rip-rap summary.pdf · hec-11 method •psheuibdl by fhwa in 1989 • combination of theory and...
TRANSCRIPT
![Page 1: RIP-RAP Summary.pdf · HEC-11 Method •Psheuibdl by FHWA in 1989 • Combination of theory and field observations • Use in rivers and streams with: – Discharges greater than](https://reader031.vdocument.in/reader031/viewer/2022030410/5a9b781a7f8b9ab6188dd3e8/html5/thumbnails/1.jpg)
RIP-RAPEquation Selection and
Rock Sizing
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![Page 3: RIP-RAP Summary.pdf · HEC-11 Method •Psheuibdl by FHWA in 1989 • Combination of theory and field observations • Use in rivers and streams with: – Discharges greater than](https://reader031.vdocument.in/reader031/viewer/2022030410/5a9b781a7f8b9ab6188dd3e8/html5/thumbnails/3.jpg)
Common Rock Sizing Relations
• HEC-11• USACE• Isbash• CALTRANS• USBR• ASCE• USGS
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DEVELOPMENT OF RELATIONSHIPS
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Common Rock Sizing Relations
• HEC-11• USACE• Isbash• CALTRANS• USBR• ASCE• USGS
![Page 6: RIP-RAP Summary.pdf · HEC-11 Method •Psheuibdl by FHWA in 1989 • Combination of theory and field observations • Use in rivers and streams with: – Discharges greater than](https://reader031.vdocument.in/reader031/viewer/2022030410/5a9b781a7f8b9ab6188dd3e8/html5/thumbnails/6.jpg)
HEC-11 Method
• Published by FHWA in 1989• Combination of theory and field
observations• Use in rivers and streams with:
– Discharges greater than 50 cfs– Uniform or gradually varied flow conditions– Straight or mildly curving reaches– Uniform cross section geometry
![Page 7: RIP-RAP Summary.pdf · HEC-11 Method •Psheuibdl by FHWA in 1989 • Combination of theory and field observations • Use in rivers and streams with: – Discharges greater than](https://reader031.vdocument.in/reader031/viewer/2022030410/5a9b781a7f8b9ab6188dd3e8/html5/thumbnails/7.jpg)
HEC-11 Method
D50 = C s CsfD50 = C s Csf
11.5Kd
3a0.001V
1.5Kd
3a0.001V
1.5Kd
3a0.001V
![Page 8: RIP-RAP Summary.pdf · HEC-11 Method •Psheuibdl by FHWA in 1989 • Combination of theory and field observations • Use in rivers and streams with: – Discharges greater than](https://reader031.vdocument.in/reader031/viewer/2022030410/5a9b781a7f8b9ab6188dd3e8/html5/thumbnails/8.jpg)
HEC-11 Method
Where:
D50 = stone size (ft)Cs = (2.12 / (Gs-1)1.5)Csf = (SF / 1.2)(1.5)
Va = average channel velocity (ft/s)d = average flow depth (ft)K1 = [ 1 – (sin2(θ) / sin2(Φ))](1/2)
D50 = C s CsfD50 = C s Csf
11.5Kd
3a0.001V
1.5Kd
3a0.001V
1.5Kd
3a0.001V
![Page 9: RIP-RAP Summary.pdf · HEC-11 Method •Psheuibdl by FHWA in 1989 • Combination of theory and field observations • Use in rivers and streams with: – Discharges greater than](https://reader031.vdocument.in/reader031/viewer/2022030410/5a9b781a7f8b9ab6188dd3e8/html5/thumbnails/9.jpg)
HEC-11 Method
• Used field observations to verify theoretical approach– Water surface slope 0.00006 – 0.0162– Maximum flow depths 4.8 – 48.5 ft– Average velocities 2.4 – 12.5 fps– Channel discharges 1,270 – 76,300 cfs– D50 range 0.5 – 2.3 ft
D50 = Cs CsfD50 = Cs Csf11.5Kd
3a0.001V1.5Kd
3a0.001V1.5Kd
3a0.001V
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HEC-11 Method
• Provides guidance for SF selection– For varying (R/W) ratios
• SF = 1 - 1.2 for R/W > 30• SF = 1.3 - 1.6 for 10 < R/W < 30• SF = 1.6 – 2 for R/W < 10
D50 = Cs CsfD50 = Cs Csf11.5Kd
3a0.001V1.5Kd
3a0.001V1.5Kd
3a0.001V 5.1
2.1_
⎟⎠⎞
⎜⎝⎛=
factorsafetyC f
![Page 11: RIP-RAP Summary.pdf · HEC-11 Method •Psheuibdl by FHWA in 1989 • Combination of theory and field observations • Use in rivers and streams with: – Discharges greater than](https://reader031.vdocument.in/reader031/viewer/2022030410/5a9b781a7f8b9ab6188dd3e8/html5/thumbnails/11.jpg)
HEC-11 Method
• Provides guidance for SF selection– For varying flow conditions
• SF = 1 - 1.2 for uniform flow, no impact from wave or floating debris and complete certainty in design parameters
• SF = 1.3 - 1.6 for gradually varying flow with moderate impact from debris or waves
• SF = 1.6 – 2 for rapidly varying or turbulent flow, significant impact from debris or ice and wave heights up to 2 feet.
