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Growth of Coal Mining Operations in the Elk River Valley (Canada) Linked to Increasing Solute Transport of Se, NO(3)(–), and SO(4)(2–) into the Transboundary Koocanusa Reservoir (USA–Canada)

[Image: see text] Koocanusa Reservoir (KOC) is a waterbody that spans the United States (U.S.) and Canadian border. Increasing concentrations of total selenium (Se), nitrate + nitrite (NO(3)(–), nitrite is insignificant or not present), and sulfate (SO(4)(2–)) in KOC and downstream in the Kootenai R...

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Autores principales: Storb, Meryl B., Bussell, Ashley M., Caldwell Eldridge, Sara L., Hirsch, Robert M., Schmidt, Travis S.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: American Chemical Society 2023
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC10653222/
https://www.ncbi.nlm.nih.gov/pubmed/37922122
http://dx.doi.org/10.1021/acs.est.3c05090
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author Storb, Meryl B.
Bussell, Ashley M.
Caldwell Eldridge, Sara L.
Hirsch, Robert M.
Schmidt, Travis S.
author_facet Storb, Meryl B.
Bussell, Ashley M.
Caldwell Eldridge, Sara L.
Hirsch, Robert M.
Schmidt, Travis S.
author_sort Storb, Meryl B.
collection PubMed
description [Image: see text] Koocanusa Reservoir (KOC) is a waterbody that spans the United States (U.S.) and Canadian border. Increasing concentrations of total selenium (Se), nitrate + nitrite (NO(3)(–), nitrite is insignificant or not present), and sulfate (SO(4)(2–)) in KOC and downstream in the Kootenai River (Kootenay River in Canada) are tied to expanding coal mining operations in the Elk River Watershed, Canada. Using a paired watershed approach, trends in flow-normalized concentrations and loads were evaluated for Se, NO(3)(–), and SO(4)(2–) for the two largest tributaries, the Kootenay and Elk Rivers, Canada. Increases in concentration (SO(4)(2–) 120%, Se 581%, NO(3)(–) 784%) and load (SO(4)(2–) 129%, Se 443%, NO(3)(–) 697%) in the Elk River (1979–2022 for NO(3)(–), 1984–2022 for Se and SO(4)(2–)) are among the largest documented increases in the primary literature, while only a small magnitude increase in SO(4)(2–) (7.7% concentration) and decreases in Se (−10%) and NO(3)(–) (−8.5%) were observed in the Kootenay River. Between 2009 and 2019, the Elk River contributed, on average, 29% of the combined flow, 95% of the Se, 76% of the NO(3)(–), and 38% of the SO(4)(2–) entering the reservoir from these two major tributaries. The largest increase in solute concentrations occurred during baseflows, indicating a change in solute transport and delivery dynamics in the Elk River Watershed, which may be attributable to altered landscapes from coal mining operations including altered groundwater flow paths and increased chemical weathering in waste rock dumps. More recently there is evidence of surface water treatment operations providing some reduction in concentrations during low flow times of year; however, these appear to have a limited effect on annual loads entering KOC. These findings imply that current mine water treatment, which is focused on surface waters, may not sufficiently reduce the influence of mine-waste-derived solutes in the Elk River to allow constituent concentrations in KOC to meet U.S. water-quality standards.
