ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
青藏高原中部班戈错富锂盐湖水位月际变化与驱动因素分析
  
关键词:lithium-rich salt lake  water level  inter-monthly variation  driving factors  Tibetan Plateau
基金项目:“第二次青藏高原综合科学考察研究”专题(编号: 2022QZKK0201); 中国地质调查局地质调查项目(编号: DD20243280); 国家自然科学基金项目(编号: 91962219); “浙江天铁实业股份有限公司”委托项目(编号: HE2210)
作者单位E-mail
李胜群 中国地质大学(北京)地球科学与资源学院 1797035381@qq.com 
叶传永 中国地质科学院矿产资源研究所 自然资源部盐湖资源与环境重点实验室
中国地质科学院矿产资源研究所 自然资源部青藏高原盐湖野外观测研究站 
chuanyongye@163.com 
赵元艺 中国地质科学院矿产资源研究所 自然资源部盐湖资源与环境重点实验室
中国地质科学院矿产资源研究所 自然资源部青藏高原盐湖野外观测研究站 
 
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摘要:
Analysis of Inter-monthly Variation and Driving Factors of Water Level Fluctuation in Bankog Co, A Lithium-rich Salt Lake, Central Tibetan Plateau
      Lithium’s unique advantages in the field of new energy have made its demand grow exponentially, and the world's major economies have listed it as a key mineral. Salt lakes in Tibet are rich in lithium resources, and changes in the water level play an important role in the dynamic evaluation of lithium resources. Bankog Co is a typical lithium-rich salt lake, making it highly representative. The main conclusions are as follows: (1) Between June 2018 and December 2021, and from January 2016 to July 2023, the Bankog Co water level exhibited drastic inter-monthly changes, first decreasing, then increasing, and again decreasing. The speed at which the water level increased was much higher than the speed at which it decreased. (2) An increase in evaporation was the main reason for the two-time water level decrease; a decrease in evaporation and an increase in temperature were the driving forces of rises in the water level. (3) Temperature and precipitation were the main factors controlling the annual variation of the lake, and temperature was mainly affected by controlling evaporation. The results of this study provide a database for regional response studies of climate change in the Tibetan Plateau and the late lithium mining of Bankog Co.
LI Shengqun,YE Chuanyong,ZHAO Yuanyi.2024.Analysis of Inter-monthly Variation and Driving Factors of Water Level Fluctuation in Bankog Co, A Lithium-rich Salt Lake, Central Tibetan Plateau[J].Acta Geoscientica Sinica,45(5):691-705.
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