Orbits

The third thing that is conserved

Energy fixes an orbit's size and angular momentum fixes its shape. Neither fixes which way it points — so a curve that closes needs a third conserved quantity, and only two force laws in the universe supply one.

Assumes Conic sections and Effective potential.

A bound orbit in a central force is a curve in a plane, and a curve in a plane needs three things said about it before it is pinned down: how big, what shape, and which way round. The first two have famous answers. The total energy fixes the semi-major axis and nothing else; the angular momentum, with the energy, fixes the eccentricity. Neither of them says anything at all about the direction of perihelion.

That is not a gap in the bookkeeping. It is a real freedom: rotate an orbit about its focus and the energy and angular momentum are unchanged, because both are scalars and the force is central. So if the orbit is to close — if the body is to come back to the same perihelion revolution after revolution — something must be holding that direction, and it has to be a conserved quantity nobody has named yet.

A vector that does not change, drawn five times. The Laplace–Runge–Lenz vector A = v × L − GM r̂, constructed at five points of one orbit at e = 0.45 under a force ∝ r^−2, each drawn from the body rather than from the focus so that its length and direction can be compared point by point. Under the inverse square every one of them is the same vector: identical to machine precision in length and in direction. Its length is 0.4500, which is the eccentricity, and it points at pericentre — so the orbit's orientation is a conserved quantity and not a constant of integration, which is why the ellipse does not turn.
Fig. 1 The thing that holds it. At five points around one orbit, the vector A=v×LGMr^\mathbf{A} = \mathbf{v}\times\mathbf{L} - GM\hat{\mathbf{r}} is constructed from the body’s own position and velocity and drawn from the body. Five different positions, five different velocities, five different terms in the construction — and one vector, identical to machine precision in length and direction. Its length is the eccentricity and it points at perihelion. The orientation of the orbit is a conserved quantity, not a constant of integration, and that is why the ellipse does not turn.

Counting what is available

For motion in a plane there are four numbers of state — two positions, two velocities — and the trajectory is fixed by them. Conservation laws cut that down. Energy takes one; angular momentum takes another. Two conserved quantities leave a two-parameter family, and a two-parameter family of curves through a given point is not a closed curve: it is a curve that fills a region.

That is exactly what a general central force gives. The radial motion oscillates between a minimum and a maximum radius with one period, the angle advances steadily with another, and unless those two periods are commensurate the path never repeats. It fills an annulus.

One initial condition, three force laws. The same pericentre and the same angular momentum, integrated under an attractive central force proportional to r^−n at n = 1.5, 2, 2.5, over 3 radial periods each. The equation solved is u″ + u = k u^(n−2)/L² with u = 1/r and the independent variable the polar angle, so the drawn apsidal angle is measured from the path rather than imposed on it: n = 1.5 advances by 144.5°, n = 2 advances by 180.0°, n = 2.5 advances by 255.0°. Only the inverse square returns its pericentre to the same direction — every other exponent draws a rosette that never closes, and the two exponents that do close every bound orbit are n = 2 and the harmonic n = −1, which is Bertrand's theorem. The eccentricity is 0.45 in the n = 2 case; the others start from the same state and have no eccentricity of their own, because their orbits are not conics.
Fig. 2 The same three-way comparison with the exponents pushed further apart. At n=1.5n = 1.5 the apsidal angle is well under 180 degrees and at n=2.5n = 2.5 well over it, so both paths sweep out visibly more of the annulus in three radial periods than the near-inverse-square cases do. The middle curve is unchanged and closes exactly. Nothing about the initial conditions differs between the three; what differs is a single exponent, and the closure is a property of that exponent alone.

The angle between one perihelion and the following aphelion is called the apsidal angle. If it is π\pi, the orbit closes after one revolution: the ellipse. If it is a rational multiple of π\pi, the orbit closes after several. If it is anything else, the orbit never closes at all, and the picture is a rosette.

