Keep the first velocity correction
Use heliocentric grain velocity and its radial component . To first order in speed divided by light speed, the radiation force adds a velocity-dependent correction to the reduced-gravity equation. The radial correction and the part opposite the full velocity both matter; retaining only a hand-drawn backwards arrow loses the radial term.
The expression describes a small grain with fixed pressure efficiency, in the usual isotropic-rest-frame reradiation approximation. It does not require a warmer afternoon hemisphere. Absorbed solar momentum and reradiation must be transformed consistently between frames; treating isotropic emission in the grain's rest frame as zero momentum loss in the solar frame misses the effect.
Reading: Burns · JPL Solar System Dynamics astronomical parameters
Check the sign with energy and angular momentum
Define specific orbital energy using the reduced gravitational parameter . Differentiate the kinetic and potential terms. The central-force contributions cancel, leaving velocity dotted into the PR acceleration. Every remaining squared speed has a nonnegative sign inside a negative factor.
The torque gives a similarly useful check. Radial forces produce no torque about the Sun. The term opposite the velocity reduces the magnitude of the orbital angular momentum. These identities test an integrator independently of whether its plotted spiral looks convincing.
Reading: Burns · Finson & Probstein
Derive the bound circular clock
For a slowly evolving nearly circular orbit, replace radius by semimajor axis and use the reduced-gravity circular speed. The specific orbital energy is negative reduced gravity divided by twice the semimajor axis. Differentiate with respect to semimajor axis and equate the result to the power above. The reduced-gravity factor cancels, leaving an especially simple inward drift.
Multiply the drift equation by twice the semimajor axis and integrate. The square of the orbital size decreases linearly with time. This is an orbit-averaged approximation for a bound orbit, distinct from a freshly released grain that retained the parent body's faster speed.
Reading: Burns · JPL Solar System Dynamics astronomical parameters
Calculate what can happen in 120 days
For the ten-micrometre teaching grain beta is about 0.0574, so the formal one-AU circular time is about 6,974 years. Over 120 days the fractional orbital-size change is only about twenty-four millionths. A large visual tail made in that time comes from the changed release orbit and launch velocities, not from rapid PR inspiral.
The table follows the same circular law, density and efficiency as chapter one. It is a saved analytic reference; the Lab never increases the drag coefficient to make the effect visible over months. The separate graph changes its time axis to actual years. A direct ten-year integration of the physical PR force checks the orbit-averaged calculation independently.
| Radius (micrometres) | Beta | Formal circular one-AU time (years) |
|---|---|---|
| 1 | 0.574 | 697 |
| 3 | 0.191 | 2090 |
| 10 | 0.0574 | 6970 |
| 100 | 0.00574 | 69700 |
Reading: Burns · JPL Solar System Dynamics astronomical parameters
A thermal lag asks a further question
A rotating solid can emit more thermal radiation from its afternoon side than from its morning side. The resulting recoil depends on a temperature map, rotation direction, obliquity, thermal conductivity and shape. This is the starting point for the diurnal Yarkovsky effect. A seasonal temperature pattern gives another contribution. Neither can be determined from beta alone.
The Lab therefore stops at central pressure and the defined PR reference. The reading guide follows a pinned paper through its thermal variables and astrometric evidence. For a comet, an empirical nongravitational acceleration can also describe asymmetric outgassing. Its fitted transverse component needs a physical interpretation that distinguishes outgassing from thermal recoil.
Reading: Vokrouhlický et al. · JPL Horizons API and observer/vector conventions