A calorimetric study of the lanthanide aluminum oxides and the lanthanide gallium oxides: Stability of the perovskites and the garnets

被引:120
作者
Kanke, Y
Navrotsky, A
机构
[1] Natl Inst Res Inorgan Mat, Tsukuba, Ibaraki 3050044, Japan
[2] Princeton Univ, Princeton Mat Inst, Princeton, NJ 08544 USA
[3] Princeton Univ, Dept Geosci, Princeton, NJ 08544 USA
基金
美国国家科学基金会;
关键词
D O I
10.1006/jssc.1998.7969
中图分类号
O61 [无机化学];
学科分类号
070301 ; 081704 ;
摘要
High-temperature solution calorimetry using a 2PbO . B2O3 solvent at 977 K was performed for LnMO(3) perovskites and Ln(3)M(5)O(12) garnets (Ln = La-Lu, Y; M = Al, Ga), alpha-Al2O3, and beta-Ga2O3. The following four reactions were discussed from the viewpoint of thermodynamic parameters, Delta H, Delta S, and Delta V; LnMO(3) = 1/5Ln(3)M(5)O(12) + 1/5Ln(2)O(3), Ln(3)M(5)O(12) = 3LnMO(3) + M2O3, 1/2Ln(2)O(3) + 1/2M(2)O(3) = LnMO(3), and (3)(2)Ln(2)O(3) + 5/2M(2)O(3) = Ln(3)M(5)O(12) The stability of LnMO(3) against the disproportionation to garnet plus sesquioxide is controlled almost entirely by Delta H and P Delta V but not by T Delta S. On the contrary, the stability of Ln(3)M(5)O(12) against disproportionation to perovskite plus sesquioxide is controlled not only by Delta H and P Delta V but also by T Delta S, The P-T boundary between Ln(3)M(5)O(12) and 3LnMO(3) + M2O3 has a negative slope. The positive ILS and negative Delta V for the disproportionation are caused by an increase in coordination number and an increase in bond distance. Delta H of perovskite formation is mainly controlled by two factors, the strengthening of the ionic bond in Ln(2)O(3) with decreasing ionic radius of Ln(3+) and the weakening of the ionic bond between Ln and the distant four O atoms in LnMO(3) with decreasing ionic radius of Ln(3+). Delta H Of garnet formation is mainly controlled by two factors, the strengthening of the ionic bond in Ln(2)O(3) with decreasing ionic radius of Ln(3+) and the deviation of the ionic radius of Ln(3+) from the optimum size for the garnet structure. Delta S values of both perovskite formation and garnet formation are deduced to be negative, which suggests that Ln(2)O(3) phases possess relatively large entropies. (C) 1998 Academic Press.
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页码:424 / 436
页数:13
相关论文
共 82 条
[1]   REVERSIBLE B-TYPE - A-TYPE TRANSITION OF SM2O3 UNDER HIGH-PRESSURE [J].
ATOU, T ;
KUSABA, K ;
TSUCHIDA, Y ;
UTSUMI, W ;
YAGI, T ;
SYONO, Y .
MATERIALS RESEARCH BULLETIN, 1989, 24 (09) :1171-1176
[2]  
Barin I.P.D., 1989, Thermochemical Data of Pure Substances
[3]   REFINEMENT OF STRUCTURE OF YTTRIUM IRON-GARNET (YIG) - CASE OF SEVERE EXTINCTION AND ABSORPTION [J].
BONNET, M ;
DELAPALME, A ;
FUESS, H ;
THOMAS, M .
ACTA CRYSTALLOGRAPHICA SECTION B-STRUCTURAL SCIENCE, 1975, 31 (SEP15) :2233-2240
[4]   STRUCTURAL ASPECTS OF THE CRYSTALLOGRAPHIC MAGNETIC TRANSITION IN LAVO3 AROUND 140-K [J].
BORDET, P ;
CHAILLOUT, C ;
MAREZIO, M ;
HUANG, Q ;
SANTORO, A ;
CHEONG, SW ;
TAKAGI, H ;
OGLESBY, CS ;
BATLOGG, B .
JOURNAL OF SOLID STATE CHEMISTRY, 1993, 106 (02) :253-270
[5]   CRYSTAL STRUCTURE OF EU4AL2O9 [J].
BRANDLE, CD ;
STEINFINK, H .
INORGANIC CHEMISTRY, 1969, 8 (06) :1320-+
[6]  
Chai L, 1996, AM MINERAL, V81, P1141
[7]  
CHERNAYA TS, 1985, KRISTALLOGRAFIYA+, V30, P72
[8]   DETERMINATION OF CRYSTAL STRUCTURE OF YTTRIUM ORTHOFERRITE AND REFINEMENT OF GADOLINIUM ORTHOFERRITE [J].
COPPENS, P ;
EIBSCHUTZ, M .
ACTA CRYSTALLOGRAPHICA, 1965, 19 :524-+
[9]   THE CRYSTAL STRUCTURE OF MONOCLINIC SM2O3 [J].
CROMER, DT .
JOURNAL OF PHYSICAL CHEMISTRY, 1957, 61 (06) :753-755
[10]   HIGH PRESSURE SYNTHESIS AND CRYSTAL DATA OF RARE EARTH ORTHOALUMINATES [J].
DERNIER, PD ;
MAINES, RG .
MATERIALS RESEARCH BULLETIN, 1971, 6 (06) :433-&