SYNTHESIS AND CRYSTAL STRUCTURE OF NEW OXIDE MATERIALS IN CaO-Y2O3-SiO2 SYSTEM

Toru Nagasawa, Hisanori Yamane and Masahiko Shimada

Institute for Advanced Materials Processing, Tohoku University, 2-1-1, Katahira, Aoba-ku, Sendai, Miyagi 980-8577, Japan, E-mail : shimada@ibis.iamp.tohoku.ac.jp

Keywords : rare-earth calcium silicates, cuspidine-type structure, silico-carnotite-type,structure, apatite-type structure

Oxides including rare-earth elements have possibility to become phosphor and laser materials because of doping activated rare-earth ions. Actually, some of these oxides are used practically as laser and phosphor materials. Finding a new compounds including rare-earth elements is needed to make more efficient materials.

In CaO-Y2O3-SiO2 ternary system, apatite-type structure compounds have been reported at the compositions of Ca2Y8Si6O26 and Ca3Y6Si6O24 [l, 2]. It was pointed out that the real chemical composition of apatite-type compounds had not been established. The preparation of Ca2Y2Si2O9 having a cuspidine-type structure was carried out [3], but the crystallographic data has not been reported yet. Generally, silicates have many isomorphs and form many complicated structures. For this reason, new compounds having new structures would be expected in this multicomponent system. The present study attempted to prepare the compounds in CaO- Y2O3-SiO2 ternary system and make clear their crystal structures.

CaCO3, SiO2 and Y8O3 powders were used as starting materials. These powders were weighed and mixed with ethanol. After drying and pelletizing, the samples were sintered on a Pt-Rh plate at 1700 K for 72 h in air. This sintering process was repeated until the X-ray diffraction pattern was unchanged. The sintered pellets were ground into powder and characterized by X-ray diffraction. The crystal structures of these compounds were refined by Rietveld analysis. Single crystals of new compounds, Ca3Y2Si3O12 and Ca3Y2Si6O18, were prepared from melts by slow cooling. The crystal structures were analyzed by single crystal X-ray diffraction. In CaO-SiO2, SiO2-Y2O3 and CaO-Y2O3 binary systems, the following compounds were prepared at 1673- 1700 K; CaSiO3, Ca3Si2O7, Ca2SiO4, Ca3SiO5, Y2Si2O7 and Y2SiO5. These results agreed with previous reports. In CaO-Y2O3-SiO2 ternary system, the compounds prepared by reaction sintering at 1700 K were Ca2Y2Si6O26 (apatite-type structure), Ca2Y2Si2O9 (cuspidine-type structure), Ca3Y2Si3O12 (silico-carnotite-type structure) and Ca3Y2Si6O18(new structure). These results are shown in Fig.1.

A single-phase having an apatite-type structure was prepared at Ca2Y8Si6O26. This phase is hexagonal, a = b = 0.9341(1), c = 0.6788(1) nm. The sample with the composition of Ca3Y6Si6O24 which was reported as apatite- type compound was two phase, Ca2Y8Si6O26 and CaSiO3. The sample prepared at the composition of Ca4Y6Si6O25 consisted of Ca2Y8Si6O26 and Ca3Y2Si3O12. It was confirmed that Ca2Y2Si2O9 had a cuspidine-type structure (monoclinic P 21/c, a = 0.74468(3), b =1.049240(3), c =1.09C61(4) nm, b =110.170(3)o).

The new compound, Ca3Y2Si3O12 is isostructual with silico-carnotite (Ca5(PO4)2SiO4). Ca3Y2Si3O12 is orthorhombic with space group Pnma, a = 0.65574(2), b =1.56066(3), c =1.00399(2) nm, and has nine -eight- and seven-coordinate sites for Ca2+ and Y3+ cations. Ca3Y2Si6O18 (monoclinic C 2/c, a =1.33422(5), b = 0.77320(3), c =1.47959(6) nm, b = 90.263(3)o) is composed of ternary SiO4 rings. Ca and Y atoms are in eight-, seven- and sixfold coordination sites between the layers of ternary SiO4 rings(Si3O9).

l. J. Ito, Am. Mineral. 53 (1968) 0-907
2. W. L. Wanmaker, J. W. Vrugt and J. G. Verlijsdonk, Philips Rep. 26 (1971 )373-381
3. I. Warshaw and R. Roy, Inorg. Chem.1 (1962) 719-720