ABSTRACT
We present new analytic theory and radiative transfer computations for the atomic-to-molecular (H i-to-H2) transitions and the buildup of atomic hydrogen (H i) gas columns in optically thick interstellar clouds irradiated by far-UV (FUV) photodissociating radiation fields. We derive analytic expressions for the total H i column densities for (one-dimensional (1D)) planar slabs, for beamed or isotropic radiation fields, from the weak- to strong-field limits, for gradual or sharp atomic-to-molecular transitions, and for arbitrary metallicity. Our expressions may be used to evaluate the H i column densities as functions of the radiation field intensity and the H2-dust-limited dissociation flux, the hydrogen gas density, and the metallicity-dependent H2 formation rate coefficient and FUV dust grain absorption cross section. We make the distinction between "H i-dust" and "H2-dust" opacity, and we present computations for the "universal H2-dust-limited effective dissociation bandwidth." We validate our analytic formulae with Meudon PDR code computations for the H i-to-H2 density profiles and total H i column densities. We show that our general 1D formulae predict H i columns and H2 mass fractions that are essentially identical to those found in more complicated (and approximate) spherical (shell–core) models. We apply our theory to compute H2 mass fractions and star-formation thresholds for individual clouds in self-regulated galaxy disks, for a wide range of metallicities. Our formulae for the H i columns and H2 mass fractions may be incorporated into hydrodynamics simulations for galaxy evolution.
1. INTRODUCTION
The atomic-to-molecular hydrogen (H i-to-H2) transition is of central importance for the evolution of the interstellar medium (ISM) and for star formation in galaxies, from local environments in the Milky Way to distant cold gas reservoirs in high-redshift systems. Stars form in molecular gas, plausibly because H2 formation enhances low-temperature cooling and cloud fragmentation or perhaps simply because the molecular formation rates are elevated in the denser and more shielded components of the gravitationally collapsing regions. The atomic-to-molecular conversion is also the critical initiating step for the growth of chemical complexity in the ISM from large to small scales, e.g., from diffuse clouds to dense star-forming cores to protoplanetary disks. Globally, the transition to H2 appears to be associated with star-formation thresholds in galaxy-wide Kennicutt–Schmidt relations and with the observed critical gas mass surface densities above which star formation becomes probable.
In this paper, we revisit the theory of the H i-to-H2 transition and the buildup of atomic hydrogen gas layers in fully optically thick interstellar clouds irradiated by far-UV (FUV) radiation fields. Atomic (H i) gas produced by rapid stellar FUV "Lyman–Werner" (LW) photodissociation undergoes conversion to H2 as the destructive radiation is absorbed. In steady state, a mass of H i is maintained in the outer FUV-irradiated photon-dominated regions (PDRs) of the dense molecular clouds. Much of the (cold) H i gas in galaxies may reside in such cloud boundary layers and envelopes, interspersed with the recently formed FUV-emitting OB-type stars.
The study of interstellar H i-to-H2 conversion has had a long and venerable history. Early theoretical discussions (e.g., Spitzer 1948; Gould & Salpeter 1963; Field et al. 1966; Stecher & Williams 1967; de Jong 1972; followed by Aaronson et al. 1974; Glassgold & Langer 1974; Jura 1974; Black & Dalgarno 1977; Federman et al. 1979; van Dishoeck & Black 1986) focused on the competing processes of (grain surface) molecule formation, photodissociation, and shielding in predominantly atomic gas—the classical warm and cold neutral medium (WNM and CNM) and diffuse gas—showing that significant concentrations of H2 could be expected in the Galactic ISM, especially in dark, dusty clouds with high visual extinctions (Mészáros 1968; Hollenbach et al. 1971; Solomon & Werner 1971; de Jong 1972). This was confirmed observationally with the first direct (FUV LW absorption line) detections of interstellar molecular hydrogen in diffuse clouds and the correlation of the H2 with E(B − V) color excess and dust extinction (Carruthers 1970; Spitzer et al. 1973; Savage et al. 1977) and with the discovery of fully molecular clouds via proxy millimeter-wave carbon monoxide (CO) emissions (Wilson et al. 1970; Rank et al. 1971).
