Hatert Frédéric
University of Liège, Laboratory of Mineralogy B.18, B-4000 Liège, Belgium.
Acta Crystallogr C. 2006 Jan;62(Pt 1):i1-2. doi: 10.1107/S0108270105037236. Epub 2005 Dec 10.
The first hydrothermal synthesis of an Al-rich alluaudite-type compound, namely disodium dimanganese aluminium tris(phosphate), which has been obtained at 1073 K and 0.1 GPa starting from the composition Na2Mn2Al(PO4)3, is reported. The crystal structure, which has been refined in the monoclinic C2/c space group, is identical to that of natural alluaudite. The structure consists of kinked chains of edge-sharing M1 and M2 octahedra, which contain Mn2+ and Al3+ ions. The chains are stacked parallel to {101} and are connected in the b direction by the P1 and P2 tetrahedra. These interconnected chains produce channels parallel to c, which contain the large A1 and A2' sites occupied by Na+ and Mn2+ ions.
报道了首次通过水热合成法制备富铝磷铝锰钠石型化合物,即二钠二锰铝三(磷酸)盐,该化合物是在1073 K和0.1 GPa条件下,以Na2Mn2Al(PO4)3为原料合成得到的。其晶体结构在单斜C2/c空间群中进行了精修,与天然磷铝锰钠石的结构相同。该结构由边缘共享的M1和M2八面体组成的扭结链构成,其中包含Mn2+和Al3+离子。这些链平行于{101}堆叠,并在b方向上通过P1和P2四面体相连。这些相互连接的链产生平行于c的通道,其中包含被Na+和Mn2+离子占据的大的A1和A2'位点。