Norberg Stefan T
Inorganic Chemistry, Chalmers University of Technology, SE-412 96 Göteborg, Sweden.
Acta Crystallogr B. 2002 Oct;58(Pt 5):743-9. doi: 10.1107/s0108768102013782. Epub 2002 Sep 24.
Three new potassium rare-earth/titanium phosphate structures, K(2)ErTi(PO(4))(3) (KErTP), K(2)YbTi(PO(4))(3) (KYbTP) and K(2)YTi(PO(4))(3) (KYTP), are presented, all of which are characterized by single-crystal X-ray diffraction studies. In addition, a fourth structure, K(2)CrTi(PO(4))(3) (KCrTP), has been reinvestigated. All structures are isostructural to the langbeinite-type structure and result from changes made to the growth constituents in high-temperature flux-growth experiments intended to give structurally modified potassium titanyl phosphate (KTP). The two crystallographically independent octahedra sites (site symmetry 3) have a mixed Ti/M (M = Er, Yb, Y or Cr) population, although the rare-earth metals favour one site while chromium favours the other. An alternative approach for the description of the channels and cation cages in langbeinite and related structures is given using [M(5)X(6)O(39)] units. The framework of langbeinite is compared with that of nasicon using these alternative building units. All of the investigated structures crystallize in space group P2(1)3 with Z = 4; a = 10.1053 (2) A, R = 0.023 (KErTP); a = 10.0939 (8) A, R = 0.022 (KYbTP); a = 10.1318 (6) A, R = 0.047 (KYTP); a = 9.8001 (2) A, R = 0.016 (KCrTP).
本文介绍了三种新型钾稀土/钛磷酸盐结构,即K₂ErTi(PO₄)₃(KErTP)、K₂YbTi(PO₄)₃(KYbTP)和K₂YTi(PO₄)₃(KYTP),所有这些结构均通过单晶X射线衍射研究进行了表征。此外,还对第四种结构K₂CrTi(PO₄)₃(KCrTP)进行了重新研究。所有结构均与无水钾镁矾型结构同构,是在高温助熔剂生长实验中对生长成分进行改变后得到的,这些实验旨在得到结构改性的钛氧磷酸钾(KTP)。尽管稀土金属倾向于占据一个位点,而铬倾向于占据另一个位点,但两个晶体学独立的八面体位点(位点对称性3)具有混合的Ti/M(M = Er、Yb、Y或Cr)占据情况。使用[M₅X₆O₃₉]单元给出了一种描述无水钾镁矾及相关结构中通道和阳离子笼的替代方法。利用这些替代构建单元,将无水钾镁矾的骨架与钠超离子导体的骨架进行了比较。所有研究的结构均结晶于空间群P2₁3,Z = 4;a = 10.1053 (2) Å,R = 0.023(KErTP);a = 10.0939 (8) Å,R = 0.022(KYbTP);a = 10.1318 (6) Å,R = 0.047(KYTP);a = 9.8001 (2) Å,R = 0.016(KCrTP)。