In the proper-eccentricity annulus, averaging over random proper phases cancels the proper vector in the first-order angular variation. The mean line density is proportional to , while the full ring width is independent of angle. Thus at corresponding radial locations
There is a forced-apocentre enhancement in number surface density of a disk, together with the proper-excursion edge profile.
For a narrow aligned eccentric ring with locally constant , its width has the same first-order factor as its line density. Their ratio is constant: the constant-eccentricity aligned ring has no first-order surface-density contrast. It still contains more particles per unit longitude at apoapsis, spread across a wider area.
The more general surface density contrast in an eccentric ring depends on the eccentricity gradient. With a smooth number distribution per unit semi-major axis and aligned apsides,
Hence decreasing can also make the aligned ring apocentre-dense; for it has the same first-order contrast as the proper-phase case. A positive gradient gives a pericentre enhancement. The problem leaves this profile unspecified, so there is no universal observational distinction based solely on the two apse densities.
Resolved ring width and a measured forced-eccentricity profile can distinguish the constant-width and similar-ellipse constructions. Interpreting observed brightness additionally requires the grain temperature, illumination, emissivity, and viewing geometry; brightness is not itself particle number density. Inferences from one contrast alone can therefore be degenerate.

Articles by others on the same topic (0)

There are currently no matching articles.