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Item
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THE ROLE OF STEADY STREAMING IN SHEETFLOW TRANSPORT
http://hdl.handle.net/20.500.12678/0000007222
http://hdl.handle.net/20.500.12678/000000722248ae07a9-0da7-4d21-991a-01eafcec1059
3d8a87c0-29c8-4843-ab6c-7e4ad8976c5b
Name / File | License | Actions |
---|---|---|
![]() |
Publication type | ||||||
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Conference paper | ||||||
Upload type | ||||||
Publication | ||||||
Title | ||||||
Title | THE ROLE OF STEADY STREAMING IN SHEETFLOW TRANSPORT | |||||
Language | en | |||||
Authors | ||||||
KYI KYI LWIN | ||||||
HAIJIANG LIU | ||||||
SHINJI SATO | ||||||
Description | ||||||
To quantitatively evaluate the role of the onshore streaming, laboratory experiments were conducted under the combined asymmetric wave-current conditions. The asymmetric flows with a wave period of 5 s and a maximum onshore velocity umax varying from 0.8 to 1.6 m/s have been applied for three well-sorted sands with different medium sand sizes. The sediment net transport rate was measured. Results show that except several cases, the onshore streaming enhanced the onshore sheetflow net transport by different extents. The streaminginduced net transport rate is found to be related to the free-stream velocity and the sand size. | ||||||
Conference papers | ||||||
APAC 2011 | ||||||
December 14 – 16, 2011 | ||||||
Proceedings of the Sixth International Conference on Asian and Pacific Coasts | ||||||
Hong Kong, China |