INTRODUCTION OF WAVE-SCREEN PARAMETER

 

 

Dr. Vahid Chegini

Soil Conservation & Watershed Management Research Center,

The Ministry of Jihad for Construction,

P O Box 13445-1136, Tehran, I R of Iran, E-mail: aquasoil @ neda.net.ir

 

 

Abstract: The prediction of reflection and transmission coefficients through single perforated sheets and walls plays an important role in the assessment of the hydraulic behaviour of upright perforated wave absorbers and perforated wall breakwaters. In this paper, a new non-dimensional parameter is introduced to describe the hydraulic characteristics of single perforated sheets. It is shown that the reflection and transmission coefficients of waves through these sheets and also the transmission coefficients of waves through upright perforated wave filters are functions of this parameter.

 

Keywords: wave screen interaction, upright perforated absorber, perforated wall breakwater

1    Introduction

Wave absorbers are used for dissipation of wave energy at the end of a wave flume or along the rigid boundaries of a wave basin. According to the research of Ouellet and Datta (1986) the wave absorbers most commonly used in laboratories throughout the world are sand, gravel stone or concrete beaches. The slopes of these absorbers are usually 1:10.

An alternative solution for dissipation of the incident wave energy at the boundaries of a wave tank is using of upright perforated wave absorbers (Jamieson and Mansard, 1987; Chegini, 1995a). The advantage of these absorbers is that they need less space for installation than the conventional inclined wave absorbers known as beach absorbers. An upright perforated wave absorber is composed of rows of vertical perforated sheets installed in front of a solid back wall which would otherwise be highly reflective. These absorbers may be made from sheets of the same porosity or variable porosity. In the latter case, the porosity is decreased progressively toward the rear of the absorber. 

Wave filters are employed for reduction of wave reflection from wave paddles. In addition the secondary modes of the generated wave can be eliminated by using a wave filter ( Chegini, 1997b).

A perforated wall breakwater consists of a perforated front wall and a wave chamber. The front wall allow flow into and out of the chamber in which energy is dissipated by turbulence reducing wave reflection, wave loads on the structure and overtopping. Perforated breakwaters can also be designed to be permeable, where some wave transmission occurs. Such a structure can consists of a slotted wave-screen supported by piling.

The prediction of reflection and transmission coefficients through single perforated sheets plays an important role in the assessment of the behaviour of these structures and their efficient design. Figure (1) shows the definition sketch for reflection and transmission of an incident wave through a perforated sheet.

The subject of wave reflection and transmission through a small aperture / porous barrier has been the subject of a number of theoretical and experimental studies within last three decades ( Tuck, 1971; Porter, 1972; Guiney, Noye and Tuck, 1972; Packham and Williams, 1972; Hattori, 1972; Mei, Liu and Ippen, 1974; Macaskill, 1979; Owen and Bhatt (1985); Chwang and Dong, 1984; Faure, Mc Bride, Smallman and Allsop, 1995; Chegini, 1995a,1997a, 1999 )

2    Wave-Screen Parameter

The reflection and transmission coefficients of a wave through a thin perforated sheet can be expressed as a function of the following variables:

                        (1)

where:

Kr    reflection coefficient

Kt    transmission coefficient

Hi   incident wave height

h    water depth

       deepwater wave length

p    porosity of perforated sheet

G   geometry of perforations

The effect of geometry of perforations may be described in terms of the discharge coefficient of the screen perforations, . Generally,  is a function of the barrier thickness, the hole diameter, the screen porosity, the geometry of perforations and the Reynolds number. For a thin barrier and high Reynolds numbers, this coefficient becomes only a parameter of the screen porosity and the geometry of perforations. The discharge coefficient increases with increasing , therefore it is possible to incorporate these two parameters into a single parameter as follows:

                              (2)

where a is the screen factor. Using (2), equation (1) becomes:

                       (3)

Dimensional analysis leads to:

                     (4)

It may be shown that for  the relative water depth has a minor effect on the coefficient of wave reflection (Chegini, 1995b).

Increasing a causes more wave energy to be transmitted through the perforated sheet and reduction of this parameter increases reflection from the screen.

Chegini (1995b) showed that the incident wave steepness has a significant effect on the coefficient of wave transmission through the perforated sheet. This coefficient decreases with increasing  (or ).

