Influence of the interactions within the water - earth materials system on the formation of river water composition in the Ob basin

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4 Citations (Scopus)

Abstract

Physicochemical calculations of the abundance of a number of minerals and organo-mineral compounds in the river waters of the Ob basin revealed that the river waters throughout a year are able to actively interact with bottom sediments and river loads. The most active interactions occur in areas and during periods with increased moduli of river flow. It is shown that the increase in concentrations of dissolved organic matter in the river waters, including in the case of waste water discharges, is limited to a relatively low solubility of a number of compounds of metals with carbonates and humic acids.

Original languageEnglish
Pages (from-to)161-166
Number of pages6
JournalGeography and Natural Resources
Volume30
Issue number2
DOIs
Publication statusPublished - 1 Jun 2009

Fingerprint

river water
river
water
interaction
basin
mineral
river flow
dissolved organic matter
humic acid
solubility
carbonate
metal
sediment
material
calculation
waste water discharge

Keywords

  • chemical composition of river waters
  • formation of chemical composition of the river waters
  • interactions within the water - earth materials system
  • Ob river basin

ASJC Scopus subject areas

  • Earth-Surface Processes
  • Management, Monitoring, Policy and Law
  • Geography, Planning and Development

Cite this

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abstract = "Physicochemical calculations of the abundance of a number of minerals and organo-mineral compounds in the river waters of the Ob basin revealed that the river waters throughout a year are able to actively interact with bottom sediments and river loads. The most active interactions occur in areas and during periods with increased moduli of river flow. It is shown that the increase in concentrations of dissolved organic matter in the river waters, including in the case of waste water discharges, is limited to a relatively low solubility of a number of compounds of metals with carbonates and humic acids.",
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AB - Physicochemical calculations of the abundance of a number of minerals and organo-mineral compounds in the river waters of the Ob basin revealed that the river waters throughout a year are able to actively interact with bottom sediments and river loads. The most active interactions occur in areas and during periods with increased moduli of river flow. It is shown that the increase in concentrations of dissolved organic matter in the river waters, including in the case of waste water discharges, is limited to a relatively low solubility of a number of compounds of metals with carbonates and humic acids.

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