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高岭石,铝土矿共生及相变的热力学讨论
引用本文:李明德.高岭石,铝土矿共生及相变的热力学讨论[J].矿物岩石,1991,11(2):85-88.
作者姓名:李明德
作者单位:四川建材学院 绵阳
摘    要:根据热力学计算,在常温常压下,铝土矿物能与石英自发反应生成高岭石;硬水铝石和三水铝石都能自发转变为勃姆石,三者可以共生;硬水铝石会自发相变为勃姆石,可能为原生的;在沉积和成岩期的环境下,SiO_2和铝土矿均能化合生成高岭石。

关 键 词:高岭石  铝矿床  相变  热力学

THERMODYNAMIC INVESTIGATION OF THE PARAGENETIC ASSEMBLAGES AND PHASE TRANSITION IN THE SYSTEM OF KAILONITE, GIBBSITE, BOEHMITE AND DIASPORE
Li Mingde.THERMODYNAMIC INVESTIGATION OF THE PARAGENETIC ASSEMBLAGES AND PHASE TRANSITION IN THE SYSTEM OF KAILONITE, GIBBSITE, BOEHMITE AND DIASPORE[J].Journal of Mineralogy and Petrology,1991,11(2):85-88.
Authors:Li Mingde
Abstract:This paper discusses the mineral assemblages and phase transition in the system of kaolinite, gibbsite, boehmite and diaspore from a thermodynamical viewpoint, Leaving out of consideration on the biological, biochemical biocatalytical and catalytical effects in the course of mineralization.
Keywords:Kaolinite  bauxite  thermodynamics of phase transition
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