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Physics · Ch 14 — Waves

Period, Angular Frequency and Frequency

14.3.3

Period, Angular Frequency and Frequency

Displacement Relation in a Progressive Wave

A wave travelling through a medium carries energy and momentum, but what exactly do we mean by "the wave" at a given instant? The answer lies in the displacement of each particle of the medium from its equilibrium position. For a wave on a string, this displacement is the vertical distance a point on the string has moved from its rest position. The key is that this displacement depends on two things: which particle you look at (its position xx) and when you look at it (the time tt).

So the displacement yy is a function of both xx and tt, written as y(x,t)y(x,t). The specific form of this function determines the shape and behaviour of the wave. For the simplest and most important case — a progressive wave travelling along the positive xx-direction without changing shape — the displacement relation takes a particularly elegant form.

y(x,t)=f(x−vt)y(x,t) = f(x - vt)

Here vv is the constant speed of the wave. The function ff describes the shape of the wave at t=0t=0 (the initial profile). As time increases, the argument x−vtx - vt remains constant if xx increases at exactly the rate vv — meaning the entire waveform slides to the right without distortion. If the wave travels in the negative xx-direction, the relation becomes y(x,t)=f(x+vt)y(x,t) = f(x + vt).

For a wave that is sinusoidal — the most fundamental periodic wave — the function ff is a sine or cosine. A sinusoidal wave travelling along the positive xx-direction can be written as:

y(x,t)=asin⁡(kx−ωt+ϕ)y(x,t) = a \sin(kx - \omega t + \phi)

where:

  • aa is the amplitude — the maximum displacement from equilibrium.
  • kk is the angular wave number (or propagation constant).
  • ω\omega is the angular frequency.
  • ϕ\phi is the initial phase (phase constant).

The argument (kx−ωt+ϕ)(kx - \omega t + \phi) is called the phase of the wave. Two points on the wave that have the same phase (e.g., both at a crest) are separated by an integer number of wavelengths.


Period, Angular Frequency and Frequency

A sinusoidal wave is periodic in both space and time. The time period TT is the time taken for one complete cycle of oscillation at any fixed point in the medium. If you sit at a fixed xx, the displacement yy varies sinusoidally with time, repeating every TT seconds. The frequency ν\nu (often denoted ff in many texts) is the number of cycles per second:

ν=1T\nu = \frac{1}{T}

The angular frequency ω\omega is related to the frequency by:

ω=2πν=2πT\omega = 2\pi \nu = \frac{2\pi}{T}

Why use ω\omega? Because the sine function's argument must be in radians, and ω\omega directly gives the rate of change of phase with time. When time increases by TT, the phase increases by 2π2\pi radians, so:

ωT=2π\omega T = 2\pi

This is the fundamental link between angular frequency and period.

Important

The angular frequency ω\omega has units of radians per second (rad/s), while ordinary frequency ν\nu has units of hertz (Hz) or s−1^{-1}. They are related by ω=2πν\omega = 2\pi\nu.


Properties of Sinusoidal Waves

The textbook lists three key properties that follow directly from the displacement relation. Each one is derived step by step below.

›Proof

Property (I): For a fixed position xx, the displacement yy varies sinusoidally with time, with angular frequency ω\omega.

Fix x=x0x = x_0. Then the displacement becomes:

y(x0,t)=asin⁡(kx0−ωt+ϕ)y(x_0, t) = a \sin(kx_0 - \omega t + \phi)

This is a function of tt alone. Write the constant part as θ=kx0+ϕ\theta = kx_0 + \phi, so:

y(t)=asin⁡(θ−ωt)=−asin⁡(ωt−θ)y(t) = a \sin(\theta - \omega t) = -a \sin(\omega t - \theta)

The form sin⁡(ωt−θ)\sin(\omega t - \theta) is a standard sinusoidal oscillation with angular frequency ω\omega. The negative sign just represents a phase shift of π\pi (since −sin⁡u=sin⁡(u+π)-\sin u = \sin(u + \pi)), which does not change the frequency. Therefore, every particle in the medium executes simple harmonic motion with the same angular frequency ω\omega as the source.

›Proof

Property (II): At any fixed time tt, the shape of the wave is sinusoidal in xx, with wavelength λ\lambda related to kk by k=2π/λk = 2\pi/\lambda.

Fix t=t0t = t_0. Then:

y(x,t0)=asin⁡(kx−ωt0+ϕ)y(x, t_0) = a \sin(kx - \omega t_0 + \phi)

This is a function of xx alone. Write the constant as θ′=−ωt0+ϕ\theta' = -\omega t_0 + \phi, so:

y(x)=asin⁡(kx+θ′)y(x) = a \sin(kx + \theta')

This is a sine wave in xx with angular wave number kk. The wavelength λ\lambda is the spatial period — the distance over which the sine function completes one full cycle. For a sine wave, sin⁡(kx+θ′)\sin(kx + \theta') repeats when kxkx increases by 2π2\pi, i.e., when xx increases by λ\lambda such that kλ=2πk\lambda = 2\pi. Hence:

k=2πλk = \frac{2\pi}{\lambda}

The angular wave number kk has units of radians per metre (rad/m). …

Figure 14.7An element of a string at a fixed location oscillates in time with amplitude a and period T, as the wave passes over it.
Fig. 14.7 — An element of a string at a fixed location oscillates in time with amplitude a and period T, as the wave passes over it.

Drawn by us to help you understand the concept clearly, and verified to make sure it's accurate. For exams, practice from your NCERT textbook's own diagram.

The figure is a simple but essential plot: the vertical axis is displacement yy of a single point on the string, and the horizontal axis is time tt. The curve is a sine wave that repeats after a time interval labelled TT. A vertical double-headed arrow runs from the equilibrium line (y=0y=0) up to a crest, and its length is marked aa. A horizontal double-headed arrow spans exactly one complete cycle of the wave, from one crest to the next crest (or from any point to the identical point one cycle later), and its length is marked TT.

What this plot captures is the local behaviour of a wave. When a progressive wave travels along a string, every fixed point on the string oscillates up and down in simple harmonic motion. The figure shows that oscillation for one such point. The amplitude aa is the maximum displacement from the mean position — the distance the string element moves from equilibrium to its highest (or lowest) point. The period TT is the time it takes for that point to complete one full back-and-forth motion.

The key formula that emerges from this picture is the displacement of a point on the string as a function of time. For a wave travelling in the positive xx-direction, the textbook writes:

y(x,t)=asin⁡(ωt−kx+ϕ)y(x,t) = a \sin(\omega t - kx + \phi)

But for a fixed location xx, say x=0x=0, this reduces to:

y(0,t)=asin⁡(ωt+ϕ)y(0,t) = a \sin(\omega t + \phi)

which is exactly the simple harmonic motion shown in the figure. Here ω=2πT\omega = \frac{2\pi}{T} is the angular frequency, and ϕ\phi is the initial phase (which determines where on the sine wave the motion starts at t=0t=0). The figure itself typically shows ϕ=0\phi = 0 for simplicity, so the curve passes through the origin.

Important

The period TT and the angular frequency ω\omega are related by ω=2πT\omega = \frac{2\pi}{T}. The amplitude aa is the same for every point on the string (assuming no energy loss), but the phase ϕ\phi changes with position xx — that is what makes the wave progressive.

Watch out

Do not confuse the period TT shown here with the time period of the wave source. They are the same quantity. But also do not mix up TT (period) with TT used for tension in other parts of the chapter — the context makes the meaning clear. …