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Central Force Problems

6.1 Reduction to One Dimension

For a particle of mass mm in a central potential V(r)V(r)Using polar coordinates (r,ϕ)(r, \phi) in the Plane of motion:

L=12m(r˙2+r2ϕ˙2)V(r)L = \frac{1}{2}m(\dot{r}^2 + r^2\dot{\phi}^2) - V(r)

The angular momentum l=mr2ϕ˙l = mr^2\dot{\phi} is conserved. Substituting ϕ˙=l/(mr2)\dot{\phi} = l/(mr^2):

L=12mr˙2+l22mr2V(r)L = \frac{1}{2}m\dot{r}^2 + \frac{l^2}{2mr^2} - V(r)

The effective potential is Veff(r)=V(r)+l22mr2V_{\mathrm{eff}(r) = V(r) + \frac{l^2}{2mr^2}}Where the second term is The centrifugal barrier.

6.2 Effective Potential Analysis

Definition. The effective one-dimensional energy is:

E=12mr˙2+Veff(r)E = \frac{1}{2}m\dot{r}^2 + V_{\mathrm{eff}(r)}

Since EE and ll are conserved, the radial motion is completely determined by Veff(r)V_{\mathrm{eff}(r)}.

Circular orbits occur at radii r0r_0 where Veff(r0)=0V_{\mathrm{eff}'(r_0) = 0}:

V(r0)l2mr03=0V'(r_0) - \frac{l^2}{mr_0^3} = 0

The orbit is stable if Veff(r0)>0V_{\mathrm{eff}''(r_0) \gt 0} and unstable if Veff(r0)<0V_{\mathrm{eff}''(r_0) \lt 0}.

For the Kepler problem V(r)=k/rV(r) = -k/r:

Veff(r)=kr+l22mr2V_{\mathrm{eff}(r) = -\frac{k}{r} + \frac{l^2}{2mr^2}}

Veff(r)=kr2l2mr3=0    r0=l2mkV_{\mathrm{eff}'(r) = \frac{k}{r^2} - \frac{l^2}{mr^3} = 0 \implies r_0 = \frac{l^2}{mk}}

Veff(r0)=2kr03+3l2mr04=m3k2l4>0V_{\mathrm{eff}''(r_0) = -\frac{2k}{r_0^3} + \frac{3l^2}{mr_0^4} = \frac{m^3k^2}{l^4} \gt 0}

So the circular orbit is always stable for the Kepler problem.

Effective Potential for Kepler Problem

The effective potential Veff(r)=k/r+l2/(2r2)V_{\mathrm{eff}}(r) = -k/r + l^2/(2r^2) (blue) combines the attractive 1/r-1/r well with the centrifugal barrier 1/r2\propto 1/r^2. Adjust sliders k (force constant), l (angular momentum), and E (total energy) to explore bound and unbound orbits.

6.3 The Orbit Equation

Starting from conservation of energy and angular momentum, we derive the orbit equation. Let u=1/ru = 1/r and use d/dt=(l/mr2)d/dϕ=(lu2/m)d/dϕd/dt = (l/mr^2)\, d/d\phi = (lu^2/m)\, d/d\phi:

r˙=drdt=lmr2drdϕ=lmdudϕ\dot{r} = \frac{dr}{dt} = \frac{l}{mr^2}\frac{dr}{d\phi} = -\frac{l}{m}\frac{du}{d\phi}

Substituting into the energy equation:

E=l22m(dudϕ)2+l2u22m+V(1u)E = \frac{l^2}{2m}\left(\frac{du}{d\phi}\right)^2 + \frac{l^2 u^2}{2m} + V\left(\frac{1}{u}\right)

Differentiating with respect to ϕ\phi:

l2mdudϕd2udϕ2+l2umdudϕ1u2V(1u)dudϕ=0\frac{l^2}{m}\frac{du}{d\phi}\frac{d^2u}{d\phi^2} + \frac{l^2 u}{m}\frac{du}{d\phi} - \frac{1}{u^2}V'\left(\frac{1}{u}\right)\frac{du}{d\phi} = 0

Dividing by l2u/(m)l^2 u'/(m) (assuming u0u' \neq 0):

d2udϕ2+u=ml2u2V(1u)\frac{d^2u}{d\phi^2} + u = -\frac{m}{l^2 u^2}V'\left(\frac{1}{u}\right)

This is the Binet equation.

6.4 The Kepler Problem

For V(r)=k/rV(r) = -k/r (gravitational or Coulomb potential):

V(1u)=dVdr=kr2=ku2V'\left(\frac{1}{u}\right) = \frac{dV}{dr} = \frac{k}{r^2} = ku^2

The Binet equation becomes:

d2udϕ2+u=mkl2\frac{d^2u}{d\phi^2} + u = \frac{mk}{l^2}

This is an inhomogeneous ODE with solution:

u(ϕ)=mkl2(1+ecos(ϕϕ0))u(\phi) = \frac{mk}{l^2}(1 + e\cos(\phi - \phi_0))

Where ee is the eccentricity and ϕ0\phi_0 is a constant. Setting ϕ0=0\phi_0 = 0:

r(ϕ)=l2/(mk)1+ecosϕ=p1+ecosϕr(\phi) = \frac{l^2/(mk)}{1 + e\cos\phi} = \frac{p}{1 + e\cos\phi}

Where p=l2/(mk)p = l^2/(mk) is the semi-latus rectum.