Absorption line spectroscopy (Lyα for H i; LW band for H2) has been carried out for H i-to-H2 conversion along many Milky Way sight lines, through low-extinction diffuse-to-translucent gas in the disk, and into the infrared cirrus and high-velocity gas in vertical directions (Savage et al. 1977; Bohlin et al. 1978; Richter et al. 2001; Liszt & Lucas 2002; Rachford et al. 2002, 2009; Gillmon & Shull 2006; Gillmon et al. 2006; Wakker 2006; Liszt 2007; France et al. 2013; Fukui et al. 2014; Röhser et al. 2014). These studies probe systems in which the H2 mass fractions range over many orders of magnitude, from ≲ 10−5 up to ∼50% in highly reddened systems. Absorption line observations of damped and sub-damped Lyα absorbers at high redshifts also directly reveal the partial conversion of H i to H2 in optically thin media (Levshakov & Varshalovich 1985; Foltz et al. 1988; Ge & Bechtold 1997; Cui et al. 2005; Ledoux et al. 2006; Noterdaeme et al. 2010; Crighton et al. 2013; Albornoz Vásquez et al. 2014). In the early universe, the formation of the first stars (Population III) was enabled by the partial conversion to H2 via negative ion chemistry. The resulting H2 rotational line gas cooling rates were likely regulated by LW photodissociation "feedback" from the first stars and FUV sources (Palla et al. 1983; Lepp & Shull 1984; Haiman et al. 1996, 1997; Abel et al. 1997; Ciardi et al. 2000; Glover & Brand 2003; Yoshida et al. 2003; Wise & Abel 2007; Dijkstra et al. 2008; Ahn et al. 2009; Bromm et al. 2009; Miyake et al. 2010; Wolcott-Green et al. 2011; Fialkov et al. 2012; Holzbauer & Furlanetto 2012; Safranek-Shrader et al. 2012; Visbal et al. 2014).
In optically thick regions, 21 cm observations of very cold (≲ 20 K) narrow-line self-absorbed H i (the Galactic "HINSA"; Li & Goldsmith 2003) in combination with CO, OH, and dust mapping for locating the H2 clouds reveal the presence of trace atomic hydrogen inside dark, dusty, and predominantly molecular clouds (Bok et al. 1955; Heiles 1969; Knapp 1974; Burton et al. 1978; McCutcheon et al. 1978; Liszt & Burton 1979; Mebold et al. 1982; van der Werf et al. 1988; Li & Goldsmith 2003; Goldsmith & Li 2005; Krčo & Goldsmith 2010). Such clouds are fully shielded against externally incident photodissociating FUV radiation, and the conversion to H2 is essentially complete. The residual atomic gas in the cloud cores is likely the product of impact ionization by penetrating low-energy cosmic rays (Spitzer & Tomasko 1968; Webber 1998; Dalgarno 2006). Somewhat warmer H i (∼100 K, so still "cold") is also observed in dissociation zones surrounding Galactic H ii regions associated with individual OB-type stars or clusters and/or as H i PDRs in molecular cloud envelopes exposed to ambient interstellar radiation (e.g., Sancisi et al. 1974; Myers et al. 1978; Read 1981; Roger & Pedlar 1981; Wannier et al. 1983; Elmegreen & Elmegreen 1987; van der Werf & Goss 1989; Wannier et al. 1991; Andersson et al. 1992; Gir et al. 1994; Reach et al. 1994; Williams & Maddalena 1996; Gomez et al. 1998; Habart et al. 2003; Matthews et al. 2003; Roger et al. 2004; Lee et al. 2007; Lee et al. 2012; van der Werf et al. 2013). In nearby galaxies, H i has been mapped in spiral arms showing that the atomic gas likely traces outer photodissociated layers in the star-forming giant molecular clouds (Allen et al. 1986, 1997; Shaya & Federman 1987; Rand et al. 1992; Madden et al. 1993; Smith et al. 2000; Heyer et al. 2004; Heiner et al. 2009, 2011; Knapen et al. 2006; Schuster et al. 2007).
