Orbits

Only two force laws let an orbit come back

That a planet returns to the same point of its own path after one lap is not a fact about orbits. It is a fact about the exponent in the force, and out of the whole continuum of attractions only two — the inverse square, and a spring — bring every bound orbit back to where it started.

Assumes Effective potential and Conic sections.

An orbit has two clocks in it and they are not the same clock. One counts the time from periapsis back to periapsis — the radial period, the time for the body to fall in, turn, and climb out again. The other counts the time to go once round in angle. For a planet the two agree exactly, and because they agree the path shuts on itself and the same ellipse is retraced for ever.

Nothing requires them to agree. The well angular momentum builds has a bottom, and a body displaced from the bottom of a well oscillates radially while it also revolves; whether the two rhythms are commensurate is a question about the shape of the well, and the shape of the well is a question about the force. Change the exponent by a hundredth and the two clocks drift apart, the path never repeats, and what was an ellipse becomes a rosette that fills an annulus.

The remarkable part is how few exponents let the clocks agree. Not a sparse set, not a family with parameters: two.

The two force laws whose orbits close. The apsidal angle — the angle swept from periapsis to the next apoapsis — against the exponent of the force law, for F ∝ r^p. The dashed curve is the near-circular limit π/√(3+p), which has a closed form; the solid curve is the same angle for an orbit of eccentricity 0.4, computed by quadrature of ∫(L/r²)dr/√(2(E−U)) between its two turning points, with U the effective potential. An orbit closes when the apsidal angle is a rational multiple of π, and an orbit closes at every eccentricity only where the two curves meet: p = −2 at exactly 180° and p = +1 at exactly 90°, which is Bertrand's theorem. The quadrature returns 180.0000° and 90.0000° at those two exponents and departs from the near-circular curve by 1.4° at p = 0. The angle diverges as p approaches −3, where the circular orbit stops being stable and there is no well left to oscillate in.
Fig. 1 The apsidal angle — the angle swept between one periapsis and the next apoapsis — against the exponent of the force law, for FrpF \propto r^{p}. The dashed curve is the near-circular limit, which has a closed form. The solid curve is the same angle for an orbit of eccentricity 0.4, obtained by quadrature of (L/r2)dr/2(EUeff)\int (L/r^2)\,dr/\sqrt{2(E-U_{\rm eff})} between the two turning points. The curves touch at exactly two places: p=2p = -2 at 180° and p=+1p = +1 at 90°. Everywhere else they separate, and where they separate the apsidal angle depends on the eccentricity — which is what stops the orbit closing for a whole family of orbits at once.

The angle that has to be measured

The quantity to compute is the angle the body sweeps while its radius goes from its smallest value to its largest. Call it the apsidal angle. If it is 180°180° the far end of the orbit is directly opposite the near end, the next half-lap retraces the first by symmetry, and the path is closed after one revolution.

Getting it is a matter of dividing one rate by another. The angular rate is fixed by the conservation law that equal areas express, θ˙=L/r2\dot\theta = L/r^2. The radial rate comes from the energy, r˙=2(EUeff(r))\dot r = \sqrt{2(E - U_{\rm eff}(r))}. Their ratio is dθ/drd\theta/dr, and integrating it between the turning points gives

Φ=rr+L/r22(EUeff(r))dr.\Phi = \int_{r_-}^{r_+} \frac{L/r^2}{\sqrt{2\left(E - U_{\rm eff}(r)\right)}}\,dr .

That integral is the whole subject, and it has an unpleasant feature: at both ends the square root vanishes, because a turning point is by definition where the radial speed is zero. The integrand goes to infinity at each limit, integrably but not gently, and no evenly spaced rule in rr survives it.

