CR AAO Bridge. Dead River Flood & Natural Channel Design. Mitch Koetje Water Resources Division UP District

Similar documents
Why Geomorphology for Fish Passage

Stream Geomorphology. Leslie A. Morrissey UVM July 25, 2012

Bank Erosion and Morphology of the Kaskaskia River

Riparian Assessment. Steps in the right direction... Drainage Basin/Watershed: Start by Thinking Big. Riparian Assessment vs.

Rosgen Classification Unnamed Creek South of Dunka Road

Four Mile Run Levee Corridor Stream Restoration

Ways To Identify Background Verses Accelerated Erosion

Working with Natural Stream Systems

Step 5: Channel Bed and Planform Changes

NATURE OF RIVERS B-1. Channel Function... ALLUVIAL FEATURES. ... to successfully carry sediment and water from the watershed. ...dissipate energy.

Black Gore Creek 2013 Sediment Source Monitoring and TMDL Sediment Budget

Limitation to qualitative stability indicators. the real world is a continuum, not a dichotomy ~ 100 % 30 % ~ 100 % ~ 40 %

Overview of fluvial and geotechnical processes for TMDL assessment

Aquifer an underground zone or layer of sand, gravel, or porous rock that is saturated with water.

PolyMet NorthMet Project

Assessment. Assessment

Natural Shoreline Landscapes on Michigan Inland Lakes

Field Methods to Determine/ Verify Bankfull Elevation, XS Area & Discharge

!"#$%&&'()*+#$%(,-./0*)%(!

Stream Restoration and Environmental River Mechanics. Objectives. Pierre Y. Julien. 1. Peligre Dam in Haiti (deforestation)

The Yellow River Initiative: The Birth of a System Approach to Challenges Facing the Everglades of the North

Implementing a Project with 319 Funds: The Spring Brook Meander Project. Leslie A. Berns

Session C1 - Applying the Stream Functions Pyramid to Geomorphic Assessments and Restoration Design

Avoiding Geohazards in the Mid-Atlantic Highlands by Using Natural Stream Principles

Diagnostic Geomorphic Methods for Understanding Future Behavior of Lake Superior Streams What Have We Learned in Two Decades?

ADDRESSING GEOMORPHIC AND HYDRAULIC CONTROLS IN OFF-CHANNEL HABITAT DESIGN

Fluvial Driven Alluvial Fans

Upper Mississippi River Basin Environmental Management Program Workshop

May 7, Roger Leventhal, P.E. Marin County Public Works Laurel Collins Watershed Sciences

Case Study 2: Twenty-mile Creek Rock Fords

Griswold Creek August 22, 2013

Do you think sediment transport is a concern?

Long Valley Meadow Restoration Project

Assignment 1. Measuring River Characteristics- Vernon Creek. Applied Fluvial Geomorphology Field Techniques EESc 435

The River Restoration Centre therrc.co.uk. Understanding Fluvial Processes: supporting River Restoration. Dr Jenny Mant

SCOPE OF PRESENTATION STREAM DYNAMICS, CHANNEL RESTORATION PLANS, & SEDIMENT TRANSPORT ANALYSES IN RELATION TO RESTORATION PLANS

Watershed Assessment of River Stability and Sediment Supply: Advancing the Science of Watershed Analysis

GENERAL SUMMARY BIG WOOD RIVER GEOMORPHIC ASSESSMENT BLAINE COUNTY, IDAHO

Session 1 Healthy Streams Stream Hydraulics Natural Channel Design

Why Stabilizing the Stream As-Is is Not Enough

Island Design. UMRS EMP Regional Workshop. Presentation for the

HAW CREEK, PIKE COUNTY, MISSOURI-TRIB TO SALT RIVER ERODING STREAM THREATHENING COUNTY ROAD #107, FOURTEEN FT TALL ERODING BANK WITHIN 4 FT OF THE

Channel Assessments of Selected Watersheds within TFL 52

Perspectives on river restoration science, geomorphic processes, and channel stability

Restoring the Napa River:

DETAILED DESCRIPTION OF STREAM CONDITIONS AND HABITAT TYPES IN REACH 4, REACH 5 AND REACH 6.

