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Brazilian Archives of Biology and Technology

Print version ISSN 1516-8913

Braz. arch. biol. technol. vol.57 no.2 Curitiba Mar./Apr. 2014

http://dx.doi.org/10.1590/S1516-89132014000200020 

ENGINEERING, TECHNOLOGY AND TECHNIQUES

 

The 3D CFD study of gliding swimmer on passive hydrodynamics drag

 

 

Vishveshwar Rajendra ManthaI, II, III, *; Daniel Almeida MarinhoII, IV; Antonio Jose SilvaII, III; Abel Ilah RouboaI, V

IDepartment of Mechanical Engineering; University of Trás-os-Montes and Alto Douro; Vila Real - Portugal
IICentre of Research in Sports; Health and Human Development; CIDESD; Vila Real - Portugal
IIIDepartment of Sport Sciences; Exercise and Health; University of Trás-os-Montes and Alto Douro; Vila Real - Portugal
IVDepartment of Sport Sciences; University of Beira Interior; Covilhã - Portugal
VDepartment of Mechanical Engineering and Applied Mechanics; University of Pennsylvania; Philadelphia - USA

 

 


ABSTRACT

The aim of this study was to analyze the effect of depth on the hydrodynamic drag coefficient during the passive underwater gliding after the starts and turns. The swimmer hydrodynamics performance was studied by the application of computational fluid dynamics (CFD) method. The steady-state CFD simulations were performed by the application of k - omega turbulent model and volume of fluid method to obtain two-phase flow around a three-dimensional swimmer model when gliding near water surface and at different depths from the water surface. The simulations were conducted for four different swimming pool size, each with different depth, i.e., 1.0, 1.5, 2.0 and 3.0 m for three different velocities, i.e., 1.5, 2.0 and 2.5 m/s, with swimmer gliding at different depths with intervals of 0.25 m, each starting from the water surface, respectively. The numerical results of pressure drag and total coefficients at individual average race velocities were obtained. The results showed that the drag coefficient decreased as depth increased, with a trend toward reduced fluctuation after 0.5m depth from the water surface. The selection of the appropriate depth during the gliding phase should be a main concern of swimmers and coaches.

Keywords: Computational Fluid Dynamics (CFD), Passive Drag, Starts, Turns, Streamline Gliding Position, Glide depth.


 

 

INTRODUCTION

The swimming race is an event of modern Olympics, in which milliseconds can make a difference between the gold and silver. Extremely small winning margins still justify the incorporation of possible improvements in strength, style, conditioning, etc. The swimmers performance is decided by the athletes' physical active strength, sport technique and resulting hydrodynamic performance (Hanna 2006).

In the swimming event, the total swim time consists of the sum of three parts: starting time, swim time and turn times (Guimarães and Hay 1985). The underwater glide after the starts and turns assumes a high influence on the outcome of a swimming event (Vilas-Boas et al. 2010). Thus, the study of existing fluid flow around the swimmer appears to be important so that there is an improvement in the performance. In the events, which have many turns, some authors (Vilas-Boas et al. 2000; Cossor and Mason 2001) suggest that, apart from the influence of starting position adopted by a swimmer, the body alignment and path chosen during the glide phase also contribute towards determining the success in the event. To enable better performance, the swimmer should minimize the hydrodynamic drag (not being the exception, the phases of starting and turning), adopting a position as hydrodynamic as possible (Barbosa et al. 2006). In an aquatic environment, three types of hydrodynamic drag forces, which oppose the movement of the swimmer, are i) friction drag, ii) form or pressure drag, and iii) wave drag (Toussaint et al. 2002; Polidori et al. 2006).

