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Computer simulation of thermal convection in Rayleigh-Bénard cell ...

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Hubert Jopek<br />

<strong>Computer</strong> <strong>simulation</strong> <strong>of</strong> <strong>thermal</strong> <strong>convection</strong> <strong>in</strong> <strong>Rayleigh</strong>-<strong>Bénard</strong> <strong>cell</strong><br />

Chapter 5: Govern<strong>in</strong>g equations<br />

There are several methods which could be used to derive the Lorenz<br />

equations system, one <strong>of</strong> them is presented below [5]. The Navier-Stokes equation<br />

for fluid flow and <strong>thermal</strong> energy diffusion equation are used. This problem, like<br />

many others, has no exact analytical solution, so approximation methods will be<br />

used <strong>in</strong> order to create a possibly reliable theoretical model. The Lorenz equations<br />

system is one <strong>of</strong> the most famous models <strong>in</strong> the doma<strong>in</strong> <strong>of</strong> nonl<strong>in</strong>ear dynamics i.e. it<br />

can be applied to describe the motion <strong>of</strong> the fluid under conditions <strong>of</strong> <strong>Rayleigh</strong>-<br />

<strong>Bénard</strong> flow which have been already presented.<br />

As a result <strong>of</strong> the assumed two-dimensional geometry, only vertical and<br />

horizontal velocity components are considered. The form <strong>of</strong> Navier-Stokes equations<br />

for this case is as follows:<br />

∂υ<br />

z<br />

ρ<br />

∂t<br />

∂υ<br />

x<br />

ρ<br />

∂t<br />

r<br />

+ ρυ ⋅ grad υ<br />

r<br />

+ ρυ ⋅ grad υ<br />

z<br />

x<br />

∂p<br />

2<br />

= −ρg<br />

− + µ ∇ υ<br />

z<br />

∂z<br />

, (5.1)<br />

∂p<br />

2<br />

= − + µ ∇ υ<br />

x<br />

∂x<br />

where: ρ - mass density <strong>of</strong> the fluid; g - strength <strong>of</strong> the local gravitational field; p -<br />

fluid pressure; µ - fluid viscosity<br />

The next step is to describe the temperature T. It’s done us<strong>in</strong>g <strong>thermal</strong><br />

diffusion equation <strong>in</strong> the form:<br />

∂T<br />

∂t<br />

2<br />

+<br />

r υ ⋅ grad T = D ∇ T , (5.2)<br />

T<br />

where<br />

D<br />

T<br />

- <strong>thermal</strong> diffusion coefficient.<br />

12

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