Iron-containing Water of the Yamal-Nenets Autonomous District
Factors of groundwater formation in the Yamal-Nenets Autonomous District predetermined its specific composition, characterized by low (ultra-fresh) mineralization, rarely exceeding 100 mg/dm3, reduced concentrations of the main macrocomponents and high concentrations of iron and manganese. Almost ev...
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ftaserspublojs:oai:ojs.pkp.sfu.ca:article/1778 2023-05-15T17:14:31+02:00 Iron-containing Water of the Yamal-Nenets Autonomous District BESHENTSEV, Vladimir A. ABDRASHITOVA, Rimma N. KOVYATKINA, Lyubov A. SALNIKOVA, Yuliya I. SABANINA, Irina G. LAZUTIN, Nikolay K. 2018-02-25 application/pdf https://journals.aserspublishing.eu/jemt/article/view/1778 https://doi.org/10.14505//jemt.v8.7(23).11 eng eng ASERS Publishing https://journals.aserspublishing.eu/jemt/article/view/1778/1337 https://journals.aserspublishing.eu/jemt/article/view/1778 doi:10.14505//jemt.v8.7(23).11 Copyright (c) 2018 ASERS Publishing Journal of Environmental Management and Tourism; Vol 8 No 7 (2017): JEMT Volume VIII Issue 7(23) Winter 2017; 1420-1426 2068-7729 info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 2018 ftaserspublojs https://doi.org/10.14505//jemt.v8.7(23).11 2022-12-24T16:48:42Z Factors of groundwater formation in the Yamal-Nenets Autonomous District predetermined its specific composition, characterized by low (ultra-fresh) mineralization, rarely exceeding 100 mg/dm3, reduced concentrations of the main macrocomponents and high concentrations of iron and manganese. Almost everywhere in the region under consideration, iron content exceeds the MAC by sanitary rules and rates 2.1.4.1074-01 "Drinking water", sometimes reaching tens of mg/dm3. On average, its values lie in the range from 1.4 to 6.5 mg/dm3 (at a rate of 0.3 mg/dm3). The presence of marshes and an increased content of organic substances in the aquifers of the Quaternary and Cretaceous-Paleogene deposits of the basin in the ice-humid and humid macrozones contribute to the creation of a primarily acidic reducing environment favorable for the migration of iron, manganese and other elements. The purpose of this study was to construct a mathematical model describing the dependence of the distribution of iron forms in the groundwater of the region on the pH which falls into the interval 5.5 - 7.5. These calculations eventually allowed us to recommend the most effective water treatment measures. Article in Journal/Newspaper nenets ASERS Publishing Journals Journal of Environmental Management and Tourism 8 7 1420 |
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Factors of groundwater formation in the Yamal-Nenets Autonomous District predetermined its specific composition, characterized by low (ultra-fresh) mineralization, rarely exceeding 100 mg/dm3, reduced concentrations of the main macrocomponents and high concentrations of iron and manganese. Almost everywhere in the region under consideration, iron content exceeds the MAC by sanitary rules and rates 2.1.4.1074-01 "Drinking water", sometimes reaching tens of mg/dm3. On average, its values lie in the range from 1.4 to 6.5 mg/dm3 (at a rate of 0.3 mg/dm3). The presence of marshes and an increased content of organic substances in the aquifers of the Quaternary and Cretaceous-Paleogene deposits of the basin in the ice-humid and humid macrozones contribute to the creation of a primarily acidic reducing environment favorable for the migration of iron, manganese and other elements. The purpose of this study was to construct a mathematical model describing the dependence of the distribution of iron forms in the groundwater of the region on the pH which falls into the interval 5.5 - 7.5. These calculations eventually allowed us to recommend the most effective water treatment measures. |
format |
Article in Journal/Newspaper |
author |
BESHENTSEV, Vladimir A. ABDRASHITOVA, Rimma N. KOVYATKINA, Lyubov A. SALNIKOVA, Yuliya I. SABANINA, Irina G. LAZUTIN, Nikolay K. |
spellingShingle |
BESHENTSEV, Vladimir A. ABDRASHITOVA, Rimma N. KOVYATKINA, Lyubov A. SALNIKOVA, Yuliya I. SABANINA, Irina G. LAZUTIN, Nikolay K. Iron-containing Water of the Yamal-Nenets Autonomous District |
author_facet |
BESHENTSEV, Vladimir A. ABDRASHITOVA, Rimma N. KOVYATKINA, Lyubov A. SALNIKOVA, Yuliya I. SABANINA, Irina G. LAZUTIN, Nikolay K. |
author_sort |
BESHENTSEV, Vladimir A. |
title |
Iron-containing Water of the Yamal-Nenets Autonomous District |
title_short |
Iron-containing Water of the Yamal-Nenets Autonomous District |
title_full |
Iron-containing Water of the Yamal-Nenets Autonomous District |
title_fullStr |
Iron-containing Water of the Yamal-Nenets Autonomous District |
title_full_unstemmed |
Iron-containing Water of the Yamal-Nenets Autonomous District |
title_sort |
iron-containing water of the yamal-nenets autonomous district |
publisher |
ASERS Publishing |
publishDate |
2018 |
url |
https://journals.aserspublishing.eu/jemt/article/view/1778 https://doi.org/10.14505//jemt.v8.7(23).11 |
genre |
nenets |
genre_facet |
nenets |
op_source |
Journal of Environmental Management and Tourism; Vol 8 No 7 (2017): JEMT Volume VIII Issue 7(23) Winter 2017; 1420-1426 2068-7729 |
op_relation |
https://journals.aserspublishing.eu/jemt/article/view/1778/1337 https://journals.aserspublishing.eu/jemt/article/view/1778 doi:10.14505//jemt.v8.7(23).11 |
op_rights |
Copyright (c) 2018 ASERS Publishing |
op_doi |
https://doi.org/10.14505//jemt.v8.7(23).11 |
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Journal of Environmental Management and Tourism |
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8 |
container_issue |
7 |
container_start_page |
1420 |
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1766071914309091328 |