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    Applied Habitat ManagementApplied Habitat Managementat Dam Removalsat Dam Removals

    Dam Removal DemystifiedDam Removal Demystified

    North CarolinaNorth Carolina

    June 14, 2011June 14, 2011

    Brian GraberBrian Graber

    American RiversAmerican Rivers

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    Outline:

    Healthy RiverCharacteristics

    Design with Habitatin Mind

    Active HabitatAdditions?

    86

    88

    90

    92

    94

    96

    98

    0 20 40 60 80 100 120 140

    distance (feet)

    e

    le

    v

    a

    tio

    n

    (fe

    e

    t)

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    Characteristics of River Habitat

    ComplexityComplexityContinuityContinuity

    Flow RegimeFlow Regime Water QualityWater Quality

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    River species need different habitats:

    Seasonally

    Through life history

    Refuge from events

    Genetic diversity

    Rivers are long, linear ecosystems

    River Health: Connectivity

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    Different species need connectivity in waterand along bed, banks, and floodplain

    River Health: Connectivity

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    Habitat Structure: Complexity

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    **Good habitat is messy**

    In-channel

    On banks

    On bed

    Complexity(habitat) isprovided by:

    Vegetation

    Substrate

    Dead wood(LWD)

    Bed features

    Dynamicplanform

    River Health: Complexity

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    Bed Feature Complexity

    Slope 0% to 1% -

    meandering

    with pools and riffles

    Slope 1% to 2% -

    transitional

    Slope > 2% -

    step-pools

    Recent research is finding thatpre-settlement rivers had even

    more complexity than currenttheory (Abbe and Montgomery2003; Walter and Merritts2008)

    River Health: Complexity

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    Designing with Habitat in Mind

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    Restoration: return to self-sustaining processes within the

    current (and future) land use

    Defining restoration

    Return to a pre-disturbance

    state?

    Recent research has been highlycritical of river restoration

    Dam removals turn rivers backinto rivers and let them do theirown work

    Restoration Theory

    Restoration Theory

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    Concept Checklist for Successful Restoration

    Think long-term

    Pursue self-sustaining approaches First, eliminate stressors Simulate nature

    Restoration Theory

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    Forget about short-term benefits

    and impacts

    Use a 50-year rule in project planning

    Think about what the river will be like in 50years and what you're doing or not doing tocontribute to that

    Restoration Theory: Think Long-Term

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    Anything that requires maintenance is notreally a long-term solution

    Natural river processes provide habitat that is

    Long-term, self-sustaining

    Broad in spatial scale instead of localized

    Beneficial to multiple species and life stages

    Don't depend on human intervention long-term

    Budgets change

    Programs change

    Institutional knowledge disappears

    Restoration Theory: Self-Sustainability

    d d ll

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    Rivers are dynamic and will repairthemselves if given the opportunity

    Restoration Theory: Eliminate Stressors

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    The majority of the habitat restoration

    comes from removing the damWater quality, flow regime, connectivity, complexity

    Restored fish passage

    Restored connectivity along bed, banks, riparian area

    Temperature regime improvement (and associateddissolved oxygen)

    Restored riverine flow characteristics

    Restored sediment dynamics

    Cleaned substrate

    Restored vegetative cover long-term

    Restored riverine bed features long-term

    Dam removal sets river on a trajectory to restorelong-term habitat if given freedom to do its ownwork

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    Simple Design Features for Habitat

    1) Remove full vertical extent of the dam

    Get any channel spanning structure outHabitat Design Features

    2) C t i i id t

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    2) Connect riparian corridor upstreamand downstream of dam

    Turn retaining walls intoriver banks if possible

    Consider more than justswimming species

    Habitat Design Features

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    3) Remove enough dam width for floodplain

    Floodplains

    Deposit sediment and nutrients

    Increase riparian corridor connectivity

    Increase roughness

    Decrease stream power

    Habitat Design Features

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    = Qswhere

    is stream power

    is the specific weight of the flowing fluid

    Q is the discharge

    s is the energy slope of the channel

    Stream Power

    Stream Power

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    Rivers are Dynamic:

    Erode and DepositAdjustment is a natural process

    and it creates habitat(Florsheim, et al. 2008)

    Bed features pools, riffles, step-pools

    Side channels Cut-off channels (ox bows)

    Wood recruitment

    Retains connectivity betweenriver and floodplain improves riparian vegetationdynamics

    Source: Mount, 1995Stream Power

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    Drained Impoundments Can BeExtremely Dynamic

    Stream Power

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    Aspect ratio:

    Ratio of impoundmentwidth to river width

    Low aspect ratio results

    in less potential forlateral migration

    Potential for verticalerosion remains

    Impoundment

    Aspect Ratio

    Stream Power

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    High aspect ratio

    impoundment

    Has high potentialfor lateral migrationfollowing dam

    removal

    Stream Power

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    Active Habitat Additions?

