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298.15 K下KBr−CaBr2−SrBr2−H2O四元体系相平衡研究
  
关键词:potassium salts  phase diagram  bromides  brine mineral systems  deep brines
基金项目:青海省自然科学基金项目(编号: 2024-ZJ-901)
作者单位E-mail
杨秋叶 中国科学院青海盐湖研究所, 盐湖资源综合高效利用重点实验室青海省盐湖资源化学重点实验室 1440265437@qq.com 
崔瑞芝 中国科学院青海盐湖研究所, 盐湖资源综合高效利用重点实验室青海省盐湖资源化学重点实验室 cuirzh@isl.ac.cn 
聂国亮 中国科学院青海盐湖研究所, 盐湖资源综合高效利用重点实验室  
任红保 成都理工大学材料与化学化工学院  
李 武 中国科学院青海盐湖研究所, 盐湖资源综合高效利用重点实验室青海省盐湖资源化学重点实验室  
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摘要:
Brine Mineral Equilibrium Studies of a KBr−CaBr2−SrBr2−H2O System at 298.15 K
      The deep underground brine of Qaidam Basin in Qinghai is rich in potassium, calcium, strontium, bromine and other elements, making it a liquid mineral resource with great comprehensive utilization value. Notably, its brine can be developed as a potential potassium salt resource. In this study, the solubility and phase equilibrium of the quaternary KBr?CaBr2?SrBr2?H2O system at 298.15 K were studied in detail using the isothermal dissolution equilibrium method, based on the compositional characteristics of the deep underground brine. The solubility and equilibrium solid-phase compositions of the relevant salts of this system were determined. Based on the experimental data, a diagram of the stable phase equilibrium and water content of the system at specific temperature conditions has been plotted. This phase diagram has no complex salt and solid solution generation at 298.15 K, has one invariant point, three univariant dissolution curves, and three solid-phase crystalline zones (KBr, CaBr2?6H2O, SrBr2?6H2O). Based on the Pitzer model, the solubility of this quaternary system at 298.15 K was predicted, and its calculated phase diagram agrees well with the experimental phase diagram.
YANG Qiuye,CUI Ruizhi,NIE Guoliang,REN Hongbao,LI Wu.2024.Brine Mineral Equilibrium Studies of a KBr−CaBr2−SrBr2−H2O System at 298.15 K[J].Acta Geoscientica Sinica,45(5):791-797.
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