Continuum Methods for Industry Draft date: 26 January 2015 1–1
1 Free boundary problems
1.1 Introduction
A free boundary problem occurs when the region in which the problem is to be solved is unknown in advance and must be found as part of the solution. We will described a canonical free boundary problem known as the Stefan problem, which describes the flow of heat through a material where a phase change occurs. For example, when a block of ice melts to form water (or when water freezes to form ice), we have to solve for free boundary between the two phases as well as for the temperature field in each phase. As we will see, these problems can become ill-posed, predicting pathalogically unstable behaviour. We will show how a well-posed and physically realistic model may be formulated by introducing a “mushy region”. The Stefan problem is a canonical “codimension-one” free boundary problem: the free boundary has dimension one below that of he space in which the problem is solved. (For example, the free boundary between ice and water in three dimensions is a two-dimensional surface.) A slightly rarer situation is a “codimension-two” free boundary problem, where the free boundary has two fewer dimensions than the space in which the problem is solved. For example, this would describe a two-dimensional problem in which the free boundary consists of a set of points. We will analyse in detail a relatively simple codimension-two free boundary problem that describes electropainting of a metal surface. As we will see, such problems often lead to singular integral equations, and we will show how a simple example can be solved analytically.
1.2 Stefan problems
Industrial problem: electric welding One convenient way to weld steel plates is to place them together, attach electrodes to the edges and then pass a large electric current through. This heats the metal, causing a neigh- bourhood of the interface between the plates to melt. When the current is switched off, the liquid metal solidifies and the two plates are welded together. Since the interfacial region cannot be observed directly, we must know in advance how long the current should be applied to ensure that the metal melts without melting the entire plates. We must also calculate how long the plates should be left once the current has been switched off to ensure that they have solidified completely.
One-dimensional Stefan problem Consider a slab of initially solid material occupying the region 0 < x < a. The temperature T (x, t) in the slab satisfies the heat equation ∂T ∂ ∂T ρc = k , (1.1) ∂t ∂x ∂x 1–2 Mathematical Institute University of Oxford where ρ, c and k are the density, heat capacity and thermal conductivity. In (1.1) we have neglected any heat sources (for example electric heating) and assumed that the heat flux q satisfies Fourier’s law ∂T q = −k . (1.2) ∂x We focus for the moment on a concrete problem in which the slab is initially at a uniform temperature T0 and the face x = a is insulated, while the temperature of the face at x = 0 is suddenly increased to a temperature T1 > T0. We then have to solve (1.1) subject to the initial and boundary conditions ∂T T (x, 0) = T , 0 < x < a; T (0, t) = T , t > 0; (a, t) = 0, t > 0. (1.3) 0 1 ∂x
If T1 is high enough, then we expect the solid to melt and become liquid in some neigh- bourhood of x = 0. If so, we must seek a solution in which the slab is liquid in 0 < x < s(t) and solid in s(t) < x < a, where x = s(t) is the free boundary separating the liquid and solid phases. The position of the free boundary is unknown in advance and must be found as part of the solution. In general we have to solve the heat equation (1.1) in both solid and liquid phases, i.e. in 0 < x < s(t) and in s(t) < x < a, with different values of the parameters ρ, c and k on either side. We also need to impose conditions at the free boundary x = s(t). First we assume that the phase change happens at a known melting temperature:
T (s(t), t) = Tm. (1.4)
The temperature is continuous so this applies on both sides of the free boundary. The second condition comes from an energy balance. At a fixed boundary, the heat flux coming in from one side must equal the heat flux exiting from the other side, i.e. q = −k∂T/∂x must be continuous. However, at a moving interface, we must also consider the energy associated with the phase change, known as the latent heat L. For example, the latent heat of water is L = 334 kJ/kg, meaning that it requires 334 kJ of energy to turn 1 kg of ice at 0◦C to 1 kg of water at 0◦C. The latent heat acts as an energy source or sink at a moving solid-liquid interface, and the resulting boundary condition
∂T ∂T ds k − k = ρL (1.5) ∂x x=s(t)+ ∂x x=s(t)− dt is known as the Stefan condition. In summary, the Stefan problem consists of the heat equation (1.1) on either side of the free boundary x = s(t), where the two conditions (1.4) and (1.5) are applied. The problem is closed by suitable boundary and initial conditions, for example (1.3). Before proceeding, we briefly review some of the assumptions that have been made so far. In using Fourier’s law (1.2), we have assumed that the heat flux is purely due to thermal conductivity. If the liquid flows at all, then there will also be a contribution due to convection. Generally there is a change in density as the material melts, so that ρ is discontinuous across x = s(t). This would inevitably mean there must be a nonzero velocity [why?] and therefore a nonzero convective heat flux. It is a good exercise to work out how the model should be modified to include convection. For the moment, we can avoid such complications by assuming that the density change at the solid-liquid interface is small enough to be neglected. Continuum Methods for Industry Draft date: 26 January 2015 1–3
