Estimating Scour. CIVE 510 October 21 st, 2008

Size: px

Start display at page:

Download "Estimating Scour. CIVE 510 October 21 st, 2008"

Kellie Cassandra O’Neal’
6 years ago
Views:

1 Estimating Scour CIVE 510 October 21 st,

2 Causes of Scour 2

3 Site Stability 3

4 Mass Failure Downward movement of large and intact masses of soil and rock Occurs when weight on slope exceeds the shear strength of bank material Typically a result of water saturating a slide-prone slope Rapid draw down Flood stage manipulation Tidal effects Seepage 4

5 Mass Failure Rotational Slide Concave failure plane, typically on slopes ranging from degrees 5

6 Translational Slide Mass Failure Shallower slide, typically along well-defined plane 6

7 Site Stability 7

8 Toe Erosion Occurs when particles are removed from the bed/bank whereby undermining the channel toe Results in gravity collapse or sliding of layers Typically a result of: Reduced vegetative bank structure Smoothed channels, i.e., roughness removed Flow through a bend 8

9 Toe Erosion 9

10 Toe Erosion 10

11 Site Stability 11

12 Avulsion and Chute Cutoffs Abrupt change in channel alignment resulting in a new channel within the floodplain Typically caused by: Concentrated overland flow Headcutting and/or scouring within floodplain Manmade disturbances Chute cutoff smaller scale than avulsion 12

13 Avulsion and Chute Cutoffs 13

14 Site Stability 14

15 Subsurface Entrainment Piping occurs when subsurface flow transports soil particles resulting in the development of a tunnel. Tunnels reduce soil cohesion causing slippage and ultimately streambank erosion. Typically caused by: Groundwater seepage Water level changes 15

16 Subsurface Entrainment 16

17 Groundwater table Normal water level Seepage flow Normal (baseflow( baseflow) ) conditions

18 Flood water level Seepage flow During flood peak

19 Area of high seepage gradients and uplift pressure Seepage flow Normal water level After flood recession

20 Site Stability 20

21 Scour Erosion at a specific location that is greater than erosion found at other nearby locations of the stream bed or bank. Simons and Sentruk (1992) 21

22 Scour Scour depths needed for: Revetment design Drop structures Highway structures Foundation design Anchoring systems Habitat enhancement 22

23 Scour Equations All empirical relationships Specific to scour type Designed for and with sand-bed systems May distinguish between live-bed and clear-water conditions Modifications for gravel-bed systems 23

24 Calculating Scour Identify type(s) of expected scour Calculate depth for each type Account for cumulative effect Compare to any know conditions 24

25 5 Types of Scour Bend scour Constriction scour Drop/weir scour Jet scour Local scour 25

26 Bend Scour 26

27 Bend Scour Caused by secondary currents Material removed from toe Field observations can be helpful in assessing magnitude Conservative first estimate: Equal to the flow depth upstream of bend Three empirical relationships 27

28 Bend Scour Three methods Thorne (1997) Flume and river experiments D 50 bed from 0.3 to 63 mm Applicable to gravel bed systems Maynord (1996) Used for sand-bed channels Provides conservative estimate for gravel-bed systems Wattanabe (Maynord 1996) Ditto 28

29 Thorne Equation d 1.07 log R c = 2 y W 1 Where d = maximum depth of scour (L) y 1 = average flow depth directly upstream of the bend (L) W = width of flow (L) R c = radius of curvature (L) R c 2< < 22 W 29

30 Maynord Equation D R W mb = c D W D u u Where D mb = maximum water depth in bend (L) D u = mean channel depth at upstream crossing (L) W = width of flow at upstream end of bend (L) R c = radius of curvature (L) R c W < < 1.5 < < W Du 30

31 Maynord Equation D R W mb = c D W D u u Notes: Developed from measured data on 215 sand bed channels Flow events between 1 and 5 year return intervals Not valid for overbank flows that exceed 20 percent of channel depth Equation is a best fit, not an envelope NO FOS Factor of safety of 1.08 is recommended English or metric units Width is that of active flow 31

