Wave and Tidal Energy Richard Gorman National Institute of Water - PowerPoint PPT Presentation
Maori and the Sustainable Energy Business 3-4 August 2005, Taupo Wave and Tidal Energy Richard Gorman National Institute of Water and Atmospheric Research Contents Waves and tides Tidal energy technologies The NZ tidal energy
Maori and the Sustainable Energy Business – 3-4 August 2005, Taupo Wave and Tidal Energy Richard Gorman National Institute of Water and Atmospheric Research
Contents • Waves and tides • Tidal energy technologies • The NZ tidal energy resource • Wave energy technologies • The NZ wave energy resource • Summary
Waves and tides • Tides vary on time scales of 6-12 hours (diurnal, semi-diurnal) • Surface wind-waves have periods of a few seconds • Tides are driven by gravitational attraction of moon and sun • Waves are created by winds blowing over the ocean
Tidal energy conversion • Underwater turbines • Hydroplane devices technologies • Tidal barrage
Rance Estuary Tidal Barrage • Rance Estuary, Brittany, France • Construction began in 1960, completed in 1967 • Dam length 330 m 22 km 2 basin • • Tidal range of 8m • Lock to allow passage for small craft • 24 turbines, each 5.4m diameter rated at 10MW were connected to the 225kV French Transmission network. • Bulb Turbines allow generation on both ebb and flood tides. • Turbines can also pump water into the basin • Total capacity 240MW, connected to French national grid • http://www.edf.fr
Tidal Power – SeaFlow turbine • Marine Current Turbines Ltd (UK) • Pilot plant installation in the Bristol Channel • horizontal axis turbine • http://www.mct.com
Tidal Power : Rotech Turbine • Rotech Tidal Turbine (RTT) • Bi-directional venturi shaped duct • Symmetrical turbine blades • Works with off-axis flows (<40 ° ) • Hydraulic transmission to generator • Power cable to shore • 1MW Prototype •http://www.lunarenergy.co.uk
Tidal Power - ENERMAR • Vertical axis Kobold turbine • Carbon fibre turbine blades • Turbine diameter 6 metres • blade span 5 metres • chord 0.4 metres • Floating platform diameter 10 metres • depth 2.5 metres • draft 1.5 metres • Mooring 4 concrete anchoring blocks
Tidal Power - ENERMAR
Messina Strait • Average tidal • 20 kW power current 2 m/s ENERMAR - output
Tidal Power: Stingray Hydroplane Device • Parallel linkage holding large hydroplanes • The angle of these hydroplanes to the flow of the tide is varied causing them to move up and down. • Motion pumps high- pressure oil in a cylinder • Hydraulic drive to an electric generator • http://www.engb.com
Tidal Power: Stingray Hydroplane Device
Measurement and prediction of tides • How do we measure tides around New Zealand? • How can we use modelling to extend the available data? • Where is the best potential for tidal power generation?
NIWA sea level network
Moturiki Is. sea level record
Tidal model of New Zealand’s EEZ
Wave energy conversion technologies • Tapered channel • Oscillating water column • Heaving buoy device • Other floating systems
Tapered Channel (TAPCHAN) A collector • concentrates incoming waves • The converter is a gradually narrowing channel in which waves increase in height • Waves overtop into a reservoir. • Hydraulic head drives flow through a turbine
The TAPCHAN at Toftestallen, Norway
Mighty Whale
Oscillating Water Column Device • Wavegen Limpet 500, Islay (Scottish west coast) • Wave capture chamber set into the rock face. • The waves cause the air in the chamber to alternately compress and decompress • Moving air drives a bidirectional Wells turbine • Presently supplying 0.5MW of power to the grid • http://www.wavegen.co.uk
Energetech OWC device • Parabolic wall focuses waves • Oscillating water Column • Dennis-Auld air turbine
Energetech OWC device - Port Kembla • Installed & tested June 2005 • Weight: 485 tonnes • 36 metres long, 35 metres wide • Will be connected to the local power grid by an 11kV cable. • Expected to produce at least 500 MWh of energy per annum. • http://www.energetech.com.au
Pendulor • Rectangular box, which is open to the sea at one end. A hinged pendulum flap swings back and forth with wave action. • Power take off through a hydraulic pump and generator. • A 15 kW prototype was tested in Muroran, Japan .
