Debasis- Tidal Energy

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    Background

    Tides, the daily rise and fall of ocean levels relative to

    coastlines, are a result of the gravitational forces of

    the moon and sun as well as the revolution of the

    earth. The principle of harnessing the energy of tides

    dates back to as early as the Middle Ages, when the

    phenomenon of tides was not yet explained and were

    used to turn waterwheels, producing mechanical

    power. A large amount of energy is stored in tides

    and it is possible to tap into this renewable resource

    with tidal power plants. Tidal electricity generation

    involves the construction of a barrage across a delta,

    estuaries, beaches, or other places that are affected

    by the tides .

    Tidal power is a means of electricity generation achieved

    by capturing the energy contained in moving water mass

    due to tides. Two types of tidal energy can be extracted:

    kinetic energy of currents between ebbing and surging tides

    and potential energy from the difference in height (or head)

    between high and low tides. The former method - generating

    energy from tidal currents - is considered much more

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    feasible today than building ocean-based dams or barrages,

    and many coastal sites worldwide are being examined for

    their suitability to produce tidal (current) energy.

    One method of extracting tidal energy involves building a

    barrage and creating a tidal lagoon. The barrage traps a

    water level inside a basin. Head is created when the water

    level outside of the basin or lagoon changes relative to the

    water level inside. The head is used to drive turbines. In any

    design this leads to a decrease of tidal range inside the basin

    or lagoon, implying a reduced transfer of water between the

    basin and the sea. This reduced transfer of water accounts

    for the energy produced by the scheme.

    Tidal power is classified as a renewable energy source,

    because tides are caused by the orbital mechanics of the

    solar system and are considered inexhaustible within a

    human timeframe. The root source of the energy comes from

    the slow deceleration of the Earth's rotation. The Moon gains

    energy from this interaction and is slowly receding from the

    Earth. Tidal power has great potential for future power and

    electricity generation because of the total amount of energy

    contained in this rotation. Tidal power is reliably predictable

    (unlike wind energy and solar power). In Europe, Tide Mills

    have been used for nearly 1,000 years, mainly for grinding

    corn.

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    The efficiency of tidal power generation in ocean dams

    largely depends on the amplitude of the tidal swell, which

    can be up to 10 m (33 ft) where the periodic tidal waves

    funnel into rivers and fjords. Amplitudes of up to 17 m (56 ft)

    occur for example in the Bay of Fundy, where tidal

    resonance amplifies the tidal waves.

    As with wind power, selection of location is critical for a tidal

    power generator. The potential energy contained in a

    volume of water is

    E = xMg

    where x is the height of the tide, M is the mass of water and

    g is the acceleration due to gravity. Therefore, a tidal energy

    generator must be placed in a location with very high-

    amplitude tides. Suitable locations are found in the former

    USSR, USA, Canada, Australia, Korea, the UK and other

    countries (see below).

    Several smaller tidal power plants have recently started

    generating electricity in Norway. They all exploit the strong

    periodic tidal currents in narrow fjords using sub-surface

    water turbines.

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    Basically there are thre methods of operation that can be

    performed in order to harness the tidal energy, which are as

    follows :-

    KINETIC ENERGY

    POTENTIAL ENERGY

    OTEC

    The details of the above methods are given below

    Another form of ocean energy is called tidal energy. When

    tides come into the shore, they can be trapped in reservoirs

    behind dams. Then when the tide drops, the water behind

    the dam can be let out just like in a regular hydroelectric

    power plant.

    In order for this to work well, you need large increases in

    tides. An increase of at least 16 feet between low tide to

    high tide is needed. There are only a few places where this

    tide change occurs around the earth. Some power plants are

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    already operating using this idea. One plant in France makes

    enough energy from tides to power 240,000 homes.

    The further categorization of the potential energy are :-

    Ebb generation

    Flood generation

    Pumping

    Two basin model

    Ebb method of generation of power from tides

    The basin is filled through the sluices and freewheeling

    turbines until high tide. Then the sluice gates and turbine

    gates are closed. They are kept closed until the sea level

    falls to create sufficient head across the barrage and the

    turbines generate until the head is again low. Then the

    sluices are opened, turbines disconnected and the basin is

    filled again. The cycle repeats itself. Ebb generation (also

    known as outflow generation) takes its name because

    generation occurs as the tide ebbs

    Flood method of generation of power from tides

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    The basin is emptied through the sluices and turbines

    generate at tide flood. This is generally much less efficient

    than ebb generation, because the volume contained in the

    upper half of the basin (which is where ebb generation

    operates) is greater than the volume of the lower half (the

    domain of flood generation). This is compounded by the fact

    that there is usually a river flowing into the basin, filling the

    basin as the tide rises and making the difference in levels

    between the basin side and the sea side of the barrage (and

    therefore the available potential energy) less than it wouldotherwise be. This is not a problem with the lagoon model:

    the reason being that there is no current from a river to slow

    the flooding current from the sea.