32 Wattanabe Equation d s D W = α + β Rc Where d s = scour depth below maximum depth in bend (L) W = channel top width (L) R c = radius of curvature (L) D = mean channel depth (L) S = bed slope (L/L) f = Darcy friction factor α = X X X WS = log 10 D 2 β = π x f 1 x = f 1.42 sinσ + cosσ f σ tan = 1.5 f 1.42 f 32

33 Wattanabe Equation d s D α β W = + Rc Notes: Results correlated will with Mississippi River data Limits of application are unknown FOS of 1.2 is recommended English or metric units may be used 33

34 5 Types of Scour Bend scour Constriction scour Drop/weir scour Jet scour Local scour 34

35 Constriction Scour 35

36 Constriction Scour Occurs when channel features created a narrowing of the channel Typically, constriction is harder than the channel banks or bed Caused from natural and/or engineered features Large woody debris Bridge crossings Bedrock Flow training structures Tree roots/established vegetation 36

37 Constriction Scour Scour equations Developed from flume tests of bridge abutments Equations can be applied for natural or other induced constrictions Most accepted methods: Laursen live-bed equation (1980) Laursen clear-water equation (1980) 37

38 Constriction Scour Live-bed conditions Coarse sediments may armor the bed Compare with clear-water depth and use lower value Requires good judgment! Equation developed for sand-bed streams Application to gravel bed: Provides conservative estimate of scour depth 38

39 Laursen Live-Bed Equation y 2 Q 2 W 1 = y1 Q1 W2 d = y y A Where d = average depth of constriction scour (L) y 0 = average depth of flow in constricted reach without scour (L) y 1 = average depth of flow in upstream main channel (L) y 2 = average depth of flow in constricted reach after scour (L) Q 2 = flow in constricted section (L 3 /T) Q 1 = flow in upstream channel (L 3 /T) W 1 = bottom width in approach channel (L) W 2 = bottom width in constricted section (L) A = regression exponent 39

40 Laursen Live-Bed Equation y 2 Q 2 W 1 = y1 Q1 W2 d = y y A ω = fall velocity of D50 bed material (L/T) U* = shear velocity (L/T) = (gy 1 S e ) 0.5 g = acceleration due to gravity (L/T 2 ) S e = EGL slope in main channel (L/L) U*/ω < 0.5 A 0.59 Mode of bed Transport Bed 0.5 to Suspended > Suspended 40

41 Laursen Live-Bed Equation 41

42 Laursen Live-Bed Equation y 2 Q 2 W 1 = y1 Q1 W2 d = y y A Notes: Assumes all flow passes through constricted reach Coarse sediment may limit live-bed scour If bed is armored, compare with at clearwater scour Both English and metric units can be used 42

43 Laursen Clear-Water Equation Where 2 Q 2 y2 = CDm W2 d = y y d = average depth of constriction scour (L) y 0 = average depth of flow in constricted reach without scour (L) y 2 = average depth of flow in constricted reach after scour (L) Q 2 = flow in constricted section (L 3 /T) D m = 1.25D50 = assumed diameter of smallest non-transportable particle in bed material in constricted reach (L) W 2 = bottom width in constricted section (L) C = unit constant; 120 for English, 40 for metric 43

44 Laursen Clear-Water Equation Notes: y Q CD 0.67 W 2 m 2 = d = y y Only uses flow through constricted section If constriction has an overbank, separate computation made for the channel and each overbank Can be used for gravel bed systems Armoring analysis or movement by size fraction 44

45 5 Types of Scour Bend scour Constriction scour Drop/weir scour Jet scour Local scour 17 OCT address mistake on equation two slides ago 45

46 Drop/Weir Scour 46

47 Drop/Weir Scour Result of roller formed by cascading flow Caused from Perched culverts Culverts under pressure flow Spillway exits Natural drops in high-gradient mountain streams 47

