An Assessment of the Water Table Dynamics in a Constructed Wetland, Fort McMurray, Alberta

Oil sand mining removes the wetland and forestlands of the Boreal Plains, and replaces this landscape with open pits, tailings ponds and overburden piles to access the oil-bearing formations below. In turn, mine regulators are forced to reclaim the disturbed, post-mined land to pre-disturbance condi...

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Main Author: Spennato, Haley
Other Authors: Carey, Sean, Environmental Science
Format: Thesis
Language:English
Published: 2016
Subjects:
Online Access:http://hdl.handle.net/11375/20427
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spelling ftmcmaster:oai:macsphere.mcmaster.ca:11375/20427 2023-05-15T16:17:39+02:00 An Assessment of the Water Table Dynamics in a Constructed Wetland, Fort McMurray, Alberta Spennato, Haley Carey, Sean Environmental Science 2016 http://hdl.handle.net/11375/20427 en eng http://hdl.handle.net/11375/20427 Thesis 2016 ftmcmaster 2022-03-22T21:13:58Z Oil sand mining removes the wetland and forestlands of the Boreal Plains, and replaces this landscape with open pits, tailings ponds and overburden piles to access the oil-bearing formations below. In turn, mine regulators are forced to reclaim the disturbed, post-mined land to pre-disturbance conditions. In 2012, Syncrude Canada Limited (SCL) constructed one of the first of two reclaimed wetlands, the Sandhill Fen Watershed (SFW), to evaluate wetland reclamation strategies. SFW is a 52-ha system atop soft-tailings that includes an inflow/outflow pump system, underdrains, upland hummock areas, and a fen lowland. This study examines trends in water table position and lateral gradients that are developing, as well as observe system response to pump management. Spanning May- Oct 2014 and 2015, precipitation was measured at three meteorological stations across the fen, artificial inflows and outflows were recorded using a series of pumps, and water table position was measured using a network of 27 near-surface wells instrumented with transducers. Water table was maintained near the peat surface for both study seasons, indicating the potential for maintenance of wetland conditions. Though data is limited, upland-lowland interactions are beginning to develop, suggesting the uplands are beginning to supply water to the lowland fen. Flow reversals are reported along the fen lowland in dry periods, and the east and west fens become hydrologically disconnected as the season progresses. Comparison with analogue sites provides reference for hydrologic processes within SFW and provides insight on the influence of pump management on the system. Thesis Master of Science (MSc) Thesis Fort McMurray MacSphere (McMaster University) Fort McMurray Canada
institution Open Polar
collection MacSphere (McMaster University)
op_collection_id ftmcmaster
language English
description Oil sand mining removes the wetland and forestlands of the Boreal Plains, and replaces this landscape with open pits, tailings ponds and overburden piles to access the oil-bearing formations below. In turn, mine regulators are forced to reclaim the disturbed, post-mined land to pre-disturbance conditions. In 2012, Syncrude Canada Limited (SCL) constructed one of the first of two reclaimed wetlands, the Sandhill Fen Watershed (SFW), to evaluate wetland reclamation strategies. SFW is a 52-ha system atop soft-tailings that includes an inflow/outflow pump system, underdrains, upland hummock areas, and a fen lowland. This study examines trends in water table position and lateral gradients that are developing, as well as observe system response to pump management. Spanning May- Oct 2014 and 2015, precipitation was measured at three meteorological stations across the fen, artificial inflows and outflows were recorded using a series of pumps, and water table position was measured using a network of 27 near-surface wells instrumented with transducers. Water table was maintained near the peat surface for both study seasons, indicating the potential for maintenance of wetland conditions. Though data is limited, upland-lowland interactions are beginning to develop, suggesting the uplands are beginning to supply water to the lowland fen. Flow reversals are reported along the fen lowland in dry periods, and the east and west fens become hydrologically disconnected as the season progresses. Comparison with analogue sites provides reference for hydrologic processes within SFW and provides insight on the influence of pump management on the system. Thesis Master of Science (MSc)
author2 Carey, Sean
Environmental Science
format Thesis
author Spennato, Haley
spellingShingle Spennato, Haley
An Assessment of the Water Table Dynamics in a Constructed Wetland, Fort McMurray, Alberta
author_facet Spennato, Haley
author_sort Spennato, Haley
title An Assessment of the Water Table Dynamics in a Constructed Wetland, Fort McMurray, Alberta
title_short An Assessment of the Water Table Dynamics in a Constructed Wetland, Fort McMurray, Alberta
title_full An Assessment of the Water Table Dynamics in a Constructed Wetland, Fort McMurray, Alberta
title_fullStr An Assessment of the Water Table Dynamics in a Constructed Wetland, Fort McMurray, Alberta
title_full_unstemmed An Assessment of the Water Table Dynamics in a Constructed Wetland, Fort McMurray, Alberta
title_sort assessment of the water table dynamics in a constructed wetland, fort mcmurray, alberta
publishDate 2016
url http://hdl.handle.net/11375/20427
geographic Fort McMurray
Canada
geographic_facet Fort McMurray
Canada
genre Fort McMurray
genre_facet Fort McMurray
op_relation http://hdl.handle.net/11375/20427
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