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西藏扎北盐湖秋季卤水(硫酸钠亚型)5℃等温蒸发实验研究
引用本文:王云生,郑绵平,乜贞,卜令忠,高峰.西藏扎北盐湖秋季卤水(硫酸钠亚型)5℃等温蒸发实验研究[J].地球学报,2011,32(4):477-482.
作者姓名:王云生  郑绵平  乜贞  卜令忠  高峰
作者单位:中国地质科学院矿产资源研究所国土资源部盐湖资源与环境重点实验室; 中国地质科学院盐湖与热水研究发展中心;中国地质科学院矿产资源研究所国土资源部盐湖资源与环境重点实验室; 中国地质科学院盐湖与热水研究发展中心;中国地质科学院矿产资源研究所国土资源部盐湖资源与环境重点实验室; 中国地质科学院盐湖与热水研究发展中心;中国地质科学院矿产资源研究所国土资源部盐湖资源与环境重点实验室; 中国地质科学院盐湖与热水研究发展中心;中国地质科学院矿产资源研究所国土资源部盐湖资源与环境重点实验室; 中国地质科学院盐湖与热水研究发展中心
基金项目:中国地质调查局地质调查项目(编号: 12120108056); 中国地质科学院矿产资源研究所基本业务费项目(编号: K0918)
摘    要:西藏扎北盐湖硫酸钠亚型卤水中富含元素Li、B、K和微量元素Rb、Cs等.为了更好地了解卤水在自然条件下的蒸发结晶规律,需对相应卤水进行低温室内等温蒸发实验研究.本文对该盐湖卤水进行了5℃等温蒸发试验,并利用Na+、K+、Mg2+//Cl-、SO42--H2O五元水盐体系0℃相图,构筑了从干基立体图Na2SO4角顶的放射...

关 键 词:相化学  5℃等温蒸发  结晶路线  盐类析出规律

5℃-Isothermal Evaporation Experiment of Autumn Brines from the Sodium Sulfate Subtype Zhabei Salt Lake in Tibet
WANG Yun-sheng,ZHENG Mian-ping,NIE Zhen,BU Ling-zhong and GAO Feng.5℃-Isothermal Evaporation Experiment of Autumn Brines from the Sodium Sulfate Subtype Zhabei Salt Lake in Tibet[J].Acta Geoscientia Sinica,2011,32(4):477-482.
Authors:WANG Yun-sheng  ZHENG Mian-ping  NIE Zhen  BU Ling-zhong and GAO Feng
Institution:MLR Key Laboratory of Saline Lake Resources and Environments, Institute of Mineral Resources, Chinese Academy of Geological Sciences; Research and Development Center of Saline Lakes and Epithermal Deposits, Chinese Academy of Geological Sciences;MLR Key Laboratory of Saline Lake Resources and Environments, Institute of Mineral Resources, Chinese Academy of Geological Sciences; Research and Development Center of Saline Lakes and Epithermal Deposits, Chinese Academy of Geological Sciences;MLR Key Laboratory of Saline Lake Resources and Environments, Institute of Mineral Resources, Chinese Academy of Geological Sciences; Research and Development Center of Saline Lakes and Epithermal Deposits, Chinese Academy of Geological Sciences;MLR Key Laboratory of Saline Lake Resources and Environments, Institute of Mineral Resources, Chinese Academy of Geological Sciences; Research and Development Center of Saline Lakes and Epithermal Deposits, Chinese Academy of Geological Sciences;MLR Key Laboratory of Saline Lake Resources and Environments, Institute of Mineral Resources, Chinese Academy of Geological Sciences; Research and Development Center of Saline Lakes and Epithermal Deposits, Chinese Academy of Geological Sciences
Abstract:The sodium sulfate subtype Zhabei salt lake in Tibet contains abundant special elements Li,B and K and trace elements Rb and Cs.It is necessary to carry out an isothermal evaporation experiment at lower temperatures to probe into the crystallization path of salt minerals at ambient temperatures.The authors conducted an experiment of 5℃-isothermal evaporation of autumn brines and studied the crystallization paths and precipitation regularities of salts in the process of isothermal evaporation by referring to the metastable diagram of the quinary water-salt system of Na+,K+,Mg2+//Cl-,SO42-H2O.The experiment and study provide an important basis for the comprehensive exploitation and use of brines of this salt lake.The experimental results show that boron is precipitated as borax in the whole evaporation process,and potassium is precipitated as sylvite and aphthitalite until the brine is extremely concentrated.
Keywords:phase chemistry  5℃-isothermal evaporation  crystallization path precipitation  regularity of salts
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