Faculty of Engineering and Applied Science
2006 Fall
Use the method of Gaussian elimination to find the inverse of the matrix
![[ 1 0 2 ]
[ 1 1 1 ]
[ 3 2 5 ]](ff06/q1a.gif)
Reduce the augmented matrix [A | I] to
[I | A-1].
![[ 1 0 2 | 1 0 0 ]
[ 1 1 1 | 0 1 0 ]
[ 3 2 5 | 0 0 1 ]](ff06/q1b.gif)
Row operations:
R 2 – R 1
and
R 3 – 3R 1:
![[reduced augmented matrix]](ff06/q1c.gif)
R 3 – 2R 2:
![[reduced augmented matrix]](ff06/q1d.gif)
R 1 – 2R 3
and
R 2 + R 3:
![[I | A^(-1)]](ff06/q1e.gif)
Therefore
![A^(-1) =
[ 3 4 -2 ]
[ -2 -1 1 ]
[ -1 -2 1 ]](ff06/q1f.gif)
The second order ordinary differential equation
![]()
may be represented by the linked pair of first order ODEs

![]()
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Therefore the critical points are
| (0, 0) and (2, 0) |
|---|
Near any critical point (a, b), the
coefficient matrix becomes
![[ 0 1 ]
[ 2a-2 -3 ]](ff06/q2b1.gif)
Near (0, 0),
![]()
Trace(A) = a + d = –3
< 0
det(A) = ad – bc
= 2 > 0
D =
(a – d)2 + 4bc
= 9 – 8 = 1
> 0
![]()
The eigenvalues are real, negative and distinct.
Therefore
| (0, 0) is a[n asymptotically] stable node |
Near (2, 0),
![]()
Trace(A) = a + d = –3
< 0
det(A) = ad – bc
= –2 < 0
D =
(a – d)2 + 4bc
= 9 + 8 = 17
> 0
![]()
The eigenvalues are real and of opposite sign.
Therefore
| (2, 0) is a[n unstable] saddle point |
Near (0, 0),
![]()
Find the eigenvector for the eigenvalue –2:

(where c1 is any non-zero
real number)
Find the eigenvector for the eigenvalue –1:

(where c2 is any non-zero
real number)
Therefore the general solution near (0, 0) is
The two straight-line trajectories are
![]()
![]()
The limiting behaviours of all other trajectories are



BONUS QUESTION
Incorporating the influences of the stable node at (0, 0)
and the saddle point at
[Enhanced Maple® phase portrait]
[A Maple file is also available for this question.]
An initial value problem is defined by
![]()
![]()
![]()
![]()
![]()
![]()

Therefore
![]()
![]()
which is a linear ODE, with P = –1
and R = x.
![]()
![]()
![]()
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The complete solution is therefore
![]()
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The standard fourth order Runge-Kutta method has therefore
provided an extremely accurate value, correct to better
than four parts in a million.
An Excel file is available to illustrate this question.
Find the extremal y(x) for the integral
![I = Integral[1 to 2] { (1 + y')^2 / (2x + 1) } dx](ff06/q4integral.gif)
that passes through the points (1, 1) and (2, 4).

The Euler equation for extremals becomes

![]()
which leads to the general solution
![]()
But the points (1, 1) and (2, 4) both lie on this curve.
![[substitute into general solution]](ff06/q4e.gif)

![]()
Therefore the extremal for the integral I is
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Find the Fourier series expansion of the function
![]()
![]()
L = 1 . Therefore (using symmetry)

For n > 0,
|
Therefore the Fourier series of f (x) is |
![]() |
The first few terms of the series are

The summation can be re-written as the equivalent form

[The graph of the partial sum of just the first three non-zero terms is displayed here. The convergence is quite rapid, except near the non-differentiable points at all integer values of x:]
![[graph of f(x) and its Fourier series partial sum]](ff06/q5graph2.gif)
For the vector field
,
where
,
Cartesian method:
First, note that
![]()
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Also note that
![]()
and, by symmetry,
![]()
By the chain rule,
![]()
and, by symmetry,
![]()
![curl F = [determinant] = vector 0](ff06/q6a7.gif)
OR
Spherical Polar Method:
F is a purely radial vector field:
![]()
The scale factors in spherical polar coordinates are:
![]()

Therefore
![]()
Note that any spherically symmetric vector field,
(that is, a vector field whose magnitude depends only
on the distance from the origin and whose direction
everywhere is directly towards or directly away from the
origin only), is necessarily irrotational:
![]()

Cartesian method:
By the results in part (a), together with the product rule
of differentiation,

and, by symmetry,


OR
Spherical Polar Method:
For the general vector field
![]()

For the vector field in this question, we have

Therefore
![]()
[Note that the inverse square law central force
has zero divergence and is therefore
free of sources and sinks everywhere (except
possibly at the origin).]