A Geospatial Approach to Display the Hydrological Impacts of Permafrost Disturbances on the Geochemistry of Streams, Lower Peel River and Western Mackenzie Basin, Northwestern Canada
Retrogressive thaw slumps are one of the most dynamic geomorphic features in ice-rich permafrost environments. These features impact aquatic environments by releasing previously frozen organic and inorganic sediments into nearby waterbodies. The objective of this study is to quantify the effect of t...
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Université d'Ottawa / University of Ottawa
2015
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Online Access: | http://hdl.handle.net/10393/32081 https://doi.org/10.20381/ruor-2779 |
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ftunivottawa:oai:ruor.uottawa.ca:10393/32081 2023-05-15T16:37:20+02:00 A Geospatial Approach to Display the Hydrological Impacts of Permafrost Disturbances on the Geochemistry of Streams, Lower Peel River and Western Mackenzie Basin, Northwestern Canada Paquette, Catherine Lacelle, Denis 2015 application/pdf http://hdl.handle.net/10393/32081 https://doi.org/10.20381/ruor-2779 en eng Université d'Ottawa / University of Ottawa http://hdl.handle.net/10393/32081 http://dx.doi.org/10.20381/ruor-2779 Hydrology Geochemistry Thermokarst Permafrost Thesis 2015 ftunivottawa https://doi.org/10.20381/ruor-2779 2021-01-04T17:10:43Z Retrogressive thaw slumps are one of the most dynamic geomorphic features in ice-rich permafrost environments. These features impact aquatic environments by releasing previously frozen organic and inorganic sediments into nearby waterbodies. The objective of this study is to quantify the effect of thaw slumps growth on the hydro-geochemical regime of streams in the Richardson Mountains–Peel Plateau region, northwestern Canada (Fig. 1), within a geospatial hydrological framework (sub-basin, watershed and sub-watershed units). The sub-basin level is determined as the most effective to represent the geochemical properties because of the higher number of sample points within each unit. Based on correlation values, the average surface area of slumps has the most impact on stream geochemistry (as opposed to the number of slumps). Larger single slumps (>5ha) contribute more to changes in geochemistry than clusters of smaller slumps. These slumps can alter the geochemistry of the water to such levels as to exceed limits for freshwater aquatic life. Thesis Ice Mackenzie Basin permafrost Thermokarst uO Research (University of Ottawa - uOttawa) Canada Peel River ENVELOPE(-135.005,-135.005,67.000,67.000) Richardson Mountains ENVELOPE(-136.171,-136.171,67.000,67.000) |
institution |
Open Polar |
collection |
uO Research (University of Ottawa - uOttawa) |
op_collection_id |
ftunivottawa |
language |
English |
topic |
Hydrology Geochemistry Thermokarst Permafrost |
spellingShingle |
Hydrology Geochemistry Thermokarst Permafrost Paquette, Catherine A Geospatial Approach to Display the Hydrological Impacts of Permafrost Disturbances on the Geochemistry of Streams, Lower Peel River and Western Mackenzie Basin, Northwestern Canada |
topic_facet |
Hydrology Geochemistry Thermokarst Permafrost |
description |
Retrogressive thaw slumps are one of the most dynamic geomorphic features in ice-rich permafrost environments. These features impact aquatic environments by releasing previously frozen organic and inorganic sediments into nearby waterbodies. The objective of this study is to quantify the effect of thaw slumps growth on the hydro-geochemical regime of streams in the Richardson Mountains–Peel Plateau region, northwestern Canada (Fig. 1), within a geospatial hydrological framework (sub-basin, watershed and sub-watershed units). The sub-basin level is determined as the most effective to represent the geochemical properties because of the higher number of sample points within each unit. Based on correlation values, the average surface area of slumps has the most impact on stream geochemistry (as opposed to the number of slumps). Larger single slumps (>5ha) contribute more to changes in geochemistry than clusters of smaller slumps. These slumps can alter the geochemistry of the water to such levels as to exceed limits for freshwater aquatic life. |
author2 |
Lacelle, Denis |
format |
Thesis |
author |
Paquette, Catherine |
author_facet |
Paquette, Catherine |
author_sort |
Paquette, Catherine |
title |
A Geospatial Approach to Display the Hydrological Impacts of Permafrost Disturbances on the Geochemistry of Streams, Lower Peel River and Western Mackenzie Basin, Northwestern Canada |
title_short |
A Geospatial Approach to Display the Hydrological Impacts of Permafrost Disturbances on the Geochemistry of Streams, Lower Peel River and Western Mackenzie Basin, Northwestern Canada |
title_full |
A Geospatial Approach to Display the Hydrological Impacts of Permafrost Disturbances on the Geochemistry of Streams, Lower Peel River and Western Mackenzie Basin, Northwestern Canada |
title_fullStr |
A Geospatial Approach to Display the Hydrological Impacts of Permafrost Disturbances on the Geochemistry of Streams, Lower Peel River and Western Mackenzie Basin, Northwestern Canada |
title_full_unstemmed |
A Geospatial Approach to Display the Hydrological Impacts of Permafrost Disturbances on the Geochemistry of Streams, Lower Peel River and Western Mackenzie Basin, Northwestern Canada |
title_sort |
geospatial approach to display the hydrological impacts of permafrost disturbances on the geochemistry of streams, lower peel river and western mackenzie basin, northwestern canada |
publisher |
Université d'Ottawa / University of Ottawa |
publishDate |
2015 |
url |
http://hdl.handle.net/10393/32081 https://doi.org/10.20381/ruor-2779 |
long_lat |
ENVELOPE(-135.005,-135.005,67.000,67.000) ENVELOPE(-136.171,-136.171,67.000,67.000) |
geographic |
Canada Peel River Richardson Mountains |
geographic_facet |
Canada Peel River Richardson Mountains |
genre |
Ice Mackenzie Basin permafrost Thermokarst |
genre_facet |
Ice Mackenzie Basin permafrost Thermokarst |
op_relation |
http://hdl.handle.net/10393/32081 http://dx.doi.org/10.20381/ruor-2779 |
op_doi |
https://doi.org/10.20381/ruor-2779 |
_version_ |
1766027623452901376 |