Introduction Ports are considered to be the most important transit locations to carry out the world trade through seaways
Ports are considered to be the most important transit locations to carry out the world trade through seaways, which need to be protected from the disturbances due to the incoming waves. A seaport plays an important role in the sector of sea transportations, exports, imports, tourism, and travel, and thus is an important ingredient of economic growth. Water transport is a major economy input for a nation with over 82% of world trade in tons and 94% of world trade in tons-kilometres which are moved by shipping and thereby through ports.
The basic requirement of any port, harbor or marina is a sheltered area free from the waves. In the coastal areas where natural protection from waves is not available, the development of harbour requires an artificial protection for the creation of calm areas. For harbours, where perfect tranquility conditions are required, large structures such as rubble mound breakwaters or vertical wall breakwaters are used. Most of the breakwaters are used to create tranquil conditions in the lagoon and at the entrance channel of ports, for maneuvering of ships and port operations. Mostly breakwaters are also used as berthing structures along with protecting the harbor area. Sometimes they are used to protect beaches from erosion due to the destructive wave forces.
Due to fast growing need of the universe and advances in technology different types of composite breakwater are being developed. Semicircular breakwater is a composite structure first developed in Japan at the beginning of the Nineties and first adopted for the formation of the harbor in Miyazaki Port, Japan. Quarter circle breakwater (QBW) is a new-type breakwater first proposed by Xie et al. (2006) on the basis of semicircle breakwater. The present study investigates the stability of an emerged seaside perforated quarter circle breakwater with varying percentage of perforations, for different water depths and wave conditions. The major objectives include the study of the effect of incident wave steepness, S/D (spacing between perforations/diameter of perforations) ratio or percentage of perforations and water depth on the stability characteristics of perforated QBW.
The experiments were conducted in a two dimensional wave flume available in the Marine Structures Laboratory of Department of Applied Mechanics and Hydraulics, National institute of technology Karnataka, Mangalore, India.
Wave Flume and Instrumentation
The physical model study for regular waves was conducted in a two dimensional wave flume 50 m long, 0.71 m wide and 1.1 m deep (Refer Figure 1). Waves of height ranging from 0.08 m to 0.24 m heights and periods from 0.8 sec to 4.0 sec can be generated with this facility.
Figure 1. Longitudinal Section of Wave Flume.
The breakwater model basically consists of two parts: a top quarter circular shaped caisson and a bottom base slab made of precast concrete founded on rubble mound base. The caisson was made with Galvanized Iron (GI) sheet of 2 mm thickness. To simulate the field conditions of wave height, wave period and diameter of perforation by application of Froude’s law, a geometrically similar model scale of 1:30 has been selected for the present experimental investigations.
Figure 2. Typical Cross section of Perforated QBW.
For present study, QBW of 0.55 m radius was selected to satisfy the condition that the model will be emerged at all water depths and remains non-overtopped under all wave conditions considered for the study. The QBW model was fixed to the base slab with the help of stiffeners. The perforations are provided in the quarter circular front portion of the breakwater model, by drilling the holes. Figure 2 shows the typical view of quarter circle breakwater considered for the study.
The model after casting was placed over the rubble mound foundation of thickness 0.05 m using stones weighing from 50 to 100 g having a slope 1:2. The QBW model together with rubble mound foundation was usually placed 30 m away from the wave flap. Three probe method proposed by the researchers 4 was used for measuring the incident and reflected wave height. The first probe was placed L distance from the centre of the probe, and the distance between the other probes were equal to L/3, where L is the wave length. A burst of five waves was generated to avoid the successive reflection. The surface elevation measured by the probes were recorded by the wave recorder and the voltage signals are converted into wave heights and wave period by using the lab wave recorder software provided by EMCON (Environmental Measurements and Controls), Kochi, India. The range of parameters selected for the studies are mentioned in Table 1.
Table 1. Range of Experimental variables.
Parameters Experimental Range
Wave Specific Parameters
Incident wave height, Hi
Water depth, d
Time period, T
Structure specific parameters
Radius of the structure
Diameter of perforation
0.03, 0.06, 0.09, 0.12, 0.15, 0.18 m
0.35, 0.40, 0.45 m
1.2, 1.4, 1.6, 1.8, 2.0, 2.2 sec
2, 2.5, 3, 4, 5
The present experimental investigations are carried out with the following test conditions:
The sea bed is rigid and horizontal and it is assumed that the sediment movement does not interfere with the wave motion and do not affect the model performance.
The waves are periodic and monochromatic.
Wave reflection from the structure does not interfere with freshly generated incident waves, since the waves are generated in bursts.
Secondary waves generated during the test are not considered.
Wave reflection from the flume bottom or flume side walls is not considered.
The density difference between freshwater and seawater is not considered.
Bottom frictional effects have not been accounted.