By the 1980s, a conceptual switch had occurred with the recognition that much of the hydrogen in galaxies is fully shielded H2 and that in dense gas in star-forming regions the H i is often a surface photodissociation "product," rather than being the dominant component within which some shielded H2 may be present, as in the diffuse medium. Over the decades, many model computations for the H i-to-H2 transition in optically thick media have been presented, with varying degrees of sophistication in treating the critical roles of FUV dust absorption and scattering and H2 absorption line self-shielding. These include one-dimensional (1D) plane-parallel (slab) models assuming steady state conditions with simplified ("isolated line") treatments of H2 self-shielding (Federman et al. 1979; de Jong et al. 1980; Tielens & Hollenbach 1985; Viala 1986; Black & van Dishoeck 1987; Sternberg 1988; Sternberg & Dalgarno 1989; Burton et al. 1990; Spaans et al. 1994; Sternberg & Neufeld 1999; Kaufman et al. 1999), models incorporating "exact" radiative transfer for the combined effects of multiple H2 absorption line overlap and dust absorption and scattering (van Dishoeck & Black 1988, 1990; Viala et al. 1988; Abgrall et al. 1992; Draine & Bertoldi 1996; Browning et al. 2003; Shaw et al. 2005; Goicoechea & Le Bourlot 2007; Le Petit et al. 2006), spherically symmetric models (Andersson & Wannier 1993; Diaz-Miller et al. 1998; Neufeld & Spaans 1996; Stoerzer et al. 1996; Spaans & Neufeld 1997; Spaans & van Dishoeck 1997; Krumholz et al. 2008, 2009; McKee & Krumholz 2010; Wolfire et al. 2010), and also time-dependent models for the H2 formation and destruction (London 1978; Roger & Dewdney 1992; Goldshmidt & Sternberg 1995; Hollenbach & Natta 1995; Lee et al. 1996; Goldsmith et al. 2007). More recently, sophisticated multidimensional (2D and 3D) radiative transfer codes have been developed for the atomic-to-molecular conversion, also incorporating hydrodynamics (Robertson & Kravtsov 2008; Gnedin et al. 2009; Glover et al. 2010; Bisbas et al. 2012; Christensen et al. 2012; Mac Low & Glover 2012; Davé et al. 2013; Offner et al. 2013; Thompson et al. 2014), although the H2 photodissociation rates and the implied H i/H2 density ratios are generally still estimated using 1D shielding prescriptions for the individual hydrodynamic particles or cells.
In recent years interstellar H i-to-H2 conversion has become an important issue in the study of galaxy evolution on large scales, across entire galaxy disks, at both low and high redshifts, and for varying metallicities (e.g., Wong & Blitz 2002; Böker et al. 2003; Blitz & Rosolowsky 2004, 2006; Bigiel et al. 2008; Leroy et al. 2008; Tacconi et al. 2010; Bolatto et al. 2011; Schruba et al. 2011; Welty et al. 2012; Genzel et al. 2012, 2013; Tacconi et al. 2013). Galaxy mapping surveys suggest that on global scales the star-formation efficiencies are determined, at least in part, by molecular gas fractions that may be sensitive to the varying midplane gas pressures and/or metallicities (e.g., Hirashita & Ferrara 2005; Fumagalli et al. 2010; Fu et al. 2010; Lagos et al. 2011; Feldmann et al. 2012; Kuhlen et al. 2013; Popping et al. 2014). Remarkably, the observations of disk galaxies on large scales (e.g., Leroy et al. 2008), and individual Galactic molecular clouds on small scales (e.g., Lee et al. 2012, 2014), indicate that for solar metallicity the H i-to-H2 conversion occurs for characteristic gas surface densities of ∼10 M☉ pc−2 (for "ambient" FUV radiation fields). This surface density corresponds to an FUV dust optical depth ∼1 for typical grain properties and dust-to-gas mass ratios, suggesting that dust absorption and hence metallicity is playing an essential role in setting the critical gas surface densities.
