Renewable Energy from the Ocean.
Transcription
Renewable Energy from the Ocean.
Renewable Energy from the Ocean North Carolina’s Coastal Conference Billy L. Edge North Carolina State University – CCEE UNC-Coastal Studies Institute 14 April 2015 Why pursue renewable ocean energy? There are substantial global resources available Energy (TWh) Source 20,205 U.S. Energy Information Administration (2010) International Energy Statistics. http://www.eia.gov 32,000 Mørk, G, Barstow, S., Pontes, M. T, Kabuth, A., (2010). Assessing the Global Wave Energy Potential, submitted to OMAE 2010, Shanghai, China, 2-6 June 2010. Theoretical global tidal range resources 7,800 Estefen, S. (2012). Ocean Energy in View of the IPCC Report with an Emphasis on Brazilian Activities. Thirteenth Meeting of the United Nations Open-Ended Informal Consultative Process on Ocean and the Lawn of the Sea. Theoretical global ocean current resources 5,000 Global electricity demand (2011) Theoretical global wave resources Outline 1. Legislative Mission 2. MHK 3. Strategic Research Directions 4. 30-Year Wave Hindcast 5. Summary Legislation Mission Use renewable ocean energy wisely to effectively and economically fulfill part of the energy needs of North Carolina and in the process create jobs and economic opportunities. UNC Coastal Studies Institute North Carolina State University UNC Charlotte NC A&T UNC – IMS UNC – Chapel Hill Renaissance Computing Institute RME, SEMREC, Verdant, TAMU, Johns Hopkins Renewable ocean energy? Renewable energy available in the waters of Earth’s oceans: • Ocean Thermal Energy Conversion (OTEC) temperature differences between warm surface waters and cold deep waters • Salinity Gradient - differences in salinity concentrations between fresh waters and the saline water that they run in to • Marine Hydrokinetic Energy (MHK) movement of water in waves, tidal currents, and ocean currents Wave energy device technologies Attenuator Surge converter Point absorber Oscillating water column Bulge Overtopping terminator Submerged pressure differential Rotating mass Animation source: http://www.emec.org.uk/marine-energy/ Ocean Power Technologies - PowerBuoy Source: http://www.oceanpowertechnologies.com/tech.htm PowerBuoy® 40 kilowatt Utility scale, Grid Compatible Wave Energy Resource Objective Develop high resolution 30 year hindcast Estimate extreme wave conditions Provide results in GIS and HTML framework Rationale Information to attract developers Requires high resolution NC data ADCIRC-UnSwan Courtesy: CORPS, NCSU, CSI & RENCI Wave Energy (1999 Floyd) ADCIRC+SWAN Current energy device technologies Oscillating hydrofoil Horizontal axis turbine Archimedes screw Enclosed Venturi tips Vertical axis turbine Tidal kite Animation source: http://www.emec.org.uk/marine-energy/ Tidal Energy Strategic Directions 1. Magnetic Gears for PTO 2. Ocean Compressed Air Energy Storage 3. Environmental, Regulatory and Environmental Assessment 4. Gulf Stream Power Support for Jennette’s Pier Research Special Projects Drawbacks of Mechanical Gears for Marine Hydrokinetic Power Generation • Reliability (physical contact between gears) • Requires lubrication and maintenance • Vibration and acoustic noise • No overload protection • Failures are often catastrophic • Short operating life time 13 A Flux Focusing Magnetic Gearbox • Magnet’s field directed along angular direction • Approach increases the field within the air-gap 2-D model of a flux focusing magnetic gear with p1=4 pole-pairs, n2=17 steel poles and p3=13 pole-pairs on outer cylinder. 1:4.25 gear ratio. Experimental Testing Stationary outer rotor Inner rotor Cage rotor Torque transducer on high speed end 3-phase generator on high speed end Magnetic gear box Torque transducer on low 3-phase motor on low speed end speed end 15 Intermittent power to meet baseload using storage Daily wave power generated Excess To storage From storage Daily electricity demand Storage: Compressed Air Energy Storage (CAES) Ocean Compressed Air Energy Storage Courtesy: Dr. Mohammad Gabr, NCSU OCAES SYSTEM – OIL/GAS SUBSEA Subsea Reservoir Air Lines and Subsea Valves Power Island Proprietary and Subject to the Terms of the Nondisclosure Agreement Capacity Building: Environmental and Stakeholder Assessment Challenge: Many users of the coastal ocean, by humans and other organisms Protected species, habitats, and cultural resources in the coastal ocean Solution: Examine the spatial extent of potential conflicts Identify potential conflicts and synergies in the coastal ocean Outcomes Conflicts were mapped for future siting purposes Potential conflicts and synergies were identified for future study Research team: Lindsay Dubbs, UNC-Chapel Hill and UNC CSI; Michael Piehler, Assessing the effects of Gulf Stream turbines on Sargassum communities Lindsay Dubbs and Michael Piehler Sargassum fluitans and natens comprise an important floating pelagic ecosystem entrained in the Gulf Stream. Sargassum is important to the ecology of the Atlantic Ocean because: Many organisms live on or within clumps and mats Shelter is provided below the macroalgae and food is provided from above and below Sargassum and its epibionts cycle nutrients – carbon uptake and nitrogen fixation 30 50 m How is Sargassum related to Gulf Stream energy? Sargassum floats at the water’s surface and Gulf Stream turbines will likely be located at depths of 30-50 m below the water’s surface. Nonetheless, wakes generated by turbines may effect Sargassum communities. Research questions: 1. What is the spatial and temporal distribution and general structure of Sargassum communities along the western wall of the Gulf Stream off the coast of Cape Hatteras, North Carolina? 2. How do changes in hydrodynamic forces affect productivity, nitrogen fixation, and respiration of Sargassum and its epibionts? The Gulf Stream • Average Gulf Stream shown in white dashed lines • COLDER blue water, WARMER red & orange water • Gulf Stream red & orange slide courtesy of Caroline Lowcher “Movie” of The Gulf Stream Gulf Stream off NC • 15 – 20 Nautical Miles NC 15-20NM • Current speeds in excess of 2m/s • 90 Sv (106 m3/s) volume transport • Steep shelf slope Use Radar Surface Currents to locate the Gulf Stream Edge Before Core Radar After Core Radar Vel cm/s 100 NC NC 50 Core Radar ADCP Measurements ADCP Measurements 0 Observations 1. 150 kHz ADCP Mooring • Long term • Entire water column • One location • 8/01/2013 - now DUCK radar NC HATY radar CORE radar * 150 kHz ADCP mooring Moored ADCP Along Stream Currents at water depth 228m Height Above Bottom 200 m 3 m/s 0 m/s 20 m -3 m/s Aug. 2013 9 Months May 2014 MAB-SAB Model Configuration Ocean Depth Based on the Regional Ocean Model System (ROMS) 2 km spatial resolution, 36 terrain following vertical layers study focus region Boundary conditions are from global data assimilative HYCOM model 35 km spatial and 3 hourly temporal resolution NCEP North America Regional Reanalysis (NARR) atmospheric forcing 15 major rivers and M2 tide Hindcast periods: 2004-2005; 2009-2014 (Gong, He, Gawarkiewicz and Savidge, 2014) Potential Turbine Site 75m over 225m isobath Conclusions Significant Amounts of Renewable Energy in the Ocean Cost of devices and operation must be reduced to be competitive Ocean environment is a highly dynamic place to model and to operate GPUSPH with embedded Open Dynamics Engine allows for modeling of wave energy devices. ATHOS Consortium