The impact of ice sheet geometry on meltwater ingress and reactive solute transport in sedimentary basins

We investigate the effect of ice sheet geometry on groundwater flow patterns and meltwater ingress in a hypothetical sedimentary basin. The simulation results indicate that meltwater ingress is much greater in 3D domains with a relatively narrow ice sheet extent compared to a wide ice sheet, or a si...

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Main Authors: Su, Danyang, Xie, Mingliang, Mayer, K. Ulrich, MacQuarrie, Kerry
Format: Other/Unknown Material
Language:unknown
Published: Zenodo 2022
Subjects:
Online Access:https://doi.org/10.5281/zenodo.7047093
id ftzenodo:oai:zenodo.org:7047093
record_format openpolar
spelling ftzenodo:oai:zenodo.org:7047093 2024-09-15T18:12:06+00:00 The impact of ice sheet geometry on meltwater ingress and reactive solute transport in sedimentary basins Su, Danyang Xie, Mingliang Mayer, K. Ulrich MacQuarrie, Kerry 2022-10-21 https://doi.org/10.5281/zenodo.7047093 unknown Zenodo https://eilinator.eos.ubc.ca:8443/index.php/s/5t8bXDnvfUAlPRF https://www.min3p.com/contact-us https://doi.org/10.5061/dryad.rjdfn2zfb https://zenodo.org/communities/dryad https://doi.org/10.5281/zenodo.7047092 https://doi.org/10.5281/zenodo.7047093 oai:zenodo.org:7047093 info:eu-repo/semantics/openAccess MIT License https://opensource.org/licenses/MIT ice sheet geometry meltwater ingress reactive transport sedimentary basin MIN3P-THCm info:eu-repo/semantics/other 2022 ftzenodo https://doi.org/10.5281/zenodo.704709310.5061/dryad.rjdfn2zfb10.5281/zenodo.7047092 2024-07-25T17:44:01Z We investigate the effect of ice sheet geometry on groundwater flow patterns and meltwater ingress in a hypothetical sedimentary basin. The simulation results indicate that meltwater ingress is much greater in 3D domains with a relatively narrow ice sheet extent compared to a wide ice sheet, or a simplified 2D model. In high permeability units (HPUs), the simulated meltwater penetration depth can reach up to 750 m in 3D domains compared to 400 m in a comparable 2D domain. In low permeability units (LPUs), very limited meltwater penetration occurs, indicating that ice sheet geometry and model dimensionality do not substantially affect water flow in these units. A conservative tracer, with a source located at a depth of 500 meters in both HPUs and LPUs, illustrates that solutes can be transported to greater depths in HPUs for a narrow ice lobe scenario, in comparison to a wide ice sheet or the 2D approach. Tracer transport in LPUs is unaffected by ice sheet geometry. Similarly, simulation results indicate that the ingress of dissolved oxygen (O 2 ) into HPUs is most substantial below a narrow ice lobe, while O 2 ingress into LPUs is not affected by ice sheet geometry. The numerical experiments indicate that 3D analysis will give more comprehensive results for flow patterns and reactive solute transport subjected to glaciation/deglaciation cycles in the case of a narrow ice lobe, but also suggest that a 2D approach might provide an adequate representation for the case of a relatively wide ice sheet. # Title of Dataset The impact of ice sheet geometry on meltwater ingress and reactive solute transport in sedimentary basins. # Brief summary of dataset contents This dataset includes the input files and simulated results of sutdy "The impact of ice sheet geometry on meltwater ingress and reactive solute transport in sedimentary basins", published in Water Resources Research. The dataset contains one 2D simulation scenario and three 3D simulation scenarios. Each simulation scenario has one folder. ## Description of ... Other/Unknown Material Ice Sheet Zenodo
institution Open Polar
collection Zenodo
op_collection_id ftzenodo
language unknown
topic ice sheet geometry
meltwater ingress
reactive transport
sedimentary basin
MIN3P-THCm
spellingShingle ice sheet geometry