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spelling pubmed-106532222023-11-16 Growth of Coal Mining Operations in the Elk River Valley (Canada) Linked to Increasing Solute Transport of Se, NO(3)(–), and SO(4)(2–) into the Transboundary Koocanusa Reservoir (USA–Canada) Storb, Meryl B. Bussell, Ashley M. Caldwell Eldridge, Sara L. Hirsch, Robert M. Schmidt, Travis S. Environ Sci Technol [Image: see text] Koocanusa Reservoir (KOC) is a waterbody that spans the United States (U.S.) and Canadian border. Increasing concentrations of total selenium (Se), nitrate + nitrite (NO(3)(–), nitrite is insignificant or not present), and sulfate (SO(4)(2–)) in KOC and downstream in the Kootenai River (Kootenay River in Canada) are tied to expanding coal mining operations in the Elk River Watershed, Canada. Using a paired watershed approach, trends in flow-normalized concentrations and loads were evaluated for Se, NO(3)(–), and SO(4)(2–) for the two largest tributaries, the Kootenay and Elk Rivers, Canada. Increases in concentration (SO(4)(2–) 120%, Se 581%, NO(3)(–) 784%) and load (SO(4)(2–) 129%, Se 443%, NO(3)(–) 697%) in the Elk River (1979–2022 for NO(3)(–), 1984–2022 for Se and SO(4)(2–)) are among the largest documented increases in the primary literature, while only a small magnitude increase in SO(4)(2–) (7.7% concentration) and decreases in Se (−10%) and NO(3)(–) (−8.5%) were observed in the Kootenay River. Between 2009 and 2019, the Elk River contributed, on average, 29% of the combined flow, 95% of the Se, 76% of the NO(3)(–), and 38% of the SO(4)(2–) entering the reservoir from these two major tributaries. The largest increase in solute concentrations occurred during baseflows, indicating a change in solute transport and delivery dynamics in the Elk River Watershed, which may be attributable to altered landscapes from coal mining operations including altered groundwater flow paths and increased chemical weathering in waste rock dumps. More recently there is evidence of surface water treatment operations providing some reduction in concentrations during low flow times of year; however, these appear to have a limited effect on annual loads entering KOC. These findings imply that current mine water treatment, which is focused on surface waters, may not sufficiently reduce the influence of mine-waste-derived solutes in the Elk River to allow constituent concentrations in KOC to meet U.S. water-quality standards. American Chemical Society 2023-11-03 /pmc/articles/PMC10653222/ /pubmed/37922122 http://dx.doi.org/10.1021/acs.est.3c05090 Text en Not subject to U.S. Copyright. Published 2023 by American Chemical Society https://creativecommons.org/licenses/by/4.0/Permits the broadest form of re-use including for commercial purposes, provided that author attribution and integrity are maintained (https://creativecommons.org/licenses/by/4.0/).
spellingShingle Storb, Meryl B.
Bussell, Ashley M.
Caldwell Eldridge, Sara L.
Hirsch, Robert M.
Schmidt, Travis S.
Growth of Coal Mining Operations in the Elk River Valley (Canada) Linked to Increasing Solute Transport of Se, NO(3)(–), and SO(4)(2–) into the Transboundary Koocanusa Reservoir (USA–Canada)
title Growth of Coal Mining Operations in the Elk River Valley (Canada) Linked to Increasing Solute Transport of Se, NO(3)(–), and SO(4)(2–) into the Transboundary Koocanusa Reservoir (USA–Canada)
title_full Growth of Coal Mining Operations in the Elk River Valley (Canada) Linked to Increasing Solute Transport of Se, NO(3)(–), and SO(4)(2–) into the Transboundary Koocanusa Reservoir (USA–Canada)
title_fullStr Growth of Coal Mining Operations in the Elk River Valley (Canada) Linked to Increasing Solute Transport of Se, NO(3)(–), and SO(4)(2–) into the Transboundary Koocanusa Reservoir (USA–Canada)
title_full_unstemmed Growth of Coal Mining Operations in the Elk River Valley (Canada) Linked to Increasing Solute Transport of Se, NO(3)(–), and SO(4)(2–) into the Transboundary Koocanusa Reservoir (USA–Canada)
title_short Growth of Coal Mining Operations in the Elk River Valley (Canada) Linked to Increasing Solute Transport of Se, NO(3)(–), and SO(4)(2–) into the Transboundary Koocanusa Reservoir (USA–Canada)
title_sort growth of coal mining operations in the elk river valley (canada) linked to increasing solute transport of se, no(3)(–), and so(4)(2–) into the transboundary koocanusa reservoir (usa–canada)
url https://www.ncbi.nlm.nih.gov/pmc/articles/PMC10653222/
https://www.ncbi.nlm.nih.gov/pubmed/37922122
http://dx.doi.org/10.1021/acs.est.3c05090
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