具有烷基链取代基的同色低自旋铁(II)化合物中结晶双层的形成。

IF 4.3 3区 材料科学 Q1 ENGINEERING, ELECTRICAL & ELECTRONIC ACS Applied Electronic Materials Pub Date : 2024-11-04 DOI:10.1039/d4dt02667e
Blaise L Geoghegan, Spyridon Koutsoukos, Wasinee Phonsri, Keith S Murray, Peter J Cragg, Marcus K Dymond, Ian A Gass
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引用次数: 0

摘要

一系列基于表面结合的三叉配体 N-甲基-1,1-二(吡啶-2-基)Cn-胺(LCn)(Cn = 丁基、己基、辛基、癸基、十二烷基、十四烷基和十六烷基烷基链)的不对称同性铁(II)化合物,其式为其中 n = 4、14 和 X = BF4(1C4 和 1C14)或 n = 6、8、10、12、16 和 X = CF3SO3(1C6-1C12 和 1C16)。1C6 至 1C16 复合物在固态下形成结晶双层,在相邻复合物层之间形成疏水和亲水区域。较短的 Fe-N 键距离(∼2.00 Å)和 SQUID 磁感应强度测量结果表明,这些复合物在所有测量温度范围内都处于低自旋状态。差示扫描量热法证实,化合物 1C6、1C12、1C14 和 1C16 在从室温加热时发生了相变。在这一温度范围内,热重分析没有发现任何自旋跃迁和热稳定性,这表明这些跃迁属于晶体学性质。1H NMR 研究表明,低自旋铁(II)中心在溶液中部分转化为顺磁性物质。在一系列常见有机溶剂中进行的紫外-可见光谱分析显示,中心铁离子仍处于 +2 氧化态,这表明溶液中磁感应强度的增加很可能是由于部分自旋交叉,或者是由于物种分化,其中一部分化合物是高自旋铁(II)络合物。
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Crystalline bilayer formation in homoleptic low-spin Fe(II) compounds with alkyl chain substituents.

A series of asymmetric, homoleptic Fe(II) compounds based on the facially-binding tridentate ligand N-methyl-1,1-di(pyridin-2-yl)Cn-amine (LCn) (Cn = butyl, hexyl, octyl, decyl, dodecyl, tetradecyl and hexadecyl alkyl chains) with formula [FeII(LCn)2](X)2·solvate, where n = 4, 14 and X = BF4 (1C4 and 1C14) or n = 6, 8, 10, 12, 16 and X = CF3SO3 (1C6-1C12 and 1C16), are reported. Complexes 1C6 to 1C16 pack in crystalline bilayers in the solid state, forming hydrophobic and hydrophilic regions between adjacent layers of complexes. The combination of short Fe-N bond distances (∼2.00 Å) and SQUID magnetic susceptibility measurements show that the complexes are in the low-spin state across all measured temperature ranges. Differential scanning calorimetry confirmed phase transitions occur in compounds 1C6, 1C12, 1C14 and 1C16 upon heating from room temperature. The lack of any spin transitions and thermal stability conferred by thermogravimetric analysis over this temperature range suggest that these transitions are crystallographic in nature. 1H NMR studies show that the low-spin Fe(II) centres undergo partial conversion to paramagnetic species in solution. UV-vis spectroscopy in a range of common organic solvents show that the central Fe ions remain in the +2 oxidation state, suggesting that the increase in magnetic susceptibility in solution is likely due to partial spin-crossover, or due to speciation, in which a proportion of the compounds are high-spin Fe(II) complexes.

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