粉末X射线衍射以及总散射数据的对分布函数分析支持了[M(en)₂]₂或[M(en)₂]客体的存在。这种相转化需要石墨烯和金属氧化还原中心的耦合,以及在石墨烯层间伴随的可逆M - M键形成。这种化学性质允许 facile 分离不寻常的氧化态,揭示M → M反应途径,并为诸如电荷存储等应用的混合转化/插层材料设计提供新的机会。

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