Abstract
The mixed convection flow near an axisymmetric stagnation point on a vertical cylinder is considered. The equations for the fluid flow and temperature fields reduce to similarity form that involves a Reynolds number R and a mixed convection parameter λ, as well as the Prandtl number σ. Numerical solutions are obtained for representative values of these parameters, which show the existence of a critical value λ c = λ c (R, σ) for the existence of solutions in the opposing (λ < 0) case. The variation of λ c with R is considered. In the aiding (λ > 0) case solutions are possible for all λ and the asymptotic limit λ → ∞ is obtained. The limits of large and small R are also treated and the nature of the solution in the asymptotic limit of large Prandtl number is briefly discussed.
Authors
C. Revnic
Tiberiu Popoviciu Institute of Numerical Analysis Cluj, Romanian Academy
T. Grosan
Applied Mathematics, Babes-Bolyai University Cluj, Romania
J. Merkin
Department of Applied Mathematics, University of Leeds, Leeds, LS2 9JT, UK
I. Pop
Applied Mathematics, Babes-Bolyai University, Cluj, Romania
Keywords
Asymptotic solutions; Axisymmetric stagnation flow; Boundary layers; Dual solutions; Mixed convection
References
Paper coordinates
C. Revnic, T. Grosan, J. Merkin, I. Pop, Mixed convection flow near an axisymmetric stagnation point on a vertical cylinder, Journal of Engineering Mathematics, 64 (2009), pp. 1–13,
doi: 10.1007/s10665-008-9248-9
About this paper
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Springer
Print ISSN
0022-0833
Online ISSN
1573-2703
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[1] Hiemenz K (1911) Die Grenzschicht an einem in den gleich formigen Flussigkeitsstrom eingetacuhten geraden Kreisszylinder. Dinglers Polytech J 326: 321–324
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Article Google Scholar
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MATH Google Scholar
[7] Gorla RSR (1978) Nonsimilar axisymetric stagnation flow on a moving cylinder. Int J Eng Sci 16: 392–400
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[8] Weidman PD, Putkaradze V (2003) Axisymmetric stagnation flow obliquely impinging on a circular cylinder. Eur J Mech B/Fluids 22: 123–131
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[9] Weidman PD, Mahalingam S (1997) Axisymmetric stagnation-point flow impinging on a transversely oscillating plate with suction. J Eng Math 31: 305–318
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MATH Article Google Scholar
[13] Kuiken HK (1974) The thick free-convective boundary-layer along a semi-infinite isothermal vertical cylinder. J Appl Math Phys (ZAMP) 25: 497–514
MATH Article Google Scholar
[14] Naraian IP, Uberoi MS (1972) Combined forced and free convection heat transfer from thin needles in a uniform stream. Phys Fluids 15: 1879–1882
Article ADS Google Scholar
[15] Naraian IP, Uberoi MS (1973) Combined forced and free convection over thin needles. Int J Heat Mass Trans 16: 1505–1511
Article Google Scholar
[16] Chen ILS (1987) Mixed convection flow about slender bodies of revolution. J Heat Trans 109: 1033–1036
Article Google Scholar
[17] Wang CY (1990) Mixed convection on a vertical needle with heated tip. Phys Fluids A 2: 622–625
Article ADS Google Scholar
[18] Merkin JH (1985) On dual solutions occurring in mixed convection in a porous medium. J Eng Math 20: 171–179
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[19] Merkin JH, Mahmood T (1989) Mixed convection boundary layer similarity solutions: prescribed wall heat flux. J Appl Math Phys (ZAMP) 40: 51–68
MATH Article MathSciNet Google Scholar
[20] Stewartson K, Jones LT (1957) The heated vertical plate at high Prandtl number. J Aeronaut Sci 24: 379–380
Google Scholar
[21] Kuiken HK (1968) The heated vertical plate at high Prandtl number free convection. J Eng Math 2: 355–371
MATH Article Google Scholar
[22] Slater LJ (1960) Confluent hypergeometric functions. Cambridge University Press, Cambridge
Google Scholar
[23] Wilks G, Bramley JS (1981) Dual solutions in mixed convection. Proc R Soc Edinb 87A: 349–358
MathSciNet Google Scholar
Paper (preprint) in HTML form
Mixed convection flow near an axisymmetric stagnation point on a vertical cylinder
Abstract
The mixed convection flow near an axisymmetric stagnation point on a vertical cylinder is considered. The equations for the fluid flow and temperature fields reduce to similarity form that involves a Reynolds number and a mixed convection parameter , as well as the Prandtl number . Numerical solutions are obtained for representative values of these parameters, which show the existence of a critical value for the existence of solutions in the opposing ( ) case. The variation of with is considered. In the aiding ( ) case solutions are possible for all and the asymptotic limit is obtained. The limits of large and small are also treated and the nature of the solution in the asymptotic limit of large Prandtl number is briefly discussed.
