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Published byBertram Chapman Modified over 9 years ago
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EVALUATING SELECTED SCOUR EQUATIONS FOR BRIDGE PIERS IN COARSE STREAMBEDS IN NEW YORK L.J. Welch, Jr. and G.K. Butch In cooperation with New York State Department of Transportation by
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Field Conditions Turbulent flow Armored streambed
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Scour is the result of work Sf= stream force (kg m/s 2 ); D 84 = grain size >84 % of armor layer (mm).
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Stream Force Sf= stream force (kg m/s 2 ); = water density (10 3 kg/m 3 ); y 1 = water depth (m); w= flow width (1 m); V 0 = flow velocity (m/s).
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Database Statistics
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Model Calibration Calculated 19 scour depths measured in 1996 (10 = 0.0 m) 1996 MEAN ERROR MEAN ERROR (m)
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New York Equation (1972-96). Sf = stream force (kg m/s 2 ); D 84 =grain size >84 % of armor layer (mm).
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Relation of Scour Depth to Stream Force and Bed Material
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Sensitivity Analysis
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FHWA Equation y s = scour depth; K 1 = pier-nose shape; a = pier width; K 2 = pier shape & flow alignment; y 1 = water depth; K 3 = streambed condition; Fr 1 = Froude number; K 4 = armoring by bed-material size.,
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K 4 (modified by Mueller) If D 50 > 2 mm and D 95 > 20 mm and f(V) > 0, otherwise K 4 = 1 D 50 = median grain size; D 95 = grain size >95 percent of armor layer; V 0 = approach flow velocity; V / cD 50 = approach velocity corresponding to critical velocity at pier for D 50 ; V / cD 95 = approach velocity corresponding to critical velocity at pier for D 95 ; V cD 50 = critical velocity for incipient motion for D 50.,
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Froehlich Equation y s = scour depth; = pier shape; g= gravity; V 0 = flow velocity; y 0 = water depth; b= pier width; D 50 = median grain size.
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Estimated Scour vs Measured Scour
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Summary of Estimated and Measured Scour
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New Hampshire Study Field measurements
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New Hampshire Study GPR & fixed instruments
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SUMMARY New York equation: - scour a function of stream force and bed material - derived from field measurements - alternative for coarse streambeds - estimates associated with specific peak discharges Mueller modified-K 4 and Froehlich equations: - less error than FHWA equation in New York study
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