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pH值对长石溶解度及次生孔隙发育的影响
引用本文:罗孝俊,杨卫东,李荣西,高丽萍.pH值对长石溶解度及次生孔隙发育的影响[J].矿物岩石地球化学通报,2001,20(2):103-107.
作者姓名:罗孝俊  杨卫东  李荣西  高丽萍
作者单位:中国科学院地球化学研究所
基金项目:国家自然科学基金!资助项目 ( 4 9773 179)
摘    要:本文从长石溶解反应的机理及各离子形态在溶液中分布的热力学角度出发 ,论述了pH值对三个长石端员及高岭石在流体中溶解度的影响。在此基础上 ,进一步探讨了流体酸碱度对长石向高岭石转化和次生孔隙发育程度的制约 ,并提出了衡量次生孔隙发育程度的参数———转化系数D。

关 键 词:长石  溶解反应  pH值  次生孔隙
文章编号:1007-2802(2001)02-0103-05
修稿时间:2000年12月28

Effects of pH on the Solubility of the Feldspar and the Development of Secondary Porosity
LUO Xiao-jun,YANG Wei-dong,LI Rong-xi,GAO Li-ping.Effects of pH on the Solubility of the Feldspar and the Development of Secondary Porosity[J].Bulletin of Mineralogy Petrology and Geochemistry,2001,20(2):103-107.
Authors:LUO Xiao-jun  YANG Wei-dong  LI Rong-xi  GAO Li-ping
Abstract:In this paper, based on the mechanism of dissolution of feldspar and the distribution of various aqueous ions, the effects of pH on the solubility of three endmembers of feldspar and Kaolinite in fluid were studied from the angle of thermodynamic.The influence of pH of the fluid on the transformation of feldspar to kaolinite and the development of secondary porosity in this process were further studied. coefficient of transformation ( D ) was offered to estimate the degree of the development of secondary porosity.
Keywords:feldspar  dissolution reaction  pH  secondary porosity
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