Metal Mobility in a Mine-Affected Floodplain

The study attempted to map and predict the remobilization of metals in a floodplain which had been heavily affected by long-term Zn–Pb mining. This research, based on Zn, Cd, Pb, Ca and Fe speciation, mineralogy and the stratigraphy of sediments which had accumulated over the distance of a dozen or...

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Main Authors: Dariusz Ciszewski, Urszula Aleksander-Kwaterczak
Format: Article
Language:English
Published: MDPI AG 2020-09-01
Series:Minerals
Subjects:
Online Access:https://www.mdpi.com/2075-163X/10/9/814
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spelling doaj-1c721a711ce144d887e6706961874b712020-11-25T03:06:47ZengMDPI AGMinerals2075-163X2020-09-011081481410.3390/min10090814Metal Mobility in a Mine-Affected FloodplainDariusz Ciszewski0Urszula Aleksander-Kwaterczak1Faculty of Geology, Geophysics and Environmental Protection, AGH University of Science and Technology, A. Mickiewicza Av. 30, 30-059 Krakow, PolandFaculty of Geology, Geophysics and Environmental Protection, AGH University of Science and Technology, A. Mickiewicza Av. 30, 30-059 Krakow, PolandThe study attempted to map and predict the remobilization of metals in a floodplain which had been heavily affected by long-term Zn–Pb mining. This research, based on Zn, Cd, Pb, Ca and Fe speciation, mineralogy and the stratigraphy of sediments which had accumulated over the distance of a dozen or so km from the mine, revealed variable potential for metal mobilization. The results suggest that a drop in the water table, something to be expected after the closure of a mine, would be accompanied by a decrease in the pH of the river water and can induce the remobilization of metals associated with carbonates and exchangeable cations over the short-reach downstream of the mine. However, the mobilization of contaminants may be impeded by the alkaline, impermeable stratum of loams, which play a pivotal role in maintaining anaerobic conditions and buffering the acidity resulting from the partial degradation of sulfides. Based on the findings of the study, it can be expected that the intrinsic attenuation will limit the need for remediation works, although monitoring river water quality is recommended to determine the need for any intervention in cases where permissible quality values have been exceeded over a longer period. Results of this research can be useful as a reference for remediation works planned in other contaminated river systems experiencing water table lowering, where the mobilization of contaminants as a consequence of sediment oxidization can be expected.https://www.mdpi.com/2075-163X/10/9/814miningmetalsmine closuresedimentpollutionmine water
collection DOAJ
language English
format Article
sources DOAJ
author Dariusz Ciszewski
Urszula Aleksander-Kwaterczak
spellingShingle Dariusz Ciszewski
Urszula Aleksander-Kwaterczak
Metal Mobility in a Mine-Affected Floodplain
Minerals
mining
metals
mine closure
sediment
pollution
mine water
author_facet Dariusz Ciszewski
Urszula Aleksander-Kwaterczak
author_sort Dariusz Ciszewski
title Metal Mobility in a Mine-Affected Floodplain
title_short Metal Mobility in a Mine-Affected Floodplain
title_full Metal Mobility in a Mine-Affected Floodplain
title_fullStr Metal Mobility in a Mine-Affected Floodplain
title_full_unstemmed Metal Mobility in a Mine-Affected Floodplain
title_sort metal mobility in a mine-affected floodplain
publisher MDPI AG
series Minerals
issn 2075-163X
publishDate 2020-09-01
description The study attempted to map and predict the remobilization of metals in a floodplain which had been heavily affected by long-term Zn–Pb mining. This research, based on Zn, Cd, Pb, Ca and Fe speciation, mineralogy and the stratigraphy of sediments which had accumulated over the distance of a dozen or so km from the mine, revealed variable potential for metal mobilization. The results suggest that a drop in the water table, something to be expected after the closure of a mine, would be accompanied by a decrease in the pH of the river water and can induce the remobilization of metals associated with carbonates and exchangeable cations over the short-reach downstream of the mine. However, the mobilization of contaminants may be impeded by the alkaline, impermeable stratum of loams, which play a pivotal role in maintaining anaerobic conditions and buffering the acidity resulting from the partial degradation of sulfides. Based on the findings of the study, it can be expected that the intrinsic attenuation will limit the need for remediation works, although monitoring river water quality is recommended to determine the need for any intervention in cases where permissible quality values have been exceeded over a longer period. Results of this research can be useful as a reference for remediation works planned in other contaminated river systems experiencing water table lowering, where the mobilization of contaminants as a consequence of sediment oxidization can be expected.
topic mining
metals
mine closure
sediment
pollution
mine water
url https://www.mdpi.com/2075-163X/10/9/814
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