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Spec mapping: OCR H556 Module 5.3 — Circular motion (centripetal acceleration a=v2/r=rω2; centripetal force F=mv2/r=mrω2 as the resultant inward force on a body in uniform circular motion; applications to horizontal and vertical circles, banked tracks, conical pendulums and orbital motion). Refer to the official OCR H556 specification document for exact wording.
In the previous lesson we discovered that an object moving in a circle at constant speed has a changing velocity, because the direction of motion is continuously turning. A changing velocity means an acceleration, and by Newton's second law (Module 3.2) an acceleration requires a net force. This lesson derives the famous formula for centripetal acceleration and applies it to real situations: cars on bends, buckets swung overhead, conical pendulums, planets in orbit, and the spinning samples in a medical centrifuge.
This is OCR A-Level Physics A Module 5.3 — the heart of circular motion, and the conceptual bridge to gravitational orbits (Module 5.4) and magnetic circular motion (Module 6.4). The single most important idea is this: the centripetal force is not a new force. It is whatever resultant inward force the existing real forces happen to add up to. The mistake of treating it as an extra force is by far the most common conceptual error at A-Level.
The word centripetal comes from the Latin centrum (centre) + petere (to seek). A centripetal force is any force that seeks the centre — it points from the moving object towards the centre of the circle it is travelling on.
Centripetal force is not a new kind of force. It is the net (resultant) inward force on the body, made up of the ordinary forces — gravity, tension, friction, normal contact, electrostatic, magnetic — that you already know about from Module 3.2. The job of a circular-motion problem is to identify which real forces have an inward component, and to set their inward resultant equal to mv2/r.
| Situation | Centripetal force provided by |
|---|---|
| Ball on a string swung in a horizontal circle | Tension in the string |
| Car rounding a flat bend | Friction between tyre and road |
| Earth orbiting the Sun | Gravitational attraction GMm/r2 |
| Electron in a (classical) Bohr orbit | Electrostatic Coulomb attraction ke2/r2 |
| Rider on a fairground "wall of death" | Normal contact force from the wall |
| Bob of a conical pendulum | Horizontal component of the string tension |
| Charged particle in a uniform magnetic field | Magnetic Lorentz force qvB (Module 6.4) |
| Bicycle on a banked velodrome | Inward component of normal contact and friction |
Exam Tip: When an OCR question asks "What provides the centripetal force?" the correct answer is the physical force — tension, friction, gravity, normal reaction, lift, magnetic. Writing "centripetal force" is never the answer and will score zero. Always name the origin of the inward pull.
Consider an object moving at constant speed v in a circle of radius r. In a short time Δt it sweeps through a small angle Δθ=ωΔt. Its velocity vector changes from v1 to v2, both of magnitude v, but pointing in slightly different directions (each is tangential to the circle at its own point).
The change in velocity, Δv=v2−v1, is what we need. Two equal-magnitude vectors with a small angle Δθ between them subtract to give a third vector of magnitude vΔθ (chord length on a circle of radius v in velocity space) pointing approximately radially inward — perpendicular to either velocity arrow, in the limit Δθ→0. This is exactly the small-angle isoceles-triangle geometry: two sides of length v, apex angle Δθ, base of length vΔθ for small Δθ.
∣Δv∣≈vΔθ
Dividing by Δt and taking the limit gives the magnitude of the acceleration:
a=limΔt→0Δt∣Δv∣=vdtdθ=vω
Substituting v=rω (from lesson 1) gives the two canonical forms used throughout the topic:
a=rv2=rω2
Both formulae give the same number; you choose whichever fits the data you are given. If the question hands you v and r, use a=v2/r; if it hands you ω and r (or rpm), use a=rω2.
Because Δv points towards the centre of the circle (in the limit), so does the acceleration. The centripetal acceleration is always radially inward, perpendicular to the instantaneous velocity. It has no tangential component — and that is why the speed remains constant even though the velocity is changing. Tangential acceleration would speed the body up or slow it down; perpendicular acceleration only rotates the velocity vector.
Applying Newton's second law F=ma to the centripetal acceleration gives the net inward force required to maintain the circular motion:
Fnet, inward=rmv2=mrω2
This is the resultant force required to keep a body of mass m moving at speed v (or angular velocity ω) on a circle of radius r. It acts towards the centre of the circle. It is not a separate force added to gravity, tension, friction etc. — it is what the inward components of those real forces must sum to. Get this conceptual point right and 90% of A-Level circular-motion mistakes evaporate.
Notice that centripetal force depends on the square of the speed. Doubling the speed quadruples the required force. This is why sharp bends become dangerous so quickly: a driver entering a corner at 60 mph instead of 30 mph needs four times as much friction — and friction has an absolute ceiling set by μsN, beyond which the tyres slide.
For any circular-motion problem at A-Level, run the same procedure:
This is a Newton-2 calculation — there is no "centripetal force" to add to the FBD; only mv2/r on the right-hand side of Fnet=ma. If your diagram has an "Fc" arrow in addition to gravity and tension, you have already gone wrong.
flowchart TD
A[Object in uniform circular motion] --> B[Draw FBD: list real forces only]
B --> C{Resolve each into radial + tangential}
C --> D[Sum inward components: F_net,in]
D --> E[Set F_net,in = mv²/r]
E --> F[Solve for unknown]
F --> G[Sanity-check: is the required force achievable? friction ≤ μN, tension ≤ breaking strength]
A 0.25 kg ball is swung in a horizontal circle of radius 0.80 m at a constant speed of 4.0 m s−1. Calculate (a) the centripetal acceleration and (b) the tension in the string.