D50 = Cs CsfD50 = Cs Csf11.5Kd
3a0.001V1.5Kd
3a0.001V1.5Kd
3a0.001V 5.1
2.1_
⎟⎠⎞
⎜⎝⎛=
factorsafetyC f
![Page 12: RIP-RAP Summary.pdf · HEC-11 Method •Psheuibdl by FHWA in 1989 • Combination of theory and field observations • Use in rivers and streams with: – Discharges greater than](https://reader031.vdocument.in/reader031/viewer/2022030410/5a9b781a7f8b9ab6188dd3e8/html5/thumbnails/12.jpg)
Common Rock Sizing Relations
• HEC-11• USACE• Isbash• CALTRANS• USBR• ASCE• USGS
![Page 13: RIP-RAP Summary.pdf · HEC-11 Method •Psheuibdl by FHWA in 1989 • Combination of theory and field observations • Use in rivers and streams with: – Discharges greater than](https://reader031.vdocument.in/reader031/viewer/2022030410/5a9b781a7f8b9ab6188dd3e8/html5/thumbnails/13.jpg)
USACE Method
• Published in 1994 in EM-1601• Use in man-made or natural channels
with:– Low turbulence– Slopes less than 2%– Not immediately downstream of turbulent
areas
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USACE Method
2.5
gd1KV
0.5
wγsγwγdtCvCsCfS30D
⎟⎟⎟⎟⎟
⎠
⎞
⎜⎜⎜⎜⎜
⎝
⎛
⎟⎟⎟
⎠
⎞
⎜⎜⎜
⎝
⎛
−=
![Page 15: RIP-RAP Summary.pdf · HEC-11 Method •Psheuibdl by FHWA in 1989 • Combination of theory and field observations • Use in rivers and streams with: – Discharges greater than](https://reader031.vdocument.in/reader031/viewer/2022030410/5a9b781a7f8b9ab6188dd3e8/html5/thumbnails/15.jpg)
USACE Method2.5
gd1KV
0.5
wγsγwγdtCvCsCfS30D
⎟⎟⎟⎟⎟
⎠
⎞
⎜⎜⎜⎜⎜
⎝
⎛
⎟⎟⎟
⎠
⎞
⎜⎜⎜
⎝
⎛
−=
Where:
D30 = stone size (ft)Sf = safety factor (1.25)Cs = stability coefficient for incipient failure
0.3 for angular rockCv = vertical velocity distribution coefficient
1.0 for straight channels, inside bends1.283 – 0.2 log (R/W), outside bends
Ct = thickness coefficient1.0 for 1*D100 or 1.5*D50
![Page 16: RIP-RAP Summary.pdf · HEC-11 Method •Psheuibdl by FHWA in 1989 • Combination of theory and field observations • Use in rivers and streams with: – Discharges greater than](https://reader031.vdocument.in/reader031/viewer/2022030410/5a9b781a7f8b9ab6188dd3e8/html5/thumbnails/16.jpg)
USACE Method2.5
gd1KV
0.5
wγsγwγdtCvCsCfS30D
⎟⎟⎟⎟⎟
⎠
⎞
⎜⎜⎜⎜⎜
⎝
⎛
⎟⎟⎟
⎠
⎞
⎜⎜⎜
⎝
⎛
−=
Where:
d = local depth of flow (ft)s = unit weight of stone (lbs/ft3)W = unit weight of water (lbs/ft3)
V = local depth averaged velocity (ft/s)g = gravitational constant (ft/s2)K1 = side slope correction factor
1.0 for bottom riprap0.5
2sinθ2sin1⎟⎟⎟
⎠
⎞
⎜⎜⎜
⎝
⎛−
φ
![Page 17: RIP-RAP Summary.pdf · HEC-11 Method •Psheuibdl by FHWA in 1989 • Combination of theory and field observations • Use in rivers and streams with: – Discharges greater than](https://reader031.vdocument.in/reader031/viewer/2022030410/5a9b781a7f8b9ab6188dd3e8/html5/thumbnails/17.jpg)
USACE Method
• Method based on lab data from late 80’s– D50: 0.5 – 2.0 inches– Thickness: 0.75 – 2 inches– Average velocity: 0.6 – 6.6 ft/s– Discharge: 15 – 100 cfs– Bed slope: 0.00087 – 0.015– Max side slope: 1.5:1
• Verified with some field data
5.2
1
5.0
30 )( ⎟⎟
⎠
⎞
⎜⎜
⎝
⎛⎟⎟⎠
⎞⎜⎜⎝
⎛−
=gdK
VdCCCSDws
wtvsf γγ
γ
![Page 18: RIP-RAP Summary.pdf · HEC-11 Method •Psheuibdl by FHWA in 1989 • Combination of theory and field observations • Use in rivers and streams with: – Discharges greater than](https://reader031.vdocument.in/reader031/viewer/2022030410/5a9b781a7f8b9ab6188dd3e8/html5/thumbnails/18.jpg)
