M3.3 - Further dynamics

Syllabus
2019
Topic
M3.3
Level
A2

Learning objectives

Solve one-dimensional motion under a variable force

For motion along one signed axis, first write the resultant force with its direction, then choose the acceleration form that matches the variable in the force law. A varying force produces a differential equation rather than a constant-acceleration problem.

Fresultant=ma,a=dvdt=vdvdxF_{\mathrm{resultant}}=ma,\qquad a=\frac{\mathrm dv}{\mathrm dt}=v\frac{\mathrm dv}{\mathrm dx}

Force information Useful equation Typical result
F=f(t)F=f(t) mdv/dt=f(t)m\,\mathrm dv/\mathrm dt=f(t) integrate for v(t)v(t), then for x(t)x(t) if needed
F=f(x)F=f(x) mvdv/dx=f(x)mv\,\mathrm dv/\mathrm dx=f(x) integrate for v2v^2 as a function of xx
work is simpler x0xF(s)ds=12m(v2v02)\int_{x_0}^{x}F(s)\,\mathrm ds=\tfrac12m(v^2-v_0^2) compare two positions directly
inverse-square attraction choose outward positive, so F=k/x2F=-k/x^2 preserve the negative force sign before integrating

Define the coordinate origin and positive direction before inserting a force. Include every force component in the resultant. Separate variables or integrate with limits, use the supplied motion condition to determine the constant, and accept only positions for which v20v^2\ge0 and the force model is defined.

A 22 kg particle moves in the positive xx-direction under resultant force F=122xF=12-2x N. At x=0x=0, its speed is 1ms11\,\mathrm{m\,s^{-1}}. Since2vdvdx=122x,2v\frac{\mathrm dv}{\mathrm dx}=12-2x,integration between the initial position and xx givesv2=1+12xx2.v^2=1+12x-x^2.At x=3x=3 m, v=28=27ms1v=\sqrt{28}=2\sqrt7\,\mathrm{m\,s^{-1}}. A turning point requires v=0v=0; the positive solution is x=6+37x=6+\sqrt{37} m.

For an attractive inverse-square force with outward coordinate x>0x>0, F=k/x2F=-k/x^2. Thenmvdvdx=kx2mv\frac{\mathrm dv}{\mathrm dx}=-\frac{k}{x^2}integrates to 12mv2=k/x+C\tfrac12mv^2=k/x+C. The plus sign on k/xk/x after integration is consistent with differentiating k/xk/x to recover k/x2-k/x^2.

Do not use constant-acceleration formulae, omit a force from the resultant, drop the factor vv in a=vdv/dxa=v\,\mathrm dv/\mathrm dx, or remove the sign from an attractive inverse-square force. A negative value of v2v^2 signals an inaccessible region, not an imaginary physical speed.

Recognise and calculate with simple harmonic motion

Motion is simple harmonic when acceleration is proportional to displacement from a fixed equilibrium point and always directed back towards that point. With signed displacement xx from equilibrium, the defining equation is

x¨=ω2x\ddot x=-\omega^2x

To prove SHM in a mechanical system, write a signed equation of motion and simplify it in terms of displacement from equilibrium. Constant force terms must cancel at equilibrium. Reaching x¨=cx\ddot x=-c x with c>0c>0 proves SHM and identifies ω=c\omega=\sqrt c; merely obtaining a periodic-looking expression is not the required force-law proof.

Quantity SHM relation
displacement x=Acos(ωt+ϕ)x=A\cos(\omega t+\phi), equivalently a sine form
speed at displacement xx v2=ω2(A2x2)v^2=\omega^2(A^2-x^2)
period T=2π/ωT=2\pi/\omega
maximum speed, at equilibrium vmax=ωAv_{\max}=\omega A
maximum acceleration, at an endpoint amax=ω2A|a|_{\max}=\omega^2A

Choose the phase from the initial state. Release from rest at x=Ax=A allows x=Acosωtx=A\cos\omega t; starting at equilibrium in the positive direction allows x=Asinωtx=A\sin\omega t. For time spent in a region, solve the boundary displacement within one cycle and use the symmetry of the cosine or sine curve without double-counting endpoints.

If x=0.12cos(5t)x=0.12\cos(5t) metres, then A=0.12A=0.12 m, ω=5rads1\omega=5\,\mathrm{rad\,s^{-1}} and T=2π/5T=2\pi/5 s. The maximum speed is 0.60ms10.60\,\mathrm{m\,s^{-1}}. Starting at the positive endpoint, the first time the particle reaches x=0.06x=0.06 m satisfies cos(5t)=1/2\cos(5t)=1/2, so t=π/15t=\pi/15 s.

Displacement must be measured from equilibrium, not an arbitrary origin. The minus sign is essential: x¨=+ω2x\ddot x=+\omega^2x drives motion away from equilibrium and is not SHM. Amplitude is a non-negative distance, whereas xx, vv and acceleration are signed.

Model elastic oscillations about equilibrium

A particle attached to an ideal spring or taut elastic string can perform SHM along the element's direction. Measure displacement from the equilibrium position: doing so makes the constant weight term cancel and exposes the restoring force.

mx¨=kx,ω=km,k=λlm\ddot x=-kx,\qquad \omega=\sqrt{\frac{k}{m}},\qquad k=\frac{\lambda}{l}

For a vertical element, let its equilibrium extension be ee. Equilibrium gives ke=mgke=mg. If downward displacement from equilibrium is xx, the extension is e+xe+x andmx¨=mgk(e+x)=kx.m\ddot x=mg-k(e+x)=-kx.Gravity shifts the equilibrium position but does not appear in ω\omega after this cancellation.

Arrangement Condition for the SHM model to remain valid
spring deformation stays within the stated Hooke-law model
one elastic string its extension never becomes negative; for equilibrium extension ee and amplitude AA, require eA0e-A\ge0
particle between two elastic strings calculate both extensions at each extreme and require both strings to remain taut
string reaches natural length tension becomes zero; subsequent motion is not governed by the same SHM equation

A 0.50.5 kg particle oscillates vertically on an elastic element with stiffness 18Nm118\,\mathrm{N\,m^{-1}}. Then ω=18/0.5=6rads1\omega=\sqrt{18/0.5}=6\,\mathrm{rad\,s^{-1}} and T=π/3T=\pi/3 s. If its amplitude is 0.080.08 m, its speed at displacement 0.040.04 m isv=60.0820.042=0.416ms1.v=6\sqrt{0.08^2-0.04^2}=0.416\,\mathrm{m\,s^{-1}}.If the element is a string, this calculation applies for the whole oscillation only after checking that the minimum extension remains non-negative.

Do not measure elastic extension and SHM displacement from the same origin without defining both, leave the equilibrium weight term in the final restoring equation, or claim one continuous SHM cycle after a string goes slack. The specified oscillation is along the string or spring, not transverse to it.