咔唑分子在荧光环境中产生的新支链铁(III)配合物:合成与结构、静态磁性和共振特性

IF 2.6 4区 化学 Q2 CHEMISTRY, INORGANIC & NUCLEAR
D. Starichenko, V. Vorobeva, M. Gruzdev, U. Chervonova, Nataliya G. Bichan, Aleksander V. Korolev, Ivan V. Yatsyk
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引用次数: 0

摘要

利用水杨醛的咔唑衍生物与 N'-乙基乙二胺的缩合反应合成了希夫碱与各种铁(III)盐的支链配合物,命名为 G2-[L2Fe]+A-(A-为 NO3-、Cl-、PF6-),并通过各种光谱方法(GPC、IR、1H NMR、UV/Vis)对其进行了表征。研究结果表明,两种配体分子通过氮离子和偶氮甲基的氧原子与金属配位,形成一个同色体系。研究人员对所有合成的配位化合物进行了热学、光学和磁学特征检测。静态磁性测量结果表明,只有 G2-[L2Fe]Cl 处于单相 HS 状态,而 G2-[L2Fe]NO3 和 G2-[L2Fe]PF6 的铁(III)离子在室温下处于低自旋(LS,S = 1/2)和高自旋(HS,S = 5/2)混合状态:G2-[L2Fe]NO3的LS态占58.9%,HS态占41.1%;G2-[L2Fe]PF6的LS态占56.1%,HS态占43.9%。所有 G2-[L2Fe]+A- 复合物都显示出相邻铁(III)离子之间的反铁磁交换相互作用。2.0 K 时的基自旋态显示,非相互作用的 LS 离子和一定比例的 HS 铁(III)离子参与了布里渊作用,但不参与反铁磁相互作用:G2-[L2Fe]Cl、G2-[L2Fe]NO3 和 G2-[L2Fe]PF6分别为 57%、18% 和 16%。EPR 测量证实了铁(III)离子存在磁活性 HS 和 LS 状态,并区分了两种 HS 类型--强的低对称性(I 型)和弱的扭曲八面体环境(II 型)。研究表明,G2-[L2Fe]+A- 复合物在磁性上是不均匀的,由两个磁性子晶格组成:层中的 AFM 相关链来自 I 型 HS 铁(III)中心,而动态短程 AFM 有序 LS/II 型 HS 铁(III)中心位于层间的顺磁相。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
New Branched Iron(III) Complexes in Fluorescent Environment Created by Carbazole Moieties: Synthesis and Structure, Static Magnetic and Resonance Properties
The branched complexes of Schiff bases with various iron(III) salts, named G2-[L2Fe]+A− (A− is NO3−, Cl−, PF6−), were synthesized using the condensation reaction between carbazole derivatives of salicylic aldehyde and N’-ethylethylenediamine and characterized by various spectroscopic methods (GPC, IR, 1H NMR, UV/Vis). The studies revealed that the coordination of the two ligand molecules to metal occurs through the nitrogen ions and oxygen atom of azomethine to form a homoleptic system. All the synthesized coordination compounds were examined for their thermal, optical, and magnetic features. Static magnetic measurements showed that only G2-[L2Fe]Cl was in a single-phase HS state, whereas the Fe(III) ions of G2-[L2Fe]NO3 and G2-[L2Fe]PF6 at room temperatures were in mixed low-spin (LS, S = 1/2) and high-spin (HS, S = 5/2) states: 58.9% LS/41.1% HS for G2-[L2Fe]NO3, 56.1% LS and 43.9% HS for G2-[L2Fe]PF6. All G2-[L2Fe]+A− complexes demonstrate antiferromagnetic exchange interactions between neighboring Fe(III) ions. The ground spin state at 2.0 K revealed a Brillouin contribution from non-interacting LS ions and a proportion of the HS Fe(III) ions not participating in AFM interactions: 57%, 18%, and 16% for G2-[L2Fe]Cl, G2-[L2Fe]NO3 and G2-[L2Fe]PF6, respectively. EPR measurements confirmed the presence of magnetically active HS and LS states of Fe(III) ions and made it possible to distinguish two HS types-with strong low-symmetry (I-type) and weak, distorted octahedral environments (II-type). It was shown that G2-[L2Fe]+A− complexes are magnetically inhomogeneous and consist of two magnetic sub-lattices: AFM-correlated chains in layers from the I-type HS Fe(III) centers and dynamic short-range AFM ordered LS/II-type HS Fe(III) centers in the paramagnetic phase located between the layers.
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来源期刊
Magnetochemistry
Magnetochemistry Chemistry-Chemistry (miscellaneous)
CiteScore
3.90
自引率
11.10%
发文量
145
审稿时长
11 weeks
期刊介绍: Magnetochemistry (ISSN 2312-7481) is a unique international, scientific open access journal on molecular magnetism, the relationship between chemical structure and magnetism and magnetic materials. Magnetochemistry publishes research articles, short communications and reviews. Our aim is to encourage scientists to publish their experimental and theoretical results in as much detail as possible. Therefore, there is no restriction on the length of the papers. The full experimental details must be provided so that the results can be reproduced.
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