A&A 451, 973-980 (2006)
DOI: 10.1051/0004-6361:20054484
N. L. J. Cox1 - M. Spaans2
1 - Astronomical Institute "Anton Pannekoek'', Universiteit van Amsterdam, Kruislaan 403, 1098-SJ Amsterdam, The Netherlands
2 -
Kapteyn Astronomical Institute, University of Groningen, PO Box 800, 9700-AV Groningen, The Netherlands
Received 7 November 2005 / Accepted 27 January 2006
Abstract
Context. The unidentified diffuse interstellar bands (DIB) are observed throughout the Galaxy, the Local Group and beyond. Their carriers are possibly related to complex carbonaceous gas-phase molecules, such as (cationic) polycyclic aromatic hydrocarbons and fullerenes.
Aims. In order to reveal the identity of the DIB carrier we investigate the effects of metallicity, radiation field and extinction curve on the PAH charge state distribution, and thus the theoretical emergent PAH spectrum, in diffuse interstellar clouds. This behaviour can then be linked to that of the DIB carrier, thus giving insight into its identity.
Methods. We use radiative transfer and chemical models to compute the physical and chemical conditions in diffuse clouds with Galactic and Magellanic Cloud types of interstellar dust and gas. Subsequently, the PAH charge state distributions throughout these clouds are determined.
Results. We find that the fraction of PAH cations is much higher in the Magellanic Cloud environments than in the Milky Way, caused predominantly by the respective lower metallicities, and mitigated by the steeper UV extinction curve. The fraction of anions is much lower in a low metallicity environment. The predicted DIB strength of cationic PAH carriers is similar to that of the Milk Way for the LMC and 40% for the SMC due to the overall metallicity. Stronger DIBs could be expected in the Magellanic Clouds if they emanate from clouds that are exposed to an average interstellar radiation field that is significantly stronger than in the Milky Way, although photo-destruction processes could possibly reduce this effect, especially for the smaller PAHs. Our results show that the presence and absence of DIB carriers in the Magellanic Cloud lines of sight can be tied to the PAH charge balance which is driven by metallicity, UV radiation and dust extinction effects.
Key words: astrochemistry - ISM: clouds - ISM: dust, extinction - ISM: molecules - ISM: lines and bands - Magellanic Clouds
In the last decade complex carbonaceous molecules (e.g. carbon chains, polycyclic aromatic hydrocarbons and fullerenes) have become viable candidates for the carriers of the numerous, as of yet unidentified, diffuse interstellar bands (DIBs). Observations of infrared characteristics of C-H and C-C stretching and bending modes in PAHs have added to the believe in this hypothesis. Since their discovery (Heger 1922) many carriers have been put forward, but none have been confirmed (see e.g. Herbig 1995 for a review).
Early observations of extra-galactic DIBs had to focus on the very broad, shallow, but strong 4430 Å DIB, but recently it has become feasible to observe the strongest narrow DIBs in Magellanic Cloud lines of sight (e.g. Ehrenfreund et al. 2002) and even beyond toward supernovae in nearby galaxies (Sollerman et al. 2005). This allows for a study of the effects of, for example, metallicity on the DIB carrier formation and destruction processes. Detailed analyses of the DIBs and the interstellar medium (ISM) of our nearest neighbours, the Large and Small Magellanic Clouds, show DIB behaviour that is similar to the MW in some sightlines while different in others (Cox et al. 2006b,a; Welty et al. 2006).
To understand the life cycle and evolution of the DIB carrier(s) we need to grasp some of the complexity of the chemistry and physics of the ISM. Unfortunately, there are still many caveats in our understanding of the chemistry in the diffuse interstellar medium, both in the Milky Way and beyond. The effect of one of the fundamental differences between galaxies in the Local Group, i.e. their metallicity, warrants further examination. Metallicities have been discussed for photo-dissociation region (PDR) models, see e.g. Maloney & Black (1988), Van Dishoeck & Black (1988), Wolfire et al. (1989), Maloney & Wolfire (1996), and for a more specific application to the LMC, see e.g. Pak et al. (1998), Kaufman et al. (1999), Stutzki (2001), Jeyakumar & Stutzki (2003). From these studies it has become clear that the metallicity affects the local physical and chemical conditions. To apply the cloud chemistry models designed for Milky Way lines of sight to other galaxies we need to take into account several fundamental differences in the nature/composition of the ISM in these external galaxies. Besides the decrease in metallicity (and related to that the decrease in the dust-to-gas ratio), these galaxies also differ in the gas and dust composition, i.e. the extinction curve, as well as the interstellar background UV radiation field.
