Properties of equilibrium states differing from theoretical
predictions in the interval of negative specific heat were found (see
above). Let us now study the nonlinear structure growth in this
interval for an increased dissipation strength, i.e., outside of
equilibrium, when
.
As previously, a relaxed, unperturbed, confined N-body sphere with
serves as the initial state for the simulations.
In order to dissipate the energy different dissipation schemes are applied. Before we discuss the appearance of long-range correlations in unstable dissipative systems let us briefly discuss the effect of the different dissipation schemes on the global system structure.
The different applied dissipation schemes (see Sect. 3.3)
lead to collapsed phases with different global structures. That is,
they have different mass fractions contained in the core and the halo.
A typical ordering is
,
where
,
and
are the density contrasts
resulting from simulations with a global dissipation scheme, dynamical
friction and a local dissipation scheme, respectively. The density
contrast is,
,
where
and
are the center of mass density and the
peripheric density, respectively. This means that for a global
dissipation scheme almost all the mass is concentrated in a dense core,
whereas a local dissipation scheme can form a persistent "massive''
halo.
The evolution of the mass distribution resulting from simulations with
the different dissipation schemes is shown in Fig. 6.
The collapse of the inner shells takes in all systems about the
same time. Yet, the uncollapsed matter distributed in the halo
is for the global dissipation scheme less than ,
whereas it
is
for the local dissipation scheme.
Next, temporary long-range correlations that develop in unforced
gravitating systems are presented depending on the different
system parameters.
![]() |
Figure 7:
Evolution of the index, ![]() ![]() ![]() ![]() ![]() ![]() ![]() |
![]() |
Figure 8: Evolution of the Lagrangian radii (top) and the specific heat (bottom) for three simulations with global dissipation and different dissipation strength. The dashed line marks the moment, when the system becomes fully self-gravitating. The dash-dotted line indicates the moment when the system enters the zone of negative specific heat. The dotted line marks the "end'' of the collapse. The evolution of the corresponding phase-space correlations are shown in Fig. 7. |
A sufficiently strong global dissipation, i.e.,
,
of a gravitating system leads during the
nonlinear phase of the collapsing transition to fragmentation and
long-range phase-space correlations, so that the index,
,
of the velocity-dispersion size relation,
,
becomes positive.
Figure 7 shows the evolution of the velocity-dispersion-size
relation, i.e., of
for different dissipation strengths. The
relations result from 3 different simulations with global dissipation
schemes and different dissipation strengths. The dissipation strength is
given through the parameter
.
Here
.
This corresponds to
.
![]() |
Figure 9:
Evolution of the index of the
velocity-dispersion-size relation for three simulations with
a local dissipation scheme and different dissipation strengths.
The particle number is
![]() ![]() ![]() ![]() ![]() ![]() ![]() |
![]() |
Figure 10: Evolution of the Lagrangian radii and the specific heat for three simulations with local dissipation and different dissipation strength. The interval of negative specific heat is depicted by the dash-dotted and dotted line. The dashed line marks the moment when the whole system becomes self-gravitating. Figure 9 shows the evolution of the corresponding long-range correlations. |
While the velocities remain uncorrelated in the simulation with
,
becomes temporarily positive over the whole dynamical
range in the simulations with the stronger dissipation.
The velocity correlations start
to develop at largest scales after the system has become
self-gravitating. After the system has entered the interval of
negative specific heat the correlation growth is accelerated.
It attains a maximum and finally disappears when the collapse
ends. The dynamical range over which
during
maximum correlation is
dex.
Correlations at small scales straight above the softening length are stronger for a stronger energy dissipation.
The maximum correlation established in the negative specific heat
interval persists for
and is characteristic for
the applied dissipation strength and softening. For instance, the
simulation with the strongest dissipation develops during
a roughly constant
over a range of 1.5 dex that
resembles Larson's relation. Yet, correlations at small scales
decay rapidly and the index
even becomes
negative at intermediate scales.
The end of the collapse and with it the disappearance of the
correlated velocity structure is marked by a diverging
negative specific heat
.
This is shown in Fig. 8.
Systems with dynamical friction and local dissipation also develop velocity correlations.
Figure 9 shows the correlations resulting from simulations with a local dissipation scheme. Contrary to the global dissipation scheme, a strong local dissipation does not extend the collapse of the whole system. Thus, local friction forces that are strong enough to develop correlations lead also to a fast collapse and correlations accordingly persist a short time compared to simulations with global dissipation.
The corresponding evolution of the Lagrangian radii and the interval of negative specific heat are shown in Fig. 10.
In the dynamical friction scheme, energy dissipation depends, as in the global dissipation scheme, on the absolute particle velocity. Thus a strong dynamical friction extends the gravitational collapse and the "lifetime'' of the correlations. Yet, the observed phase-space correlations are weaker, compared to those appearing in simulations with global and local dissipation, respectively, meaning that the reduced dissipation strength for fast particles, accordingly to the dynamical friction scheme, destroys the correlations.
