The Wave Equation: The fundamental relationship governing wave motion is , where is velocity, is frequency, and is wavelength. This equation implies that for a constant speed, frequency and wavelength are inversely proportional.
Principle of Superposition: When two or more waves overlap in the same medium, the resulting displacement at any point is the vector sum of the individual displacements of the waves. This principle is the logical foundation for all interference phenomena.
Frequency Invariance: When a wave transitions between different media, its frequency remains constant because it is determined by the source. Consequently, any change in wave speed must result in a proportional change in wavelength.
The Frequency Rule: Always remember that frequency is a property of the source. If a question asks what happens to frequency when light enters water, the answer is almost always 'it remains unchanged'.
Unit Consistency: Wavelengths are often given in nanometers () or micrometers (). Convert all values to standard SI units (meters) before using them in the wave equation .
Sanity Check: In refraction, if a wave slows down (e.g., light entering glass), the wavelength must decrease. If your calculation shows an increase, re-check your algebraic ratios.
Diffraction Limits: Significant diffraction only occurs when the size of the opening or obstacle is comparable to or smaller than the wavelength. If the gap is much larger than , the wave travels through relatively undisturbed.
Phase vs. Path Difference: Students often confuse the physical distance difference (path difference) with the phase angle difference. Remember that a path difference of corresponds to a phase difference of radians or .
Wavelength Measurement: Ensure you measure wavelength between identical points. Measuring from a crest to the very next trough provides only half a wavelength ().
Medium Density: Do not assume that 'denser' always means 'slower' for all wave types. While light slows down in optically denser media, sound actually travels faster in denser solids than in air.