The angle between one pericentre and the next. The apsidal angle against the force exponent, measured from ninety-one integrated orbits at e = 0.45 rather than from a formula, with the small-eccentricity closed form π/√(3−n) drawn under it. An orbit closes when the angle divides 360° into a whole number of steps, and the two exponents at which every bound orbit closes — 180° at the inverse square and 90° at the harmonic law — are the whole of Bertrand's theorem. The gap between the two curves is the eccentricity's doing: at e = 0.45 the integrated angle departs from the near-circular value by up to 3.6°, and the departure vanishes as e → 0. What the figure cannot show is the third dimension it would need: the apsidal angle depends on the orbit as well as on the law, and this is one slice through that surface.
Fig. 3 The apsidal angle itself, against the force-law exponent. It passes through exactly 180 degrees at n=2n = 2 and through 90 at n=1n = -1, which is the linear spring — the two cases where the angle is a rational fraction of a turn for every orbit, and therefore the two laws that close. Everywhere else the angle is an irrational multiple of π\pi and the path fills its annulus. The curve is the classification the previous section defers to, drawn rather than cited, and the two points where it crosses a commensurable value are the whole of the answer.

What a different force law does

The cleanest way to see this is to keep everything about the initial conditions fixed and change only the exponent in the force. Write FrnF \propto r^{-n} and integrate — not in time, but in the angle, where the orbit equation is

d2udθ2+u=kun2L2,u=1r.\frac{d^2u}{d\theta^2} + u = \frac{k\,u^{\,n-2}}{L^2},\qquad u = \frac{1}{r}.

At n=2n = 2 that is the equation of a harmonic oscillator in θ\theta with period 2π2\pi — which is precisely the statement that the ellipse closes, and the reason the inverse square is special is visible in one line.

One initial condition, three force laws. The same pericentre and the same angular momentum, integrated under an attractive central force proportional to r^−n at n = 1.7, 2, 2.3, over 3 radial periods each. The equation solved is u″ + u = k u^(n−2)/L² with u = 1/r and the independent variable the polar angle, so the drawn apsidal angle is measured from the path rather than imposed on it: n = 1.7 advances by 156.3°, n = 2 advances by 180.0°, n = 2.3 advances by 216.1°. Only the inverse square returns its pericentre to the same direction — every other exponent draws a rosette that never closes, and the two exponents that do close every bound orbit are n = 2 and the harmonic n = −1, which is Bertrand's theorem. The eccentricity is 0.45 in the n = 2 case; the others start from the same state and have no eccentricity of their own, because their orbits are not conics.
Fig. 4 The same pericentre and the same angular momentum, under three different force laws, over three radial periods each. The apsidal angle is measured from the drawn path rather than imposed on it: 156° at n=1.7n = 1.7, exactly 180° at the inverse square, 216° at n=2.3n = 2.3. Only the middle one returns its pericentre to the same direction. The other two are perfectly good bound orbits obeying perfectly good conservation laws — they simply have nothing holding their orientation, and they precess. Note which way: a force falling off more slowly than the inverse square makes the apsides regress, and a steeper one makes them advance.

Which force laws close every bound orbit is a separate question, and it is not this essay’s. It is a classification — Bertrand’s — and the answer is that exactly two laws qualify, the inverse square and the linear spring. What is taken from it here is one fact and no argument: the inverse square is in the list, and this essay is about what puts it there. The mechanism is a conserved quantity, and a conserved quantity is a different kind of object from a theorem about exponents.

The vector, and what it is made of

The conserved quantity behind the inverse square’s closure is the Laplace–Runge–Lenz vector, and it has been discovered and forgotten about six times — by Hermann and Bernoulli in 1710, by Laplace in 1799, by Hamilton, by Gibbs, by Runge, by Lenz, and finally by Pauli, who used it to solve the hydrogen atom before Schrödinger’s equation was available. It is

A=v×LGMr^,\mathbf{A} = \mathbf{v}\times\mathbf{L} - GM\,\hat{\mathbf{r}},

a vector in the orbital plane, and the demonstration that it is constant takes three lines of differentiation and works only because the force goes as r2r^{-2}: any other exponent leaves a term over.

Two facts about it do all the work. Its magnitude is GMeGMe, so it is the eccentricity, written as a vector. And its direction is towards perihelion, which is the missing third piece of information. Conserving it conserves the orientation, and an orbit whose orientation is conserved is an orbit that closes.

A vector that does not change, drawn five times. The Laplace–Runge–Lenz vector A = v × L − GM r̂, constructed at five points of one orbit at e = 0.7 under a force ∝ r^−2, each drawn from the body rather than from the focus so that its length and direction can be compared point by point. Under the inverse square every one of them is the same vector: identical to machine precision in length and in direction. Its length is 0.7000, which is the eccentricity, and it points at pericentre — so the orbit's orientation is a conserved quantity and not a constant of integration, which is why the ellipse does not turn.
Fig. 5 The same construction on a much more eccentric orbit. The five sampled points are now at wildly different distances and speeds — the body is moving several times faster at one of them than at another — and the vector built from them is again one vector. Its length has grown, because the length is the eccentricity, and its direction has not changed at all. That the construction survives a factor of several in both position and velocity is the whole of the demonstration: nothing about it is a property of a particular part of the orbit.

