The pressureless dust fluid in a shearing sheet has no pressure restoration and is driven by drag force toward the prescribed gas velocity; gas backreaction is omitted in the given model. After linearizing about the common background shear, axisymmetry givesApply to the first equation and use the second to eliminate . The exact linear scalar equation isFor the supplied leading-order epicycle, set . Since and , this becomesThe final cosine term is missing from the printed equation. Dropping it is justified at leading order in , recovering the intended forcing, but the printed equation retains an order- frequency term on the left and is not an exact derivation at that order. A direct countercheck is : the drag vanishes and the pair solves both dust equations exactly, while leaves residual in the printed scalar equation. This is the forced dust epicycle with aerodynamic drag; its damping time is .
For either scalar equation, the complementary solution isso initial velocity transients decay when . In the exact corrected forced dust epicycle with aerodynamic drag, is a particular solution, and the original radial equation then gives . ConsequentlyThis is resonant dust entrainment by an epicyclic gas wave: in the adopted long-wavelength gas approximation, the forcing is a free epicycle of the dust too, so matching the gas makes the drag zero. The convergence holds for every in this linear model; at transients never decay, so the zero-drag and late-time limits do not commute.
If instead the printed scalar equation is treated literally for finite , its particular solution isIt has amplitude and phase offset , not exact phase/amplitude agreement. Agreement in that truncated equation means only leading order as . This distinguishes the intended approximation from a false exact reading of the printed assertion.
There is a further order-of-limits condition: a real finite-wavelength gas wave has . Leading resonant entrainment over the damping time requires , or . Otherwise solve the dust transfer equations at the actual ; detuning can reduce the dust response even though .
Let be the uniform dust background and put . The linearized continuity equation is because background shear has no divergence or axisymmetric advection. Using the late entrained velocity givesThus the coherent travelling wave has maximum fractional excess , and its crest density is when the stationary part is absent. This is the density contrast of an entrained dust wave, and requires in the present linear approximation. Its fractional oscillating density amplitude is the same as the gas's long-wavelength amplitude, so the coherent wave produces no additional dust-to-gas concentration ratio at this order.
Velocity damping alone does not erase the time-independent ; initial density and the history of the forcing are needed to fix it. The printed data therefore determine the travelling-wave contrast, rather than a unique total late-time concentration for arbitrary initial histories. As an explicit example, switch on the prescribed gas epicycle at with initially uniform dust and . The corrected velocity pair gives . Integrating continuity then leavesat late times. It is smaller by order in the stipulated weak-coupling regime, and confirms the stated leading wave-crest estimate while showing why arbitrary stationary density structure is not removed by the velocity transient.
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