The effects of Ca++ on the strength of polycrystalline ice
Recent studies have suggested a physical link between Ca++ ions and an increase in the ductility or ‘softening’ of polycrystalline ice. In order to investigate the potential effects of Ca++ on deformation, we created sets of both undoped and CaSO4-doped specimens of polycrystalline ice for testing i...
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Cambridge University Press
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ftdoajarticles:oai:doaj.org/article:09be5ee5ee6a4b6e8fc5949394c4bbfc 2023-05-15T16:57:33+02:00 The effects of Ca++ on the strength of polycrystalline ice KEVIN HAMMONDS IAN BAKER 2016-10-01T00:00:00Z https://doi.org/10.1017/jog.2016.84 https://doaj.org/article/09be5ee5ee6a4b6e8fc5949394c4bbfc EN eng Cambridge University Press https://www.cambridge.org/core/product/identifier/S0022143016000848/type/journal_article https://doaj.org/toc/0022-1430 https://doaj.org/toc/1727-5652 doi:10.1017/jog.2016.84 0022-1430 1727-5652 https://doaj.org/article/09be5ee5ee6a4b6e8fc5949394c4bbfc Journal of Glaciology, Vol 62, Pp 954-962 (2016) glacier flow glacier mechanics ice chemistry ice engineering ice rheology Environmental sciences GE1-350 Meteorology. Climatology QC851-999 article 2016 ftdoajarticles https://doi.org/10.1017/jog.2016.84 2023-03-12T01:30:59Z Recent studies have suggested a physical link between Ca++ ions and an increase in the ductility or ‘softening’ of polycrystalline ice. In order to investigate the potential effects of Ca++ on deformation, we created sets of both undoped and CaSO4-doped specimens of polycrystalline ice for testing in uniaxial tension or compression. Deformation tests in tension were carried out under a constant load at an initial stress of 0.75 MPa and a temperature of −6°C. Compression tests were carried out at −10 and −20°C at constant strain rates of 1×10−4 s−1, 1 × 10−5 s−1 and 1 × 10−6 s−1 and taken to 5% strain. Our results show that CaSO4 increases the strength of polycrystalline ice at higher strain rates and lower temperatures, an effect that decreases with decreasing strain rate and higher temperatures. A microstructural analysis of the post-test compression specimens reveals mean grain diameters much larger in the CaSO4-doped specimens tested at the lowest applied strain rate of 1 × 10−6 s−1. Precipitates were found to have formed along grain boundaries in some doped specimens and evidence of intergranular fracture was observed in all specimens tested at 1 × 10−4 and 1 × 10−5 s−1. In tension-tested specimens, there was no difference in the mean grain diameter between doped and undoped specimens at 25% strain. Article in Journal/Newspaper Journal of Glaciology Directory of Open Access Journals: DOAJ Articles Journal of Glaciology 62 235 954 962 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
glacier flow glacier mechanics ice chemistry ice engineering ice rheology Environmental sciences GE1-350 Meteorology. Climatology QC851-999 |
spellingShingle |
glacier flow glacier mechanics ice chemistry ice engineering ice rheology Environmental sciences GE1-350 Meteorology. Climatology QC851-999 KEVIN HAMMONDS IAN BAKER The effects of Ca++ on the strength of polycrystalline ice |
topic_facet |
glacier flow glacier mechanics ice chemistry ice engineering ice rheology Environmental sciences GE1-350 Meteorology. Climatology QC851-999 |
description |
Recent studies have suggested a physical link between Ca++ ions and an increase in the ductility or ‘softening’ of polycrystalline ice. In order to investigate the potential effects of Ca++ on deformation, we created sets of both undoped and CaSO4-doped specimens of polycrystalline ice for testing in uniaxial tension or compression. Deformation tests in tension were carried out under a constant load at an initial stress of 0.75 MPa and a temperature of −6°C. Compression tests were carried out at −10 and −20°C at constant strain rates of 1×10−4 s−1, 1 × 10−5 s−1 and 1 × 10−6 s−1 and taken to 5% strain. Our results show that CaSO4 increases the strength of polycrystalline ice at higher strain rates and lower temperatures, an effect that decreases with decreasing strain rate and higher temperatures. A microstructural analysis of the post-test compression specimens reveals mean grain diameters much larger in the CaSO4-doped specimens tested at the lowest applied strain rate of 1 × 10−6 s−1. Precipitates were found to have formed along grain boundaries in some doped specimens and evidence of intergranular fracture was observed in all specimens tested at 1 × 10−4 and 1 × 10−5 s−1. In tension-tested specimens, there was no difference in the mean grain diameter between doped and undoped specimens at 25% strain. |
format |
Article in Journal/Newspaper |
author |
KEVIN HAMMONDS IAN BAKER |
author_facet |
KEVIN HAMMONDS IAN BAKER |
author_sort |
KEVIN HAMMONDS |
title |
The effects of Ca++ on the strength of polycrystalline ice |
title_short |
The effects of Ca++ on the strength of polycrystalline ice |
title_full |
The effects of Ca++ on the strength of polycrystalline ice |
title_fullStr |
The effects of Ca++ on the strength of polycrystalline ice |
title_full_unstemmed |
The effects of Ca++ on the strength of polycrystalline ice |
title_sort |
effects of ca++ on the strength of polycrystalline ice |
publisher |
Cambridge University Press |
publishDate |
2016 |
url |
https://doi.org/10.1017/jog.2016.84 https://doaj.org/article/09be5ee5ee6a4b6e8fc5949394c4bbfc |
genre |
Journal of Glaciology |
genre_facet |
Journal of Glaciology |
op_source |
Journal of Glaciology, Vol 62, Pp 954-962 (2016) |
op_relation |
https://www.cambridge.org/core/product/identifier/S0022143016000848/type/journal_article https://doaj.org/toc/0022-1430 https://doaj.org/toc/1727-5652 doi:10.1017/jog.2016.84 0022-1430 1727-5652 https://doaj.org/article/09be5ee5ee6a4b6e8fc5949394c4bbfc |
op_doi |
https://doi.org/10.1017/jog.2016.84 |
container_title |
Journal of Glaciology |
container_volume |
62 |
container_issue |
235 |
container_start_page |
954 |
op_container_end_page |
962 |
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1766049110100541440 |