Changes in hydrogeological conditions at the territories adjacent to tailings storage facilities in Kryvyi Rih iron ore basin
Tailings of mining and processing plants of Kryvbas are new areas of groundwater supply which have led to significant changes in the hydrodynamic and hydrogeochemical regimes of aquifers. The purpose of the research was to assess the degree of damage to the areas adjacent to the tailings of mining e...
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description | Tailings of mining and processing plants of Kryvbas are new areas of groundwater supply which have led to significant changes in the hydrodynamic and hydrogeochemical regimes of aquifers. The purpose of the research was to assess the degree of damage to the areas adjacent to the tailings of mining enterprises by dangerous The purpose of the research was to assess the degree of damage to the areas adjacent to the tailings of mining enterprises by dangerous hydrogeological processes, flooding and inundation. The quantitative regime of groundwater is in a stable state and corresponds to the modern conditions of operation of industrial facilities. During the research, chemical pollution in groundwater of all aquifers was recorded. At the time of research, there was an increased content of such microcomponents as: carcinogenic cadmium and nickel (up to 1.9-34 MPC; and 2.6-8.4 MPC, respectively); non-carcinogenic lead (up to 1.7-7 MPC); manganese (up to 2-320 MPC); bromine (up to 14-94 MPC) in the groundwater of all aquifers in the north. In the center, there was the accumulation of abnormally high concentrations of elements such as iron, manganese (up to 36-1420 MPC rate of 0.3 mg / dm
3
and 1.3-66 MPC rate of 0.1 mg / dm
3
, respectively, and a significant increase in the value of dry residue and the content of major macrocomponents in all aquifers. In the south for the modern period there is pollution of groundwater of the Quaternary and Neogene systems with such elements as total iron (15-2800 MPC), manganese (1.9-132 MPC), sometimes vanadium, cadmium. The geochemical essence of the formation of the chemical composition of polluted waters lies in the intensity of changes in the hydrogeochemical system and in the change in the migratory properties of chemical elements. The newest techniques and scientific developments on localization and the prevention of migration of heavy metals with the subsequent pollution of waters are required. |
doi_str_mv | 10.1088/1755-1315/1049/1/012001 |
format | Article |
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3
and 1.3-66 MPC rate of 0.1 mg / dm
3
, respectively, and a significant increase in the value of dry residue and the content of major macrocomponents in all aquifers. In the south for the modern period there is pollution of groundwater of the Quaternary and Neogene systems with such elements as total iron (15-2800 MPC), manganese (1.9-132 MPC), sometimes vanadium, cadmium. The geochemical essence of the formation of the chemical composition of polluted waters lies in the intensity of changes in the hydrogeochemical system and in the change in the migratory properties of chemical elements. The newest techniques and scientific developments on localization and the prevention of migration of heavy metals with the subsequent pollution of waters are required.</description><identifier>ISSN: 1755-1307</identifier><identifier>EISSN: 1755-1315</identifier><identifier>DOI: 10.1088/1755-1315/1049/1/012001</identifier><language>eng</language><publisher>Bristol: IOP Publishing</publisher><subject>Aquifers ; Bromine ; Cadmium ; Carcinogens ; Chemical composition ; Chemical elements ; Chemical pollution ; Damage ; Flooding ; Geology ; Groundwater ; Groundwater pollution ; Groundwater supply ; Heavy metals ; Hydrogeochemistry ; Hydrogeology ; Industrial plants ; Industrial pollution ; Iron ; Iron ores ; Localization ; Manganese ; Mine tailings ; Neogene ; Nickel ; Pollution ; Storage facilities ; Tailings ; Vanadium</subject><ispartof>IOP conference series. Earth and environmental science, 2022-06, Vol.1049 (1), p.12001</ispartof><rights>Published under licence by IOP Publishing Ltd</rights><rights>Published under licence by IOP Publishing Ltd. This work is published under http://creativecommons.org/licenses/by/3.0/ (the “License”). Notwithstanding the ProQuest Terms and Conditions, you may use this content in accordance with the terms of the License.