Astron. Astrophys. 342, 233-256 (1999)
6. Time scales and stability
One of the primary purposes of the work presented in this paper is
to examine whether substantial star formation has occurred, or is
likely to occur, in the fingers of the Eagle nebula. The IR
observations indicate that there are no young stellar objects embedded
inside the dense fingertips. This is corroborated by the relatively
narrow line widths present in the molecular line observations,
indicating a lack of outflow activity. By examining the time scales
associated with the various physical processes acting on the clouds,
we hope to create a plausible picture of their eventual fate.
The fingers are estimated to have number densities typically
n(H 2 ) 2
104 cm-3, but in the clumps located near the
tips, the density increases to n(H 2)
2 105 cm-3. For
the purpose of the following discussion, we adopt a simple model for a
dense clump at a fingertip which is assumed to be spherical, with a
radius r = 0.085 pc, and a mass of M
31 .
We further assume that the ionising sources are located 2 pc away from
the fingertip, and produces 2 1050 photons s-1.
It is observed that the peak submm continuum emission from the clumps
is located 0.1 pc deeper into the
fingers than their photoionised front surfaces.
A substantial amount of theoretical work has been carried out to
try to understand the evolution of dense, gaseous clumps that are
being subjected to the ionising radiation of nearby OB stars. A
discussion of propagating ionisation fronts is presented in Spitzer
(1968), and a number of more recent papers have been written on the
subject, though with emphasis on the radiatively driven implosion
(RDI) stage (Bertoldi 1989, Lefloch & Lazareff 1994, 1995), and
the cometary globule stage (Bertoldi & McKee 1990).
The analysis of propagating ionisation fronts indicates that there
are two distinct types, which are characterised by their propagation
speed. The R -type (`Rarified') ionisation fronts travel
through a low density medium with a velocity of
, where c i
= sound speed of the ionised medium. Typically, c
i 11.4 km s
-1. The second type of ionisation front is referred to as
D -type (`Dense'), and these travel through denser gas with a
velocity of , where c
I = the ound speed in the pre-ionised material and
. Often a dense gaseous clump will
not satisfy the conditions necessary for either an R -type or a
D -type front when initially subjected to a strong ionising
source. A front formed under these circumstances is called M-type, and
will result in a shock being driven into the clump (RDI stage), which
compresses the gas until pressure equilibrium between the ionisation
front and the cloud interior is attained. Under these circumstances,
the gas just ahead of the ionisation front is compressed initially by
the preceding shock wave so that an approximately D -critical
ionisation front is able to form (i.e.
) behind the shock front which
continues to compress the cloud ahead of it. The structure of the
cloud during this implosion stage, moving from the cloud surface
towards its interior, consists of a hot, photoevaporating, ionised
region, an approximately D -critical ionisation front, a dense,
neutral post-shock region, a shock front, and then a pre-shocked
neutral region composed of the undisturbed gas in its original state.
Provided that the implosion does not induce the cloud to collapse, the
post-implosion cloud then undergoes a period of slow evolution as the
ionisation front slowly propagates into the cloud.
The high mass stars that provide the ionising radiation are formed
within Giant Molecular Clouds (GMCs). The cloud complexes are observed
to be composed of clumps, with typical densities
103 cm-3, and
radii 1 pc, which are embedded in a
warm, tenuous interclump medium (ICM ). The ignition of an O or
B star causes an R -type ionisation front to propagate out
rapidly through the ICM to the Strömgren radius:
![[EQUATION]](img214.gif)
where n i = particle number density of the
ICM and = the hydrogen
recombination coefficient. The heating of the gas by the ionising flux
leads to temperatures of T i
104 K, and sound speeds of
c i
11.4 km s-1. When the
R -type front reaches a dense clump, it stalls and a shock is
driven into the clump (RDI) until it is sufficiently compressed that a
steady D -type ionisation front may be maintained. It is this
general scenario that we have in mind when making the following
numerical estimates for conditions in the fingers of the Eagle
nebula.
It is necessary first of all to compare the pressure at the surface
of the gas columns with that in their interior, to determine whether
or not shocks are being driven into the heads of the fingers. If the
pressures were approximately equal, it suggests that the fingers had
already been compressed by an ionising-shock front (IS-front).
Conditions in the cloud interior would allow the formation of a steady
D -type ionisation front at the surface, which will slowly eat
into the cloud. If, on the other hand, the external pressure is found
to greatly exceed the internal pressure, we will interpret this to
mean that an IS-front is currently being driven into the columns.
The line widths of the C18O spectra are
= 2 km s-1. The pressure
inside the cloud is composed of both a turbulent and a thermal
contribution, so that
![[EQUATION]](img217.gif)
where T is the temperature,
is the density, µ is
the mean molecular weight, and is
the gas constant. Assuming low temperature cores, then the thermal
component of the line-width is negligible and
=
2 / (8 ln 2)
represents the square of the inferred turbulent velocity in the cloud.
Both the observations and the thermal and chemical modelling, indicate
that the temperature in the interior of the cloud is
15-20 K and the average number
density n (H 2)
2 104 cm-3
However the density in the clumps is estimated to be somewhat larger,
with n(H 2) 2.2
105 cm-3 (these values are similar to those
estimated by Pound 1998). We take the upper value of the internal
density to be n (H 2)
2 105 cm-3,
giving an estimate for the total internal pressure of P
int / = 3.5
107 cm-3 K. The thermal pressure at the tip of
the , estimated by Hester et al.
