Chapter 7: Gravitation

7.1: Central Forces

A central force on a particle is directed toward or away from a fixed point in three dimensions and is spherically symmetric about that point. For example, gravitational attraction force between earth and sun is a central force, where FF is equal to:

F=Gm1m2r2r^F=-G\frac{m_1m_2}{r^2}\hat{r}

The corresponding gravitational potential energy is”

U=F(r)dr=Gm1m2rU=-\int F(r)dr=-G\frac{m_1m_2}{r}

with the choice U()=0U(\infty)=0. Similarly, for a spring, we have:

F=krr^F=-kr\hat{r}
U(r)=12kr2U(r)=\frac{1}{2}kr^2

7.2: The Two Body Problem

The section shows that the two body problem is equivalent to a one-body central force problem with the right choice of coordinate. For a two body system, there is a kinetic energy for each body and a potential energy between two bodies. Altogether, there are six coordinates: three coordinates r1=(x1,y1,z1)r_1=(x_1, y_1, z_1) for the first body and three coordinates r2=(x2,y2,z2)r_2=(x_2, y_2, z_2) for the second body.

In order to reduce a two-body problem to a one-body central force problem, we use center of mass RcmR_{cm} with three coordinates.

Rcm=m1r1+m2r2m1+m2+m1r1+m2r2M\begin{equation} R_{cm}=\frac{m_1r_1+m_2r_2}{m_1+m_2}+\frac{m_1r_1+m_2r_2}{M} \end{equation}

There are also three relative coordinates:

rr2r1\begin{equation} r\equiv r_2-r_1 \end{equation}

where the relative coordinate vector points from the first body to the second, and the length is the distance between the

Vectors r1r_1 and r2r_2 can be expressed in terms of RcmR_{cm} and rr, giving us:

r1=Rcmm2Mrandr2=Rcm+m1Mr\begin{equation} r_1=R_{cm}-\frac{m_2}{M}r \quad \text{and} \quad r_2=R_{cm}+\frac{m_1}{M}r \end{equation}

The total kinetic energy of the two bodies is equal to:

T=12m1r˙12+12m2r˙22\begin{equation} T=\frac{1}{2}m_1\dot r_1^2+\frac{1}{2}m_2\dot r_2^2 \end{equation}

This is equal to:

T=12MR˙cm2+12μr˙2\begin{equation} \boxed{T=\frac{1}{2}M\dot R_{cm}^2+\frac{1}{2}\mu\dot r^2} \end{equation}

where μ\mu is the reduced mass and is equal to:

μ=m1m2m1+m2=m1m2M\mu=\frac{m_1m_2}{m_1+m_2}=\frac{m_1m_2}{M}

The Lagrangian LL is equal to:

L=TU=12MR˙cm+12μr˙2U(r)L=T-U=\frac{1}{2}M\dot R_{cm}+\frac{1}{2}\mu\dot r^2-U(r)

The Lagrangian shows that RcmR_{cm} is cyclic, so the corresponding momentum p=MRcmp=MR_{cm} is conserved. This means that the center of mass of the two-body system drifts through space with a constant velocity and momentum, reducing the two-body system to a one-body central force problem (The statement is explained further in the following section).

7.21: Interpretation of the Lagrangian(CM Frame)

he Lagrangian is we derived has two portions: the Lagrangian of the center of mass and the Lagrangian for μ\mu, the relative motion between m1m_1 and m2m_2.

L=Lcm+Lrel=12MR˙cm+12μr˙2U(r)L=L_{cm}+L_{rel}=\frac{1}{2}M\dot R_{cm}+\frac{1}{2}\mu\dot r^2-U(r)

The portion of the Lagrangian 1/2μr˙2U(r){1}/{2}\mu\dot r^2-U(r) has the same form as that a single particle with mass μ\mu orbiting around a force centered at the origin. Using spherical coordinates, position r=(r,rθ,rsinθϕ)\vec{r}=(r, r\theta, r\sin\theta\phi) and velocity is equal to v=r˙=(r˙,rθ˙,rsinθϕ˙)\vec{v}=\dot{r}=(\dot r, r\dot\theta, r\sin\theta\dot\phi).

