The Speed Formula: The fundamental calculation used in this investigation is the average speed formula: where is the total distance traveled and is the mean time taken.
Wave Equation Connection: While this experiment often uses a single pulse, the speed is also governed by the wave equation , where is frequency and is wavelength.
Depth-Speed Relationship: In shallow water, wave speed is dependent on depth; as depth increases, the speed of the wave also increases, though the relationship is non-linear.
| Feature | Single Pulse Method | Continuous Wave Method |
|---|---|---|
| Measurement | Distance / Time | Frequency Wavelength |
| Equipment | Tray and Stopwatch | Ripple Tank and Stroboscope |
| Focus | Mean speed over distance | Instantaneous wave properties |
| Application | Shallow water depth studies | General wave behavior studies |
Distance vs. Displacement: In this experiment, we measure the total distance the wave travels (including reflections) rather than the displacement from the start point.
Linear vs. Non-linear: It is critical to distinguish that while speed increases with depth, doubling the depth does not necessarily double the speed.
Accuracy in Timing: Always time multiple reflections (e.g., 3 lengths) rather than just one; this increases the total time measured and significantly reduces the percentage uncertainty caused by human reaction time.
Unit Consistency: Ensure that if the tray length is in cm and time is in seconds, the speed is recorded as . If the exam asks for SI units, convert the final answer to .
Graphing Skills: When plotting results, depth should be on the x-axis and speed on the y-axis. Expect a curve of best fit rather than a straight line, as the relationship is non-linear.
Parallax Error: When measuring water depth or tray length, ensure your eyes are level with the ruler markings to avoid measurement inaccuracies.
Counting Reflections: A common error is miscounting the number of lengths traveled; for example, if a wave travels to the end and back, it has traveled 2 lengths, not 1.
Reaction Time: Students often underestimate the impact of reaction time on short intervals; this is why measuring multiple lengths is a mandatory procedural step.
Surface Leveling: If the surface is not perfectly flat, the water depth will vary across the tray, leading to inconsistent wave speeds and unreliable data.