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Chemical analysis of Lake Shira water (1997-2000)
Kalacheva, G.S.; Gubanov, V.G.; Gribobskaya, I.; Gladchenko, I.A.; Zinenko, G.K.; Savitsky, S.V. (2002). Chemical analysis of Lake Shira water (1997-2000). Aquat. Ecol. 36(2): 123-141
In: Aquatic Ecology. Springer: Dordrecht; London; Boston. ISSN 1386-2588; e-ISSN 1573-5125, more
Peer reviewed article  

Available in  Authors 

Keywords
    Analysis > Chemical analysis
    Countries > Developed countries > Europe > Central europe > Asia > Russia > Siberia
    Saline
    Saline intrusion
    Siberia
    Stratification
    Water bodies > Inland waters > Lakes > Meromictic lakes
    Water chemistry
    Water quality
    PNE, Russia, Siberia

Authors  Top 
  • Kalacheva, G.S.
  • Gubanov, V.G.
  • Gribobskaya, I.
  • Gladchenko, I.A.
  • Zinenko, G.K.
  • Savitsky, S.V.

Abstract
    The paper presents the results of chemical analysis of Shira during summer (July-August). The chemical composition of waters in the water body was found to be fairly homogeneous horizontally. However, the concentrations of most ions increased with depth. The near-bottom layers were characterised by higher total mineral content and ash content, higher concentration of sulphates, sulphites, sulphide, phosphorus, ammonium nitrogen, as compared to the layers above. Maximum concentration of oxygen was recorded in 6-8 m stratum, where the photosynthetic processes were most active. The anaerobic layer which lay below the 12 m depth contained high concentrations of sulphide and sulphite. The composition of the lake water could be characterised as sulphate-chloride-bicarbonate sodium-magnesium. The changes in the water quality due to any anthropogenic emissions were not marked.

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