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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.m\ddot{x}+c\dot{x}+kx=0.

Dividing by mm gives x¨+2ζω0x˙+ω02x=0\ddot{x}+2\zeta\omega_0\dot{x}+\omega_0^2 x=0, where ω0=k/m\omega_0=\sqrt{k/m} and ζ=c/(2km)\zeta=c/(2\sqrt{km}). Take x(0)=1x(0)=1 and x˙(0)=0\dot{x}(0)=0.

1.2Deriving the solution

Substitute x(t)=ertx(t)=e^{rt} to obtain

r2+2ζω0r+ω02=0,r=−ζω0±ω0ζ2−1.r^2+2\zeta\omega_0r+\omega_0^2=0,\qquad r=-\zeta\omega_0\pm\omega_0\sqrt{\zeta^2-1}.

For 0≤ζ<10\leq\zeta<1, let ωd=ω01−ζ2\omega_d=\omega_0\sqrt{1-\zeta^2}. The initial conditions give

x(t)=e−ζω0t[cos⁡(ωdt)+ζ1−ζ2sin⁡(ωdt)].x(t)=e^{-\zeta\omega_0t}\left[\cos(\omega_dt)+\frac{\zeta}{\sqrt{1-\zeta^2}}\sin(\omega_dt)\right].

Increasing damping changes both the decay envelope and the frequency.

1.3Critical and overdamped motion

At ζ=1\zeta=1, the root repeats and

x(t)=(1+ω0t)e−ω0t.x(t)=(1+\omega_0t)e^{-\omega_0t}.

For ζ>1\zeta>1, both roots are real and negative. Increasing damping beyond the critical value slows the long-term return to equilibrium.