Discharge. Discharge (Streamflow) is: Q = Velocity (L T -1 ) x Area (L 2 ) Units: L 3 T -1 e.g., m 3 s -1. Velocity. Area

Fish Passage at Road Crossings

OBJECTIVES. Fluvial Geomorphology? STREAM CLASSIFICATION & RIVER ASSESSMENT

CASE STUDIES. Introduction

Lower South Fork McKenzie River Floodplain Enhancement Project

Stream Classification

Solutions to Flooding on Pescadero Creek Road

NATURAL RIVER. Karima Attia Nile Research Institute

Tom Ballestero University of New Hampshire. 1 May 2013

STREAM SYSTEMS and FLOODS

Precipitation Evaporation Infiltration Earth s Water and the Hydrologic Cycle. Runoff Transpiration

Little Blackfoot TPA 2009 Sediment and Habitat Assessment QAQC Review March 9, 2010

Field Observations and One-Dimensional Flow Modeling of Summit Creek in Mack Park, Smithfield, Utah

Stop 1: Marmot Dam Stop 1: Marmot Dam

Squaw Creek. General Information

Wetland & Floodplain Functional Assessments and Mapping To Protect and Restore Riverine Systems in Vermont. Mike Kline and Laura Lapierre Vermont DEC

Forest Service AOP Meeting Objectives of Stream Simulation: Examples and Talking Points

Earth Science Chapter 6 Section 2 Review

APPENDIX E. GEOMORPHOLOGICAL MONTORING REPORT Prepared by Steve Vrooman, Keystone Restoration Ecology September 2013

Summary of Hydraulic and Sediment-transport. Analysis of Residual Sediment: Alternatives for the San Clemente Dam Removal/Retrofit Project,

Carmel River Bank Stabilization at Rancho San Carlos Road Project Description and Work Plan March 2018

Dan Miller + Kelly Burnett, Kelly Christiansen, Sharon Clarke, Lee Benda. GOAL Predict Channel Characteristics in Space and Time

Great Lakes Tributary Modeling: Canaseraga Creek Watershed

Running Water Earth - Chapter 16 Stan Hatfield Southwestern Illinois College

Woodstock, Route 26 Stream Relocation Project

Erosion Surface Water. moving, transporting, and depositing sediment.

Appendix E Rosgen Classification

Technical Memorandum. To: From: Copies: Date: 10/19/2017. Subject: Project No.: Greg Laird, Courtney Moore. Kevin Pilgrim and Travis Stroth

Dam Removal Analysis Guidelines for Sediment

How Do Human Impacts and Geomorphological Responses Vary with Spatial Scale in the Streams and Rivers of the Illinois Basin?

Geomorphic Assessment of the Middle and Lower Swan Lake Watershed, Calhoun Division of Two Rivers National Wildlife Refuge.

Illinois State Water Survey Division

Chris Lenhart, John Nieber, Ann Lewandowski, Jason Ulrich TOOLS AND STRATEGIES FOR REDUCING CHANNEL EROSION IN MINNESOTA

Geomorphic Importance of Winter Peak Flows and Annual Snowmelt Hydrographs in a Sierra Nevada Boulder-Bedrock River

Kaskaskia Morphology Study Headwaters to Lake Shelbyville

UPPER KETTLE CREEK FISH HABITAT CONSERVATION PLAN TRIBUTARIES ADDENDUM

Sediment and nutrient transport and storage along the urban stream corridor

Development of a Fluvial Erosion Hazard Mitigation Program for Indiana

Conceptual Model of Stream Flow Processes for the Russian River Watershed. Chris Farrar

NORTHUMBERLAND COUNTY, PA

A GEOMORPHOLOGICAL APPROACH TO RESTORATION OF INCISED RIVERS. David L. Rosgen 1

EAGLES NEST AND PIASA ISLANDS

The Reference Reach - a Blueprint for Natural Channel Design. Dave Rosgen, P.H. 1