Common Rock Sizing Relations
• HEC-11• USACE• Isbash• CALTRANS• USBR• ASCE• USGS
![Page 19: RIP-RAP Summary.pdf · HEC-11 Method •Psheuibdl by FHWA in 1989 • Combination of theory and field observations • Use in rivers and streams with: – Discharges greater than](https://reader031.vdocument.in/reader031/viewer/2022030410/5a9b781a7f8b9ab6188dd3e8/html5/thumbnails/19.jpg)
ISBASH Method
• Developed by Isbash in 1936• Adopted by USACE in 1971• Developed for construction of dams by
placing rock in flowing water
![Page 20: RIP-RAP Summary.pdf · HEC-11 Method •Psheuibdl by FHWA in 1989 • Combination of theory and field observations • Use in rivers and streams with: – Discharges greater than](https://reader031.vdocument.in/reader031/viewer/2022030410/5a9b781a7f8b9ab6188dd3e8/html5/thumbnails/20.jpg)
ISBASH Method
( )1sG22gC
2aV
50D−
=
![Page 21: RIP-RAP Summary.pdf · HEC-11 Method •Psheuibdl by FHWA in 1989 • Combination of theory and field observations • Use in rivers and streams with: – Discharges greater than](https://reader031.vdocument.in/reader031/viewer/2022030410/5a9b781a7f8b9ab6188dd3e8/html5/thumbnails/21.jpg)
ISBASH Method
( )1sG22gC
2aV
50D−
=
Where:
D50 = stone size (ft)Va = average channel velocity (ft/s)Gs = specific gravity of stoneG = gravitational constant (ft/s2)C = 0.86 for high turbulence zones
1.20 for low turbulence zones
![Page 22: RIP-RAP Summary.pdf · HEC-11 Method •Psheuibdl by FHWA in 1989 • Combination of theory and field observations • Use in rivers and streams with: – Discharges greater than](https://reader031.vdocument.in/reader031/viewer/2022030410/5a9b781a7f8b9ab6188dd3e8/html5/thumbnails/22.jpg)
ISBASH Method
• Empirical values for C determined to be 0.86 for minimum velocity required to move stones
• Empirical values for C determined to be 1.20 for maximum velocity required to move stones
• Rock size ranged from 4.7 to 9.8 inches
( )1sG22gC
2aV
50D−
=
![Page 23: RIP-RAP Summary.pdf · HEC-11 Method •Psheuibdl by FHWA in 1989 • Combination of theory and field observations • Use in rivers and streams with: – Discharges greater than](https://reader031.vdocument.in/reader031/viewer/2022030410/5a9b781a7f8b9ab6188dd3e8/html5/thumbnails/23.jpg)
Common Rock Sizing Relations
• HEC-11• USACE• Isbash• CALTRANS• USBR• ASCE• USGS
![Page 24: RIP-RAP Summary.pdf · HEC-11 Method •Psheuibdl by FHWA in 1989 • Combination of theory and field observations • Use in rivers and streams with: – Discharges greater than](https://reader031.vdocument.in/reader031/viewer/2022030410/5a9b781a7f8b9ab6188dd3e8/html5/thumbnails/24.jpg)
CALTRANS Method
• Developed the California Bank and Shore Protection method to protect highway embankments
• Result of a study by the Joint Bank Protection Committee appointed in 1949
• Incorporated lab and field data• Recommends individually designed
layers of protection
![Page 25: RIP-RAP Summary.pdf · HEC-11 Method •Psheuibdl by FHWA in 1989 • Combination of theory and field observations • Use in rivers and streams with: – Discharges greater than](https://reader031.vdocument.in/reader031/viewer/2022030410/5a9b781a7f8b9ab6188dd3e8/html5/thumbnails/25.jpg)
CALTRANS Method
( ) ( )⎟⎟⎟⎟
⎠
⎞
⎜⎜⎜⎜
⎝
⎛
−−=
θρ3sin31sGsG60.00002V
33W