48 Drop/Weir Scour Two methods U.S. Bureau of Reclamation Equation Vertical Drop Structure (1995) Used for scour estimation immediately downstream of a vertical drop Provides conservative estimate for sloping sills Laursen and Flick (1983) Sloping sills of rock or natural material 48

49 USBR Vertical Drop Equation = s t m d KH q d Where d s = scour depth immediately downstream of drop (m) q = unit discharge (m 3 /s/m) H t = total drop in head, measured from the upstream to downstream energy grade line (m) d m = tailwater depth immediately downstream of scour hole (m) K = regression constant of

50 USBR Vertical Drop Equation = s t m d KH q d Notes: Calculated scour depth is independent of bed-material grain size If large material is present, it may take decades for scour to reach final depth Must use metric units 50

51 Laursen and Flick Equation y R d = 4 3 y d c 50 s c m D50 yc Where d s = scour depth immediately downstream of drop (L) y c = critical flow depth (L) D 50 = median grain size of bed material (L) R 50 = median grain size of sloping sill (L) d m = tailwater depth immediately downstream of scour hole (L) 51

52 Laursen and Flick Equation y R d = 4 3 y d c 50 s c m D50 yc Notes Developed specifically for sloping sills constructed of rock Non-Conservative for other applications Can use English or metric units 52

53 5 Types of Scour Bend scour Constriction scour Drop/weir scour Jet scour Local scour 53

54 Jet Scour 54

55 Jet Scour Lateral bars Sub-channel formation 55

56 Jet Scour High energy side channel or tributary discharges 56

57 Jet Scour Tight radius of curvature 57

58 Jet Scour Very difficult problem to solve Simons and Senturk (1992) provide some guidance Good case for adding a substantial FOS 58

59 Jet Scour 59

60 Jet Scour 60

61 Jet Scour 61

62 5 Types of Scour Bend scour Constriction scour Drop/weir scour Jet scour Local scour 62

63 Local Scour 63

64 Local Scour Appears as tight scallops along a bank-line Depressions in a channel bed Generated by flow patterns around an object or obstruction Extent varies with obstruction Can be objective of design 64

65 Local Scour Pier Scour Equations 65

66 Local Scour Pier Scour Equations Developed for sand-bed rivers Provides conservative estimate for gravel-bed systems Can be applied to other obstructions Assumes object extends above water surface Colorado State University Equation 66

67 Local Scour Colorado State University Equation Can be applied to both live-bed and clear-water conditions Provides correction factor for bed material > 6 cm gravel beds Field verification shows equation to be conservative 67

68 CSU Pier Scour Equation d y y b = 2.0K KKK Fr 0.43 Where d = maximum depth of scour, measured below bed elevation (m) y 1 = flow depth directly upstream of pier (m) b = pier width (m) F r = approach Froude number K 1 K 4 = correction factors 68

69 CSU Pier Scour Equation d y y b = 2.0K KKK Fr K 1 = correction factor for pier nose shape

70 CSU Pier Scour Equation d y y b = 2.0K KKK Fr 0.43 K 1 = correction factor for pier nose shape For angle of attach > 5 o, K 1 = 1.0 For angle of attach 5 o Square nose K 1 = 1.1 Circular K 1 = 1.0 Group of cylinders K 1 = 1.0 Sharp nose K 1 =

71 CSU Pier Scour Equation d y y b = 2.0K KKK Fr 0.43 K 2 = correction factor for angle of attach of flow L K2 = Cosθ + Sinθ b Where L = length of pier (along flow line of angle of attach) (m) b = pier width (m) Θ = angle of attach (degrees)

72 CSU Pier Scour Equation d y y b = 2.0K KKK Fr 0.43 K 2 = correction factor for angle of attach of flow Θ L/b = 4 L/b = 8 L/b =

