Channel geomorphology differences between stream reaches with grass- or tree-dominated riparian vegetation in southern Manitoba

Removal of trees for pasture or crop production is common along the stream reaches in the Canadian Prairies, resulting in a patchwork of forested and nonforest riparian vegetation along most streams. The effect of vegetation type on channel geomorphology and potential to influence sediment dynamics...

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Main Authors: Sanjayan Satchithanantham, Henry F. Wilson, Patsy Michiels, Melanie Dubois, Sheng Li, Alexander J. Koiter
Format: Article
Language:English
Published: Canadian Science Publishing 2019-07-01
Series:FACETS
Subjects:
Online Access:https://www.facetsjournal.com/doi/10.1139/facets-2018-0036
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spelling doaj-1b703314f6cd4de5b83097cb54244f7f2020-11-25T02:01:47ZengCanadian Science PublishingFACETS2371-16712371-16712019-07-014133634910.1139/facets-2018-0036Channel geomorphology differences between stream reaches with grass- or tree-dominated riparian vegetation in southern ManitobaSanjayan Satchithanantham0Henry F. Wilson1Patsy Michiels 2Melanie Dubois3Sheng Li4Alexander J. Koiter5Brandon Research and Development Centre, Agriculture and Agri-Food Canada, Brandon, MB R7A 5Y3, CanadaBrandon Research and Development Centre, Agriculture and Agri-Food Canada, Brandon, MB R7A 5Y3, CanadaBrandon Research and Development Centre, Agriculture and Agri-Food Canada, Brandon, MB R7A 5Y3, CanadaBrandon Research and Development Centre, Agriculture and Agri-Food Canada, Brandon, MB R7A 5Y3, CanadaFredericton Research and Development Centre, Agriculture and Agri-Food Canada, Fredericton, NB E3B 4Z7, CanadaDepartment of Geography, Brandon University, Brandon, MB R7A 6A9, CanadaRemoval of trees for pasture or crop production is common along the stream reaches in the Canadian Prairies, resulting in a patchwork of forested and nonforest riparian vegetation along most streams. The effect of vegetation type on channel geomorphology and potential to influence sediment dynamics was studied using eight paired reaches (forested and nonforest) within agricultural watersheds in southern Manitoba, Canada. High potential for bank erosion was observed at all sites (bank erosion hazard index scores), but Pfankuch channel stability scores were significantly higher for forested reaches compared with nonforested reaches. Furthermore, forested reaches had higher width to depth ratios, but flood-prone widths did not differ significantly, resulting in lower entrenchment ratios. Reduced channel width and cross-sectional area in nonforested reaches created an overall reduction of in-stream habitat, increased velocity, and increased potential for exceedance of channel capacity and floodplain access during high-flow events. Channel widening in response to riparian afforestation efforts has been observed in a variety of other locations globally and the results of this study suggest that widening with afforestation can still be anticipated in this region where stream gradients are low, hydrology is dominated by snowmelt, and forest cover is minimal.https://www.facetsjournal.com/doi/10.1139/facets-2018-0036riparian vegetationstream channel geomorphologyPrairie streamschannel stability
collection DOAJ
language English
format Article
sources DOAJ
author Sanjayan Satchithanantham
Henry F. Wilson
Patsy Michiels
Melanie Dubois
Sheng Li
Alexander J. Koiter
spellingShingle Sanjayan Satchithanantham
Henry F. Wilson
Patsy Michiels
Melanie Dubois
Sheng Li
Alexander J. Koiter
Channel geomorphology differences between stream reaches with grass- or tree-dominated riparian vegetation in southern Manitoba
FACETS
riparian vegetation
stream channel geomorphology
Prairie streams
channel stability
author_facet Sanjayan Satchithanantham
Henry F. Wilson
Patsy Michiels
Melanie Dubois
Sheng Li
Alexander J. Koiter
author_sort Sanjayan Satchithanantham
title Channel geomorphology differences between stream reaches with grass- or tree-dominated riparian vegetation in southern Manitoba
title_short Channel geomorphology differences between stream reaches with grass- or tree-dominated riparian vegetation in southern Manitoba
title_full Channel geomorphology differences between stream reaches with grass- or tree-dominated riparian vegetation in southern Manitoba
title_fullStr Channel geomorphology differences between stream reaches with grass- or tree-dominated riparian vegetation in southern Manitoba
title_full_unstemmed Channel geomorphology differences between stream reaches with grass- or tree-dominated riparian vegetation in southern Manitoba
title_sort channel geomorphology differences between stream reaches with grass- or tree-dominated riparian vegetation in southern manitoba
publisher Canadian Science Publishing
series FACETS
issn 2371-1671
2371-1671
publishDate 2019-07-01
description Removal of trees for pasture or crop production is common along the stream reaches in the Canadian Prairies, resulting in a patchwork of forested and nonforest riparian vegetation along most streams. The effect of vegetation type on channel geomorphology and potential to influence sediment dynamics was studied using eight paired reaches (forested and nonforest) within agricultural watersheds in southern Manitoba, Canada. High potential for bank erosion was observed at all sites (bank erosion hazard index scores), but Pfankuch channel stability scores were significantly higher for forested reaches compared with nonforested reaches. Furthermore, forested reaches had higher width to depth ratios, but flood-prone widths did not differ significantly, resulting in lower entrenchment ratios. Reduced channel width and cross-sectional area in nonforested reaches created an overall reduction of in-stream habitat, increased velocity, and increased potential for exceedance of channel capacity and floodplain access during high-flow events. Channel widening in response to riparian afforestation efforts has been observed in a variety of other locations globally and the results of this study suggest that widening with afforestation can still be anticipated in this region where stream gradients are low, hydrology is dominated by snowmelt, and forest cover is minimal.
topic riparian vegetation
stream channel geomorphology
Prairie streams
channel stability
url https://www.facetsjournal.com/doi/10.1139/facets-2018-0036
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