One-phase Stefan problem To make progress we will make some more simplifying assumptions. We will assume that ρ, c and k are all constant on either side of the solid-liquid interface — in general they may all be functions of temperature. We will also for the moment suppose that the initial temperature T0 is equal to the melting temperature Tm. This means that the solid region s(t) < x < a is always at temperature Tm and we only need to solve the heat equation in the liquid phase 0 < x < s(t): this is a one-phase Stefan problem. We nondimensionalise as follows: 2 0 ρLa 0 x = ax , t = t ,T = Tm + (T1 − Tm)u. (1.6) k(T1 − Tm) Then with primes dropped, we get a normalised one-phase Stefan problem in the form ∂u ∂2u St = 0 < x < s(t), t > 0, (1.7a) ∂t ∂x2 u = 1 x = 0, t > 0 (1.7b) ∂u ds u = 0, − = x = s(t), t > 0 (1.7c) ∂x dt s(0) = 0. (1.7d) Clearly generalised versions of (1.7) would be obtained if we relaxed some of the simplifying assumptions made above. The dimensionless parameter1 c(T − T ) St = 1 m , (1.8) L called the Stefan number, measures the relative importance of the sensible heat and the latent heat; in other words, the energy needed to raise the temperature of the material and the energy needed to melt it. We can seek a similarity solution of (1.7) in which √ x s(t) = β t and u(x, t) = f(η), where η = √ , (1.9) t for some constant β, and d2f St df + η = 0 0 < η < β, (1.10a) dη2 2 dη f = 1 η = 0, (1.10b) df β f = 0, = − η = β. (1.10c) dη 2 This is again a free boundary problem: the three boundary conditions imposed on a second- order ODE in principle determine β as part of the solution. The solution is given by √ erf η St/2 f(η) = 1 − √ , (1.11) erf β St/2
1beware: some authors define the Stefan number to be the reciprocal of our definition 1–4 Mathematical Institute University of Oxford
β
1
0.50
0.10
0.05 St 10-2 1 100 104
Figure 1.1: The relation between the parameter β and the Stefan number St determined by equation (1.12). The dashed curves show the asymptotic limits (1.13).
where β satisfies the transcendental equation
√ 2 √ πβeStβ /4 erf β St/2 √ = 1. (1.12) 2 St The relation between β and the Stefan number St is plotted in Figure 1.1, along with the asymptotic limits √ 2 as St → 0, s β ∼ 2 St (1.13) √ log √ as St → ∞. St π It is a good exercise to try and derive these, either by analysing equation (1.12) or by starting from the problem (1.10). Given the value√ of St, we can thus determine β and hence the evolution of the free boundary s(t) = β t. This square-root behaviour of the free boundary as a function of time is characteristic of Stefan problems. The entire slab has melted when s(t) = 1, and the dimensionless time taken is thus given by 1/β2. By reversing the nondimensionalisation (1.6) and using (1.13), we find two alternative approximations for the dimensional melting time tm, namely ρLa2 St 1, 2k(T − T ) t ∼ 1 m (1.14) m ρca2 √ St 1. 4k log (St/ π) When the Stefan number is small, the melting of the slab is mainly limited by the latent heat required. At the other extreme, the main barrier is the energy needed to heat up the slab, and the melting time depends only weakly on the latent heat L. The limit St 1 is very helpful and often valid: Figure 1.1 suggests that the small-St approximation works well even for values of St up to around 1. For example, suppose we try Continuum Methods for Industry Draft date: 26 January 2015 1–5 to melt a block of ice by heating one face to 5◦C. The relevant parameters are L = 334 kJ/kg and c = 4.2 kJ/kg K so that St ≈ 0.06. In this case, the value√ of β obtained by solving the transcendental equation (1.12) differs from the limiting value 2 by around 1%.
Two-phase Stefan problem The two-phase version of the dimensionless Stefan problem considered above reads
∂u ∂2u St = 0 < x < s(t), t > 0, (1.15a) ∂t ∂x2 St ∂u ∂2u = s(t) < x < 1, t > 0, (1.15b) κ ∂t ∂x2 u = 1 x = 0, t > 0, (1.15c) ∂u = 0 x = 1, t > 0, (1.15d) ∂x ∂u+ ∂u− ds u = 0,K − = x = s(t), t > 0 (1.15e) ∂x ∂x dt u = −θ, s = 0 t = 0, (1.15f) where the new dimensionless parameters are
c k k T − T κ = 1 2 ,K = 2 , θ = m 0 . (1.16) c2k1 k1 T1 − Tm
Here we have denoted the values of the specific heat and thermal conductivity in the solid and liquid phases by c1, k1 in 0 < x < s and c2, k2 in s < x < 1. In general, this problem must be solved numerically. However, analytical progress can be made in some special cases. As noted above, it is often valid and helpful to consider the limit St → 0, in which case the PDEs (1.15a) and (1.15b) are quasi-steady and may be integrated directly. We then quickly get x 1 − 0 < x < s(t) < 1, u(x, t) = s(t) (1.17) 0 0 < s(t) < x < 1,
and the Stefan condition (1.15e) then leads to
ds 1 = , (1.18) dt s and hence √ s(t) = 2t, (1.19) √ which is equivalent to (1.9) in the small-St limit where β = 2. However, the approximate solution (1.17) does not satisfy the initial condition (1.15f), except in the special case where θ = 0 (i.e. T0 = Tm). This may easily be resolved by considering a small-t boundary layer in which u adjusts from the initial value −θ to the “outer” solution (1.17) — see Exercise 2. 1–6 Mathematical Institute University of Oxford
y LIQUIDSOLIDSOLID LIQUID