7 Reservoirs and Dams

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    Dams and reservoirs

    Dams

    Types

    Forces on a dam

    Geology and dam sites Rock types and dams

    Dams on soils

    Ground improvement

    Reservoirs

    Site selection

    Leakage from

    reservoirs

    Sedimentation

    Stability: effect ofraised WT

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    Dams and reservoirs - literature

    Bell F.G., Engineering geology andgeotechnics

    Ch 6 (Reservoirs)

    Ch 7 (Dams)

    Blyth F.G.H. and de Freitas M.H., Ageology for engineers

    Ch 14 (Reservoirs and dams)

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    Reservoirs: purpose

    Water storage Flood prevention

    Power

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    Reservoirs: site selection

    Hydrological considerations

    Fundamental controls topography

    climate geology

    Water

    added

    Net amount of water

    available for storage

    Water

    subtracted+

    Rainfall in river

    basin

    Infiltration

    EvaporationTranspiration

    Runoff

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    Reservoirs: leakage

    - -WateraddedWater

    subtracted

    Net amount of water

    available for storageLeakage from

    reservoir

    Rainfall in

    river basin

    Infiltration

    EvaporationTranspiration

    Runoff

    1. Dam bypass

    2. Water table effects

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    Reservoirs: leakage

    Leakage via subsurface bypass due to siphon effect

    Devonian strata

    Devonians

    trata

    Devonian strata

    Dol-y-gaer dam

    Carboniferous strata:

    Subsurface water flow

    reservoir level

    fracture and dissolution

    flow routes

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    Reservoirs: leakage

    Leakage buried channels beneath drift

    50 km

    Modern river/valley

    Ancient river/valley

    RDrac

    Sautet

    dam and

    reservoir

    Bypass of reservoir in drift

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    Reservoirs: water table leakage-1

    landsurface

    watertable

    river

    beforewater table divide

    Bedrock with a water

    table and finite

    permeability

    reservoir

    Leakage to next valleynew

    water

    table

    after

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    Reservoirs: water table leakage-2

    Landsu

    rface

    river

    High

    permeability

    layer

    Water table in aquifer

    before

    Bedrock with low

    permeability: aquiclude

    reservoir

    after

    High

    permeability

    layer

    Modified water table in aquifer

    Leakage to next valley

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    Reservoirs: sedimentation

    Worlds largest dam;

    180m tall, 2km wide 84% sediment in rainy

    season (june-sept)

    drawdown andsediment sluicing

    during this period

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    Reservoirs: raised water table

    Before

    Water table

    river

    After - 1

    reservoir Raised water table

    After - 2

    reservoirFailure and

    slumping

    due to

    weakened

    rock mass

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    Viaont dam disaster, Italy

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    Reservoirs: raised water table

    s = c + . (n - p)

    p = pore fluid pressuren p = effective stress

    1,WT3, WT

    UnstableStable

    13

    Shearstresss

    Raising water table

    Normal stress n

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    Dams: types Gravity dam: rigid monolithic structure

    Trapezoidal cross section

    Minimal differential movement tolerated

    Dispersed moderate stress on valley floor and

    walls

    Arch dam: high strength concrete wall

    Convex faces upstream

    Thin walled structure

    Relatively flexible

    Huge stresses imposed on valley walls and floor

    Earth dams: bank or earth or rock withimpermeable core

    Core of clay or concrete, extended below ground

    Sand or gravel drains built to cut fluid pressure

    Low stress applied to valley floor and walls

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    Types of dam

    Arch Buttress

    Embankment

    or Earth

    Gravity

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    Emosson Dam, Switzerland

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    The Vaiont dam today

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    Dams: forces applied

    Vertical static forces Lateral force applied by water body

    Dynamic forces

    wave action

    overflow of water (controlled by spillway

    channels) earthquakes and tremors

    ice/freezing

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    Dam failure: earthquake

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    Dam failure: asteroids

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    Dam failure: bombs

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    Dam sites: geology

    Poor geological characterisation of dam foundation

    responsible for 40% of dam failures

    Need proper site investigation

    D d i t

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    Dams: ground improvement

    Poor geological conditions can be improved in 2 ways improving load bearing properties

    controlling seepage

    gravel sand silt clay

    >10 2 0.07 0.002

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    Dams: ground improvement

    Rock bolts

    Rolling and preloading compresses ground in prep for structure

    improves post dam compaction

    Gravity drainage and well points: sand and gravel channels and shallow wells (for pumping) Electro-osmosis: insert conductionrods into fine grained clay-rich bedrock and have an electric field - de-waters ground via theflow of electric current

    Vibroflotation mechanical vibrating plate with load compresses low density gravels and sands

    Explosives useful in water-saturated gravel and scree increases bulk density

    Grouts material injected into the ground

    Chemical treatments

    react solutions injected into ground. React with material to alter properties. NaCl solutioninjected into smectite-rich mud, shale etc. to alter expansivity of smectite stabilizes groundpre-construction

    Thermal treatment Freezing with injected liquid N2 to consolidate loose ground during excavation. Heatingby

    burning petroleum under pressure in subsurface causes thermal metamorphism - hardensground and cuts porosity

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    Injected

    grout curtain

    Pre-stressed

    anchors

    Drain

    Apron drains (to

    individual aquifers)

    Excavationto rock

    Regolith

    Reservoir

    Rip

    rap

    tok

    ill

    wave

    energy

    Hard face to dam

    Aquifer layers

    Aquiclude layers

    Core and rear of dam