The how, why, and lessons learned

Appendix G. Riverbank Stabilization Techniques

Watershed concepts for community environmental planning

Fluvial Geomorphology

GEOL 1121 Earth Processes and Environments

C. STUDENT FIELD DATA SHEETS

Laboratory Exercise #3 The Hydrologic Cycle and Running Water Processes

Elwha River response to dam removals through four years and a big flood:

Case Study 14. Rocky Creek Vented Box Culvert Ford

Historical channel change on the Upper Gila River, Arizona and New Mexico in response to anthropogenic modifications and extreme floods

River Restoration and Rehabilitation. Pierre Y. Julien

Transcription:

CR AAO Bridge Dead River Flood & Natural Channel Design Mitch Koetje Water Resources Division UP District

Old County Road AAO Bridge

Map courtesy of Marquette County Silver Lake Basin McClure Basin Tourist Park Basin Dead River Basin Forestville Basin

The Event was Reported at 4 p.m. on May 14, 2003 Actively Draining Silver Lake Look Downstream From Silver Lake Through Fuse Plug Fuse Plug Area 30 foot deep erosion trench

Start of Connors Creek Area/Reach B - Looking Upstream on 7-15-04

Once forested, there are now several sand plains left from the flood damage downstream of the fuse plug failure at Silver Lake Basin. (Connors Ck. Area 10/15/03) Dead River Look Downstream

Dead River Basin Sand Delta in May 2004 Photo courtesy of Central Lake Superior Watershed Partnership, 5/2004

Flood Events High waters cause an earthen levee to breach at Tourist Park about 2 p.m. on May 15, 2003

Tourist Park Basin Looking Upstream - Right after the Event on 5/16/03

Old CR 550 Bike Path Bridge

Is this it? Get off your rear ends and get something done would ya!

So Restoration Planning Collaborative Effort Two Phased Watershed Approach Natural Channel Design Studies - Riverine Habitat (Rosgen) - Revegetative Stabilization Techniques - Wetlands/Floodplains - Fish, Mussels, Macroinvertebrates

$8.7 Million in Assessment & Recovery (without lower river) $1.3 Million in Mitigation Silver Lake Rebuild estimated at $10 M

Sand Plug of the Mulligan Creek Mouth

Sand Trap area looking US to Mulligan Mouth 7-15-04

4/23/04 Mulligan Creek Confluence

Clay Banks Interim Restoration Project 2003

Post Construction: Clay Banks Interim Project Completed 11/03 Photo on 7/15/04

5-4-05 Riprap Bank

5-4-05

Same spot 6/3/10 4 years post construction

$1.7M total from Flood Control and Costal Emergency funding was utilized by USACE 80,000 yd3 of debris removed

Woody Debris Mulch Pile Photo Courtesy of Central Lake Superior Watershed Partnership

Channel Stability The ability of a stream, over time, to maintain its pattern, Channel Stability Channel Stability The ability of a stream, over time, to maintain its pattern, dimension The ability and of profile a stream, dimension and profile such that, the channel neither aggrades or degrades and over is able time, to to transport maintain its such that, the channel without adverse impact the flow and sediment from it s watershed. pattern, dimension and neither aggrades or profile such that, the These degrades physical and is channel able features are described as a function channel of neither to transport bankfull elevation. the flow aggrades or degrades and sediment from it s and is able to transport watershed without without adverse impact the flow and sediment adverse impact. from it s watershed. These physical channel features are described as a function of the bankfull elevation. These physical channel features are described as a function of the bankfull elevation.