73 CSU Pier Scour Equation d y y1 K 3 = correction factor for bed conditions Selected for type and size of dunes Use 1.1 for gravel-bed rivers 0.65 b = 2.0K KKK Fr

74 CSU Pier Scour Equation d y y b = 2.0K KKK Fr K 3 = correction factor for bed conditions 0.43 Bed Condition clear water scour plane bed/anti-dune small dunes medium dunes large dunes Dune Height (m) n/a n/a 0.6 to 3 3 to 9 >9 K

75 CSU Pier Scour Equation d y y1 K 4 = correction factor for armoring of bed material K 4 varies between 0.7 and 1.0 K 4 = 1.0 for D 50 < 60 mm, or for V r > 1.0 K 4 = [1 0.89(1-V r ) 2 ] 0.5, for D 50 > 60 mm 0.65 b = 2.0K KKK Fr 0.43 V r = V ( ) V ( ) c90 V i V i V i D 0.65 b 50 = V c50 V = 6.19 y D c 1/6 1/3 1 c 75

76 V r = CSU Pier Scour Equation V ( ) V ( ) c90 V i V i d y y b = 2.0K KKK Fr V i D 0.65 b 50 = V c V = 6.19 y D c 1/6 1/3 1 c Where V = approach velocity (m/s) V r = velocity ratio V i = approach velocity when particles at pier begin to move (m/s) V c90 = critical velocity for D 90 bed material size (m/s) V c50 = critical velocity for D 50 bed material size (m/s) Y 1 = flow depth upstream of pier (m) D c = particle size selected to compute V c (m) 76

77 CSU Pier Scour Equation d y y b = 2.0K KKK Fr 0.43 Where d = maximum depth of scour, measured below bed elevation (m) y 1 = flow depth directly upstream of pier (m) b = pier width (m) F r = approach Froude number K 1 K 4 = correction factors 77

78 Local Scour Abutment scour 78

79 Local Scour Abutment scour Developed for sand-bed systems Provides conservative estimate for gravel-bed systems Can be applied to other obstructions Results can be reduced based on experience Froelich Equation 79

80 Local Scour Froehlich Equation Predicts scour as a function of shape, angle with respect to flow, length normal to flow and approach flow conditions Provides conservative estimate for gravel-bed systems Can be applied to other obstructions Assumes object extends above water surface 80

81 Froehlich Equation for Live- Bed Scour at Abutments d y 0.43 L' KK 1 2 Fr 1.0 = + y Where d = maximum depth of scour, measured below bed elevation (m) y = flow depth at abutment (m) F r = approach Froude number L = length of abutment projected normal to flow (m) K 1 K 2 = correction factors 81

82 Froehlich Equation for Live- Bed Scour at Abutments d y 0.43 L' = KK F r y L = length of abutment projected normal to flow (m) θ 82

83 Froehlich Equation d y 0.43 L' KK 1 2 Fr 1.0 = + y K 1 = correction factor for abutment shape K 1 = 1.0 for vertical abutment K 1 = 0.82 for vertical abutment with wing walls K 1 = 0.55 for spill through abutments 83

84 Froehlich Equation d y 0.43 L' KK 1 2 Fr 1.0 = + y K 2 = correction factor for angle of embankment to flow θ 84

85 Froehlich Equation d y 0.43 L' KK 1 2 Fr 1.0 = + y K 2 = correction factor for angle of embankment to flow 0.13 Where = angle between channel bank and abutment is > 90 degrees of embankment points upstream is < 90 degrees if embankment points downstream K 2 θ = 90 85

86 Check Method U.S. Bureau of Reclamation 86

87 Check Method U.S. Bureau of Reclamation Provides method to compute scour at: Channel bends Piers Grade-control structures Vertical rock banks or walls May not be as conservative as previous approaches 87

88 Check Method U.S. Bureau of Reclamation Computes scour depth by applying an adjustment to the average of three regime equations Neil equation (1973) Modified Lacey Equation (1930) Blench equation (1969) 88

