Temporal fluctuations in water contamination from abandoned pyrite Wieściszowice mine (Western Sudetes, Poland)
Production of acid mine drainage may occur during mining operations and may continue for many years after closure. In some cases, especially when host rock is capable of reacting with acidic drainage, metal concentrations may decrease over time and distance. Seasonal variations in water flow rate al...
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| Veröffentlicht in: | Environmental geochemistry and health 2021-08, Vol.43 (8), p.3115-3132 |
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| creator | Costa, Maria R. Marszałek, Henryk da Silva, Eduardo Ferreira Mickiewicz, Agata Wąsik, Mirosław Candeias, Carla |
| description | Production of acid mine drainage may occur during mining operations and may continue for many years after closure. In some cases, especially when host rock is capable of reacting with acidic drainage, metal concentrations may decrease over time and distance. Seasonal variations in water flow rate also play an important role in metals concentration both in surface and groundwater. The present study evaluates the contamination of an abandoned pyrite mining area (Wieściszowice, SW Poland) and the temporal variation of the water contamination in selected locations of 2 sampling campaigns (2000 and 2015). The mining surrounding Rudawy Janowickie Mountains range is well known for the rich mining history and is considered as one of the oldest in Europe. The Wieściszowice pyrite mine was exploited for several hundreds of years and processed Fe and Cu sulfides, and sulfur. This mine was closed in 1925 because of the high competition of pyrites from Spain. Results show clearly that water samples collected in the mining area are mainly Ca–SO
4
and acid/high metal, while spring water and surface water samples, representing the local geochemical background, are Ca–HCO
3
and neutral-low metal. The analysis of data shows an improvement in water quality from 2000 to 2015 as well as a decreasing of water risk assessment for human use. This improvement can be related to the fact that 2015 was a very dry year, with over 60% less flow than in 2000, leading to less water contamination. |
| doi_str_mv | 10.1007/s10653-021-00809-1 |
| format | Article |
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4
and acid/high metal, while spring water and surface water samples, representing the local geochemical background, are Ca–HCO
3
and neutral-low metal. The analysis of data shows an improvement in water quality from 2000 to 2015 as well as a decreasing of water risk assessment for human use. This improvement can be related to the fact that 2015 was a very dry year, with over 60% less flow than in 2000, leading to less water contamination.</description><identifier>ISSN: 0269-4042</identifier><identifier>EISSN: 1573-2983</identifier><identifier>DOI: 10.1007/s10653-021-00809-1</identifier><identifier>PMID: 33507468</identifier><language>eng</language><publisher>Dordrecht: Springer Netherlands</publisher><subject>Abandoned mines ; Acid mine drainage ; Calcium ; Contamination ; Copper ; Earth and Environmental Science ; Environment ; Environmental Chemistry ; Environmental Health ; Flow rates ; Flow velocity ; Geochemistry ; Groundwater ; Metal concentrations ; Metals ; Mine drainage ; Mining ; Mountains ; Original Paper ; Public Health ; Pyrite ; Risk assessment ; Seasonal variation ; Seasonal variations ; Soil Science & Conservation ; Spring water ; Sulfur ; Sulphates ; Sulphur ; Surface water ; Temporal variations ; Terrestrial Pollution ; Water analysis ; Water flow ; Water pollution ; Water quality ; Water sampling</subject><ispartof>Environmental geochemistry and health, 2021-08, Vol.43 (8), p.3115-3132</ispartof><rights>The Author(s), under exclusive licence to Springer Nature B.V. part of Springer Nature 2021</rights><rights>The Author(s), under exclusive licence to Springer Nature B.V. part of Springer Nature 2021.</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a425t-9907ba04f6f801957973d72205a19f4388effe06ec38801b2d6943f8e21b3ebe3</citedby><cites>FETCH-LOGICAL-a425t-9907ba04f6f801957973d72205a19f4388effe06ec38801b2d6943f8e21b3ebe3</cites><orcidid>0000-0001-6664-8545 ; 0000-0002-3019-8471 ; 0000-0003-0102-5595 ; 0000-0002-4283-8712 ; 0000-0003-0894-1553</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1007/s10653-021-00809-1$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1007/s10653-021-00809-1$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,776,780,27901,27902,41464,42533,51294</link.rule.ids><backlink>$$Uhttps://www.ncbi.nlm.nih.gov/pubmed/33507468$$D View this record in MEDLINE/PubMed$$Hfree_for_read</backlink></links><search><creatorcontrib>Costa, Maria R.</creatorcontrib><creatorcontrib>Marszałek, Henryk</creatorcontrib><creatorcontrib>da Silva, Eduardo Ferreira</creatorcontrib><creatorcontrib>Mickiewicz, Agata</creatorcontrib><creatorcontrib>Wąsik, Mirosław</creatorcontrib><creatorcontrib>Candeias, Carla</creatorcontrib><title>Temporal fluctuations in water contamination from abandoned pyrite Wieściszowice mine (Western Sudetes, Poland)</title><title>Environmental geochemistry and health</title><addtitle>Environ Geochem Health</addtitle><addtitle>Environ Geochem Health</addtitle><description>Production of acid mine drainage may occur during mining operations and may continue for many years after closure. In some cases, especially when host rock is capable of reacting with acidic drainage, metal concentrations may decrease over time and distance. Seasonal variations in water flow rate also play an important role in metals concentration both in surface and groundwater. The present study evaluates the contamination of an abandoned pyrite mining area (Wieściszowice, SW Poland) and the temporal variation of the water contamination in selected locations of 2 sampling campaigns (2000 and 2015). The mining surrounding Rudawy Janowickie Mountains range is well known for the rich mining history and is considered as one of the oldest in Europe. The Wieściszowice pyrite mine was exploited for several hundreds of years and processed Fe and Cu sulfides, and sulfur. This mine was closed in 1925 because of the high competition of pyrites from Spain. Results show clearly that water samples collected in the mining area are mainly Ca–SO