meltwater ingress
reactive transport
sedimentary basin
MIN3P-THCm
Su, Danyang
Xie, Mingliang
Mayer, K. Ulrich
MacQuarrie, Kerry
The impact of ice sheet geometry on meltwater ingress and reactive solute transport in sedimentary basins
topic_facet ice sheet geometry
meltwater ingress
reactive transport
sedimentary basin
MIN3P-THCm
description We investigate the effect of ice sheet geometry on groundwater flow patterns and meltwater ingress in a hypothetical sedimentary basin. The simulation results indicate that meltwater ingress is much greater in 3D domains with a relatively narrow ice sheet extent compared to a wide ice sheet, or a simplified 2D model. In high permeability units (HPUs), the simulated meltwater penetration depth can reach up to 750 m in 3D domains compared to 400 m in a comparable 2D domain. In low permeability units (LPUs), very limited meltwater penetration occurs, indicating that ice sheet geometry and model dimensionality do not substantially affect water flow in these units. A conservative tracer, with a source located at a depth of 500 meters in both HPUs and LPUs, illustrates that solutes can be transported to greater depths in HPUs for a narrow ice lobe scenario, in comparison to a wide ice sheet or the 2D approach. Tracer transport in LPUs is unaffected by ice sheet geometry. Similarly, simulation results indicate that the ingress of dissolved oxygen (O 2 ) into HPUs is most substantial below a narrow ice lobe, while O 2 ingress into LPUs is not affected by ice sheet geometry. The numerical experiments indicate that 3D analysis will give more comprehensive results for flow patterns and reactive solute transport subjected to glaciation/deglaciation cycles in the case of a narrow ice lobe, but also suggest that a 2D approach might provide an adequate representation for the case of a relatively wide ice sheet. # Title of Dataset The impact of ice sheet geometry on meltwater ingress and reactive solute transport in sedimentary basins. # Brief summary of dataset contents This dataset includes the input files and simulated results of sutdy "The impact of ice sheet geometry on meltwater ingress and reactive solute transport in sedimentary basins", published in Water Resources Research. The dataset contains one 2D simulation scenario and three 3D simulation scenarios. Each simulation scenario has one folder. ## Description of ...
format Other/Unknown Material
author Su, Danyang
Xie, Mingliang
Mayer, K. Ulrich
MacQuarrie, Kerry
author_facet Su, Danyang
Xie, Mingliang
Mayer, K. Ulrich
MacQuarrie, Kerry
author_sort Su, Danyang
title The impact of ice sheet geometry on meltwater ingress and reactive solute transport in sedimentary basins
title_short The impact of ice sheet geometry on meltwater ingress and reactive solute transport in sedimentary basins
title_full The impact of ice sheet geometry on meltwater ingress and reactive solute transport in sedimentary basins
title_fullStr The impact of ice sheet geometry on meltwater ingress and reactive solute transport in sedimentary basins
title_full_unstemmed The impact of ice sheet geometry on meltwater ingress and reactive solute transport in sedimentary basins
title_sort impact of ice sheet geometry on meltwater ingress and reactive solute transport in sedimentary basins
publisher Zenodo
publishDate 2022
url https://doi.org/10.5281/zenodo.7047093
genre Ice Sheet
genre_facet Ice Sheet
op_relation https://eilinator.eos.ubc.ca:8443/index.php/s/5t8bXDnvfUAlPRF
https://www.min3p.com/contact-us
https://doi.org/10.5061/dryad.rjdfn2zfb
https://zenodo.org/communities/dryad
https://doi.org/10.5281/zenodo.7047092
https://doi.org/10.5281/zenodo.7047093
oai:zenodo.org:7047093
op_rights info:eu-repo/semantics/openAccess
MIT License
https://opensource.org/licenses/MIT
op_doi https://doi.org/10.5281/zenodo.704709310.5061/dryad.rjdfn2zfb10.5281/zenodo.7047092
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