2021
DOI: 10.1088/1742-6596/1889/3/032007
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Environmental monitoring of water quality in the interstate Ural river

Abstract: This article analyzes the content of biological oxygen demand, chemical oxygen demand, heavy metals using the example of the content of copper and zinc and oil products in the Ural River, which is transboundary and runs along Bashkiria, Chelyabinsk and Orenburg regions, as well as in The Republic of Kazakhstan, West Kazakhstan and Atyrau regions. An excess is noted for all indicators. So the content of biological oxygen demand exceeds from 2 to 15 maximum permissible concentration, the content of chemical oxyg… Show more

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Cited by 8 publications
(7 citation statements)
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“…The To determine the index of contamination of substances (ICS) with trace elements related to trace elements, the sum of the concentration coefficients is divided by the number of studied indicators [4,[13][14][15]:…”
Section: Resultsmentioning
confidence: 99%
“…The To determine the index of contamination of substances (ICS) with trace elements related to trace elements, the sum of the concentration coefficients is divided by the number of studied indicators [4,[13][14][15]:…”
Section: Resultsmentioning
confidence: 99%
“…Several newspapers have reported the occasional use of Shagan river water (site #2) as a drinking water source due to groundwater deficit. 1 Namely, residents of the Oktyabrsky village reported using surface water throughout 2019. It is not feasible to determine the frequency of direct water consumption from the river; therefore, risks associated with regular water drinking were calculated to demonstrate potential human health risks.…”
Section: Drinking Pathwaymentioning
confidence: 99%
“…With a length of 2428 km, the Ural River starts in the Russian Federation, crosses the western part of the territory of Kazakhstan, and reaches the Caspian Sea. 1 It flows through the main industrial cities of Russia and two big cities in Kazakhstan, Uralsk and Atyrau, providing multipurpose water sources and recreational spots for residents.…”
Section: Introductionmentioning
confidence: 99%
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“…The formation waters of the subsalt part of the section (deposits of carboniferous and Lower Permian age) were studied in the Desert and Karaton areas adjacent to Tengiz, where they are represented by strong brines, the mineralization of which reaches 320 g/l. Hydrogeological data on the Karaton area, characterizing the section from the Tournaisian to the Lower Permian age, indicate the hydraulic connection of this range of deposits [8]. In the stratigraphic section of the Tengiz deposit, two hydrogeological floors are distinguished: the upper one is above-salt and the lower one is below-salt [9].…”
Section: Introductionmentioning
confidence: 99%