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1)  Chagcam Caka Salt Lake
扎仓茶卡盐湖
1.
Phase Diagram Analysis of Producing Potassium Chloride from the Brine of Chagcam Caka Salt Lake in Tibet
西藏扎仓茶卡盐湖卤水制取氯化钾的相图分析
2)  Zhachang Caka
扎仓茶卡
3)  Chaka salt lake
茶卡盐湖
1.
Assessment of enrichment bacterial community in Keke and Chaka salt lakes of Qinghai by DGGE;
青海柯柯盐湖、茶卡盐湖细菌富集培养后DGGE带谱比较
2.
Denaturing gradient gel electrophoresis (DGGE) was used to assess the enrichment bacterial community in two adjacent lakes,the Keke salt lake and the Chaka salt lake,Qinghai,China.
分别对青海相邻两盐湖柯柯盐湖、茶卡盐湖土样、泥样进行富集培养后 ,从中提取的DNA用两套不同的细菌通用引物进行扩增 ,分别得到包含V8和V9高变区的 16SrDNA片断。
4)  Zabuye salt lake
扎布耶茶卡
1.
Petrogenesis and implications of the volcanic rocks in Zabuye salt lake area,western Lhasa terrane,Tibet,China
西藏拉萨地块西部扎布耶茶卡火山岩的成因与意义
5)  Zhabuye salt lake
扎布耶盐湖
1.
The Preliminary Study on the Equilibrium Solubility and Crystallization Laws of Lithium Carbonate Based on the Composition of Zhabuye Salt Lake Brine
扎布耶盐湖卤水碳酸锂恒温平衡浓度和结晶规律初步研究
2.
This paper presents the experimental data of metastable phase equilibrium of Li~+/Cl~-,CO_3~(2-),B_4O_7~(2-)-H_2O quaternary system at 298 K for Zhabuye salt lake in Tibet,from which the metastable phase diagram and physicochechemical properties(density,pH value,conductivity and refractive index) vs composition diagram is drawn.
根据对西藏扎布耶盐湖四元子体系L i+/C l-,CO32-,B4O72--H2O 298 K介稳平衡实验数据,绘制出的介稳平衡相图及物化性质(密度、pH值、电导率、折光率)组成图的研究结果表明:该四元体系属简单共饱型,无复盐或固溶体形成;其溶解度等温图含有一个共饱点、3条单变量曲线和3个结晶相区;3个结晶相区分别对应为L i2B4O7。
6)  Zabuye Salt Lake
扎布耶盐湖
1.
Study on the Crystallization Law of Salts form the Brine after Freezing through the Normal Temperature(20℃)Evaporation in Zabuye Salt Lake;
扎布耶盐湖冷冻后卤水常温蒸发(20℃)析盐规律
2.
25℃-Isothermal Evaporation of Autumn Brines from the Zabuye Salt Lake,Tibet,China;
西藏扎布耶盐湖秋季卤水25℃等温蒸发研究
3.
Sedimentary Characteristics and Paleoenvironmental Records of Zabuye Salt Lake,Tibetan Plateau,since 128 ka BP;
西藏高原扎布耶盐湖128ka以来沉积特征与古环境记录
补充资料:扎仓茶卡
      西藏自治区盐湖。亦称张张茶卡。地处北纬32°33′~32°35′,东经82°15′~82°31′,自治区西部阿龙干累山北麓,阿里地区革吉县盐湖区,黑阿公路北侧。东西长32公里,南北宽3~6公里。总面积132.5平方公里,由3个湖泊组成。湖水深0.15~1.20米,pH值7.51~7.99,矿化度290.200~340.580克/升,属硫酸镁型盐湖。扎仓茶卡四周第四纪湖相地层广泛分布,发育了三级阶地,属荒漠草原地带。气候寒冷干旱,年降水量稀少。湖中含有丰富的石膏、芒硝、食盐、钾芒硝等矿产资源。
  

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