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Physics · Ch 4 — Motion in a Plane

Uniform Circular Motion

4.10

Uniform Circular Motion

Uniform Circular Motion

When an object moves along a circular path at a constant speed, we call this uniform circular motion. The word "uniform" here refers strictly to the speed — the magnitude of the velocity does not change. However, because the direction of the velocity is continuously changing as the object goes around the circle, the object is always accelerating. This is a crucial point: a change in velocity (even without a change in speed) means there is acceleration.

Consider an object moving with constant speed vv in a circle of radius RR. At any instant, its velocity vector is tangent to the circle at that point. Since the direction of this tangent changes from point to point, the velocity is not constant. Our task is to find both the magnitude and the direction of the resulting acceleration.

Direction of Acceleration

Let the object be at point PP at time tt, with position vector r\mathbf{r}, and at point P′P' at time t′t', with position vector r′\mathbf{r}'. The corresponding velocities are v\mathbf{v} (tangent at PP) and v′\mathbf{v}' (tangent at P′P'). The change in velocity, Δv=v′−v\Delta \mathbf{v} = \mathbf{v}' - \mathbf{v}, is found using the triangle law of vector addition.

Because the path is circular, v\mathbf{v} is perpendicular to r\mathbf{r}, and v′\mathbf{v}' is perpendicular to r′\mathbf{r}'. This geometric fact leads to a key result: Δv\Delta \mathbf{v} is perpendicular to Δr\Delta \mathbf{r} (where Δr=r′−r\Delta \mathbf{r} = \mathbf{r}' - \mathbf{r}). Since average acceleration is aˉ=Δv/Δt\bar{\mathbf{a}} = \Delta \mathbf{v} / \Delta t, the average acceleration is also perpendicular to Δr\Delta \mathbf{r}.

If we examine the geometry for a very small time interval (as Δt→0\Delta t \to 0), Δr\Delta \mathbf{r} becomes perpendicular to r\mathbf{r} itself. In that limit, Δv\Delta \mathbf{v} becomes perpendicular to v\mathbf{v}, and therefore points directly toward the centre of the circle. This is the instantaneous acceleration. Thus, the acceleration of an object in uniform circular motion is always directed towards the centre of the circle. This is called centripetal acceleration (from the Greek for "centre-seeking").

Important

The acceleration in uniform circular motion is always directed towards the centre of the circle. It is never tangential.

Magnitude of Centripetal Acceleration

Let the angle between the position vectors r\mathbf{r} and r′\mathbf{r}' be Δθ\Delta \theta. Because the velocity vectors are always perpendicular to the position vectors, the angle between v\mathbf{v} and v′\mathbf{v}' is also Δθ\Delta \theta.

Now, consider the triangle formed by the position vectors CPP′C P P' (with sides RR, RR, and ∣Δr∣|\Delta \mathbf{r}|) and the triangle formed by the velocity vectors v\mathbf{v}, v′\mathbf{v}', and Δv\Delta \mathbf{v} (with sides vv, vv, and ∣Δv∣|\Delta \mathbf{v}|). These two triangles are similar (both are isosceles with the same vertex angle Δθ\Delta \theta).

From similarity, the ratio of the base to the equal side is the same for both triangles:

∣Δv∣v=∣Δr∣R\frac{|\Delta \mathbf{v}|}{v} = \frac{|\Delta \mathbf{r}|}{R}

Rearranging:

∣Δv∣=vR ∣Δr∣|\Delta \mathbf{v}| = \frac{v}{R} \, |\Delta \mathbf{r}|

The magnitude of the instantaneous acceleration aa is:

a=lim⁡Δt→0∣Δv∣Δt=lim⁡Δt→0vR∣Δr∣Δta = \lim_{\Delta t \to 0} \frac{|\Delta \mathbf{v}|}{\Delta t} = \lim_{\Delta t \to 0} \frac{v}{R} \frac{|\Delta \mathbf{r}|}{\Delta t}

For small Δt\Delta t, the arc length PP′PP' is approximately equal to the chord length ∣Δr∣|\Delta \mathbf{r}|. The arc length is vΔtv \Delta t, so:

∣Δr∣≈vΔt|\Delta \mathbf{r}| \approx v \Delta t

Therefore:

lim⁡Δt→0∣Δr∣Δt=v\lim_{\Delta t \to 0} \frac{|\Delta \mathbf{r}|}{\Delta t} = v

Substituting this into the expression for acceleration gives:

ac=vR⋅v=v2Ra_c = \frac{v}{R} \cdot v = \frac{v^2}{R}

ac=v2Ra_c = \frac{v^2}{R}

This is the magnitude of the centripetal acceleration. It depends only on the speed vv and the radius RR of the circle. Since vv and RR are constant in uniform circular motion, the magnitude of the acceleration is also constant. However, because its direction is always changing (always pointing towards the centre), the acceleration vector itself is not constant.

