![]() | Annu. Rev. Astron. Astrophys. 2013. 51:
207-268 Copyright © 2013 by Annual Reviews. All rights reserved |
In recent years there has been much progress in updating PDR models, and in combining hydrodynamic simulations, chemical modeling, and radiation transfer codes.
3.1. Photodissociation Regions
Since CO production mainly occurs through ion-neutral chemistry
(van
Dishoeck & Black 1988)
the ionization structure through the PDR
is important in setting the depth of the CO formation. Recombination
of metal ions on PAHs can modify the abundance of free electrons. For
a typical GMC with n ~ 103 cm-3
illuminated by a radiation field ~ 10 times the Galactic ISRF (the
interstellar radiation field in the vicinity of the Sun), the
CO = 1
surface is at a depth of AV ~ 1 when PAHs are
included. Without
PAHs the electron abundance stays high, and the ion-neutral chemistry
is slowed due to H3+
recombination. Consequently, the
CO = 1 surface is
pushed deeper into the cloud
(AV ~ 2). The PAH rates are estimated by
Wolfire et
al. (2008)
by considering the C0 / C+ ratio in
diffuse lines of sight, but there is considerable uncertainty both in
the rates
(Liszt 2011)
and in the PAH abundance and their variation with cloud depth.
Bell et al. (2006)
carry out a parameter study of XCO using
PDR models with constant microturbulent line width.
The calculated XCO versus AV plots
have a characteristic shape with
high XCO at low AV, dropping to a
minimum value at AV ~ 2-4
and then slowly rising for increasing AV. The
XCO dependence at low
AV arises from molecular gas with low CO abundance.
After the CO line intensity becomes
optically thick, XCO slowly rises again as
N(H2) increases.
Increasing density up to the critical density
of CO J = 1 → 0 (n(H2)cr,1 ~
2200 cm-3)
enhances the CO excitation and causes XCO to drop.
In addition, the minimum moves closer to the cloud surface
as does the CO =
1 surface. An increase in XCO by a factor of more than
100 is found when decreasing dust and metallicity to 1% of the local
Galactic ISM, reflecting the larger column of H2 at a given
AV.
Bell, Viti &
Williams (2007)
suggest that the appropriate XCO value to use in
various extragalactic environments can
be estimated from the minimum in the XCO versus
AV plot.
Wolfire,
Hollenbach & McKee (2010)
use an updated version of their PDR models, including a self-consistent
calculation for the median density expected from a turbulent density
distribution. The models provide a theoretical basis for predicting
the molecular mass fraction outside of the CO emitting region in terms
of incident radiation field and gas metallicity. They assume that the
median density is given by < n >med =
exp(µ), where
is the volume averaged
density distribution
1/r, and µ = 0.5ln(1 +
0.25
2)
(Padoan, Jones
& Nordlund 1997).
The sound speed that enters in the Mach
number,
, is calculated
from the PDR model output while the
turbulent velocity is given by the size-linewidth relation (Eq. 9).
As an alternative to PDR models with simple geometries and densities, hydrodynamical models can be used to calculate the line width, and density, but with only limited spatial resolution and approximate chemistry and thermal balance. Glover & Mac Low ( 2007, 2007b) carry out simulations of the formation of molecular clouds using a modified version of the magnetohydrodynamical code ZEUS-MP. They include a time-dependent chemistry, in particular for H2 formation and destruction, and thermal balance. Glover et al. (2010) enhance the code to account for CO chemistry in a turbulent GMC. A turbulent picture of a GMC is not one with well defined clumps surrounded by an interclump medium but one with a continuous density distribution and constant mixing between low and high density regions. The CO abundance varies within the cloud depending on the gas density and penetration of the dissociating radiation field. Calculations of XCO are carried out by Glover & Mac Low (2011), and Shetty et al. (2011, 2011b). The latter two references include non-LTE CO excitation and line transfer in the LVG approximation. These authors carry out 3D turbulent simulations in a box of fixed size (20 pc), and turbulence generated with uniform power between wavenumbers 1 ≤ k ≤ 2, but with various initial densities and metallicities. For their standard cloud model the saturation amplitude of the 1D velocity dispersion is 2.4 km s-1. Each line of sight has a different CO intensity, and CO and H2 column density depending on the past and present physical conditions along it. Thus, for a given N(H2) there is a range in XCO values (see Figs. 5 and 6 in Shetty et al. 2011). The dispersion generally increases for clouds with lower density and lower metallicity.
Figure 7 in
Shetty et
al. (2011)
shows the calculated mean XCO in different
AV bins for several initial densities and
metallicities. The variation in XCO with
AV is qualitatively similar to that shown in
Bell et al. (2006)
for microturbulent models. Lower densities and metallicities
drive XCO to higher values due to lower CO excitation
and CO/H2
ratios respectively. At AV
7 the models with
different initial densities converge as the CO line becomes optically
thick. The minimum in XCO
occurs at larger AV in the hydrodynamic simulations
compared to
the one sided PDR models, likely due to the dissociating radiation incident
on all sides of the box and due to its greater penetration along low
density lines of sight.
