Hydrodynamic drag of a free-standing wall partially submerged in inundation flow was experimentally investigated in a natural river. A wall plate and sensors for measuring drag force, fluid velocity, and water depth were installed in a testing frame made of stainless steel. Regulator plates were immersed on the river bed in the up and down streams of the frame to provide a uniform and steady flow in the testing area. The drag coefficient
CD was significantly influenced by Froude number
Fr, but not by Reynolds number
Re in the ranges of 0.5<
Fr<2.0 and 4×10
4<
Re<4×10
5. The
CD had a minimum value slightly over 1.0 at around
Fr=1.0, and increased up to 2.0 with the changes of
Fr toward 0.5 and 2.0. The blockage ratio of the wall in the flume showed a large effect on the
CD for subcritical flow (
Fr<1.0), but little effect for supercritical flow (
Fr>1.0). With the decrease of incoming fluid depth, wave drag became predominant to form drag. The
Fr-based formula for estimating
CD, i.e.,
CD=1.0+
Fr2/4, is conservatively suitable to test data for
Fr>1.0, but is radical or of underestimation for
Fr<1.0 due to the blockage effect.
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