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Problem Irodov 1.227

A satellite of mass mm circles the Moon (mass MM, radius RR) in a circular orbit of radius r=ηRr=\eta R. A weak drag force of magnitude F=αv2F=\alpha v^2, with α\alpha a known constant and vv the satellite’s speed, continually removes energy from the orbit. Find the time τ\tau until the satellite spirals down onto the Moon’s surface.

The satellite m on its present circular orbit of radius η R about the Moon M, at speed v. The decay ends at the Moon's surface, so the final orbit R lies on the rim itself.

The satellite mm on its present circular orbit of radius ηR\eta R about the Moon MM, at speed v\vect v. The decay ends at the Moon’s surface, so the final orbit RR lies on the rim itself.

Given
  • orbit radius r=ηRr=\eta R
  • resistance F=αv2F=\alpha v^2
  • satellite mass mm
Find
the time τ\tau until the satellite falls onto the Moon’s surface

Solution

Step 1Energy of a circular orbit at radius rr

At any instant the orbit is very nearly circular at its current radius rr, so gravity supplies the centripetal force there; combining this with the kinetic and potential energy at that radius gives the total mechanical energy as a function of rr alone.

γMmr2=mv2r  ⟹  v2=γMr,E(r)=12mv2−γMmr=γMm2r−γMmr.\begin{align*} \frac{\gamma Mm}{r^2} = \frac{mv^2}{r} &\;\Longrightarrow\; v^2 = \frac{\gamma M}{r}, \tag{1} \\ E(r) = \frac12 mv^2 - \frac{\gamma Mm}{r} &= \frac{\gamma Mm}{2r}-\frac{\gamma Mm}{r}. \tag{2}\end{align*}
E(r)=−γMm2rE(r) = -\frac{\gamma Mm}{2r}
(3)
Step 2Rate of energy loss to drag

The drag force opposes the motion, so it removes mechanical energy at the rate it does work against the satellite, FvFv; writing F=αv2F=\alpha v^2 turns this into a pure power of vv.

−dEdt=Fv=αv3.(4) -\frac{dE}{dt} = Fv = \alpha v^3. \tag{4}
Step 3Convert the energy loss into a rate of change of rr

Differentiating (3) with respect to rr, then using the chain rule dE/dt=(dE/dr)(dr/dt)dE/dt = (dE/dr)(dr/dt) together with (4), isolates dr/dtdr/dt; substituting v2=γM/rv^2=\gamma M/r from (1) leaves an equation in rr and tt alone.

dEdr=γMm2r2  ⟹  γMm2r2drdt=−αv3,drdt=−2αv3r2γMm=−2αr2γMm(γMr)3/2.\begin{align*} \frac{dE}{dr} = \frac{\gamma Mm}{2r^2} &\;\Longrightarrow\; \frac{\gamma Mm}{2r^2}\frac{dr}{dt} = -\alpha v^3, \\ \frac{dr}{dt} &= -\frac{2\alpha v^3 r^2}{\gamma Mm} = -\frac{2\alpha r^2}{\gamma Mm}\left(\frac{\gamma M}{r}\right)^{3/2}. \tag{5}\end{align*}
drdt=−2αγMm r1/2\frac{dr}{dt} = -\frac{2\alpha\sqrt{\gamma M}}{m}\,r^{1/2}
(6)
Step 4Integrate from the present orbit down to the surface

Separating rr and tt in (6) and integrating from r=ηRr=\eta R at t=0t=0 to r=Rr=R at t=τt=\tau, when the satellite reaches the surface, gives τ\tau.

∫ηRRr−1/2 dr=−2αγMm∫0τdt2R−2ηR=−2αγMm ττ=mR (η−1)αγM=m(η−1)αγM/R.\begin{align*} \int_{\eta R}^{R} r^{-1/2}\,dr &= -\frac{2\alpha\sqrt{\gamma M}}{m}\int_0^\tau dt \\ 2\sqrt{R}-2\sqrt{\eta R} &= -\frac{2\alpha\sqrt{\gamma M}}{m}\,\tau \\ \tau &= \frac{m\sqrt{R}\,(\sqrt\eta-1)}{\alpha\sqrt{\gamma M}} = \frac{m(\sqrt\eta-1)}{\alpha\sqrt{\gamma M/R}}. \tag{7}\end{align*}

Since γM/R2\gamma M/R^2 is the Moon’s own surface gravity gg, the ratio γM/R\gamma M/R equals gRgR.

τ≈m(η−1)αgR\tau \approx \frac{m(\sqrt\eta-1)}{\alpha\sqrt{gR}}
(8)
Check

Dimensionally α\alpha carries units kg/m, since F=αv2F=\alpha v^2; multiplying by gR\sqrt{gR}, a speed, gives kg/s, and dividing the mass mm by that leaves a time, as required. As η→1\eta\to1 (the satellite already grazing the surface) the boxed τ→0\tau\to0, consistent with no distance left to spiral through.

Remark

The trick worth keeping is converting a tt-integral into an rr-integral by writing EE and vv as functions of rr alone (Step 1), valid whenever the perturbation is weak enough that the orbit stays nearly circular at every instant; the same reduction works for any drag law F(v)F(v), not only αv2\alpha v^2, since it only ever used E(r)E(r) and −dE/dt=Fv-dE/dt=Fv.