18-tidal energy

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    Tidal action caused by gravitational effectsof moon and sun on earths oceans.

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    Common tidal energy system is a barragesystem as shown in the following slide.

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    250 m

    200 m

    barrage

    Top view

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    F ront view

    12 m

    6 m

    High tide

    Low tide

    turbine blades

    4 m

    20 m

    200 m

    4 m

    8 m

    3 m

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    High tide depth (h) = 6 m Width = 200 m Length = 250 m

    Depth of water at low tide = 12

    mSeawater V !1027 kg/m 3Tidal period = 1 2 hrsArea behind barrage (A) = 200 m x 250 m = 50,000 m2

    Estimate of total energy stored at high tide (assuming allmass is located at mid- high tide depth (11 m):

    2 8 2 23 2

    9

    h 1E = mass water g A h g h

    2 21 1 kg m

    A g h 1 0 m 1 027 9 .81 (3 m)2 2 m sec

    E 2 .27 x10 joules = 6 29 .7 kWhr.

    ! ! !

    !

    V

    V

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    Assume power generated only during ebb tide(flow out). Time of flow out = 6 hrs.

    Assume all water stored during flow in isdischarged during ebb tide

    Volume of water stored during inflow:

    V = 6 m ( 250 m x 200 m) = 3 x 1 05 m3

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    Assume average flow rate out of barrage is given by:

    5V mF 5 x 1 0 6 hrs hr

    ! !

    Assume all of this flow passes through the barrageopening of 20 m by 4 m. Let a = 20 m x 4 m = 8 0 m2

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    Average fluid velocity through this opening is given by:

    v = F /a = ( 5 x 1 04 m3/hr)/8 0 m2 = 625 m/hr

    In this opening there will be 5 turbine generators with bladeradius equal to 2 ft.

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    Turbine power equation (same as for wind

    turbine) for each turbine generator is:

    3t

    t

    2t

    1P A v

    2A area covered during rotation of rotor blades.

    A = r

    r length single blade

    ! !

    !

    V

    T

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    32

    3

    total

    total

    1 kg mP ( 2 m) 1 027 625 34w

    2 m hr

    F or 5 turbines , P 5 P 16 9w

    Total Energy for one tidal cycle

    = P 6 hr 0 .20 3 kWh

    ! T !

    ! !

    !

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    Power calculations for tidal currents andunderwater turbine generators:

    Assumptions:

    3

    mTidal current (v) 0 .1sec

    Turbine blade radius (r) 5 m

    kgeawater density ( ) 1 027 m

    y

    y

    y V

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    2 3 2 33

    1 1 kg mP r v ( 5 m) 1 027 (0 .1

    P 4 0

    )2 2 m sec

    (per turbine genew rator)

    ! T V ! T

    !

    F airly low power output , but can run 24 hrs aday in all weather (tidal currents are reasonablyconstant)

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    F or comparison a person riding a bicyclewith the rear wheel linked to a generator canproduce about 75 watts of electricity. Theproblem is that most people cant keep thisup for more than an hour.

    (A possibility for Appledore is to open arecreation/fitness center with 1 0 or 1 5 bikes

    connected to generators).

    By contrast Lance Armstrong can generate500 watts --- but only for 20 minutes

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    In all of these options energy is lost in thetransfer from mechanical to electricalenergy. Typical efficiency of the overall

    processes is 4 0 50% .

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    O ther ocean power options includecapturing wave energy. Some of theseoptions are shown in the following slides.

    There are only a few of these schemes inactual operation so there is not sufficientdata to assess their effectiveness plusAppledore Island generally doesntexperience significant wave action.

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    ShoreO cean

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