Miyazaki A, Yamazaki H, Aimatsu M, Enoki T, Watanabe R, Ogura E, Kuwatani Y, Iyoda M
Department of Chemistry, Tokyo Institute of Technology, O-okayama, Meguro-ku, Tokyo 152-8551, Japan.
Inorg Chem. 2007 Apr 16;46(8):3353-66. doi: 10.1021/ic061871y. Epub 2007 Mar 17.
The crystal structure and physical properties of radical ion salts (EDO-TTFBr2)2FeX4 (X = Cl, Br) based on halogen-substituted organic donor and magnetic anions are investigated, including the comparison with the isomorphous compounds (EDO-TTFBr2)2GaX4 with nonmagnetic anions. The crystal structure of these four salts consists of uniformly stacked donor molecules and tetrahedral counter anions, and the Br substituents of the donor molecules are connected to halide ligands of anions with remarkably short intermolecular atomic distances. These salts show metallic behavior around room temperature and undergo a spin-density-wave transition in the low-temperature range, as confirmed with the divergence of the electron spin resonance (ESR) line width. Although close anion-anion contacts are absent in these salts, the FeCl4 salt undergoes an antiferromagnetic transition at TN = 4.2 K, and the FeBr4 salt shows successive magnetic transitions at TN = 13.5 K and TC2 = 8.5 K with a helical spin structure as a candidate for the ground state of the d-electron spins. The magnetoresistance of the FeCl4 salt shows stepwise anomalies, which are explained qualitatively using a pi-d interaction-based frustrated spin system model composed of the donor pi-electron and the anion d-electron spins. Although on the ESR spectra of the FeX4 salts signals from the pi- and d-electron spins are separately observed, the line width of the pi-electron spins broadens under the temperature where the susceptibility deviates from the Curie-Weiss behavior, showing the presence of the pi-d interaction.
研究了基于卤素取代有机给体和磁性阴离子的自由基离子盐(EDO-TTFBr2)2FeX4(X = Cl, Br)的晶体结构和物理性质,包括与具有非磁性阴离子的同构化合物(EDO-TTFBr2)2GaX4的比较。这四种盐的晶体结构由均匀堆叠的给体分子和四面体抗衡阴离子组成,给体分子的Br取代基与阴离子的卤化物配体相连,分子间原子距离非常短。这些盐在室温附近表现出金属行为,并在低温范围内经历自旋密度波转变,电子自旋共振(ESR)线宽的发散证实了这一点。尽管这些盐中不存在紧密的阴离子-阴离子接触,但FeCl4盐在TN = 4.2 K时发生反铁磁转变,FeBr4盐在TN = 13.5 K和TC2 = 8.5 K时表现出连续的磁转变,其螺旋自旋结构是d电子自旋基态的候选结构。FeCl4盐的磁电阻显示出逐步异常,使用由给体π电子和阴离子d电子自旋组成的基于π-d相互作用的受挫自旋系统模型进行了定性解释。尽管在FeX4盐的ESR光谱上分别观察到了来自π电子和d电子自旋的信号,但在磁化率偏离居里-外斯行为的温度下,π电子自旋的线宽变宽,表明存在π-d相互作用。