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Astron. Astrophys. 320, 378-394 (1997)
6. Conclusions
We have provided a detailed spectral investigation of the extended
soft X-ray emission associated with the starburst galaxy M 82.
Point sources have been located and removed from the diffuse wind
emission, and the effects of contamination by the nuclear source
allowed for. The diffuse emission was divided into a set of distinct
regions as a function of distance from the galactic plane, allowing
temperature, emission measure and absorbing column to be derived as a
function of distance along the minor axis. The metallicity was found
to be apparently low (0.00- ) throughout the
wind, in agreement with results from ASCA. This work has shown the
following:
- The observed soft X-ray morphology differs significantly
between north and south, and is not well described as a conical
outflow. The emission extends out to
from the
plane of the galaxy. There is no evidence for any limb brightening, as
would be expected if the soft emission came from the shock heated halo
surrounding the hot wind.
- The emission from the wind is thermal. The temperature drops
slowly along the wind, from
near the nucleus,
to in the outer wind. Numerical models of
galactic winds predict the majority of the emission in the
ROSAT band to be shocked halo, with effective temperatures in
the range .
- Since the entropy of the gas is not constant, at least in the
south, the observed emission cannot originate from a free wind itself.
Our baseline analysis is based on an assumed cylindrical geometry, but
a more divergent geometry only makes the southern wind less
isentropic.
- The emission cannot come from a static halo of gas around
M 82, given that the mass required to bind a hydrostatic halo is
an order of magnitude higher than that inferred from the
HI rotational velocity in the outer disk.
- For reasonable mass and energy input from the starburst, a simple
model for emission from shock heated clouds using the observed density
of the X-ray emitting gas to predict post-shock temperatures is
consistent with the observed temperatures.
© European Southern Observatory (ESO) 1997
Online publication: June 30, 1998
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