Christopher Lid Stone

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    Applied Geomorphology Hydrologic Design Considerations to theStabilization and Reclamation ofMining Disturbed Lands

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    30 Years: Changes in GeomorphicThought Applied to the Reclamation ofDisturbed Lands

    A Continuum of Changes Engineering approaches and hard fixes

    Riprap

    Concrete

    Steel

    To a pure Geomorphic approach, coupled with

    soft bio-fixes Vegetation retardance

    Template design

    Large Woody Debris

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    Permanent ChannelDiversion: Use of

    Culverts as Grade Controls

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    Failure of 1968 ChannelDiversion: Little Medicine

    Bow River

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    Downstream Impact ofFailed Channel

    Diversion

    Depth of Downcutting30 to 40 feet

    Two Deaths

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    Channel Breach into Mine Pit-Failed Levee

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    Revegetation Efforts to StabilizeFailed Breach

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    Three Phase Approach - Reclamationof Mining Disturbed Lands

    1. Qualitative Geomorphology

    2. Quantitative Engineering Analysis

    3. Final Design and Construction

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    Three Phase Approach - Reclamationof Mining Disturbed Lands-Phase 1

    1. Qualitative Geomorphic Evaluation of thePremining Landscape and Hydrologic Features

    Establish Design Basis for Channel Stability

    Controlling Variables in Slope Stability Define Your Mines Physical Position Within the

    Landscape

    Define Morphometric Parameters Which will beImportant in Predictive Modeling

    Consider Impact of Mining on Defined Variables

    Consider Opportunities

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    Drainage Pattern Analysis

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    Second Order Basin ReclamationCordero Mine

    (courtesy of Rio Tinto)

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    Field Data Collection

    Geomorphic Observations

    Existing Channel Geometry

    Natural Grade Controls and GeologicInformation

    Material Quality (overburden drilling)

    Topsoil Characteristics and Handling Flow Gaging and Rating

    Sediment Sampling (Bars and Banks)

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    SEDIMENT SAMPLINGArmor and Subarmor AnalysisWolman CountParticle Size Analysis

    Sediment Routing by Size FractionAtterberg Limits of Bank Material

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    Understanding the Importance ofSlope Morphology toErosion and Sedimentation

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    Acidic Spoils Slope OverlookingFailed Reclamation

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    Office Analysis of Data

    Historical Air Photograph Interpretation

    Base Mapping and Photogrammetry

    Horton Analysis of Basins

    Morphometric Analysis of Watershed

    Landform Stability Correlations to Gradient, SlopeAspect and Slope Shape

    USGS and Baseline Gaging Data (water andsediment)

    Soils Mapping Data

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    Historical Air Photo

    Analysis

    Review of HistoricalPatterns

    Planform

    Sinuosity, Length,Width

    Channel Geometry

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    Hydraulic GeometryCharacteristics

    Upstream (or Template)Reach

    Downstream Reach

    Reconstructed Reach

    Leopold and Maddock,

    1953 relationsVelocity vs. Discharge

    Top Width vs. Discharge

    Depth vs. Discharge

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    Three Phase Approach - Reclamationof Mining Disturbed Lands-Phase 2

    2. Detailed Engineering Analysis IntegratingGeomorphology with Hydraulic and SedimentTransport Analysis

    Hydrology and Geomorphic Models

    Integrate Previously Developed Baseline and GeomorphicTrend Data into Modeling Effort

    Earthwork Models (Digital Terrain Model) Balance Landscape and Land Feature Design with Mining

    Economics (earthworks, slope stability, haul distances andcost)

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    There is an Abundance ofCOMPUTER MODELS Out There!!

    Dont Let Your Pre-Occupation withImprovements in Numerical Methods, UserFriendliness or Other Peripheral Considerations

    Allow You to Lose Sight of REALITY

    REALITY IS THE PHYSICAL PROCESS OF

    LANDFORM DEVELOPMENT and ALLUVIALCHANNEL FORMATION

    Calibrate Your Model to Your PhysicalObservations!

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    Reality Check

    Calibration Use the baseline data, which you collected

    Compare hydrology against regional regressions, historicgaging

    Compare hydraulics to field or gaging data, known floodlevels or field observations

    Sensitivity Analysis

    Adjust select parameters like CN, mannings n, channelgrade or baselevel

    Vegetation retardance (early reclamation versus latereclamation)

    Verification Use monitoring data (sediment yield, profile changes)

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    Develop WatershedHydrology

    Example: 160 square mile basin Shirley Mountains to Shirley

    Basin

    Q100= 4721 cfs Q10=1438 cfs Q5= 783 cfs Q2=319 cfs

    Compared results to

    regional regressions andgage/basin area reductionmethods

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    Basin Delivery:Water and Sediment

    HEC RAS H d li St d

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    HEC-RAS Hydraulic StudyComparison of Reach

    Hydraulics

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    Three Phase Approach - Reclamationof Mining Disturbed Lands-Phase 3

    3. Final Engineering Design andConstruction

    Earthwork balance with defined balancepoints

    Simplicity

    Operator (contractor) buy-in Revegetation

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    Slope Shaping and Reclamation

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    Revegetation Efforts:Scarifying, Pitting and Seeding

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    Upper Reach West Fork Kicken Draw

    Caballo Rojo Mine, Powder River Basin

    Final Reclamation of Mine

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    Final Reclamation of MinePit Impoundment

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    Reconstructed Wetlands-Cordero MinePowder River Basin

    Little Medicine Bow

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    Little Medicine BowAbove Reclamation Area

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    Reconstructed Little Medicine Bow River

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    Little Medicine Bow River5 Years Later

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    Little Medicine Bow River12 Years Later

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    Questions??

    Develop Design Concept: Sediment Transfer andPressure Relief

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    Pressure Relief

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