Introduction to Wave Propagation
Waves are one of the most beautiful and fundamental phenomena in physics. From the ripples on a quiet pond to the light traveling across the vastness of space, waves carry energy and information from one place to another without transferring matter.
In this problem, we dive deep into the kinematics of a plane progressive wave. We are tasked with finding two key quantities: the phase difference and the amplitude difference between two points separated by a distance of 6 m along the line of propagation.
Let's break down the physics step-by-step and see how beautifully the math aligns with physical reality.
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Step 1
Finding the Spatial Period (Wavelength)
Before we can talk about phase differences, we need to understand the spatial scale of our wave. Just as a wave has a temporal period T (the time it takes for one complete oscillation at a single point), it also has a spatial period λ, known as the wavelength.
The wavelength is the distance over which the wave's shape repeats itself in space. We are given:
- Frequency of the wave, f=25 Hz
- Velocity of the wave, v=300 m/s
These quantities are bound together by the fundamental wave speed equation:
Rearranging this equation to solve for the wavelength λ, we get:
Substituting the given values:
This tells us that one complete cycle of our wave spans exactly 12 m in space.
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Step 2
Calculating the Phase Difference
Now, let's think about phase. Phase represents the position of a point in time or space on a wave cycle. A full cycle corresponds to a phase of 2π radians (or 360∘).
If a full cycle of 12 m corresponds to a phase change of 2π radians, then any spatial separation Δx (path difference) will correspond to a proportional phase difference Δϕ:
We are interested in two points separated by Δx=6 m. Let's substitute our values:
# Physical Interpretation of π Phase Difference
A phase difference of π radians (or 180∘) has a profound physical meaning. It means the two points are in opposite phase (completely out of phase).
When the particle at the first point is at its maximum positive displacement (a crest), the particle at the second point is at its maximum negative displacement (a trough). They are moving in opposite directions at any given instant, perfectly mirroring each other's motion across the equilibrium line.
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Step 3
Analyzing the Amplitude Difference
The second part of the question asks for the amplitude difference between these two points.
To answer this, we must look closely at the type of wave described: a plane progressive wave propagating in a non-absorbing medium.
In a plane wave, the wavefronts are parallel planes. Unlike spherical waves (where energy spreads out over an increasing spherical surface area), the energy of a plane wave remains confined to a constant cross-sectional area as it propagates.
Because there is no spreading of energy and we assume no absorption by the medium, the energy density—and consequently, the amplitude of the wave—remains absolutely constant at all points along the direction of propagation.
Therefore:
The amplitude difference ΔA is:
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Summary of Results
- Phase Difference: π radians
- Amplitude Difference: 0 m
This elegant result highlights the clean, symmetric nature of plane waves in ideal media. It serves as a foundational building block for understanding wave interference, standing waves, and diffraction!