The surprise: a symmetry that is not in the picture

The uncomfortable question is why an extra conservation law should exist. Noether’s theorem attaches a conserved quantity to a continuous symmetry, and energy and angular momentum come from the obvious ones: time translation and rotation in space. There is no third obvious symmetry of an inverse-square problem lying about.

There is a third symmetry, and it is not a symmetry of space. In 1935 Fock showed that the bound inverse-square problem, transformed appropriately, becomes free motion on the surface of a four-dimensional sphere; the hidden symmetry is the rotation group of that sphere, and the Laplace–Runge–Lenz vector is what the extra three rotations conserve. Nothing in the orbital plane rotates. The symmetry is in a space constructed from the momenta, and it exists only for the inverse square.

That is the connection worth carrying away from this rung, because it is where celestial mechanics turns out to have been solving a problem in atomic physics. The same hidden symmetry is why the hydrogen atom’s energy levels depend only on the principal quantum number and not on the angular momentum — states of different shape at the same energy, exactly as ellipses of different eccentricity at the same semi-major axis have the same period. The degeneracy in a spectrum and the closure of an orbit are the same fact. Break the inverse square in an atom, by screening it with other electrons, and the levels split by angular momentum; break it in an orbit, by any of the ways below, and the perihelion moves.

Breaking it, three ways

Nothing in the solar system is an exact inverse-square two-body problem, so nothing in it has an exactly conserved A\mathbf{A}, and every perihelion in it moves.

The same construction under r⁻2.3. The Laplace–Runge–Lenz vector A = v × L − GM r̂, constructed at five points of one orbit at e = 0.45 under a force ∝ r^−2.3, each drawn from the body rather than from the focus so that its length and direction can be compared point by point. The vector's length changes by 1.94e-1 and its direction by 40.61° over this arc, and the direction is the one that matters: it points at pericentre wherever it is evaluated, so a vector that turns is a pericentre that turns. What the picture cannot show is the rate — this is one radial period, and an apsidal drift of a few arcseconds a century is the same construction with the same conclusion at a scale no drawing has.
Fig. 6 The same construction under a force law that is not the inverse square. The vector still has a definition — it can be built at any point from the position and velocity — and it is no longer the same vector at every point: its direction changes by nineteen degrees over one radial period, and the direction is what matters, because it points at pericentre. A vector that turns is a pericentre that turns. What the picture cannot show is the rate: an apsidal drift of a few arcseconds per century is this same construction with this same conclusion, at a scale no drawing has.

The three ways it breaks in practice are worth separating, because they have different signs and different sizes.

The first is other bodies. A planet perturbed by the rest of the solar system is not in a two-body problem at all, and the time-averaged effect of the others is a slow rotation of its apsidal line. This is by far the largest term for Mercury: about 530 arcseconds per century, of which Venus supplies 277 and Jupiter 153. It is computed from the elements that do not stay constant and was known to a fraction of an arcsecond by 1860.

The same construction under r⁻1.9. The Laplace–Runge–Lenz vector A = v × L − GM r̂, constructed at five points of one orbit at e = 0.45 under a force ∝ r^−1.9, each drawn from the body rather than from the focus so that its length and direction can be compared point by point. The vector's length changes by 3.94e-2 and its direction by 12.06° over this arc, and the direction is the one that matters: it points at pericentre wherever it is evaluated, so a vector that turns is a pericentre that turns. What the picture cannot show is the rate — this is one radial period, and an apsidal drift of a few arcseconds a century is the same construction with the same conclusion at a scale no drawing has.
Fig. 7 The construction under a force shallower than the inverse square, which is the opposite sign to the previous example. The vector turns the other way — the pericentre regresses rather than advances — and the rate is comparable, because the departure from the exponent 2 is comparable. That sign is worth having, because the three physical mechanisms the section describes do not all push the same way: an oblate primary and general relativity both advance the pericentre, and a perturbation that effectively softens the central force can regress it.

