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Blade element momentum theory for a tidal turbine
- Source :
- Ocean Engineering. 169:215-226
- Publication Year :
- 2018
- Publisher :
- Elsevier BV, 2018.
-
Abstract
- A key hydrodynamic difference between tidal current and wind turbines is the volume-flux constrained flow field in which tidal turbines operate and the resulting streamwise static pressure difference that develops in the flow passage. Blade Element Momentum (BEM) theory is extended to account analytically for the effects of blockage and the development of the static pressure difference in the flow passage and shows agreement in thrust and power predictions to within ± 3 % of equivalent blade resolved simulations. The confined flow BEM model is employed to study two different power capping strategies: varying the rotational speed with fixed pitch blades; and pitching the blades to feather at constant rotational speed. Pitch-to-feather achieves reduced thrust above rated flow speed which leads to a greater extractable resource than achievable with overspeed control, due to the feedback between device thrust and available tidal resource. Flow confinement is shown to reduce the flow speed at which rated power occurs, and increases the rotor loads and power below rated conditions. It is also shown that root bending moments, which affect fatigue damage rates, increase with flow confinement.
- Subjects :
- Physics
Momentum (technical analysis)
Environmental Engineering
business.industry
020209 energy
Blade element momentum theory
Flow (psychology)
Ocean Engineering
Thrust
Rotational speed
02 engineering and technology
Static pressure
Mechanics
01 natural sciences
010305 fluids & plasmas
Physics::Fluid Dynamics
Flow velocity
0103 physical sciences
0202 electrical engineering, electronic engineering, information engineering
business
Tidal power
Subjects
Details
- ISSN :
- 00298018
- Volume :
- 169
- Database :
- OpenAIRE
- Journal :
- Ocean Engineering
- Accession number :
- edsair.doi.dedup.....ac2ec91f1ab2f49d916effddbf09266d
- Full Text :
- https://doi.org/10.1016/j.oceaneng.2018.09.018