MICROSCOPIC OBSERVATIONS OF THE AIR HYDRATE-BUBBLE. TRANSFORMATION PROCESS IN GLACIER ICE
Microscopie examinations for air hydrate inclusions were made on specimens of the Dye-3 and Camp Century, Greenland and Byrd Station, Antarctica deep ice cores. The shallowest depths at which air hydrates are observed in the Dye-3, Camp Century and Byrd Station cores are at 1092 m, 1099 m and 727 m...
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ftccsdartic:oai:HAL:jpa-00226321v1 2023-11-12T04:04:27+01:00 MICROSCOPIC OBSERVATIONS OF THE AIR HYDRATE-BUBBLE. TRANSFORMATION PROCESS IN GLACIER ICE Shoji, H. Langway, C. Jr 1987 https://hal.science/jpa-00226321 https://hal.science/jpa-00226321/document https://hal.science/jpa-00226321/file/ajp-jphyscol198748C175.pdf https://doi.org/10.1051/jphyscol:1987175 en eng HAL CCSD info:eu-repo/semantics/altIdentifier/doi/10.1051/jphyscol:1987175 jpa-00226321 https://hal.science/jpa-00226321 https://hal.science/jpa-00226321/document https://hal.science/jpa-00226321/file/ajp-jphyscol198748C175.pdf doi:10.1051/jphyscol:1987175 info:eu-repo/semantics/OpenAccess Journal de Physique Colloques https://hal.science/jpa-00226321 Journal de Physique Colloques, 1987, 48 (C1), pp.C1-551-C1-556. ⟨10.1051/jphyscol:1987175⟩ [PHYS.HIST]Physics [physics]/Physics archives info:eu-repo/semantics/article Journal articles 1987 ftccsdartic https://doi.org/10.1051/jphyscol:1987175 2023-10-21T23:42:00Z Microscopie examinations for air hydrate inclusions were made on specimens of the Dye-3 and Camp Century, Greenland and Byrd Station, Antarctica deep ice cores. The shallowest depths at which air hydrates are observed in the Dye-3, Camp Century and Byrd Station cores are at 1092 m, 1099 m and 727 m depths respectively. For the Dye-3 and Camp Century cores, the observed depths for air hydrate appearance agree with Miller's calculation [1]. For the Byrd Station core, the observed depth for the appearance is about 100 m shallower than the calculation result by Miller. This apparent difference at Byrd Station may be attributed to the general upward ice flow trajectory which begins about 5 km upstream from the Byrd Station location. The phase/grain boundary observations and deformation experiments revealed that phase boundary energy is much higher than grain boundary energy and that the transformation process from air hydrate to bubble is clearly related to the strain-induced nucleation process. These findings suggest that the air hydrate/bubble transformation process is strongly controlled by both in situ and post ice core recovery nucleation activation process. Article in Journal/Newspaper Antarc* Antarctica Dye 3 Dye-3 glacier Greenland ice core Archive ouverte HAL (Hyper Article en Ligne, CCSD - Centre pour la Communication Scientifique Directe) Greenland Byrd Byrd Station ENVELOPE(-119.533,-119.533,-80.017,-80.017) |
institution |
Open Polar |
collection |
Archive ouverte HAL (Hyper Article en Ligne, CCSD - Centre pour la Communication Scientifique Directe) |
op_collection_id |
ftccsdartic |
language |
English |
topic |
[PHYS.HIST]Physics [physics]/Physics archives |
spellingShingle |
[PHYS.HIST]Physics [physics]/Physics archives Shoji, H. Langway, C. Jr MICROSCOPIC OBSERVATIONS OF THE AIR HYDRATE-BUBBLE. TRANSFORMATION PROCESS IN GLACIER ICE |
topic_facet |
[PHYS.HIST]Physics [physics]/Physics archives |
description |
Microscopie examinations for air hydrate inclusions were made on specimens of the Dye-3 and Camp Century, Greenland and Byrd Station, Antarctica deep ice cores. The shallowest depths at which air hydrates are observed in the Dye-3, Camp Century and Byrd Station cores are at 1092 m, 1099 m and 727 m depths respectively. For the Dye-3 and Camp Century cores, the observed depths for air hydrate appearance agree with Miller's calculation [1]. For the Byrd Station core, the observed depth for the appearance is about 100 m shallower than the calculation result by Miller. This apparent difference at Byrd Station may be attributed to the general upward ice flow trajectory which begins about 5 km upstream from the Byrd Station location. The phase/grain boundary observations and deformation experiments revealed that phase boundary energy is much higher than grain boundary energy and that the transformation process from air hydrate to bubble is clearly related to the strain-induced nucleation process. These findings suggest that the air hydrate/bubble transformation process is strongly controlled by both in situ and post ice core recovery nucleation activation process. |
format |
Article in Journal/Newspaper |
author |
Shoji, H. Langway, C. Jr |
author_facet |
Shoji, H. Langway, C. Jr |
author_sort |
Shoji, H. |
title |
MICROSCOPIC OBSERVATIONS OF THE AIR HYDRATE-BUBBLE. TRANSFORMATION PROCESS IN GLACIER ICE |
title_short |
MICROSCOPIC OBSERVATIONS OF THE AIR HYDRATE-BUBBLE. TRANSFORMATION PROCESS IN GLACIER ICE |
title_full |
MICROSCOPIC OBSERVATIONS OF THE AIR HYDRATE-BUBBLE. TRANSFORMATION PROCESS IN GLACIER ICE |
title_fullStr |
MICROSCOPIC OBSERVATIONS OF THE AIR HYDRATE-BUBBLE. TRANSFORMATION PROCESS IN GLACIER ICE |
title_full_unstemmed |
MICROSCOPIC OBSERVATIONS OF THE AIR HYDRATE-BUBBLE. TRANSFORMATION PROCESS IN GLACIER ICE |
title_sort |
microscopic observations of the air hydrate-bubble. transformation process in glacier ice |
publisher |
HAL CCSD |
publishDate |
1987 |
url |
https://hal.science/jpa-00226321 https://hal.science/jpa-00226321/document https://hal.science/jpa-00226321/file/ajp-jphyscol198748C175.pdf https://doi.org/10.1051/jphyscol:1987175 |
long_lat |
ENVELOPE(-119.533,-119.533,-80.017,-80.017) |
geographic |
Greenland Byrd Byrd Station |
geographic_facet |
Greenland Byrd Byrd Station |
genre |
Antarc* Antarctica Dye 3 Dye-3 glacier Greenland ice core |
genre_facet |
Antarc* Antarctica Dye 3 Dye-3 glacier Greenland ice core |
op_source |
Journal de Physique Colloques https://hal.science/jpa-00226321 Journal de Physique Colloques, 1987, 48 (C1), pp.C1-551-C1-556. ⟨10.1051/jphyscol:1987175⟩ |
op_relation |
info:eu-repo/semantics/altIdentifier/doi/10.1051/jphyscol:1987175 jpa-00226321 https://hal.science/jpa-00226321 https://hal.science/jpa-00226321/document https://hal.science/jpa-00226321/file/ajp-jphyscol198748C175.pdf doi:10.1051/jphyscol:1987175 |
op_rights |
info:eu-repo/semantics/OpenAccess |
op_doi |
https://doi.org/10.1051/jphyscol:1987175 |
_version_ |
1782341620276920320 |