Reference Reach A reference reach is a channel segment that is stable, neither aggrading nor degrading, and of the same morphological type as the channel being assessed. The reference reach should also have the same potential valley type, flow regime, sediment regime, streambank type and riparian community as that of the assessment reach. The reference reach is used as the standard against which the assessment reach is being judged. To account for differences in drainage area and discharge between a reference site and an assessment site, data on channel characteristics (dimension, pattern, and profile) in the form of dimensionless ratios are developed for the reference reach. Wildland Hydrology 2013

NCD Measurements Used for the Design Process There are 67 variables that are measured or studied. These variables are used in dimensionless rations for the channel design. Variable Categories: Streamflow Regime Sediment Regime Valley Morphology, Bed & Bank Materials, Roughness, & Riparian Veg. Channel Feature Dimensions: Riffle, Run, Pool, Glide, (step) & Floodplain Channel Pattern: Sinuosity, Meander Length, Radius of Curvature, Pool Length and Spacing Channel Profile: Water Surface & Bed Feature Slopes and Depths

Bankfull discharge: Bankfull Definitions The momentary maximum flow associated with the bankfull elevation. Is the discharge which reoccurs every 1 or 2 years; approximately 1.5 years on average. Is the discharge which performs most of the work transports most of the sediment, determines channel dimensions, forms or removes bars and meanders, etc. This is considered the effective or channel forming flow

Bankfull Elevation

Once forested, there are now several sand plains left from the flood damage downstream of the fuse plug failure at Silver Lake Basin. (Connors Ck. Area 10/15/03) Dead River Look Downstream

Dead River Flow Flow Connors Creek

4 miles of River Channel Pre Reach A 3,650 feet Completed in 2005 Mulligan Creek Overlook Photo Pt. Reach A 3,956 feet Completed in 2005 Reach B 2005 1,200 feet 2006 Reach B 11,725 feet AAT Bridge AAO Bridge Connors Creek

Sand Plug of Original Silver Lake Dam Outlet Channel Reference Point for Following Photos 7-14-04 Look Upstream at Channel Restoration Photo Monitoring Point Downstream of Fuse Plug Photo Point

Recovery Efforts 2005 New Wetland New Channel Old Channel and Future Wetland Photo courtesy of UPPCO

Recovery Efforts 2006- Pre-Reach A Start of Year 1 New Wetland New Channel Old Channel and Future Wetland Photo courtesy of UPPCO

Same Area on August 2, 2007 Year 2 New Channel Old Channel and Future Wetland New Wetland

Same Area on 6-9-09 Year 4 New Wetland New Channel Old Channel and Future Wetland

6/3/10 Start of Year 5 New Channel Old Channel and Future Wetland New Wetland

How do you get this stability on 4 miles of River Channel? Pre Reach A 3,650 feet Completed in 2005 Mulligan Creek Overlook Photo Pt. Reach A 3,956 feet Completed in 2005 Reach B 2005 1,200 feet 2006 Reach B 11,725 feet AAT Bridge AAO Bridge Connors Creek

This is not just Ditch Diggin $120-200/linear ft. design & construction. Compared to $244/linear ft. emergency riprap measures placed after the flood. UP projects - small to large channel range In-Stream Structures Reach B- 2005

Live Stake Shrubs on all Banks

June 2010

Cross Vane 10-30-09

7-18-06 Pre-A Cross Vane

J-Hook 5-15-07

Riffle 6-9-09

Root Wads FLOW

Series of Structure types

6/9/09 Reach A Stabilized Channel Forever?

Post-Event Water Line and white tree May 2003 - Sand Plug of Channel from Silver Lake Dam November 2005 May 2003 Top of Event Deposited Sand Post-Event Water Line Top of Pre- Reach A July 2006

6/3/10 4.5 years post construction Post-Event Water Line and white tree

CR AAT Overlook Upstream of Mulligan Creek on the Dead River 6-30-03 Overlook Note: wetted soil line

County Road AAT Overlook on 8-1-06 (3 years later) Overlook Note: wetted soil line

6/9/03

6/9/03

6/9/03

View of previous photo Look pstream from the Road Overlook on 7-9-09 6 years after the event Less than 3 years after construction

5-10-13

8-21-13

CR 550 to Superior Recovery 2011 57 foot wide channel Riffles 3 to 4.5 ft deep Pools Max. of 7.5 ft deep with 20ft bottom

THE END