Keywords Asymptotic solutions • Axisymmetric stagnation flow • Boundary layers • Dual solutions • Mixed convection
1 Introduction
Combined forced- and free-convection flows (mixed convection) are encountered in many technological and industrial applications including solar receivers exposed to wind currents, electronic devices cooled by fans, nuclear reactors cooled during emergency shutdown, heat exchanges placed in a low-velocity environment and many more. Two-dimensional stagnation-point flows arise in the vicinity of a stagnation line resulting from a two-dimensional flow impinging on a curved surface at right angles to it and thereafter flowing symmetrically about the stagnation line. Hiemenz [1] was the first to study two-dimensional stagnation-point flows. Later Eckert [2] and Gorla [3] considered the corresponding forced-convection heat-transfer problem. Three-dimensional stagnation-point flows have been studied by Homann [4] and Smith [5] and the axisymmetric stagnation-point flow on a circular cylinder by Wang [6] and Gorla [7]. The three-dimensional flow resulting from an axisymmetric stagnation flow
T. Grosan • I. Pop Applied Mathematics, Babes-Bolyai University, CP 253, 3400 Cluj, Romania
J. Merkin ( ) Department of Applied Mathematics, University of Leeds, Leeds LS2 9JT, UK
e-mail: amtjhm@maths.leeds.ac.uk
impinging obliquely on a body surface has been treated by Weidman and Putkaradze [8]. The problem of axisymmetric stagnation-point flow acting on a porous flat plate oscillating transversely in its own plane has been investigated by Weidman and Mahalingam [9]. In this case a three-dimensional flow results from a stagnation-point flow on a flat plate oscillating in its own plane. Gorla [10] has studied the unsteady viscous flow in the vicinity of an axisymmetric stagnation point on a circular cylinder.
The steady mixed convection flow near the stagnation region of a vertical flat plate has been studied by Ramachandran etal. [11] and by Gorla [12] for the flow near an axisymmetric stagnation point on a slender impermeable vertical cylinder. Mixed convection flows arise when the buoyancy forces resulting from temperature differences within the flow become comparable to the pressure gradient forces arising from the forced flow. As a consequence, both the flow and thermal fields are significantly affected by the buoyancy forces. The study of thick axisymmetric free-convection boundary layers along slender bodies has been shown by Kuiken [13] to have an unusual structure at large distances along the cylinder. When the boundary-layer variables are scaled so as to be of order unity within the boundary layer, the boundary conditions that hold on the surface of the slender body are given at a value of the independent variable which is close to zero. As a result, when a perturbation analysis is used to obtain the solution at large distances along the cylinder, the body is reduced to a line at the first approximation.
Several papers have been published previously on axisymmetric mixed convection boundary-layer flows along slender bodies. Naraian and Uberoi [14, 15] and Chen [16] have studied the mixed convection boundary layer on a vertical needle. These are bodies of revolution whose diameter is of the same order as the thickness of the velocity or thermal boundary layers that develop on it. By appropriately varying the radius of the needle, the boundary-layer equations admit similarity solutions. Wang [17] found a similarity solution for the mixed convection boundary layer on an adiabatic vertical needle with a heat source at the tip, a situation that arises, for example, for a stick burning at its lower end.