12μ(r˙2+r2θ˙2+r2sin2θϕ˙2)U(r)\frac{1}{2}\mu(\dot r^2+r^2\dot\theta^2+r^2\sin^2\theta\dot\phi^2)-U(r)

Written in spherical coordinates and let θ=π/2\theta=\pi/2, the Lagrangian is equal to:

L=12μ(r˙2+r2ϕ˙2)U(r)L=\frac{1}{2}\mu(\dot r^2+r^2\dot\phi^2)-U(r)

The notion simplifies the two-body problem significantly if considering the inertial CM frame. The center of mass drifts with a constant velocity. In the CM frame, R˙=0\dot{R}=0, so Lcm=0L_{cm}=0. The Lagrangian is simplified into:

L=12μr˙2U(r)=12μ(r˙2+r2ϕ˙2)U(r)L=\frac{1}{2}\mu\dot r^2-U(r)=\frac{1}{2}\mu(\dot r^2+r^2\dot\phi^2)-U(r)

Interpretation of the Lagrangian and Motion in CM Frame

We make several observations from the Lagrangian:

  1. LL is not an explicit function of time, so Hamiltonian HH is conserved, which in this case is the sum of kinetic and potential energies:
    E=H=12μ(r˙2+r2ϕ˙2)+U(r)E=H=\frac{1}{2}\mu(\dot r^2+r^2\dot\phi^2)+U(r)
  1. The angle ϕ\phi is cyclic, so the corresponding angular momentum pϕp_\phi is conserved.
    pϕ=μr2ϕ˙=r×p=lp_\phi=\mu r^2\dot\phi=r\times p=l

7.3: The Effective Potential Energy

Recall that in section 7.2, we have derived the equation

E=12μ(r˙2+r2ϕ˙2)+U(r)E=\frac{1}{2}\mu(\dot r^2+r^2\dot\phi^2)+U(r)

where angular momentum pϕ=r(μrϕ˙)=lp_\phi=r(\mu r\dot\phi)=l is conserved. Expanding the expression, EE is equal to:

E=12μr˙2+12μr2ϕ˙2+U(r)E=\frac{1}{2}\mu\dot r^2+\frac{1}{2}\mu r^2\dot\phi^2+U(r)

The first term is similar 1/2mv21/2mv^2 for linear kinetic energy, and the second term 1/2μr2ϕ˙21/2\mu r^2\dot \phi^2 rotational kinetic energy. We rewrite the equation in the form

E=12μr˙2+(12μr2ϕ˙2+U(r))=12μr˙2+Ueff(r)\begin{equation} E=\frac{1}{2}\mu\dot r^2+(\frac{1}{2}\mu r^2\dot\phi^2+U(r))=\frac{1}{2}\mu\dot r^2+U_{eff}(r) \end{equation}

and defined effective potential as:

Ueff(r)=l22μr2+U(r)\begin{equation} U_{eff}(r)=\frac{l^2}{2\mu r^2}+U(r) \end{equation}

Then, energy EE is equal to:

E=12μr˙2+l22μr2+U(r)\begin{equation} E=\frac{1}{2}\mu\dot r^2+\frac{l^2}{2\mu r^2}+U(r) \end{equation}

The angular momentum ll allows us to convert rotational kinetic energy 1/2μr2θ˙21/2\mu r^2\dot \theta^2 into a term depending on position rr only, which behaves like a potential energy. The sum of this term and the “real” potential energy is defined as effective potential energy. The “fake” potential energy is called centrifugal potential

Ucent(r)=l22μr2\begin{equation} U_{cent}(r)=\frac{l^2}{2\mu r^2}\end{equation}

Because its corresponding “force” Fcent=dUcent/dt=l3/μr3F_{cent}=-dU_{cent}/dt=l^3/\mu r^3 tends to push the orbiting particle away from the force center at the origin (this can be seen by having a positive sign. An attractive force towards the origin is defined as the negative direction and vice versa). In general, Ueff(r)U_{eff}(r) has a minimum:

Ueff(r)=l3μr3+U(r)=0U'_{eff}(r)=-\frac{l^3}{\mu r^3}+U'(r)=0

the system admits circular orbit at r=Rr=R. Such an orbit would be stable if Ueff(r)>0U''_{eff}(r)>0 and unstable if Ueff(r)<0U''_{eff}(r)<0.