![Page 26: RIP-RAP Summary.pdf · HEC-11 Method •Psheuibdl by FHWA in 1989 • Combination of theory and field observations • Use in rivers and streams with: – Discharges greater than](https://reader031.vdocument.in/reader031/viewer/2022030410/5a9b781a7f8b9ab6188dd3e8/html5/thumbnails/26.jpg)
CALTRANS Method
( ) ( )⎟⎟⎟⎟
⎠
⎞
⎜⎜⎜⎜
⎝
⎛
−−=
θρ3sin31sGsG60.00002V
33W
Where:
W33 = minimum weight of outside stone (lbs)V = stream velocity at bank (ft/s)
4/3 Va for impinging flow2/3 Va for tangential flowVa = average channel velocity (ft/s)
= 700 for randomly placed rubble= bank angle (degrees)
Gs = specific gravity of stone
![Page 27: RIP-RAP Summary.pdf · HEC-11 Method •Psheuibdl by FHWA in 1989 • Combination of theory and field observations • Use in rivers and streams with: – Discharges greater than](https://reader031.vdocument.in/reader031/viewer/2022030410/5a9b781a7f8b9ab6188dd3e8/html5/thumbnails/27.jpg)
CALTRANS Method
• Face of slope revetment no steeper than 1.5:1
• Stone weight values tested:– 3 – 30.4 lbs for impinging flow– 1 – 950 lbs for tangential flow
• Velocities examined– Average velocity 4.5 – 24 fps– Impinging velocity 6 – 32 fps– Tangential velocity 3 – 16 fps
( ) ( )⎟⎟⎟⎟
⎠
⎞
⎜⎜⎜⎜
⎝
⎛
−−=
θρ3sin31sGsG60.00002V
33W
![Page 28: RIP-RAP Summary.pdf · HEC-11 Method •Psheuibdl by FHWA in 1989 • Combination of theory and field observations • Use in rivers and streams with: – Discharges greater than](https://reader031.vdocument.in/reader031/viewer/2022030410/5a9b781a7f8b9ab6188dd3e8/html5/thumbnails/28.jpg)
Common Rock Sizing Relations
• HEC-11• USACE• Isbash• CALTRANS• USBR• ASCE• USGS
![Page 29: RIP-RAP Summary.pdf · HEC-11 Method •Psheuibdl by FHWA in 1989 • Combination of theory and field observations • Use in rivers and streams with: – Discharges greater than](https://reader031.vdocument.in/reader031/viewer/2022030410/5a9b781a7f8b9ab6188dd3e8/html5/thumbnails/29.jpg)
USBR Method
• Developed by Peterka and published in EM-25 in 1958
• Developed for estimating rock size for use downstream of stilling basins
• Procedure based on prototype installations
![Page 30: RIP-RAP Summary.pdf · HEC-11 Method •Psheuibdl by FHWA in 1989 • Combination of theory and field observations • Use in rivers and streams with: – Discharges greater than](https://reader031.vdocument.in/reader031/viewer/2022030410/5a9b781a7f8b9ab6188dd3e8/html5/thumbnails/30.jpg)
USBR Method
2.06aV0.012250D =
![Page 31: RIP-RAP Summary.pdf · HEC-11 Method •Psheuibdl by FHWA in 1989 • Combination of theory and field observations • Use in rivers and streams with: – Discharges greater than](https://reader031.vdocument.in/reader031/viewer/2022030410/5a9b781a7f8b9ab6188dd3e8/html5/thumbnails/31.jpg)
USBR Method2.06aV0.012250D =
Where:
D50 = stone size (ft)Va = average channel velocity (ft/s)
![Page 32: RIP-RAP Summary.pdf · HEC-11 Method •Psheuibdl by FHWA in 1989 • Combination of theory and field observations • Use in rivers and streams with: – Discharges greater than](https://reader031.vdocument.in/reader031/viewer/2022030410/5a9b781a7f8b9ab6188dd3e8/html5/thumbnails/32.jpg)
USBR Method
• Prototype velocities ranged from 1-8 ft/s• Tests conducted on sands, gravels and
stone up to 2.5 inches• Field observations of riprap up to 18
