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Laplace transform isotherm .pdf - University of Hertfordshire ...

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This is the most general form <strong>of</strong> the heat equation.<br />

In our work, we consider the case where K is constant and ρ and c are<br />

independent <strong>of</strong> time and we use the following form <strong>of</strong> the heat equation,<br />

which is the most convenient for our purposes:<br />

where α = K<br />

pc<br />

∇ 2 u = 1 ∂u<br />

α ∂t<br />

is the thermal diffusivity.<br />

(2.2)<br />

The partial differential equation for diffusion problems is set up in a<br />

similar manner (Crank 1979) and its form is<br />

∂2C 1 ∂C<br />

=<br />

∂x2 D ∂t<br />

C is the concentration <strong>of</strong> the diffusing substance and D is the diffusion<br />

coefficient and the law equivalent to Fourier’s law in equation (2.1) is Fick’s<br />

law<br />

q = −DgradC<br />

The heat equation is a partial differential equation and in the next section<br />

we look at the classification <strong>of</strong> partial differential equations, because the<br />

nature <strong>of</strong> the solution depends on the classification <strong>of</strong> the equation.<br />

2.1.1 Classification <strong>of</strong> partial differential equations<br />

In order to classify the equations, we will consider the linear partial differ-<br />

ential operator L in two independent variables for simplicity, which can be<br />

extended to three or more variables (Weinberger 1965). We define the linear<br />

partial differential operator as<br />

L [u] ≡ A(x,y) ∂2u ∂y2 +B (x,y) ∂2u ∂x∂y +C (x,y) ∂2u ∂u ∂u<br />

∂x2+D (x,y) +E (x,y) +F (x,y)u<br />

∂y ∂x<br />

and if<br />

L [u] = G<br />

6

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