Wang Guangmei, Valldor Martin, Spielberg Eike T, Mudring Anja-Verena
Inorganic Chemistry III-Materials Engineering and Characterization, Ruhr-Universität Bochum , D-44780 Bochum, Germany.
Inorg Chem. 2014 Mar 17;53(6):3072-7. doi: 10.1021/ic4029904. Epub 2014 Mar 5.
A new framework cobalt(II) hydroxyl phosphate, Co2PO4OH, was prepared by ionothermal synthesis using 1-butyl-4-methyl-pyridinium hexafluorophosphate as the ionic liquid. As the formation of Co2PO4F competes in the synthesis, the synthesis conditions have to be judiciously chosen to obtain well-crystallized, single phase Co2PO4OH. Single-crystal X-ray diffraction analyses reveal Co2PO4OH crystallizes with space group I41/amd (a = b = 5.2713(7) Å, c = 12.907(3) Å, V = 358.63(10) Å(3), and Z = 4). Astonishingly, it does not crystallize isotypically with Co2PO4F but rather isotypically with the hydroxyl minerals caminite Mg1.33[SO4(OH)0.66(H2O)0.33] and lipscombite Fe(2–y)PO4(OH) (0 ≤ y ≤ 2/3). Phosphate tetrahedra groups interconnect four rod-packed face-sharing ∞(1){CoO(6/2)} octahedra chains to form a three-dimensional framework structure. The compound Co2PO4OH was further characterized by powder X-ray diffraction, Fourier transform–infrared, and ultraviolet–visible spectroscopy, confirming the discussed structure. The magnetic measurement reveals that Co2PO4OH undergoes a magnetic transition and presents at low temperatures a canted antiferromagnetic spin order in the ground state.
采用1-丁基-4-甲基吡啶六氟磷酸盐作为离子液体,通过离子热合成法制备了一种新型骨架钴(II)羟基磷酸盐Co2PO4OH。由于在合成过程中会竞争生成Co2PO4F,因此必须谨慎选择合成条件,以获得结晶良好的单相Co2PO4OH。单晶X射线衍射分析表明,Co2PO4OH结晶为空间群I41/amd(a = b = 5.2713(7) Å,c = 12.907(3) Å,V = 358.63(10) Å(3),Z = 4)。令人惊讶的是,它与Co2PO4F不是同型结晶,而是与羟基矿物水碳镁石Mg1.33[SO4(OH)0.66(H2O)0.33]和磷铁锂石Fe(2–y)PO4(OH)(0 ≤ y ≤ 2/3)同型结晶。磷酸四面体基团连接四个棒状堆积、面共享的∞(1){CoO(6/2)}八面体链,形成三维骨架结构。通过粉末X射线衍射、傅里叶变换红外光谱和紫外可见光谱对化合物Co2PO4OH进行了进一步表征,证实了所讨论的结构。磁性测量表明,Co2PO4OH发生了磁转变,在低温下基态呈现倾斜反铁磁自旋序。