The standard escape is a change of variable that makes the singularities cancel. Write the radius as the midpoint of the two turning points plus a sine, r=A+Bsinθr = A + B\sin\theta with AA the mean and BB the half-difference. Then drdr carries a factor of cosθ\cos\theta, and near each end the vanishing square root also behaves like cosθ\cos\theta, so the two cancel and what is left is a smooth function of θ\theta over half a turn. Every apsidal angle in this essay is that integral, evaluated at the midpoints of four thousand equal steps, which never lands on either end.

The other half of the setup is less obvious and matters more. To compare force laws fairly, every orbit drawn has to be the same orbit in some sense, and the natural sense is that it spans the same pair of radii. So the energy and angular momentum are solved for from the turning points rather than chosen: demanding that the radial speed vanish at both rr_- and r+r_+ is two equations in the two unknowns, and it fixes them. An orbit that runs from 0.6 to 1.4 under one force law is compared with an orbit that runs from 0.6 to 1.4 under another, and nothing else about them is held fixed, because nothing else can be.

Why the easy answer is not the answer

There is a closed form, and it is the reason this question looks settled until it is examined.

Take an orbit only slightly eccentric. The body sits near the bottom of the well and executes small radial oscillations about the circular radius. A well is quadratic near its minimum, so the oscillation is simple harmonic, and its frequency follows from the second derivative of the effective potential there. Dividing that by the angular frequency gives

Φcirc=π3+p,\Phi_{\rm circ} = \frac{\pi}{\sqrt{3+p}} ,

for a force FrpF \propto r^{p}. It is three lines of algebra and it contains a great deal. At p=2p = -2 it gives π\pi, which is the closed ellipse. At p=+1p = +1 it gives π/2\pi/2: a quarter turn from periapsis to apoapsis, so four of them make a full revolution and the orbit closes after two radial periods. As pp falls toward 3-3 the denominator vanishes and the angle diverges, which is the statement that the circular orbit is losing its stability — below 3-3 there is no minimum in the effective potential at all, only a monotone slide, and a body perturbed inward keeps going.

The temptation is to stop there. If Φcirc/π\Phi_{\rm circ}/\pi is a rational number the orbit closes, and rational numbers are dense, so closure looks common: p=2.25p = -2.25 gives Φ=120°\Phi = 120°, three of which make a full turn, and the path shuts after three radial periods.

It does — for that one orbit. The trap is that Φcirc\Phi_{\rm circ} is the limit of the apsidal angle as the eccentricity goes to zero, and a force law that closes only in that limit closes only the orbits that are already circles.

The two force laws whose orbits close. The apsidal angle — the angle swept from periapsis to the next apoapsis — against the exponent of the force law, for F ∝ r^p. The dashed curve is the near-circular limit π/√(3+p), which has a closed form; the solid curve is the same angle for an orbit of eccentricity 0.7, computed by quadrature of ∫(L/r²)dr/√(2(E−U)) between its two turning points, with U the effective potential. An orbit closes when the apsidal angle is a rational multiple of π, and an orbit closes at every eccentricity only where the two curves meet: p = −2 at exactly 180° and p = +1 at exactly 90°, which is Bertrand's theorem. The quadrature returns 180.0000° and 90.0000° at those two exponents and departs from the near-circular curve by 4.9° at p = 0. The angle diverges as p approaches −3, where the circular orbit stops being stable and there is no well left to oscillate in.
Fig. 2 The same comparison at an eccentricity of 0.7 rather than 0.4. The near-circular curve has not moved, because it does not know about eccentricity; the quadrature has, and the gap between them has roughly tripled. At p=0p = 0 — a force of constant strength, which is what a body feels inside a long uniform cylinder of matter — the two answers differ by five degrees. The two crossings have not moved at all. That immobility is the theorem: at p=2p = -2 and p=+1p = +1 the apsidal angle is independent of the eccentricity, and at every other exponent it is not.

The distinction is worth stating plainly because it is the difference between a curiosity and a theorem. A force law closes a single orbit if its apsidal angle for that orbit is a rational multiple of π\pi; it closes every bound orbit only if its apsidal angle is the same rational multiple for all of them at once. The second is an enormously stronger demand, and Bertrand proved in 1873 that exactly two power laws meet it.