The present paper considers the steady mixed convection flow that develops near an axisymmetric stagnation point on a vertical isothermal cylinder in the case when the boundary layer is thick compared to the radius of the cylinder. We start by describing the governing equations, following closely [9,12] for the forced-convection problem. This results in two ordinary differential equations for the flow and temperature fields that involve, as well as the Prandtl number , the two further parameters , which is measure of the forced flow, and a mixed convection parameter . We consider both aiding flows (when the outer flow and the buoyancy forces are in the same direction, ) and opposing flows (when the outer flow and the buoyancy forces act in opposite directions, ). We start by giving numerical solutions to these equations for representative values of and , finding dual solutions for negative with critical points , requiring for the existence of a solution. We determine how varies with , before considering the asymptotic limits of (free-convection limit) and and .
2 Equations
We consider the steady mixed convection flow near an axisymmetric stagnation point on an infinite cylinder. The cylinder is taken as mounted vertically and the flow is assumed to be axisymmetric about the -axis, which measures distance along the cylinder in a vertical direction with gravity acting in the negative -direction. The stagnation point is at , where measures distance radially from the centre of the cylinder of radius . The ambient fluid has a constant temperature and the cylinder is maintained at a temperature . Having corresponds to assisting flow, with corresponding to opposing flow. The outer flow in this situation, taken directly from [12], is
| (1) |
where is the planar flow at large distances from the cylinder and where and are the velocity components in the and directions, respectively.
Again following [12], we introduce the variables
| (2) |
where is the temperature of the fluid. Applying (2) in the governing equations and making the standard Boussinesq approximation, we find that our flow is described by the similarity equations, again from [12],
| (3) | |||
| (4) |
subject to the boundary conditions, from (1), that
| (5) |
(primes denote differentiation with respect to ) where is the Prandtl number and where
| (6) |
are, respectively, a Reynolds number and a mixed convection parameter, with corresponding to assisting flow and corresponding to opposing flow. In (6) is the kinematic viscosity of the fluid, the acceleration due to gravity and the coefficient of thermal expansion.
The parameters perhaps of most physical interest are the skin friction parameter and the Nusselt number Nu, defined as
| (7) |
and where and are the dynamic viscosity and thermal conductivity, respectively. From (2), we have that
| (8) |
The problem given by (3-5) has been considered previously by Gorla [12] who presented a range of numerical results for both aiding and opposing flows. The results given by [12] are only for a specific value of , namely , with critical points giving a finite range of existence for opposing flows not being identified in [12]. We start by first describing our numerical solutions to Eqs. (3) and (4) subject to boundary conditions (5) for a range of values of and , thus adding to the numerical treatment given by Gorla [12]. Throughout we assume that the Prandtl number is of , our numerical results are all for the case when .
3 Numerical results
Equations (3) and (4) subject to boundary conditions (5) were solved numerically using a standard shooting method for solving boundary-value problems (D02AGF in the NAG library). In Fig. 1 we plot and against for (with ). This figure shows that, for , there is a critical value with solutions possible only for and for there are dual solutions. The value of decreases as is increased, thus giving a greater range of negative for possible solutions. For there is only one solution with the values of increasing and decreasing as is increased (for a given value of ). For the larger values of , the values of for becomes greater than those for the larger values of , indicating that, for sufficiently large values of increases as is decreased. However, the values of increase as is increased (for a given value of ).
In Fig. 2 we take values for representative respectively of aiding and opposing mixed convection and plot the corresponding values of and against . We see that in both cases decreases as is increased. However, for has a minimum value, of at , before increasing again for the larger values of . For there is a critical value of below which there are no solutions, as might be expected from Fig. 1.
3.1 Critical points
We saw in Fig. 1 the existence of a critical value of , requring for a solution to exist. We can calculate how varies with using the appproach described in [18,19]. Essentially we perturb about the solution given by to obtain a linear homogeneous problem. It is then the existence of a nontrivial solution to this homogeneous problem that determines for a given value of (and ). In Fig. 3 we plot against , with the figure showing
that decreases as is increased, seemingly in a linear manner for the larger values of , and increases towards zero as is reduced. The region in the ( ) parameter space where solutions exist is labelled on this figure.
Our numerical solutions suggest that considering various limiting forms would give some further insights into the nature of the solution. We now discuss these in more detail, starting with the free-convection limit, .
4 Asymptotic results
large
To obtain a solution valid for large we start by putting
,
leaving unscaled. This results in the equations
,
,
where primes now denote differentiation with respect to , subject to the boundary conditions
as .
