American Journal of Fluid Dynamics
p-ISSN: 2168-4707 e-ISSN: 2168-4715
2016; 6(1): 1-10
doi:10.5923/j.ajfd.20160601.01

Md. Nurul Amin Helal 1, Bishnu Pada Ghosh 2, Rabindra Nath Mondal 2
1Additional Director (Education), Training Directorate, BGB Head Quarter, Pilkhana, Dhaka, Bangladesh
2Department of Mathematics, Jagannath University, Dhaka, Bangladesh
Correspondence to: Rabindra Nath Mondal , Department of Mathematics, Jagannath University, Dhaka, Bangladesh.
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Copyright © 2016 Scientific & Academic Publishing. All Rights Reserved.
This work is licensed under the Creative Commons Attribution International License (CC BY).
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Numerical simulation on fully developed two-dimensional laminar flow of viscous incompressible fluid through a rotating curved square channel with curvature 0.2 has been performed by using a spectral method and applying a temperature difference across the vertical sidewalls. The outer wall of the channel is heated while the inner wall cooled, the top and bottom walls being adiabatic. Water is used as a working fluid of the study. A rotation of the channel about the center of curvature is imposed in the positive direction, and combined effects of centrifugal, Coriolis and buoyancy forces are investigated in detail. As a result, three branches of asymmetric steady solutions with two-, three- and four-vortex solutions are obtained by the Newton-Raphson iteration method. Then, in order to study the non-linear behavior of the unsteady solutions, time evolution calculations as well as their phase spaces are obtained, and it is found that time periodic flow turns into chaos/transitional chaos through multi-periodic oscillations, if Tr is increased. Streamlines of secondary flows and isotherms of temperature profiles are obtained, and it is found that the unsteady flow consists of asymmetric two- to four-vortex solutions. Convective heat transfer is also investigated, and it is found that chaotic flow enhances heat transfer more effectively than the periodic or multi-periodic solutions due to strong secondary vortices. External heating is shown to generate a significant temperature gradient at the outer concave wall of the channel.
Keywords: Rotating curved duct, Secondary flow, Steady solutions, Time evolution, Dean number, Taylor number
Cite this paper: Md. Nurul Amin Helal , Bishnu Pada Ghosh , Rabindra Nath Mondal , Numerical Simulation of Two-Dimensional Laminar Flow and Heat Transfer through a Rotating Curved Square Channel, American Journal of Fluid Dynamics, Vol. 6 No. 1, 2016, pp. 1-10. doi: 10.5923/j.ajfd.20160601.01.
and
axes are taken to be in the horizontal and vertical directions respectively, and
is the coordinate along the center-line of the duct, i.e., the axial direction. The system rotates at a constant angular velocity
around the
axis. It is assumed that the outer wall of the duct is heated while the inner wall cooled. It is also assumed that the flow is uniform in the axial direction, which is driven by a constant pressure gradient G along the centre-line of the duct. The dimensional variables are non-dimensionalized by using the representative length d and the representative velocity
where
is the kinematic viscosity of the fluid. We introduce the non-dimensional variables defined as:
where
are the non-dimensional velocity components in the
directions, respectively;
is the non-dimensional time, P is the non-dimensional pressure,
is the non-dimensional curvature defined as
and temperature is non-dimensionalized by
![]() | Figure 1. Physical model and the coordinate system |
is introduced in the x- and y-directions as![]() | (1) |
, the stream function
and temperature T are expressed in terms of non-dimensional variables as![]() | (2) |
![]() | (3) |
![]() | (4) |
The non-dimensional parameters Dn, the Dean number; Gr, the Grashof number; Tr, the Taylor number and Pr, the Prandtl number, which appear in equations (2) to (4) are defined as![]() | (5) |
are the viscosity, the coefficient of thermal expansion, the co-efficient of thermal diffusivity and the gravitational acceleration respectively. The rigid boundary conditions for
and
are used as![]() | (6) |
![]() | (7) |
![]() | (8) |
and Pr are fixed as Dn = 2000, Gr = 1000,
and Pr = 7.0 (water).