The proof is an expansion of the apsidal angle in the eccentricity. The first correction beyond the near-circular value involves the third and fourth derivatives of the potential, and setting it to zero for all orbits forces the potential into one of two forms. Continuing to the next order confirms there is nothing else. The result is short to state and was not easy to find, and it is one of the few theorems in classical mechanics whose content is an absence.

Watching the clocks separate

The quadrature produces a number; a number is easier to believe when the path is drawn from the same integral that measured it.

An orbit under F ∝ r^-2, which comes back to where it started. A bound orbit of eccentricity 0.4 drawn in the plane, under a force falling as the 2 power of the radius. Between one apoapsis and the next the body sweeps 360.00°, and that is a whole turn, so every apoapsis falls in the same place — the path closes, and the 5 radial periods drawn lie on one curve. That is the property Bertrand's theorem says only two force laws in the whole family have. The trajectory is generated from the same quadrature that measures the angle, so the closure is a result rather than a construction.
Fig. 3 Five radial periods of a bound orbit under the inverse square, traced from the cumulative form of the same quadrature. The five apoapsis points are drawn and there is one mark on the page, because they coincide. The path is one ellipse gone round five times, and the closure is an output of the computation rather than something the drawing was constructed to show.
An orbit under F ∝ r^-2.5, traced for 7 radial periods. The same bound orbit of eccentricity 0.4 drawn in the plane, under a force falling as the 2.5 power of the radius. Between one apoapsis and the next the body sweeps 515.59°, against the 360° an inverse-square orbit sweeps — so the path is a rosette rather than a closed curve, and the 7 apoapsis points marked are 515.59° apart. Nothing here is a perturbation of an ellipse: the force law is exact and the orbit simply does not close. The trajectory is generated from the same quadrature that gives the apsidal angle, so the picture and the number are one computation.
Fig. 4 The same eccentricity under a force falling as the 2.5 power instead of the 2 — a change a quarter as large as the difference between gravity and a spring. The apsides now advance by 156° a lap and the path is a rosette that never repeats. The annulus between the two turning radii is the region the body is confined to, and given long enough it passes arbitrarily close to every point of it.

The second of those is what a non-closing orbit looks like when the departure is not small, and the eye reads it as a different kind of motion. It is not. It is the same two clocks running at rates whose ratio is irrational, and the ellipse of the first figure is the exceptional case rather than the normal one.

An orbit under F ∝ r^1, which comes back to where it started. A bound orbit of eccentricity 0.55 drawn in the plane, under a force rising in proportion to the radius. Between one apoapsis and the next the body sweeps 180.00°, and 2 of those come to a single full turn, so the apsides occupy 2 fixed directions and no more — the path closes, and the 4 radial periods drawn lie on one curve. That is the property Bertrand's theorem says only two force laws in the whole family have. The trajectory is generated from the same quadrature that measures the angle, so the closure is a result rather than a construction.
Fig. 5 The other closing law, at a higher eccentricity: a force proportional to the distance, which is a spring. The apsides are 180° apart, so the orbit closes after two radial periods rather than one, and the resulting figure is an ellipse centred on the source rather than focused on it. That is the second of the two exceptions, and it is worth seeing because it is so obviously not a Kepler orbit while being just as closed.

The centred ellipse deserves a sentence of its own. A body on a spring moves as two independent harmonic oscillators, one along each of two perpendicular axes, at the same frequency and with whatever relative phase the initial conditions supply. The sum of two perpendicular sinusoids of equal frequency is an ellipse about the origin, always, and the source of the force sits at the middle. So both closing laws give ellipses and the ellipses are not the same ellipse: one has the attractor at a focus and the other at the centre, and no continuous change of the exponent carries one into the other, because everything between them fails to close.