A range in density n = 100-1000 cm-3 and
metallicity Z = 0.1-1
Z
produces a range of only XCO,20 ~ 2-10. Thus
although there can be large variations in XCO along
different lines of sight in the cloud the emission weighted
XCO is close to the typical Galactic value
(Section 4). In addition, the low metallicity
case has higher XCO at low AV but
approaches the Galactic value
for higher density (higher AV) lines of
sight. Although the models were run with constant box size, the
dependence on AV suggests
that clouds with sufficiently small size so that CO does not become
optically thick will have higher XCO. The results
seem to confirm the suggestion by
Bell et al. (2006)
that the mean XCO
value should be near the minimum when plotted as XCO
versus AV.
Shetty et
al. (2011b)
investigate the results of varying the temperature,
CO abundance, and turbulent line width. They find only a weak
dependence on temperature with XCO
Tkin-0.5 for
20 K < Tkin < 100 K, and thus over the range of
temperatures typically found in Galactic clouds XCO is
not expected to vary significantly
due to temperature. At low (fixed) CO abundance (nCO
/ nH2 ~ 10-6) , the line does not
become optically thick and thus
W(CO) follows N(H2) with constant
XCO up to at least
logN(H2) = 22.5. Varying the turbulent line
width increases
the CO line intensity as expected since decreasing the self-absorption
allows more CO line emission to escape the cloud. They also find,
however, a decreasing brightness temperature and over the range
of velocity dispersion
= 2-20 km s-1, W(CO) changes
as W(CO)
0.5
instead of changing linearly. The higher turbulent velocities create
dense shocks but also larger voids of low density material. The
competing effects produce a dependence on
that is slower than
linear. Increasing the column density as well as the line width might
produce a model result closer to W(CO)
.
An interesting result is that XCO is not sensitive to the internal velocity profile within the cloud but only to the total line width, however that might be generated. A cloud need not obey a power law size-linewidth relation to have the same XCO as one with a Gaussian distribution and identical dispersion velocity. Thus, clouds need not be "virialized" nor obey a size-linewidth relation to have the same XCO. The modeled XCO converges for high AV clouds and thus the XCO factor is not expected to vary from cloud to cloud as long as the there is a large enough column density. Shetty et al. (2011b) conclude that a nearly constant XCO is the result of the limited range in column densities, temperatures, and linewidths found in Galactic molecular clouds and that applying a constant XCO is approximately correct to within a factor of ~ 2.
Global models of XCO using hydrodynamic simulations to
investigate the variation due to galactic environment are carried out by
Feldmann,
Gnedin & Kravtsov (2012)
and Narayanan et al.
( 2011,
2012).
A significant problem in numerical simulations is how to handle the
physical conditions and/or line emission within regions smaller than
the spatial grid.
Feldmann,
Gnedin & Kravtsov (2012)
use high resolution (~ 0.1 pc) simulations from
Glover & Mac
Low (2011)
for "sub-grid" solutions
to cosmological simulations of 60 pc resolution. These models used
constant Tkin = 10 K, LTE excitation for CO, with
either constant CO line width or one proportional to
mol0.5. By comparing results at
their highest resolutions with those at 1 kpc, and 4 kpc, they asses
the effects of spatial averaging on XCO. The averaging
tends to reduce the variation of XCO on
N(H2) and UV radiation field
intensity. At greater than kiloparsec scales, and H2 column
densities between 1021 cm-2 and 1023
cm-2, XCO
changes by only a factor of 2. They find essentially no variation in
XCO with UV field strength between 0.1 and 100 times
the Galactic ISRF.
Feldmann,
Gnedin & Kravtsov (2012)
do find a significant variation with metallicity,
with a scaling XCO
Z-0.5 for virial line widths. Note
that this relation is much shallower than found by, for example,
(Genzel et
al. 2012,
Section 8.2). The authors suggest
that low metallicity high-redshift galaxies may not obey the same gas
surface-density to star formation relation observed in local disks.
The results of
Narayanan et
al. (2011)
and
Narayanan et
al. (2012)
will be discussed in Section 7.2. Here
we note that their effective
resolution of ~ 70 pc requires adopting sub-grid cloud
properties. Although the surfaces of GMCs more massive than ~
7× 105
M are
resolved, their internal structure is
not. The resulting line and continuum transfer, and temperature and
chemical structure can only be approximate. The resolution problem
also enters in simulations of individual clouds. We showed in
Section 1 that CO becomes optically thick
within a column N(H2)
2-3 ×
1020 cm-2. Thus for
sub parsec resolution ( ~ 0.1 pc) and density greater than
n
103 cm-3, the physical conditions (temperature,
density, and abundances) are averaged over the line forming region and
the calculated emitted intensity can be in error. The resolution
problem is much more severe for H2
dissociation. Self-shielding of
H2 starts within a column of only N(H2) ~
1014 cm-2
(de Jong, Boland
& Dalgarno 1980).
Thus with a resolution of ~ 0.1 pc, and density of n
10
cm-3, the optical depth to
dissociating radiation is already
104 in
a resolution element. A complementary approach is to apply a
state-of-the-art PDR code with well resolved
H2 formation to the output of hydrodynamic simulations
Levrier et
al. 2012.
With increasing
computing power the issues of resolution will continue to improve. We
suggest that high priority should be placed on creating large scale
galactic simulations that are well matched to small scale simulations
with resolved cloud structure. The former provide environmental
conditions and cloud boundary conditions while the latter provide the
chemistry and line emission in a realistic turbulent cloud. Expanding
the library of GMC models with a range of column densities, line
widths, and external heating, and thoroughly checking them against
observations, would be most helpful.