The relative abundance deficiencies, compared to the local ISM, are
-0.3 dex (Rolleston et al. 2002, and references therein) and
-0.6 dex (Lee et al. 2005 and references therein) for
the LMC and SMC, respectively. The (dust) extinction properties differ
between the MW, LMC and SMC. For example, on average the LMC and SMC
gas-to-dust ratios are about 4 and 10 times higher than in the MW,
respectively (e.g. Bohlin et al. 1978; Gordon et al. 2003;
Cartledge et al. 2005).
Recent results by Misselt et al. (1999) and Gordon et al. (2003)
showed that lines of sight toward 30 Doradus have a rather steep FUV rise,
and a weak 2175 Å bump (often related to carbonaceous material), whereas the
rest of the LMC has extinction curves much more like those observed in our Galaxy.
However, only four SMC extinction curves have been
constructed thus far, of which one (AzV 456) does show a bump and a weak FUV rise (Rocca-Volmerange et al. 1981; Prevot et al. 1984;
Gordon et al. 2003; Cartledge et al. 2005), and includes DIBs.
Ruiterkamp et al. (2005) investigated the PAH-DIB hypothesis (Van der Zwet & Allamandola 1985; Leger & D'Hendecourt 1985) by deriving how the charge state distribution for different (large) complex carbonaceous molecules (i.e. PAHs in this study) is determined by the local diffuse interstellar cloud conditions, such as e.g. the temperature (structure), the electron and hydrogen density, the UV field and the optical extinction within a diffuse cloud (similar to the treatment of PDRs by Bakes & Tielens 1998). They compared the resulting theoretical PAH absorption spectrum to the observed DIB spectrum for the translucent line of sight toward HD 147889, and showed that the strong DIBs, if indeed PAHs, are probably related to specific series of PAHs that have strong cationic electronic transitions.
The aim of this paper is to quantify the effect of metallicity, (dust) extinction properties and the interstellar radiation field on the cloud chemistry in general, and the PAH charge state in particular. In Sect. 2 we outline our previously constructed diffuse cloud model (Ruiterkamp et al. 2005), and the incorporation of the metallicity/elemental abundances. The next section describes first the results for clouds with Galactic type dust but different metallicities (Sect. 3.1) and for the low metallicity ISM in Magellanic Cloud type environments (Sect. 3.2). Section 4 shows how these different environments affect the emerging diffuse cloud PAH absorption spectrum. We discuss the consequences for the PAH-DIB carrier hypothesis in Sect. 5, and conclude with an application of the results to two well studied SMC sightlines that probe two very different interstellar diffuse cloud environments.
The PAH charge state distribution is determined by the reaction rates for
photo-ionization, electron recombination,
electron attachment and photo-detachment.
These reactions depend on the local interstellar conditions (e.g. temperature T,
electron density
,
hydrogen density
and effective strength of the interstellar radiation field
), as well as the properties of the considered molecule, e.g.
the size (the number of carbon atoms
)
and the ionization potential (IP).
We refer to Ruiterkamp et al. (2005) for the details on the adopted reaction rates.
The basic properties (i.e.
and IP) of the selected PAHs (one kind of
large carbonaceous molecules) are listed in Table 1.
Models for the chemical and thermal balance of the considered diffuse clouds (single-sided irradiated slabs) were constructed using the Monte Carlo code as described in Spaans (1996) and Spaans & Van Dishoeck (1997). This code solves the gas phase chemical network and is driven by ion-molecule reactions, typical for diffuse clouds. Although the code does not include grain surface chemistry, dust is included as it causes the attenuation of the interstellar radiation field. Subsequently, the PAH charge state distribution is computed as a function of depth into the cloud.
