A new explanation of bending of a snow density profile
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概要
- 論文の詳細を見る
The physical meaning of bending of a snow density profile at G2 in Antarctica (665kg/m^3,32m depth below the snow surface) was investigated. It was found that the bending occurred at pressures around 0.1-0.2 MPa. Examination of snow densification mechanisms as a pressure-sintering phenomenon suggested that the bending is related to the initiation of dominance of the dislocation creep mechanism.
- 国立極地研究所の論文
著者
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Nishimura Hiroshi
Institute Of Low Temperature Science Hokkaido University
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EBINUMA Takao
Institute for Energy Utilization, National Institute of Advanced Industrial Science and Technology (
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Ebinuma Takao
Institute Of Low Temperature Science Hokkaido University
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Maeno N
Hokkaido Univ. Sapporo
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Maeno Norikazu
Institute Of Low Temperature Science Hokkaido University
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Nishimura Hiroshi
Department Of Geosciences Faculty Of Science Naruto University Of Education
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Nishimura Hiroshi
Institute Of Geological Sciences College Of General Education Osaka University
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