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Investigation of Local Scour in Cohesionless Sediments Using a Tunnel-Model
Two dimensional sand erosion tests in a closed water tunnel (velocities up to 2 m/s) produced a scour hole downstream a sill or a flat bottom protection, the slope of the scour hole being independent of flow velocity, partially dependent on scale and wholly dependent on grain size and gradation and sill geometry. The tractive forces of single grains and liquefaction are the mechanisms scour.
Investigation of Local Scour in Cohesionless Sediments Using a Tunnel-Model
Two dimensional sand erosion tests in a closed water tunnel (velocities up to 2 m/s) produced a scour hole downstream a sill or a flat bottom protection, the slope of the scour hole being independent of flow velocity, partially dependent on scale and wholly dependent on grain size and gradation and sill geometry. The tractive forces of single grains and liquefaction are the mechanisms scour.
Investigation of Local Scour in Cohesionless Sediments Using a Tunnel-Model
M. Buchko (Autor:in) / P. Kolkman (Autor:in) / K. Pilarczyk (Autor:in)
1988
14 pages
Report
Keine Angabe
Englisch
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