(a) Using a=v2/r:
a=rv2=0.80(4.0)2=0.8016=20 m s−2
The acceleration is 20 m s−2 (≈2g) directed toward the centre of the circle at every instant.
(b) If the ball is moving in a horizontal circle on a frictionless smooth surface, the only horizontal force on the ball is the string tension, pulling inward toward the centre.
T=ma=0.25×20=5.0 N
So the string tension equals the required centripetal force: T=mv2/r=5.0 N. (For a ball swung in a conical pendulum the string is tilted upward and only the horizontal component of tension supplies the centripetal force — see Example 4 below.)
A car of mass 1200 kg drives round a flat (unbanked) bend of radius 45 m. The coefficient of static friction between the tyres and the road is μs=0.70. Calculate the maximum speed at which the car can round the bend without skidding. Take g=9.81 m s−2.
The centripetal force is supplied entirely by friction between the tyres and the road — there is nothing else with an inward horizontal component. The maximum static friction available is
Fmax=μsN=μsmg=0.70×1200×9.81=8240 N
Setting this equal to the required centripetal force at the limit:
rmv2v2vmax=μsmg=μsgr=0.70×9.81×45=309 m2 s−2=309=17.6 m s−1≈63 km h−1
Notice that the mass cancels — the maximum speed on a flat bend does not depend on how heavy the car is. Examiners like this result because it is counter-intuitive. An empty Mini and a fully laden lorry share the same skid-speed at a given μ and r. The same principle is why an HGV and a sports car spin out at similar speeds on the same icy corner.
Wet road sanity check. If rain drops μs from 0.7 to 0.3, vmax falls by a factor of 0.3/0.7≈0.65 — a 35% reduction in safe cornering speed. The squared dependence (v2∝μ) is the physical basis for "slow down in the wet" advice.
A bucket of water of total mass m is swung in a vertical circle of radius r=1.0 m. What is the minimum speed at the top of the circle for the water to stay in the bucket? Take g=9.81 m s−2.
At the top of the circle, both gravity (mg downward, toward the centre) and the normal contact force from the bottom of the bucket on the water (N, downward, also toward the centre) act radially inward. Newton 2 (radial direction, inward positive):
N+mg=rmv2
For the water to just stay in contact with the bucket — the borderline case — the contact force N=0. Then gravity alone supplies the centripetal force:
mgv2vmin=rmv2=gr=9.81×1.0=9.81 m2 s−2=3.13 m s−1
Swing any slower and gravity is more than the required centripetal force; the surplus accelerates the water out of the bucket and you get wet. Swing faster and the bucket-bottom has to push the water inward (positive N) to make up the additional centripetal requirement.
At the bottom of the same loop, gravity acts away from the centre (downward, but the centre is now above), while normal force acts toward the centre. Newton 2 gives N−mg=mv2/r, so N=mg+mv2/r>mg. The water experiences "apparent weight" greater than mg — a familiar sensation at the bottom of a roller-coaster loop, and an OCR favourite for follow-up questions.
A bob of mass m=0.20 kg hangs from a light string of length L=0.50 m and traces out a horizontal circle of radius r at constant speed. The string makes a constant angle θ=25° with the vertical. Find (a) the period of the motion and (b) the tension in the string.
Geometry: r=Lsinθ=0.50×sin25°=0.211 m.
The bob has two forces on it: tension T along the string (inward and upward) and weight mg vertically downward. Resolve into vertical (balanced) and horizontal (provides centripetal):
From the horizontal equation, ω2=Tsinθ/(mr)=2.17×sin25°/(0.20×0.211)=21.7 rad2 s−2, so ω=4.66 rad s−1 and Tperiod=2π/ω=1.35 s. Notice the string angle and the period are linked by a single condition — they cannot be set independently.
Important conceptual point: the tension itself is not "the centripetal force". Only its horizontal component Tsinθ is. The vertical component Tcosθ does no circular-motion work; it balances gravity. This is the inward-force audit in action.
A laboratory centrifuge rotates at 4500 rpm. A sample tube is 8.0 cm from the rotation axis. Find the centripetal acceleration experienced by the sample in units of g.
First convert rpm to rad s−1:
ω=4500×602π=471 rad s−1
Then
a=rω2=0.080×(471)2=0.080×2.22×105=1.78×104 m s−2
In units of g:
ga=9.811.78×104≈1810g
A typical medical centrifuge can generate thousands of g, which is why centrifugation separates blood cells from plasma so effectively. Plasma proteins, red blood cells, white blood cells and platelets have slightly different densities, and at ∼2000g they stratify into clean layers within minutes rather than the days it would take under Earth's 1g.
Ultracentrifuges used in biochemistry research routinely run at 50000–100000 rpm, generating up to 106g — enough to separate molecules by molecular weight.
A car of mass m rounds a curve of radius r=80 m on a road banked at angle θ to the horizontal. Find the angle θ at which the car can negotiate the bend at v=22 m s−1 (≈50 mph) with no friction required.
Forces on the car: weight mg down, normal contact N perpendicular to the road surface. Resolve into vertical and horizontal:
Dividing equation 2 by equation 1:
tanθ=grv2=9.81×80(22)2=785484=0.617⇒θ=31.7°
So at 32° banking, v=22 m s−1 is the natural speed: a frictionless car holds the curve without any sideways pull. Below that speed, friction must point up-slope to keep the car from sliding down; above it, friction must point down-slope. This is exactly the physics behind highway banking, racetrack design and velodrome geometry.
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