Next: About this document ...

Last Time
Electromigration

Anisotropy and Onsager Coefficients

The Diffusion Equation

The Diffusion Equation for Uniform Diffusivity

The Steady-State Condition

3.21 Spring 2002: Lecture 07

Scaling and the Diffusion Equation

Note that the diffusivity has units (number    cm)/s; therefore, is dimensionless.

Introduce a dimensionless variable :

 (07-1)

Suppose for a particular problem, that the boundary and initial conditions are also invariant to this scaling implied by , in other words, if the length scale is tripled (yards instead of feet) then the time scale for the boundary conditions is multiplied by a factor of nine. Or, under the scaling,

 then: (07-2)

the boundary conditions can be written entirely in terms of the one dimensionless variable .

An example of such a problem would be the step-function'' initial conditions with either Dirichlet or zero-flux Neumann boundary conditions at :

Initial conditions:

 (07-3)

or

 (07-4)

with boundary conditions:

 or (07-5)

and

 or (07-6)

Using the definition for :

 (07-7)

The diffusion equation becomes:

 (07-8)

Because everything in the above equation depends only on , the partial differential equation becomes an ordinary differential equation ( ) that can be integrated without too much difficulty.

Let

 (07-9)

so that

 (07-10)

which can be integrated

 (07-11)

where is an integration constant and this can be integrated again

 (07-12)

Let and with the step-function initial conditions, ,

 (07-13)

or, by introducing another constant for ,

 (07-14)

The integral with an argument is just some function with a peculiar name:

 (07-15)

that has the properties: , (this is where the comes from),

So, the solution to the one-dimensional step function IC uniform diffusion equation is:

 (07-16)

or

 (07-17)

Short Distances, Long Times

An additional and useful property of the error function is that for

Because the scaling parameter is small for long times where is the characteristic diffusion time:1

 (07-18)

or for short distances where is the characteristic diffusion length:

 (07-19)

the solution of the step-function IC becomes:

 (07-20)

The flux at the origin varies as,

 (07-21)

The total amount of material that flows past the origin (per unit area) up to a time goes as :

 (07-22)

Superposition Example

The simple solution that was developed above can be used with the method of superposition to develop a large number of solutions.

For example, suppose the initial conditions are changed so that there is a finite source of material diffusing into an infinite material and the finite source is confined to slab of with in the -direction but extending infinitely in the - and -directions.2

These initial conditions can be obtained by summing two known solutions, i.e. those for the initial conditions:

 (07-23)

and

 (07-24)

The solution is just the sum:

 (07-25)

 (07-26)

It will be beneficial to reflect on what kinds of problems (i.e. which initial and boundary conditions) will admit solutions from scaling and then subsequent summing of solutions. First for the scaling solution, the boundary and initial conditions had to be invariant under the scale factor --this is usually the case for infinite domains with zero flux conditions at . Second, the summing method works when each solution that is to be summed also satisfies scaling--therefore the initial conditions for the particular problem must also be invariant. Typically, these methods are useful in the infinite domain.

The One-Dimensional Fundamental Solution

The solution for point-source'' initial conditions will prove to be quite useful for cases when the addition of a large number of solutions generate the initial conditions for a particular problem. The solution obtained in Eq. 7-26 can be used to obtain the fundamental solution. Expanding in powers of small :3

 (07-27)

This is the fundamental solution for a point source in a 1D infinite domain.

Many other solutions by summing point source solutions,

In general,4for almost any initial conditions on the 1D infinite domain with zero flux at ,

 (07-28)

Otherwise known as the the Green's function solution.5

Other Fundamental Solutions

The same method can be used to find fundamental solutions for cases where the finite source is a object of a given dimensionality embedded in an infinite space of larger dimension. This is called the co-dimension'' and it is the dimensionality of the infinite region minus the dimensionality of the embedded object.

All the pertinent examples are contained in the following table:
 Co-dimension Example Symmetric Part of Fundamental Solution Point on Line 1 Line on Plane Plane in 3D 2 Point in Plane Line in 3D 3 Point in 3D

Next: About this document ...
W. Craig Carter 2002-02-22