Table 1:
Basic properties of the selected PAHs: ionization potential IP (eV)
and number of carbon atoms
.
The two adopted types (1) and (2) correspond to two PAH symmetry groups (i.e.
geometric structure) (D6h coronenes and D2h acenes) that have a different IP-
dependence. Type (2) PAHs are more easily ionized than type (1).
See also Fig. B.1. in Ruiterkamp et al. (2005).
We assume a generic electron affinity of 3 eV, and a sticking coefficient of unity.
Carbon and oxygen are important elements in the chemical network.
Ionized carbon and carbon monoxide are the most critical species in the cooling,
while the dust abundance is critical in heating the interstellar gas (i.e. lowering
the dust grain abundance reduces the heating rate).
Generic PAHs are also included in the chemical network and the thermal
balance, with an abundance
for Solar
metallicity (Bakes & Tielens 1998).
A lower C and O abundance makes it harder to sustain cool phase gas.
This also happens when the UV radiation field is high (Wolfire et al. 1995).
A lower dust abundance, and hence lower H2 formation rate and higher UV field
intensity may cause H I to dominate over H2 even in regions with higher
density (compared to the MW).
This indicates that in the Magellanic Clouds H I absorption traces not only
diffuse, but also denser clouds.
These dense clouds remain atomic in the Magellanic Clouds, but would be molecular
in the Milky Way (Dickey & Garwood 1989).
The electron density is approximately related to the metallicity and the
dust-to-gas ratio, via:
Stutzki (2001) concluded that N(dust)
Z, and thus the same
is reached at a larger
column.
The
/
ratio drives the charge balance. The shape of
(
)
is independent of the dust-to-gas ratio, but
,
(=
)
and T are a function of
(for a given
),
the unattenuated interstellar radiation field and the observed extinction
curve. Jeyakumar & Stutzki (2003) conclude that for their PDR model (spherical
cloud,
cm-3) the surface temperature is affected by Zonly for strong UV fields, log
> 1, whereas for weak fields,
log
< 1, no change is predicted. This is consistent with our
models that show a variation of the surface temperature and temperature structure
with metallicity for UV field strengths of
= 1 and 10, with
= 100
and 300 cm-3 (Table 2).
In terms of
both cases are equivalent.
The charge state of PAHs is (roughly) proportionally to
(
), which depends on the
availability of electrons for recombination, and is extinction dependent.
See also Sect. 3 and Fig. 2.
The main source of electrons, for strong UV fields, is the ionization of
neutral carbon. At the cloud surface all the neutral carbon is ionized,
therefore,
.
Kaufman et al. (1999) show that for a weak radiation field (i.e.
/
)
the C+ is destroyed by collisions with neutral
and anion PAHs. The abundance of neutral and anion PAHs increases with C(and thus Z) because there are more gas phase electrons. Therefore, the
C+ abundance per Z increases if Z decreases.
Table 2: Diffuse cloud physical parameters for the four distinct cloud configurations A, B, C and D. Each of these configurations consists of a single-sided irradiated slab with specified extinction properties and metallicities (for detailed discussion see main text, Sects. 3.1 and 3.2).
![]() |
Figure 1: The top left and right panel show the electron abundance structure for the diffuse cloud types B and C, respectively. The respective basic cloud parameters are listed in Table 2. For each cloud type we show the results for different extinction curves and metallicities (Sects. 3.1 and 3.2). The bottom panels show the corresponding temperature structures. The local temperature and electron density are important for the charge state balance, and their extinction dependency is crucial to solve the PAH charge state throughout the diffuse cloud. Note the difference in electron density and temperature structure (as a function of extinction) between the two models B and C. |
| Open with DEXTER | |
![]() |
Figure 2:
|
| Open with DEXTER | |
First we construct a small grid of diffuse clouds (a single-sided irradiated slab model,
Spaans 1996) with typical Milky Way properties.