Results and discussions
Studies were conducted on emerged seaside perforated QBW with different spacing to diameter (S/D) ratios under different water depths (say 0.35, 0.40 and 0.45 m) and varying wave conditions. Variations of minimum weight required for sliding stability with different wave specific and structural specific parameters were studied, and the variations were then plotted graphically using non-dimensional parameters. The stability based on sliding performance was represented by a non-dimensional stability parameter (W/?Hi2), where W is the minimum weight of the QBW required to resist the sliding per unit length of the breakwater, ? is the specific weight of water and Hi is the incident wave height.
4.1 Influence of incident wave steepness on W/?Hi2
The variation of W/?Hi2 with Hi/gT2 at different water depths for QBW radius 0.55 m and S/D ratio equal to 2, 2.5,3,4 and 5 were plotted as shown in Figure 3. It was clear from the graphs that W/?Hi2 decreases with increase in Hi/gT2 for all values of d/hs.
For S/D = 2 (b) For S/D= 2.5
For S/D = 3 (d) For S/D= 4
(e) For S/D= 5
Figure 3. Influence of Hi/gT2 on W/?Hi2 for S/D= 2,2.5,3,4 and 5 and at different water depths.
For all models, it was observed that when the incident wave steepness increases, the dimensionless stability parameter decreases. This is because for a given wave height and long period waves (low steepness) exert more force on the caisson demanding more minimum weight and short period (steep) waves transfer less force, hence low minimum weight. The sliding due to increase in wave force is overcome by increasing the weight of breakwater by adding additional weight into the caisson. The variation of W/?Hi2 with wave steepness for different water depths and S/D ratio for seaside perforated QBW were summarized in table 2.
Table 2 Variation of W/?Hi2 with Hi/gT2
S/D ratio Water depth in cm d/ hs Variation of W/?Hi2 with Hi/gT2
0.569 3.335 – 10.532
3.236 – 8.766
2.225 – 7.249
0.569 3.198 – 10.269
3.155 – 8.546
2.110 – 6.967
0.569 3.566 – 11.223
2.472 – 7.989
0.569 3.882 – 11.668
3.555 – 9.711
2.729 – 8.412
0.569 4.056 – 12.850
3.779 – 10.695
3.006 – 9.355
4.2 Influence of water depth on W/?Hi2
From the results, it is clear that as the water depth increases, the value of W/?Hi2 increases and the minimum value for W/?Hi2 are observed at a water depth of 0.35 m. As water depth increases from 0.35 m to 0.40 m there is an increase in W/?Hi2 by 17.30 % to 31.24%. When water depth increases from 0.35 m to 0.45m there is an increase in W/?Hi2 by 31.17 % to 33.28%. Therefore it is clear that the structure is safe against sliding with minimum weight including additional weight at lower water depths. This is because higher the water depth, greater is the area of the QBW model structure exposed to wave action, and hence, the increase in d/hs imparts more force and therefore increase in W/?Hi2. This means that for a constant S/D ratio more structure weight is required for sliding stability in larger depths compared to smaller water depth.
4.3 Influence of S/D ratio on W/?Hi2
From the results for W/?Hi2 for varying ranges of Hi/gT2, it is observed that W/?Hi2 increases with increase in S/D ratio. At a water depth equal to 0.40 m, the percentage reduction in W/?Hi2 for S/D = 4 , 3, 2.5 and 2 are 5.92% to 9.20% , 10.42% to 10.55% , 16.51% to 20.09% and 14.36% to 18.04% with respect to S/D = 5. At a water depth equal to 0.45 m, the percentage reduction in W/?Hi2 for S/D = 4 is 4.29% to 9.19% compared to S/D = 5. The percentage reduction in W/?Hi2 for S/D = 3, 2.5 and 2 are 12.32% to 12.66%, 20.08% to 21.15% and 17.77% to 18.03% with respect to S/D = 5.For lower values of S/D, W/?Hi2 is found to very less compared to higher values except in the case of S/D ratio equal to 2. For lower values of S/D perforations encountered are more resulting in dissipating of major portion of the wave energy and hence force exerted on the QBW caisson will be very less. Therefore the weight required for resisting sliding stability will be very less and resulting in lower values for W/?Hi2.
4.4 Equations developed for stability parameter
The results for the experimental studies on stability characteristics for impermeable QBW for different breakwater radius at different water depths and wave conditions are combined into suitable dimensionless terms. The regression analysis is done by using Excel statistical software – XLSTAT and the equation for the best fit curve is obtained.
The equation for W/?Hi2 for seaside perforated QBW was derived as follows:
“W/?Hi2 = 6.813(Hi/gT2)-0.503″+”31.580(d/hs)8.357 “+”0.0008(d/hs)4.524 “-0.0″841”
Figure 4 shows the comparison between the measured and predicted values of stability parameter W/?Hi2 for perforated QBW.
Figure 3. Comparison between measured and predicted values of W/?Hi2 for perforated QBW.