So far the velocity correlations dependent on the different dissipative factors were studied. Next the effect of different short distance regularizations of the Newtonian potential, removing its singularity, are checked. That is, simulations with and without short distance repulsive forces and with different dissipation strengths are carried out. Energy is dissipated via the global dissipation scheme.
In Fig. 11 the velocity correlations resulting from three
simulations with three different regularizations are compared. The
regularizations are characterized by two parameters, namely, the
softening length
and the parameter
that determines
the strength of the repulsive force. The softening length and
of
the three simulations, compared in Fig. 11, are,
(
,
), (
,
and
(
,
), where
means that a Plummer
potential is applied and
means that short distance repulsive
forces are at work (see Sect. 3.5). The dissipation strength is
for all three simulations the same,
,
and the collapsing
time is consequently the same as well (see Fig. 12).
During the first
long-range correlations resulting
from the three simulations are identical. Then the
starts
to separate. Indeed, the repulsive forces cause an increase of
at small scales, compared to the simulation with the same
softening length, but without repulsive forces. Yet, large scales
remain unaffected.
The index
resulting from the simulation with the large
softening length is larger compared to the other two simulations after
one
.
Also, the
curve is flatter after
that time.
The large difference between the simulation with the long softening
length and the corresponding simulation with the short softening
length is astonishing, because there is a clear deviation even at large
scales. This may be because the two simulations were carried out with the same
particle number,
.
Consequently, the volume filling factors are
different, namely,
and
,
meaning that
for the long softening length, i.e., the large
,
the mass
resolution is greater than the force resolution and vice versa for the
small softening length. Whereas a small volume-filling factor
describes a granular phase, a large volume-filling factor describes
rather a fluid phase. Thus the deviation of the velocity
correlations may mainly be due to the different volume-filling factors
and not due to the different softening lengths.
In order to check this, some complementary numerical experiments are carried out, whose results are presented subsequently.
![]() |
Figure 11:
Evolution of the velocity correlations
for three simulations with global dissipation
scheme and different potential regularizations.
That is, the softening
length and the form of the softening, respectively,
change from simulation to simulation. For ![]() ![]() ![]() ![]() ![]() ![]() |
![]() |
Figure 12: Same as Fig. 10 for three simulations with different potential regularizations, i.e., different softening lengths and forms of the softening potential, respectively. The evolution of the corresponding phase-space correlations are shown in Fig. 11. |
The upper panels in Fig. 13 show the velocity-dispersion-size
relation that develop in simulations with different volume-filling
factors, but equal softening length,
.
The particle
numbers are, N=6400,
and
.
Thus, the
volume-filling factors are,
,
and
,
respectively. The strongest phase-space correlations
appear in the simulation with the highest mass resolution, i.e., for
the "fluid phase'', and weakest correlations appear in the "granular
phase''. The flattest
curve results from the simulation
in which force and mass resolution are equal.
This result suggests that the volume filling factor
(and
not the softening length) is the crucial parameter determining the
correlation strength in simulations with equal dissipation strength,
as long as a substantial part of the system forces stem from
interactions of particles with relative distances larger than the
softening length.
The lower panels in Fig. 13 show, for the same simulations,
the evolution of the index, D(r), of the mass-size relation,
.
The deviation from homogeneity is strongest for
the "granular phase'' and weakest for the "fluid phase''. Thus the
order of the correlation strength in space is inverse to the order of
the correlation strength in phase-space. Such an inverse order is
expected in self-gravitating system with
,
where U is
the potential energy and T is the kinetic energy (Pfenniger &
Combes 1994; Pfenniger 1996; Combes
1999).
The corresponding Lagrangian radii and the interval of negative specific heat are shown in Fig. 14.
![]() |
Figure 13:
Upper panels: Evolution of the
index, ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() |
![]() |
Figure 14: Same as Fig. 10 for three simulations with different volume filling factor. Figure 13 shows the evolution of the corresponding long-range correlations. |
Assuming a constant softening length, different volume filling
factors
imply different particle numbers N that
introduce different Poisson noise,
.
Then, the
statistical roughness of the initial uniform Poisson particle
distribution decreases as
.
Thus the initial roughness of the latter simulations (see Fig. 13)
differ from each other by a factor 2.2 and one might suppose
that the different correlation strengths in these simulations are
the result of the different inital, statistical roughness.
![]() |
Figure 15:
Upper panels: Evolution of the
phase-space correlations resulting from two
simulations with identical volume filling factor,
![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() |
![]() |
Figure 16:
Same as Fig. 10 for two
simulations with identical volume filling factor and
unequal initial roughness, ![]() ![]() |
In order to check this possibility, long-range correlations, resulting
from two simulations with
and with statistical
roughness differing by a factor of
2.2, are compared. The
results are presented in Fig. 15 and the corresponding
Lagrangian radii are shown in Fig. 16. The simulation with
was already presented in Fig. 13. It is now compared
with a simulation with stronger initial roughness.
