Subsurface flow measurements using passive flux meters in variably‐saturated cold‐regions landscapes
Abstract To date, passive flux meters have predominantly been applied in temperate environments for tracking the movement of contaminants in groundwater. This study applies these instruments to reduce uncertainty in (typically instantaneous) flux measurements made in a low‐gradient, wetland dominate...
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crwiley:10.1002/hyp.13900 2024-06-02T08:13:03+00:00 Subsurface flow measurements using passive flux meters in variably‐saturated cold‐regions landscapes Devoie, Élise G. Connon, Ryan F. Craig, James R. Quinton, William L. ArcticNet Polar Knowledge Canada 2020 http://dx.doi.org/10.1002/hyp.13900 https://onlinelibrary.wiley.com/doi/pdf/10.1002/hyp.13900 https://onlinelibrary.wiley.com/doi/full-xml/10.1002/hyp.13900 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Hydrological Processes volume 34, issue 23, page 4541-4546 ISSN 0885-6087 1099-1085 journal-article 2020 crwiley https://doi.org/10.1002/hyp.13900 2024-05-03T11:55:41Z Abstract To date, passive flux meters have predominantly been applied in temperate environments for tracking the movement of contaminants in groundwater. This study applies these instruments to reduce uncertainty in (typically instantaneous) flux measurements made in a low‐gradient, wetland dominated, discontinuous permafrost environment. This method supports improved estimation of unsaturated and over‐winter subsurface flows which are very difficult to quantify using hydraulic gradient‐based approaches. Improved subsurface flow estimates can play a key role in understanding the water budget of this landscape. Article in Journal/Newspaper permafrost Wiley Online Library Hydrological Processes 34 23 4541 4546 |
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Wiley Online Library |
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English |
description |
Abstract To date, passive flux meters have predominantly been applied in temperate environments for tracking the movement of contaminants in groundwater. This study applies these instruments to reduce uncertainty in (typically instantaneous) flux measurements made in a low‐gradient, wetland dominated, discontinuous permafrost environment. This method supports improved estimation of unsaturated and over‐winter subsurface flows which are very difficult to quantify using hydraulic gradient‐based approaches. Improved subsurface flow estimates can play a key role in understanding the water budget of this landscape. |
author2 |
ArcticNet Polar Knowledge Canada |
format |
Article in Journal/Newspaper |
author |
Devoie, Élise G. Connon, Ryan F. Craig, James R. Quinton, William L. |
spellingShingle |
Devoie, Élise G. Connon, Ryan F. Craig, James R. Quinton, William L. Subsurface flow measurements using passive flux meters in variably‐saturated cold‐regions landscapes |
author_facet |
Devoie, Élise G. Connon, Ryan F. Craig, James R. Quinton, William L. |
author_sort |
Devoie, Élise G. |
title |
Subsurface flow measurements using passive flux meters in variably‐saturated cold‐regions landscapes |
title_short |
Subsurface flow measurements using passive flux meters in variably‐saturated cold‐regions landscapes |
title_full |
Subsurface flow measurements using passive flux meters in variably‐saturated cold‐regions landscapes |
title_fullStr |
Subsurface flow measurements using passive flux meters in variably‐saturated cold‐regions landscapes |
title_full_unstemmed |
Subsurface flow measurements using passive flux meters in variably‐saturated cold‐regions landscapes |
title_sort |
subsurface flow measurements using passive flux meters in variably‐saturated cold‐regions landscapes |
publisher |
Wiley |
publishDate |
2020 |
url |
http://dx.doi.org/10.1002/hyp.13900 https://onlinelibrary.wiley.com/doi/pdf/10.1002/hyp.13900 https://onlinelibrary.wiley.com/doi/full-xml/10.1002/hyp.13900 |
genre |
permafrost |
genre_facet |
permafrost |
op_source |
Hydrological Processes volume 34, issue 23, page 4541-4546 ISSN 0885-6087 1099-1085 |
op_rights |
http://onlinelibrary.wiley.com/termsAndConditions#vor |
op_doi |
https://doi.org/10.1002/hyp.13900 |
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Hydrological Processes |
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34 |
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23 |
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4541 |
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4546 |
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1800759699109314560 |