Laplace Transform
Problem
Find L{e^(2t) sin(3t)}. Use the shifting theorem and the standard transform of sin(bt). Show the s-domain representation on a pole-zero diagram.
Explanation
What is the Laplace transform?
The Laplace transform maps a function of time (defined for ) to a function of a complex variable via the integral valid for all with real part large enough that the integral converges (the region of convergence, ROC).
Why this transform is so useful for ODEs: it converts differentiation in time into multiplication by in the transformed domain, i.e. which turns differential equations into algebraic equations. Solve the algebra, then invert the transform (see #190) to recover .
Laplace also handles discontinuous and impulsive forcing cleanly (step functions, delta functions — #191, #192), which is why it's the standard tool in control theory and electrical engineering.
A handful of standard transforms (memorize)
- (integer )
- (ROC: )
Two key theorems we'll use today
1. First shifting theorem (s-shift / frequency shift). where . In words: multiplying by in the time domain shifts the Laplace variable by in the -domain.
2. Derivative theorem.
These bring initial conditions into the algebra automatically, unlike the you'd chase in the time domain.
The given problem
Find .
This is a textbook application of the shifting theorem with and .
Step-by-step
Step 1 — Transform of .
Step 2 — Apply the shift .
Step 3 — (Optional) expand the denominator.
Region of convergence: (shifted from the original ).
Verification by direct integration (optional)
The integral (a standard result). With , :
Pole-zero structure
has:
- No finite zeros in this transform.
- Poles where the denominator vanishes: . Two complex conjugate poles.
Pole location tells you a lot about the time-domain function:
- Pole at : real part means the time-domain function grows like ; imaginary part gives oscillation frequency .
Reading pole locations directly:
- Left half-plane → decaying
- Right half-plane → growing
- Imaginary axis → pure oscillation
- Real axis → non-oscillating (decay or growth)
- Imaginary part → oscillation frequency
- Distance from imaginary axis → damping rate
Linearity of the Laplace transform
Combined with the small table above, linearity covers an enormous range of practical transforms. Example: .
Other useful properties (for reference)
- Time shift: (see #192 for , the Heaviside step).
- Multiplication by : .
- Convolution: (see #193).
- Periodic function of period : .
Common mistakes
- Missing the in the numerator of . It's , not .
- Forgetting and in the derivative theorem. These "fall out" of the integration-by-parts proof and are what let Laplace naturally handle initial conditions.
- Wrong direction of the shift. Time-domain multiplication by gives (shift right by ), not .
- Treating the ROC casually. only for . Outside the ROC, the integral diverges.
Try it in the visualization
Place a pole pair on the complex -plane and watch the corresponding time-domain waveform emerge (decaying / growing / oscillating). Drag the pole's real part across the imaginary axis to see decay flip into growth; drag the imaginary part to change the oscillation frequency.
Interactive Visualization
Parameters
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