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Mathematical Methods for Physicists: A concise introduction - Site Map

Mathematical Methods for Physicists: A concise introduction - Site Map

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SOME METHODS OF SOLUTION<br />

Note that g…x† is a constant as far as the t integration is concerned, hence it may<br />

be taken outside the integral sign and we have<br />

Now<br />

u…x† ˆf …x†‡ Xn<br />

Z b<br />

a<br />

iˆ1<br />

g i …x†<br />

Z b<br />

a<br />

h i …t†u…t†dt:<br />

h i …t†u…t†dt ˆ C i …ˆ const:†:<br />

Substituting this into Eq. (11.7) and solving <strong>for</strong> u…t†, we obtain<br />

u…t† ˆf …x†‡C Xn<br />

iˆ1<br />

g i …x†:<br />

…11:7†<br />

…11:8†<br />

…11:9†<br />

The value of C i may now be obtained by substituting Eq. (11.9) into Eq. (11.8).<br />

The solution is only valid <strong>for</strong> certain values of , and we call these the eigenvalues<br />

of the integral equation. The homogeneous equation has non-trivial solutions<br />

only if is one of these eigenvalues; these solutions are called eigenfunctions of<br />

the kernel (operator) K.<br />

Example 11.1<br />

As an example of this method, we consider the following equation:<br />

u…x† ˆx ‡ <br />

Z 1<br />

0<br />

…xt 2 ‡ x 2 t†u…t†dt:<br />

…11:10†<br />

This is a Fredholm equation of the second kind, with f …x† ˆx and<br />

K…x; t† ˆxt 2 ‡ x 2 t. If we de®ne<br />

ˆ<br />

then Eq. (11.10) becomes<br />

Z 1<br />

0<br />

t 2 u…t†dt;<br />

ˆ<br />

Z 1<br />

u…x† ˆx ‡ …x ‡ x 2 †:<br />

0<br />

tu…t†dt;<br />

To determine A and B, we put Eq. (11.12) back into Eq. (11.11) and obtain<br />

Solving this <strong>for</strong> and we ®nd<br />

…11:11†<br />

…11:12†<br />

ˆ 1<br />

4 ‡ 1 4 ‡ 1 5 ; ˆ 1<br />

3 ‡ 1 3 ‡ 1 4<br />

: …11:13†<br />

60 ‡ <br />

ˆ<br />

240 120 2 ; ˆ 80<br />

240 120 2 ;<br />

and the ®nal solution is<br />

u…t†<br />

ˆ…240 60†x ‡ 80x2<br />

240 120 2 :<br />

415

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