An analytic theory for the H i-to-H2 transition was presented by Sternberg (1988, hereafter S88),who derived a scaling law for the growth of the H i column density and the associated FUV-excited infrared H2 vibrational emission intensities produced in optically thick irradiated cloud surfaces, for application to Galactic emission line sources (see also Jura 1974; Hill & Hollenbach 1978; Elmegreen 1993). S88 included a general-purpose analytic formula for the total H i column density as a function of the FUV radiation intensity, the cloud gas density, and the metallicity-dependent H2 formation rate coefficient and FUV dust attenuation cross section. S88 also identified the fundamental dimensionless parameter that controls the H i-to-H2 transitions and the buildup of the atomic hydrogen columns.
More recently, and motivated by the possible metallicity dependence of molecular mass fractions in galaxy disks, Krumholz et al. (2008, 2009) and McKee & Krumholz (2010; hereafter KMT/MK10) presented new models for the H i-to-H2 transition and for the associated metallicity-dependent H2 mass fractions and star-formation surface density thresholds. A novel feature of the KMT/MK10 study is their analytic focus on (idealized) spherical clouds embedded in ambient isotropic fields, as opposed to the (also idealized) planar geometry and beamed fields adopted in much of the earlier PDR literature, including S88.
Our main goal and motivation in this paper is to reintroduce and extend the S88 theory for applications to global galaxy evolution studies. In Section 2 we elaborate on S88 and present a detailed overview and discussion of the basic theoretical ingredients and parameters controlling the H i-to-H2 transition in FUV-irradiated clouds. We rederive the fundamental S88 equation for the total H i column density produced for beamed radiation into a (1D) optically thick slab. We then extend the theory and consider irradiation by isotropic fields. This will enable our direct comparison with the more complicated (and more approximate) formalism for spheres. In Section 3 we present detailed numerical (Meudon PDR code) radiative transfer computations for the H i-to-H2 transitions and integrated H i columns for a wide range of interstellar conditions. The ratio of the free-space FUV field intensity (or dissociation rate) to the gas density (or H2 formation rate) is an essential parameter, as is the metallicity and dust-to-gas mass ratio. We present numerical computations for a verification of our analytic formulae for beamed and isotropic irradiation from the weak- to strong-field limits (gradual to sharp H i-to-H2 transitions) and for low- to high-metallicity gas. In Section 4 we compare our planar formulae with the KMT/MK10 theory for spheres. This includes a discussion of the dimensionless parameters and a comparison of the expressions for the total H i columns, H2 mass fractions, and star-formation thresholds, as functions of the metallicity. An important application and comparison is for "self-regulated gas" in which the FUV intensity–to–gas density ratio is set by the condition of two-phased equilibrium for H i. We demonstrate that our simpler, more general, and fully analytic 1D formulae predict H i columns and H2 mass fractions that are essentially identical to results for spheres in the more restricted regime in which the spherical models are applicable (intense fields, sharp transitions, low metallicity).
This is a lengthy paper, and we develop the theory and present our step-by-step comparisons in a pedagogical style. In Section 5 we summarize and recap our basic analytic results for the H i column densities and molecular mass fractions in FUV-irradiated clouds, including for self-regulated star-forming galaxies. A glossary of symbols is in the Appendix.
2. ANALYTIC OVERVIEW
In this section we present an analytic discussion and overview of the basic processes and quantities that control the H i-to-H2 transitions and total H i columns in interstellar clouds exposed to photodissociating FUV radiation fields. Our overview anticipates and also provides analytic representations for the detailed numerical results that we present in Section 3. We focus on idealized static 1D semi-infinite uniform density isothermal and optically thick plane-parallel clouds that are irradiated by steady fluxes of FUV LW-band photons. We rederive the S88 formula for the steady state H i column densities produced in slabs irradiated by normally incident unidirectional beamed fields as appropriate for interstellar clouds exposed to localized FUV sources. We then show that this formula can be generalized to clouds embedded in isotropic radiation fields. Isotropic irradiation may be more representative of global ambient conditions in galaxies.