We fix
= 100 or 300 cm-3,
= 1.0 or 10.0 (see Table 2).
The visual extinction
,
from the illuminated side of the slab to the dark side of the
slab is set to 2.0 mag.
We construct the models for the typical Galactic extinction curve, parametrized by
= 3.1
(Fig. 3, adopted from Fitzpatrick 1999,2004)
for a range in metallicity, Z = 1.0, 0.5 and 0.1
.
Figure 1 shows the electron density (top panels) and temperature
(bottom panels) structure within the two cloud types B and C, for
the different metallicities Z with Galactic type (dust) extinction.
The electron and density structure for cloud types A and D are not
shown, since they are quite similar to cloud types B and C, respectively.
In addition, Fig. 2 shows the extinction dependent charge balance indicator
(Sect. 2) for all four cloud types.
These results for the diffuse cloud physical conditions are subsequently used to
calculate the
dependent PAH charge state distribution.
The charge state fractions of cations, neutrals and anions, as a function of
,
for the Galactic B and C cloud types (A and D omitted, but
again very similar) are shown in Fig. 4.
The effect of a decrease in metallicity on the total integrated charge state
distribution is discussed in detail in Sect. 4.
![]() |
Figure 3: Extinction curves adopted for the MW, LMC and SMC environments. Galactic extinction curve (dashed) adopted from Fitzpatrick (1999, 2004). Magellanic Cloud extinction curves (solid) adapted from Gordon et al. (2003) and Cartledge et al. (2005). |
| Open with DEXTER | |
Now we apply the above results on the metallicity effects to diffuse clouds
in the Large and Small Magellanic Clouds.
However, before this can be done, there are two main points that need to
be taken into account.
First, we need to adopt a value for the overall metallicity and the gas
phase metal abundance of the interstellar medium (ISM) in these Galaxies.
We adopt Z = 0.25
and 0.10
for the LMC and SMC,
respectively.
Second, the model calculations will be affected not only by the metallicity
but also by changes in the gas and dust composition.
The appropriate extinction curves (
/
)
for the LMC
(LMC-2 and LMC-av) and SMC (SMC bar and SMC wing) are those derived by
Gordon et al. (2003) and further extended by Cartledge et al. (2005).
The adopted extinction curves are shown in Fig. 3.
For each of these Magellanic Cloud extinction properties we calculate
the charge state distribution for each of the four cloud types defined
in Table 2.
The extinction dependent ionization distribution for four specific PAHs
(Table 1) is shown in Fig. 4 for the
scenarios B and C, for each of the four Magellanic Cloud extinction and metallicity properties.
![]() |
Figure 4:
Charge state distribution of PAHs as function of visual
extinction |
| Open with DEXTER | |
![]() |
Figure 5:
Total (fractional) charge state distribution for cloud types X(
|
| Open with DEXTER | |
How do the radiation field, the metallicity and the (dust) extinction properties affect the PAH charge balance, and subsequently the PAH absorption spectrum? In order to compare the derived model results with observations, the charge state distributions need to be averaged over the line of sight. The total (integrated) fractions of anions, neutrals and cations for the different scenarios and environments (MW, LMC and SMC) are shown in Fig. 5. Next we discuss the effect of the different environmental model parameters on the charge balance.
Increasing the strength of the radiation field
increases the PAH ionization rate. For the investigated scenarios for diffuse clouds in the
Galaxy and the Magellanic Clouds the results from Sect. 3.2
show that a tenfold increase of
greatly enhances the fraction of cations
and prohibits the presence of anions (fraction less than 0.5%).
For thin diffuse clouds (
= 1.0 mag) the PAH cation fraction is larger than 90
and 80% for scenarios B (
= 100,
= 10) and D
(
= 300,
= 10), respectively.