Ueffr=R=3l3μr4+U(r)r=R{>0:stable<0:unstable=0:critically stable\begin{equation}U''_{eff}\Big |_{r=R}=3\frac{l^3}{\mu r^4}+U''(r)\Big|_{r=R} \begin{cases} >0: \text{stable} \\ <0: \text{unstable} \\ =0: \text{critically stable}\end{cases} \end{equation}
{rmin<r<rmax:bounded noncircular orbits<r<rmin:unboundedrmax<r<:unbounded\begin{equation} \begin{cases} r_{min}<r<r_{max}: \text{bounded noncircular orbits} \\ -\infty<r<r_{min}: \text{unbounded} \\ r_{max}<r<\infty: \text{unbounded} \end{cases} \end{equation}

7.31: Radial Motion for the Central-Spring Problem

Recall that effective potential energy is defined as:

Ueff(r)=l22μr2+U(r)U_{eff}(r)=\frac{l^2}{2\mu r^2}+U(r)

where U(r)=12kr2U(r)=\frac{1}{2}kr^2 for a spring. Then, Ueff(r)U_{eff}(r) is equal to:

Ueff(r)=l22μr2+12kr2U_{eff}(r)=\frac{l^2}{2\mu r^2}+\frac{1}{2}kr^2

For l=0l=0, the angular momentum barrier vanishes, corresponding to a particle moving toward the origin. The motion is then entirely radial (truly on-dimensional) and the particle oscillates back and force through the origin.

From equation (8), we can see that energy EE is equal to:

E=12μr˙2+l22μr2+U(r)\begin{equation} E=\frac{1}{2}\mu\dot r^2+\frac{l^2}{2\mu r^2}+U(r) \end{equation}

where r˙=dr/dr\dot r=dr/dr. Solving for drdr, we get:

drdt=±2μ(E12kr2l22μr2)\frac{dr}{dt}=\pm\sqrt{\frac{2}{\mu}(E-\frac{1}{2}kr^2-\frac{l^2}{2\mu r^2})}

Using separable integration, the time t(r)t(r) to move from radius r0r_0 to rr is equal to:

t(r)=±μ2rorrdrEr2kr4/2l2/2μ\begin{equation}t(r)=\pm\sqrt{\frac{\mu}{2}}\int^r_{r_o}\frac{rdr}{\sqrt{Er^2-kr^4/2-l^2/2\mu}}\end{equation}

7.32: Radial Motion in Central Gravity

The effective potential energy of a particle in a central gravitational field is:

Ueff(r)=l22μr2GMmr\begin{equation} U_{eff}(r)=\frac{l^2}{2\mu r^2}-\frac{GMm}{r} \end{equation}

There are two types of orbits: bound orbits with energy E<0E<0 and unbound orbits with energy E0E≥0.

Bound Orbits:

Unbound Orbits

Energy EE is equal to:

E=12μr˙2+l22μr2GMmr\begin{equation} E=\frac{1}{2}\mu\dot r^2+\frac{l^2}{2\mu r^2}-\frac{GMm}{r} \end{equation}

where r˙=dr/dt\dot r=dr/dt. Solving for drdr, we get:

drdt=±2μ(E+GMμrl22μr)\frac{dr}{dt}=\pm\sqrt{\frac{2}{\mu}(E+\frac{GM\mu}{r}-\frac{l^2}{2\mu r})}

with the fact m1m2=Mμm_1m_2=M\mu. Using separable integration, t(r)t(r) is equal to:

t(r)=±2μr0rrdrEr2+GMμrl2/2μ\begin{equation}t(r)=\pm\sqrt{\frac{2}{\mu}}\int^r_{r_0}\frac{rdr}{\sqrt{Er^2+GM\mu r-l^2/2\mu}}\end{equation}
{E<0:bound orbits, ellipseEmin:bound orbit, circleE=0:barely unbound, parabolasE>0:ubound orbits, hyperbolas\begin{equation} \begin{cases} E<0: \text{bound orbits, ellipse} \\ E_{min}: \text{bound orbit, circle} \\ E=0: \text{barely unbound, parabolas} \\ E>0: \text{ubound orbits, hyperbolas} \end{cases} \end{equation}

