Simple Harmonic Motion -- background material

This page supports the multimedia tutorial Simple Harmonic Motion

Simple harmonic motion as a projection of uniform circular motion

    Here we see that the vertical component of uniform circular motion is SHM. For uniform circular motion with θ = ωt and radius r, the vertical component is

      y  =  r sin θ  =  r sin ωt

Displacement, velocity and acceleration in simple harmonic motion

    In the animation above, the purple curve is the displacement y as a funciton of t, ie y(t). The red tangent shows its slope, which is dy/dt, the velocity vy, which is shown in the next graph. On that graph, the blue tangent shows the slope dvy/dt, which is the vertical acceleration ay., which is shown in the third graph. (Revise calculus)

    Let's look at how vy and ay depend on ω. For SHM with amplitude A, let's write

      y  =  A sin ωt       so
      vy  =  dy/dt  =  Aω cos ωt       and
      ay  =  dvy/dt  =  − Aω2 cos ωt .
    These are plotted below, for two different values of ω: in the faint version ω is doubled.

    Displacement, velocity and acceleration graphs for SHM

    Displacement, velocity and acceleration graphs for SHM

    If we double ω we double the number of cycles per unit time, so we cover twice as much distance in the same time -- vy is doubled. Similarly, the acceleration goes through twice as many cycles in the same time. But more than that, the acceleration involves velocities that are twice as large, so ay is four times greater.

Chladni patterns as examples of simple harmonic motion

    Experimental set up for Chladni patterns

    Experimental set up for Chladni patterns

    In Chladni patterns, points in an object undergo SHM with varying amplitudes. Small particles (sand in this case) collect at the nodes, ie along lines where the amplitude of SHM is small.

    More about chladni patterns

    The same object usually has more than one resonance.

A spectrum represents the sum of simple harmonic oscillations

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