Archimedes Wave Swing • Float moves up and down relative to a fixed pontoon due to wave-induced pressure changes • Interior of the system is pressurised with air • The air spring, together with the mass of the moving part, is resonant with the frequency of the wave. • Power take off through a linear electrical generator and a nitrogen-filled damping cylinder.
Offshore device – Power Magnet Linear Generator • Works by electromagnetic induction • An electric coil fixed to the buoy, moving to a magnetic shaft anchored to the sea floor. • Each buoy could potentially produce 250 kilowatts of power • http://www.wave- energy.net/RTD/ProjDescriptions/I PS.htm
Offshore device - OPT PowerBuoy • Buoy moves up and down with the wave motion. • The resultant mechanical stroking drives the electrical generator. • The generated AC power is converted into high voltage DC and transmitted ashore via an underwater power cable. •http://www.oceanpowertechnologie s.com
Offshore device - OPT PowerBuoy
Offshore device - Pelamis • Semi-submerged, articulated structure composed of cylindrical sections linked by hinged joints. • The wave-induced motion of these joints is resisted by hydraulic rams that pump high-pressure oil through hydraulic motors. • The hydraulic motors drive electrical generators to produce electricity. • Umbilical cable to a junction on the seabed. • Several devices can be linked to shore via a single sub-sea cable. •http://www.oceanpd.com
Wave information for assessment of energy potential • How can we assess the wave climate at a given location? • How can we use modelling to extend the available data? • What variability can be expected in wave energy over various time scales? • How can we best predict wave conditions?
Datawell directional waverider buoy Accelerometers measure in x, y, z directions Integrated to give orbital velocities and x, y, z displacements Computes directional wave spectral estimates
Wave buoy data (> 1 year duration) directional non-directional
Wave buoys (present) non-directional directional
Wave statistics H T significant wave height H 1/3 = average of highest 1/3 of waves zero-crossing period T z = average of all periods
Satellite altimeter wave data A radar altimeter GEOSAT measures wave height from the spread in the return signal. Missions: SEASAT (1978) GEOSAT (1985- 1989) ERS1 & ERS2 (1991+) Topex/Poseidon (1992+)
Significant wave height from Topex/Poseidon altimeter
Wave measurement from X-band radar • WaMoS II system connected to a commercially available marine X-Band radar • Determines directional wave and surface current information from the sea clutter (up to 3 miles from the antenna )
Wave measurement from X-band radar Sea surface elevation map Radar image (sea clutter)
WAM wave generation model
New Zealand regional WAM model • spatial grid: 1.125° × 1.125° lat/lon • spectral grid 25 wave frequencies × 24 wave directions • windfields input from ECMWF reanalysis
New Zealand regional wave hindcast • A model has been established to simulate wave generation for the New Zealand region. • The model simulates deep water waves processes - wind forcing, propagation, whitecap dissipation, and nonlinear interactions. • The model has been used to hindcast 20-years (1979-1998) of deep water wave conditions at 1.125° resolution. • The hindcast has been validated against buoy and satellite data.
Hindcast: mean wave height and direction Satellite data: mean Hsig (m) 20°S 2.0 2.5 30°S 2.5 3.0 3.0 40°S 3.5 3.5 50°S 4.0 4.0 60°S
Hindcast: mean wave energy flux
Hindcast data near the coast • The hindcast is derived from a deep-water model, at relatively coarse resolution. • Most applications of hindcast data are near the coast. • The model needs to be validated against measurements, generally obtained near the coast.
Foveaux Strait buoy - 1989 Wave height from buoy and filtered WAM hindcast 8 model 7 buoy 6 Foveaux Str. buoy 5 Hsig (metres) 100 m water depth 4 3 2 1 0 21 May 10 Jun 30 Jun 20 Jul 9 Aug 29 Aug 18 Sep
Assessment of wave energy potential at Waipoua, Northland • Part of a study of renewable energy potential for remote communities • Wave energy flux was computed from WAM 20-year hindcast, for a site off the Northland coast • Work also includes wave data collection and nearshore wave refraction modelling
Wave energy flux at Waipoua Site 11 (−35.689,173.472) refracted to 30m 15 Flux Magnitude (kW/m) mean: 19.236 std. dev.: 22.531 min: 0.378 max: 514.890 % Occurrence 10 % Occurrence 5 0 0 10 20 30 40 50 60 70 80 90 100 |energy flux| (kW/m) 30m depth energy flux (kW/m)
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