| Project/Area Number |
09555157
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| Research Category |
Grant-in-Aid for Scientific Research (B)
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| Allocation Type | Single-year Grants |
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| Section | 展開研究 |
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| Research Field |
水工水理学
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| Research Institution | KYOTO UNIVERSITY |
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Principal Investigator |
YAMASHITA Takao Kyoto Univ., Dis.Prev.Res.Inst., Assoc.Prof., 防災研究所, 助教授 (30111983)
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| Co-Investigator(Kenkyū-buntansha) |
SERIZAWA Shigeatsu Kyoto Univ., Dis.Prev.Res.Inst., Res.Associate, 防災研究所, 助手 (70301249)
MASE Hajime Kyoto Univ., Dis.Prev.Res.Inst., Assoc.Prof., 防災研究所, 助教授 (30127138)
YOSHIOKA Hiroshi Kyoto Univ., Dis.Prev.Res.Inst., Res.Associate, 防災研究所, 助手 (10027287)
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| Project Period (FY) |
1997 – 1998
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| Project Status |
Completed (Fiscal Year 1998)
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| Budget Amount *help |
¥3,400,000 (Direct Cost: ¥3,400,000)
Fiscal Year 1998: ¥3,400,000 (Direct Cost: ¥3,400,000)
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| Keywords | nerashore current / surf zone / ADCP / suspended sediment / sediment transport |
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| Research Abstract |
Beach erosion due to offshore-going sediment transport is a serious problem in Japan's coasts facing the Japan Sea. It has hot yet been made clear the mechanism of sediment transport offshore. The main aim of this study is to unveil the nearshore current structure in the surf zone by ADCP observation with the T-shaped Observation Pier(TOP), on the Ogata Coast, Niigata. Prefecture.
From the observation, we estimated current characteristics as :
(1) Velicity Profile : When the longshore currents become strong due to oblique winds and waves, intensity of the offshore currents becomes weak with undertow-like velocity profile are formed. Velocity profiles of both longshore and offshore currents are almost uniform below the wave trough level.
(2) Longshore Currents : Strong and uniform longshore currents are generated in the surf zone by oblique winds and waves. Its direction well responds to changes in wind direction, ex. westerly wind excites east word longshore currents and vice versa.
(3) Off-Shore Currents : Almost all current below the wave trough direct offshore in the surf zone. When wind and wave direction changed, W(westward) -> NW(shore-normal) ->N (eastward), the typical wind evolution pattern in this coast, strong offshore currents are observed in the shore-normal wind phase.
(4) Wind Drag Coefficient near the surf zone : Wind drag coefficient near extremely shallow and high wave condition including wave breaking is derived by using Turbulent Dissipation Method (TDM), as shown in Fig.3. The fitting curve is
Cd=0.0223 exp(10/3)**(-U/15) when U(10m)> 10m/s.
(5) Turbidity concentration vs Echo intensity of ADCP : under analyzing.
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