|Title||Wetland surface and groundwater interactions monitoring program|
|Download||Download (whole publication) |
|Licence||Please note the adoption of the Open Government Licence - Canada
supersedes any previous licences.|
|Author||Strakowski, J; Renic, T; Clark, J|
|Source||Regional-scale groundwater geoscience in southern Ontario: an Ontario Geological Survey, Geological Survey of Canada, and Conservation Ontario open house; by Russell, H A J; Ford, D; Priebe, E H; Geological Survey of Canada, Open File 8212, 2017 p. 34,
https://doi.org/10.4095/299801 Open Access|
|Publisher||Natural Resources Canada|
|Meeting||Ontario Geological Survey and Geological Survey of Canada groundwater geoscience open house; Guelph; CA; March 1-2, 2017|
|Related||This publication is contained in Regional-scale groundwater
geoscience in southern Ontario: an Ontario Geological Survey, Geological Survey of Canada, and Conservation Ontario open house |
|NTS||30M/04; 30M/05; 30M/12; 40P/08; 40P/09|
|Area||Halton; Burlington; Oakville; Milton; Hamilton|
|Lat/Long WENS|| -80.2500 -79.5000 43.7500 43.1667|
|Subjects||hydrogeology; wetlands; surface waters; groundwater; aquifers; resource management; regional planning; watersheds; hydrologic environment; hydraulic gradients; hydrologic budget; modelling; groundwater
levels; pressure; temperature; precipitation; Conservation Halton Watershed; monitoring|
|Program||Groundwater Geoscience Aquifer Assessment & support to mapping|
|Released||2017 02 22|
|Abstract||Wetlands are important elements of the natural environment. More than 63 km2 of the Conservation Halton watershed is covered with wetlands, 94% of which lie above the Niagara Escarpment, an area which
is headwaters to major Conservation Halton creeks. Wetlands have various functions and properties and their understanding draws on multiple disciplines from terrestrial and aquatic ecology, chemistry, hydrology to engineering. From a hydrological
point of view, wetlands can store water, lose water through evapotranspiration, recharge underlying aquifers, or collect groundwater discharge and convey it to local streams and rivers. Based on local topographical settings, geology, groundwater
levels, climatic conditions the wetland hydrological conditions may differ. To understand the wetland hydrological functions, its hydroperiod and vertical hydraulic gradient need to be understood.|
In the fall of 2012 Conservation Halton, in
collaboration with the Regional Municipality of Halton, initiated a wetland monitoring project to address a lack of data identified during the development and calibration of an integrated surface and groundwater GSFLOW numerical model for drinking
water source protection water budget studies in the Halton-Hamilton Source Protection Region. Specifically, the wetland monitoring program was designed to enhance the understanding of surface and groundwater interactions, their timing and fluxes.
Five wetlands within Conservation Halton watershed were selected and instrumented. Wetlands 1 through 4 are located above the Niagara Escarpment and Wetland 5 is located below it. Wetland 1 is located in the Mountsberg Conservation Area, Wetland 2
just north of 5th Concession Road and west of Highway 6 in Hamilton, Wetland 3 in Crawford Lake Conservation Area, Wetland 4 in Hilton Falls Conservation Area, and Wetland 5 on private lands in North Oakville west of Sixth Line. Wetland 1 is
classified as a swamp, Wetlands 2 and 5 are marshes, and Wetlands 3 and 4 are vernal pools.
Each wetland was instrumented with two drive point piezometers completed at different depths in close proximity. The shallow piezometers are completed at a
maximum depth of 0.1 metres and effectively measure the wetlands' hydroperiod. The deep drive point piezometers were completed at depths between 0.4 and 1.5 meters to monitor shallow groundwater levels underneath wetlands. Each drivepoint piezometer
was instrumented with an electronic datalogger measuring absolute pressure and temperature and collecting data at 10 minute or 1 hour intervals. To obtain accurate water height above sensor, the absolute pressure data were then corrected for
barometric pressure changes using atmospheric pressure data.
The results show that the wetlands above the Niagara Escarpment are very dynamic and depending on the wetland type and local conditions, they behave differently during precipitation
events. The instrumented wetland below the Escarpment is not as dynamic and mostly depends on surface water. In 2015 and 2016 three additional wetlands were added to the network in collaboration with Conservation Halton staff. Together with our
neighboring conservation authorities, who have similar monitoring programs, having more instrumented wetlands will allow to develop relationships between wetland type, hydrology and occupying species. Collected data are an invaluable dataset to
replicate natural processes in numerical modeling and a critical tool in local decision making, wetland management and watershed planning.
|Summary||(Plain Language Summary, not published)|
Proceedings for Regional-Scale Groundwater Geoscience in Southern Ontario open house organized by the Ontario Geological Survey, Geological Survey of
Canada and Conservation Ontario Geoscientists. Open house is on 2017-03-01 and 02. Purpose is public engagement and dissemination of geoscience completed in Southern Ontario during the past year.