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青藏高原钠硼解石在水中溶解动力学和热力学的研究
引用本文:陈若愚,夏树屏.青藏高原钠硼解石在水中溶解动力学和热力学的研究[J].盐湖研究,1994,2(1):52-56.
作者姓名:陈若愚  夏树屏
作者单位:中国科学院青海盐湖研究所
摘    要:本工作采用pH值,电导率和Na+、Ca(2+)选择电极的电极电位四种物理参数跟踪测定了钠硼解石在10℃~35℃纯水中的溶解过程,结合取样进行化学分析和对固相的物相鉴定确定了溶解机制.拟合出溶解动力学方程,计算了Arrhanius活化能,并根据最终平衡的各离子浓度计算出溶度积常数、溶解度、溶解热和溶解熵等热力学函数.

关 键 词:钠硼解石,动力学,热力学

Study on Kinetics and Thermodynamics of Dissolution of Ulexite in water in Qinghai-Tibet Plateau
Chen Ruoyu,Xia Shuping and Gao Shiyang.Study on Kinetics and Thermodynamics of Dissolution of Ulexite in water in Qinghai-Tibet Plateau[J].Journal of Salt Lake Research,1994,2(1):52-56.
Authors:Chen Ruoyu  Xia Shuping and Gao Shiyang
Abstract:Dissolution kinetics and thermodynamics of Ulexite in water has been studied by the following the changes in electromotive force of ion selective electrods and the change in conductivity. The solid phase was identified by chemical analyisis. X-ray POwer diffration, IR spectra analysis. From the curves of c ̄t. it is considered that the dissolution rate is controlled by interface reaction and calculate Arrhenius energy. Based on the equlibrium concentration. the values of △G, △H. △S and crystallization reaction energy can be calculated.
Keywords:Ulexite  Kinetic  Thermodynamics  
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