ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
碳酸盐型盐湖卤水的模拟太阳池结晶试验
  
关键词:saline lake brine  simulation on solar pond crystallization  Li and Mg  precipitation rate
基金项目:国家自然科学基金重点项目(编号: 40531002)和国家大地调项目(编号: 1212010633809)联合资助
作者单位E-mail
唐力君 国土资源部盐湖资源与环境重点实验室室, 北京 100037
中国地质科学院国家地质实验测试中心
, 北京 100037中国地质科学院盐湖与热水资源研究发展中心, 北京 100037 
tanglijun@cags.net.cn 
郑绵平 国土资源部盐湖资源与环境重点实验室, 北京 100037
中国地质科学院盐湖与热水资源研究发展中心, 北京 100037 
 
刘建华 国土资源部盐湖资源与环境重点实验室, 北京 100037
中国地质科学院盐湖与热水资源研究发展中心, 北京 100037 
 
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摘要:
Simulation Experiments on Solar Pond Crystallization of Carbonate-type Saline Lake Brine
      The solar pond plays an important role in the process of lithium extraction from the carbonate saline lake in that it can store solar energy to extract lithium carbonate. The authors used the heating method for the first time to perform simulation experiments on solar pond crystallization in laboratory. In the experiments, the evaporation quantity of brine increased with increasing temperatures, but the difference in evaporation quantity had little effect on salt precipitation. In different time intervals, the concentration of Mg2+ in precipitated salt was higher than that of Li+ in 24 hours and gradually decreased with time, whereas the concentration of Li+ increased. Moreover, the precipitation rate of Mg2+ gradually decreased with time while the precipitation rate of Li+ on the whole remained constant. In simulation experiments at different temperatures, the total precipitation rates of the main components of the brine had a positive correlation with temperatures. The concentration lowering rates of CO32? and Li+ were higher than those of other components, and the precipitation rates of CO32? and Li+ were by far higher than those of other components. The main mineral identified by microscopic observation at different temperatures was zabuyelite.
TANG Li-jun,ZHENG Mian-ping1,LIU Jian-hua.2009.Simulation Experiments on Solar Pond Crystallization of Carbonate-type Saline Lake Brine[J].Acta Geoscientica Sinica,30(2):249-255.
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