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Evaluating the Hydrological Response of a Boreal Fen Following the Removal of a Temporary Access Road
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Removal and reclamation should be considered as a worthwhile venture for roads that extend through fens and are no longer in use.
Graminoids Vary in Functional Traits, Carbon Dioxide and Methane Fluxes in a Restored Peatland: Implications for Modeling Carbon Storage
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One metric of peatland restoration success is the re-establishment of a carbon sink, yet considerable uncertainty remains around the timescale of carbon sink trajectories. Conditions post-restoration...
Groundwater in Peat and Peatlands
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Peatlands are wetlands with soil comprised of undecomposed remains of plants that accumulate in such a way that both responds to and controls the flux and storage of surface water and groundwater, as...
How Mounds are Made Matters: Seismic Line Restoration Techniques Affect Peat Physical and Chemical Properties Throughout the Peat Profile
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This resource is available on an external database and may require a paid subscription to access it. It is included on the CCLM to support our goal of capturing and sharing the breadth of all...
Impact of Heat Advection on the Thermal Regime of Roads Built on Permafrost
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This resource is available on an external database and may require a paid subscription to access it. It is included on the CCLM to support our goal of capturing and sharing the breadth of all...
Impact of Linear Disturbances on Boreal Wetland Carbon and Greenhouse Gas Exchange
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This presentation provides and overview of linear disturbance impacts on carbon and greenhouse gas exchange and links various research posters also presented at the NAIT 7th Seminar on Linear...
Impacts of Seismic Line Restoration on CO2, CH4, and Biomass
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This thesis explores how seismic line mounding treatments affect vegetation cover and composition, above- and belowground biomass, and carbon dioxide (CO 2) and methane (CH 4) fluxes in the first two...
Increasing Contributions of Peatlands to Boreal Evapotranspiration in a Warming Climate
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The response of evapotranspiration (ET) to warming is of critical importance to the water and carbon cycle of the boreal biome, a mosaic of land cover types dominated by forests and peatlands. The...
Influence of Operational Sex Ratio and Male Age on Mating Competition Intensity in Reindeer (Rangifer tarandus)
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This resource is available on an external database and may require a paid subscription to access it. It is included on the CCLM to support our goal of capturing and sharing the breadth of all...
Integrated Surface-subsurface Water and Solute Modeling of a Reclaimed In-pit Oil Sands Mine: Effects of Ground Freezing and Thawing
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The upland and wetlands substrate in reclaimed oil sands landforms will be constructed of post-mining materials with an objective of replicating the landscape and hydrology of the surrounding boreal...
Interweaving Local, Expert, and Indigenous Knowledge into Quantitative Wildlife Analyses: A Systematic Review
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Inclusion of local, expert, or Indigenous knowledge about wildlife populations and their habitats can inform wildlife research, while also increasing knowledge holder engagement and support for...
Lichens: A Limit to Peat Growth?
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The fruticose lichens Cladina stellaris and Cladina rangiferina, form thick mats that can cover large areas of northern peatlands (above c. 50° latitude), including the extensive peatlands of the...
Linear Disturbances Shift Boreal Peatland Plant Communities Toward Earlier Peak Greenness
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Vast areas of boreal peatlands are impacted by linear disturbances known as seismic lines. Tree removal and ground disturbance alter vegetation communities and are expected to change ecosystem...