In order to clarify the transportation of floating sand in a sea sand mining area of the Seto Inland Sea, the sectional measurements of current and suspended sediment (
SS) were conducted with an Acoustic Doppler Current Profiler (ADCP) in the Mihara Seto Strait. The relationship between the backscatter strength (
Sv) of ADCP and the concentration of
SS had a high correlation. Then,
Sv could be converted into the concentration of
SS, and the flux of the
SS was estimated. In each section, the total flux of the
SS was calculated assuming that the tidal current was sinusoidal wave. As a result, the net of the flux of the
SS showed the inflow in the Mihara Seto Strait.
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