A magnetic resonance study of temperature-dependent microstructural evolution and self-diffusion of water in Arctic first-year sea ice
The microstructural evolution of brine inclusions in granular and columnar sea ice has been investigated through magnetic resonance imaging (MRI) for temperatures between –28 and –3 ˚C. Thin-section and salinity measurements were completed on core samples obtained from winter sea ice near Barrow, Al...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.546.7961 2023-05-15T15:12:18+02:00 A magnetic resonance study of temperature-dependent microstructural evolution and self-diffusion of water in Arctic first-year sea ice H. Eicken The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.546.7961 http://www2.gi.alaska.edu/snowice/sea-lake-ice/papers/05BE.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.546.7961 http://www2.gi.alaska.edu/snowice/sea-lake-ice/papers/05BE.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www2.gi.alaska.edu/snowice/sea-lake-ice/papers/05BE.pdf text ftciteseerx 2016-01-08T11:19:35Z The microstructural evolution of brine inclusions in granular and columnar sea ice has been investigated through magnetic resonance imaging (MRI) for temperatures between –28 and –3 ˚C. Thin-section and salinity measurements were completed on core samples obtained from winter sea ice near Barrow, Alaska. Sub-samples of granular (2-5 cm depth in core) and columnar sea ice (20-23 cm depth), were investigated with 2morphological spin-echo and diffusion-weighted imaging in a Bruker 4.7 T 400 mm bore MRI system operating at field gradients of 200 mT/m at temperatures of approximately –28, –15, –6 and –3 ˚C. Average linear pore dimensions range between 0.2 and 1 mm and increase with bulk liquid volume fraction as temperatures rise from –15 to –3 ˚C. Granular ice pores are significantly larger than columnar ice pores and exhibit a higher degree of connectivity. No evidence is found of strongly non-linear increases in pore connectivity based on the MRI data. This might be explained by shortcomings in resolution, sensitivity and lack of truly three-dimensional data, differences between laboratory and field conditions or the absence of a percolation transition. Pore connectivity increases between –6 and –3 ˚C. Pore number densities average at 1.4 ± 1.2 mm–2. The pore number density distribution as a function of cross-sectional area conforms with power-law and lognormal distributions previously identified, although significant variations occur as a function of ice type and temperature. At low temperatures (<–26 ˚C), pore sizes were estimated from 1H self-diffusivity measurements, with self-diffusivity lower by up to an order of magnitude than in the free liquid. Analysis of diffusional length scales suggests characteristic pore dimensions of <1 µm at <–26 ˚C. 31. Text Arctic Barrow Sea ice Alaska Unknown Arctic |
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The microstructural evolution of brine inclusions in granular and columnar sea ice has been investigated through magnetic resonance imaging (MRI) for temperatures between –28 and –3 ˚C. Thin-section and salinity measurements were completed on core samples obtained from winter sea ice near Barrow, Alaska. Sub-samples of granular (2-5 cm depth in core) and columnar sea ice (20-23 cm depth), were investigated with 2morphological spin-echo and diffusion-weighted imaging in a Bruker 4.7 T 400 mm bore MRI system operating at field gradients of 200 mT/m at temperatures of approximately –28, –15, –6 and –3 ˚C. Average linear pore dimensions range between 0.2 and 1 mm and increase with bulk liquid volume fraction as temperatures rise from –15 to –3 ˚C. Granular ice pores are significantly larger than columnar ice pores and exhibit a higher degree of connectivity. No evidence is found of strongly non-linear increases in pore connectivity based on the MRI data. This might be explained by shortcomings in resolution, sensitivity and lack of truly three-dimensional data, differences between laboratory and field conditions or the absence of a percolation transition. Pore connectivity increases between –6 and –3 ˚C. Pore number densities average at 1.4 ± 1.2 mm–2. The pore number density distribution as a function of cross-sectional area conforms with power-law and lognormal distributions previously identified, although significant variations occur as a function of ice type and temperature. At low temperatures (<–26 ˚C), pore sizes were estimated from 1H self-diffusivity measurements, with self-diffusivity lower by up to an order of magnitude than in the free liquid. Analysis of diffusional length scales suggests characteristic pore dimensions of <1 µm at <–26 ˚C. 31. |
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The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
H. Eicken |
spellingShingle |
H. Eicken A magnetic resonance study of temperature-dependent microstructural evolution and self-diffusion of water in Arctic first-year sea ice |
author_facet |
H. Eicken |
author_sort |
H. Eicken |
title |
A magnetic resonance study of temperature-dependent microstructural evolution and self-diffusion of water in Arctic first-year sea ice |
title_short |
A magnetic resonance study of temperature-dependent microstructural evolution and self-diffusion of water in Arctic first-year sea ice |
title_full |
A magnetic resonance study of temperature-dependent microstructural evolution and self-diffusion of water in Arctic first-year sea ice |
title_fullStr |
A magnetic resonance study of temperature-dependent microstructural evolution and self-diffusion of water in Arctic first-year sea ice |
title_full_unstemmed |
A magnetic resonance study of temperature-dependent microstructural evolution and self-diffusion of water in Arctic first-year sea ice |
title_sort |
magnetic resonance study of temperature-dependent microstructural evolution and self-diffusion of water in arctic first-year sea ice |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.546.7961 http://www2.gi.alaska.edu/snowice/sea-lake-ice/papers/05BE.pdf |
geographic |
Arctic |
geographic_facet |
Arctic |
genre |
Arctic Barrow Sea ice Alaska |
genre_facet |
Arctic Barrow Sea ice Alaska |
op_source |
http://www2.gi.alaska.edu/snowice/sea-lake-ice/papers/05BE.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.546.7961 http://www2.gi.alaska.edu/snowice/sea-lake-ice/papers/05BE.pdf |
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Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
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1766343005756719104 |