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Structure of the new iron(II) oxalate potassium salt K2Fe[(C2O4)2(H2O)2]·0.18H2O
Acta Crystallographica Section B ( IF 2.684 ) Pub Date : 2023-06-22 , DOI: 10.1107/s2052520623004602
Sara Amanchar 1 , Thierry Schweitzer 1 , Thomas Mazet 1 , Bernard Malaman 1 , Leopold V B Diop 1 , Michel Francois 1
Affiliation  

The discovery of a new FeII oxalate framework of composition K2Fe[(C2O4)2(H2O)2]·0.18H2O is reported. Its crystal structure was solved by means of single crystal and powder X-ray diffraction. The new organic–inorganic hybrid compound crystallizes in the orthorhombic space group Pca21 with unit-cell parameters: a = 12.0351 (4) Å, b = 15.1265 (5) Å, c = 10.5562 (4) Å. This crystal structure, containing eight chemical formula, consists of a succession of FeO4(H2O)2 octahedra and K+ cations growing along b direction. Magnetization measurements indicate that the title compound is paramagnetic over the investigated temperature range (2–300 K). Both magnetization and 57Fe Mössbauer data indicate that Fe2+ is in a high-spin state.

中文翻译:

新型草酸亚铁钾盐K2Fe[(C2O4)2(H2O)2]·0.18H2O的结构

报道了一种新的草酸铁II骨架的发现,其组成为K 2 Fe[(C 2 O 4 ) 2 (H 2 O) 2 ]·0.18H 2 O。通过单晶和粉末X射线衍射解析了其晶体结构。新的有机-无机杂化化合物在斜方空间群Pca 2 1中结晶,晶胞参数为:a = 12.0351 (4) Å, b = 15.1265 (5) Å, c = 10.5562 (4) Å。该晶体结构包含八个化学式,由一系列沿b方向生长的FeO 4 (H 2 O) 2八面体和K +阳离子组成。磁化测量表明标题化合物在研究的温度范围 (2–300 K) 内具有顺磁性。磁化强度和57 Fe 穆斯堡尔数据都表明 Fe 2+处于高自旋状态。
更新日期:2023-06-22
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