Core drilling at Syowa Station, Antarctica
The first core drilling at Syowa Station in Antarctica was carried out by the 21st Japanese Antarctic Research Expedition (JARE-21) by a rotary core drilling method using air as the drilling fluid. After 26 days of drilling work, a 20m-deep borehole was obtained in March 1980. In order to deepen thi...
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National Institute of Polar Research
1983
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ftdoajarticles:oai:doaj.org/article:69feba41573148e5a76802eca332ada5 2023-05-15T14:01:46+02:00 Core drilling at Syowa Station, Antarctica Katsutada Kaminuma 1983-01-01T00:00:00Z https://doi.org/10.15094/00008341 https://doaj.org/article/69feba41573148e5a76802eca332ada5 EN JA eng jpn National Institute of Polar Research https://doi.org/10.15094/00008341 https://doaj.org/toc/0085-7289 https://doaj.org/toc/2432-079X doi:10.15094/00008341 0085-7289 2432-079X https://doaj.org/article/69feba41573148e5a76802eca332ada5 Antarctic Record, Iss 77, Pp 134-143 (1983) Geography (General) G1-922 article 1983 ftdoajarticles https://doi.org/10.15094/00008341 2023-01-08T01:29:05Z The first core drilling at Syowa Station in Antarctica was carried out by the 21st Japanese Antarctic Research Expedition (JARE-21) by a rotary core drilling method using air as the drilling fluid. After 26 days of drilling work, a 20m-deep borehole was obtained in March 1980. In order to deepen this borehole, the core drilling was succeeded by JARE-22 using water as the drilling fluid. However, drilling rods were stuck in the hole during the removal of the frozen drilling fluid. The part of the hole which is deeper than 5m could not be used for underground temperature measurements. Though a new 30m-deep hole was drilled in March 1981,drilling rods were stuck in the hole again. Only the upper part of the hole which is shallower than 7m could be used for the temperature measurements. Another 30m-deep hole was drilled in January 1982. It was done well to make the 30m-deep hole. However, the hole could not be used for the temperature measurements, because drilling rods were stuck in the hole again during the removal of the drilling fluid. Though the leakage and/or flood of water in the drilling hole on East Ongul Island was beyond prediction, a few cracks at the depth from the surface to 10m were found to act as waterways. To keep water from leakage and/or flood is the most important in the core drilling at Syowa Station. Article in Journal/Newspaper Antarc* Antarctic Antarctica East Ongul Island Ongul Island Directory of Open Access Journals: DOAJ Articles Antarctic Syowa Station Ongul ENVELOPE(39.533,39.533,-69.017,-69.017) Ongul Island ENVELOPE(39.533,39.533,-69.017,-69.017) East Ongul Island ENVELOPE(39.583,39.583,-69.017,-69.017) |
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Open Polar |
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Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English Japanese |
topic |
Geography (General) G1-922 |
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Geography (General) G1-922 Katsutada Kaminuma Core drilling at Syowa Station, Antarctica |
topic_facet |
Geography (General) G1-922 |
description |
The first core drilling at Syowa Station in Antarctica was carried out by the 21st Japanese Antarctic Research Expedition (JARE-21) by a rotary core drilling method using air as the drilling fluid. After 26 days of drilling work, a 20m-deep borehole was obtained in March 1980. In order to deepen this borehole, the core drilling was succeeded by JARE-22 using water as the drilling fluid. However, drilling rods were stuck in the hole during the removal of the frozen drilling fluid. The part of the hole which is deeper than 5m could not be used for underground temperature measurements. Though a new 30m-deep hole was drilled in March 1981,drilling rods were stuck in the hole again. Only the upper part of the hole which is shallower than 7m could be used for the temperature measurements. Another 30m-deep hole was drilled in January 1982. It was done well to make the 30m-deep hole. However, the hole could not be used for the temperature measurements, because drilling rods were stuck in the hole again during the removal of the drilling fluid. Though the leakage and/or flood of water in the drilling hole on East Ongul Island was beyond prediction, a few cracks at the depth from the surface to 10m were found to act as waterways. To keep water from leakage and/or flood is the most important in the core drilling at Syowa Station. |
format |
Article in Journal/Newspaper |
author |
Katsutada Kaminuma |
author_facet |
Katsutada Kaminuma |
author_sort |
Katsutada Kaminuma |
title |
Core drilling at Syowa Station, Antarctica |
title_short |
Core drilling at Syowa Station, Antarctica |
title_full |
Core drilling at Syowa Station, Antarctica |
title_fullStr |
Core drilling at Syowa Station, Antarctica |
title_full_unstemmed |
Core drilling at Syowa Station, Antarctica |
title_sort |
core drilling at syowa station, antarctica |
publisher |
National Institute of Polar Research |
publishDate |
1983 |
url |
https://doi.org/10.15094/00008341 https://doaj.org/article/69feba41573148e5a76802eca332ada5 |
long_lat |
ENVELOPE(39.533,39.533,-69.017,-69.017) ENVELOPE(39.533,39.533,-69.017,-69.017) ENVELOPE(39.583,39.583,-69.017,-69.017) |
geographic |
Antarctic Syowa Station Ongul Ongul Island East Ongul Island |
geographic_facet |
Antarctic Syowa Station Ongul Ongul Island East Ongul Island |
genre |
Antarc* Antarctic Antarctica East Ongul Island Ongul Island |
genre_facet |
Antarc* Antarctic Antarctica East Ongul Island Ongul Island |
op_source |
Antarctic Record, Iss 77, Pp 134-143 (1983) |
op_relation |
https://doi.org/10.15094/00008341 https://doaj.org/toc/0085-7289 https://doaj.org/toc/2432-079X doi:10.15094/00008341 0085-7289 2432-079X https://doaj.org/article/69feba41573148e5a76802eca332ada5 |
op_doi |
https://doi.org/10.15094/00008341 |
_version_ |
1766271797872820224 |