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Groundwater-driven wetland-stream connectivity in the Prairie Pothole Region : Inferences based on electrical conductivity data / Genevieve Ali, Aminul Haque, Nandita Basu, Pascal Badiou, and Henry Wilson.

By: Contributor(s): Material type: TextTextSeries: Wetlands. 37: 773-785 Publication details: 2017.Description: colour illustrations ; 28 cmLOC classification:
  • ALI
Online resources: Summary: This study examined the potential for electrical conductivity (EC) to serve as an indicator of groundwater- driven wetland-stream connectivity in the Prairie Pothole Region. Focus was on the Broughton ’ s Creek Watershed (Manitoba, Canada) where thirteen wetlands and a creek were monitored in 2013 – 2014. A connectivity index (CI), comput- ed by incorporating EC data in a hyperbolic solute export model, identified a potential for both shallow and deep groundwater-driven wetland-stream connectivity to occur, al- though shallower connections were rarer. Both raw EC and CI values were strongly correlated to wetland volume capacity, indicating the importance of storage and flow generation processes for wetland-stream connectivity potential. The proposed CI was instrumental in reaching that conclusion, making it a simple yet physically-based metric of wetland behavior that should be tested in multiple environments to confirm or infirm its validity.
Holdings
Item type Current library Collection Call number Status Date due Barcode
Electronic Journal Electronic Journal IWWR Supported Research Non-fiction ALI (Browse shelf(Opens below)) Available 16934

Includes bibliographical references (pages 784-785).

This study examined the potential for electrical
conductivity (EC) to serve as an indicator of groundwater-
driven wetland-stream connectivity in the Prairie Pothole
Region. Focus was on the Broughton

s Creek Watershed
(Manitoba, Canada) where thirteen wetlands and a creek were
monitored in 2013

2014. A connectivity index (CI), comput-
ed by incorporating EC data in a hyperbolic solute export
model, identified a potential for both shallow and deep
groundwater-driven wetland-stream connectivity to occur, al-
though shallower connections were rarer. Both raw EC and CI
values were strongly correlated to wetland volume capacity,
indicating the importance of storage and flow generation
processes for wetland-stream connectivity potential. The
proposed CI was instrumental in reaching that conclusion,
making it a simple yet physically-based metric of wetland
behavior that should be tested in multiple environments to
confirm or infirm its validity.

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