Preferential recharge in a reclaimed tailings sand upland: Implications on solute flushing

Study region: A peatland watershed was constructed on a post-mined oil sands lease in Northern Alberta, Canada, with the intention of replicating the function of natural wetlands removed by surface mining. Study focus: Given the potential for moisture limited conditions due to the sub-humid regional...

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Autores principales: Eric D. Kessel, Owen F. Sutton, Jonathan S. Price
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Lenguaje:EN
Publicado: Elsevier 2021
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Acceso en línea:https://doaj.org/article/efc8e3eb87cc4254ad377bf74d1b7f7a
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spelling oai:doaj.org-article:efc8e3eb87cc4254ad377bf74d1b7f7a2021-11-10T04:27:15ZPreferential recharge in a reclaimed tailings sand upland: Implications on solute flushing2214-581810.1016/j.ejrh.2021.100953https://doaj.org/article/efc8e3eb87cc4254ad377bf74d1b7f7a2021-12-01T00:00:00Zhttp://www.sciencedirect.com/science/article/pii/S2214581821001828https://doaj.org/toc/2214-5818Study region: A peatland watershed was constructed on a post-mined oil sands lease in Northern Alberta, Canada, with the intention of replicating the function of natural wetlands removed by surface mining. Study focus: Given the potential for moisture limited conditions due to the sub-humid regional climate, ensuring sufficient water availability in these landscapes is a principal concern. This research demonstrates how small recharge basins can modify the hydrology to promote groundwater recharge critical for sustaining saturated conditions in a downgradient wetland. New hydrological insights for the region: Location was important in determining the efficacy of recharge basins. Specifically, basins placed at the confluence of two hillslopes detained substantial volumes of runoff due to large upslope areas, contributing ~30% of the groundwater budget to the fen, while only occupying 1% of the upland area. Basins situated near low relief hillslopes or altogether isolated from a hillslope did not detain appreciable runoff and therefore had a minor role in recharging groundwater. Groundwater in the vicinity and downgradient of active recharge basins had considerably lower solute concentrations because of dilution. This suggests that basins can not only enhance recharge within engineered landscapes, providing a consistent and focused supply of water to upland aquifers, but offer relatively fresh groundwater to downgradient ecosystems. This could ameliorate the impact of high salinity present in oil sands process-affected materials.Eric D. KesselOwen F. SuttonJonathan S. PriceElsevierarticleRecharge basinsReclamationOil sands process-affected waterTailings sandAthabasca oil sands regionConstructed wetlandPhysical geographyGB3-5030GeologyQE1-996.5ENJournal of Hydrology: Regional Studies, Vol 38, Iss , Pp 100953- (2021)
institution DOAJ
collection DOAJ
language EN
topic Recharge basins
Reclamation
Oil sands process-affected water
Tailings sand
Athabasca oil sands region
Constructed wetland
Physical geography
GB3-5030
Geology
QE1-996.5
spellingShingle Recharge basins
Reclamation
Oil sands process-affected water
Tailings sand
Athabasca oil sands region
Constructed wetland
Physical geography
GB3-5030
Geology
QE1-996.5
Eric D. Kessel
Owen F. Sutton
Jonathan S. Price
Preferential recharge in a reclaimed tailings sand upland: Implications on solute flushing
description Study region: A peatland watershed was constructed on a post-mined oil sands lease in Northern Alberta, Canada, with the intention of replicating the function of natural wetlands removed by surface mining. Study focus: Given the potential for moisture limited conditions due to the sub-humid regional climate, ensuring sufficient water availability in these landscapes is a principal concern. This research demonstrates how small recharge basins can modify the hydrology to promote groundwater recharge critical for sustaining saturated conditions in a downgradient wetland. New hydrological insights for the region: Location was important in determining the efficacy of recharge basins. Specifically, basins placed at the confluence of two hillslopes detained substantial volumes of runoff due to large upslope areas, contributing ~30% of the groundwater budget to the fen, while only occupying 1% of the upland area. Basins situated near low relief hillslopes or altogether isolated from a hillslope did not detain appreciable runoff and therefore had a minor role in recharging groundwater. Groundwater in the vicinity and downgradient of active recharge basins had considerably lower solute concentrations because of dilution. This suggests that basins can not only enhance recharge within engineered landscapes, providing a consistent and focused supply of water to upland aquifers, but offer relatively fresh groundwater to downgradient ecosystems. This could ameliorate the impact of high salinity present in oil sands process-affected materials.
format article
author Eric D. Kessel
Owen F. Sutton
Jonathan S. Price
author_facet Eric D. Kessel
Owen F. Sutton
Jonathan S. Price
author_sort Eric D. Kessel
title Preferential recharge in a reclaimed tailings sand upland: Implications on solute flushing
title_short Preferential recharge in a reclaimed tailings sand upland: Implications on solute flushing
title_full Preferential recharge in a reclaimed tailings sand upland: Implications on solute flushing
title_fullStr Preferential recharge in a reclaimed tailings sand upland: Implications on solute flushing
title_full_unstemmed Preferential recharge in a reclaimed tailings sand upland: Implications on solute flushing
title_sort preferential recharge in a reclaimed tailings sand upland: implications on solute flushing
publisher Elsevier
publishDate 2021
url https://doaj.org/article/efc8e3eb87cc4254ad377bf74d1b7f7a
work_keys_str_mv AT ericdkessel preferentialrechargeinareclaimedtailingssanduplandimplicationsonsoluteflushing
AT owenfsutton preferentialrechargeinareclaimedtailingssanduplandimplicationsonsoluteflushing
AT jonathansprice preferentialrechargeinareclaimedtailingssanduplandimplicationsonsoluteflushing
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