For slightly thicker clouds (
= 2.0 mag) the fraction of neutral PAHs
(still no anions) increases up to 20 and 40% for scenarios B and D, respectively. However, for larger PAHs the neutral fraction decreases
again. For scenarios A (
= 100,
= 1) and C
(
= 300,
= 1) the differences are more pronounced. Therefore,
in the remainder of this section we will focus on the results for these
scenarios which are summarized in Fig. 5.
Note that all high energy UV photons are assumed to ionize PAHs,
as photo-dissociation processes are not included.
For diffuse clouds exposed to a strong (
= 10) radiation field the
high energy photon flux could potentially lead also to the destruction of,
mostly small, PAHs (see also Sect. 5).
For the Galactic diffuse clouds (Fig. 5), scenarios A and C show that a decrease in metallicity causes an increase in the cation fraction. This results directly from Eq. (1) which constitutes a proportionality between metallicity and the electron density. A lower electron density will result, all other parameters being equal, in a lower recombination rate, a lower electron attachment rate and thus a higher ionization fraction.
Let us consider the charge state fraction for a PAH with 20 carbon atoms
and an ionization potential of 7.6 eV (i.e. PAH #1, Table 1).
For scenario C we have a relatively dense model cloud
(
= 300 cm-2) which is irradiated by a relatively weak UV field (
= 1).
The radiation is attenuated throughout the cloud (
= 2.0 mag) by Galactic type dust.
For a gas with solar abundance the PAH cations, neutrals and anions constitute 2, 47
and 51% (3, 42 and 55%, respectively halfway through the cloud) of the
total PAH column density. For regions with a lower metallicity (e.g. 0.1
)
the anion fraction decreases to 7%, while the neutral and cation fractions both increase to 68 and 25%.
For larger PAHs (NC > 40) the neutral fraction first increases with
decreasing Z, but then decreases again as the cation fraction increases strongly,
more than linearly, with decreasing Z.
Due to the low metallicities, the Magellanic Cloud diffuse clouds show low
anion and large cation fractions, similar to the low Z Galactic clouds.
The effect of dust extinction properties is discussed next.
Introducing Magellanic Cloud dust extinction properties into the lower
metallicity diffuse cloud models (Z = 0.25 and 0.10
)
changes
the distribution of photons penetrating the cloud and thus changes the
ionization balance.
The results are shown in Fig. 5.
Differences arise in charge state fractions between the MW Z = 0.1
,
SMC-wing and SMC bar cases, which differ in the adopted
extinction curve. The small anion contributions (0 to 7%) differ less than 3%.
The neutral fraction for both SMC extinction curves differs between 2 and 14%,
and the cation fraction between 3 to 14%. Compared to the MW the SMC differ even more;
the cation and neutral fractions are up to 15% higher and lower, respectively.
There is little difference between the two LMC extinction curves, i.e. 1 to 6% differences.
The more efficient attenuation of the far UV flux by the SMC dust
(both bar and wing) results in a lower ionization fraction than that expected
solely from the lower metallicity.
Although the SMC bar and wing extinction curves differ in shape the overall
ionizing radiation penetrating the dust results in a similar level of ionization.
On the other hand, the bar region is exposed to relatively more high energy
(>11 eV) photons which are more prone to photo-dissociate PAHs (Sect. 5).
On the other hand, these high energy photons are much more attenuated by the
dust in the SMC than in the LMC or MW. Thus, for similar
and
the PAHs are more protected against ionization and destruction
in environments with SMC-like dust extinction properties (i.e. extinction curves).
The electron density is directly related to the metallicity (Sect. 2.2),
and the electron recombination rate is lower for lower metallicity environments,
which results therefore in a higher ionization fraction.
From the above it is already clear that the differences between
= 100 and 300 cm-3
are subtle, the latter showing an overall larger fraction of anions and neutrals.
The difference between "little'' extinction (
= 1.0 mag, diffuse cloud) and "high''
extinction (
= 2.0 mag, translucent cloud) clouds is similar,
in that the total fraction of neutrals increases for higher
due to a higher fraction
of neutrals towards the dark side of the slab.
In practice, the observed (in the optical spectral range) diffuse cloud lines of sight
in the LMC and SMC have visual extinctions less than one magnitude.
