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Iowa’s River Restoration Toolbox Level 1 / Base Training

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Presentation on theme: "Iowa’s River Restoration Toolbox Level 1 / Base Training"— Presentation transcript:

1 Iowa’s River Restoration Toolbox Level 1 / Base Training
Module # 13 Understanding the Key Instability Drivers to Inform Design/Decision Matrix Iowa’s River Restoration Toolbox Level 1 / Base Training

2 Key Design Parameters

3 Key Drivers Floodplain Access Bank Height Ratio Entrenchment
Bankfull Properties Area Discharge Width Depth Channel Evolution Stage Dominant BEHI Buffer Width

4 Bank Height Ratio (BHR)
BHR= LBH/Dbkf Lowest Bank Height (LBH) Bankfull Depth (Dbkf)

5 Geomorphic Floodplain
Entrenched Channel Bankfull Depth Geomorphic Floodplain Bankfull Width

6 Bankfull Geometry

7 Channel Evolution Models
Simon’s Modification of Schumm’s Model

8 Shear Stresses in Streams
Discharge Return Interval Shear Stress Natural Stream Channelized Stream 2-Year Storm 100-Year Storm D100 D2 Channelized Stream 100-Year Storm D100 2-Year Storm D2 Natural Stream

9 BEHI Study Bank Height Bankfull Height Root Depth Bank Angle
Surface Protection Bank Material Adjustment Stratification Adjustment Bank Length Reach Length

10 Heading for Text Over a Photo
Riparian Buffer

11 Additional Key Drivers
Pattern/Geometry Radius of Curvature Meander Width Ratio Pool to Pool Spacing Width to Depth Ratio Channel Length Channel Slope Stream Type Presence of Headcuts/Bed Stability Geomorphic Region/Geology Sediment Supply/Bed Materials Constraints

12 Pattern/Geometry Wbkf = Bankfull Width Lm = Meander Wavelength
Wblt = Belt Width Am = Amplitude Lm = Meander Wavelength Rc = Radius of Curvature

13 Channel Slope

14 BKF Width / Mean BKF Depth
Stream Type Classification A B C E DA D F G Entrenchment ratio* <1.4 >2.2 >4.0 n/a FP width / BKF Width BKF Width / Mean BKF Depth W / D ratio* <12 >12 <40 >40 Typical sinuosity 1 -1.2 >1.2 >1.5 Not predictive Well-defined point bars Veg. islands Heavy veg. Both banks erode in wide dirt canyon Confined, u-shaped valley Often bedrock / log controlled Visual Cues Gully in soft materials Sed. islands Typical slope <.02 <.005 <.04 Typical stability Usually Stable Likely Unstable Classifications from Rosgen, 1996

15 Headcuts/Bed Stability
Caused by Excess Shear Stress Often Triggered by Downstream Straightening of Channel Will Propagate Upstream Increases Channel Entrenchment

16 Sediment Supply/Bed Materials

17 Constraints

18 Key Design Parameters

19 Functional Status

20 The Assessment Process
8. Submit final analysis for review 7. Perform analysis of appropriate practices/techniques 6. Receive adjusted recommendations based on design intent 5. Update Key Drivers for design based on step 4 4. Make initial decisions that will affect the project design 3. Receive initial assessment based on site conditions 2. Fill out data collection Excel workbook 1. Assess project site conditions

21 Purpose of Decision Matrix
Documentation of intuitive knowledge used in stream restoration design Establish logic used to determine appropriate practices & techniques Note that there are multiple “right answers”

22 Channel Evolution Models
Simon’s Modification of Schumm’s Model

23 Decision Matrix – Channel Evolution

24 Bank Height Ratio (BHR)
BHR= LBH/Dbkf Lowest Bank Height (LBH) Bankfull Depth (Dbkf)

25 Decision Matrix – Bank Height Ratio

26 Decision Matrix - Slope

27 Decision Matrix – Bankfull Width

28 Design Assessment Tab

29 Technique Ranking

30 Iowa’s River Restoration Toolbox Level 1 / Base Training
Module # 13 Understanding the Key Instability Drivers to Inform Design/Decision Matrix Iowa’s River Restoration Toolbox Level 1 / Base Training


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