and
are expressed as ![]() | (9) |
is the n-th order Chebyshev polynomial.
and
are expanded in terms of
and
as:![]() | (10) |
and
are obtained. The collocation points
are taken to be![]() | (11) |
and
. The steady solutions are obtained by the Newton-Rapshon iteration method. The convergence is assured by taking
defined as:![]() | (12) |
![]() | (13) |
![]() | (14) |
![]() | (15) |
and
are the non-linear terms. Then applying the Adams-Bashforth method for the second term of R.H.S of Eqs. (13) to (15) and simplifying we calculate
,
and
by numerical computation.
obtained for Dn = 2000, Gr = 1000 and Tr = 1000 at
are shown, where Q is the flux through the duct and
is the axial velocity of the steady solutions at
|
to
be 0.0084%;
to
is 0.0017%;
to
be 0.0011% and
to
be 0.0001%. Also the change of the axial velocityis 0.0562% from
to
; 0.0741% from
to
; 0.048% from
to
and 0.0072% from
to
. Therefore, it is evident that
gives sufficient accuracy of the present numerical solutions.
through the duct in the rotating coordinate system is calculated by: ![]() | (16) |
![]() | (17) |
is expressed as
In the present study,
is used to denote the steady solution branches and to perform time-evolution of the unsteady solutions.
for curvature
The solution structure of the steady solutions is shown in Fig. 2, where the first steady solution branch (first branch) is shown by thin solid line, the second steady solution branch (second branch) by thick solid line and the third steady solution branch (third branch) by dashed line. The steady solution branches are obtained by using path continuation technique as discussed in Keller [20]. It is found that there is no bifurcating relationship among the branches. The first branch exists throughout the whole range of Tr investigated in this study. The second branch consists of two parts, the lower part and the upper part. The lower part contains two-vortex solution while the upper part four-vortex solution. The branch starts at small Tr (Tr = 0) and extends in the direction of increasing Tr (decreasing Q) up to Tr = 1425, and then the branch turns to the opposite direction with increasing Q (decreasing Tr) and finally stop at Tr = 0. The third branch has nearly the same characteristics as of the second branch, which starts at Tr = 0 and extends up to Tr = 2000 and then it turns to the opposite direction and finally end at Tr = 0. ![]() | Figure 2. Solution structure of steady solutions for Dn = 2000, Gr = 1000 at ![]() |
= constant) and temperature profiles (isotherms, T = constant) are drawn on various branches of steady solutions as shown in Fig. 3. To draw the contours of
and T, the increments
= 0.6 and ∆T = 0.2 are used. The same increments of
and T are used for all the figures in this paper, unless specified. The right-hand side of each duct box of
and T indicates outside direction of the duct curvature. In the figures of the streamlines, solid lines
show that the secondary flow is in the counter clockwise direction while dotted lines
in the clockwise direction. Similarly, in the figures of isotherms, solid lines are those for
and dotted ones for T < 0. As seen in Fig. 3, the secondary flow is an asymmetric two-vortex solution on the first branch, while asymmetric two- to four-vortex on the second and third branches. It is readily noted that the patterns of secondary flows are fundamentally different from those in a straight channel; even at low flow rate (low Dean number), the flow profile has two large counter-rotating vortices. This vortex flow is developed consequent to the combined action of the centrifugal, Coriolis and buoyancy forces induced by the duct stream-wise curvature.
atand Gr = 1000. Time evolution of Q for
showed that the unsteady flow is a steady-state solution. Then, in order to observe unsteady flow characteristics for
time evolution calculations are performed at Tr = 200, 500, 700 and 900. Time evolution of Q for Tr = 200 is shown in Fig. 4(a), where it is seen that the flow oscillates periodically. With a view to observe the change of the flow characteristics as time proceeds, typical contours of secondary flow patterns and temperature distributions are shown in Fig. 4(b) for one period of oscillation at
, and it is found that the periodic flow at Tr = 200 oscillates between asymmetric two-vortex solutions.
