FeC4H4O6·2.5H2O晶体生长、结构和热研究

T. Fukami, S. Tahara
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引用次数: 0

摘要

采用硅胶凝胶法制备半五水酒石酸铁(II)单晶FeC4H4O6·2.5H2O。对单晶进行了差示扫描量热法、热重-差示热分析和x射线衍射测量。在室温下测定了空间群对称性(正交P212121)和结构参数。晶体结构由轻微扭曲的FeO6八面体、C4H4O6和H2O分子、由Fe-O键连接的C4H4O6 - fe - C4H4O6链和相邻分子之间的O - h···O氢键框架组成。在300 - 1060k的温度范围内,由于晶体的热分解引起的重量损失被发现。我们推测失重是由结合水分子蒸发和由C4H4O6分子演化出H2CO、CO和O2气体引起的,分解后的黑色残渣由四氧化三铁(Fe3O4)和碳组成。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Crystal Growth, Structural and Thermal Studies of FeC4H4O6·2.5H2O
Single crystals of iron(II) tartrate hemi-pentahydrate, FeC4H4O6·2.5H2O, were grown by the gel method using silica gels. Differential scanning calorimetry, thermogravimetric-differential thermal analysis, and X-ray diffraction measurements were performed on the single crystals. The space group symmetry (orthorhombic P212121) and structural parameters were determined at room temperature. The crystal structure consisted of slightly distorted FeO6 octahedra, C4H4O6 and H2O molecules, C4H4O6–Fe–C4H4O6 chains jointed by Fe–O bonds, and O–H···O hydrogen-bonding frameworks between adjacent molecules. Weight losses due to thermal decomposition of the crystal were found to occur in the temperature range of 300–1060 K. We inferred that the weight losses were caused by the evaporation of bound water molecules and the evolution of H2CO, CO, and O2 gases from C4H4O6 molecules, and that the black residue after decomposition was composed of triiron tetraoxide (Fe3O4) and carbon.
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