river bank erosion

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Detroit District, Hydraulics & Hydrology Office US Army Corps of Engineers River Bank Erosion Siskiwit River, Cornucopia, WI

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River Bank Erosion. Siskiwit River, Cornucopia, WI. How Do we Measure Bank Erosion?. The Big Questions…continued. Are there simple methods that can be used to estimate bank erosion rates in the field?. Answer…No. Lateral Movement of bank. Measured in feet/year. Resisting Force - PowerPoint PPT Presentation

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Page 1: River Bank Erosion

Detroit District, Hydraulics & Hydrology OfficeUS Army Corpsof Engineers

River Bank Erosion

Siskiwit River, Cornucopia, WI

Page 2: River Bank Erosion

Detroit District, Hydraulics & Hydrology OfficeUS Army Corpsof Engineers

How Do we Measure Bank Erosion?

Page 3: River Bank Erosion

Detroit District, Hydraulics & Hydrology OfficeUS Army Corpsof Engineers

The Big Questions…continued

• Are there simple methods that can be used to estimate bank erosion rates in the field?

• Are there simple methods that can be used to estimate bank erosion rates in the field?

Answer…NoAnswer…No

Page 4: River Bank Erosion

Detroit District, Hydraulics & Hydrology OfficeUS Army Corpsof Engineers

ErosivityyErodibilitErosionBank

Lateral Movement of

bank.

Measured in feet/year

Resisting Force

Intrinsic property of bank.

Function of:Soil

VegetationBank Angle

Etc.

Driving Force

Property of the hydraulics.

Function of:Near Bank

Shear Stress

Bank Erosion

Page 5: River Bank Erosion

Detroit District, Hydraulics & Hydrology OfficeUS Army Corpsof Engineers

Bank Erodability

How do we determine how susceptible a bank is to erosion?

How do we determine how susceptible a bank is to erosion?

Page 6: River Bank Erosion

Detroit District, Hydraulics & Hydrology OfficeUS Army Corpsof Engineers

ErosivityyErodibilitErosionBank

Predicting Bank Erosion

Bank Erosion

Hazard Index (BEHI)

Page 7: River Bank Erosion

Detroit District, Hydraulics & Hydrology OfficeUS Army Corpsof Engineers

• Bank Height Ratio

• Root Depth Ratio

• Weighted Root Density

• Bank Angle

• Surface Protection

• Bank Material

• Stratification

• Bank Height Ratio

• Root Depth Ratio

• Weighted Root Density

• Bank Angle

• Surface Protection

• Bank Material

• Stratification

BEHI Variables

Page 8: River Bank Erosion

Detroit District, Hydraulics & Hydrology OfficeUS Army Corpsof Engineers

Low Erosion Potential

Black River, Michigan (UP)

Page 9: River Bank Erosion

Detroit District, Hydraulics & Hydrology OfficeUS Army Corpsof Engineers

Moderate Erosion Potential

Coldwater Creek, Union City, Michigan

Page 10: River Bank Erosion

Detroit District, Hydraulics & Hydrology OfficeUS Army Corpsof Engineers

Very High / Extreme Erosion Potential

Ontonagon River, Michigan (UP)

Page 11: River Bank Erosion

Detroit District, Hydraulics & Hydrology OfficeUS Army Corpsof Engineers

ErosivityyErodibilitErosionBank

Bank Erosion

Bank Erosion

Hazard Index (BEHI)

Near Bank Stress (NBS)

Index

Page 12: River Bank Erosion

Detroit District, Hydraulics & Hydrology OfficeUS Army Corpsof Engineers

NBS#1 - Channel Patterns

• Transverse and/or central bars – short and/or discontinous

– NBS = High or Very High

• Extensive deposition

– NBS = Extreme

• Chute cutoffs, down-valley meander migration, converging flow

– NBS = Extreme

• Transverse and/or central bars – short and/or discontinous

– NBS = High or Very High

• Extensive deposition

– NBS = Extreme

• Chute cutoffs, down-valley meander migration, converging flow

– NBS = Extreme

Page 13: River Bank Erosion

Detroit District, Hydraulics & Hydrology OfficeUS Army Corpsof Engineers

NBS#2 – Ratio of Radius of Curvature (Rc) to Bankfull Width (Wbkf)