If indeed the DIB carriers are complex carbonaceous molecules, and more specifically, fullerenes or polycyclic aromatic hydrocarbons (PAHs) the DIB band strength should vary with their abundance along the line of sight. If furthermore the DIB carriers are PAHs or fullerenes in a certain charge state (e.g. anion, neutral or cation) then their abundance would vary with local interstellar conditions along the observed line of sight, due to shifts in the charge state balance. The total integrated PAH column density along the line of sight then directly yields the corresponding DIB strength. In practise, most lines of sight probe multiple diffuse clouds, each of which can have different environmental conditions that result in both a different total PAH column density and a specific PAH charge state balance. Nevertheless, several conclusions can be extracted from the results described above.
The total charge state fractions imply that
the fraction of PAH cations is much higher in the Magellanic Cloud environment
(due to the low metallicity) than in the Milky Way (solar metallicity).
The dust extinction properties specific for the LMC and SMC, i.e. increased
attenuation of high energy photons, counter the effect of lower metallicity
and thus (slightly) mitigate the ionization level.
The fraction of anions is much lower in the low metallicity environment.
The carbon abundance, with respect to solar, is on average
a factor 4 and 10 lower for the LMC and SMC, respectively.
Thus, although the cation fraction for, for example, PAH #7 (
= 100, IP = 5 eV)
increases from 20 to 60% between MW and LMC, the PAH cation column density
in the LMC is still only 3/4 of that in the MW (for a diffuse cloud with identical
visual extinction, hydrogen density and impinging UV radiation field) assuming that
the total PAH column density scales with the carbon abundance and thus metallicity.
For the SMC the cation fraction for this PAH is 75%, thus the cationic PAH column
density is a factor two lower than in the LMC, and 3/8th that of the MW.
In Fig. 6 we show the predicted PAH band strength,
i.e., the cation fraction multiplied by metallicity integrated up to a certain
(
), as a function
of that visual extinction
.
The band strength is shown for the diffuse clouds of types B and C
with MW, LMC and SMC metallicities.
The strength of an optical thin absorption line, e.g. a DIB, is directly proportional
to the carriers column density (which is proportional to the carbon abundance,
the relative PAH abundance and the fraction of cations).
In this scenario one would expect DIBs in the LMC and SMC to be about 1.3
and 2.6 times weaker (per
)
than in the MW.
Stronger DIBs could be expected in the Magellanic Clouds if they
emanate from clouds that are exposed to an average interstellar radiation
field that is significantly stronger than in the Milky Way; if the total
extinction of the cloud is reduced; or
if the carbon abundance along a particular line of sight is higher,
for example indicated by a higher dust-to-gas ratio. Vice versa, weaker DIBs
can be caused by a weak UV field and/or lower metallicity, and thus lower PAH cation abundance.
A stronger UV field,
= 10, would result in a high cation fraction of 75
to 100%, subsequently resulting in SMC DIB strengths half those for the MW,
and LMC DIB strengths similar (or even slightly enhanced) to those observed in
the MW, despite the lower metallicity of the ISM. Thus, if DIBs were detected
in similar (regarding metallicity, density and extinction) interstellar
environments, and their carriers would be a PAH-like molecule, then their ratio
is a measure of the relative strengths of the effective UV field penetrating
the clouds.
Recent studies by Cox et al. (2006b,a) and Welty et al. (2006) show that indeed there
are environments within the LMC and SMC where DIBs have strengths similar to those
observed for Galactic UV dominated diffuse clouds, as well as those
where DIBs are very weak or even absent, typical for shielded Galactic diffuse clouds.
It is therefore important to obtain information on
the strength of the UV field permeating the Magellanic Clouds.
excitation
can be used to get a handle on the
/
ratio
(Black & van Dishoeck 1987). Also, if present, C2 rotational lines can be
used to independently derive
(Van Dishoeck & Black 1989). Possibly, more
stringent results could be obtained from detailed modelling of specific
Magellanic Cloud diffuse lines of sight.