Watch out

A constant magnitude does not mean a constant vector. The centripetal acceleration vector changes direction continuously, so it is a variable vector.

Angular Speed

There is another useful way to describe uniform circular motion. As the object moves from PP to P′P' in time Δt\Delta t, the line from the centre CC to the object turns through an angle Δθ\Delta \theta. This angle is called the angular displacement. We define the angular speed ω\omega (Greek letter omega) as the rate of change of angular displacement:

ω=ΔθΔt\omega = \frac{\Delta \theta}{\Delta t}

If the distance travelled along the arc during Δt\Delta t is Δs\Delta s, then the linear speed is v=Δs/Δtv = \Delta s / \Delta t. But Δs=RΔθ\Delta s = R \Delta \theta, so:

v=RΔθΔt=Rωv = \frac{R \Delta \theta}{\Delta t} = R \omega

v=Rωv = R \omega

This gives a direct relationship between linear speed and angular speed.

We can now express centripetal acceleration in terms of ω\omega:

ac=v2R=(Rω)2R=Rω2a_c = \frac{v^2}{R} = \frac{(R \omega)^2}{R} = R \omega^2

ac=ω2Ra_c = \omega^2 R

Time Period and Frequency

The time period TT is the time taken to complete one full revolution. The frequency ν\nu (nu) is the number of revolutions per second. They are related by ν=1/T\nu = 1/T.

In one revolution, the object travels a distance equal to the circumference of the circle, 2πR2\pi R. Therefore:

v=2πRT=2πRνv = \frac{2\pi R}{T} = 2\pi R \nu

Using v=Rωv = R \omega, we also get:

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

And for centripetal acceleration:

ac=v2R=(2πRν)2R=4π2ν2Ra_c = \frac{v^2}{R} = \frac{(2\pi R \nu)^2}{R} = 4\pi^2 \nu^2 R …

Figure 3.18Velocity and acceleration in uniform circular motion; Δt decreases (a)→(c); acceleration toward the centre.
Fig. 3.18 — Velocity and acceleration in uniform circular motion; Δt decreases (a)→(c); acceleration toward the centre.

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

The figure is a three-panel sequence that builds the idea of centripetal acceleration from scratch. In panel (a), you see a circle with centre C. Two position vectors, r\mathbf{r} and r′\mathbf{r}', are drawn from C to two nearby points P and P' on the circle. The angle between them is Δθ\Delta\theta, and the chord joining P to P' is labelled Δr\Delta r. At each point, the velocity vectors v\mathbf{v} and v′\mathbf{v}' are drawn tangent to the circle — they have the same magnitude vv but different directions. Off to the side, a separate velocity triangle shows these two vectors placed tail-to-tail; the vector from the tip of v\mathbf{v} to the tip of v′\mathbf{v}' is Δv\Delta\mathbf{v}, the change in velocity over the short time Δt\Delta t.

Panel (b) repeats the same idea but with a smaller Δθ\Delta\theta — the points are closer together, the chord Δr\Delta r is shorter, and the velocity triangle is narrower. The key visual point is that as Δθ\Delta\theta shrinks, Δv\Delta\mathbf{v} points more and more nearly toward the centre C.

Panel (c) is the limit Δt→0\Delta t \to 0. The chord Δr\Delta r becomes the instantaneous tangent velocity v\mathbf{v} at P, and the acceleration a=lim⁡Δt→0Δv/Δt\mathbf{a} = \lim_{\Delta t\to 0} \Delta\mathbf{v}/\Delta t is drawn as an arrow from P directly toward C. The velocity remains tangent to the circle; the acceleration points radially inward.

Important

The central lesson of the figure is that in uniform circular motion, the acceleration is always directed toward the centre, even though the speed never changes. The velocity changes only in direction, not magnitude, and that directional change requires an inward (centripetal) acceleration.

The textbook uses this geometric reasoning to derive the magnitude of centripetal acceleration. From the velocity triangle, when Δθ\Delta\theta is small, the chord length ∣Δv∣≈v Δθ|\Delta\mathbf{v}| \approx v\,\Delta\theta. Since the particle moves through an arc length v Δt=r Δθv\,\Delta t = r\,\Delta\theta, we have Δθ=v Δt/r\Delta\theta = v\,\Delta t / r. Substituting:

∣Δv∣≈v⋅v Δtr=v2r Δt|\Delta\mathbf{v}| \approx v \cdot \frac{v\,\Delta t}{r} = \frac{v^2}{r}\,\Delta t

Dividing by Δt\Delta t and taking the limit gives the instantaneous acceleration:

a=v2ra = \frac{v^2}{r}

where vv is the constant speed of the particle and rr is the radius of the circular path. The direction of a\mathbf{a} is toward the centre, perpendicular to v\mathbf{v}. …