The eccentricity is determined by the energy:

e=1+2El2mk2e = \sqrt{1 + \frac{2El^2}{mk^2}}

Classification of orbits:

EnergyEccentricityOrbit Type
E<0E \lt 0e<1e \lt 1Ellipse (bound)
E=0E = 0e=1e = 1Parabola (marginally bound)
E>0E \gt 0e>1e \gt 1Hyperbola (unbound)

Bertrand’s Theorem: The only central potentials that give closed orbits for all bound states are V(r)1/rV(r) \propto 1/r (Kepler/Coulomb) and V(r)r2V(r) \propto r^2 (harmonic oscillator).

Key results for Kepler orbits:

  • Orbits are conic sections (ellipses, parabolas, or hyperbolas).
  • The semi-major axis aa satisfies E=k/(2a)E = -k/(2a) for bound orbits.
  • The period is T=2πma3/kT = 2\pi\sqrt{ma^3/k} (Kepler’s third law).

6.5 Worked Example: Satellite Orbit

Problem. A satellite of mass mm orbits Earth (M=5.97×1024kgM = 5.97 \times 10^{24}\,\mathrm{kg}) in an elliptical orbit with perigee (closest approach) rp=7000kmr_p = 7000\,\mathrm{km} and apogee (farthest point) ra=42000kmr_a = 42000\,\mathrm{km}. Find the eccentricity, semi-major axis, and orbital period.

Solution

The semi-major axis is a=(rp+ra)/2=(7000+42000)/2=24500kma = (r_p + r_a)/2 = (7000 + 42000)/2 = 24500\,\mathrm{km}.

From the orbit equation, at perigee (ϕ=0\phi = 0): rp=p/(1+e)r_p = p/(1 + e)And at apogee (ϕ=π\phi = \pi): ra=p/(1e)r_a = p/(1 - e).

Therefore:

e=rarpra+rp=42000700042000+7000=35000490000.714e = \frac{r_a - r_p}{r_a + r_p} = \frac{42000 - 7000}{42000 + 7000} = \frac{35000}{49000} \approx 0.714

The energy is E=k/(2a)E = -k/(2a) where k=GMm=6.674×1011×5.97×1024×m=3.986×1014mm3/s2k = GMm = 6.674 \times 10^{-11} \times 5.97 \times 10^{24} \times m = 3.986 \times 10^{14} m\,\mathrm m^3/\mathrm s^2.

The period (independent of mass mm):

T=2πma3k=2πa3GM=2π(2.45×107)33.986×1014T = 2\pi\sqrt{\frac{ma^3}{k}} = 2\pi\sqrt{\frac{a^3}{GM}} = 2\pi\sqrt{\frac{(2.45 \times 10^7)^3}{3.986 \times 10^{14}}}

=2π1.471×10223.986×1014=2π3.691×1072π×607538170s10.6hours= 2\pi\sqrt{\frac{1.471 \times 10^{22}}{3.986 \times 10^{14}}} = 2\pi\sqrt{3.691 \times 10^7} \approx 2\pi \times 6075 \approx 38170\,\mathrm s \approx 10.6\,\mathrm{hours}

\blacksquare

6.6 Worked Example: Rutherford Scattering

Problem. A particle of mass mm and energy E>0E \gt 0 is scattered by a repulsive Coulomb potential V(r)=k/rV(r) = k/r (k>0k \gt 0). Find the scattering angle Θ\Theta as a function of the impact parameter bb.

Solution

The angular momentum is l=mvbl = mv_\infty b where v=2E/mv_\infty = \sqrt{2E/m}. The eccentricity is:

e=1+2El2mk2=1+(2Ebk/m)2e = \sqrt{1 + \frac{2El^2}{mk^2}} = \sqrt{1 + \left(\frac{2Eb}{k/m}\right)^2}

The orbit is a hyperbola. The asymptotic angles satisfy rr \to \inftyI.e., 1+ecosϕ=01 + e\cos\phi = 0Giving ϕ±=π±arccos(1/e)\phi_{\pm} = \pi \pm \arccos(1/e). The scattering angle is:

Θ=π2arccos(1/e)=2arcsin(1/e)\Theta = \pi - 2\arccos(1/e) = 2\arcsin(1/e)

Using sin(Θ/2)=1/e\sin(\Theta/2) = 1/e:

cotΘ2=2Ebk/m=mv2bk/m\cot\frac{\Theta}{2} = \frac{2Eb}{k/m} = \frac{mv_\infty^2 b}{k/m}

This is the Rutherford scattering formula relating the scattering angle to the impact parameter. \blacksquare