Arctic soil patterns analogous to fluid instabilities

Slow-moving arctic soils commonly organize into striking large-scale spatial patterns called solifluction terraces and lobes. Although these features impact hillslope stability, carbon storage and release, and landscape response to climate change, no mechanistic explanation exists for their formatio...

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Published in:Proceedings of the National Academy of Sciences
Main Authors: Glade, Rachel C., Fratkin, Michael M., Pouragha, Mehdi, Seiphoori, Ali, Rowland, Joel C.
Language:unknown
Published: 2023
Subjects:
Online Access:http://www.osti.gov/servlets/purl/1835789
https://www.osti.gov/biblio/1835789
https://doi.org/10.1073/pnas.2101255118
id ftosti:oai:osti.gov:1835789
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spelling ftosti:oai:osti.gov:1835789 2023-07-30T04:01:04+02:00 Arctic soil patterns analogous to fluid instabilities Glade, Rachel C. Fratkin, Michael M. Pouragha, Mehdi Seiphoori, Ali Rowland, Joel C. 2023-02-23 application/pdf http://www.osti.gov/servlets/purl/1835789 https://www.osti.gov/biblio/1835789 https://doi.org/10.1073/pnas.2101255118 unknown http://www.osti.gov/servlets/purl/1835789 https://www.osti.gov/biblio/1835789 https://doi.org/10.1073/pnas.2101255118 doi:10.1073/pnas.2101255118 54 ENVIRONMENTAL SCIENCES 2023 ftosti https://doi.org/10.1073/pnas.2101255118 2023-07-11T10:09:00Z Slow-moving arctic soils commonly organize into striking large-scale spatial patterns called solifluction terraces and lobes. Although these features impact hillslope stability, carbon storage and release, and landscape response to climate change, no mechanistic explanation exists for their formation. Everyday fluids—such as paint dripping down walls—produce markedly similar fingering patterns resulting from competition between viscous and cohesive forces. Here we use a scaling analysis to show that soil cohesion and hydrostatic effects can lead to similar large-scale patterns in arctic soils. A large dataset of high-resolution solifluction lobe spacing and morphology across Norway supports theoretical predictions and indicates a newly observed climatic control on solifluction dynamics and patterns. Our findings provide a quantitative explanation of a common pattern on Earth and other planets, illuminating the importance of cohesive forces in landscape dynamics. These patterns operate at length and time scales previously unrecognized, with implications toward understanding fluid–solid dynamics in particulate systems with complex rheology. Other/Unknown Material Arctic Climate change SciTec Connect (Office of Scientific and Technical Information - OSTI, U.S. Department of Energy) Arctic Norway Proceedings of the National Academy of Sciences 118 21
institution Open Polar
collection SciTec Connect (Office of Scientific and Technical Information - OSTI, U.S. Department of Energy)
op_collection_id ftosti
language unknown
topic 54 ENVIRONMENTAL SCIENCES
spellingShingle 54 ENVIRONMENTAL SCIENCES
Glade, Rachel C.
Fratkin, Michael M.
Pouragha, Mehdi
Seiphoori, Ali
Rowland, Joel C.
Arctic soil patterns analogous to fluid instabilities
topic_facet 54 ENVIRONMENTAL SCIENCES
description Slow-moving arctic soils commonly organize into striking large-scale spatial patterns called solifluction terraces and lobes. Although these features impact hillslope stability, carbon storage and release, and landscape response to climate change, no mechanistic explanation exists for their formation. Everyday fluids—such as paint dripping down walls—produce markedly similar fingering patterns resulting from competition between viscous and cohesive forces. Here we use a scaling analysis to show that soil cohesion and hydrostatic effects can lead to similar large-scale patterns in arctic soils. A large dataset of high-resolution solifluction lobe spacing and morphology across Norway supports theoretical predictions and indicates a newly observed climatic control on solifluction dynamics and patterns. Our findings provide a quantitative explanation of a common pattern on Earth and other planets, illuminating the importance of cohesive forces in landscape dynamics. These patterns operate at length and time scales previously unrecognized, with implications toward understanding fluid–solid dynamics in particulate systems with complex rheology.
author Glade, Rachel C.
Fratkin, Michael M.
Pouragha, Mehdi
Seiphoori, Ali
Rowland, Joel C.
author_facet Glade, Rachel C.
Fratkin, Michael M.
Pouragha, Mehdi
Seiphoori, Ali
Rowland, Joel C.
author_sort Glade, Rachel C.
title Arctic soil patterns analogous to fluid instabilities
title_short Arctic soil patterns analogous to fluid instabilities
title_full Arctic soil patterns analogous to fluid instabilities
title_fullStr Arctic soil patterns analogous to fluid instabilities
title_full_unstemmed Arctic soil patterns analogous to fluid instabilities
title_sort arctic soil patterns analogous to fluid instabilities
publishDate 2023
url http://www.osti.gov/servlets/purl/1835789
https://www.osti.gov/biblio/1835789
https://doi.org/10.1073/pnas.2101255118
geographic Arctic
Norway
geographic_facet Arctic
Norway
genre Arctic
Climate change
genre_facet Arctic
Climate change
op_relation http://www.osti.gov/servlets/purl/1835789
https://www.osti.gov/biblio/1835789
https://doi.org/10.1073/pnas.2101255118
doi:10.1073/pnas.2101255118
op_doi https://doi.org/10.1073/pnas.2101255118
container_title Proceedings of the National Academy of Sciences
container_volume 118
container_issue 21
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