Q.A cyclist starts from the centre O of a circular park of radius 1km and rides along the path O→P→R→Q→O. Here P is a point on the boundary circle reached by riding straight out along a radius (due east of O); the cyclist then rides along the circular boundary from P to R (R lies on the circle midway, in the north-east direction) and on to Q (the point on the circle due north of O); finally the cyclist returns straight along the radius QO back to the centre. Throughout the ride the speed is a constant 10ms−1. Find the magnitude and direction of the cyclist's acceleration at point R.
Uniform circular motion is motion along a circular path at constant speed. Although the speed stays the same, the velocity does not — its direction keeps changing at every instant — so the motion has an acceleration even though the speed never changes. This concept covers the kinematics of that motion; the force that causes it (centripetal force) belongs to the Laws of Motion unit.
1. Angular Quantities
As the body sweeps through an angle θ, its angular velocity is
ω=dtdθ
For one full revolution in a period T, at frequency f:
ω=T2π=2πf,T=f1
To convert rpm to rad/s:
ω=602π⋅(rpm)=30π(rpm)
The linear (rim) speed v and the angular speed ω are related by
v=ωr
2. Centripetal Acceleration
Even though the speed is constant, the velocity vector keeps turning — this produces an acceleration directed toward the centre of the circle:
ac=rv2=ω2r=T24π2r=4π2f2r
Use whichever form matches the data you are given. This acceleration is often expressed as a multiple of g (as ac/g, taking g=10m/s2).
3. Directions
The velocity is always tangential (along the direction of motion); the acceleration is centripetal — radial, pointing inward, and perpendicular to the velocity.
Because the direction of the velocity keeps changing, the change in the velocity vector over an angle Δθ has magnitude
∣Δv∣=2vsin(2Δθ)
So a quarter turn gives ∣Δv∣=v2, a half turn gives 2v, and a full turn gives 0.
The average acceleration over an arc is ∣Δv∣/Δt — this is smaller in magnitude than the instantaneous centripetal acceleration v2/r, and its direction lies along the perpendicular bisector of the chord joining the two points (which, for a circle, always passes through the centre) rather than being radially inward from either endpoint's own position.
4. Points on a Rotating Body
Every point on a rigid rotating body (a wheel, a disc, a clock hand, the Earth) shares the same ω, but the rim speed v=ωr grows with the radius.
Clock hands: the second hand turns at ω=602π rad/s, the minute hand at 36002π rad/s, the hour hand at 432002π rad/s.
The Earth spins with ω=864002π≈7.3×10−5 rad/s. A point on the equator moves at ωR≈465 m/s, and a point at latitude λ moves at ωRcosλ (since the circle of latitude has radius Rcosλ).
5. Connected Systems
Wheels joined by a belt (or two gears in mesh) share the same rim speed, so ω1r1=ω2r2 — the larger wheel turns with the smaller ω.
Wheels on the same axle (concentric) share the same ω, so the outer rim moves faster (v∝r).
6. Non-Uniform Circular Motion
If the speed also changes, there is a tangential acceleration
at=dtdv=rα
(from the angular acceleration α=dω/dt), in addition to the radial ac=v2/r. These two are perpendicular, so the total acceleration is
At R the cyclist is moving along the circular boundary at constant speed, so the acceleration is purely centripetal: a=v2/r=(10)2/1000=0.1ms−2, directed from R toward the centre O (along RO). …
At R the cyclist is on the circular part of the path moving at constant speed, so there is no tangential acceleration — only centripetal acceleration toward the centre. Its magnitude is a=v2/r=0.1ms−2 and it points along RO (from R to O).
Concept
Acceleration has two parts: a tangential part at=dv/dt that changes the speed, and a centripetal part ac=v2/r that changes the direction and always points toward the centre of the circular path.
Steps
The speed is constant (10ms−1) everywhere, so at=dv/dt=0.
Point R lies on the circular boundary (radius r=1km=1000m), so the motion there is along a circle and the centripetal term is present:
a=ac=rv2=1000m(10ms−1)2=1000100=0.1ms−2. …
Concept: Differentiate the Cyclist's Position Vector Twice Along the Arc, Then Evaluate at θ=45∘
Method: Explicit Rotating-Position-Vector Derivation, Not the "No Tangential + v2/r" Recipe
Rather than simply stating "constant speed on a circle means only centripetal acceleration, a=v2/r," this method builds the cyclist's position on the arc as an explicit function of the angle swept from P, differentiates it twice with respect to time, and reads the direction of acceleration at R directly off the resulting vector formula.
Step 1 -- Set up the position vector along the arc P→R→Q
Put the centre O at the origin, with P due east of O (angle 0∘ from the x-axis) and Q due north of O (angle 90∘). As the cyclist rides the arc from P through R to Q, their angular position sweeps θ from 0∘ to 90∘. With radius r=1000m:
ρ(θ)=rcosθi^+rsinθj^
Since R is described as midway (north-east) between P and Q on the arc, it corresponds to θ=45∘.
Step 2 -- Convert to a function of time using θ=ωt (constant ω, since speed is constant)
On the circular part of the path, constant speed v=10m s−1 on radius r means constant angular speed ω=v/r. So θ(t)=ωt, and:
ρ(t)=rcos(ωt)i^+rsin(ωt)j^
Step 3 -- Differentiate once (velocity), confirming the speed matches the given value
v(t)=−rωsin(ωt)i^+rωcos(ωt)j^,∣v∣=rω=v=10m s−1✓
Step 4 -- Differentiate again (acceleration) -- this is where the direction comes from automatically
The bracket is exactly ρ(t) from Step 1 -- so the acceleration is automatically a negative multiple of the position vector (measured from the centre O), for every point on the arc, without needing to separately argue "it must point toward the centre."