    Pumping

    Turbines can be powered in reverse by excess energy in the

    grid to increase the water level in the basin at high tide (for

    ebb generation and two-way generation). This energy is

    returned during generation.

    Two basin method

    With two basins, one is filled at high tide and the other is

    emptied at low tide. Turbines are placed between the basins.

    Two-basin schemes offer advantages over normal schemes

    in that generation time can be adjusted with high flexibility

    and it is also possible to generate almost continuously. In

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    normal estuarine situations, however, two-basin schemes

    are very expensive to construct due to the cost of the extra

    length of barrage. There are some favourable geographies,

    however, which are well suited to this type of scheme.

    The major draw back of the potential energy method is that it requires large investments

    and the environmental impact of this method is large .

    What are the current developments in the Tidal

    Energy technology?

    For many hundreds of years tiny amounts of this energy source have

    been harnessed for agricultural purposes. In more recent years variousriver and estuary schemes have been proposed where the opportunity

    of generating electrical power in close proximity to the energyconsumer is recognised. However with a couple of notable exceptions,

    these tidal barrage schemes have stalled due to concerns related tothere environmental impact. Within the UK the Severn Estuary has

    been extensively considered as a potential site for a tidal barrage

    scheme, the grandest proposal for a 6.8 GW development scheme wasabandoned in 1987.

    Within the last decade interest has concentrated upon the offshore

    tidal resource with several development teams achieving large scaleprototype deployment in real marine

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    Kinetic energy (movement) exists in the moving waves ofthe ocean. That energy can be used to power a turbine. In

    this simple example, to the right, the wave rises into a

    chamber. The rising water forces the air out of the chamber.

    The moving air spins a turbine which can turn a generator.

    When the wave goes down, air flows through the turbine and

    back into the chamber through doors that are normally

    closed.

    This is only one type of wave-energy system. Others actually

    use the up and down motion of the wave to power a piston

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    Intermittent nature of power output

    Tidal power schemes do not produce energy 24 hours a day.

    A conventional design, in any mode of operation, would

    produce power for 6 to 12 hours in every 24 and will not

    produce power at other times. As the tidal cycle is based on

    the period of revolution of the Moon (24.8 hours) and the

    demand for electricity is based on the period of revolution of

    the Sun (24 hours), the energy production cycle will not

    always be in phase with the demand cycle. This causes

    problems for the electric power transmission grid, as

    capacity with short starting and stopping times (such as

    hydropower or gas fired power plants) will have to be

    available to alternate power production with the tidal power

    scheme

    The energy from the sun heats the surface water of the

    ocean. In tropical regions, the surface water can be 40 or

    more degrees warmer than the deep water. This

    temperature difference can be used to produce electricity.

    The OTEC system must have a temperature difference of at

    least 25 degrees Celsius to operate, limiting use to tropical

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    regions. Hawaii has experimented with OTEC since the

    1970s. There is no large-scale operation of OTEC today.

    There are many challenges. First, the OTEC systems are not

    very energy efficient. Pumping water is a giant engineering

    challenge. Electricity must also be transported to land. It will

    probably be 10 to 20 years before the technology is

    available to produce and transmit electricity economically

    from OTEC systems.

    Advantages

    Once you've built it, tidal power is free.

    It produces no greenhouse gases or other waste.

    It needs no fuel.

    It produces electricity reliably.

    Not expensive to maintain.

    Tides are totally predictable.

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    Offshore turbines and vertical-axis turbines are not

    ruinously expensive to build and do not have a large

    environmental impact.

    Local environmental impact

    The placement of a barrage into an estuary has aconsiderable effect on the water inside the basin and on thefish. Lagoons, on the other hand, could be used for fish orlobster farming, adding to their economic viability.

    Turbidity

    Turbidity (the amount of matter in suspension in the water)

    decreases as a result of smaller volume of water being

    exchanged between the basin and the sea. This lets light

    from the Sun to penetrate the water further, improving

    conditions for the phytoplankton. The changes propagate up

    the food chain, causing a general change in the ecosystem.

    Pollutants

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    Once again, as a result of reduced volume, the pollutants

    accumulating in the basin will be less efficiently dispersed.

    Their concentrations will increase. For biodegradable

    pollutants, such as sewage, an increase in concentration is

    likely to lead to increased bacteria growth in the basin,

    having impacts on the health of the human community and

    the ecosystem.

    The concentrations of conservative pollutants will also

    increase.

    Tidal energy is the energy of the future and lots of research

    are needed to be done on it and bench marks are to be set

    so that the generation of the power form this source is

    environmental friendly as well as its economical.

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