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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.

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Presentation on theme: "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."— Presentation transcript:

1 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

2 Field Conditions Turbulent flow Armored streambed

3 Scour is the result of work Sf= stream force (kg  m/s 2 ); D 84 = grain size >84 % of armor layer (mm).

4 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).

5 Database Statistics

6 Model Calibration Calculated 19 scour depths measured in 1996 (10 = 0.0 m) 1996 MEAN ERROR MEAN ERROR (m)

7 New York Equation (1972-96). Sf = stream force (kg  m/s 2 ); D 84 =grain size >84 % of armor layer (mm).

8 Relation of Scour Depth to Stream Force and Bed Material

9 Sensitivity Analysis

10 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.,

11 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.,

12 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.

13 Estimated Scour vs Measured Scour

14 Summary of Estimated and Measured Scour

15 New Hampshire Study Field measurements

16 New Hampshire Study GPR & fixed instruments

17 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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