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别勒滩低品位钾盐固液转化试验水动力与水化学条件分析 被引量:7

Hydrodynamic and hydrochemical condition analysis of low grade solid potassium liquefy exploitation experiment
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摘要 文章从溶剂、原地晶间卤水、溶出液三个方面,通过察尔汗盐湖别勒滩区段低品位固体钾矿驱动溶解开采试验所取得的监测数据,定性的分析了水位和水质在在纵向和横向上的变化,并且分析了晶间卤水各离子浓度随深度的变化,最后分析了S2T1孔晶间卤水各离子浓度随时间的变化,并根据固液转化的特征划分了不同的阶段,即:对于供卤渠与S2T1孔之间的盐层,第1~11天,处于溶解驱动前阶段,第12~100天,处于光卤石阶段。 The article pointed out the change of underground brine level and components in cross section orientation and transection orientation by analyzing the data from driving and dissolving experiment in Qarhan Salt Lake,and the article also pointed out the concentration change with depth.The article analysed ion concentration changes over time of S2T1 well and divided the experiment into different stages according to the features of the solid-liquid transformation.
出处 《中国矿业》 北大核心 2013年第7期114-119,共6页 China Mining Magazine
基金 国家863计划课题"青海别勒滩低品位固体钾矿液化开发的关键技术"资助(编号:2006AA06Z133) 中国地质大学(北京)中央高校基本科研业务费专项资金资助(编号:2011PY0222)
关键词 察尔汗盐湖 卤水 固液转化 溶解驱动 Qarhan salt lake brine solid-liquid transformation dissolving and driving
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  • 1任国佐.青海盐湖矿产资源实施可持续发展战略的思考[J].青海国土经略,2002(z1):86-88. 被引量:2
  • 2童阳春,廖鹏飞.盐湖卤水开采工程输卤渠设计优化浅谈[J].化工矿物与加工,2005,34(2):28-29. 被引量:2
  • 3青海钾肥厂地质大队.察尔汗盐湖钾镁盐矿综合地质报告[R].格尔木:青海钾肥厂地质大队,1988.
  • 4Harvie,C. E. and J. H. Weare.The prediction of mineral solubilities in natural water: the Na-K-Mg-Ca-Cl-SO4-H2O system from zero to high concentration at 25℃ [J]. Geochim.Cosmochim. Acta, 1980,44:981-997.
  • 5Felmy, A.R. and J.H.Weare.The prediction of borate mineral equilibria in natural water:Application to Searles Lake, California[J].Geochim.Cosmochim. Acta,1986,50:2771-2783.
  • 6Harvie, C. E., N. Moller and J. H. Weare. The prediction of mineral solubilities in natural water: the Na-K-Mg-Ca-H-Cl-SO4-OH-HCO3-CO3-CO2-H2O system to high ionic strengths at 25℃[J].Geochim.Cosmochim. Acta, 1984,48:723- 751.
  • 7Pabalan,R.T.and K.S. Pitzer.Thermodynamics of concentrated electrolyte mixtures and the prediction of mineral solubilities to high temperatures for mixtures in the system Na-K-Mg-Cl-SO4-OH-H2O[J]. Geochim. Cosmochim. Acta, 1987,51:2429 -2443.
  • 8Moller, N..The prediction of mineral solubilities in natural water: A chemical equilibrium model for the Na-Ca-Cl-SO4-H2O system to high temperature and concentration [ J ]. Geochim.Cosmochim. Acta, 1989:2,821 - 837.
  • 9Greenberg,J.P.and N.Moller. The prediction of mineral solubilities in natural water: A chemical equilibrium model for the Na-K-Ca-Cl-SO4-H2O system to high concentration from 0 to 250℃ [J]. Geochim. Cosmochim. Acta, 1989, 53:2503 -2518.
  • 10Spencer, R. J., N. Moller and J. H. Weare. The prediction of mineral solubilities in natural water: A chemical equilibrium model for the Na-K-Ca-Mg-Cl-SO4-H2O system at temperature below 25℃[J].Geochim. Cosmochim. Acta, 1989,54:575-590.

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