High-temperature heat capacity and thermal expansion of SrTiO3 and SrZrO3 perovskites

被引:301
作者
deLigny, D
Richet, P
机构
[1] Laboratoire des Géomatériaux, URA CNRS 734, Institut de Physique du Globe de Paris, 75252 Paris Cédex 05, 4, place Jussieu
来源
PHYSICAL REVIEW B | 1996年 / 53卷 / 06期
关键词
D O I
10.1103/PhysRevB.53.3013
中图分类号
T [工业技术];
学科分类号
08 ;
摘要
The heat capacity and thermal expansion of SrZrO3 and SrTiO3 have been determined by drop calorimetry and energy-dispersive x-ray diffraction from 300 up to 1800 K or more. For both compounds, thermal history has a slight influence on relative enthalpies in the range 900-1400 K but a satisfactory precision was obtained through systematic quenches from 1820 K before the calorimetric measurements. Strontium titanate is cubic at room temperature. Up to 1800 K, its heat capacity increases smoothly and its thermal-expansion coefficient remains almost independent of temperature with a value of 3.23(2) 10(-5) K-1. At room temperature, strontium zirconate is orthorhombic (space group Pbnm). The phase transitions from orthorhombic Pbnm to orthorhombic Cmcm at 995 K and then to tetragonal I4/mcm at 1105 K are revealed by symmetric, lambda-type variations of the heat capacity. A more diffuse thermal effect characterizes the I4/mcm to cubic Pm3m transition at 1440 K, above which the cubic phase shows an apparently low heat capacity at the highest temperatures. With the resolution of the x-ray technique, only the transition from orthorhombic Pbnm to orthorhombic Cmcm at 970 K was detected with a small volume change of 0.14%. Thermal expansion below 970 K is constant at 2.98(2) 10(-5) K-1. At higher temperatures, the apparent thermal expansion decreases smoothly from 2.78(2) to 2.43(2) 10(-5) K-1 between 1000 and 1800 K. With recent data on CaTiO3, the effects of (Ca,Sr) and (Ti,Zr) substitutions on thermal expansion and on the energetics of the phase transitions are discussed.
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页码:3013 / 3022
页数:10
相关论文
共 41 条
[11]  
Fomichev EN, 1973, OGNEUPORY, V7, P36
[12]  
Fontana M., 1984, Journal of Physics C: Solid State Physics, V17, P483
[13]   OXYGEN DIFFUSION IN PEROVSKITE - IMPLICATIONS FOR ELECTRICAL-CONDUCTIVITY IN THE LOWER MANTLE [J].
GAUTASON, B ;
MUEHLENBACHS, K .
SCIENCE, 1993, 260 (5107) :518-521
[14]   CLASSIFICATION OF TILTED OCTAHEDRA IN PEROVSKITES [J].
GLAZER, AM .
ACTA CRYSTALLOGRAPHICA SECTION B-STRUCTURAL SCIENCE, 1972, B 28 (NOV15) :3384-&
[15]   SIMPLE WAYS OF DETERMINING PEROVSKITE STRUCTURES [J].
GLAZER, AM .
ACTA CRYSTALLOGRAPHICA SECTION A, 1975, 31 (NOV1) :756-762
[16]  
GUYOT F, 1993, PHYS CHEM MINER, V20, P141
[17]   CRITICAL BEHAVIOR OF HEAT-CAPACITY IN SRTIO3 [J].
HATTA, I ;
SHIROISHI, Y ;
MULLER, KA ;
BERLINGER, W .
PHYSICAL REVIEW B, 1977, 16 (03) :1138-1145
[18]  
Itoh K., 1994, Ferroelectrics, V159, P85, DOI 10.1080/00150199408007553
[19]  
KING EG, 1960, US BUR MINES REP INV, P5571
[20]  
LEVITSKII VA, 1976, TEPLOFIZ VYS TEMP, V14, P78