Elsevier

Marine Structures

Volume 20, Issue 4, October 2007, Pages 185-201
Marine Structures

Review
A review of wave-energy extraction

https://doi.org/10.1016/j.marstruc.2007.09.001Get rights and content

Abstract

Comparing ocean-wave energy with its origin, wind energy, the former is more persistent and spatially concentrated. In this paper wave spectrum parameters related to transport, distribution and variability of wave energy in the sea are educed. Many different types of wave-energy converters, of various categories, have been proposed. It is useful to think of primary conversion of wave energy by an oscillating system as a wave-interference phenomenon. Corresponding to optimum wave interference, there is an upper bound to the amount of energy that can be extracted from a wave by means of a particular oscillating system. Taking physical limitations into account, another upper bound, for the ratio of extracted energy to the volume of the immersed oscillating system, has been derived. Finally, the significance of the two different upper bounds is discussed.

Introduction

Impressed by the force of ocean waves, inventors have, for more than two centuries, proposed many different devices for utilising wave power for human purposes [1], [2], [3], [4], [5]. As petroleum became the most important modern source of energy, the interest for wave-energy utilisation faded after the First World War. In the late 1940s, the Japanese wave-power pioneer Yoshio Masuda [6] started to test and develop wave-energy devices. Two inventive European pioneers, Stephen Salter and Kjell Budal, initiated in 1973 wave-power research at universities in Scotland and Norway, respectively. In the US, Michael E. McCormick was an early academic wave-power researcher. In years following the oil crisis in 1973, many researchers at universities and other institutions took up the subject of wave energy. Larger government-funded R&D programmes were started, during the late 1970s, in some European countries, the UK, Sweden and Norway—subsequently also in other countries. During the early 1980s, when the petroleum price declined, wave-energy funding was drastically reduced [7]. A few first-generation prototypes were, nevertheless, tested in the sea. More recently, following the Kyoto protocol on reduction of CO2 emission to the atmosphere, there is again a growing interest for wave-energy R&D in many countries. As many new young researchers are now entering into this research field, the present paper is intended to convey an overview on knowledge accrued until now, but in particular during years around 1980.

The global power potential represented by waves that hit all coasts worldwide, has been estimated to be in the order of 1 TW (1 terawatt=1012 W) [8]. If wave energy is harvested on open oceans, energy that is otherwise lost in friction and wave breaking, may be utilised. Then the global wave-power input is estimated to be one order of magnitude larger (∼1013 W), a quantity that is comparable with the world's present power consumption. Although this is only a small proportion of the world's wind power potential, which, in turn, is only a small portion of global solar power, ocean waves represent an enormous source of renewable energy. As solar energy is converted to wind energy, the time-averaged power flow is spatially concentrated, from an intensity of typically 0.1–0.3 kW/m2 horizontal surface of the earth to 0.5 kW/m2 envisaged area perpendicular to wind direction. As wind energy is converted to wave energy, even more spatial concentration takes place. Just below the ocean surface, average power flow intensity is typically 2–3 kW/m2 of envisaged area perpendicular to direction of wave propagation. This increase in power intensity, and also the fact that wave energy is more persistent than wind energy, stimulate motivation and hope for developing the, still rather undeveloped, wave-power technology to a prosperous mature level in the future. If the technology can be successfully developed, the market potential is enormous.

In the present paper, the main subject of the next section is the energy associated with ocean waves. Then follow, first, a section on fundamental principles for absorption of wave energy and on various ways of classifying wave-energy converters into different categories, and secondly, a section on mathematical description of wave-energy extraction. Before the final section with concluding remarks, there is a section, where upper bounds to the extracted wave energy are discussed.

