Zonal Features of Bog and Lake Water Chemistry Along a Transect from Boreal to Arid Landscapes in the South of Western Siberia, Russia

Marina N. Kolpakova, Olga S. Naymushina

Research output: Contribution to journalArticle

3 Citations (Scopus)

Abstract

Western Siberia is a unique territory where more than 12000 water reservoirs are located. The region is characterized by high bogginess up to 90% in the north. Bog and lake systems are able to accumulate natural and technogenic resources, including trace elements and organic matter. The article presents the results of a surface water chemical composition along a 5-year monitoring. The obtained data allow concluding that dynamics of water chemistry is predetermined by their location in various landscape zones and subordinated to zonal distribution of such major landscape elements as moistening, evaporation, rate of groundwater flow, etc.

Original languageEnglish
Article number022025
JournalIOP Conference Series: Earth and Environmental Science
Volume44
Issue number2
DOIs
Publication statusPublished - 19 Oct 2016
EventWorld Multidisciplinary Earth Sciences Symposium, WMESS 2016 - Prague, Czech Republic
Duration: 5 Sep 20169 Sep 2016

Fingerprint

bog
water chemistry
lake water
transect
groundwater flow
evaporation
chemical composition
trace element
surface water
organic matter
lake
monitoring
resource
rate
distribution
water reservoir

ASJC Scopus subject areas

  • Environmental Science(all)
  • Earth and Planetary Sciences(all)

Cite this

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AB - Western Siberia is a unique territory where more than 12000 water reservoirs are located. The region is characterized by high bogginess up to 90% in the north. Bog and lake systems are able to accumulate natural and technogenic resources, including trace elements and organic matter. The article presents the results of a surface water chemical composition along a 5-year monitoring. The obtained data allow concluding that dynamics of water chemistry is predetermined by their location in various landscape zones and subordinated to zonal distribution of such major landscape elements as moistening, evaporation, rate of groundwater flow, etc.

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