PREDICTION OF ENTHALPY OF FORMATION BASED ON REFINED CRYSTAL-STRUCTURES OF MULTISITE COMPOUNDS .1. THEORIES AND EXAMPLES

被引:34
作者
VIEILLARD, P
机构
[1] Laboratoire de Pétrologie de la Surface, URA 721, 86022 Poitiers Cedex
关键词
D O I
10.1016/0016-7037(94)90266-6
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
The method of prediction of enthalpy of formation is based on the parameter Delta HO2- cation (comp). The calculation of this parameter requires the knowledge of crystallographical and optical properties of minerals: refractive index, molecular volume, average distances, and shortest bond lengths of cation-oxygen, in all sites involved in the compounds. From the initial work on the two oxides minerals and extended to three oxide and three site bearing compounds valid for sites occupied by a single cation, the generalisation of the method of prediction to multisite compounds has been undertaken by proposing some new considerations in the calculation of Delta H(f,oxides)degrees which are the following: 1) make the distinction between sites occupied either by one either by more than one cation; 2) use a new formulation of the parameter Delta HO2- cation (comp) of sites occupied by more than one cation; 3) consider the existence in some polyhedra, of extra long bond length cation oxygen; 4) take into consideration the nonoxygen bridges between two nearest neighbor polyhedra, necessary to the calculation of the enthalpy of formation from the constituent oxides; 5) introduce an evaluation of the prediction error related to the error standard deviation of measured bond lengths. This method has been tested on a great number of minerals and artificial compounds belonging to the system Li2O-Na2O-K2O-BeO-MgO-CaO-MnO-FeO-Fe2O3-Al2O3-SiO2-H2O. An example of calculation of Delta H(f,oxides)degrees and Delta H-f degrees has been given in detail with a new evaluation of the error of prediction on a well-known mineral, muscovite.
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页码:4049 / 4063
页数:15
相关论文
共 38 条
[1]  
AJA SU, 1992, EUR J MINERAL, V4, P1251
[2]  
[Anonymous], 1967, MICROSCOPICAL CHARAC
[3]  
BORN M, 1923, ATOMTHEORIE FESTEN Z
[4]  
Born M., 1932, Z PHYS, V75, P1, DOI [10.1007/BF01340511, DOI 10.1007/BF01340511]
[5]   METHOD OF ESTIMATION OF STANDARD FREE-ENERGIES OF FORMATION OF SILICATE MINERALS AT 298.15 DEGREES K [J].
CHEN, CH .
AMERICAN JOURNAL OF SCIENCE, 1975, 275 (07) :801-817
[6]  
CHERMAK JA, 1989, AM MINERAL, V74, P1023
[7]  
GARTNER L, 1979, THESIS STRASBOURG
[8]  
HOLLAND TJB, 1989, AM MINERAL, V74, P5
[9]  
KARAPETYANTS MK, 1965, METHODE COMP CALCULA
[10]   REFINEMENT OF MN-SUBSTITUTED MUSCOVITE AND PHLOGOPITE [J].
KNURR, RA ;
BAILEY, SW .
CLAYS AND CLAY MINERALS, 1986, 34 (01) :7-16