Section snippets

Ocean waves and their energy resource

The term wind sea is used for waves that are actively growing due to forcing from local wind. These waves travel in or close to the local wind direction. Swell is the term used to describe long-period waves that have moved out from the storm area where they were generated. Swells spread out over the ocean with little energy loss. They are somehow analogous to waves spreading out from the splash of a stone thrown into a pond. Swells in deep water will, typically, have wavelengths of 100–500 m

Principles for extraction of wave energy

The physical law of conservation of energy requires that the energy-extracting device must interact with the waves such as to reduce the amount of wave energy that is otherwise present in the sea. The device must generate a wave, which interferes destructively with the sea waves [13]. “In order for an oscillating system to be a good wave absorber it should be a good wave generator”[14]. It should be considered as an advantage that practically all the volume, of e.g. a heaving-float system (cf.

Mathematical description of wave-energy extraction

As a mathematical illustration of wave-energy extraction, we shall, for simplicity, consider a body oscillating in one mode only, e.g. the heave mode. We shall, in the following, assume that amplitudes of waves and oscillations are sufficiently small to make linear theory applicable. In cases where latching control [14], [27], [28], [29] is applied, the system is not time invariant. Then instead of studying system dynamics in the frequency domain, it is better to apply time-domain analysis, as

Budal's upper bound

By extending the above arguments, Budal presented [35] an upper bound to the wave power that can be absorbed by a given immersed oscillating volume. As a more detailed derivation is published previously [36], we shall here just indicate the derivation. Based on Eq. (21) we have the inequalityPu<(1/2)Fe,0u0cos(ϕ)(1/2)Fe,0u0<ωρgA0V,where V is the volume of the heaving body, and A0 is the elevation amplitude of the incident wave. In the last step we took the maximum heave amplitude smax into

Concluding remarks

In the first part of this paper, we have discussed some wave spectrum parameters that are related to transport, distribution and variability of wave energy in the sea. For a fully developed wind sea, Eq. (6) shows that the power flow intensity is up to five times larger for ocean waves than for the wind that generates the waves. Moreover, wave energy is more persistent than wind energy. These facts give good hope for developing wave-energy technology, which is, however, still less mature than

Acknowledgement

Mr. Jørgen Hals carried out the numerical and graphical computer work related to Fig. 2.

References (39)

  • D.V. Evans et al.

    Submerged cylinder wave energy device: theory and experiment

    Appl Ocean Res

    (1979)
  • J. Falnes

    Radiation impedance matrix and optimum power absorption for interacting oscillators in surface waves

    Appl Ocean Res

    (1980)
  • A. Stahl

    The utilization of the power of ocean waves

    Trans Am Soc Mech Eng

    (1892)
  • J.M. Leishman et al.

    The development of wave power-a techno-economic study

    (1976)
  • M.E. McCormick

    Ocean wave energy conversion

    (1981)
  • R. Shaw

    Wave energy-a design challenge

    (1982)
  • Engineering Committee on Oceanic Resources Working Group on Wave Energy Conversion. Wave Energy Conversion

    (2003)
  • Y. Masuda

    An experience of wave power generator through tests and improvement

  • D. Ross

    Power from the waves

    (1995)
  • Panicker NN. Power resource potential of ocean surface waves. In: Proceedings of the wave and salinity gradient...
  • M.J. Tucker

    Waves in ocean engineering-measurement analysis interpretation

    (1991)
  • K. Torsethaugen

    The Norwegian “wave climate mapping” programme

  • D. Mollison

    Wave climate and the wave power resource

  • Saulnier JMG, Pontes MT. Standardizing wave energy resource data. In Johnstone CM, Grant AD, editors. Proceedings of...
  • Budal K, Falnes J. A resonant point absorber of ocean-wave power. Nature 1975; 256: 478–9 [With Corrigendum in vol 257,...
  • J. Falnes et al.

    Wave power conversion by point absorbers

    Norwegian Maritime Res

    (1978)
  • D.V. Evans

    A theory for wave-power absorption by oscillating bodies

    J Fluid Mech

    (1976)
  • J.N. Newman

    The interaction of stationary vessels with regular waves

    Proc. 11th Symp Naval Hydrodyn

    (1976)
  • C.C. Mei

    Power extraction from water waves

    J Ship Res

    (1976)
  • Cited by (0)

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