1992
DOI: 10.1299/kikaib.58.1990
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Basic Study on Scour around Bridge Piers and Its Prevention.

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“…The same tendency was observed in Cases 2 and 7, where the water level history was iterated using Type 1 model. In summary, when the local scouring progresses under the condition of iterated rise and fall of the water level for Type 1 model, a deep zone of the local scour hole, which has a slope gradient similar to the repose angle in water, is formed as an inverted cone affected by downflow due to the horseshoe-shaped eddies around the bridge piers, as reported in previous studies, until the maximum local scour depth reaches the equilibrium state [27][28][29]. After the maximum scouring depth reaches the equilibrium state, the top soil layer in the local scour hole, which has a slope gradient smaller than the repose angle in water, is scoured away by the scouring force of the water flowing into the local scour hole, and the erosion phenomenon progresses.…”
Section: Type 1 Modelmentioning
confidence: 87%
“…The same tendency was observed in Cases 2 and 7, where the water level history was iterated using Type 1 model. In summary, when the local scouring progresses under the condition of iterated rise and fall of the water level for Type 1 model, a deep zone of the local scour hole, which has a slope gradient similar to the repose angle in water, is formed as an inverted cone affected by downflow due to the horseshoe-shaped eddies around the bridge piers, as reported in previous studies, until the maximum local scour depth reaches the equilibrium state [27][28][29]. After the maximum scouring depth reaches the equilibrium state, the top soil layer in the local scour hole, which has a slope gradient smaller than the repose angle in water, is scoured away by the scouring force of the water flowing into the local scour hole, and the erosion phenomenon progresses.…”
Section: Type 1 Modelmentioning
confidence: 87%