A way of minimizing the hydrodynamic drag is to increase the depth of the underwater slide, since the contribution of wave drag seems to decrease when the swimmers perform their glide at higher depths (Lyttle et al. 2000; Polidori et al. 2006; Marinho et al. 2009). The hydrodynamics study of the glide movement in the passive underwater position has been carried out using the experimental methods (Clarys and Jiskoot 1975; Kolmogorov and Duplishcheva 1992; Lyttle et al. 1999; Vilas-Boas et al. 2010). More recently, it was concluded that, to a depth less than 0.7 m, drag produced could be 2.4 times higher than for deeper than 0.7 m; also that the wave drag produced was responsible for 50-60% of the total drag (Vennell et al. 2006). However, there is need to study this, not only because there are few studies conducted, but because of the variability in results obtained, along with the difficulties involved in performing these experimental protocols (Bixler et al. 2007).

In the investigative studies of this type, the application of CFD method in swimming could be an alternative to the experimental studies (Bixler et al. 1996). The possibility of obtaining data, without performing the experimental tests using human beings, is a huge asset not only in terms of the costs, but also in terms of time efficiency, since, at any time, there is ability to make a new simulation and change the variables, allowing the comparative studies. In this sense, this work aimed to investigate the effect of depth in the hydrodynamic drag of a swimmer during the underwater glide, using CFD method. The hypothesis of the current study was that the hydrodynamic drag decreased along with the reduction in the fluctuation with increasing depth of the gliding swimmer. There would be a range of optimum depth, which could be chosen by the swimmer during the glide.

 

MATERIALS AND METHODS

To carry out the numerical simulation studies, the geometry under consideration could be studied to calculate and deduce the parameters required for the analysis. The fluid flow can be completely simulated by solving Navier - Stokes equations, but this requires expensive computational resources. To save on the economics, these equations are transformed into algebraic form and solved by solver algorithms on the finite discretized domain consisting of volumetric mesh with the prediction of fluctuating velocities with the help of turbulent model. The air-water two-phase fluid flow is estimated by the VOF model.

The steady state numerical simulations were performed for the velocity of 1.5, 2.0 and 2.5 m/s. The simulation of swimmer gliding with steady velocity was implemented by keeping the swimmer static in the fluid flowing at constant velocity. The flow around the swimmer was turbulent, corresponding to the Reynolds number varying between the orders of 5 to 6 (Bixler et al. 2007). Due to that reason, the Reynolds averaged Navier - Stokes equations with the Boussinesq hypothesis to model the Reynolds stresses (Hinze 1975) were considered. The closure problem of the turbulent modeling was solved using k - ω model. The advantage of the k-ω model over the k-ε model was its improved performance for the boundary layers under adverse pressure gradients and it could be applied throughout the boundary layer, including the viscous-dominated region, without further modification (Wilcox 1998). The detailed terms of the k - ω model transport equations used in the present study are provided in user manual of Fluent documentation (Fluent 2006).

In reality, the swimmer moved through two fluid, i.e., air (which was in gas phase) and water (which was in liquid phase) when gliding at water surface and also there was displacement of surface water when swimmer was gliding below the surface, leading to energy losses. The two-phase simulations by implementation of volume of fluid (VOF) method simulated the actual physics of the problem with flow of air-water as seen in pool environment. Most of the previous studies have not simulated two-phase flow around the swimmer while studying the passive glide.

The simulations were based on the finite volume method of discretization (Patankar 1980). In order to limit the numerical dissipation, particularly when the geometry was complex consisting of an unstructured grid, as seen in Figure 1, with the choice of second order upwind discretization scheme for the convection terms in the solution equations, and Pressure-Implicit with Splitting of Operators (PISO) pressure-velocity coupling scheme for the double precision, pressure-based solver was chosen. The PISO pressure-velocity coupling scheme, part of the SIMPLE family of algorithms, was based on the higher degree of the approximate relation between the corrections for the pressure and velocity (Fluent 2006). The convergence criterion chosen was equal to 10-6.