However, currently, the information available is not sufficient to adequately
constrain the hydrogen density and the temperature structure. Additionally, reality
is more complex, and most sightlines probe a complex of individual or connected
interstellar clouds.
![]() |
Figure 6:
PAH cation band strength, i.e., the cation fraction multiplied by
metallicity integrated up to a certain |
| Open with DEXTER | |
In the models presented above we refrained from introducing additional PAH destruction and formation processes, such as (de)hydrogenation,
fractionation, C2H2 and Cn photo-dissociation and C+ addition.
These processes are not well understood for the
large carbon molecules, such as PAHs and fullerenes, considered here.
Destruction of carbonaceous molecules by removal of carbon is likely to be important only
for small, i.e. less than 20 carbon atoms, molecules.
For large PAHs, more than 30 carbon atoms, the effective photo-dissociation drops rapidly with size
(Allain et al. 1996a,b; Le Page et al. 2001,2003).
Furthermore, the photo-ionization rate is competing with the
bond destruction rate for suitable photons.
Predictions by Le Page et al. (2001)
suggest that C2H2 photo-dissociation rates rapidly drop with increasing PAH size,
for hydrogenated PAHs between 20 to 100 carbon atoms exposed to a standard interstellar radiation field and typical diffuse cloud conditions.
For dehydrogenated PAHs (which may occur for strong UV fields) the photo-dissociation
is more efficient and C2H2 loss may also become important for larger (
) PAHs.
Allain et al. (1996a,b) predict that most PAHs with less than 50 carbon atoms are
destroyed through C2H2 ejection which only requires about 5.5 eV.
Note that this is more than is required for H and H2 loss (
4-5 eV) which is
the preferred photo-dissociation process.
In addition, C2H2 loss is higher for catacondensed PAHs than for
the peri-condensed PAHs, i.e. UV photons convert open structures to compact structures.
Loss of a C, C2 or C3 requires activation energies of about 7 to 8 eV (Leger et al. 1989),
which is significantly higher than the energy required for H loss (about 5 eV).
Large PAHs (
)
are photostable as they can redistribute photon energies efficiently,
and can remain in their normal hydrogenation state even for radiation fields of
= 100
(Le Page et al. 2001).
PAH anions are more sensitive to loss/abstraction of small hydrocarbons than PAH neutrals or cations.
If sufficiently present C+ addition can (partly) balance the carbon photo-dissociation processes.
Two photon PAH destruction processes are considered to contribute significantly for radiation
fields
> 103. Again, experimental data for these processes is only
available for smaller (up to 20 carbon atoms) PAHs. To understand the importance
of photo-dissociation of carbon atoms from large PAHs and fullerenes there is a great need for theoretical calculations and/or experimental laboratory data.
Madden et al. (2005) found that for dwarf galaxies the PAH band strength (normalized to the number of very small grains) is proportional to their metallicity, possibly because of the hardness of the radiation field, or alternatively the lack of PAH producing AGB stars. Vermeij et al. (2002) studied the infra-red PAH emission from H II regions in the LMC and SMC and inferred that PAHs with an open uneven structure are dominant in Galactic and non-30 Dor LMC H II regions, while compact PAHs are dominant in 30 Dor and SMC H II regions, in line with a strong UV field impinging these regions. Obviously, the environments probed by these studies differ in many ways (extinction, density, UV field strength) from the diffuse medium studied in this work, and one should take caution when comparing.
Within the SMC there are two distinct types of diffuse sightline.
The lines of sight towards the SMC bar (e.g. AzV 18) show no UV bump,
a strong far UV extinction, and no DIBs, whereas, the (only) line of sight
towards the SMC wing (AzV 456) shows the UV bump, a flatter MW like
far-UV extinction and DIBs strengths similar to those observed in the Galactic
-type diffuse cloud toward HD 149757.
Dust extinction properties are well known for lines of sight towards the early
type SMC stars AzV 456 and AzV 18 (Gordon et al. 2003; Cartledge et al. 2005).
Both sightlines have a similar visual extinction
of 0.57 and 0.49 mag, respectively (Table 3).