Therefore, generally, simulating the dissipation of waves due to the perforated sheet to the wave attenuation by an inclined permeable structure, it may be concluded that:

                           (5)

where:

                           (6)

is defined as wave-screen parameter.

This parameter is comparable with the surf similarity parameter, which is used for sloping porous structures. It should be noted that the screen factor, a, is indeed a representative of the screen perforations. Therefore for a thick perforated barrier the effect of the barrier thickness should also be incorporated in equation (2).

3    Experimental Studies

A set of experimental studies was carried out in the Water Research Laboratory of the University of New South Wales (WRL) to measure the reflection and transmission coefficients of waves through single perforated sheets and upright perforated wave filters.

Two kinds of porous sheets, i.e. expanded metals of 26, 42 and 58 percent porosity and perforated plates of 23, 40 and 62 percent porosity were employed for the experimental tests on single perforated sheets. Only the normal position was used for the former screens. This position is defined with the louvres of the sheets oriented downwards in the direction of a wave propagation from the wave generator toward the sheet. The diameters of screen perforations for sheets of 23, 40 and 62 percent porosity were 1.6, 6.35 and 7.94 mm, respectively. The support frame for the perforated sheet was made of  mm steel angle.

Reflection and transmission coefficients of waves were measured for double perforated plates and wave filters composed of four perforated plates of the same porosity. The screens were aligned normally to the direction of wave propagation. The porosity of the sheets was 40 and 62 percent.

The experiments were carried out in the deeper section of the 0.9 m wide, 1.75 m deep, 50 m long wave flume of WRL. All the tests were undertaken in water at a depth of 0.8 m. Only regular waves were used in the laboratory experiments. The wave periods were 1.25, 1.35, 1.50, 1.75 and 2.50 seconds ( = 0.125 to 0.34). The reflection and transmission coefficients were measured for waves of steepness ratios (Hi / L) ranging from 0.003 to 0.01. To attenuate the energy of transmitted waves through perforated sheets, a permeable sloping wave absorber made of artificial horse hair was installed at the end of the flume (Chegini, 1993).

Wave profiles were measured by four fixed capacitive-wire wave probes located in either side of the screen / wave filter. The distance between the probes at each side of the screen / wave filter was 40 cm. Lotus-Measure Software was employed to transfer the collected data to a Portable Microcomputer. Four channels of data were recorded simultaneously at a sampling rate of 50 samples per second on each channel. Fourier analysis was used to evaluate the wave amplitude of the fundamental frequency. The reflection coefficients were calculated from the “two probes technique” reported by Thornton and Calhoun (1972).

4    Discussion

Figure (2) indicates the coefficients of wave reflection and transmission through single perforated sheets as a function of the wave-screen parameter. As can be seen from this figure, the coefficient of wave transmission (Kt) increases with increasing the wave-screen parameter, whereas the coefficient of wave reflection (Kr) decreases as this parameter increases.

The comparison between the experimental results of the present study and other investigations is shown in figure (3).

The discharge coefficients of screen perforations were evaluated from the following empirical formula from Dailey et al., 1966 (also used by Mei et al., 1974):

                         (7)

where and A are the perforated and the total area of the screen, respectively.

Figures (4) and (5) depict the variation of transmission coefficients of upright perforated wave filters composed of two and four sheets, respectively, as a function of the wave-screen parameter.

5    Conclusions

The results of laboratory tests have been presented for the reflection and transmission coefficients of waves through single perforated sheets and the transmission coefficients of waves through upright perforated wave filters aligned normally to the direction of wave propagation.

A new non-dimensional parameter was introduced to describe the hydraulic characteristics of single perforated sheets. This variable is called the wave-screen parameter (G).

The coefficient of wave transmission through a perforated sheet or an upright perforated wave filter increases with increasing this parameter. The coefficient of wave reflection from the perforated sheet decreases as the wave-screen parameter decreases.

The results obtained from the present study and the other investigations have shown that the coefficients of wave reflection and transmission through single perforated sheets can be described as a function of this new non-dimensional parameter.

References

Chegini, V.: “Reflection and Transmission of Water Waves through Single Perforated Sheets”, Iranian J. of Water Resources Eng. (IJWRE), Vol. 4, No. 4, Win 1997a.

Chegini, V. : “Dissipation of Wave Energy through Upright Perforated Wave Filters”, Proc. of the 1st Int. Conf. Port, Coast, Environment, Vol. 1, Varna, Bulgaria, 30 June – 4 July, 1997b, pp 19-28.

