Grain growth of ice doped with soluble impurities
The grain size of polycrystalline ice affects key parameters related to the dynamics of ice masses, such as the rheological and dielectric properties of terrestrial ice as well as the ice shells of icy satellites. To investigate the effect of soluble impurities on the grain-growth kinetics of polycr...
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Copernicus Publications
2024
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ftdoajarticles:oai:doaj.org/article:b127ac63fa07417986ec31723f42d308 2024-09-15T18:38:59+00:00 Grain growth of ice doped with soluble impurities Q. Wang S. Fan C. Qi 2024-03-01T00:00:00Z https://doi.org/10.5194/tc-18-1053-2024 https://doaj.org/article/b127ac63fa07417986ec31723f42d308 EN eng Copernicus Publications https://tc.copernicus.org/articles/18/1053/2024/tc-18-1053-2024.pdf https://doaj.org/toc/1994-0416 https://doaj.org/toc/1994-0424 doi:10.5194/tc-18-1053-2024 1994-0416 1994-0424 https://doaj.org/article/b127ac63fa07417986ec31723f42d308 The Cryosphere, Vol 18, Pp 1053-1084 (2024) Environmental sciences GE1-350 Geology QE1-996.5 article 2024 ftdoajarticles https://doi.org/10.5194/tc-18-1053-2024 2024-08-05T17:49:53Z The grain size of polycrystalline ice affects key parameters related to the dynamics of ice masses, such as the rheological and dielectric properties of terrestrial ice as well as the ice shells of icy satellites. To investigate the effect of soluble impurities on the grain-growth kinetics of polycrystalline ice, we conducted annealing experiments on polycrystalline ice samples doped with different concentrations of KCl (10 −2 , 10 −3 , 10 −4 and 10 −5 mol L −1 ) or MgSO 4 (10 −2 and 10 −5 mol L −1 ). Samples were annealed for a maximum of 100 h at a hydrostatic confining pressure of 20 MPa (corresponding to a depth of about 2 km) and different constant temperatures of 268, 263, 258 and 253 K (corresponding to − 5, − 10, − 15 and − 20 °C, respectively). After each experiment, images of a polished sample surface were obtained using an optical microscope equipped with a cold stage. With grain boundaries detected, grains were reconstructed from the images, and an average grain size was determined for each sample. Normal grain growth occurred in all samples. Grain-size data are interpreted using the following grain-growth model: d n - d 0 n = k t <svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="63pt" height="15pt" class="svg-formula" dspmath="mathimg" md5hash="460baa849c7d73d1781529949316097c"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="tc-18-1053-2024-ie00001.svg" width="63pt" height="15pt" src="tc-18-1053-2024-ie00001.png"/></svg:svg> ( d : grain size; d 0 : starting grain size; n : grain-growth exponent; k : growth constant; t : duration). Values of the best-fit grain-growth exponent, n , for all samples range from 2.6 to 6.2, with an average value of 4.7. Pure ice exhibits 3.1 ⩽ n ⩽ <svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="29pt" height="10pt" class="svg-formula" dspmath="mathimg" md5hash="85cb61edab7e06b832fc006f6ac93996"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="tc-18-1053-2024-ie00002.svg" width="29pt" height="10pt" ... Article in Journal/Newspaper The Cryosphere Directory of Open Access Journals: DOAJ Articles The Cryosphere 18 3 1053 1084 |
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Open Polar |
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Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
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English |
topic |
Environmental sciences GE1-350 Geology QE1-996.5 |
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Environmental sciences GE1-350 Geology QE1-996.5 Q. Wang S. Fan C. Qi Grain growth of ice doped with soluble impurities |
topic_facet |
Environmental sciences GE1-350 Geology QE1-996.5 |
description |
The grain size of polycrystalline ice affects key parameters related to the dynamics of ice masses, such as the rheological and dielectric properties of terrestrial ice as well as the ice shells of icy satellites. To investigate the effect of soluble impurities on the grain-growth kinetics of polycrystalline ice, we conducted annealing experiments on polycrystalline ice samples doped with different concentrations of KCl (10 −2 , 10 −3 , 10 −4 and 10 −5 mol L −1 ) or MgSO 4 (10 −2 and 10 −5 mol L −1 ). Samples were annealed for a maximum of 100 h at a hydrostatic confining pressure of 20 MPa (corresponding to a depth of about 2 km) and different constant temperatures of 268, 263, 258 and 253 K (corresponding to − 5, − 10, − 15 and − 20 °C, respectively). After each experiment, images of a polished sample surface were obtained using an optical microscope equipped with a cold stage. With grain boundaries detected, grains were reconstructed from the images, and an average grain size was determined for each sample. Normal grain growth occurred in all samples. Grain-size data are interpreted using the following grain-growth model: d n - d 0 n = k t <svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="63pt" height="15pt" class="svg-formula" dspmath="mathimg" md5hash="460baa849c7d73d1781529949316097c"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="tc-18-1053-2024-ie00001.svg" width="63pt" height="15pt" src="tc-18-1053-2024-ie00001.png"/></svg:svg> ( d : grain size; d 0 : starting grain size; n : grain-growth exponent; k : growth constant; t : duration). Values of the best-fit grain-growth exponent, n , for all samples range from 2.6 to 6.2, with an average value of 4.7. Pure ice exhibits 3.1 ⩽ n ⩽ <svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="29pt" height="10pt" class="svg-formula" dspmath="mathimg" md5hash="85cb61edab7e06b832fc006f6ac93996"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="tc-18-1053-2024-ie00002.svg" width="29pt" height="10pt" ... |
format |
Article in Journal/Newspaper |
author |
Q. Wang S. Fan C. Qi |
author_facet |
Q. Wang S. Fan C. Qi |
author_sort |
Q. Wang |
title |
Grain growth of ice doped with soluble impurities |
title_short |
Grain growth of ice doped with soluble impurities |
title_full |
Grain growth of ice doped with soluble impurities |
title_fullStr |
Grain growth of ice doped with soluble impurities |
title_full_unstemmed |
Grain growth of ice doped with soluble impurities |
title_sort |
grain growth of ice doped with soluble impurities |
publisher |
Copernicus Publications |
publishDate |
2024 |
url |
https://doi.org/10.5194/tc-18-1053-2024 https://doaj.org/article/b127ac63fa07417986ec31723f42d308 |
genre |
The Cryosphere |
genre_facet |
The Cryosphere |
op_source |
The Cryosphere, Vol 18, Pp 1053-1084 (2024) |
op_relation |
https://tc.copernicus.org/articles/18/1053/2024/tc-18-1053-2024.pdf https://doaj.org/toc/1994-0416 https://doaj.org/toc/1994-0424 doi:10.5194/tc-18-1053-2024 1994-0416 1994-0424 https://doaj.org/article/b127ac63fa07417986ec31723f42d308 |
op_doi |
https://doi.org/10.5194/tc-18-1053-2024 |
container_title |
The Cryosphere |
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18 |
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3 |
container_start_page |
1053 |
op_container_end_page |
1084 |
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1810483381984559104 |