Quasi-stationary states in the self-gravitating sheet model
Michael Joyce, Tirawut Worrakitpoonpon

TL;DR
This paper investigates the accuracy of Lynden-Bell theory in predicting quasi-stationary states in a one-dimensional self-gravitating sheet model, revealing it works well at low energies but fails at higher energies where core-halo structures form.
Contribution
The study provides a detailed analysis of Lynden-Bell theory's applicability across different energy regimes in the self-gravitating sheet model, highlighting the emergence of degenerate cores when the theory fails.
Findings
Lynden-Bell theory predicts QSS accurately at low energies.
At higher energies, Lynden-Bell theory often fails to describe QSS.
Degenerate core-halo structures are observed when LB theory does not apply.
Abstract
We study quasi-stationary states (QSS) resulting from violent relaxation in the one-dimensional self-gravitating "sheet model", revisiting in particular the question of the adequacy of the theory of Lynden-Bell (LB) to describe them. For "waterbag" initial conditions characterized by a single phase space density, the prediction of this theory is, in this model, a function of only one parameter, which can conveniently be chosen to be the ratio of the energy to that in the degenerate limit. Studying a class of such initial conditions in which the shape of the initial waterbag is varied, we find that the LB predictions are reasonably good always in the low energy region, while at higher energies (i.e. in the non-degenerate limit) they are generally not even qualitatively correct, although certain initial conditions can still be found where they are as good as at low energy. We find notably…
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