Equations suggest looking for a solution by expanding
| (13) |
We can scale the leading-order problem obtained by substituting expansion (13) in (10, 11) by putting
.
This results in
,
,
subject to
as ,
where primes now denote differentiation with respect to . A numerical solution of (15-17) gives, for , .
We can continue to the next order by first rescaling
.
This gives, with (14),
,
,
subject to
as .
A numerical solution gives, again for , that .
From ( 9,14 ) and (18) we have
| (22) | |||
Expressions (22) show that, for sufficiently large values of increases as is increased and that decreases as is increased, in line with Fig. 1. In Fig. 4 we plot the values of and obtained from the numerical solution of against for . In both cases the asymptotic limit for large given by (22) is approached as increases, though more slowly for than for as might be expected from (22).
large
To obtain a solution for large, we follow the approach given in [8] for the forced-convection case and start by writing
| (23) |
and leaving unscaled. This results in the equations
| (24) |
| (25) |
subject to the boundary conditions given in ( 5 ) and where primes now denote differentiation with respect to . Equations suggest an expansion in powers of , the leading-order term just being the forced-convection limit discussed in [8].
For convection to have an effect at leading order we require to be large, specifically of . This leads us to put
| (26) |
The problem for the leading-order terms is now
| (27) |
| (28) |
still subject to the boundary conditions that
| (29) |
Equations (27-29) have to solved numerically and graphs of and for plotted against are shown in Fig. 5. From these figures we see that there is a critical value of with dual solutions for and no solutions for . For , we find that , giving
| (30) |
For there is only one solution with both and increasing as is increased.
Expression (30) shows a linear increase in with , as noted previously about Fig.3, and to confirm this asymptotic behaviour we plot the values of obtained from our numerical integrations to find against in Fig. 6. The numerically determined values approach this asymptotic limit (shown by the broken line), though only slowly as is increased, suggesting that the correction has a significant effect even at moderately large values of .
For large we can recover expressions (22) by putting
| (31) |
When (31) is substituted in equations (27-29) and then , we obtain equations (15-17) and, on using (26), the leading-order terms in (22).
small
The behaviour of the solution for small depends on whether is small or of . We start with the latter case, assuming that .
4.3.1 of
For this case we start in an inner region where is of and scale
.
The scaling factors and are to be determined, though we assume that
.
When (32) is substituted in and is taken, the leading-order terms are given by, on satisfying the boundary condtions on ,
| (34) |
for constants to be determined. Before continuing the solution in the inner region, we next consider the outer region.
For the outer region we write
where
with the scaling factor also to be determined. When (35) is substituted in (3,4) and the assumptions for given in (35) applied, we find that the leading-order problem in the outer region is
,
subject to the outer boundary conditions at leading order that
as .
To find the inner boundary conditions for (36) we need to match with the inner region.
We can express the inner solution (34) as, on using (35),
,
.
From (38) we choose
.
Hence is given implicitly by
with as .
We note that are consistent with the assumptions in and . Expressions then give, at leading order,
as .
To get higher order terms in (41) we need to consider the inner region again. On using (39) we see that an expansion of the form
| (42) |
is required, where the terms in (42) also include terms in
and for some constant . When ( 42 ) is substituted in ( 3,4 ) and using ( 32,35 ) we find, after some calculation, that the inner boundary condition (41) for the outer region becomes modified to
,
as .
We can remove the parameter from this problem by writing and then the problem in the outer region becomes
,
subject to the conditions that
as
and
,
as ,
where and .
The problem given by (44-46) has to be solved numerically to determine the constants and and we find, for , that . This then gives for small and ,
,
,
with given in terms of by (40). Equations (3,4) were solved numerically with for small values of . The solution domain increases as is decreased, in line with (35), and the outer boundary condition had to be applied at increasingly larger values of as was decreased, the results shown in Fig. 7 were obtained using . In Fig. 7 we give plots of and against obtained from our numerical integrations, the values obtained from (47) are shown by broken lines. The agreement with the asymptotic forms for small is not particularly good, though both solutions are following the same trend. This difference can, perhaps, be explained by the fact that the approach to the asymptotic forms (47) is only very slow, with correction terms of and hence has to be extremely small for these correction terms to have only a small effect. In practice we probably require values of too small for obtaining reasonably accurate numerical solutions. At these very small values of needs to be extremely large leading to errors in the shooting method employed to solve the two-point boundary-value problem.
