To investigate the stability properties of polar disks we performed
two-dimensional hydrodynamical simulations for flat polytropic gaseous
self-gravitating disks which were perturbed by a central S0-like component. Our
disk was constructed to resemble that of the proto-typical galaxy NGC 4650A.
This central perturbation induces initially a stationary two-armed
tightly-wound leading spiral in the polar disk. For a hot disk (Toomre
parameter Q>1.7), the structure does not change over the simulation time of 4.5
Gyr. In case of colder disks, the self-gravity of the spiral becomes dominant,
it decouples from the central perturbation and grows, until reaching a
saturation stage in which an open trailing spiral is formed, rather similar to
that observed in NGC4650A. The timescale for developing non-linear structures
is 1-2 Gyr; saturation is reached within 2-3 Gyr. The main parameter
controlling the structure formation is the Toomre parameter. The results are
surprisingly insensitive to the properties of the central component. If the
polar disk is much less massive than that in NGC4650A, it forms a weaker
tightly-wound spiral, similar to that seen in dust absorption in the dust disk
of NGC2787. Our results are derived for a polytropic equation of state, but
appear to be generic as the adiabatic exponent is varied between \gamma = 1
(isothermal) and \gamma = 2 (very stiff).Comment: 14 pages including 23 figures, accepted for publication in Astronomy
& Astrophysic