Newton got there first and got the number wrong

The apsidal angle was a test of the force law a hundred and eighty years before Bertrand classified the laws, and the episode is worth recounting because it shows the measurement being used in the direction it is actually useful.

In the first book of the Principia Newton works out what happens when an inverse-cube term is added to any central force: the orbit keeps its shape in a rotating frame, so a closed orbit becomes a precessing one at a rate the added term fixes exactly. He then runs the argument backwards. The Moon’s line of apsides makes a complete circuit in 8.85 years, which is a precession of about three degrees a lunar month, and inverting his own result turns that into an effective exponent for the force holding the Moon.

The answer came out near 2.016-2.016 rather than 2-2, and Newton reported it as a confirmation with a discrepancy he attributed to the Sun’s perturbation. He was right about the cause and wrong about the size: the solar perturbation accounts for the whole of the Moon’s apsidal motion, but the first-order calculation he could do gives only half of it. The missing half occupied Clairaut, d’Alembert and Euler for a decade in the 1740s, and was briefly taken as evidence that the inverse-square law needed an extra term. Clairaut carried the expansion to second order in 1749, found the other half, and withdrew the objection.

The whole of that argument rests on the fact this essay is about. An apsidal motion is a measurement of the force law only because the exact inverse square has none, and a disagreement about a precession is therefore a disagreement about gravity rather than about an orbit. The eighteenth century’s near-miss and the nineteenth’s genuine residual at Mercury are the same measurement made twice, with the difference that the second one survived every subtraction.

The modern bound from the same observable is tight. Lunar laser ranging determines the Moon’s distance to a centimetre and its apsidal motion correspondingly well, and after every Newtonian term has been removed the residual constrains a departure in the exponent to a few parts in 101110^{11}. The measurement Newton made with a calendar is still the measurement, six orders of magnitude better.

The two cases are not obscure

It would be a tidier story if the two exceptions were mathematical accidents with no physical tenants. They are the two most common force laws in the subject.

The inverse square is gravity outside any spherical body, which the shell theorem guarantees exactly rather than approximately. Everything this collection says about planets, moons, binary stars and spacecraft lives there.

The linear law is gravity inside a uniform sphere. Enclosed mass grows as the cube of the radius, the inverse-square attraction of that mass falls as the square, and the product is proportional to rr. So a body dropped down a shaft through an idealised planet executes simple harmonic motion, which is why the tunnel takes the same time whichever pair of points it joins, and a body given some sideways motion in the same shaft traces a closed centred ellipse.

The only two force laws in the continuum that close every orbit are the field outside a sphere of matter and the field inside one. Nothing in Bertrand’s proof knows about spheres. The theorem is about the exponents 1 and 2-2, and it happens that those are the two exponents that a lump of matter actually produces, on either side of its own surface.

That is the kind of coincidence worth being suspicious of, and the suspicion does not survive inspection: the two exponents are related by nothing except that 11 and 2-2 both give 3+p3+p equal to a perfect square of a rational, which is what the closed form needs. There is no deeper connection, and the collection is entitled to find the arrangement fortunate rather than meaningful.

There is also a direction to the failure, and it is easy to lose. Between p=3p = -3 and p=2p = -2 the denominator 3+p\sqrt{3+p} is less than one, the apsidal angle exceeds 180°180°, and the apsides advance — the orbit precesses the way the body goes round. Between p=2p = -2 and p=+1p = +1 the angle is under 180°180° and the apsides regress. So the inverse square is not merely a point where closure happens; it is the boundary between two qualitatively different behaviours, and a measured precession has a sign that says which side of it the force is on. Mercury’s residual advances, which excludes a shallower-than-inverse-square attraction outright and was noticed as a constraint long before anyone could explain the number.

What a small departure does

Between the two exceptions the whole continuum fails, and most real systems sit slightly off one of them rather than far from both. The useful question is therefore not whether an orbit closes but how fast its apsides turn when it nearly does.

