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Projecting the hydrochemical trajectory of a constructed fen watershed: Implications for long-term wetland function. | LitMetric

Projecting the hydrochemical trajectory of a constructed fen watershed: Implications for long-term wetland function.

Sci Total Environ

Dept. of Geography and Env. Management, University of Waterloo, Waterloo, Ontario N2L 3G1, Canada.

Published: November 2022

AI Article Synopsis

  • Surface mining in the Athabasca Oil Sands has significantly damaged boreal forests and peatlands, prompting pilot projects that explore constructing fens as a potential reclamation strategy.
  • This study developed a groundwater flow and sodium transport model to evaluate the hydrologic and geochemical behavior of a constructed fen, predicting a stable water table and sufficient water to support local ecosystems despite variability in water quality.
  • The findings suggest that while high salt concentrations may hinder moss growth for years, salt-tolerant plants like sedges will thrive, and increasing the size of the fen could enhance overall peatland restoration without negatively impacting water retention.

Article Abstract

Surface mining operations for bitumen have fundamentally altered large areas of boreal forest and fen peatland in the Athabasca Oil Sands Region (AOSR) of Alberta, Canada. Pilot projects intended to assess the feasibility of fen construction as a reclamation option have been designed, built, and are currently undergoing monitoring. Initial assessments of ecohydrologic function have been conducted for these systems but offer limited insight into their evolution and likely successional pathway. Thus, this study projects the hydrologic and geochemical behaviour of a constructed fen watershed to understand whether the system will be capable of supporting peatland processes into the future. A numerical groundwater flow and sodium transport model was calibrated and validated with 7 years of hydraulic head, water flux, and water chemistry data. Based on Monte Carlo simulations, the projected fen water table would be stable and remain close to the surface (<15 cm), indicating that the design of the system can generate sufficient water quantity to meet evaporative demand and maintain surface water discharge. However, water quality was more sensitive to climatic variability, which induced a large range in potential sodium concentrations at the fen surface (450-850 mg L). Evapoconcentration of salts across the surface of the fen will likely limit moss establishment for decades following construction. Yet stress-thresholds of salt-tolerant vegetation like sedges will not be exceeded. Ultimately, these projections support the original design principles and philosophy that guided the creation of the watershed. Nonetheless, this work indicates that increasing the area of the fen relative to the upland would not have a detrimental impact on the ability of the system to maintain a high water table. This could allow for the proportion of peatlands on the reclamation landscape to reflect the pre-disturbance environment more faithfully.

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Source
http://dx.doi.org/10.1016/j.scitotenv.2022.157543DOI Listing

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