    Assess riskAssess risk Simulate natureSimulate natureGrade control,Grade control,

    bank stabilizationbank stabilization

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    Will short-term erosioncause long-term damage?

    Species of concern

    Particle sizes

    2) Sediment Transport

    Active Habitat: Assess Risk

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    Is the river free to createhabitat?

    Urban settings

    Give the river as muchspace as possible

    Stream Power:Baseflow dominatedspring creeks take

    longer to form habitatthan powerful rivers

    3) Habitat Formation

    Active Habitat: Assess Risk

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    Failure risk of active habitat management

    Consider potential for lateral and vertical

    migration

    Look at aspect ratio and stream power

    4) Failure potential of habitat work

    Active Habitat: Assess Risk

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    Simulate Nature

    Consider naturalanalogs to guide

    restoration

    Consider historicalchanges to reference

    conditions

    Consider limitations

    to simulating nature

    Active Habitat: Simulate Nature

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    Benefits of Simulating Nature

    Only way to really restore multiple native

    species and multiple life stages

    **Over time, the river will win**

    Work with the rivers natural tendency Consider 50-year timeframe

    Active Habitat: Simulate Nature

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    What provides habitat in natural rivers?

    Active Habitat: Simulate Nature

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    Woody habitatprovides:

    Habitat cover

    Bed complexity Creates and maintains pools

    Habitat stability:

    Decreased erosive power

    wood only 2% of streambedarea, but accounted for 50%of the total flow resistance(Manga and Kirchner 2000)

    Active Habitat: Wood

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    Consider jump starting the riparian

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    Consider jump-starting the ripariansuccession

    plant trees

    It takes 80 to 150 years of tree growth before wood is

    sustainably recruited into river

    Active Habitat: Wood

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    How Long-Term Riparian Growth Helps Rivers

    Allows succession

    Provides cover

    Equilibrium channel

    stability

    Increases infiltration

    Reduces temperature

    Increases DO Reduces sediment

    Recruits woody habitat

    Photo by Tim WattsActive Habitat: Wood

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    Some Thoughts on Bank

    Stabilization

    What provides bank stability

    in natural rivers?

    Channel cross section dimensions

    more important to bank stability than

    what is on the banks

    Appropriate channel dimensionsallow use of vegetation for stability

    rather than heavy rock

    (assess infrastructure risk)

    Riffle X-Section at 83 on long profileDist FS HI elevation

    -3.4 4.27 100 95.73 2 feet up to top of slope, top of bank is ferns and rush-2.7 4.45 100 95.55

    5 10.96 100 89.04

    7.6 12.5 100 87.5

    9 13.7 100 86.3 bankfull-top of mini-point bar

    12.6 14.31 100 85.69 on point bar15 14.94 100 85.06 LEW

    18 15.52 100 84.48

    20.8 15.96 100 84.04 deepest point

    25.5 15.88 100 84.12

    30.3 15.73 100 84.27

    35.5 15.47 100 84.53

    40 14.99 100 85.01 REW

    42.3 13.71 100 86.29 grassy

    45.3 12.28 100 87.72 trees overhang

    47 11.51 100 88.49

    49.7 10.31 100 89.69

    56.3 9.02 100 90.98 slopes gently up to steep forested valley after 40 ft.

    North Fish Creek

    82

    84

    86

    88

    90

    92

    94

    96

    -10 0 10 20 30 40 50 60

    distance (ft.)

    elevation(

    ft.)

