Pore-water pressure distribution of solid-water phase flow in a rolling mill
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- HOTTA Norifumi
- 東京大学大学院農学生命科学研究科
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- MIYAMOTO Kuniaki
- 鳥取大学地域共同研究センター
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- SUZUKI Masakazu
- 東京大学大学院農学生命科学研究科
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- OHTA Takehiko
- 東京大学大学院農学生命科学研究科
Bibliographic Information
- Other Title
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- 回転円筒水路を用いた高濃度固液混相流における間隙水圧分布の測定
- カイテン エントウ スイロ オ モチイタ コウ ノウド コエキ コンソウリュウ
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Abstract
Pore-water pressure distribution of a solid-water phase flow, that is difficult to measure in an open channel, was measured in a rolling mill. The result confirmed that pore-water pressure was higher than the hydrostatic pressure supposed to exist so far.<br>Theoretically, the gradient of excess pore-water pressure from hydrostatic pressure, dpf /dy, is proportional to the square of the particle diameter, d, and is known as Reynolds stress. The results of the experiments were consistent with the above theory in characteristics and value for large d, but not for small d. The difference between theory and the results of experiments for small d was caused by infiltration flow which occurred due to the characteristics of the rolling mill. In this case, the dpf /dy was inversely proportional to the square of d based on Darcy's law.
Journal
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- Sabo Gakkaishi
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Sabo Gakkaishi 50 (6), 11-16, 1998
Japan Society of Erosion Control Engineering
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Details 詳細情報について
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- CRID
- 1390282679044821632
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- NII Article ID
- 10007512363
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- NII Book ID
- AN0012035X
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- NDL BIB ID
- 4425361
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- ISSN
- 02868385
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- Data Source
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- JaLC
- NDL
- CiNii Articles
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- Abstract License Flag
- Disallowed