(1996), is P i / k = 6
107 cm-3 K, which is almost double the internal
pressure. We therefore conclude that equilibrium does not exist
between the cloud surface and the interior, and that an IS-front is
currently propagating into the column (Megeath & Wilson 1997 find
similar values for the pressure difference
( a factor of 2) in the sample of
objects they observed). We further note that the conservation
conditions across a D -critical ionisation front predict that
the pressure just ahead of the front is twice the thermal pressure
just behind the front (i.e. P n = 2 P
i, where the subscripts are n for `neutral'
and Ifor `ionised'. This arises because ionised material leaves
the front at a velocity v i = c
i.
If pressure equilibrium has in fact been attained between the
ionisation front and the cloud interior, and the additional internal
pressure required is provided by a magnetic field, then the field
required is:
![[EQUATION]](img223.gif)
Work presented by Myers & Goodman (1988) indicates that there
is usually an approximate equipartition between the magnetic and
kinetic energies in molecular clouds, so that the turbulent line
widths should be Alfvénic. If a magnetic field is responsible
for providing an internal pressure inside the fingers which is capable
of balancing the pressure at the ionisation font, then it is apparent
that equipartition does not hold, since the Alfvén speed
corresponding to a field of 5.4 10-4 G is v
A = 1.9 km s-1. Alfvénic motions
would then lead to an observational linewidth of:
![[EQUATION]](img224.gif)
which is about twice as large as that observed from the
C18O lines which trace the material in the core.
The pressure of the large scale magnetic field is anisotropic, and
provides a stress that is in a direction perpendicular to the field
direction. Alfvén waves, on the other hand, are able to provide
an isotropic pressure, which is given by:
![[EQUATION]](img225.gif)
where B is the
perturbation to the mean magnetic field associated with the
Alfvén wave. The fluid velocity perturbation associated with
this travelling wave is (from McKee & Zweibel 1995):
![[EQUATION]](img227.gif)
We therefore have the relation:
![[EQUATION]](img228.gif)
where B is the mean magnetic field strength, and
is the Alfvén speed
associated with the mean field. For
, the mean field dominates over the
random field component, and internal stresses provided by the magnetic
field are strongly anisotropic. If this were the case in the Eagle
nebula, then the morphology of the fingers should reflect this
internal, anisotropic pressure. The observations of the fingers, and
of in particular, indicate a
substantial degree of cylindrical symmetry. The direction of
elongation of the fingers points towards the ionising sources, and is
therefore most probably caused by the ionising radiation rather than
by an ordered magnetic field. We therefore conclude that a large-scale
ordered magnetic field does not produce an internal pressure that can
balance the pressure of the ionisation front. A magnetic field in
which the disordered component was comparable to the ordered component
would yield internal motions
since:
![[EQUATION]](img232.gif)
This equipartition of kinetic and magnetic energy is observed in
numerical simulations of MHD turbulence (e.g. Gammie & Ostriker
1996). As described above, these motions would lead to linewidths
4.4 km s-1, which are not
seen in the data. We conclude that there is insufficient internal
pressure in the fingers of the Eagle nebula to balance the pressure at
the ionisation front, and that an ionisation-shock front is currently
being driven into the cloud.
The presence of a shock front currently propagating into the
columns indicates that the dense clumps located towards their tips are
probably not the result of radiatively driven implosion. When an
IS-shock front propagates into a cloud, the shock front precedes the
ionisation front (located at the optical surface of the cloud) by a
small distance. This would preclude it from traversing the top
r 0.2 pc of
, and forming the clump there.
Instead, it seems likely that the dense clumps located towards the
tips of the fingers are part of a larger, dense structure that
pre-existed the expansion of the HII region, but have now come into
stark contrast with their local environment due to the photoionisation
of the surrounding, lower density material. The pre-existence of this
dense structure, and its associated shadowing effect, have probably
contributed to the formation and appearance of the pillars, and the
fact that they point towards the external O-stars.
The shock propagation velocity may be derived from the usual shock
discontinuity jump conditions, leading to the equation
![[EQUATION]](img234.gif)
where and
are the pressure and density of the
shocked, neutral material and P n and
are the pressure and density of the
pre-shocked neutral material. We have no direct knowledge of what to
expect for , since we only know the
pressure and do not have an independent estimate of the density and
sound speed in this region. If we assume that 2
/
then the previous equation may be expressed as:
![[EQUATION]](img241.gif)
where 1
2,
so that the maximum error that we incur in our estimate of V
s, as a result of guessing the value of
, is a factor of
. We take
and
= 2 105 m
(H 2), where m (H 2) is the
mass of a hydrogen molecule, which then leads to a shock velocity of
V s
1.3 km s-1. The time-scale for this shock to propagate
through the top 0.2 pc of the finger tip is then
= 0.2 pc / V
s 1.5
105 years, which is comparable to shock crossing times
derived by Bertoldi (1989) for the dense clumps located in the Rosette
nebula that appear to be undergoing implosion.
These shock crossing times are considerably shorter that the
estimated ages of the O-stars in the Rosette and Eagle nebula (i.e.
1 Myr), indicating that the
structures being observed now (cometary globules or elephant trunks)
have only been exposed to the ionising radiation of the nearby stars
for a relatively short time. An upper limit for the time taken for an
R-type ionisation front to reach the elephant trunks during the
initial expansion of the Strömgren sphere is given by
= (2 pc / 2 c
i) = 8.8 104 years (i.e. a relatively
short time after the switch-on of the O stars). The implication of
this rapid time for the initial expansion of the HII region is that
previously there must have been intervening dense structures shielding
the pillars from the ionising flux of the stars, which have only
recently been eroded away, exposing the pillars to the UV
radiation.
© European Southern Observatory (ESO) 1999
Online publication: December 22, 1998
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