7.4: The Shape of Central-Force Orbits

In this section, we want to determine the shape of the orbits for the time evolution determined above. To do this, we will eliminate tt from the equations and find equations involving rr and ϕ\phi only. Recall that energy EE is equal to:

E=12μr˙2+l22μr+U(r),l=mr2ϕ˙E=\frac{1}{2}\mu\dot r^2+\frac{l^2}{2\mu r}+U(r), \quad l=mr^2\dot\phi

and r˙=dr/dt\dot r=dr/dt. Because we want to find equations involving rr and ϕ\phi only (this is done by finding differential equations first), we use separable integration. We first find dr/dϕdr/d\phi. Using chain rule, we get

drdϕ=dr/dtdϕ/dt\frac{dr}{d\phi}=\frac{dr/dt}{d\phi/dt}

Solving for dr/dtdr/dt using EE and dϕ/dtd\phi/dt using angular momentum ll, dr/dϕdr/d\phi is equal to:

drdϕ=2ml2r2El2/2mr2U(r)\frac{dr}{d\phi}=\sqrt{\frac{2m}{l^2}}r^2\sqrt{E-l^2/2mr^2-U(r)}

Using separable integration, ϕ\phi is equal to:

ϕ=dϕ=±rdr/r2El2/2mr2U(r)\begin{equation} \phi=\int d\phi=\pm\int^r\frac{dr/r^2}{\sqrt{E-l^2/2mr^2-U(r)}}\end{equation}

7.41: Central Spring-Force Orbits

ϕ=dϕ=±rdr/r2El2/2mr2(1/2)kr2\begin{equation} \phi=\int d\phi=\pm\int^r\frac{dr/r^2}{\sqrt{E-l^2/2mr^2-(1/2)kr^2}}\end{equation}

Substitute z=r2z=r^2, the intergral becomes:

ϕ=dϕ=±rdz/z2El2/2mr2(1/2)kz\begin{equation} \phi=\int d\phi=\pm\int^r\frac{dz/z^2}{\sqrt{E-l^2/2mr^2-(1/2)kz}}\end{equation}

7.42: The Shape of Gravitational Orbits

7.421: By Integration

Gravitational potential energy is equal to U(r)=GMm/rU(r)=-GMm/r, so ϕ(r)\phi(r) is equal to:

ϕ=±rdr/r2E+GMm/rl2/2mr2=±rdr/rEr2+GMmrl2/2m\phi=\pm\int^r\frac{dr/r^2}{\sqrt{E-+GMm/r-l^2/2mr^2}}=\pm\int^r\frac{dr/r}{\sqrt{Er^2+GMmr-l^2/2m}}

In order to simplify the integral, we use the technique that:

dr/ra+br+cr2=1asin1(br+2arb24ac)\int \frac{dr/r}{a+br+cr^2}=\frac{1}{\sqrt{-a}}\sin^{-1}\Big(\frac{br+2a}{r\sqrt{b^2-4ac}}\Big)

where a=l2/2m,b=GMma=-l^2/2m, b=GMm and c=Ec=E. Then, ϕ\phi is equal to:

