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SÉMINAIRE DU LERMA
OBSERVATOIRE DE PARIS
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Vendredi 21 octobre 2005 à 14H


77 avenue Denfert Rochereau, Paris 14



Salle de l'Atelier, Observatoire de Paris





Globular Clusters Dynamics in a Galactic Tidal Field



Paola Di MATTEO

Observatoire de Paris/LERMA



Résumé : Since Shapley's pioneering work, globular clusters (GCs) have played a key role in our understanding of the Universe and of the manner in which our Galaxy formed. They are the best systems for studying stellar dynamics, having relaxation times smaller than their age, so that, at least in the core, stars are expected to have lost memory of their initial conditions. Together with internal processes, also perturbations due to an external field (in particular, shocks due to the passage through the Galactic disk and to the interaction with the bulge) can significantly affect the evolution of a GC. Indeed, it is commonly accepted that the present GC population represents the survivor of an initially more numerous one, depopulated by many disruptive processes.
In the last decade, many observational evidences of the interaction of GCs with the tidal field have been found, suggesting that many GCs are likely surrounded by halos or tails made up of stars that were tidally stripped from these systems. The detection of tidal tails gives not only strong support to the hypothesis that GCs have already lost an important fraction of their mass, probably now deposited in the form of individual stars in the halo of the Galaxy; it is also fundamental to obtain constraints on the GC local orbits, usually unknown unless contemporary available data on proper motions and radial velocities.
In this seminar, I will present and discuss the results obtained by means of detailed numerical simulations of globular clusters orbiting in the tidal field of a triaxial galaxy. In particular, the formation and evolution of tidal tails outside the cluster limiting radius will be investigated, in order to understand to what extent it is possible to reconstruct the GC orbits from the elongation of their tidal streams.