The line of sight towards AzV 18 has a gas-to-dust ratio about 3.5 times that towards
AzV 456; 19.3
1021 and 5.6
1021 cm-2 mag-1, respectively.
Additionally, they differ in the observed molecular hydrogen fraction f as well as
the
excitation temperature:
= 0.045 and 0.525,
and
175 K and 270
52 K for
AzV 18 and AzV 456, respectively (Cartledge et al. 2005).
The H2 formation rate is proportional to
,
with
.
The H2 abundance is thus determined by the dust abundance and
the ratio
/
.
Hence, it seems plausible that the high H2 fraction toward
AzV 456 compared to AzV 18 is a direct consequence of the larger
dust-to-gas ratio and a lower
toward the former.
If the metallicity Z increases (as indicated by the dust-to-gas ratio),
then the cation fraction decreases, resulting in a predicted DIB strength ratio between AzV 456 and AzV 18 of about 3 for a cationic PAH carrier, all other physical parameters being the same.
The ratio for a specific DIB in these two SMC lines of sight may be further
influenced most significantly by the ambient
because the differences in temperature and hydrogen density are small.
Table 3: The reddening, ratio of the total-to-selective visual extinction, visual extinction, atomic gas-to-dust ratio, molecular gas-to-dust ratio and the total hydrogen gas-to-dust ratio are given for the diffuse interstellar SMC clouds in the lines of sight towards the bar star AzV 18 and the wing star AzV 456.
Note then that DIBs of almost Galactic strength have been observed along the
line of sight towards AzV 456, while not towards AzV 18.
If the DIBs towards AzV 18 would indeed be at least a factor of three
weaker with respect to those toward AzV 456 then they could have
remained undetected up to now, as current upper limits on equivalent widths are
only half those of DIBs observed for the Galactic
-type sightline
toward HD 149757 (Cox et al. 2006b).
If upper limits would be observed below the level of the above predicted strength this would
hint strongly towards unaccounted for destruction processes.
At the moment, the absence of DIBs can be explained satisfactorily by the increased
ionization level together with a decrease in carbon abundance, relative to the SMC-wing sightline.
For AzV 456 the 2175 Å bump, often associated with carbonaceous material,
is strong, while non-existent for AzV 18.
This lack of carbonaceous material agrees with the higher gas-to-dust ratio,
lower dust-to-gas ratio, lower metallicity and thus weak (or absent) DIBs
observed for AzV 18. In addition, a cosmic mixture of PAHs (and other complex carbonaceous molecules) may partly contribute to this 2175 Å UV extinction feature (e.g. Lee & Wdowiak 1993; Boulanger et al. 1994; and Li & Draine 2001).
Lack of PAH-like bump carrier molecules may thus be directly related to a reduced presence of
molecules that can give rise (e.g. electronic transitions of the cation can occur in the visible)
to the diffuse interstellar bands. This is consistent with our results.
Li & Draine (2002) studied the molecular cloud SMC B1 # 1.
It has a density of
cm-2, and extinction
mag,
with an extinction curve of
and metallicity
(the gas-to-dust ratio N(H I)/
1021, similar to AzV 18), and found it exposed to an average radiation field of
= 2-3.
In terms of
/
this roughly corresponds to our model cloud C.
If applicable, this would suggest PAH band strengths about twice as strong.
Unfortunately, the molecular cloud itself is unsuited for optical observations,
and the physical conditions of even nearby diffuse clouds can be vastly different.
Applying diffuse cloud models to specific sightlines requires knowledge of some properties of the gas and dust probed (e.g. (dust) extinction, UV field, metallicity, gas phase abundances of key species, etc.). Once available, this allows for detailed modelling of specific situations. Currently, the models can be used "only'' for uncovering general trends in the behaviour of large carbonaceous molecules (such as PAHs) in environments with specific differences.
Acknowledgements
We thank Pascale Ehrenfreund and Lex Kaper for their encouragement and constructive comments, and the referee for several constructive suggestions. N.C. acknowledges support from NOVA.