Experimental hydrological forcing to illustrate water flow processes of a subarctic ladder fen peatland
Abstract Large peatland complexes dominate the landscape of the James Bay Lowland in subarctic Ontario, Canada. However, there is not a thorough understanding of the hydrological processes occurring in these important systems, particularly how ladder fens connect large domed bogs to the aquatic ecos...
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crwiley:10.1002/hyp.11127 2024-06-23T07:57:02+00:00 Experimental hydrological forcing to illustrate water flow processes of a subarctic ladder fen peatland McCarter, Colin P. R. Price, Jonathan S. 2017 http://dx.doi.org/10.1002/hyp.11127 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fhyp.11127 https://onlinelibrary.wiley.com/doi/pdf/10.1002/hyp.11127 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Hydrological Processes volume 31, issue 8, page 1578-1589 ISSN 0885-6087 1099-1085 journal-article 2017 crwiley https://doi.org/10.1002/hyp.11127 2024-06-06T04:22:39Z Abstract Large peatland complexes dominate the landscape of the James Bay Lowland in subarctic Ontario, Canada. However, there is not a thorough understanding of the hydrological processes occurring in these important systems, particularly how ladder fens connect large domed bogs to the aquatic ecosystems that drain the peatland complex. Ladder fens consist of a pool‐rib topography where flow downgradient is controlled by the peat ribs. Within the ribs, low‐lying preferential flow paths typically enhance the transmission of water, whereas the elevated ridge microforms impede water flow to downgradient aquatic ecosystems. To assess the hydrological connectivity, we study the role of the water table, peat transmissivity, and microtopography of a small ladder fen for 3 summers (2013–2015) in the James Bay Lowland. The system was manipulated with a sustained hydrological forcing (water addition) to the upslope boundary of the fen during 2014 (38 m 3 /day) and 2015 (30 m 3 /day). There was an exponential increase in transmissivity towards the peat surface due to extremely high‐hydraulic conductivities within the upper few centimeters of the peat deposit. At the maximum water table, the saturated hydraulic conductivity of the 0.1 m layer of peat below the water table varied depending on peat microtopography (preferential flow paths = 42–598 m/day and ridges = 16–52 m/day), resulting in high‐hydrological connectivity periods. Furthermore, during 2015, there was an abnormally large amount of precipitation (300 mm vs. long‐term average ~ 100 mm) that resulted in complete surface water connectivity of the site. This caused rapid movement of water from the head of system to the outlet (~15 hr) and runoff ratios >1, compared to low‐water table periods (runoff ratio ~ 0.05). This study highlights the profound importance of the transmissivity–water table feedback mechanism in ladder fens, on controlling the water retention and drainage of large peatland complexes. Article in Journal/Newspaper Subarctic James Bay Wiley Online Library Canada The Ribs ENVELOPE(-55.781,-55.781,52.750,52.750) Hydrological Processes 31 8 1578 1589 |
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Open Polar |
collection |
Wiley Online Library |
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crwiley |
language |
English |
description |
Abstract Large peatland complexes dominate the landscape of the James Bay Lowland in subarctic Ontario, Canada. However, there is not a thorough understanding of the hydrological processes occurring in these important systems, particularly how ladder fens connect large domed bogs to the aquatic ecosystems that drain the peatland complex. Ladder fens consist of a pool‐rib topography where flow downgradient is controlled by the peat ribs. Within the ribs, low‐lying preferential flow paths typically enhance the transmission of water, whereas the elevated ridge microforms impede water flow to downgradient aquatic ecosystems. To assess the hydrological connectivity, we study the role of the water table, peat transmissivity, and microtopography of a small ladder fen for 3 summers (2013–2015) in the James Bay Lowland. The system was manipulated with a sustained hydrological forcing (water addition) to the upslope boundary of the fen during 2014 (38 m 3 /day) and 2015 (30 m 3 /day). There was an exponential increase in transmissivity towards the peat surface due to extremely high‐hydraulic conductivities within the upper few centimeters of the peat deposit. At the maximum water table, the saturated hydraulic conductivity of the 0.1 m layer of peat below the water table varied depending on peat microtopography (preferential flow paths = 42–598 m/day and ridges = 16–52 m/day), resulting in high‐hydrological connectivity periods. Furthermore, during 2015, there was an abnormally large amount of precipitation (300 mm vs. long‐term average ~ 100 mm) that resulted in complete surface water connectivity of the site. This caused rapid movement of water from the head of system to the outlet (~15 hr) and runoff ratios >1, compared to low‐water table periods (runoff ratio ~ 0.05). This study highlights the profound importance of the transmissivity–water table feedback mechanism in ladder fens, on controlling the water retention and drainage of large peatland complexes. |
format |
Article in Journal/Newspaper |
author |
McCarter, Colin P. R. Price, Jonathan S. |
spellingShingle |
McCarter, Colin P. R. Price, Jonathan S. Experimental hydrological forcing to illustrate water flow processes of a subarctic ladder fen peatland |
author_facet |
McCarter, Colin P. R. Price, Jonathan S. |
author_sort |
McCarter, Colin P. R. |
title |
Experimental hydrological forcing to illustrate water flow processes of a subarctic ladder fen peatland |
title_short |
Experimental hydrological forcing to illustrate water flow processes of a subarctic ladder fen peatland |
title_full |
Experimental hydrological forcing to illustrate water flow processes of a subarctic ladder fen peatland |
title_fullStr |
Experimental hydrological forcing to illustrate water flow processes of a subarctic ladder fen peatland |
title_full_unstemmed |
Experimental hydrological forcing to illustrate water flow processes of a subarctic ladder fen peatland |
title_sort |
experimental hydrological forcing to illustrate water flow processes of a subarctic ladder fen peatland |
publisher |
Wiley |
publishDate |
2017 |
url |
http://dx.doi.org/10.1002/hyp.11127 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fhyp.11127 https://onlinelibrary.wiley.com/doi/pdf/10.1002/hyp.11127 |
long_lat |
ENVELOPE(-55.781,-55.781,52.750,52.750) |
geographic |
Canada The Ribs |
geographic_facet |
Canada The Ribs |
genre |
Subarctic James Bay |
genre_facet |
Subarctic James Bay |
op_source |
Hydrological Processes volume 31, issue 8, page 1578-1589 ISSN 0885-6087 1099-1085 |
op_rights |
http://onlinelibrary.wiley.com/termsAndConditions#vor |
op_doi |
https://doi.org/10.1002/hyp.11127 |
container_title |
Hydrological Processes |
container_volume |
31 |
container_issue |
8 |
container_start_page |
1578 |
op_container_end_page |
1589 |
_version_ |
1802650468077273088 |