The second is that the primary is not a point. An oblate body’s potential contains a J2J_2 term, which is a small addition falling off as r4r^{-4}, and it turns the apsides too — read off a satellite’s node and its perigee rather than off a planet’s.

One initial condition, three force laws. The same pericentre and the same angular momentum, integrated under an attractive central force proportional to r^−n at n = 1.7, 2, 2.3, over 3 radial periods each. The equation solved is u″ + u = k u^(n−2)/L² with u = 1/r and the independent variable the polar angle, so the drawn apsidal angle is measured from the path rather than imposed on it: n = 1.7 advances by 157.6°, n = 2 advances by 180.0°, n = 2.3 advances by 215.4°. Only the inverse square returns its pericentre to the same direction — every other exponent draws a rosette that never closes, and the two exponents that do close every bound orbit are n = 2 and the harmonic n = −1, which is Bertrand's theorem. The eccentricity is 0.2 in the n = 2 case; the others start from the same state and have no eccentricity of their own, because their orbits are not conics.
Fig. 8 The same three force laws at a much lower eccentricity, which is the regime a satellite in a nearly circular orbit occupies. The rosettes are still rosettes — the apsidal angles are unchanged, because the angle depends on the exponent and not on the eccentricity — and they are far harder to see, because a nearly circular orbit has no visible long axis for the turning to be visible in. That is why an oblateness-driven precession is measured from a satellite’s node rather than from its perigee: at low eccentricity the perigee is a poorly determined direction and the node is not.

The third is that the force is not exactly Newton’s.

What the rate looks like

The three sources add, and what they add up to is a rosette so tight that the drawing has to lie about the rate to show it at all.

What was actually measured

A perihelion is not observed. What is observed is a sequence of positions, and a perihelion direction is a parameter fitted to them — so the statement “Mercury’s perihelion advances by 574 arcseconds per century” is the output of an orbit determination and carries whatever the determination carried.

For most of the nineteenth century those positions were meridian-circle transits: the time at which the planet crossed a wire, turned into a right ascension, with the observer’s own clock and latitude in the chain. Le Verrier’s 1859 value came from a century of such observations plus the transits of Mercury across the solar disc, which are far more precise than any transit across a wire because they are timed against the Sun’s limb rather than against a star catalogue. The 43 arcseconds he could not account for were about a tenth of the scatter in any individual determination and were believable only because there were so many of them.

The modern number comes from a different measurement entirely. Since the 1960s Mercury’s orbit has been fixed by radar ranging — the round-trip time of a pulse, which gives a distance and not a direction — and since 2011 by tracking the MESSENGER spacecraft, whose position relative to the planet is known to metres. The residual is now known to about one part in 10410^4 of itself, and it is worth noticing that the two methods have almost nothing in common: one measures angles from a moving platform against a star catalogue, the other measures times of flight. An orbit determined from directions alone and one determined from ranges alone are conditioned in completely different ways, and agreement between them is a stronger result than either.

The cleanest apsidal measurements are not in the solar system at all. In a close binary pulsar the periastron advance is degrees per year rather than arcseconds per century — four degrees a year for PSR B1913+16 — because the relativistic term rises steeply as the orbit tightens, and the timing of an orbit measured through its pulse arrival times is precise enough to see it accumulate within a single observing season. There, the failure of the Laplace–Runge–Lenz vector to be conserved is not a residual after other effects are removed. It is the signal.

The vector as a coordinate

A conserved quantity that points somewhere and has a length is also a pair of numbers to describe an orbit with, and using it that way removes a defect that the classical elements have.

The trouble with the classical set is that two of its angles are undefined in the cases anybody cares most about. The argument of pericentre is the angle from the ascending node to the point of closest approach — and on a circular orbit there is no closest approach, so the angle is undefined and the numerical derivatives of anything computed from it blow up. The longitude of the node has the same problem for an orbit with no inclination.

Neither defect is in the physics. A nearly circular orbit is a perfectly ordinary orbit, and a satellite in one is not doing anything singular; the singularity is in the description.

The remedy is to carry the eccentricity vector itself — two components in the orbital plane, usually written h=esinϖh = e\sin\varpi and k=ecosϖk = e\cos\varpi — instead of the eccentricity and the angle separately. At zero eccentricity both components are zero, which is a perfectly good value for a number to take, and nothing is undefined. The same trick applied to the inclination gives two more components, and the resulting equinoctial elements are non-singular everywhere except for a retrograde equatorial orbit.

