ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
我国盐田首次产出南极石
  
关键词:Antarcticite  underground brine  solar pond experiment  Qaidam basin  climate environment
基金项目:中国地质调查局地质调查项目(编号: 1212011085523);国家自然科学基金项目(编号: 41073050);中国地质科学院重点实验室基金项目(编号: C0908)
作者单位E-mail
乜贞 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 nieezhen518@163.com 
董亚萍 中国科学院青海盐湖研究所  
李武 中国科学院青海盐湖研究所  
卜令忠 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  
袁伟 青海油田边远油田开发公司  
乌志明 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  
张雪飞 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  
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摘要:
The First Precipitation of Antarcticite in Solar Ponds in China
      Antarcticite, formed in areas of very arid and cold climate, was first discovered in the Don Juan Pond in Victoria Land, Antarctica. The mineral is named after the place it was found. The Antarcticite was reported to be found in Qaidam basin in 1983. Nanyishan area of Qaidam basin is also extremely dry and very cold, especially in winter. A solar pond experiment was carried out to extract potash in Nanyishan from the underground brine at the depth of 1940 m, which is rich in calcium and potassium. In the experiment, the Antarcticite was crystallized out in the solar pond with halite and potash during the winter. The X-ray powder diffraction measurement, chemical analysis and crystal optical study of this mineral has proved that the mineral is Antarcticite. This is for the first time that the Antarcticite is reported in solar ponds because there was no such report before. Through the research, the climate environment for the formation of Antarcticite is determined. The results obtained by the authors will give some useful information to the study of the environment changes in Qaidam basin.
NIE Zhen,DONG Ya-ping,LI Wu,BU Ling-zhong,YUAN Wei,WU Zhi-ming,ZHANG Xue-fei.2013.The First Precipitation of Antarcticite in Solar Ponds in China[J].Acta Geoscientica Sinica,34(6):763-766.
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