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Targeting Practices -- Lesson from the Pecatonica River Watershed

Jun 01, 2018

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    Rapid Channel Assessments

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    Rapid Channel AssessmentsSediment Fingerprinting

    Outlet USGSgaging station

    In-situ suspendedsediment sampler

    * DNR biology

    Rapid channelassessment

    (Background of Field P Index)

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    Bank Erosion/Lateral Recession Rates

    Lateral RecessionRate ft/yr(cm/yr) Category Description

    0.01-0.05(0.3 - 1.5)

    Slight Some bare bank but active erosion not readily apparent. Some rillsbut no vegetative overhang. No exposed tree roots.

    0.06-0.2(1.8 – 6.0)

    Moderate Bank is predominantly bare with some rills and vegetativeoverhang. Some exposed tree roots but no slumps or slips.

    0.3-0.5(7.0 – 15)

    Severe Bank is bare with rills and severe vegetative overhang. Many exposed

    tree roots and some fallen trees and slumps or slips. Some changes incultural features such as fence corners missing and realignment ofroads or trails. Channel cross section becomes U-shaped as opposed toV-shaped.

    0.5+(>15)

    Verysevere

    Bank is bare with gullies and severe vegetative overhang. Manyfallen trees, drains and culverts eroding out and changes in culturalfeatures as above. Massive slips or washouts common. Channelcross section is U-shaped and stream course may be meandering.

    WI NRCS technical document (2003)

    Bank retreat rate this study = 4.1 cm/yr based on Fever River/Pioneer Farm 2004-07

    P I l t ti W t h d S di t B dg t

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    UPLAND SOIL EROSION0.8 tons/ac/y

    FINE SEDIMENTSAVINGS AND LOAN

    1.2 tons/ac

    Pre-Implementation Watershed Sediment BudgetPleasant Valley Outlet/USGS Gage

    BANK EROSION0.06 tons/ac/y

    ANNUAL WATERSHEDEXPORT (GAGE)0.14 tons/ac/y

    (2006 -10 data, various sources)

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    Suspended Sediment Loads

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    010

    2030405060708090

    100

    R e

    l a t i v e C o n t r i b u t i o n

    ( % )

    Stream Banks

    Woolands

    Agriculture

    Lamba, et al., 2014

    Woodlands

    Streambanks

    Suspended Sediment LoadsFingerprinting/Source Apportionment

    Outlet/USGS Gage

    44

    2010 2011 2012Average = 30% eroding banks, 70% upland agriculture

    In situ suspendedsediment samplersphoto: Curt Diehl

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    0

    100

    200

    300

    400

    500

    600

    P a r t i c u

    l a t e B o u n

    d P

    L o a

    d (

    l b s

    )StreambanksWoodlandsAgriculture

    Particulate P in Suspended SedimentFingerprinting/Source Apportionment

    45

    2010 2011 2012Average = 30% eroding banks, 70% upland agriculture

    In situ suspendedsediment samplersphoto: Curt Diehl

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    Bank ErosionPre-Implementation Sediment Budget (2009)

    Grazed/feeding areas

    Barnyard/night pasture

    Kittleson Valley bank erosion photo: Curt Diehl

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    Barnyard/Night Pasture

    2009 Pre-implementation 2012 Post-implementation

    Barnyard: Clean Water Diversion, Heavy UseArea Protection, Vegetative TreatmentStrips, Fence, Roof Runoff, Milkhouse WasteTreatment System, Animal Trail and Walkway

    P Savings fromchannel = ~16 lb/yr

    2009 Phosphorus Concentrations

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    Barnyard/night pasture

    (no fine sedimentdeposition in the othertwo grazed feedingareas)

    2009 Phosphorus ConcentrationsEroding Bank and Fine Sediment

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    Grazed woods/feeding area

    2009 Pre-implementation

    [Stream bank protection from over-grazing, trampling; Feeding area moved]

    2012 Post-implementation

    P Savings = ~25 lb/yr

    Ph h i Fi S di t D iti

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    Phosphorus in Fine Sediment DepositionPre-Implementation (2009)

    0

    200

    400

    600

    800

    1000

    1200

    1400

    0 10 20 30

    T P i n F i n e

    S e d i m e n t D e p o s i t i o n

    ( l b s / m

    i )

    Drainage area (square miles)

    Concentration Storage

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    Pleasant Valley Delisted

    Trout photo credit: Curt Diehl

    [Gaged reach had boxelder removed and bank toeriprapping in 2006]

    d d h l

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    • A sediment budget and fingerprinting approach werehelpful for estimating channel sources and sinks of finegrained sediment and P.

    • On average, agriculture makes up the majority of thesource of suspended sediment at the outlet (~70%).

    • Relative contributions of P from bank erosion areseason/flow dependent.

    • There is about 8 yrs worth of annual export ofsuspended sediment stored in soft sediment deposition.

    • Targeted rehabilitation work in channels is important – need information on riparian land use history andlongitudinal continuum of legacy erosion/deposition.

    Coon Creek Restoration,October 2010

    Targeted Conservation and Channel ProcessesPleasant Valley Experience

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    STUDY PARTNERS, ASSISTANCE, AND FUNDINGDane County, Land Conservation DivisionIowa County Land Conservation DepartmentGreen County Land Conservation DepartmentUniversity of Wisconsin-MadisonUniversity of Wisconsin-ExtensionU.S. Geological SurveyUSDA Natural Resource Conservation ServiceWisconsin DNRWisconsin Department of Agriculture, Trade, and Consumer ProtectionThe Nature ConservancyLandowners and FarmersMonsanto CorporationMcKnight FoundationUSGS cooperative program

    Research funding provided by USDA-NIFA award #2009-51130-06049

    Questions?

    Contact: Faith Fitzpatrick [email protected], 608-821-3818

    Acknowledgments