Barpanda Prabeer, Ling Chris D, Oyama Gosuke, Yamada Atsuo
Department of Chemical System Engineering, The University of Tokyo, 7-3-1 Hongo, Bunkyo-ku, Tokyo 113-8656, Japan.
Acta Crystallogr B Struct Sci Cryst Eng Mater. 2013 Dec;69(Pt 6):584-8. doi: 10.1107/S2052519213024093. Epub 2013 Nov 1.
The crystal structure of the NaMnSO4F fluorosulfate phase prepared by low-temperature solid-state synthesis has been solved and refined by the Rietveld analysis of synchrotron X-ray powder diffraction data. Isostructural to the naturally occurring triplite family of minerals, this compound crystallizes in monoclinic C2/c symmetry (No. 15) with unit-cell parameters of a = 13.77027 (17), b = 6.63687 (8), c = 10.35113 (14) Å, β = 121.4795 (3)° and V = 806.78 (2) Å(3). Its structure is built of edge-sharing chains of distorted MO4F2 octahedra, which are interconnected by constituent SO4 tetrahedra to form a robust three-dimensional polyanionic framework. MO4F2 octahedra are randomly occupied by Na and Mn with close to 1:1 occupancy. This random mixing of cations among polyhedral building blocks means that there are no channels for Na-ion conduction, rendering it electrochemically inactive. The structure is discussed and compared with other known alkali metal fluorosulfates as well as to naturally occurring triplite-type minerals.
通过对同步辐射X射线粉末衍射数据进行Rietveld分析,已解析并精修了通过低温固态合成制备的NaMnSO₄F氟硫酸盐相的晶体结构。该化合物与天然存在的磷铁锂矿族矿物同构,结晶于单斜C2/c对称(编号15),晶胞参数为a = 13.77027 (17),b = 6.63687 (8),c = 10.35113 (14) Å,β = 121.4795 (3)°,V = 806.78 (2) ų。其结构由扭曲的MO₄F₂八面体的边共享链构成,这些链通过组成的SO₄四面体相互连接,形成一个坚固的三维聚阴离子框架。MO₄F₂八面体由Na和Mn随机占据,占有率接近1:1。阳离子在多面体结构单元之间的这种随机混合意味着不存在Na离子传导通道,使其在电化学上不活跃。本文对该结构进行了讨论,并与其他已知的碱金属氟硫酸盐以及天然存在的磷铁锂矿型矿物进行了比较。