Despite the different initial roughness, long-range correlations in phase-space are almost identical for the two simulations.
As regards
fragmentation, in addition to the parameters of the
mass-size relation, the mass distributions in space were compared.
We actually find a stronger fragmentation for small particle numbers.
Yet
seems to be the crucial parameter for the
fragmentation strength in Fig. 13.
Consequently, the different correlation strengths in Fig. 13 cannot be accounted for by Poisson noise, but are mainly the result of the different volume-filling factors, or more precisely, due to the different ratio of force and mass resolution. Thus, dark matter clustering in high-resolution cosmological N-body simulations in which the force resolution is typically an order of magnitude smaller than the mass resolution, may be too strong compared to the physics of the system (Hamana et al. 2001).
Here, long-range correlations are discussed that develop in cold,
gravitationally unstable systems without energy dissipation. The
correlation strength appearing in such dissipationless systems depends
on the initial ratio between kinetic and potential energy, a=T/|U|,
i.e., on the number of thermal Jeans masses given through
.
![]() |
Figure 17:
Upper panels: Phase-space correlations
that develop during the free fall of three cold,
dissipationless systems. All systems have the same volume
filling factor,
![]() ![]() ![]() ![]() ![]() ![]() |
This is shown in Fig. 17. For a=0.01 the index
of
the velocity-dispersion-size relation remains zero at small scales
during the entire free fall, whereas for a=0.0 the index becomes
over the whole dynamical range, over a period of
.
That is, 350
are not sufficient to develop
small-scale phase-space correlations in a dissipationless system.
In order to show the dependence of the result on the initial
Poisson noise, the absolutely cold simulation with
is
compared with a
-body simulation. As above, it follows that
the initial roughness of the two systems differs by a factor of
2.2.
Figure 17 shows that the non-equilibrium structures resulting
from the simulations with equal a but unequal particle number differ
from each other during the entire free fall period. Indeed, during the
first half of the free fall time the two initial conditions produce
velocity correlations that differ on small and large scales. After
the differences approximately disappear.
However, the behavior of the spatial correlations (see lower panels of
Fig. 17) is inverse, meaning that differing spatial
correlations appear after
and persist for the
rest of the free fall.
These results suggest that non-equilibrium structures appearing in cold systems or in systems with very effective energy dissipation depend more strongly on initial noise than those appearing in warm systems with less effective dissipation (see also Fig. 15).
The evolution of the Lagrangian radii during the free fall of the cold, dissipationless systems are shown in Fig. 18. Because these systems are adiabatic and self-gravitating during the whole simulation, the corresponding intervals are not plotted in the figure.
Long-range spatial and phase-space correlations appear naturally
during the collapsing phase transition in the interval of negative
specific heat if the energy dissipation time is
so that the time-scale of correlation
growth is smaller than the time-scale of chaotic mixing, which
is
,
where
is the maximum Liapunov exponent (Miller 1994).
Actually, the details of the long-range correlations depend on the
applied dissipation scheme, but there are also some generic
properties. That is, phase space correlations start to grow at large
scales, whereas spatial correlations seem to grow from the bottom-up.
Moreover, there is an upper limit for the index of the
velocity-dispersion-size relation within the dynamical range, namely,
.
Besides the dissipation strength and initial conditions, the volume
filling factor
is a crucial parameter for the correlation
strength. That is, phase-space correlations are strong in the fluid
limit and weak for a granular phase. The behavior of the spatial
correlations is exactly the other way around.
The softening length does not affect correlations within the dynamical range. Yet, sub-resolution repulsive forces affect correlations on small scales above the resolution scale. Of course, this does not hold for the onset of the correlation growth, but only after sufficient particles have attained sub-resolution distances.
The above considerations suggest that the correlations found are physically relevant and not a numerical artifact.
The long-range spatial and phase-space correlations appearing during the collapsing transition are qualitatively similar to the mass-size and the velocity-dispersion-size relation observed in the ISM (e.g. Blitz & Williams 1999; Chappell & Scalo 2001; Fuller & Myers 1992), showing that in the models, gravity alone can account for ISM-like correlations.
Furthermore, the time-scale of the correlation lifetime is the free
fall time,
,
which is consistent with a dynamical
scenario in which ISM-structures are highly transient
(Vázquez-Semadeni 2002; Larson 2001; Klessen
et al. 2000), which is related to rapid star formation
and short molecular cloud lifetimes (Elmegreen 2000),
that is, the corresponding time-scales are about an order of magnitude
smaller than in the classical Blitz & Shu (1980) scenario.
Copyright ESO 2002