STABILITY OF CANISI2O6 (NIOPSIDE) AND ACTIVITY COMPOSITION RELATIONS OF CAMGSI2O6-CANISI2O6 SOLID-SOLUTIONS AT 1350-DEGREES-C

被引:7
作者
PRETORIUS, EB
MUAN, A
机构
[1] PENN STATE UNIV,COLL EARTH & MINERAL SCI,UNIV PK,PA 16802
[2] PENN STATE UNIV,COLL EARTH & MINERAL SCI,UNIV PK,PA 16802
关键词
STABILITY; NICKEL; DIOPSIDE; SOLID SOLUTION; EQUILIBRIUM;
D O I
10.1111/j.1151-2916.1992.tb04210.x
中图分类号
TQ174 [陶瓷工业]; TB3 [工程材料学];
学科分类号
0805 ; 080502 ;
摘要
A complete solid-solution series exists between diopside (CaMgSi2O6) and its nickel analogue, "niopside" (CaNiSi2O6). Activity-composition relations within this solid solution, and the stability of the end member CaNiSi2O6, have been determined by equilibrating CaNiSi2O6 with SiO2, CaSiO3, and metallic Ni in atmospheres of known oxygen pressures. Within limits of accuracy of the experiments, the solution is ideal at 1350-degrees-C. From the experimental data obtained in the present investigation, the standard free energy (DELTA-G-degrees) of formation of CaNiSi2O6 according to the equation CaO + NiO + 2SiO2 = CaNiSi2O6 is calculated to be DELTA-G-degrees = -165862 + 42.40T J. Experiments in the system CaO-NiO-SiO2 have shown that the nickel analogue of the phase pseudo-enstatite (MgSiO3) is unstable with respect to SiO2 and nickel olivine (Ni2SiO4), and the nickel analogues of the phases akermanite (Ca2MgSi2O7) and monticellite (CaMgSiO4) are unstable relative to the phase assemblage pseudo-wollastonite (CaSiO3) PIUS NiO. In the system CaO-MgO-NiO-SiO2, however, substitution of Ni for Mg in these phases was observed. The percentage substitution of Ni for Mg in the phases is given in parentheses: diopside (100%), olivine (100%), enstatite (18%), akermanite (20%), and monticellite (57%).
引用
收藏
页码:1458 / 1462
页数:5
相关论文
共 25 条
[1]  
ANNERSTEN H, 1982, AM MINERAL, V67, P1212
[2]   SYSTEM CAO-NIO-SIO2 [J].
BIGGAR, GM .
JOURNAL OF THE AMERICAN CERAMIC SOCIETY, 1969, 52 (06) :316-&
[3]  
BISH DL, 1981, AM MINERAL, V66, P770
[4]  
CAMPBELL FE, 1968, AM MINERAL, V53, P257
[5]  
CASTRIGNANO R, 1976, SOC ITAL MINERAL REN, V32, P159
[6]  
GHOSE S, 1975, EOS T AM GEOPHYS UN, V56, P1076
[7]  
Gjessing L., 1941, NOR GEOL TIDSSKR, V20, P265
[8]   PHASE-RELATIONS AT LIQUIDUS TEMPERATURES IN THE SYSTEM MGO-NIO-SIO2 [J].
GRUTZECK, MW ;
MUAN, A .
JOURNAL OF THE AMERICAN CERAMIC SOCIETY, 1988, 71 (08) :638-643
[9]   ACTIVITY MEASUREMENTS IN OXIDE SOLID SOLUTIONS - THE SYSTEMS NIO-MGO AND NIO-MNO IN THE TEMPERATURE INTERVAL 1100-1300-DEGREES-C [J].
HAHN, WC ;
MUAN, A .
JOURNAL OF PHYSICS AND CHEMISTRY OF SOLIDS, 1961, 19 (3-4) :338-348
[10]  
HIGGINS BB, 1973, AM J SCI, VA273, P511