On the Nusselt Solution of a Nonisothermal Two-Fluid Inclined Film Flow
Nonisothermal viscous two-fluid flows occur in numerous kinds of coating devices. The corresponding mathematical models often represent two-dimensional free boundary value problems for the Navier-Stokes equations or their modifications. In the present paper we are concerned with a particular problem of coupled heat and mass transfer. Marangoni convection is incorporated, too. The solvability of a corresponding stationary problem is discussed. The obtained results generalize previous results for a similar isothermal problem.
Thermocapillary convection describes a fluid motion driven by surface-tension gradients on a liquid-liquid interface, where these gradients arise from the temperature dependence of interface tension. This type of convection is quite important in several technological and scientific applications; interesting examples may be found in the field of materials science, particularly in coating and solidification processes or in crystal-growth processes (cf. [1–5]).
In this paper we study a problem for a 2D stationary flow with two viscous incompressible heat-conducting fluids (having kinematic viscosities , densities and thermal conductivities , ) down an inclined bottom having a slope (cf. Figure 1). In fact, the bottom represents a perturbed plane. Assume that the bottom is given by the formula with having a compact support, that is, for , and suppose that the direction of the gravitational force is the vector which makes (with respect to the chosen coordinate system) an angle with the -axis. Note that the corresponding problem will be formulated in dimensionless form. The concrete transition to that formulation can be found in .
Let us formulate the problem. We consider the two-fluid flow down the inclined bottom caused by gravity , only. This means mathematically that the positive (final) layer thickness in each liquid layer is a priori prescribed. In slide coaters, such flows occur on some parts of the coater. The corresponding flow fields and layer profiles are essential there.
Suppose that the free interface separating the two fluid layers and the upper free surface admit the parametrizations , where the functions are a priori unknown and have to be found. Let be the prescribed constant limits of , at infinity. The problem under consideration has the following form: to find a vector of velocity , a pressure , a temperature , and functions satisfying in the domain with and , then the following equations of a coupled heat and mass transfer are
and the boundary and integral conditions are
By we denote the thermal conductivity of the th fluid () in Problem (1.1)–(1.4). The symbol means the acceleration of gravity. The value is the (constant) given temperature of the wall . Without loss of generality one can suppose that and that is in fact the difference between the physical temperature and . By and we denote the given (constant) pressure and temperature of the ambient air, respectively.
Furthermore, the subsequent notations have been used: and are unit vectors normal and tangential to and oriented as , respectively. By we mean the inner product of is the gradient operator, , is the restriction of to (analogously for and ) and denotes the Laplace operator. By we denote the deviatoric stress tensor, that is, a matrix with elements . The symbol denotes the jump of crossing the free interface , that is,
and the symbol denotes the limit from below at the interface ; more precisely
Note that the left-hand side of (1.3)6 (i.e., of the sixth equation in (1.3)) is equal to the curvature of . The same is true for in case of . Furthermore, (1.3)5 represents the mathematical expression of the so-called Marangoni convection.
2. General Solution Technique
Mathematical problems for the stationary flows of a viscous incompressible fluid with a free boundary were studied by many authors. Numerous references on this topic can be found, for example, in the bibliographies of [7–10]. In the analytical investigations [1–3, 5, 11], the temperature dependence was additionally taken into account. Numerical studies of nonisothermal free boundary problems can be found in the papers [1, 6].
In order to solve such kind of problems—in , and independently in , an appropriate scheme was proposed based on a linearization of the original problem on a corresponding exact solution in the unperturbed “uniform” flow domain, say: . The main difference of this scheme from previous applied ones is that on each step of iterations the determination of is not separated from the determination of the free boundaries (i.e., from the determination of the functions describing ). For Problem (1.1)–(1.4) this scheme can be illustrated by the diagram
where on each step of iterations the linearized problem is solved in the same “strip-like” domain and the functions , and are determined simultaneously.
A significant part in deriving the correct linearization takes the determination of exact solutions of the nonlinear problems in a “uniform” (not distorted) flow domain. These exact (basic) solutions in the uniform domain will be calculated in the appendix. They are also important for the numerical flow simulation: they can be used as inlet boundary data in more complicated problems. In  the analogous isothermal problem (without any inclusion of temperature) to Problem (1.1)–(1.4) was solved by numerical methods.
3. Function Spaces
and their union. We introduce the space of functions on with restrictions belonging to having the finite norms
where is the usual Sobolev space. The norm in is given by
If , then elements of vanish exponentially as , and if , then elements might exponentially increase as .
The spaces of functions defined on can be introduced analogously. Let be a line. Denote by the spaces of traces on of functions from . Then coincides with , that is, if , then .
In the paper the spaces of scalar and vector-valued functions are not distinguished in notations. The norm for vector-valued functions is then the sum of the norms of the corresponding coordinate functions.
4. Solvability Results
Theorem 4.1. Let with , and , where denotes the slope of the inclined bottom . Assume that is sufficiently small. Then there exist positive numbers such that for every . Problem (1.1)–(1.4) has a unique solution . The solution admits the representation where are the functions of the basic solution from (A.3)–(A.6), while and the following inequalities hold:
We would like to present a short sketch of the proof of this theorem by successive approximations. First, the original (perturbed) and unknown flow domain (cf. Figure 1) is transformed onto the uniform (strip-like) domain . Then, using this transformation mapping, the original flow Problem (1.1)–(1.4) is linearized over the basic solution (A.3)–(A.6) (see the appendix) in domain . By we denote the operator of the left-hand side of that linearized auxiliary problem. In virtue of a corresponding theorem for the linear auxiliary problem (see, e.g., ), there exists a bounded inverse operator such that
with . Herein is independent of and depends on eigenvalues of the operator pencils associated with the corresponding linear problem (cf. ). Also, the multidimensional space to which the right-hand side of the linearized problem belongs is introduced in a similar way as that of the space (see above). Moreover, one can show that there holds the estimate
where and , denotes the long vector of right-hand side after the linearization. The elements of the right-hand side vector depend on via the transformation mapping of the original flow domain. In order to show the convergence of the successive approximations , it is sufficient to show that the operator is a contraction mapping in a ball of the space for small values of and .
Note that the corresponding isothermal problem to Problem (1.1)–(1.4) (i.e., without any inclusion of temperature) was analytically examined in details in the papers [8, 13]. In order to prove Theorem 4.1 in details, one has to repeat and to modify all the investigations from those papers. Since the temperature equation is also nonlinear elliptic there, are not essential changes in the proof. Thus we omit the detailed proof here.
On the Nonisothermal Base Flow
Let us now investigate the two-fluid flow in the “uniform” two-fluid domain down the really inclined plane, that is, in the case where is replaced by the inclined straight line . We suppose that the (unknown) free interface and the free surface permit the representations , and we are looking for stationary unidirectional flows. Such flows fulfil the assumptions
As a consequence we obtain that the pressure gradient downstream is a constant Since the motion is generated by gravity, only the pressure gradient downstream must be equal to 0. Under these assumptions, the nonisothermal Navier-Stokes equations reduce to
and the equation of continuity (1.1)2 is automatically fulfilled. Problem (1.1)–(1.4) can now be transformed to three systems of equations containing the unknowns , and , independently. These three systems have the following solutions:
The so-called fluxes for both liquid layers that are the integrals
Recall that if is small, then for the fluxes the same is true. Furthermore, let us emphasize that solution (A.3)–(A.6) to problem (A.2) is frequently called Nusselt solution of the inclined film flow in the fluid mechanical literature.
The author is grateful for the comments and suggestions of the anonymous referee.
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