Salam Academy
Paper 1 · Module

Periodic motion

Circular motion and simple harmonic motion (section 3.6.1)

5 subtopics≈ 175 min in total
  1. Kinematics of circular motion

    Angles in circular motion are measured in radians: θ=sr\theta=\dfrac sr, so a full turn is 2π2\pi rad. Angular speed ω\omega is the rate of change of angle, ω=2πT=2πf\omega=\dfrac{2\pi}T=2\pi f. A point at radius rr moves with linear speed v=rωv=r\omega. Every point on a rigid rotating object has the same ω\omega, but points further out move faster.

    ≈ 30 min
  2. Simple harmonic motion

    An oscillation is simple harmonic when the acceleration is proportional to the displacement from a fixed point and always directed towards that point: a=−ω2xa=-\omega^2x. The angular frequency is ω=2πf=2πT\omega=2\pi f=\dfrac{2\pi}T. The solution is sinusoidal: x=x0sin⁡ωtx=x_0\sin\omega t (starting from equilibrium). The period doesn't depend on the amplitude. A mass on a spring and a small-angle pendulum are both approximately simple harmonic.

    ≈ 35 min
  3. Centripetal acceleration and force

    An object moving in a circle accelerates towards the centre: a=v2r=rω2a=\dfrac{v^2}r=r\omega^2. This needs a resultant force towards the centre, F=mv2r=mrω2F=\dfrac{mv^2}r=mr\omega^2, called the centripetal force. It isn't a new kind of force: tension, gravity, friction or a normal reaction provides it. Being perpendicular to the velocity, it changes direction but does no work.

    ≈ 40 min
  4. Velocity and energy in SHM

    In SHM the speed is greatest at equilibrium, v0=ωx0v_0=\omega x_0, and zero at the extremes. At displacement xx, v=±ωx02−x2v=\pm\omega\sqrt{x_0^2-x^2}. Energy continually swaps between kinetic and potential, but the total stays constant (with no damping): E=12mω2x02E=\tfrac12m\omega^2x_0^2. Kinetic energy is 12mω2(x02−x2)\tfrac12m\omega^2(x_0^2-x^2) and potential energy is 12mω2x2\tfrac12m\omega^2x^2.

    ≈ 35 min
  5. Damping and resonance

    A resistive force (friction, air or fluid resistance) removes energy from an oscillator, so its amplitude decays: damping. Light damping gives slowly decaying oscillations; critical damping returns the system to equilibrium in the shortest time without oscillating; heavy damping returns it slowly without oscillating. When a periodic driving force matches the natural frequency, the amplitude becomes a maximum: resonance. More damping lowers and broadens the resonance peak.

    ≈ 35 min