ϕ=1l2/2msin1(GMmrl2/mrG2M2m2+2l2E/m)=1l2/2msin1(GMmrl2/mr1+2El2/G2M2m31GMm)=1l2/2msin1(GMm2rl2rϵ1GMm2)=1l2/2msin1(GMm2rl2ϵGMm2r)\begin{align*} \phi &=\frac{1}{\sqrt{l^2/2m}}\sin^{-1}\Big(\frac{GMmr-l^2/m}{r\sqrt{G^2M^2m^2+2l^2E/m}}\Big) \\ &=\frac{1}{\sqrt{l^2/2m}}\sin^{-1}\Big(\frac{GMmr-l^2/m}{r\sqrt{1+2El^2/G^2M^2m^3}}\frac{1}{GMm}\Big ) \\ &=\frac{1}{\sqrt{l^2/2m}}\sin^{-1}\Big(\frac{GMm^2r-l^2}{r\epsilon}\frac{1}{GMm^2}\Big) \\ &=\frac{1}{\sqrt{l^2/2m}}\sin^{-1}\Big(\frac{GMm^2r-l^2}{\epsilon GMm^2r}\Big) \end{align*}

where ϵ\epsilon is defined as the eccentricity:

ϵ=1+2El2G2M2m3\begin{equation} \epsilon=\sqrt{1+\frac{2El^2}{G^2M^2m^3}} \end{equation}

Solving for rr, we get:

r=l2/GMm21±ϵsin(ϕϕ0)\begin{equation} r=\frac{l^2/GMm^2}{1\pm\epsilon\sin(\phi-\phi_0)} \end{equation}

By convention, we choose the plus sign in the denominator with ϕ0=π/2\phi_0=\pi/2, which in effect locates ϕ=0\phi=0 at the point of closest approach to the center, the periapse of the ellipse. The choice changes sine to cosine, giving us:

r=l2/GMm21+ϵcos(ϕ)\begin{equation} r=\frac{l^2/GMm^2}{1+\epsilon\cos(\phi)} \end{equation}

7.422: By Differentiation

Return to the step for dr/dϕdr/d\phi

drdϕ=2ml2r2El2/2mr2U(r)\frac{dr}{d\phi}=\sqrt{\frac{2m}{l^2}}r^2\sqrt{E-l^2/2mr^2-U(r)}

Let u=1/ru=1/r. Using chain rule, the equation is equal to:

d(1/u)dt=1u2dudϕ\frac{d(1/u)}{dt}=-\frac{1}{u^2}\frac{du}{d\phi}

Square the equation, we get:

(dudϕ)2=(u)2=u4(drdϕ)2(\frac{du}{d\phi})^2=(u')^2=-u^4(\frac{dr}{d\phi})^2

which is equal to:

(u)2=2ml2(El22mr2+GMmr)=2ml2(El2u22m+GMmu)(u')^2={\frac{2m}{l^2}}{(E-\frac{l^2}{2mr^2}+\frac{GMm}{r}})=\frac{2m}{l^2}(E-\frac{l^2u^2}{2m}+GMmu)

Differentiating both sides again, we get:

2uu=2ml2(l2umu+GMmu)2u'u''=\frac{2m}{l^2}(-\frac{l^2u}{m}u'+GMmu')
2uu=2uu+2GMm2lu2u'u''=-2uu'+\frac{2GMm^2}{l}u'

This gives us a second order differential equation:

u+u=GMm2l2uu''+u=\frac{GMm^2}{l^2}u'
rp=l2/GMm21+ϵ\begin{equation} r_p=\frac{l^2/GMm^2}{1+\epsilon} \end{equation}

Then, eccentricity is equal to:

ϵ=1+2El2G2M2m3\begin{equation} \epsilon=\sqrt{1+\frac{2El^2}{G^2M^2m^3}} \end{equation}

Conic sections:

The long axis of the ellipse is called the major axis, and half of this distance is the semi-major axis, denoted by aa. The shorter axis is the minor axis, and half of this distance is the semi-minor axis, denoted by bb.

One can derive several properties of the ellipses using the equation for eccentricity.

rp=a(1ϵ),ra=a(1+ϵ)\begin{equation} r_p=a(1-\epsilon), \quad r_a=a(1+\epsilon) \end{equation}
ϵ=d2a\epsilon=\frac{d}{2a}
b=a1ϵ2b=a\sqrt{1-\epsilon^2}
A=πab\begin{equation} A=\pi ab \end{equation}

Example 7.1: Orbital Geometry and Orbital Physics

Let us relate the geometrical parameters of a gravitational orbit to the physical parameters, the energy EE and angular momentum ll. The relationships follow from equations we derived. We first consider circles and ellipses, and then parabolas and hyperbolas. Find energy EE.


