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Laplace, Fourier and PDEs (PDE): free practice, theory and problems
The Laplace transform turns a function of time, , into a function of a complex variable : . The key point is that it turns differential equations into algebraic equations – instead of differentiating and integrating in the time domain, you multiply and divide in the -domain. This is the very tool engineers use to analyze circuits, mechanical systems and control systems without solving the differential equation directly.
Contents
1. The Laplace transform
What is it about?
The Laplace transform turns a function of time, , into a function of a complex variable : . The key point is that it turns differential equations into algebraic equations – instead of differentiating and integrating in the time domain, you multiply and divide in the -domain. This is the very tool engineers use to analyze circuits, mechanical systems and control systems without solving the differential equation directly.
Key concepts and formulas
- Linearity: .
- Derivatives: , .
- Standard transforms: , , , , .
- s-shift: .
- t-shift (second shifting theorem): , where is the unit step function.
- Convolution theorem: , where .
- Initial and final value theorems: , and (if the limit exists).
- Dirac impulse: .
How to solve the problems
- Transform the whole differential equation term by term, using the derivative rules together with the initial conditions.
- Solve the resulting algebraic equation for .
- Split with partial fractions into simple terms you recognize from the table.
- Transform back term by term to get .
- Check the answer: does match the initial condition?
Example
Solve , , .
- Transform: .
- Solve for : , so .
- We recognize this as the transform of : .
- Check: . Correct.
Common mistakes
- Forgetting the initial conditions when using or .
- Mixing up s-shift () with t-shift () – they give completely different results.
- Sign or factor errors in the partial fraction expansion.
- Assuming the final value theorem holds even when the system is unstable (poles with positive real part, or more than one pole at the origin).
Concepts in this part
2. Fourier series
What is it about?
Any reasonable periodic function can be written as a sum of sine and cosine terms of different frequencies – a Fourier series. This is powerful because linear systems (circuits, mechanical oscillators) respond simply to each individual sine wave, so you can analyze the response to a complicated periodic signal term by term. Fourier series are the foundation of signal processing, acoustics, and solving partial differential equations with periodic or bounded boundary conditions.
Key concepts and formulas
- For a -periodic function: .
- Coefficients: , .
- Even function: only cosine terms (). Odd function: only sine terms ().
- Half-range series on : extend as odd (only , a sine series) or as even (only , a cosine series), depending on which boundary conditions you need.
- Fundamental angular frequency: .
- Parseval's identity: – the energy of the signal is the sum of the energy in each term.
Convergence (Dirichlet's theorem): the series converges to where is continuous, and to the average of the left- and right-hand limits at a jump discontinuity. Gibbs phenomenon: an overshoot of about 9% near a jump, which does not disappear even with more terms.
How to solve the problems
- Check symmetry first: is even, odd, or neither? This decides whether you can skip or .
- Compute , and with the integral formulas (use integration by parts where is a polynomial times sine/cosine).
- Assemble the series, or use a known standard result (square wave, sawtooth, triangle wave) if the problem asks for it.
- For half-range series: decide whether the problem needs a sine or a cosine expansion based on the boundary conditions.
- Use Parseval's identity to compute power/energy without summing the whole series explicitly.
Example
A sawtooth wave has on , periodic with period . Find .
- is odd, so for all , and we only need .
- The standard result for this function is .
- .
Common mistakes
- Forgetting to check symmetry, and computing for an odd function (it comes out zero, but it is wasted work – and easy to get wrong).
- Confusing -periodic with -periodic in the formulas for and .
- Believing the Gibbs overshoot disappears with more terms – it moves closer to the jump, but does not shrink.
- Using the wrong symmetry (odd instead of even) for a half-range expansion.
Concepts in this part
3. Partial differential equations
What is it about?
Partial differential equations (PDEs) describe quantities that vary both in space and time – temperature in a rod, displacement of a string, potential in a region. The three classic examples are the heat equation (diffusion), the wave equation (propagating oscillations) and Laplace's equation (steady states). Separation of variables breaks a PDE into simpler ordinary differential equations, and Fourier series glue the solutions together so the boundary and initial conditions are satisfied.
Key concepts and formulas
- Heat equation: (parabolic). Wave equation: (hyperbolic). Laplace's equation: (elliptic).
- General classification: for the PDE is elliptic if , parabolic if , and hyperbolic if .
- Separation of variables: assume . Substituting into the PDE gives two coupled ordinary differential equations with a separation constant .
- Eigenvalue problem with Dirichlet boundary : eigenvalues , eigenfunctions ,
- Eigenvalue problem with Neumann boundary (insulated ends) : eigenfunctions , (including the trivial constant solution ).
- Heat equation solution: – each mode dies out, higher modes fastest.
- D'Alembert's solution of the wave equation: , two waves that travel their own way without changing shape.
How to solve the problems
- Identify the type of equation (heat/wave/Laplace) and the boundary conditions (Dirichlet: value given; Neumann: derivative given).
- Set , substitute into the PDE, and separate so that one side depends only on and the other only on .
- Solve the eigenvalue problem for with the boundary conditions – this gives the allowed and eigenfunctions.
- Solve the equation for with the same .
- Sum up the modes with coefficients determined by the initial condition (often via a Fourier series).
Example
A string of length and wave speed has an initial shape that is a pure mode : , with zero initial velocity. Find .
- With only mode 1 present, the solution is , where .
- At : .
- At : , and .
- .
Common mistakes
- Using Dirichlet eigenfunctions (sine) when the boundary condition is actually Neumann (insulated end, cosine).
- Forgetting that the general solution of the wave equation has two arbitrary functions (a forward and a backward wave), not one.
- Mixing up the sign of the separation constant – the wrong sign gives growing solutions instead of decaying or oscillating ones.
- Believing Laplace's equation has a time-dependent solution – it describes a steady state.
Concepts in this part
Example problems with solutions
Here are some of the problems in laplace, Fourier and PDEs. In the app, calculation problems get new numbers every time, so you can practise until it sticks – and take a graded practice exam before the real one.
The Laplace transform:
Answer:
for .
Fourier series: An odd function has a Fourier series with only …
Answer: sine terms
is odd and is even. Hence .
Partial differential equations: Which equation is the heat equation (in one dimension)?
Answer:
It is first order in time and describes diffusion.
The Laplace transform:
Answer:
In general .
Matches these university courses
The content covers the syllabus found in engineering degrees, for example:
- DAVE3705 (OsloMet)
- TMA4130 (NTNU)