</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><cites>FETCH-LOGICAL-a2261-2e71f6470086cf0840775262f47efc22321a7539b8ce05d10739caf2c279a1093</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://iopscience.iop.org/article/10.1088/1755-1315/1049/1/012001/pdf$$EPDF$$P50$$Giop$$Hfree_for_read</linktopdf><link.rule.ids>314,780,784,27924,27925,38868,38890,53840,53867</link.rule.ids></links><search><creatorcontrib>Hrytsai, O</creatorcontrib><creatorcontrib>Petrukhin, A</creatorcontrib><creatorcontrib>Kulkova, T</creatorcontrib><title>Changes in hydrogeological conditions at the territories adjacent to tailings storage facilities in Kryvyi Rih iron ore basin</title><title>IOP conference series. Earth and environmental science</title><addtitle>IOP Conf. Ser.: Earth Environ. Sci</addtitle><description>Tailings of mining and processing plants of Kryvbas are new areas of groundwater supply which have led to significant changes in the hydrodynamic and hydrogeochemical regimes of aquifers. The purpose of the research was to assess the degree of damage to the areas adjacent to the tailings of mining enterprises by dangerous The purpose of the research was to assess the degree of damage to the areas adjacent to the tailings of mining enterprises by dangerous hydrogeological processes, flooding and inundation. The quantitative regime of groundwater is in a stable state and corresponds to the modern conditions of operation of industrial facilities. During the research, chemical pollution in groundwater of all aquifers was recorded. At the time of research, there was an increased content of such microcomponents as: carcinogenic cadmium and nickel (up to 1.9-34 MPC; and 2.6-8.4 MPC, respectively); non-carcinogenic lead (up to 1.7-7 MPC); manganese (up to 2-320 MPC); bromine (up to 14-94 MPC) in the groundwater of all aquifers in the north. In the center, there was the accumulation of abnormally high concentrations of elements such as iron, manganese (up to 36-1420 MPC rate of 0.3 mg / dm
3
and 1.3-66 MPC rate of 0.1 mg / dm
3
, respectively, and a significant increase in the value of dry residue and the content of major macrocomponents in all aquifers. In the south for the modern period there is pollution of groundwater of the Quaternary and Neogene systems with such elements as total iron (15-2800 MPC), manganese (1.9-132 MPC), sometimes vanadium, cadmium. The geochemical essence of the formation of the chemical composition of polluted waters lies in the intensity of changes in the hydrogeochemical system and in the change in the migratory properties of chemical elements. The newest techniques and scientific developments on localization and the prevention of migration of heavy metals with the subsequent pollution of waters are required.</description><subject>Aquifers</subject><subject>Bromine</subject><subject>Cadmium</subject><subject>Carcinogens</subject><subject>Chemical composition</subject><subject>Chemical elements</subject><subject>Chemical pollution</subject><subject>Damage</subject><subject>Flooding</subject><subject>Geology</subject><subject>Groundwater</subject><subject>Groundwater pollution</subject><subject>Groundwater supply</subject><subject>Heavy metals</subject><subject>Hydrogeochemistry</subject><subject>Hydrogeology</subject><subject>Industrial plants</subject><subject>Industrial pollution</subject><subject>Iron</subject><subject>Iron ores</subject><subject>Localization</subject><subject>Manganese</subject><subject>Mine tailings</subject><subject>Neogene</subject><subject>Nickel</subject><subject>Pollution</subject><subject>Storage facilities</subject><subject>Tailings</subject><subject>Vanadium</subject><issn>1755-1307</issn><issn>1755-1315</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2022</creationdate><recordtype>article</recordtype><sourceid>O3W</sourceid><sourceid>ABUWG</sourceid><sourceid>AFKRA</sourceid><sourceid>AZQEC</sourceid><sourceid>BENPR</sourceid><sourceid>CCPQU</sourceid><sourceid>DWQXO</sourceid><sourceid>GNUQQ</sourceid><recordid>eNqFkEtLxDAQx4souK5-BgOePKydpI-0R1nWBy4IPs4hmyZtlprUpCv04Hc3pbIiCJ5mmP9j4BdF5xiuMBRFjGmWLXCCsxhDWsY4BkwA8EE02yuH-x3ocXTi_RYgp2lSzqLPZcNNLT3SBjVD5WwtbWtrLXiLhDWV7rU1HvEe9Y1EvXRO99bpEODVlgtpgmBRz3WrTe2RDyKvJVJchEuvp-IHN3wMGj3pBmlnDbJOog332pxGR4q3Xp59z3n0erN6Wd4t1o-398vr9YITkuMFkRSrPKUARS4UFClQmpGcqJRKJQhJCOY0S8pNISRkFQaalIIrIggtOYYymUcXU2_n7PtO-p5t7c6Z8JKRvMgCxjwtgotOLuGs904q1jn9xt3AMLCRNRspspEoG1kzzCbWIXk5JbXtfqpXq-ffPtZVKniTP7z_ffgCRBSOcQ</recordid><startdate>20220601</startdate><enddate>20220601</enddate><creator>Hrytsai, O</creator><creator>Petrukhin, A</creator><creator>Kulkova, T</creator><general>IOP Publishing</general><scope>O3W</scope><scope>TSCCA</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>ABUWG</scope><scope>AFKRA</scope><scope>ATCPS</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BHPHI</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>GNUQQ</scope><scope>HCIFZ</scope><scope>PATMY</scope><scope>PIMPY</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PRINS</scope><scope>PYCSY</scope></search><sort><creationdate>20220601</creationdate><title>Changes in hydrogeological conditions at the territories adjacent to tailings storage facilities in Kryvyi Rih iron ore basin</title><author>Hrytsai, O ; Petrukhin, A ; Kulkova, T</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a2261-2e71f6470086cf0840775262f47efc22321a7539b8ce05d10739caf2c279a1093</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2022</creationdate><topic>Aquifers</topic><topic>Bromine</topic><topic>Cadmium</topic><topic>Carcinogens</topic><topic>Chemical composition</topic><topic>Chemical elements</topic><topic>Chemical