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Grant: Collaborative Research and Development Grants

University of Western Ontario

$12,000.00

Large scale climate chamber simulations of permafrost environments

FY 2009-10

Summary
The proposed research is a critical step in our long-term research program to provide new insight and quantification of the effects of climate change on the groundwater and surface water of Canada's subarctic regions. The overall long-term focus is on quantifying the hydrologic, geotechnical, and biogeochemical response of wetland-dominated discontinuous permafrost to atmospheric temperature and solar variations. Specifically, for this CRD project, large-scale experiments on peat samples from the central Mackenzie River basin will be coupled with on-going field studies to better elucidate active layer moisture transport processes. Central to the research is a Canadian Foundation for Innovation (CFI) funded climate chamber, at the University of Western Ontario Biotron facility, which can reproduce the Canadian subarctic solar and atmospheric environment and house soil monoliths up to 1.5 m in diameter and 4 m in height. No other similar facility exists in Canada, U.S., or perhaps the world. Undisturbed peat cores 60 cm in diameter and ~ 75 cm deep, inclusive of vegetation, were taken in August 2007 at our field site near Fort Simpson NWT. Once the chamber and soil monolith operational parameters have been verified to field conditions, a key component of this CRD project, a wide range of climate forcing experiments (varying solar energy, air temperatures, precipitation, CO2) will be performed. Of particular interest is to quantify the moisture dynamics at the active-layer / permafrost transition zone and develop numerical models for estimating the position of this interface and the water table during seasonal ground thawing. These dynamics need to be understood in order to estimate the volume and timing of runoff from wetland-dominated basins in discontinuous permafrost zones. The experiments will answer critical questions, not addressable by field data alone, on how Canada's subarctic ecosystems will respond to climate change. Furthermore, validating the climate chamber as a tool to study cold region ecohydrological processes will allow the facility and BioChambers Inc. to be recognized nationally / internationally and stimulate further research and development.
Program
Collaborative Research and Development Grants
Location
Ontario, Canada
Recipient Type
Academia
Type
Grant
Source
NSERC's Awards Data

As published

Application id
379766-2008
Name nom
Schincariol, Robert
Department département
Earth Sciences
Organization id
36
Institution établissement
University of Western Ontario
Province en
Ontario
Province fr
Ontario
Country en
CANADA
Country fr
CANADA
Fiscal year exercice financier
2009
Competition year année de concours
2008
Award amount
12000
Program id
CRDPJ
Program nane en
Collaborative Research and Development Grants
Program name fr
Subventions de recherche et développement coopérative
Group en
Research partnerships programs
Group fr
Programmes de partenariat
Committee code
96
Committee name en
RPP Internal Decision Cttee
Committee name fr
Cté de décision interne - PPR
Area of application code
403
Area of application group en
Environment
Area of application group fr
Environnement
Area of application en
Inland waters
Area of application fr
Eaux intérieures
Research subject code
4504
Research subject group en
Hydrology
Research subject group fr
Hydrologie
Research subject en
Groundwater
Research subject fr
Eaux souterraines
Partie
1
Nb partie
1
Application title
Large scale climate chamber simulations of permafrost environments
Keyword
NA
Application summary
The proposed research is a critical step in our long-term research program to provide new insight and quantification of the effects of climate change on the groundwater and surface water of Canada's subarctic regions. The overall long-term focus is on quantifying the hydrologic, geotechnical, and biogeochemical response of wetland-dominated discontinuous permafrost to atmospheric temperature and solar variations. Specifically, for this CRD project, large-scale experiments on peat samples from the central Mackenzie River basin will be coupled with on-going field studies to better elucidate active layer moisture transport processes. Central to the research is a Canadian Foundation for Innovation (CFI) funded climate chamber, at the University of Western Ontario Biotron facility, which can reproduce the Canadian subarctic solar and atmospheric environment and house soil monoliths up to 1.5 m in diameter and 4 m in height. No other similar facility exists in Canada, U.S., or perhaps the world. Undisturbed peat cores 60 cm in diameter and ~ 75 cm deep, inclusive of vegetation, were taken in August 2007 at our field site near Fort Simpson NWT. Once the chamber and soil monolith operational parameters have been verified to field conditions, a key component of this CRD project, a wide range of climate forcing experiments (varying solar energy, air temperatures, precipitation, CO2) will be performed. Of particular interest is to quantify the moisture dynamics at the active-layer / permafrost transition zone and develop numerical models for estimating the position of this interface and the water table during seasonal ground thawing. These dynamics need to be understood in order to estimate the volume and timing of runoff from wetland-dominated basins in discontinuous permafrost zones. The experiments will answer critical questions, not addressable by field data alone, on how Canada's subarctic ecosystems will respond to climate change. Furthermore, validating the climate chamber as a tool to study cold region ecohydrological processes will allow the facility and BioChambers Inc. to be recognized nationally / internationally and stimulate further research and development.