7.5: Bertrand’s Theorem

Betrand’s theorem: The only central force potential U(r)U(r) for which all bounded orbits are closed are the following:

  1. The gravitational potential U(r)U(r) is directly proportional to 1/r-1/r
  1. The central spring potential U(r)U(r) is directly proportional to r2r^2

7.6: Orbital Dynamics

Recall from chapter 5 From Classical to Quantum Back, Kepler identified three laws governing planetary motion.

  1. Planets move in elliptical orbits, which the sun at one focus.
  1. Planetary orbits sweep out equal areas in equal time.
  1. The periods squared of planetary orbits are proportional to their semi-major axes cubed.
T2...a3T^2...a^3

7.61: Kepler’s Second Law

Kepler’s law states that planetary orbits sweep out equal areas in equal time. The theorem is purely a result of angular momentum conservation with some approximations.

For a thin slice of triangle, where angle ϕ\phi approaches zero, areaAA is equal to Area=(1/2)(Base)(height)\text{Area=(1/2)(Base)(height)}. Because ϕ\phi is small, base is approximated using the orbit’s arc length and height is approximately equal to radius rr. Then, area AA is equal to:

A=12r(rϕ)A=\frac{1}{2}r(r\phi)

Differentiating AA with respect to time tt (notice we have assumed radius rr as a constant), we get:

dAdt=12r2ϕ˙=μr2ϕ˙2μ=l22μ\frac{dA}{dt}=\frac{1}{2}r^2\dot\phi=\frac{\mu r^2\dot\phi}{2\mu}=\frac{l^2}{2\mu}

Using separable integration, the area swiped between t1t_1 and t2t_2 is equal to:

A=t1t2l22μdt=l22μ(t2t1)A=\int^{t_2}_{t_1}\frac{l^2}{2\mu} dt=\frac{l^2}{2\mu}(t_2-t_1)

which is equal to the area sweeped between t3t_3 and t4t_4 if time intervals are equal. Thus, we have proved Kepler’s second law.

7.62: Kepler’s Third Law

Period TT is equal to:

T=2mlAT=\frac{2m}{l}A

where AA is the area of the ellipses, given by A=πabA=\pi ab. Then, TT is equal to:

T=2πGMa3/2\begin{equation} T=\frac{2\pi}{\sqrt{GM}}a^{3/2} \end{equation}

Example 7.2:

From the comet’s (Halley’s Comet) current period of T=75.3yearsT = 75.3 years and observed perihelion distance rp=0.586AUr_p = 0.586 AU (which lies between the orbits of Mercury and Venus), we can calculate the orbit’s (a) semi-major axis aa, (b) aphelion distance rar_a , and (c) eccentricity εε. (Note that 1 AU is the length of the semi-major axis of earth’s orbit, 1AU=1.5×1011m1AU=1.5×10^{11} m.)


7.6.3: Minimum Energy Transfer Orbits

When sending a spacecraft, we want to find a trajectory requiring least fuel (ignoring gravitational assist from other planets). The trajectory is called minimum-energy transfer orbit or or Hohmann transfer orbit, taking advantages to earth’s motion.

Typically, the spacecraft is first lifted into low-earth orbit (LEO), where it circles the earth a few hundred kilometers above the surface. Then, at the right time, the spacecraft is given a velocity boost Δv\Delta v the sends it away from the earth and into an orbit around the sun that reaches all the way to its destination. Once the spacecraft coasts far enough from earth and the sun’s gravity dominates, it obeys central motion we have discussed so far, including Kepler’s law. It coasts towards its destination in an elliptical orbit with the sun at one focus.

