Skip to content

Physics · Ch 3 — Motion in a Plane

Expression for Centripetal Acceleration

3.4.2

Expression for Centripetal Acceleration

To find the acceleration responsible for uniform circular motion, set up coordinates with the centre of the circular path at the origin O, and let the particle start (for convenience) at point P0P_0 on the positive x-axis. At a later instant tt, the particle has moved anticlockwise to point P, and its radius vector makes an angle θ=ωt\theta = \omega t with the x-axis (since dθdt=ω\dfrac{d\theta}{dt}=\omega, a constant). The x and y components of the radius vector are therefore rcos⁡θ=rcos⁡(ωt)r\cos\theta = r\cos(\omega t) and rsin⁡θ=rsin⁡(ωt)r\sin\theta = r\sin(\omega t), so r⃗=rcos⁡(ωt) i^+rsin⁡(ωt) j^\vec{r} = r\cos(\omega t)\,\hat{i} + r\sin(\omega t)\,\hat{j} (Eq. 3.50).

Differentiating the position vector with respect to time gives the instantaneous velocity, and differentiating the velocity gives the instantaneous acceleration — with rr and ω\omega both constant throughout: v⃗=dr⃗dt=−rωsin⁡(ωt) i^+rωcos⁡(ωt) j^\vec{v} = \dfrac{d\vec{r}}{dt} = -r\omega\sin(\omega t)\,\hat{i} + r\omega\cos(\omega t)\,\hat{j} (Eq. 3.51), and differentiating once more, a⃗=dv⃗dt=−rω2cos⁡(ωt) i^−rω2sin⁡(ωt) j^=−ω2r⃗\vec{a} = \dfrac{d\vec{v}}{dt} = -r\omega^2\cos(\omega t)\,\hat{i} - r\omega^2\sin(\omega t)\,\hat{j} = -\omega^2\vec{r} (Eq. 3.52). The minus sign shows the acceleration is opposite in direction to the radius vector r⃗\vec{r} — that is, it points from the particle straight back toward the centre — confirming this is exactly the centripetal acceleration described qualitatively in section 3.4. Its magnitude is a=ω2r=v2ra = \omega^2 r = \dfrac{v^2}{r} (Eq. 3.53), using v=ωrv=\omega r from section 3.4.1.

The force producing this acceleration is the centripetal force, F⃗=ma⃗=−mω2r⃗\vec{F} = m\vec{a} = -m\omega^2\vec{r} (Eq. 3.54), with magnitude F=mv2r=mω2rF = \dfrac{mv^2}{r} = m\omega^2 r (Eq. 3.55).

Conical pendulum. A conical pendulum is a mass mm (the bob) hung from a fixed point O by a string of length ll, but instead of swinging in a vertical plane like an ordinary simple pendulum, it revolves steadily so that it traces a horizontal circle, while the string itself sweeps out the surface of a cone of constant half-angle θ\theta (measured from the vertical) — hence the name. In the absence of friction, once started, such a system keeps revolving indefinitely at constant speed.

Only two forces act on the bob: its weight mgmg, straight down, and the string tension TT, directed along the string toward O. Resolving the tension into a vertical component Tcos⁡θT\cos\theta and a horizontal component Tsin⁡θT\sin\theta: for the bob to stay in its horizontal circle (no net vertical motion), the vertical component must exactly balance gravity, Tcos⁡θ=mgT\cos\theta = mg; the horizontal component, being the only unbalanced force, must supply the centripetal force needed for the circular motion, Tsin⁡θ=mv2rT\sin\theta = \dfrac{mv^2}{r}. …

Figure Fig.3.6Geometry of a particle performing uniform circular motion

What this figure shows. A circle of radius r centred at the origin O, drawn in the x-y plane. A particle P0 starts on the positive x-axis (theta = 0). At a later instant t, the particle has moved anticlockwise along the circle to a new position P, and its radius vector (from O to P) now makes an angle theta = omega*t with the positive x-axis, where omega is the constant angular speed. The x and y components of this radius vector are marked as r cos(theta) and r sin(theta) respectively, forming a right triangle with the radius as hypotenuse — this geometry is the starting point for differentiating the position vector to obtain …

Figure Fig.3.7Conical pendulum

What this figure shows. A mass m (the bob) is suspended by a string of length l from a fixed support point O at the apex, and instead of swinging back and forth in a vertical plane like a simple pendulum, it revolves steadily in a horizontal circle of radius r, so the string itself continuously sweeps out the surface of a cone with a constant half-angle theta measured from the vertical. Two forces act on the bob: its weight mg, drawn as a vertical arrow pointing straight down, and the string tension T, drawn along the string from the bob toward the apex O. The vertical distance from the fixed point O down to the plane of the horizontal circle is marked h, so …

Misc Ex.3.8Radius and centripetal force from angular speed and linear speed

Worked out. An object of mass 50 g moves uniformly along a circular orbit with angular speed 5 rad/s, and its linear speed is given as 25 m/s. The problem asks for the radius of the circle and the centripetal force acting on the particle. The method uses the relation between linear and angular speed, v = omegar, to solve for r = v/omega, then substitutes into the centripetal force formula F = mv^2/r (equivalently momega^2r) to get the for …

Misc Ex.3.9Magnitude of average acceleration when circular-motion velocity reverses

Worked out. A particle travels in a horizontal circle with uniform speed. At t = 0 its velocity is u = 20i + 35j m/s; after one minute its velocity has become v = -20i - 35j m/s, i.e. exactly reversed in direction with the same magnitude. The problem asks for the magnitude of the (average) acceleration over that one-minute interval. The method first finds the common speed from the given components, |u| = sqrt(20^2 + 35^2) ≈ 40.3 m/s, recognises that a velocity reversal in uniform circular motion corresponds to exactly half a revolution, so the period T is twice the given 1-minute interval (T = 2 min = 120 s), and then estimates the magnitude of acceleration as (2*pi …