DIAMETER MEASUREMENTS OF A 700-M DEEP BORE-HOLE AT MIZUHO STATION, EAST ANTARCTICA

P(論文) The closure rate was obtained by measuring the change in diameter of the bore-hole. The diameter measurements were firstly made on 3rd August 1984,the second day after the completion of the drilling. It was repeated eighttimes for one year and a half, and the last measurements were carried out...

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Main Authors: オクヒラ, フミオ, ナルセ, レンジ, ナカオ, マサヨシ, カワダ, クニオ, OKUHIRA, Fumio, NARUSE, Renji, NAKAWO, Masayoshi, KAWADA, Kunio
Language:English
Published: National Institute of Polar Research 1987
Subjects:
Online Access:https://nipr.repo.nii.ac.jp/record/3549/files/KJ00000767757.pdf
https://doi.org/10.15094/00003549
https://nipr.repo.nii.ac.jp/records/3549
_version_ 1829300899530407936
author オクヒラ, フミオ
ナルセ, レンジ
ナカオ, マサヨシ
カワダ, クニオ
OKUHIRA, Fumio
NARUSE, Renji
NAKAWO, Masayoshi
KAWADA, Kunio
author_facet オクヒラ, フミオ
ナルセ, レンジ
ナカオ, マサヨシ
カワダ, クニオ
OKUHIRA, Fumio
NARUSE, Renji
NAKAWO, Masayoshi
KAWADA, Kunio
author_sort オクヒラ, フミオ
collection National Institute of Polar Research Repository, Japan
description P(論文) The closure rate was obtained by measuring the change in diameter of the bore-hole. The diameter measurements were firstly made on 3rd August 1984,the second day after the completion of the drilling. It was repeated eighttimes for one year and a half, and the last measurements were carried out on 19th January 1986. The strain rate of the bore-hole was calculated from these observations. It decreased with time at shallow depths continuously, indicating that the steady state had not been reached for the observation period. At deeper depths, the strain rate decreased in the early period, but icreased at later stages, taking a minimum value in between. The minimum strain rate was achieved earlier at deep depths than at shallow depths. A power law was obtained between the minimum strain rate and the shear stress at various depths. The power law was compatible with that derived from observations of surface flow at Mizuho Plateau. departmental bulletin paper
genre Antarc*
Antarctica
East Antarctica
Polar meteorology and glaciology
Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology
genre_facet Antarc*
Antarctica
East Antarctica
Polar meteorology and glaciology
Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology
geographic East Antarctica
Mizuho
Mizuho Station
Mizuho Plateau
geographic_facet East Antarctica
Mizuho
Mizuho Station
Mizuho Plateau
id ftnipr:oai:nipr.repo.nii.ac.jp:00003549
institution Open Polar
language English
long_lat ENVELOPE(44.317,44.317,-70.683,-70.683)
ENVELOPE(44.317,44.317,-70.683,-70.683)
ENVELOPE(40.000,40.000,-73.000,-73.000)
op_collection_id ftnipr
op_doi https://doi.org/10.15094/00003549
op_relation Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology
1
156
AA10756213
https://nipr.repo.nii.ac.jp/record/3549/files/KJ00000767757.pdf
https://doi.org/10.15094/00003549
https://nipr.repo.nii.ac.jp/records/3549
publishDate 1987
publisher National Institute of Polar Research
record_format openpolar
spelling ftnipr:oai:nipr.repo.nii.ac.jp:00003549 2025-04-13T14:09:09+00:00 DIAMETER MEASUREMENTS OF A 700-M DEEP BORE-HOLE AT MIZUHO STATION, EAST ANTARCTICA オクヒラ, フミオ ナルセ, レンジ ナカオ, マサヨシ カワダ, クニオ OKUHIRA, Fumio NARUSE, Renji NAKAWO, Masayoshi KAWADA, Kunio 1987-09 application/pdf https://nipr.repo.nii.ac.jp/record/3549/files/KJ00000767757.pdf https://doi.org/10.15094/00003549 https://nipr.repo.nii.ac.jp/records/3549 eng eng National Institute of Polar Research Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology 1 156 AA10756213 https://nipr.repo.nii.ac.jp/record/3549/files/KJ00000767757.pdf https://doi.org/10.15094/00003549 https://nipr.repo.nii.ac.jp/records/3549 1987 ftnipr https://doi.org/10.15094/00003549 2025-03-19T10:19:56Z P(論文) The closure rate was obtained by measuring the change in diameter of the bore-hole. The diameter measurements were firstly made on 3rd August 1984,the second day after the completion of the drilling. It was repeated eighttimes for one year and a half, and the last measurements were carried out on 19th January 1986. The strain rate of the bore-hole was calculated from these observations. It decreased with time at shallow depths continuously, indicating that the steady state had not been reached for the observation period. At deeper depths, the strain rate decreased in the early period, but icreased at later stages, taking a minimum value in between. The minimum strain rate was achieved earlier at deep depths than at shallow depths. A power law was obtained between the minimum strain rate and the shear stress at various depths. The power law was compatible with that derived from observations of surface flow at Mizuho Plateau. departmental bulletin paper Other/Unknown Material Antarc* Antarctica East Antarctica Polar meteorology and glaciology Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology National Institute of Polar Research Repository, Japan East Antarctica Mizuho ENVELOPE(44.317,44.317,-70.683,-70.683) Mizuho Station ENVELOPE(44.317,44.317,-70.683,-70.683) Mizuho Plateau ENVELOPE(40.000,40.000,-73.000,-73.000)
spellingShingle オクヒラ, フミオ
ナルセ, レンジ
ナカオ, マサヨシ
カワダ, クニオ
OKUHIRA, Fumio
NARUSE, Renji
NAKAWO, Masayoshi
KAWADA, Kunio
DIAMETER MEASUREMENTS OF A 700-M DEEP BORE-HOLE AT MIZUHO STATION, EAST ANTARCTICA
title DIAMETER MEASUREMENTS OF A 700-M DEEP BORE-HOLE AT MIZUHO STATION, EAST ANTARCTICA
title_full DIAMETER MEASUREMENTS OF A 700-M DEEP BORE-HOLE AT MIZUHO STATION, EAST ANTARCTICA
title_fullStr DIAMETER MEASUREMENTS OF A 700-M DEEP BORE-HOLE AT MIZUHO STATION, EAST ANTARCTICA
title_full_unstemmed DIAMETER MEASUREMENTS OF A 700-M DEEP BORE-HOLE AT MIZUHO STATION, EAST ANTARCTICA
title_short DIAMETER MEASUREMENTS OF A 700-M DEEP BORE-HOLE AT MIZUHO STATION, EAST ANTARCTICA
title_sort diameter measurements of a 700-m deep bore-hole at mizuho station, east antarctica
url https://nipr.repo.nii.ac.jp/record/3549/files/KJ00000767757.pdf
https://doi.org/10.15094/00003549
https://nipr.repo.nii.ac.jp/records/3549