Porosity dependence of elastic moduli of snow and firn

Measurements of elastic wave velocities enable non-destructive estimation of the mechanical properties, elastic moduli and density of snow and firn. The variation of elastic moduli with porosity in dry snow and firn is modeled using a differential effective medium scheme modified to account for the...

Full description

Bibliographic Details
Published in:Journal of Glaciology
Main Author: Colin M. Sayers
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press 2021
Subjects:
Online Access:https://doi.org/10.1017/jog.2021.25
https://doaj.org/article/a7cee77cd46b45feb6e2920553b9f86c
id ftdoajarticles:oai:doaj.org/article:a7cee77cd46b45feb6e2920553b9f86c
record_format openpolar
spelling ftdoajarticles:oai:doaj.org/article:a7cee77cd46b45feb6e2920553b9f86c 2023-05-15T16:57:33+02:00 Porosity dependence of elastic moduli of snow and firn Colin M. Sayers 2021-10-01T00:00:00Z https://doi.org/10.1017/jog.2021.25 https://doaj.org/article/a7cee77cd46b45feb6e2920553b9f86c EN eng Cambridge University Press https://www.cambridge.org/core/product/identifier/S0022143021000253/type/journal_article https://doaj.org/toc/0022-1430 https://doaj.org/toc/1727-5652 doi:10.1017/jog.2021.25 0022-1430 1727-5652 https://doaj.org/article/a7cee77cd46b45feb6e2920553b9f86c Journal of Glaciology, Vol 67, Pp 788-796 (2021) Polar firn snow snow physics Environmental sciences GE1-350 Meteorology. Climatology QC851-999 article 2021 ftdoajarticles https://doi.org/10.1017/jog.2021.25 2023-03-12T01:30:57Z Measurements of elastic wave velocities enable non-destructive estimation of the mechanical properties, elastic moduli and density of snow and firn. The variation of elastic moduli with porosity in dry snow and firn is modeled using a differential effective medium scheme modified to account for the critical porosity above which the bulk and shear moduli of the ice frame vanish. A comparison of predicted and measured elastic moduli indicates that the shear modulus of ice in snow is lower than that computed from single crystal elastic stiffnesses of ice. This may indicate that the bonds between snow particles are more deformable under shear than under compression. A partial alignment of ice crystals also may contribute. Good agreement between elastic stiffnesses of the ice frame obtained from elastic wave velocity measurements and the predictions of the theory is observed. The approach is simple and compact, and does not require the use of empirical fits to the data. Owing to its simplicity, this model may prove useful in a variety of potential applications such as construction on snow, interpretation of seismic measurements to monitor and locate avalanches and estimation of density within compacting snow deposited on glaciers and ice sheets. Article in Journal/Newspaper Journal of Glaciology Directory of Open Access Journals: DOAJ Articles Journal of Glaciology 67 265 788 796
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Polar firn
snow
snow physics
Environmental sciences
GE1-350
Meteorology. Climatology
QC851-999
spellingShingle Polar firn
snow
snow physics
Environmental sciences
GE1-350
Meteorology. Climatology
QC851-999
Colin M. Sayers
Porosity dependence of elastic moduli of snow and firn
topic_facet Polar firn
snow
snow physics
Environmental sciences
GE1-350
Meteorology. Climatology
QC851-999
description Measurements of elastic wave velocities enable non-destructive estimation of the mechanical properties, elastic moduli and density of snow and firn. The variation of elastic moduli with porosity in dry snow and firn is modeled using a differential effective medium scheme modified to account for the critical porosity above which the bulk and shear moduli of the ice frame vanish. A comparison of predicted and measured elastic moduli indicates that the shear modulus of ice in snow is lower than that computed from single crystal elastic stiffnesses of ice. This may indicate that the bonds between snow particles are more deformable under shear than under compression. A partial alignment of ice crystals also may contribute. Good agreement between elastic stiffnesses of the ice frame obtained from elastic wave velocity measurements and the predictions of the theory is observed. The approach is simple and compact, and does not require the use of empirical fits to the data. Owing to its simplicity, this model may prove useful in a variety of potential applications such as construction on snow, interpretation of seismic measurements to monitor and locate avalanches and estimation of density within compacting snow deposited on glaciers and ice sheets.
format Article in Journal/Newspaper
author Colin M. Sayers
author_facet Colin M. Sayers
author_sort Colin M. Sayers
title Porosity dependence of elastic moduli of snow and firn
title_short Porosity dependence of elastic moduli of snow and firn
title_full Porosity dependence of elastic moduli of snow and firn
title_fullStr Porosity dependence of elastic moduli of snow and firn
title_full_unstemmed Porosity dependence of elastic moduli of snow and firn
title_sort porosity dependence of elastic moduli of snow and firn
publisher Cambridge University Press
publishDate 2021
url https://doi.org/10.1017/jog.2021.25
https://doaj.org/article/a7cee77cd46b45feb6e2920553b9f86c
genre Journal of Glaciology
genre_facet Journal of Glaciology
op_source Journal of Glaciology, Vol 67, Pp 788-796 (2021)
op_relation https://www.cambridge.org/core/product/identifier/S0022143021000253/type/journal_article
https://doaj.org/toc/0022-1430
https://doaj.org/toc/1727-5652
doi:10.1017/jog.2021.25
0022-1430
1727-5652
https://doaj.org/article/a7cee77cd46b45feb6e2920553b9f86c
op_doi https://doi.org/10.1017/jog.2021.25
container_title Journal of Glaciology
container_volume 67
container_issue 265
container_start_page 788
op_container_end_page 796
_version_ 1766049123063037952