Video summary
Time Scaling of Continuous-Time Signals
Main summary
Key takeaways
Main ideas / concepts
- The lecture explains time scaling of continuous-time signals (with amplitude scaling saved for the next lecture).
- Time scaling definition: Compressing or expanding a signal along the time axis is called time scaling.
Notation
- Original signal: (X(t))
- Time-scaled signal: (Y(t))
Core rule used
- In time scaling, the time variable (t) is multiplied by a constant (\alpha) (where (\alpha \neq 0)).
- Conceptually: [ Y(t) = X(\alpha t) ]
Two cases
Depending on (|\alpha|):
- Time compression when (|\alpha| > 1)
- Time expansion when (|\alpha| < 1)
Method / procedure (time scaling)
General understanding (what changes)
- Amplitude stays the same during time scaling (as shown in the examples).
- Time locations change: the signal appears over a different interval on the time axis.
Step-by-step construction
Given (X(t)) and scaling factor (\alpha) ((\alpha \neq 0)):
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Step 1: Keep the amplitude the same
- Use the same output amplitude values as in (X(t)).
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Step 2: Transform the time boundaries
- If the original waveform is defined over a time interval (e.g., (0 \le t \le 2)),
- then in the scaled signal you divide the original time boundaries by (\alpha).
- Equivalently, since (Y(t)=X(\alpha t)), the “active” time interval scales by (1/\alpha).
Detailed example outcomes from the lecture
Case 1: Compression ((|\alpha| > 1))
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Original signal: [ X(t) = 2 \quad \text{for } 0 \le t \le 2,\ \text{otherwise } 0 ]
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Choose (\alpha = 2)
- Consider the scaled argument (X(2t)) and where it equals 2:
- Original “on” region: (0 \le t \le 2)
- Scaled region: (0 \le t \le 1) (since the time boundary is effectively divided by 2)
Result: The waveform is compressed in time (it occupies a shorter time interval). Amplitude remains (2).
Shortcut idea: If (X(t)=2) over (0 \le t \le 2), then (X(\alpha t)) with (\alpha=2) makes the “2” region become (0 \le t \le 1).
Case 2: Expansion ((|\alpha| < 1))
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Use the same original signal: [ X(t) = 2 \quad \text{for } 0 \le t \le 2,\ \text{otherwise } 0 ]
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Choose (\alpha = 0.5)
- Compute the scaled “on” region:
- New interval becomes (0 \le t \le 4) (since (2/0.5 = 4))
Result: The waveform is expanded in time (it occupies a longer time interval). Amplitude remains (2).
Shortcut idea: Divide the original time boundary by (\alpha): (2 / 0.5 = 4), so the region stretches to (t=4).
Speaker / sources featured
- No named speakers or external sources are mentioned.
- The content is presented by an instructor/lecturer speaking directly.