4.3.2 small
We can see, particularly from ( 36,37 ), that, when is of , the flow is driven at leading order only by the natural-convection effects. The forced flow enters the solution at higher order. However, when is small, this cannot be the case and to get an estimate on when the forced-convection effects have an influence at leading order, we see from (35) that the buoyancy term included in equation (36) is of whereas the forced-convection term is of . This suggests, on using (40), that these two effects will be comparable when and leads us to put
with of for small.
We start our solution for this case in the inner region where we have at leading order, motivated by our previous solution for of ,
| (49) |
for constants and to be determined. For the outer region we now put
| (50) |
Applying (50) in (3,4) gives, at leading order,
| (51) |
now subject to the outer boundary conditions
| (52) |
and, on matching with the inner region,
| (53) |
We note that cannot be scaled out of problem (51-53) (as it could previously) and that, for (forced-convection limit)
| (54) |
giving
.
Plots of against obtained by solving (51-53) numerically are given in Fig. 8. This figure shows that there is a critical value of , with for , and dual solutions for . This gives
| (55) |
For there is only one solution and the problem given by (44-46) can be recovered for large by putting in (51-53) and letting .
5 Solution for large
Our previous numerical results were for the case and we expect qualitatively similar behaviour when is of , typical of gases. For liquids (water) is somewhat larger and it is thus worth briefly considering the large limit. Following the treatment in [20,21] we expect that, for large, the solution to involve a relatively thin thermal inner layer and a thicker outer viscous flow region. In the inner region we have
| (56) |
with left unscaled. At leading order, for large, we obtain
| (57) |
subject to
| (58) |
with the outer condition on relaxed at this stage and where primes denote differentiation with respect to .
Equations give
| (59) |
for some constant to be determined and
| (60) |
in terms of confluent hypergeometric functions [22]. Expressions (56) and (60) give
| (61) |
Expression (61) shows that the heat transfer increases as is increased, being of for large.
To determine the constant we need to consider the outer region, in which we can neglect the temperature and write . This leads to
| (62) |
and, on matching with the inner region, that
| (63) |
Equations are essentially the forced-convection limit with the solution given by [8]. Their solution then gives in terms of . For large [8] show that , giving of for and large.
The leading-order problem (57,58,62,63) for large does not give a critical value for . In fact, the solution is independent of at leading order, with the buoyancy forces arising at in the inner region. This suggests that the critical value will, for a given value of , decrease to large negative values as is increased. We illustrate this in Fig. 9 with a plot of against for and to compare with the results for . This figure clearly shows that the critical values has decreased for over that for , giving a greater range of for solutions in the opposing case. The values of have, for a given , also decreased for , in line with expression (61). In Fig. 10 we plot against again for , showing that decreases relatively slowly as is increased, as can be expected from the above analysis for the large case.
6 Conclusions
We have considered the mixed convection boundary-layer flow around an axisymmetric stagnation point. The equations for the flow and temperature fields reduce to similarity form ( ) and involve the three parameters, the Prandtl number , a Reynolds number and a mixed convection parameter , as defined in (6). The similarity equations were solved numerically for representative values of the parameters and ; see Figs. 1 and 2 . The main conclusions from these numerical integrations were that, for (opposing flow), there was a critical value of at which there was a saddle-node bifurcation with dual solutions for and no solutions for . For (aiding flow) there was a single solution for all . An asymptotic solution for large was derived, with the results summarized in (22).
The occurrence of dual solutions for opposing flows is not unexpected and is consistent with many previous studies of similarity solutions in mixed convection, see [18,19,23] for example. The critical value was seen to depend on (and on ), see Fig. 3. The possibilities of solutions having only a limited range of existence and the existence of dual solutions for opposing flows was not noticed by Gorla [12]. The reason for this is that the results in [12] were all for and our study suggests that the value of for this value of is quite large, well beyond the values for the mixed convection parameter taken in [12]. A solution for large was obtained which showed that is of in this case, as given in (30) for . Thus for strong external flows (large ) boundary-layer flows are still possible even when there are strongly opposing buoyancy forces. For small the flow was seen to be driven predominantly by the buoyancy forces when is of , as summarized in (47). However, for small both buoyancy and the external flow have comparable effects, giving a critical value of for small, as given by (55) for . The effect of weak external flows is then to severely limit the range of where there can be opposing flows.
