A method for imaging water transport in soil–snow systems with neutron radiography

Abstract Liquid water at the ground–snow interface is thought to play a crucial role in the release of glide-snow avalanches, which can be massive and threaten infrastructure in alpine regions. Several mechanisms have been postulated to explain the formation of this interfacial water. However, these...

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Published in:Annals of Glaciology
Main Authors: Lombardo, Michael, Lehmann, Peter, Kaestner, Anders, Fees, Amelie, Van Herwijnen, Alec, Schweizer, Jürg
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 2023
Subjects:
Online Access:http://dx.doi.org/10.1017/aog.2023.65
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0260305523000654
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spelling crcambridgeupr:10.1017/aog.2023.65 2024-06-09T07:38:26+00:00 A method for imaging water transport in soil–snow systems with neutron radiography Lombardo, Michael Lehmann, Peter Kaestner, Anders Fees, Amelie Van Herwijnen, Alec Schweizer, Jürg 2023 http://dx.doi.org/10.1017/aog.2023.65 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0260305523000654 en eng Cambridge University Press (CUP) http://creativecommons.org/licenses/by/4.0/ Annals of Glaciology page 1-10 ISSN 0260-3055 1727-5644 journal-article 2023 crcambridgeupr https://doi.org/10.1017/aog.2023.65 2024-05-15T13:09:21Z Abstract Liquid water at the ground–snow interface is thought to play a crucial role in the release of glide-snow avalanches, which can be massive and threaten infrastructure in alpine regions. Several mechanisms have been postulated to explain the formation of this interfacial water. However, these mechanisms remain poorly understood, in part because suitable measurement techniques are lacking. Here, we demonstrate the use of neutron radiography for imaging water transport in soil–snow systems. Columns of sand, gravel and snow were used to simulate the capillary forces of the soil–vegetation–snow layering found in nature. The columns were connected to a water reservoir to maintain a constant-pressure boundary condition and placed in a climatic chamber within the neutron beam. We show that neutron radiography is capable of measuring changes in the optical density distribution (related to liquid water content) within all three layers of the model system. Results suggest that a porous interface between the sand and snow may induce the formation of a water layer in the basal snowpack. Improved understanding of the water transport in soil–snow systems should lead to better prediction of glide-snow avalanche release and could also benefit other fields such as snow hydrology. Article in Journal/Newspaper Annals of Glaciology Cambridge University Press Annals of Glaciology 1 10
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
description Abstract Liquid water at the ground–snow interface is thought to play a crucial role in the release of glide-snow avalanches, which can be massive and threaten infrastructure in alpine regions. Several mechanisms have been postulated to explain the formation of this interfacial water. However, these mechanisms remain poorly understood, in part because suitable measurement techniques are lacking. Here, we demonstrate the use of neutron radiography for imaging water transport in soil–snow systems. Columns of sand, gravel and snow were used to simulate the capillary forces of the soil–vegetation–snow layering found in nature. The columns were connected to a water reservoir to maintain a constant-pressure boundary condition and placed in a climatic chamber within the neutron beam. We show that neutron radiography is capable of measuring changes in the optical density distribution (related to liquid water content) within all three layers of the model system. Results suggest that a porous interface between the sand and snow may induce the formation of a water layer in the basal snowpack. Improved understanding of the water transport in soil–snow systems should lead to better prediction of glide-snow avalanche release and could also benefit other fields such as snow hydrology.
format Article in Journal/Newspaper
author Lombardo, Michael
Lehmann, Peter
Kaestner, Anders
Fees, Amelie
Van Herwijnen, Alec
Schweizer, Jürg
spellingShingle Lombardo, Michael
Lehmann, Peter
Kaestner, Anders
Fees, Amelie
Van Herwijnen, Alec
Schweizer, Jürg
A method for imaging water transport in soil–snow systems with neutron radiography
author_facet Lombardo, Michael
Lehmann, Peter
Kaestner, Anders
Fees, Amelie
Van Herwijnen, Alec
Schweizer, Jürg
author_sort Lombardo, Michael
title A method for imaging water transport in soil–snow systems with neutron radiography
title_short A method for imaging water transport in soil–snow systems with neutron radiography
title_full A method for imaging water transport in soil–snow systems with neutron radiography
title_fullStr A method for imaging water transport in soil–snow systems with neutron radiography
title_full_unstemmed A method for imaging water transport in soil–snow systems with neutron radiography
title_sort method for imaging water transport in soil–snow systems with neutron radiography
publisher Cambridge University Press (CUP)
publishDate 2023
url http://dx.doi.org/10.1017/aog.2023.65
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0260305523000654
genre Annals of Glaciology
genre_facet Annals of Glaciology
op_source Annals of Glaciology
page 1-10
ISSN 0260-3055 1727-5644
op_rights http://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.1017/aog.2023.65
container_title Annals of Glaciology
container_start_page 1
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