inches• Riprap layer must have no more than 40%
smaller than stable stone size
2.06aV0.012250D =
![Page 33: RIP-RAP Summary.pdf · HEC-11 Method •Psheuibdl by FHWA in 1989 • Combination of theory and field observations • Use in rivers and streams with: – Discharges greater than](https://reader031.vdocument.in/reader031/viewer/2022030410/5a9b781a7f8b9ab6188dd3e8/html5/thumbnails/33.jpg)
Common Rock Sizing Relations
• HEC-11• USACE• Isbash• CALTRANS• USBR• ASCE• USGS
![Page 34: RIP-RAP Summary.pdf · HEC-11 Method •Psheuibdl by FHWA in 1989 • Combination of theory and field observations • Use in rivers and streams with: – Discharges greater than](https://reader031.vdocument.in/reader031/viewer/2022030410/5a9b781a7f8b9ab6188dd3e8/html5/thumbnails/34.jpg)
ASCE
• Published by Vanoni in 1977• Based on Isbash (1936)• Modified to account for channel slope• Rocks size dependent on:
– Flow velocity– Unit weight of stone– Channel side slope
![Page 35: RIP-RAP Summary.pdf · HEC-11 Method •Psheuibdl by FHWA in 1989 • Combination of theory and field observations • Use in rivers and streams with: – Discharges greater than](https://reader031.vdocument.in/reader031/viewer/2022030410/5a9b781a7f8b9ab6188dd3e8/html5/thumbnails/35.jpg)
ASCE Method
1/3
sπγ6W
50D⎟⎟
⎠
⎞
⎜⎜
⎝
⎛=
![Page 36: RIP-RAP Summary.pdf · HEC-11 Method •Psheuibdl by FHWA in 1989 • Combination of theory and field observations • Use in rivers and streams with: – Discharges greater than](https://reader031.vdocument.in/reader031/viewer/2022030410/5a9b781a7f8b9ab6188dd3e8/html5/thumbnails/36.jpg)
ASCE Method1/3
sπγ6W
50D⎟⎟
⎠
⎞
⎜⎜
⎝
⎛=
Where:
W = ( ) ( )θ3cos31sG
6Vs0.000041G−
D50 = stone size (ft)W = weight of stone (lbs)V = local depth averaged velocity (ft/sec)
s = unit weight of stone (ib/ft3)W = unit weight of water (lb/ft3)
Gs = specific gravity of stone ( s/ w)
![Page 37: RIP-RAP Summary.pdf · HEC-11 Method •Psheuibdl by FHWA in 1989 • Combination of theory and field observations • Use in rivers and streams with: – Discharges greater than](https://reader031.vdocument.in/reader031/viewer/2022030410/5a9b781a7f8b9ab6188dd3e8/html5/thumbnails/37.jpg)
ASCE Method
• Based on Isbash equation with a modification to account for channel bank slope
• Uses Isbash because it is “in line with experience” to rock size that will resist movement by flow
• Velocity taken 10 feet from bank• Angle of attack less than 30 degrees
1/3
sπγ6W
50D⎟⎟
⎠
⎞
⎜⎜
⎝
⎛=
![Page 38: RIP-RAP Summary.pdf · HEC-11 Method •Psheuibdl by FHWA in 1989 • Combination of theory and field observations • Use in rivers and streams with: – Discharges greater than](https://reader031.vdocument.in/reader031/viewer/2022030410/5a9b781a7f8b9ab6188dd3e8/html5/thumbnails/38.jpg)
Common Rock Sizing Relations
• HEC-11• USACE• Isbash• CALTRANS• USBR• ASCE• USGS
![Page 39: RIP-RAP Summary.pdf · HEC-11 Method •Psheuibdl by FHWA in 1989 • Combination of theory and field observations • Use in rivers and streams with: – Discharges greater than](https://reader031.vdocument.in/reader031/viewer/2022030410/5a9b781a7f8b9ab6188dd3e8/html5/thumbnails/39.jpg)
USGS Method
• Result of analysis by Blodgett (1981) examining field data from Washington, Oregon, California, Nevada and Arizona