7.6.3.1: Time Taking to Reach the Destination

We will find the time taking to reach the destination using Kepler’s third law. The major axis of the craft’s orbit is 2ac=re+rp2a_c=r_e+r_p, where rer_e is the distance between the earth and the sun and rpr_p is the distance between the sun and the planet. The semi-major axis is equal to:

ac=re+rp2\begin{equation} a_c=\frac{r_e+r_p}{2} \end{equation}

From Kepler’s third law, we know that (Tc/Te)2=(ac/ae)3(T_c/T_e)^2=(a_c/a_e)^3, where TcT_c is the craft’s elliptical orbit period and TeT_e is the period when orbiting around earth. However, because the craft only use one half of the period when traveling from earth to planet, indicated by dotted lines in the figure, period TT is equal to:

T=12Tc=12(re+rp2re)3/2Te\begin{equation} \boxed{T=\frac{1}{2}T_c=\frac{1}{2}(\frac{r_e+r_p}{2r_e})^{3/2}T_e} \end{equation}

7.6.3.2: Velocity When aa Away

Now, we can outline the steps required for the spacecraft to reach Mars or an outer planet.

  1. Orbital velocity v0v_0 when r0r_0 away from earth: As mentioned before, the craft is lifted to lower orbits first with a orbital speed v0v_0, so it is in circular motion at a distance r0r_0 around earth. By equalizing centripetal and gravitational attraction force, v0v_0 is equal to:
GMer02=v02r0\frac{GM_e}{r_0^2}=\frac{v_0^2}{r_0}
v0=GMer0\begin{equation} v_0=\sqrt{\frac{GM_e}{r_0}} \end{equation}
  1. Velocity when escapes earth’s gravity: Then, at the right moment, a rocket provides a boost velocity Δv\Delta v in the same direction of v0v_0, so the craft has a velocity Δv+v0\Delta v+v_0. The applied velocity at the right moment allows the craft to escape from earth in the most efficient way. Using energy conservation, we get
    12mv2=12m(v0+Δv)2GMemr0\begin{equation} \frac{1}{2}mv_\infty^2=\frac{1}{2}m(v_0+\Delta v)^2-\frac{GM_em}{r_0} \end{equation}

    where vv_\infty is the speed at the destination. Solving for vv_\infty, we get:

    v=(v0+Δv)22GMe/r0=(v0+Δv)22v02\begin{equation} v_\infty=\sqrt{(v_0+\Delta v)^2-2GM_e/r_0}=\sqrt{(v_0+\Delta v)^2-2v_0^2} \end{equation}

  1. If the boost velocity Δv\Delta v is provided at the time when the spacecraft is moving in the same direction as earth’s velocity vev_e around the same, the craft’s velocity in the sun’s frame of reference is:
v=v+ve=(v0+Δv)22v02+ve\begin{equation} v=v_\infty+v_e=\sqrt{(v_0+\Delta v)^2-2v_0^2}+v_e \end{equation}
  1. The velocity vv we have just calculated will be the speed of the spacecraft at the perihelion point of some elliptical Hohmann transfer orbit. The required velocity vv to reach the desired orbit for the semi-major axis is calculated using energy conservation, giving us
    12mv2GMmr=GMm2a\begin{equation} \frac{1}{2}mv^2-\frac{GMm}{r}=-\frac{GMm}{2a} \end{equation}

    Thus, the required velocity for craft to be injected from Earth is equal to:

    v2=GM(2r1a)\begin{equation} v^2=GM\Big(\frac{2}{r}-\frac{1}{a}\Big) \end{equation}

Example 7.3: A Voyage to Marts

We will use this scenario to plan a trip to Mars by Hohmann transfer orbit. First, we can use Kepler’s third law to find how long it will take for the spacecraft to arrive and the boost velocity Δv\Delta v. Earth and Mar have radius of 1.5×108m1.5\times 10^8m and 2.28×108m2.28\times 10^8m.


Example 7.4: Gravitational Assists

Suppose we want to send a heavy spacecraft to Saturn, but it has only enough room for fuel to make it to Jupiter. If the timing is just right and the planets are also aligned just right, it is possible to aim for Jupiter, causing the spacecraft to fly just behind Jupiter as it swings by that planet. Jupiter can pull on the spacecraft, turning its orbit to give it an increased velocity in the sun’s frame of reference, sufficient to propel it out to Saturn. Explain how.


