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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2021
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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) |
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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 |
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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 |
_version_ |
1718440706310144000 |