Damped oscillations
Solve a second-order linear equation and explore how characteristic roots determine the motion.
1.1A second-order model
A mass attached to a spring and viscous damper obeys
mx¨+cx˙+kx=0.
Dividing by m gives x¨+2ζω0x˙+ω02x=0, where ω0=k/m and ζ=c/(2km). Take x(0)=1 and x˙(0)=0.
1.2Deriving the solution
Substitute x(t)=ert to obtain
r2+2ζω0r+ω02=0,r=−ζω0±ω0ζ2−1.
For 0≤ζ<1, let ωd=ω01−ζ2. The initial conditions give
x(t)=e−ζω0t[cos(ωdt)+1−ζ2ζsin(ωdt)].
Increasing damping changes both the decay envelope and the frequency.
1.3Critical and overdamped motion
At ζ=1, the root repeats and
x(t)=(1+ω0t)e−ω0t.
For ζ>1, both roots are real and negative. Increasing damping beyond the critical value slows the long-term return to equilibrium.