• Published equation stated to apply to all channels, curved or straight, with side slopes less than or equal to 1.5:1
• Incorporated HEC-11 relationship
![Page 40: RIP-RAP Summary.pdf · HEC-11 Method •Psheuibdl by FHWA in 1989 • Combination of theory and field observations • Use in rivers and streams with: – Discharges greater than](https://reader031.vdocument.in/reader031/viewer/2022030410/5a9b781a7f8b9ab6188dd3e8/html5/thumbnails/40.jpg)
USGS Method
44.250 01.0 aVD =
![Page 41: RIP-RAP Summary.pdf · HEC-11 Method •Psheuibdl by FHWA in 1989 • Combination of theory and field observations • Use in rivers and streams with: – Discharges greater than](https://reader031.vdocument.in/reader031/viewer/2022030410/5a9b781a7f8b9ab6188dd3e8/html5/thumbnails/41.jpg)
USGS Method
Where:
D50 = stone size (ft)Va = average cross section velocity (ft/s)
44.250 01.0 aVD =
![Page 42: RIP-RAP Summary.pdf · HEC-11 Method •Psheuibdl by FHWA in 1989 • Combination of theory and field observations • Use in rivers and streams with: – Discharges greater than](https://reader031.vdocument.in/reader031/viewer/2022030410/5a9b781a7f8b9ab6188dd3e8/html5/thumbnails/42.jpg)
USGS Method
• Incorporated 26 sites and 39 flow events• 14 failure points due to particle erosion• Utilized HEC-11 velocity/D50 values to add
points to plot• Approximate range of velocities utilized:
2.5 <Vaverage < 17 fps• Approximate range of median rock sizes:
0.5 < D50 < 3.0 ft
44.250 01.0 aVD =
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Abt and Johnson
• Steep slope sizing equation• Result of flume testing by Abt and
Johnson (1991)• Developed for the NRC to protect low
level waste impoundments
![Page 44: RIP-RAP Summary.pdf · HEC-11 Method •Psheuibdl by FHWA in 1989 • Combination of theory and field observations • Use in rivers and streams with: – Discharges greater than](https://reader031.vdocument.in/reader031/viewer/2022030410/5a9b781a7f8b9ab6188dd3e8/html5/thumbnails/44.jpg)
Abt and Johnson (1991)56.043.0
50 23.5 dqSD =Rule of thumb:
Increase qd by 35% to use as an envelope relationship
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Abt and Johnson (1991)
56.043.050 23.5 dqSD =
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Abt and Johnson Method
• Tested on slopes of 1, 2, 8, 10 and 20%• Unit discharges up to ~7cfs/ft• Rock sizes of 1, 2, 4, 5 and 6 inches
56.043.050 23.5 dqSD =
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Abt and Johnson (1991)56.043.0
50 23.5 dqSD =Where:
D50 = stone size (in)S = bed slopeqd = unit discharge (ft2/s)
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Summary of MethodsY=10ft, z=2, SF =1.5
0.0
1.0
2.0
3.0
4.0
5.0
6.0
7.0
8.0
9.0
10.0
5 7 9 11 13 15 17 19 21
Flow Velocity (ft/sec)
Rock
Siz
e (f
t) HEC-11IsbashUSBRASCEUSACE
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Riprap Design Criteria, Riprap Design Criteria, Specifications and Quality Specifications and Quality
ControlControl
NCHRP Report 568NCHRP Report 568
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NCHRP Project 24NCHRP Project 24--2323ObjectivesObjectives
Riprap applicationsRiprap applications::
•• Channel banks Channel banks •• Bridge piersBridge piers•• Bridge abutmentsBridge abutments•• Guide banks and other countermeasuresGuide banks and other countermeasures•• Overtopping flowOvertopping flow