The effect of having large values for the Prandtl number is to confine the thermal effects to a thin layer, of thickness , next to the cylinder with the outer flow being essentially given by forced convection. A consequence of this is, for opposing flows, to decrease to large negative values, with solutions then being possible for a large range of the mixed convection parameter.
Acknowledgements CR was supported by the CEEX grant No 2-CEx06-11-96/2006. JM and IP were both supported by a Royal Society (London) Joint Project Grant.
References
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1.
Hiemenz K (1911) Die Grenzschicht an einem in den gleich formigen Flussigkeitsstrom eingetacuhten geraden Kreisszylinder. Dinglers Polytech J 326:321-324
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2.
Eckert ERG (1942) Die Berechnung des Wärmeüberganges in der laminaren Grenzschicht um stromter Korper. VDI - Forchungsheft 416:1-24
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3.
Gorla RSR (1976) Heat transfer in an axisymmetric stagnation flow on a cylinder. Appl Sci Res 32:541-553
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4.
Hommann F (1936) Der Einfluss grosser Zähigkeit bei der Stromung um den Cylinder und um die Kugel. J Appl Math Phys (ZAMP) 16:153-164
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5.
Smith FT (1974) Three dimensional stagnation point flow in a corner. Proc R Soc Lond A 344:489-507
-
6.
Wang CY (1974) Axisymmetric stagnation flow on a cylinder. Quart Appl Math 32:207-213
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7.
Gorla RSR (1978) Nonsimilar axisymetric stagnation flow on a moving cylinder. Int J Eng Sci 16:392-400
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8.
Weidman PD, Putkaradze V (2003) Axisymmetric stagnation flow obliquely impinging on a circular cylinder. Eur J Mech B/Fluids 22:123-131
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9.
Weidman PD, Mahalingam S (1997) Axisymmetric stagnation-point flow impinging on a transversely oscillating plate with suction. J Eng Math 31:305-318
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10.
Gorla RSR (1979) Unsteady viscous flow in the vicinity of an axisymmetric stagnation point on a circular cylinder. Int J Eng Sci 17:87-93
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11.
Ramachandran N, Chen TS, Armaly BF (1988) Mixed convection in stagnation flows adjacent to vertical surface. J Heat Trans 110:173-177
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12.
Gorla RSR (1993) Mixed convection in an axisymmetric stagnation flow on a vertical cylinder. Acta Mech 99:113-123
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13.
Kuiken HK (1974) The thick free-convective boundary-layer along a semi-infinite isothermal vertical cylinder. J Appl Math Phys (ZAMP) 25:497-514
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14.
Naraian IP, Uberoi MS (1972) Combined forced and free convection heat transfer from thin needles in a uniform stream. Phys Fluids 15:1879-1882
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15.
Naraian IP, Uberoi MS (1973) Combined forced and free convection over thin needles. Int J Heat Mass Trans 16:1505-1511
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Chen ILS (1987) Mixed convection flow about slender bodies of revolution. J Heat Trans 109:1033-1036
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17.
Wang CY (1990) Mixed convection on a vertical needle with heated tip. Phys Fluids A 2:622-625
-
18.
Merkin JH (1985) On dual solutions occurring in mixed convection in a porous medium. J Eng Math 20:171-179
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Merkin JH, Mahmood T (1989) Mixed convection boundary layer similarity solutions: prescribed wall heat flux. J Appl Math Phys (ZAMP) 40:51-68
-
20.
Stewartson K, Jones LT (1957) The heated vertical plate at high Prandtl number. J Aeronaut Sci 24:379-380
-
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Kuiken HK (1968) The heated vertical plate at high Prandtl number free convection. J Eng Math 2:355-371
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Slater LJ (1960) Confluent hypergeometric functions. Cambridge University Press, Cambridge
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Wilks G, Bramley JS (1981) Dual solutions in mixed convection. Proc R Soc Edinb 87A:349-358