    Bank Stabilization

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    Erosion can occur

    in two stages:(where there is a large quantity

    of fine-grained sediment)

    Stage 1: Initialvertical erosion(headcutting)

    Stage 2: Long-term

    bank erosion

    Consider managing it

    in two stagesBank Stabilization

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    Two-Stage

    Process

    Slowly drainimpoundment to allow

    sediment to stabilize inplace

    Later, pull back banksto a more stable crosssection

    May be higher cost

    may need to mobilizetwice

    Bank Stabilization

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    Some Thoughts on Grade Control

    Grade Control

    Intro to

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    Intro toInstream

    Structures

    Grade control

    cross vanes, vortex

    weirs, W-weirs

    Instream habitatstructures

    J-hook

    vanes, wing deflectors,lunker structures

    Instream bankstabilization

    flow

    deflectors

    Grade Control

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    Some Grade Control Considerations

    Grade control can inhibit cleaning of bed material

    Grade control does not inhibit lateral migration

    It may take river out of context (simulate nature)

    Cross vanes create step-pools

    Step-pools only occur naturally at steeper slopes

    Remember stream power:

    Steep streams will create their own step-pools naturally

    Grade Control

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    Instream Structure Failures

    Mooney, et al. (2007) analyzed 127 instream structures:

    Found a 42% failure rate and 32% partial failure rate

    Frissell and Nawa (1992) analyzed 161 instream structuresfrom 1

    5 years old:

    Found 18.5% failure rate and 60% damage (impairment)rate

    Miller, et al. (2010) analyzed 391 instream structures in NorthCarolina:

    30% of structures were damaged, with cross vanes and

    double wing deflectors sustaining the most damage

    **Over time, the river will win**

    Grade Control

    Grade Control: Think Long-Term

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    Grade Control: Think Long-Term

    Because of failure rate, dont count on gradecontrol alone to protect at-risk infrastructure

    If grade control is critical to sediment

    management, consider that it will fail over time

    Consider deformable

    structures

    Plan for intentional failure

    Design rock sizes for a smaller flood such as 10-year or25-year floodGrade Control

    D i i M ki P f

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    Decision-Making Process for

    Applied Habitat Management

    1) What will happen if we do nothing

    besides remove the dam?

    -

    consider 50-100 year timeframe

    2) Assess risk (many types)

    3) Simulate nature if actively managing

    Summary of Habitat Management

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    Summary of Habitat ManagementSteps to Consider

    1) Remove full vertical extent of dam2) Remove enough width for banksand some floodplain3)

    Consider letting river reconstruct itsown habitat

    4)

    Consider jump-starting riparian

    succession (plant trees)5) If active management desired,consider using wood

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    For more information:

    Brian Graber, [email protected]

    Thank You!

    References

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    ReferencesAbbe, T.B. and Montgomery, D.R. 2003. Patterns and processes of wood

    debris

    accumulation in the Queets River basin, Washington. Geomorphology 51:81-107.Florsheim, J.; Mount, J.; and Chin, A. 2008. Bank erosion as a desirable attribute of

    rivers. BioScience 58(6):519-529.Frissell, C. and Nawa, R.K. 1992. Incidence and causes of physical failure of artificial

    habitat structures in streams of Western Oregon and Washington. North AmericanJournal of Fisheries Management 12:182-197.

    Manga, M. and Michael and Kirchner, J.W. 2000. Stress partitioning in

    streams by largewoody debris. Water Resources Research 36(8):2373-2379.

    Miller, J.C. and Kochel, R.C. 2010. Assessment of channel dynamics, in-stream structuresand post-project channel adjustments in North Carolina and its implications toeffective stream restoration. Environmental Earth Sciences 59:1681-1692.

    Miller, S.W.; Budy, P.; and Schmidt, J.C. 2010. Quantifying macroinvertebrate

    responses

    to in-stream habitat restoration: applications of meta-analysis to river restoration.

    Restoration Ecology 18(1):8-19.Mooney, D.; Holmquist-Johnson, C.; and Holburn, E. 2007. Qualitative evaluation of rock

    weir field performance and failure mechanisms. U.S. Bureau of Reclamation TechnicalServices Center.

    Palmer, M.A.; Menninger, H.L.; and Bernhardt, E. 2010. River restoration, habitatheterogeneity and biodiversity: a failure of theory or practice?

    Freshwater Biology

    55: 205-222.Thompson, D. 2002. Long-term effect of instream

    habitat-improvement structures on

    channel morphology along the Blackledge

    and Salmon Rivers, Connecticut, USA.

    Environmental Management 29(1):250-265.Stewart, et al. 2006. Does the use of in-stream structures and woody debris increase the

    abundance of salmonids? Centre for Evidence-Based Conservation Systematic ReviewReport No. 12.

    Thompson, D. 2006. Did the pre-1980 use of in-stream structures improve streams? Areanalysis of historical data. Ecological Applications 16(2): 784-796.