A&A 472, 141-153 (2007)
DOI: 10.1051/0004-6361:20042120
The evolution of interstellar clouds in a streaming hot plasma including heat conduction
W. Vieser1, 2 and G. Hensler11 Institute of Astronomy, University of Vienna, Türkenschanzstr. 17, 1180 Vienna, Austria
e-mail: hensler@astro.univie.ac.at
2 Christoph-Probst-Gymnasium, Talhofstr. 7, 82205 Gilching, Germany
(Received 5 October 2004 / Accepted 13 October 2006)
Abstract
Context.The interstellar medium contains warm clouds that are embedded in a hot
dilute gas produced by supernovae. Because both gas phases are in
contact, an interface forms where mass and energy are exchanged.
Whether heat conduction leads to evaporation of these clouds or
whether condensation dominates has been analytically derived.
Both phases behave differently dynamically
so that their relative motion has to be taken into account.
Aims.Real clouds in static conditions that experience saturated heat
conduction are stabilized against evaporation if self-gravity and cooling
play a role. Here, we investigte to what extent heat conduction can
hamper the dynamical disruption of clouds embedded in a streaming hot plasma.
Methods.To examine the evolution of giant molecular clouds in the stream
of a hot plasma we performed two-dimensional hydrodynamical simulations
that take full account of self-gravity, heating and cooling effects and
heat conduction by electrons.
We use the thermal
conductivity of a fully ionized hydrogen plasma proposed by Spitzer
and a saturated heat flux according to Cowie & McKee in regions where the
mean free path of the electrons is large compared to the temperature
scaleheight.
Results.Significant structural and evolutionary differences occur between simulations
with and without heat conduction. Dense clouds in pure dynamical models
experience dynamical destruction by Kelvin-Helmholtz (KH) instability.
In static models heat conduction leads to evaporation of such clouds.
Heat conduction acting on clouds in a gas stream smooths out steep
temperature and density gradients at the edge of the cloud because the
conduction timescale is shorter than the cooling timescale. This
diminishes the velocity gradient between the streaming plasma and the
cloud, so that the timescale for the onset of
KH instabilities increases, and the surface of the cloud becomes less
susceptible to KH instabilities.
The stabilisation effect of heat conduction against KH instability is more
pronounced for smaller and less massive clouds.
As in the static case more realistic cloud conditions allow heat
conduction to transfer hot material onto the cloud's surface and
to mix the accreted gas deeper into the cloud.
Conclusions.In contrast to pure dynamical models of clouds in a plasma and to analytical
considerations of heat conduction that can evaporate such clouds embedded in a hot plasma,
our realistic numerical simulations demonstrate that this destructive effect
of KH instability is significantly slowed by heat conduction so that clouds
can survive their passage through hot gas.
Key words: ISM: clouds -- conduction -- hydrodynamics -- instabilities
© ESO 2007
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