Expand the apsidal angle about p=2p = -2. A small excess δ\delta in the exponent shifts Φcirc\Phi_{\rm circ} by πδ/2-\pi\delta/2 to first order, which means the apsides advance or regress by πδ\pi\delta per revolution — a precession rate directly proportional to the departure from the inverse square, with no threshold beneath which it vanishes.

That linearity is why the measurement is worth making. The forty-three arcseconds a century left over in Mercury’s motion are a departure of this kind, though not a change in the exponent: general relativity adds a third term to the effective potential rather than altering the second, and the third term is negative and steep. The observable is the same, and so is the logic — an orbit that did not shut was the evidence, and it was evidence because for an inverse square it had to.

The effective potential, for three angular momenta. The radial motion of an orbiting body is one-dimensional motion in an effective potential: the attraction −GM/r plus the centrifugal term L²/2r² that the angular momentum contributes. The barrier at small radius is what stops a body with any angular momentum at all from reaching the centre, and the bottom of each well is the circular orbit.
Fig. 6 The wells themselves, for three angular momenta under the unmodified inverse square, which is the object all of the above is an interrogation of. Nothing in this drawing announces that the orbits in these wells close: the shape looks generic, the minima are ordinary minima, and a well of the same general appearance produced by any other exponent gives a rosette. Closure is not visible in the effective potential. It is a property of how the radial and angular periods happen to relate, and reading it off requires the integral rather than the picture.

That last point is the honest limitation of the drawing this whole argument is built on, and it is worth being blunt about. The effective potential answers where a body can go with complete authority. It answers how the body’s angle advances only through an integral that has to be done, and the two closing exponents are invisible in the curve.

What actually closes, and what has been checked

The theorem is about idealised power laws, and no physical system is one. It is fair to ask what the observational content is.

The strongest statement is negative and it is about the solar system. Planetary apsides do turn: Mercury’s line of apsides advances by 574 arcseconds a century, of which all but 43 comes from the pull of the other planets. The departures from a pure inverse-square problem are therefore large and known, and what makes the residual interesting is that everything else was subtracted first. Bertrand’s theorem is what licenses treating an unexplained precession as evidence of new physics, because under the exact inverse square there is no precession to explain away.

The laboratory version is sharper. Torsion-balance experiments look for departures from the inverse square at short range by comparing the force between masses at different separations, and they constrain a fractional change in the exponent to better than a part in 101010^{10} over laboratory distances. Planetary ranging does the same over astronomical ones. Neither experiment is described as a test of Bertrand’s theorem, but the quantity being bounded is exactly the δ\delta whose linear consequence is a precession.

And there is a case where the exponent is genuinely different and the rosettes are the observed behaviour. A star orbiting inside a galaxy feels the enclosed mass rather than a point mass, and in the region where the rotation curve is flat the enclosed mass grows in proportion to the radius, so the force falls as 1/r1/r — the logarithmic potential, p=1p = -1.

An orbit under F ∝ r^-1, traced for 6 radial periods. The same bound orbit of eccentricity 0.5 drawn in the plane, under a force falling as the 1 power of the radius. Between one apoapsis and the next the body sweeps 248.60°, against the 360° an inverse-square orbit sweeps — so the path is a rosette rather than a closed curve, and the 6 apoapsis points marked are 248.60° apart. Nothing here is a perturbation of an ellipse: the force law is exact and the orbit simply does not close. The trajectory is generated from the same quadrature that gives the apsidal angle, so the picture and the number are one computation.
Fig. 7 Six radial periods in a logarithmic potential, which is what a star in the flat part of a galaxy’s rotation curve moves in. The apsidal angle is 124°, so the apsides regress by about 111° a lap and the orbit is a rosette by an enormous margin rather than a marginal one. Every disc star’s path looks like this, and the reason a galaxy’s disc looks smooth rather than striped is that it is made of many such orbits caught at every point of their own cycles.

