Geochemistry and chemical evolution of saline lakes of western mongolia

S. L. Shvartsev, Marina Nikolaevna Kolpakova, V. P. Isupov, A. G. Vladimirov, S. Ariunbileg

Research output: Contribution to journalArticlepeer-review

24 Citations (Scopus)


This paper presents data on the major and trace element composition of saline lakes of western Mongolia. The main geochemical types of lakes distinguished in the study are soda-, chloride-, and sulfate-rich lakes. Lake water equilibria with major carbonate, sulfate, chloride, and other rock-forming minerals were calculated. The results show that the major factors controlling the formation of each lake type include evaporation and water–rock interaction processes, and the latter factor plays a critical role in freshwater and soda lakes and only a minor role in chloride lakes. Special attention was given to the soda lakes and the factors controlling lake water chemistry.

Original languageEnglish
Pages (from-to)388-403
Number of pages16
JournalGeochemistry International
Issue number5
Publication statusPublished - 1 Jan 2014


  • Aqueous migration of elements
  • Evolution of lake water composition
  • Geochemical types of lakes
  • Metal geochemistry
  • Mongolia’s lakes
  • Soda lakes
  • Water equilibrium with secondary minerals
  •  lake water geochemistry

ASJC Scopus subject areas

  • Geophysics
  • Geochemistry and Petrology

Fingerprint Dive into the research topics of 'Geochemistry and chemical evolution of saline lakes of western mongolia'. Together they form a unique fingerprint.

Cite this