Groundwater storage – streamflow relations during winter in a subarctic wetland, Saskatchewan
Wetland drainage systems are shown to be hydrologically active during winter. Water storage in various terrain types changed over the winter as a result of intrabasin transfers between terrain types, primarily from outlying mineral terrains to centrally located groundwater controlled wetlands, and d...
Published in: | Canadian Journal of Earth Sciences |
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Language: | English |
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Canadian Science Publishing
1987
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Online Access: | http://dx.doi.org/10.1139/e87-196 http://www.nrcresearchpress.com/doi/pdf/10.1139/e87-196 |
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crcansciencepubl:10.1139/e87-196 2024-05-12T08:11:43+00:00 Groundwater storage – streamflow relations during winter in a subarctic wetland, Saskatchewan Price, Jonathan S. Fitzgibbon, John E. 1987 http://dx.doi.org/10.1139/e87-196 http://www.nrcresearchpress.com/doi/pdf/10.1139/e87-196 en eng Canadian Science Publishing http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining Canadian Journal of Earth Sciences volume 24, issue 10, page 2074-2081 ISSN 0008-4077 1480-3313 General Earth and Planetary Sciences journal-article 1987 crcansciencepubl https://doi.org/10.1139/e87-196 2024-04-18T06:54:51Z Wetland drainage systems are shown to be hydrologically active during winter. Water storage in various terrain types changed over the winter as a result of intrabasin transfers between terrain types, primarily from outlying mineral terrains to centrally located groundwater controlled wetlands, and due to winter streamflow. Mineral terrain and bog lost 97 and 25 mm of water, respectively, whereas fens gained 28–51 mm. A water balance indicated that mineral terrain yielded almost twice as much water as was released as streamflow, and that much of this excess was being stored in the fens where groundwater seepage at the surface resulted in icings. Bogs had little ability to sustain winter streamflow. Diminishing streamflow in early winter coincided with freezing of the surface layers of peat, which normally transmit most of the water. However, streamflow was maintained throughout winter by water transmitted through the fens. Article in Journal/Newspaper Subarctic Canadian Science Publishing Canadian Journal of Earth Sciences 24 10 2074 2081 |
institution |
Open Polar |
collection |
Canadian Science Publishing |
op_collection_id |
crcansciencepubl |
language |
English |
topic |
General Earth and Planetary Sciences |
spellingShingle |
General Earth and Planetary Sciences Price, Jonathan S. Fitzgibbon, John E. Groundwater storage – streamflow relations during winter in a subarctic wetland, Saskatchewan |
topic_facet |
General Earth and Planetary Sciences |
description |
Wetland drainage systems are shown to be hydrologically active during winter. Water storage in various terrain types changed over the winter as a result of intrabasin transfers between terrain types, primarily from outlying mineral terrains to centrally located groundwater controlled wetlands, and due to winter streamflow. Mineral terrain and bog lost 97 and 25 mm of water, respectively, whereas fens gained 28–51 mm. A water balance indicated that mineral terrain yielded almost twice as much water as was released as streamflow, and that much of this excess was being stored in the fens where groundwater seepage at the surface resulted in icings. Bogs had little ability to sustain winter streamflow. Diminishing streamflow in early winter coincided with freezing of the surface layers of peat, which normally transmit most of the water. However, streamflow was maintained throughout winter by water transmitted through the fens. |
format |
Article in Journal/Newspaper |
author |
Price, Jonathan S. Fitzgibbon, John E. |
author_facet |
Price, Jonathan S. Fitzgibbon, John E. |
author_sort |
Price, Jonathan S. |
title |
Groundwater storage – streamflow relations during winter in a subarctic wetland, Saskatchewan |
title_short |
Groundwater storage – streamflow relations during winter in a subarctic wetland, Saskatchewan |
title_full |
Groundwater storage – streamflow relations during winter in a subarctic wetland, Saskatchewan |
title_fullStr |
Groundwater storage – streamflow relations during winter in a subarctic wetland, Saskatchewan |
title_full_unstemmed |
Groundwater storage – streamflow relations during winter in a subarctic wetland, Saskatchewan |
title_sort |
groundwater storage – streamflow relations during winter in a subarctic wetland, saskatchewan |
publisher |
Canadian Science Publishing |
publishDate |
1987 |
url |
http://dx.doi.org/10.1139/e87-196 http://www.nrcresearchpress.com/doi/pdf/10.1139/e87-196 |
genre |
Subarctic |
genre_facet |
Subarctic |
op_source |
Canadian Journal of Earth Sciences volume 24, issue 10, page 2074-2081 ISSN 0008-4077 1480-3313 |
op_rights |
http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining |
op_doi |
https://doi.org/10.1139/e87-196 |
container_title |
Canadian Journal of Earth Sciences |
container_volume |
24 |
container_issue |
10 |
container_start_page |
2074 |
op_container_end_page |
2081 |
_version_ |
1798833913237340160 |