Chegini, V. : “Theoretical Analysis of Upright Perforated Wave Absorbers”, Proc. of the 4th Int. Conf. On Coastal and Port Eng. In Developing Countries (COPEDEC IV), RJ, Brazil, 25-29 Sept., 1995a, pp 2354-2365.

Chegini, V. : “Design of Upright Energy Dissipators for Use in Wave Basins”, A Thesis Submitted in Fulfilment of the Requirements for the degree of Doctor of Philosophy, Dept. of Water Eng., School of Civil Eng., Univ. of New South Wales, Australia, March, 1995b.

Chegini, V. : “Experimental Study of a Permeable Sloping Wave Absorber”, Res. Rep. No. 184, The Univ. of New South Wales, The Water Res. Lab., Australia, Nov. 1993, 33 pages.

Chwang, A. T. and Dong, Z. : “Wave - Trapping Due to a Porous Plate”, Proc. of the 15th Office of Naval Research Symposium, Hamburg, 1984, pp. 407-417.

Dailey, J. W. and Harleman, D. R. F. : “Fluid Dynamics”, Addison - Wesley Publishing Co., Inc., New York, N.Y., 1966, pp. 320.

Faure, T. D. : “Numerical Modeling of Wave Reflection from Upright Variable Porosity Wave Absorbers”, National Research Council Canada, Institute for Mechanical Eng., Hydraulics Lab., Coastal Zone Eng. Program, Tech. Rep. No. 1 IME - CZE - TR - 005, Nov. 1992, 51 pages.

Guiney, D. C., Noye, B. J. and Tuck, E. O. : “Transmission of Water Waves through Small Apertures”, J. of Fluid Mechanics, Vol. 55, Part 1, 1972, pp. 149-161.

Hattori, M. : “Transmission of Water Waves through Perforated Wall”, Coastal Eng. in Japan, Vol. 15, 1972, pp. 69-79.

Jamieson, W. W. and Mansard, E. P. D. : “An Efficient Upright Wave Absorber”, ASCE Specialty Conf. on Coastal Hydrodynamics, Univ. of Delaware, Newark, Delaware, June 1987, pp. 124-139.

Macaskill, C. : “Reflexion of Water Waves by a Permeable Barrier”, J. of Fluid Mechanics, Vol. 95, Part 1, 1979, pp. 141-157.

McBride, M. W., Smallman, J. V. and Allsop, N. W. H. : “Vertical Walls and Low Reflection Alternatives – Numerical Modelling of Absorbing Wave Screens”, Report IT 400, H R Wallingford, April 1995.

Mei, C. C., Liu, L. F. and Ippen, A. T. : “Quadratic Loss and Scattering of Long Waves”, J. of the Waterways, Harbours and Coastal Eng., ASCE, Vol. 100, No. WW3, Aug. 1974, pp. 217-239.

Owen, D. and Bhatt, B. S. : “Transmission of Water Waves through Small Aperture in a Vertical Thick Barrier”, Q. J. Mech. Appl. Math., Vol. 38, Pat. 3, 1985, pp. 397-409.

Packham, B. A. and Williams, W. E. : “A Note on The Transmission of Water Waves through Small Apertures”, J. Inst. Math. Applics., Vol. 10, 1972, pp. 176-184.

Porter, D. : “The Transmission of Surface Waves through a Gap in a Vertical Barrier”, Proc. Camb. Phil. Soc., Vol. 71, 1972, pp. 411- 421.

Thornton, E. B. and Calhoun, R. J. : “Spectral Resolution of Breakwater Reflected Waves”, J. of the Waterways, Harbor and Coastal Eng. Div., ASCE, Vol. 98, No. WW4, Nov. 1972, pp. 443-460.

Tuck, E. O. : “Transmission of Water Waves through Small Apertures”, J. of Fluid Mechanics, Vol. 49, Part 1, 1971, pp. 65-74.

 

Fig. 1    Definition sketch for reflection and transmission of an incident wave through a perforated sheet

Fig. 2    Characteristics of single perforated sheets as a function of the wave-screen parameter

Fig. 3    The comparison between the experimental results of the present study and other investigations

 

  

Fig. 4    Transmission coefficients of double perforated plates as a function of the wave-screen parameter

Fig. 5    Transmission coefficients of upright perforated wave filters composed of four sheets as a function of the wave-screen parameter