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NCHRP Report 568NCHRP Report 568ObjectivesObjectives
ProductProduct::
•• Design guidelinesDesign guidelines•• Material specifications & test methodsMaterial specifications & test methods•• Construction & Quality Control guidelinesConstruction & Quality Control guidelines
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Riprap size, shape, and qualityRiprap size, shape, and quality
C (thickness)
A (length)
B (width)
•• Characteristic diameter Characteristic diameter ““dd”” corresponds to the corresponds to the intermediate (B) axisintermediate (B) axis
•• A/C ratio should not exceed 3.0 so that particles A/C ratio should not exceed 3.0 so that particles are not needleare not needle--like, nor are they platylike, nor are they platy
•• Particles should be angular, not round Particles should be angular, not round
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Riprap gradationRiprap gradation0.10 m0.25 m0.50 m0.75 m1.0 m
0
10
20
30
40
50
60
70
80
90
100
012243648
Stone Size, inches
Perc
ent F
iner
by
Wei
ght,
%
Allowable d85/d15minimum: 27.3/18.3 = 1.5ideal: 30.0/16.0 = 1.9 maximum: 32.3/12.8 = 2.5
d85
d15
Allowable range of sizes for Class VI riprap (d50 = 21 inches)
d50
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Revetment RiprapRevetment Riprap
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Maximum slope 1V:1.5H Ambient bed elevation
Geotextile orgranular filter
Design high water
Minimum freeboard 2 ft (0.6 m)
Minimum riprap thickness = larger of (1.5d50 or d100)
Toe down riprap tomaximum scour depth
Maximum scour depth :
(Long-term degradation) + (Toe scour) + (Contraction scour)
Revetment RiprapRevetment Riprap
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Riprap mound height =desired toe down depth
Ambient bed elevation
Design high water
Minimum freeboard 2 ft (0.6 m)
Riprap mound thickness =2x layer thickness on slope
Revetment RiprapRevetment Riprap
Alternative toe detailAlternative toe detail
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5.2
g1
destvsf30 gy)1S(K
V)CCCS(yd⎥⎥⎦
⎤
⎢⎢⎣
⎡
−=
US Army Corps of Engineers EMUS Army Corps of Engineers EM--16011601
Revetment RiprapRevetment Riprap
Note: dNote: d5050 ~ 1.2(d~ 1.2(d3030))
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EM-1601
0.01
0.1
1
0.1 1
V/[gd(Sg-1)]0.5
D30
/dFailed D85/D15 < 1.6Stable D85/D15 < 1.6Failed D85/D15 = 2.8Stable D85/D15 = 2.8Failed D85/D15 = 3.9Stable D85/D15 = 3.9Failed D85/D15 = 4.6Stable D85/D15 = 4.6EM 1601
5.2
g
30
gd)1S(V30.0
dD
⎥⎥⎦
⎤
⎢⎢⎣
⎡
−=
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HEC-11
0.01
0.1
1
0.1 1
V/[gd(Sg-1)]0.5
D50
/dFailed D85/D15 < 1.6Stable D85/D15 < 1.6Failed D85/D15 = 2.8Stable D85/D15 = 2.8Failed D85/D15 = 3.9Stable D85/D15 = 3.9Failed D85/D15 = 4.6Stable D85/D15 = 4.6HEC-11
3
g
50
gd)1S(V295.0
dD
⎥⎥⎦
⎤
⎢⎢⎣
⎡
−=
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Pier RiprapPier Riprap
Schoharie Creek, NYSchoharie Creek, NY
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Pier RiprapPier Riprap
Schoharie Creek bridge pier No. 2Schoharie Creek bridge pier No. 2
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Pier RiprapPier Riprap