 

 

The 3D surface geometry model was acquired through the standard commercial L.A.S.E.R. scanner, which had an average maximal error circumference of less than 1.0 mm, with point cloud density 27 points/ cm2. The swimmer who served as the basis for obtaining a digital model was 2.40 m tall in streamline glide position, with a perimeter of the head, chest, waist and hip of 0.58, 1.02, 0.87 and 0.93 m, respectively. The 3D surface geometry data of swimmer model was generated in Solidworks(R) CAD software (Fig.1) and exported in IGES format for import into GAMBIT preprocessor. The grid structure and the computational domain are shown in Figure 1. The upstream boundary was located at two swimmer height from the tip of fingers. The downstream extent was located more than six times swimmer height from the tip of toe fingers. In the fluid domain, swimmer was positioned proportionately near to the inlet, instead of middle. By doing so, flow in the back of the swimmer could be resolved more accurately, and also limited the front region that had no practical interest, since the fluid was mostly unperturbed by the swimmer before it touched the fingers. The appropriate boundary conditions were applied on the computational domain, with wall boundary condition on swimmer surface and bottom surface of computational domain, symmetric boundary condition on top, rear and front surfaces of computational domain, velocity inlet and pressure outlet on the remaining side surfaces of computational domain, respectively. The simulation of swimmer glide motion with steady velocity was implemented by keeping the swimmer static in the fluid flowing at constant velocity. The study of drag was simplified by not considering the effect of surface wind waves, generally present on the swimming pool water surface, since their contribution to drag was presumed to be less predominant.

 

RESULTS AND DISCUSSION

In swimming, the total drag is composed of the friction drag, pressure drag and wave drag. When the swimmer glided immediately below the water surface, the displacement of water surface around the swimmer occurred, which generated the waves (Fig. 2A). The water waves around the swimmer clearly showed variation, as water flew over the swimmer's body. Swimming near the surface of the water caused the formation of waves on the surface, resulting in the so-called drag effect of the wave. For the swimmer gliding at the surface, the wave drag component was not calculated in this study due to inherent limitation of CFD software's available, but the estimated drag was considered as component of the total drag, which excluded the contribution from wave drag.

The pressure drag was caused by the pressure differential between the front and the rear the swimmer, which was proportional to the square of swimming speed, the density of water and frontal cross-sectional area of the swimmer. The contours of static pressure showed variation over the body and the value increased with increase in depth (Fig. 2B). The simulation of two-phases, i.e., air and water as seen in the pool environment was important to predict the drag forces realistically. When the pressure drag (pressure force) variation from all the four swimming pools was studied at different velocities, different glide depths in respective swimming pools, it indicated a rise initially, followed by brief calm down with less amount of variation and fluctuation in the later stage (Fig. 3) with similar tendency observed by variation of hydrodynamic drag coefficient (Fig. 4). In general, for all the speeds, the hydrodynamic drag decreased with increasing depth and there was a tendency to stabilize (with less amount of variation) the coefficient of drag between 0.5 m to 0.15 m, but the range varied depending upon the depth of swimming pool. The lower value of drag when the swimmer was just below the surface of water, could be attributed to the drag contributed only by the pressure effects and entirely from the swimmers body exposed by the water and remaining prominent contribution was from the wave drag, which was not estimated in the current study. The drag experienced by the swimmer must be more when gliding near the air-water interface and the wave component will decrease thereafter as swimmer glides deeper, giving rise to prominence of pressure drag (Toussaint et al. 2002; Vennell et al. 2006). Naturally, the increase in swimmer glide velocity, will witness augmentation in all the components of drag depending upon respective location of swimmer during glide.

The main objective of this study was to evaluate the effect of swimmer glide depth on the hydrodynamic drag and its coefficient by using CFD method. It is noteworthy that with increase in the depth of underwater glide, the hydrodynamic drag decreased and became stable (with reduced amount of variation) in a range depending upon the depth of the swimming pool. The location of the stabilized region was where the contribution from the surface waves was also minimal (Lyttle et al. 1999; Toussaint et al. 2002; Vennell et al. 2006). This could be of practical application to choose the sustainable optimal glide path depending upon the glide velocity and depth of the swimming pool. The current study showed that the hydrodynamic drag coefficient decreased as the depth increased, which was in agreement with previous studies (Lyttle et al. 1999; Vennell et al. 2006; Bixler et al. 2007; Marinho et al. 2009).

