Astron. Astrophys. 322, 489-492 (1997)
5. Discussion
5.1. Distance distribution
The inclusion of a spread in the DM in the population
synthesis has two effects on the results of the simulation. The first
is that the DM distribution of the simulated population changes
(see Fig. 2). The second effect is a change of the sample of
simulated pulsars that is retained for comparison with the real
pulsars, because these pulsars are selected on the basis of the
derived distance instead of the actual distance. In the new simulation
both real and simulated pulsars with are placed
at a derived kpc. Pulsars with an actual
distance projected on the Galactic Plane kpc
thus can have a projected derived distance kpc
(see Fig. 3). In fact, at kpc, almost half
of the pulsars in the simulated comparison sample has
kpc. More importantly, the derived luminosity
is based on the derived distance, and is lower than the real
luminosity for pulsars above the electron layer. Thus, the luminosity
distribution derived from the fluxes in the simulation shifts towards
lower values; to compensate for this, a higher intrinsic luminosity
distribution of the pulsars is required. (In terms of Eq. 3 of
Hartman et al. (1997) for the luminosity distribution, the best value
of a changes from 1.5 in their model B to 0.9 in our
model.)
![[FIGURE]](img57.gif) |
Fig. 3. Actual distances projected on the Galactic Plane , as function of actual distance to the Galactic Plane of the pulsars in the sample obtained with Model B of Hartman et al. (1997) with the variations in the DM. The high z pulsars cover a large fraction of the pulsars with large actual distances
|
5.2. Cloud size
Because some of the parameters we use can be derived independently,
we can determine the actual cloud size given by our model. From
EM and DM measurements Reynolds (1991) derived a filling
factor (see also Anantharamaiah &
Bhattacharya 1986). For an average electron density
(e.g. Weisberg et al. 1979) together with the
obtained value of and Eq. 2we find
![[EQUATION]](img62.gif)
Remarkably, this is similar to the sizes of clouds containing both
neutral and ionized hydrogen that have been found by Reynolds et al.
(1995).
From we can check the assumption made in the
appendix, that we can replace with infinity in
the summation over the Poisson probabilities. This is strictly only
possible if , i.e. . From
the filling factor and the equation for L (see Appendix) we
find . However since the Poisson distribution
drops off rapidly, the error in replacing with
in the summations in the Appendix is smaller
than 1 %.
For small distances, and therefore small DM, we make an
error in applying this model since the individual inhomogeneities
become important. However, the sizes of the clouds are relatively
small compared to the scales involved in the simulation
( kpc), and the number of pulsars in our
simulations at distances less than the free path length L is
negligible.
5.3. DM variations in other pulsar simulations
Lorimer et al (1993) model the spread in the dispersion measures
expected at a given distance, by assuming that the logarithm of the
ratio has a Gaussian distribution with width
. (In a model of constant electron density this
is identical to the assumption by Gunn & Ostriker (1970) that the
logarithm of the ratio of real to derived distance of radio pulsars
has a Gaussian distribution.) In the description by Lorimer et al.
(1993) the spread in the DM is roughly proportional to
DM itself. In principle, the relation between DM and
can be derived from the deviation of the
directly measured distances (i.e. by HI absorption, association with
an object of known distance, or parallax) from the distances derived
from the dispersion measure, but in practice the number of accurate
distance measurements is too small.
Because of the wide applicability of the central limit theorem, the
simple model discussed in Sect. 2 suggests that
for a wide variety of models for small scale
structure in the electron density distribution. Our simulations show
that such a variance adequately describes the currently available
observations.
© European Southern Observatory (ESO) 1997
Online publication: June 5, 1998
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