That is the practical descendant of the whole essay. The quantity that is conserved because the force is exactly inverse-square is also the quantity whose components make the best coordinates when the force is not quite inverse-square — because the components go smoothly to zero where the classical angles fall apart, and a perturbation that would be described as “the pericentre swung through 180 degrees” is described instead as the vector passing near the origin.

What it looks like when it is nearly conserved

The essay’s three breaking mechanisms make the vector move. Where the perturbation is small and slow, the motion has a shape worth knowing, because it is the whole content of secular perturbation theory.

Average the perturbing force over both orbits — the perturbed one and the perturber’s — and what remains is a slow drift of the eccentricity vector. For a satellite perturbed by a distant companion on a fixed orbit, that drift traces a circle in the plane of the two components, at constant speed, with a centre displaced from the origin.

The displacement is the forced eccentricity: the value the orbit would settle at if it were being held, imposed by the perturber’s own eccentricity and geometry. The radius of the circle is the free eccentricity: whatever the orbit was born with, preserved in magnitude and rotating in direction.

Two consequences follow immediately, and neither is obvious from the classical elements. An orbit whose free eccentricity happens to equal its forced eccentricity passes exactly through the origin once per circuit — meaning it becomes precisely circular, briefly, and then eccentric again with the pericentre pointing the opposite way. And an orbit’s maximum eccentricity is the sum of the free and forced values, which is what has to be checked when asking whether a body will ever cross another’s orbit.

The vector’s conservation is therefore the zeroth-order statement and its slow circulation is the first-order one, and the whole of classical secular theory is the calculation of where the centre of that circle sits and how fast the drift runs.

Where the circulation is measured

The picture above is not only a computational convenience; it is read directly off two populations.

The asteroid belt. Every asteroid’s eccentricity vector is the sum of a forced part imposed mainly by Jupiter and a free part of its own. Plotting the whole belt in the plane of the two components shows the forced centre displaced from the origin and the free eccentricities scattered around it — and a collisional family, being fragments of one parent body, appears as a tight clump, because the fragments began with nearly the same vector and drift around the same circle together.

That is how families are identified. Their members are not close together in space, since they have long since spread all the way around the belt, and they are not close in the classical elements either. They are close in the free eccentricity and free inclination, which are the parts of the description the perturbations leave alone.

The planets themselves. The solar system’s own secular solution is the same calculation with eight mutually perturbing bodies rather than one perturber, and its output is a set of frequencies at which the eccentricity vectors circulate — periods of tens to hundreds of thousands of years. The Earth’s eccentricity oscillates between about 0.005 and 0.06 as a result, and that oscillation is one of the orbital cycles that pace the ice ages.

So a quantity conserved exactly in the two-body problem becomes, in the real system, a slow clock, and its frequencies are among the few things about the solar system’s long-term behaviour that can be stated without integrating it.

The frequencies themselves are not stable over the age of the solar system, which is the one caveat that has to travel with them: the secular system is weakly chaotic, and two of its frequencies pass close enough to a resonance that the solution’s long-term behaviour cannot be extrapolated beyond a few tens of millions of years.

Which is the ordinary condition of the subject: an exact statement about two bodies, a good approximation for many, and a horizon beyond which the approximation and the system part company.

What the ladder has done

The first rung of this anchor established that a single inverse-square force allows exactly one family of curves, the conics, and that one number chooses among them. This rung says what holds a member of that family still.

The two statements together are a strong claim about the inverse square: it is not merely one force law among many that happens to be the one gravity uses, it is one of exactly two that produce closed orbits, and it possesses a symmetry that no drawing of the orbital plane contains. Both of those are properties of the exponent 2 and of nothing else.

Where the ladder goes next

Two rungs are visible from here. One is Bertrand’s theorem proper — not the two closing laws but the proof that there are no others, which is a statement about which functions can make an apsidal angle independent of the orbit and is more delicate than the near-circular formula suggests. The other is the quantum end: the same hidden symmetry, the same vector, and a spectrum whose accidental degeneracy is neither accidental nor about spectra.

About the same objects

Not linked from either essay — found by the objects both name.

What links here

Essays that link to this one from their own argument.

The objects this essay names

Each one links to every other essay that touches it.

Apsidal precessionCentral forceConic sectionsConserved quantityDegeneracyEffective potentialInverse square lawLaplace runge lenz vectorOrbital elementsRelativistic precession