7.7: The Virial Theorem in Astrophysics

Consider a collection of NN point like non-relativistic partiles, where the ithith particle is at position rir_i, has momentum pip_i, and is subject to a net force FiF_i. We define a quantity GipiriG\equiv\sum_i p_i\cdot r_i, whose time derivative is:

dGdt=ip˙iri+ipir˙i\begin{equation} \frac{dG}{dt}=\sum_i \dot p_i\cdot r_i+\sum_i p_i\cdot\dot r_i \end{equation}

We know that p˙i=Fi\dot p_i=F_i and piri=mivi2=2Ti2p_i\cdot r_i=m_iv_i^2=2T_i^2. Then, the time derivative is equal to:

dGdt=iFiri+i2Ti=iFiri+2T\begin{equation} \frac{dG}{dt}=\sum_i F_i\cdot r_i+\sum_i 2T_i=\sum_i F_i\cdot r_i+2T \end{equation}

We then take the time average of each term in the equation, where the total time is τ\tau. This gives us:

<dGdt>=1τ0τdGdtdt=1τ(G(t)G(0))\begin{equation} \Big <\frac{dG}{dt}\Big >=\frac{1}{\tau}\int^\tau_0\frac{dG}{dt}dt=\frac{1}{\tau}(G(t)-G(0)) \end{equation}

If the motion is periodic such that G(t)=G(0)G(t)=G(0), the average of time derivatives is equal to zero. This is true for central force motion, such as central gravitational or spring force, where τ\tau is the orbital period. More generally, suppose all motion are at least bounded, with an upper limit to GG. Then, over a long period of time, the left-hand side of the equation is zero, such that

<dGdt>=12<Firi>\begin{equation} \Big <\frac{dG}{dt}\Big >= -\frac{1}{2}\Big <\sum F_i\cdot r_i\Big> \end{equation}
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More generally, suppose all motion are at least bounded, with an upper limit to GG. Then, over a long period of time, the average of time derivatives dG/dt=0dG/dt=0.

Because F=UF=-\nabla U, the expression becomes:

<dGdt>=12<Ur>=12<(dU/dr)r>\begin{equation} \Big <\frac{dG}{dt}\Big >= -\frac{1}{2}\Big <-\nabla U\cdot r\Big> = -\frac{1}{2}\Big <(-dU/dr)\cdot r\Big> \end{equation}

Example 7.5:

Now consider NN particles that pull on one another with central gravitational forces, so all forces on a particle are due to other particles in the system. This might be a good approximation for the gravitational attractions of stars on one another in a globular cluster, for example, or for entire galaxies attracting one another in a cluster of galaxies like the Coma Cluster or the Virgo Cluster. Let us start simply, by considering the case N=3N = 3. The force of particle 2 on particle 1 is F12F_{12} , and the force of particle 1 on particle 3 is F31F_{31}, and so on. Therefore counting all six interactions:


Summary

Key Equations

E=12μr˙2+l22μr2+U(r)E=\frac{1}{2}\mu\dot r^2+\frac{l^2}{2\mu r^2}+U(r)
t(r)=±2μr0rrdrEr2+GMμrl2/2μt(r)=\pm\sqrt{\frac{2}{\mu}}\int^r_{r_0}\frac{rdr}{\sqrt{Er^2+GM\mu r-l^2/2\mu}}
rp=l2/GMm21+ϵ,rp=a(1ϵ)r_p=\frac{l^2/GMm^2}{1+\epsilon}, \quad r_p=a(1-\epsilon)
Eccentricity:ϵ=1+2El2G2M2m3\text{Eccentricity:}\quad \epsilon=\sqrt{1+\frac{2El^2}{G^2M^2m^3}}
Semi-major axis:a=GMm2E\text{Semi-major axis:}\quad a=-\frac{GMm}{2E}
Required injection velocity from earth:v2=GM(2r1a)\text{Required injection velocity from earth:} \quad v^2=GM\Big(\frac{2}{r}-\frac{1}{a}\Big)

Practice Problems