pollution</topic><topic>Damage</topic><topic>Flooding</topic><topic>Geology</topic><topic>Groundwater</topic><topic>Groundwater pollution</topic><topic>Groundwater supply</topic><topic>Heavy metals</topic><topic>Hydrogeochemistry</topic><topic>Hydrogeology</topic><topic>Industrial plants</topic><topic>Industrial pollution</topic><topic>Iron</topic><topic>Iron ores</topic><topic>Localization</topic><topic>Manganese</topic><topic>Mine tailings</topic><topic>Neogene</topic><topic>Nickel</topic><topic>Pollution</topic><topic>Storage facilities</topic><topic>Tailings</topic><topic>Vanadium</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Hrytsai, O</creatorcontrib><creatorcontrib>Petrukhin, A</creatorcontrib><creatorcontrib>Kulkova, T</creatorcontrib><collection>Institute of Physics Open Access Journal Titles</collection><collection>IOPscience (Open Access)</collection><collection>CrossRef</collection><collection>ProQuest Central (Alumni Edition)</collection><collection>ProQuest Central UK/Ireland</collection><collection>Agricultural & Environmental Science Collection</collection><collection>ProQuest Central Essentials</collection><collection>ProQuest Central</collection><collection>Natural Science Collection</collection><collection>ProQuest One Community College</collection><collection>ProQuest Central Korea</collection><collection>ProQuest Central Student</collection><collection>SciTech Premium Collection</collection><collection>Environmental Science Database</collection><collection>Publicly Available Content Database</collection><collection>ProQuest One Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><collection>ProQuest Central China</collection><collection>Environmental Science Collection</collection><jtitle>IOP conference series. Earth and environmental science</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Hrytsai, O</au><au>Petrukhin, A</au><au>Kulkova, T</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Changes in hydrogeological conditions at the territories adjacent to tailings storage facilities in Kryvyi Rih iron ore basin</atitle><jtitle>IOP conference series. Earth and environmental science</jtitle><addtitle>IOP Conf. Ser.: Earth Environ. Sci</addtitle><date>2022-06-01</date><risdate>2022</risdate><volume>1049</volume><issue>1</issue><spage>12001</spage><pages>12001-</pages><issn>1755-1307</issn><eissn>1755-1315</eissn><abstract>Tailings of mining and processing plants of Kryvbas are new areas of groundwater supply which have led to significant changes in the hydrodynamic and hydrogeochemical regimes of aquifers. The purpose of the research was to assess the degree of damage to the areas adjacent to the tailings of mining enterprises by dangerous The purpose of the research was to assess the degree of damage to the areas adjacent to the tailings of mining enterprises by dangerous hydrogeological processes, flooding and inundation. The quantitative regime of groundwater is in a stable state and corresponds to the modern conditions of operation of industrial facilities. During the research, chemical pollution in groundwater of all aquifers was recorded. At the time of research, there was an increased content of such microcomponents as: carcinogenic cadmium and nickel (up to 1.9-34 MPC; and 2.6-8.4 MPC, respectively); non-carcinogenic lead (up to 1.7-7 MPC); manganese (up to 2-320 MPC); bromine (up to 14-94 MPC) in the groundwater of all aquifers in the north. In the center, there was the accumulation of abnormally high concentrations of elements such as iron, manganese (up to 36-1420 MPC rate of 0.3 mg / dm
3
and 1.3-66 MPC rate of 0.1 mg / dm
3
, respectively, and a significant increase in the value of dry residue and the content of major macrocomponents in all aquifers. In the south for the modern period there is pollution of groundwater of the Quaternary and Neogene systems with such elements as total iron (15-2800 MPC), manganese (1.9-132 MPC), sometimes vanadium, cadmium. The geochemical essence of the formation of the chemical composition of polluted waters lies in the intensity of changes in the hydrogeochemical system and in the change in the migratory properties of chemical elements. The newest techniques and scientific developments on localization and the prevention of migration of heavy metals with the subsequent pollution of waters are required.</abstract><cop>Bristol</cop><pub>IOP Publishing</pub><doi>10.1088/1755-1315/1049/1/012001</doi><tpages>11</tpages><oa>free_for_read</oa></addata></record> |
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subjects | Aquifers Bromine Cadmium Carcinogens Chemical composition Chemical elements Chemical pollution Damage Flooding Geology Groundwater Groundwater pollution Groundwater supply Heavy metals Hydrogeochemistry Hydrogeology Industrial plants Industrial pollution Iron Iron ores Localization Manganese Mine tailings Neogene Nickel Pollution Storage facilities Tailings Vanadium |
title | Changes in hydrogeological conditions at the territories adjacent to tailings storage facilities in Kryvyi Rih iron ore basin |
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