When the swimmer glided at 1.0 m glide depth in a 1.5 m deep swimming pool at the speed of 2.5 m/s, the numerical study predicted 18% more drag as compared with the experimental measurements (Vennell et al. 2006). This could be attributed to the variation and differences in the experimental and numerical conditions, such as the characteristics of swimmers, depth of swimming pool, differences in streamline glide positions, fluctuations in actual glide depth during the swimming, and combined error in the measurement instruments and numerical errors (Bixler et al. 2007). This could also be attributed to the differences in the position of hands, due to procedures followed during the scanning process in obtaining three-dimensional model, location of the model's hands (side by side and slightly apart), which also contributed to higher values of overall drag values (Vorontsov and Rumyantsev 2000). The differences between the previous numerical studies could be also attributed to the limitation in previous studies with the lack of use of real 3D swimmer model and limitations on the simulation of actual physics as compared with the present study, which was complete in this aspect, leading to more accurate prediction.

The values of the friction drag were noticeably similar. This was as expected, as the friction drag was produced depending upon the amount of exterior surface area of swimmer's body in contact with water; this value would not suffer large oscillations, since the model used was the same and the swimmer was fully submerged, except when gliding near the water surface (Vennell et al. 2006). For glide depths in proximity to the water surface, the swimmers body was submerged partly and it depended upon the velocity and irregularity in formation and dissipation of water waves. This introduced deviation in the estimation of wetted surface area and also submerged frontal cross section area of the swimmers body, which in turn produced fluctuations in drag. However, it would be essential to quantify the wave drag numerically, which in the present study was not analyzed due to limitations presented by the numerical code.

With reference to the variation of drag coefficient with glide depth, there was a brief initial affinity for fluctuation and reduction in drag for all the three glide velocities at different glide depths in the four types of swimming pools studied. There was also a marked tendency to retain the comparable value of drag between 0.5 m to 1.75 m, depending upon the depth of swimming pool under the study. Some of the previous studies indicated that after 0.6 m of glide depth from water surface, the wave drag was almost negligible, and it did not contribute significantly towards total drag (Lyttle et al. 1999). It is noteworthy that with increase in the depth of underwater glide, the hydrodynamic drag decreased and became almost unwavering, which could be identified as a stabilized region (with less amount of variation) depending upon the depth of the swimming pool. The location of the stabilized region was at a depth, where the contribution from the surface waves was predicted to be minimal (Toussaint et al. 2002; Vennell et al. 2006). Although, wave drag was not calculated due to inherent limitations, this did not affect the aim and outcome of the present study, as swimmers are practically instructed to glide deep, especially after the starts and turns, and this was seen to be implemented in practice. This study could be of practical application to the swimmers, helping them choose the sustainable optimal glide path, glide depth depending upon the glide velocity and depth of the swimming pool.

 

CONCLUSION

The drag decreased as the depth increased and there was a tendency for stabilization of the value, which varied for the glide velocities and depth of the swimming pool. With increase in the depth of underwater glide, the hydrodynamic drag decreased and became almost stable, which was identified as stabilized region depending upon the depth of the swimming pool. This could be of practical application to the swimmers, helping them choose the sustainable optimal glide path, glide depth depending upon the glide velocity and depth of the swimming pool. Thus, the selection of the appropriate depth for the underwater glide should be a vital concern of the swimmers and coaches. However, the ideal depth must be one that allows to reduce the hydrodynamic drag as much as possible, but at the same time, allowing a optimum vertical distance from the water surface, so that the swimming could be restarted. The balance of the drag reducing (increasing depth) and increasing the vertical distance traveled are the key aspects to consider. The current study presented the knowledge of hydrodynamics, which could be utilized by an athlete or a coach during the progression at different race velocities in different swimming pool environments.

 

ACKNOWLEDGMENTS

This work was supported by a grant of the Science and Technology Foundation Portugal (PTDC/DES/098532/2008).

 

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Received: August 05, 2013
Accepted: December 23, 2013

 

 

* Author for correspondence: vishveshwar@gmail.com

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