Rc/Wbkf Rating

> 3.00 Very Low

2.21 – 3.00 Low

2.01 – 2.20 Moderate

1.81 – 2.00 High

1.50 – 1.80 Very High

< 1.50 Extreme

Generally Rc Performed Using Aerial PhotographyGenerally Rc Performed Using Aerial Photography

Page 14: River Bank Erosion

Detroit District, Hydraulics & Hydrology OfficeUS Army Corpsof Engineers

NBS#3 & #4 – Ratio of Pool Slope to Average Slope (Sp/S) or Riffle Slope (Sp/Srif)

Sp/Srif Rating

< 0.40 Very Low

0.41 – 0.60 Low

0.61 – 0.80 Moderate

0-81 – 1.00 High

1.01 – 1.20 Very High

> 1.20 Extreme

Page 15: River Bank Erosion

Detroit District, Hydraulics & Hydrology OfficeUS Army Corpsof Engineers

dnb/dbkf Rating

< 1.00 Very Low

1.00 – 1.50 Low

1.51 – 1.80 Moderate

1.81 – 2.50 High

2.51 – 3.00 Very High

> 3.00 Extreme

NBS#5 – Pool Depth to

Average Depth

Page 16: River Bank Erosion

Detroit District, Hydraulics & Hydrology OfficeUS Army Corpsof Engineers

Measuring Bank Erosion

Page 17: River Bank Erosion

Detroit District, Hydraulics & Hydrology OfficeUS Army Corpsof Engineers

ErosivityyErodibilitErosionBank

Bank Erosion

Bank Pins & Bank Profiles

Bank Erosion

Hazard Index (BEHI)

Near Bank Stress (NBS)

Index

Page 18: River Bank Erosion

Detroit District, Hydraulics & Hydrology OfficeUS Army Corpsof Engineers

Bank Profile Measurement

Equipment

• Toe Pin (rebar)

• Toe Pin Cap

• Hammer

• Survey Rod (2) or

• Survey Rod & Pocket Rod

• Line Level

• Rod Level

• Field Forms

Equipment

• Toe Pin (rebar)

• Toe Pin Cap

• Hammer

• Survey Rod (2) or

• Survey Rod & Pocket Rod

• Line Level

• Rod Level

• Field Forms

Page 19: River Bank Erosion

Detroit District, Hydraulics & Hydrology OfficeUS Army Corpsof Engineers

Measuring Bank Profile

Source: Arkansas Department of Environmental Quality

Page 20: River Bank Erosion

Detroit District, Hydraulics & Hydrology OfficeUS Army Corpsof Engineers

Comparison of Bank Profiles

Page 21: River Bank Erosion

Detroit District, Hydraulics & Hydrology OfficeUS Army Corpsof Engineers

Bring it all

Together

Regional Curves

Page 22: River Bank Erosion

Detroit District, Hydraulics & Hydrology OfficeUS Army Corpsof Engineers

Great Lakes Curves - Preliminary

Page 23: River Bank Erosion

Detroit District, Hydraulics & Hydrology OfficeUS Army Corpsof Engineers

Is there a better correlation for predicting bank erosion?

• Remotely-sensed data

• Radius of curvature

• Meander wavelength

• Beltwidth:valley width

• Valley slope

• Soils maps for resistance and infiltration

• Remotely-sensed data

• Radius of curvature

• Meander wavelength

• Beltwidth:valley width

• Valley slope

• Soils maps for resistance and infiltration

Page 24: River Bank Erosion

Detroit District, Hydraulics & Hydrology OfficeUS Army Corpsof Engineers

Questions?

Contact: Dr. Jim Selegean, P.E., P.H.

U.S. Army Corps of Engineers, Detroit DistrictGreat Lakes Hydraulics and Hydrology Office

477 Michigan AveDetroit, MI 48226

313.226.6791

[email protected]