Experimental data for paper "hydraulic transmissivity inferred from ice-sheet relaxation following Greenland supraglacial lake drainages"
This setup mimics ice lying above the drainage system. In the experiment, a fluid-filled blister is generated via liquid injection into the interface between a transparent elastic layer and a porous substrate. After injection of liquid, the fluid permeates from the blister through the porous substra...
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ftprincetonuniv:oai:dataspace.princeton.edu:88435/dsp019g54xm73k 2023-05-15T16:27:54+02:00 Experimental data for paper "hydraulic transmissivity inferred from ice-sheet relaxation following Greenland supraglacial lake drainages" Lai, Ching-Yao 2021-05-18 http://arks.princeton.edu/ark:/88435/dsp019g54xm73k https://doi.org/10.34770/mx55-jz51 en_US eng https://doi.org/10.1038/s41467-021-24186-6 http://arks.princeton.edu/ark:/88435/dsp019g54xm73k https://doi.org/10.34770/mx55-jz51 Dataset 2021 ftprincetonuniv https://doi.org/10.34770/mx55-jz51 https://doi.org/10.1038/s41467-021-24186-6 2022-04-10T21:04:24Z This setup mimics ice lying above the drainage system. In the experiment, a fluid-filled blister is generated via liquid injection into the interface between a transparent elastic layer and a porous substrate. After injection of liquid, the fluid permeates from the blister through the porous substrate, the blister volume V(t) relaxes exponentially with time. Our lab experiments show that varying the permeability of the porous substrate k significantly impacts the relaxation timescale in the experiments. Dataset Greenland Ice Sheet DataSpace at Princeton University Greenland |
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Open Polar |
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DataSpace at Princeton University |
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ftprincetonuniv |
language |
English |
description |
This setup mimics ice lying above the drainage system. In the experiment, a fluid-filled blister is generated via liquid injection into the interface between a transparent elastic layer and a porous substrate. After injection of liquid, the fluid permeates from the blister through the porous substrate, the blister volume V(t) relaxes exponentially with time. Our lab experiments show that varying the permeability of the porous substrate k significantly impacts the relaxation timescale in the experiments. |
format |
Dataset |
author |
Lai, Ching-Yao |
spellingShingle |
Lai, Ching-Yao Experimental data for paper "hydraulic transmissivity inferred from ice-sheet relaxation following Greenland supraglacial lake drainages" |
author_facet |
Lai, Ching-Yao |
author_sort |
Lai, Ching-Yao |
title |
Experimental data for paper "hydraulic transmissivity inferred from ice-sheet relaxation following Greenland supraglacial lake drainages" |
title_short |
Experimental data for paper "hydraulic transmissivity inferred from ice-sheet relaxation following Greenland supraglacial lake drainages" |
title_full |
Experimental data for paper "hydraulic transmissivity inferred from ice-sheet relaxation following Greenland supraglacial lake drainages" |
title_fullStr |
Experimental data for paper "hydraulic transmissivity inferred from ice-sheet relaxation following Greenland supraglacial lake drainages" |
title_full_unstemmed |
Experimental data for paper "hydraulic transmissivity inferred from ice-sheet relaxation following Greenland supraglacial lake drainages" |
title_sort |
experimental data for paper "hydraulic transmissivity inferred from ice-sheet relaxation following greenland supraglacial lake drainages" |
publishDate |
2021 |
url |
http://arks.princeton.edu/ark:/88435/dsp019g54xm73k https://doi.org/10.34770/mx55-jz51 |
geographic |
Greenland |
geographic_facet |
Greenland |
genre |
Greenland Ice Sheet |
genre_facet |
Greenland Ice Sheet |
op_relation |
https://doi.org/10.1038/s41467-021-24186-6 http://arks.princeton.edu/ark:/88435/dsp019g54xm73k https://doi.org/10.34770/mx55-jz51 |
op_doi |
https://doi.org/10.34770/mx55-jz51 https://doi.org/10.1038/s41467-021-24186-6 |
_version_ |
1766017470666113024 |