Minimum riprap thickness t = 3dMinimum riprap thickness t = 3d5050 , depth of , depth of contraction scour, or depth of bedform trough, contraction scour, or depth of bedform trough, whichever is greatestwhichever is greatest
Filter placement = 4/3(a) from pier (all around)Filter placement = 4/3(a) from pier (all around)
t
Filter
FLOWPier
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Pier RiprapPier Riprap
Pier width = Pier width = ““aa”” (normal to flow)(normal to flow)
Riprap placement = minimum 2(a) from pier (all around)Riprap placement = minimum 2(a) from pier (all around)
aFLOW 2a
2a
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Pier RiprapPier Riprap
2
g
des50 g2)1S(
V692.0d⎥⎥⎦
⎤
⎢⎢⎣
⎡
−=
FHWA Hydraulic Engineering Circular 23FHWA Hydraulic Engineering Circular 23
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Abutment RiprapAbutment Riprap
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Abutment RiprapAbutment Riprap
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Abutment RiprapAbutment Riprap
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Abutment RiprapAbutment Riprap
1V:2H
FloodplainGeotextile or
Granular Filter
Apron
Design High Water
2’ (0.6 m) Freeboard
Abu
tmen
t
Riprap Thickness = 1.5D50 or D100
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Abutment RiprapAbutment Riprap
0.8Fforyg
V1)(S
KD r
2
g≤⎟⎟
⎠
⎞⎜⎜⎝
⎛−
= y50
0.8Fforyg
V1)(S
KD r
0.142
g>⎟⎟
⎠
⎞⎜⎜⎝
⎛−
= y50
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Abutment RiprapAbutment Riprap
Abutment riprap sizing based on Abutment riprap sizing based on ““Setback RatioSetback Ratio”” (SBR) method:(SBR) method:
Distance from main channelDistance from main channelFlow depth in main channelFlow depth in main channelSBR =SBR =
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Abutment Riprap, SBR > 5Abutment Riprap, SBR > 5
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Abutment Riprap, SBR < 5Abutment Riprap, SBR < 5
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Abutment Riprap, SBR > 5Abutment Riprap, SBR > 5SBR < 5SBR < 5
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Minimum of: 2y or 25 feet
RiprapExtent
Abutment
Apron
FLOW
Main Channel
Channel Bank
Floodplain
Maximum of: 2y or 25 feet
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3.4 m/s
3.0 m/s2.72.42.11.81.51.20.90.60.30.0
Abutment vs. Abutment vs. guide bankguide bank
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ISBASH Method
• Developed by Isbash in 1936• Adopted by USACE in 1971• Developed for construction of dams by placing rock in flowing water
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ISBASH Method
( )1sG22gC
2aV
50D−
=
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ISBASH Method
( )1sG22gC
2aV
50D−
=
Where:
D50 = stone size (ft)Va = average channel velocity (ft/s)Gs = specific gravity of stoneG = gravitational constant (ft/s2)C = 0.86 for high turbulence zones
1.20 for low turbulence zones
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5.2
g1
destvsf30 gy)1S(K
V)CCCS(yd⎥⎥⎦
⎤
⎢⎢⎣
⎡
−=
US Army Corps of Engineers EMUS Army Corps of Engineers EM--16011601
Revetment RiprapRevetment Riprap
Cv = 1.25Note: dNote: d5050 ~ 1.2(d~ 1.2(d3030))