Sinuous oscillations and steady WARPS of polytropic disks

Details Sinuous oscillations and steady WARPS of polytropic disks Sinuous oscillations and steady WARPS of polytropic disks

May 1995

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1995stin...9534216b&link_type=abstract

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Astronomy and Astrophysics

Astrophysics

Astrophysics, Asymptotic Methods, Centrifugal Force, Disks, Galaxies, Gravitation, Gravitational Fields, Polytropic Processes, Pressure Oscillations, Rotation, Eigenvalues, Equations Of Motion, Integral Equations, Motion Stability, Partial Differential Equations, Pressure Gradients, Torque

Scientific paper

In an asymptotic development of the equations governing the equilibria and linear stability of rapidly rotating polytropes we employed the slender aspect of these objects to reduce the three-dimensional partial differential equations to a somewhat simpler, ordinary integro-differential form. The earlier calculations dealt with isolated objects that were in centrifugal balance, that is the centrifugal acceleration of the configuration was balanced largely by self gravity with small contributions from the pressure gradient. Another interesting situation is that in which the polytrope rotates subject to externally imposed gravitational fields. In astrophysics, this is common in the theory of galactic dynamics because disks are unlikely to be isolated objects. The dark halos associated with disks also provide one possible explanation of the apparent warping of many galaxies. If the axis of the highly flattened disk is not aligned with that of the much less flattened halo, then the resultant torque of the halo gravity on the disk might provide a nonaxisymmetric distortion or disk warp. Motivated by these possibilities we shall here build models of polytropic disks of small but finite thickness which are subjected to prescribed, external gravitational fields. First we estimate how a symmetrical potential distorts the structure of the disk, then we examine its sinuous oscillations to confirm that they freely decay, hence suggesting that a warp must be externally forced. Finally, we consider steady warps of the disk plane when the axis of the disk does not coincide with that of the halo.

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