89 Neil Equation y n q = y d bf q bf m Where y n = scour depth below design flow level (L) y bf = average bank-full flow depth (L) q d = design flow discharge per unit width (L 2 /T) q bf = bankfull flow discharge per unit width (L 2 /T) m = exponent varying from 0.67 for sand and 0.85 for coarse gravel 89

90 Neil Equation y n q = y d bf q bf m Obtain field measurements of an incised reach Compute bank-full discharge and associated hydraulics Determine scour depth 90

91 Modified Lacey Equation y L Q = 0.47 f 3.3 Where y L = mean depth at design discharge (L) Q = design discharge (L 3 /T) f = Lacey s silt factor = 1.76 D D 50 = median size of bed material (must be in mm!) 91

92 Blench Equation y B = q F 0.67 d 0.33 bo Where y B = depth for zero bed sediment transport (L) q d = design discharge per unit width (L 2 /T) F bo = Blench s zero bed factor 92

93 Blench Equation y B = q F 0.67 d 0.33 bo F bo = Blench s zero bed factor 93

94 Check Method U.S. Bureau of Reclamation Computes scour depth by applying an adjustment to the average of three regime equations Neil equation (1973) Modified Lacey Equation (1930) Blench equation (1969) Adjust as follows 94

95 Check Method U.S. Bureau of Reclamation d d d = N N N = K y L L L = K y K y B b B Where d N, d L, d B = depth of scour from Neil, Lacey and Blench equations, respectively K N, K L, K B = adjustment coefficients for each equation 95

96 Check Method U.S. Bureau of Reclamation K N, K L, K B Condition Neil-K N Lacey-K L Blench-K B Bend Scour Straight reach (wandering thalweg) Moderate bend Severe bend Right-angle bend Vertical rock bank or wall Nose of Piers Small dam or grade control

97 Check Method U.S. Bureau of Reclamation d d d = N N N = K y L L L = K y K y B b B Average values and compare to results of previous methods Appropriate level of conservatism?? 97

98 REFERENCES 1. Lane, E.W Design of stable channels. Transactions of the American Society of Civil Engineers. 120: U.S. Department of Transportation, Federal Highway Administration Design of Roadside Channel with Flexable Linings. Hydraulic Engineering Circular No. 15. Publication No. FHWA-IP Richardson, E.V. and S.R. Davis. U.S. Department of Transportation, Federal Highway Administration, Evaluating Scour at Bridges, Hydraulic Engineering Circular No. 18. Publication No. FHWA-IP U.S. Department of Transportation, Federal Highway Administration Highways in the River Environment. 5. Thorne, C.R., R.D. Hey and M.D. Newson Applied Fluvial Geomorphology for River Engineering and Management. John Wiley and Sons, Inc. New York, N.Y. 98

99 REFERENCES 6. Maynord, S Toe Scour Estimation on Stabilized Bendways. Journal of Hydraulic Engineering, American Society of Civil Engineers, Vol. 122, No U.S. Department of Transportation, Federal Highway Administration. 1955a. Stream Stability at Highway Structures. Hydraulic Engineering Circular No Laursen, E.M. and Flick, M.W Final Report, Predicting Scour at Bridges: Questions Not Fully Answered Scour at Sill Structures, Report ATTI-83-6, Arizona Department of Transportation. 9. Simons, D.B and Senturk, F Sediemnt Transport Technology, Water Resources Publications, Littleton, CO. 10. Bureau of Reclamation, Sediment and River Hydraulics Section Computing Degradation and Local Scour, Technical Guideline for Bureau of Reclamation, Denver, CO. 99

A STUDY OF LOCAL SCOUR AT BRIDGE PIERS OF EL-MINIA

A STUDY OF LOCAL SCOUR AT BRIDGE PIERS OF EL-MINIA Dr. Gamal A. Sallam 1 and Dr. Medhat Aziz 2 ABSTRACT Bridges are critical structures that require a substantial investment to construct and serve an important