2026-08-25T09:16:58Z https://meral.edu.mm/oai

oai:meral.edu.mm:recid/00007222 2022-03-24T23:14:26Z 1608151108672:1608152148040 user-mmu

THE ROLE OF STEADY STREAMING IN SHEETFLOW TRANSPORT KYI KYI LWIN HAIJIANG LIU SHINJI SATO 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. http://hdl.handle.net/20.500.12678/0000007222 https://meral.edu.mm/records/7222