The Anatomy of a Wave
Imagine standing by a calm lake and tossing a pebble into the water. The ripples that travel outward are a perfect physical manifestation of a progressive wave. In physics, we describe this elegant motion using a mathematical equation that captures both space and time.
The general equation for a progressive wave travelling in the positive x-direction is given by:
Let's break down this beautiful equation. The variable y represents the displacement of a particle from its mean position. A is the amplitude, the maximum height the wave reaches. The term kx tells us how the wave varies in space, where k is the wave number. The term ωt tells us how the wave oscillates in time, where ω is the angular frequency.
But what about ϕ? This is the phase constant or initial phase. It is the crucial piece of information that tells us exactly where the wave cycle begins at x=0 and t=0. Finding this ϕ is the core objective of our problem.
Freezing Time
The Snapshot
The problem provides us with a "snapshot" of the wave at t=0. Think of this as taking a photograph of the lake exactly at the moment your stopwatch starts.
Mathematically, taking a snapshot at t=0 means we substitute t=0 into our wave equation.
This simplified equation now describes the shape of the wave frozen in space, exactly as shown in the provided graph.
The Origin Story
Boundary Conditions
To find the unknown phase constant ϕ, we need to act like detectives and look for clues in the graph. The most obvious clue is right at the origin, where x=0.
Looking at the graph, we can clearly see that the wave passes exactly through the origin. This means that at x=0, the displacement y is also 0. Let's plug this boundary condition into our snapshot equation:
Since the amplitude A is not zero (otherwise there would be no wave!), it must be that sin(ϕ)=0.
From our knowledge of trigonometry, we know that the sine function is zero at multiple angles. The two most common principal values are:
We have narrowed down the possibilities, but we are not done yet. We need a tie-breaker.
The Decisive Slope
Breaking the Tie
How do we choose between ϕ=0 and ϕ=π? The secret lies in the direction the wave is heading right after the origin.
Look closely at the graph just to the right of the y-axis (for small positive values of x). The wave curve dips downwards below the x-axis. This means that for a small x>0, the displacement y must be negative.
Let's test our two candidate values for ϕ to see which one produces this negative displacement.
Case 1: What if ϕ=0?
If we substitute ϕ=0 into our snapshot equation, we get:
y(x,0)=Asin(kx+0)=Asin(kx)
For a small positive x, the value of kx is a small positive angle in the first quadrant. The sine of a first-quadrant angle is positive. Therefore, y would be positive. This would mean the wave goes upwards from the origin. But our graph clearly shows it going downwards! So, ϕ=0 is incorrect.
Case 2: What if ϕ=π?
Let's substitute ϕ=π into our snapshot equation:
Using the trigonometric identity sin(θ+π)=−sin(θ), we can simplify this to:
Now, for a small positive x, sin(kx) is positive, but the negative sign in front makes the entire expression for y negative. This perfectly matches our visual observation of the wave dipping below the x-axis!
The Final Verdict
By carefully analyzing both the position of the wave at the origin and its initial slope, we have conclusively proven that the phase constant must be π.
This elegant interplay between the visual geometry of a graph and the rigorous algebra of trigonometric functions is what makes wave mechanics so deeply satisfying to study. The correct option is indeed (b).