, and it is found that the unsteady flow at Tr = 700 oscillates between asymmetric two-vortex solution. Similarly, time evolution of Q for Tr = 900 is studied as presented in Fig. 7(a). Figure Fig. 7(a) shows that the unsteady flow at Tr = 900 oscillates multi-periodically. Typical contours of secondary flow patterns and temperature profiles are then shown in Fig. 7(b) for
where it is seen that the unsteady flow at Tr = 900 also oscillates between the asymmetric two-vortex solutions. In fact, the periodic oscillation, which is observed in the present study, is a traveling wave solution advancing in the downstream direction which is well justified in the recent investigation by Yanase et al. [21] for a three-dimensional (3D) travelling wave solutions as an appearance of 2D periodic oscillation.![]() | Figure 5. Unsteady solution for Tr = 500, Dn = 2000 and Gr = 1000. (a) Time evolution of Q. (b) Contours of secondary flow patterns (top) and temperature profiles (bottom) at ![]() |
![]() | Figure 6. Unsteady solution for Tr = 700, Dn = 2000 and Gr = 1000. (a) Time evolution of Q. (b) Contours of secondary flow patterns (top) and temperature profiles (bottom) at ![]() |
plane, where
as shown in Figs. 8(a) to 8(d) for Tr = 200, 500, 700 and 900 respectively. The orbits are drawn by tracing the time evolution of the solutions. As seen in Fig. 8(a), the time evolution result presented in Fig. 4 for Tr = 200 is periodic. But as seen in Fig. 8(b), which shows the phase orbits of the time evolution result for Tr = 500 (Fig. 5) shows that the flow is chaotic, though it was not clear in the time evolution result. This type of flow evolution is termed as transitional chaos (Mondal et al. [8]). Similarly, phase space (Fig. 8(c)) of the time evolution result for Tr = 700 (Fig. 6) shows that it is also chaotic. However, Fig. 8(d) shows that the flow is a transitional chaos for Tr = 900 at some extent rather than multi-periodic as predicted in Fig. 7.![]() | Figure 7. Unsteady solution for Tr = 900, Dn = 2000 and Gr = 1000. (a) Time evolution of Q. (b) Contours of secondary flow patterns (top) and temperature profiles (bottom) at ![]() |
![]() | Figure 8. Phase plots in the plane for Dn = 2000 and Gr = 1000 at (a) Tr = 200, (b) Tr = 500, (c) Tr = 700, (d) Tr = 900 |
. In the present study, flow characteristics are investigated for Dn = 2000 and Gr = 1000 for a constant curvature of the channel at
. After a comprehensive survey over the parametric ranges, three branches of asymmetric steady solutions are obtained by using path continuation technique. It is found that there exist asymmetric two-, three- and four- vortex solutions on the steady solution branches. These vortices are generated due to combined action of the centrifugal, Coriolis and buoyancy forces. It is found that the first steady solution branch exists throughout the whole range of Tr, which consists of asymmetric two-vortex solutions. The second branch is composed of asymmetric two- and four-vortex solutions while the third branch asymmetric two- and four-vortex solutions but different from those of the second steady solution branch. Then in order to study non-linear behavior of the unsteady solutions, time-evolution calculations were performed, and it is found that the unsteady flow becomes periodic first, then chaotic (transitional chaos) and finally turns into multi-periodic if Tr is increased. Drawing the phase spaces was found to be very fruitful to well identify the transition of the unsteady flow characteristics. In the case of heat transfer from the heated wall to the fluid, it is found that convective heat transfer is significantly enhanced as the rotation increases. It is also found that there is a strong interaction between the heating-induced buoyancy force and the centrifugal-Coriolis instability of the flow in the curved channel that stimulates fluid mixing and consequently enhance heat transfer in the fluid. It should be noted here that irregular oscillation of the flow through a curved duct has been observed experimentally by Ligrani and Niver [14] for the large aspect ratio and by Wang and Yang [22] for the curved square duct.