4
and acid/high metal, while spring water and surface water samples, representing the local geochemical background, are Ca–HCO
3
and neutral-low metal. The analysis of data shows an improvement in water quality from 2000 to 2015 as well as a decreasing of water risk assessment for human use. This improvement can be related to the fact that 2015 was a very dry year, with over 60% less flow than in 2000, leading to less water contamination.</description><subject>Abandoned mines</subject><subject>Acid mine drainage</subject><subject>Calcium</subject><subject>Contamination</subject><subject>Copper</subject><subject>Earth and Environmental Science</subject><subject>Environment</subject><subject>Environmental Chemistry</subject><subject>Environmental Health</subject><subject>Flow rates</subject><subject>Flow velocity</subject><subject>Geochemistry</subject><subject>Groundwater</subject><subject>Metal concentrations</subject><subject>Metals</subject><subject>Mine drainage</subject><subject>Mining</subject><subject>Mountains</subject><subject>Original Paper</subject><subject>Public Health</subject><subject>Pyrite</subject><subject>Risk assessment</subject><subject>Seasonal variation</subject><subject>Seasonal variations</subject><subject>Soil Science & Conservation</subject><subject>Spring water</subject><subject>Sulfur</subject><subject>Sulphates</subject><subject>Sulphur</subject><subject>Surface water</subject><subject>Temporal variations</subject><subject>Terrestrial Pollution</subject><subject>Water analysis</subject><subject>Water flow</subject><subject>Water pollution</subject><subject>Water quality</subject><subject>Water 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fluctuations in water contamination from abandoned pyrite Wieściszowice mine (Western Sudetes, Poland)</title><author>Costa, Maria R. ; Marszałek, Henryk ; da Silva, Eduardo Ferreira ; Mickiewicz, Agata ; Wąsik, Mirosław ; Candeias, Carla</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a425t-9907ba04f6f801957973d72205a19f4388effe06ec38801b2d6943f8e21b3ebe3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2021</creationdate><topic>Abandoned mines</topic><topic>Acid mine drainage</topic><topic>Calcium</topic><topic>Contamination</topic><topic>Copper</topic><topic>Earth and Environmental Science</topic><topic>Environment</topic><topic>Environmental Chemistry</topic><topic>Environmental Health</topic><topic>Flow rates</topic><topic>Flow velocity</topic><topic>Geochemistry</topic><topic>Groundwater</topic><topic>Metal concentrations</topic><topic>Metals</topic><topic>Mine 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Carla</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Temporal fluctuations in water contamination from abandoned pyrite Wieściszowice mine (Western Sudetes, Poland)</atitle><jtitle>Environmental geochemistry and health</jtitle><stitle>Environ Geochem Health</stitle><addtitle>Environ Geochem Health</addtitle><date>2021-08-01</date><risdate>2021</risdate><volume>43</volume><issue>8</issue><spage>3115</spage><epage>3132</epage><pages>3115-3132</pages><issn>0269-4042</issn><eissn>1573-2983</eissn><abstract>Production of acid mine drainage may occur during mining operations and may continue for many years after closure. In some cases, especially when host rock is capable of reacting with acidic drainage, metal concentrations may decrease over time and distance. Seasonal variations in water flow rate also play an important role in metals concentration both in surface and groundwater. The present study evaluates the contamination of an abandoned pyrite mining area (Wieściszowice, SW Poland) and the temporal variation of the water contamination in selected locations of 2 sampling campaigns (2000 and 2015). The mining surrounding Rudawy Janowickie Mountains range is well known for the rich mining history and is considered as one of the oldest in Europe. The Wieściszowice pyrite mine was exploited for several hundreds of years and processed Fe and Cu sulfides, and sulfur. This mine was closed in 1925 because of the high competition of pyrites from Spain. Results show clearly that water samples collected in the mining area are mainly Ca–SO
4
and acid/high metal, while spring water and surface water samples, representing the local geochemical background, are Ca–HCO
3
and neutral-low metal. The analysis of data shows an improvement in water quality from 2000 to 2015 as well as a decreasing of water risk assessment for human use. This improvement can be related to the fact that 2015 was a very dry year, with over 60% less flow than in 2000, leading to less water contamination.</abstract><cop>Dordrecht</cop><pub>Springer Netherlands</pub><pmid>33507468</pmid><doi>10.1007/s10653-021-00809-1</doi><tpages>18</tpages><orcidid>https://orcid.org/0000-0001-6664-8545</orcidid><orcidid>https://orcid.org/0000-0002-3019-8471</orcidid><orcidid>https://orcid.org/0000-0003-0102-5595</orcidid><orcidid>https://orcid.org/0000-0002-4283-8712</orcidid><orcidid>https://orcid.org/0000-0003-0894-1553</orcidid><oa>free_for_read</oa></addata></record> |
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| subjects | Abandoned mines Acid mine drainage Calcium Contamination Copper Earth and Environmental Science Environment Environmental Chemistry Environmental Health Flow rates Flow velocity Geochemistry Groundwater Metal concentrations Metals Mine drainage Mining Mountains Original Paper Public Health Pyrite Risk assessment Seasonal variation Seasonal variations Soil Science & Conservation Spring water Sulfur Sulphates Sulphur Surface water Temporal variations Terrestrial Pollution Water analysis Water flow Water pollution Water quality Water sampling |
| title | Temporal fluctuations in water contamination from abandoned pyrite Wieściszowice mine (Western Sudetes, Poland) |
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