For a spherical grain of density , the radiation-pressure coefficient is
The dependence of radiation pressure cancels that of stellar gravity. Here radiation-pressure efficiency includes absorption and the momentum-transfer part of scattering, averaged over the stellar spectrum. In the geometrical optics regime, exceeds the important stellar wavelengths, is of order unity, and : cross-sectional area grows as , whereas mass grows as . Around the stellar wavelength, Mie scattering can produce a broad maximum and material-dependent structure. In the Rayleigh scattering regime, absorption gives , while scattering gives . Thus small absorbing grains approach an approximately constant , whereas nearly transparent grains have . A universal fall to zero at small is therefore inappropriate without specifying the optical properties. The sketch shows both possible small-grain limits; its vertical normalization is illustrative.
Figure 1.
Radiation-to-gravity ratios for absorbing and scattering grains, and the signed angular lag over five dust orbits for beta equal to 0.01 and 0.04
. Details.
Assume release with negligible velocity relative to the planet, negligible planetary gravity after release, and a constant radiation-pressure coefficient. Put and . The inherited speed and specific angular momentum are and . The new specific orbital energy is
For , the dust orbit released from a circular parent ring is an ellipse. Using and gives
For , release is at periapsis, since . At the radiation-pressure blowout threshold, , the orbit is parabolic. For it is hyperbolic: the signed semimajor axis is negative and . For the central force ceases to be attractive, so the elliptical interpretation and the positive-eccentricity formula cannot be extended unchanged.
With measured from release, it is the true anomaly. The polar equation of a Kepler orbit and conservation of specific angular momentum give
Define the signed dust-tail angular lag by , with and both angles unwrapped. For fixed , expansion to first order in gives
so . The dust trails the planet, hence the signed lag is negative. Its slope is ; it decreases monotonically, has horizontal tangents at successive release-direction passages, and has a sinusoidal ripple about . At the end of orbit , and . At five orbits this is for and for . The upper- sketch remains a first-order approximation; its accumulated error is .
For the subsequent positive-distance statements, set . The mean motion of the grain is
A full relative wrap, , therefore takes after averaging over the orbital ripple. During this time Poynting–Robertson drag changes the semimajor axis by
The signed change is negative. This estimate treats as fixed in the rate and computes the drag accumulated over the radiation-pressure wrap time. Since , drag causes little migration over that time. For an arbitrarily tiny , however, this small migration can itself alter the relative phase appreciably: neglecting that feedback on the wrap time additionally requires .
Rapid dust sublimation is a plausible sink near a hot planet: a grain can evaporate long before it completes a relative wrap. Destructive collisions can also remove visible grains. Poynting–Robertson drag alone, with the estimate above, does not explain immediate removal from a short tail. If the destruction time is , a short tail requires roughly .
For a steady dust-tail continuity equation, assume a constant injection rate , grains with the same fixed , negligible release-speed dispersion, and negligible destruction within the segment being calculated. A finite destruction lifetime can terminate that segment, or multiply its density by a survival probability. To first order,
To obtain the explicit trigonometric profile, make the additional secular phase approximation for a dust tail, , discarding the bounded term in the angle-to-age map while retaining the periodic instantaneous drift speed. Then
Since the square is even, the same written profile applies to the signed if number intervals are interpreted with positive orientation. The result is an approximate phase-substitution profile, not a uniformly valid consequence of . The consistent first-order description is instead parametric:
In particular, immediately after release, and , whereas the phase-substitution expression would give . Nor does by itself justify neglecting the orbital ripple. The formal enhancements where are dust-tail caustics; a spread of radiation-pressure coefficients, finite release velocities, and destruction smooth them. With constant lifetime , the parametric profile acquires . These qualifications state precisely the extra assumptions behind the explicit profile.
Assume negligible fragment release speed relative to a circular parent planetesimal. Its initial speed is , but radiation pressure reduces the grain's gravitational parameter to . Its specific orbital energy and specific angular momentum are
For , the resulting dust orbit released from a circular parent ring has
Release is at periapsis: the inherited tangential speed exceeds the new circular speed. Low- grains remain near the dust birth ring; higher bound gives increasingly eccentric orbits extending well outside it. Uniform release longitude produces an approximately axisymmetric dust halo, with long residence times near apoapsis. At the conservative release orbit is parabolic; above this radiation-pressure blowout threshold it is initially unbound. For , zero or repulsive effective gravity also prevents a bound ellipse.
Figure 1. . Left: representative orbits released at one point on the birth ring, including the parabolic release limit. Right: the formal averaged lifetime of bound grains as a function of the radiation-pressure coefficient. Details.
The left panel shows one release longitude; rotating it around the ring fills the halo. At longer times Poynting–Robertson drag also carries bound grains inward, so an initially outward-spanning release distribution does not imply an empty inner region in a continuously supplied, collision-free population.