The measurement that reaches this is not of one star’s rosette, which nobody will watch for a hundred million years. It is the ratio of the radial to the angular frequency in the solar neighbourhood, read off the velocity distribution of nearby stars, and it comes out near 1.41.4 rather than the 11 a closed orbit would need. The rosette is inferred from a statistic rather than watched, which is the ordinary situation in this field and worth saying out loud.

Where the theorem stops

It is about power laws, and gravity in a real system is not one. A potential that is inverse-square at one radius and logarithmic at another has an apsidal angle that varies from orbit to orbit, and Bertrand’s classification simply does not apply to it. What survives is the local statement: at each radius the effective exponent sets the local precession rate.

It is Newtonian. Adding the relativistic GML2/c2r3-GML^2/c^2r^3 term to the effective potential produces an apsidal angle greater than 180°180° for every bound orbit, so no relativistic orbit closes, including the ones around the Sun. The ellipse of the first figure is an approximation that happens to be superb, and the precession it fails to contain is how the failure was found.

And it says nothing about stability. A closed orbit and an unclosed one are equally stable or unstable; closure is about commensurability, stability about the sign of a second derivative. Both change at p=3p = -3, where the well disappears, and at every other exponent they are unrelated properties — which is worth holding onto, because “the orbit does not close” has the sound of an instability and is not one.

Energy levels in the effective potential, L = 1.2. The same curve read as a one-dimensional problem. A horizontal line is a total energy; the body moves along it between the two radii where it meets the curve, and cannot go outside them. The lowest line touches the curve at one point, which is the circular orbit; the highest lies above the curve everywhere beyond one radius, which is an unbound orbit.
Fig. 8 The reading the closure question is always asked about: one well, four energies, and the pair of radii each energy allows. Everything on this page is true under every force law that has a well — the body is confined between its turning points and reaches both. What changes from one force law to the next is only how much angle passes between the two visits, and the drawing cannot show it, because the angle is not one of its axes.

Why an absence is the interesting result

A theorem that classifies is usually valued for what it admits. This one is valued for what it excludes, and the pattern is worth naming because it recurs throughout this subject.

The strength of the result is not that the inverse square closes orbits — that was known from the conic sections and is visible in the conserved vector that points at periapsis, whose very existence is the closure written as a constant of the motion. The strength is that nothing else does. Before Bertrand, an unexplained precession could be attributed to a slightly different exponent, and the attribution was not obviously wrong. After Bertrand, any exponent other than 2-2 predicts a precession for every orbit with a magnitude tied to the departure, so one clean measurement of one planet bounds the exponent for all of them.

That is the same structure as the over-determination arguments elsewhere in this collection, arrived at from the other direction. A cluster weighed three ways is convincing because three independent routes agree; this is convincing because one route excludes a continuum. Both replace a fit with a test, and a test is what a measurement has to be able to fail.

There is a last consequence worth drawing out, about what the extra conserved quantity is doing. A general central force conserves energy and angular momentum, which between them reduce the problem to the radial one these essays are built on and no further. The inverse square conserves something more, and so does the spring — a vector in the first case and a tensor in the second — and those extra constants are precisely what pins the orbit’s orientation and stops the apsides moving. Bertrand’s theorem and the existence of that extra constant are two statements of the same fact, and the second is the one that generalises: look for a closed orbit and one finds a conservation law that was not asked for.

Still open: what the next question is

The well has been treated throughout as a fixed curve with a body sliding along it, and the next question is what happens when the curve itself moves — when the mass at the centre changes, or the angular momentum is slowly taken away. The energy is then not conserved and neither is the shape of the orbit, and what does survive is neither of the two quantities this essay has been dividing by. It is the area enclosed in the radial phase plane, it is conserved only if the change is slow, and how slow is slow enough is the whole of the argument.

About the same objects

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

The objects this essay names

Each one links to every other essay that touches it.

Apsidal angleBertrands theoremCentrifugal barrierClosed orbitEffective potentialLogarithmic potentialOrbital stabilityPower law forceRadial periodRosette orbit