We investigate the viscous oscillatory instability (overstability) of an un
perturbed dense planetary ring, an instability that might play a role in th
e formation of radial structure in Saturn's B-ring. We generalize existing
hydrodynamic models by including the heat flow equation in the analysis and
compare our results to the development of overstable modes in local partic
le simulations. With the heat flow, in addition to the balance equations fo
r mass and momentum, we take into account the balance law for the energy of
the random motion; i.e., we allow for a thermal mode in a stability analys
is of the stationary Keplerian flow. We also incorporate the effects of non
local transport of momentum and energy on the stability of the ring. In a c
ompanion paper (Salo, H., J. Schmidt, and F. Spahn 2001. Icarus, doi:10.100
6/icar.2001.6680) we describe the determination of the local and nonlocal p
arts of the viscosity, the heat conductivity, the pressure, as well as the
collisional cooling, together with their dependences on temperature and den
sity, in local event-driven simulations of a planetary ring. The ring's sel
f-gravity is taken into account in these simulations by an enhancement of t
he frequency of vertical oscillations Omega (z) > Omega. We use these value
s as parameters in our hydrodynamic model for the comparison to overstabili
ty in simulated rings of meter-sized inelastic particles of large optical d
epth with Omega (z)/Omega = 3.6. We find that the inclusion of the energy-b
alance equation has a stabilizing influence on the overstable modes, shifti
ng the stability boundary to higher optical depths, and moderating the grow
th rates of the instability, as compared to a purely isothermal treatment.
The non-isothermal model predicts correctly the growth rates and oscillatio
n frequencies of overstable modes in the simulations, as well as the phase
shifts and relative amplitudes of the perturbations in density and radial a
nd tangential velocity. (C) 2001 Academic Press.