We begin with our normalizations for the beamed and isotropic ultraviolet radiation fields and for the associated H2 photodissociation rates (Section 2.1). We then define the dissociation bandwidth and its derivative—the H2 self-shielding function (Section 2.2.1). We then describe our treatment of dust grains (Section 2.2.2). The grains provide FUV continuum opacity and are also the H2 formation sites. The metallicity of the gas then enters as an important parameter because it controls the dust-to-gas mass ratio and therefore also the associated H2 formation efficiency and the FUV dust optical depth per gas column density. We make the simplifying assumption that the dust-to-gas mass ratio scales linearly with the metallicity. If star formation requires the conversion from H i to H2, the metallicity will be an essential parameter in controlling the star-formation thresholds.
We put the physical ingredients together and write down the depth-dependent steady state H i/H2 formation–destruction equation for semi-infinite slabs exposed to beamed fields (Section 2.2.3). Crucially, the differential equation is separable, and this enables our definition of the "universal H2-dust-limited LW dissociation bandwidth" (Section 2.2.4) and the "effective dissociation flux" (Section 2.2.5). The H2-dust-limited dissociation bandwidth is a fundamental quantity in the theory, and we present analytic expressions and numerical computations for it in this paper.
We then integrate the H i/H2 formation–destruction equation to derive our analytic formula for the H i column density for clouds irradiated by beamed fields (Section 2.2.6). Our formula gives the H i column density as a function of the physical variables, including gas density, FUV intensity, effective dissociation flux, H2 formation rate coefficient, FUV dust absorption cross section, and metallicity.
As we discuss in Section 2.2.6, the H i-to-H2 transition profiles and the total atomic column densities are controlled by a single dimensionless parameter, "αG," first introduced by S88. In a nutshell, αG determines the LW-band optical depth in the cloud due to the dust associated with the H i gas (which we refer to in this paper as "H i-dust"), whether or not the H i is mixed with the H2. The total H i-dust optical depth is a critical quantity in the theory; for beamed fields our formula for it (as derived in Section 2.2.6) is
As we show in Section 2.2.7, αG can be expressed in terms of the physical variables in several ways. Most simply, α (also dimensionless) is the ratio of the free-space photodissociation rate to the H2 formation rate, and G is a cloud-averaged H2 self-shielding factor. The product αG is then similar to the ionization parameter "U" for H ii Strömgren regions, where U is proportional to the ratio of the photoionization rate to the H i formation rate via electron–proton recombination. However, αG is also a measure of the dust absorption efficiency of the H2-dissociating photons. For the H i/H2 density ratio in an optically thin "free-space" radiation field, αG is the ratio of the H i-dust to H2-line absorption rates of LW-band photons that are effectively available for H2 dissociation. For sufficiently large metallicities, this excludes LW photons "between the lines" that are inevitably absorbed by dust associated with just the H2 ("H2-dust") in a predominantly molecular and dusty cloud. As we will discuss, the mean shielding factor G depends on the competition between H2-line absorption and H2-dust absorption. Because of this competition, a metallicity dependence is introduced into G and therefore also into our fundamental parameter αG.
An important physical distinction occurs between the limits of small and large αG (Section 2.2.8). Small αG is the "weak-field limit" for which H i-dust opacity is negligible and does not contribute to the absorption of the radiation, although a substantial (observable) atomic column can nevertheless exist in this limit. Large αG is the "strong-field limit" for which the atomic column becomes so large that H i-dust dominates the attenuation of the radiation fields, reducing the fraction of the incident radiation that is absorbed by the H2.
In general, αG is the dimensionless "free parameter" in the problem, with a value that is determined by local conditions (density, radiation intensity, metallicity, etc.). However, as invoked by KMT/MK10, on global scales in star-forming galaxy disks the gas density and radiation intensity may be correlated or self-regulated to conditions enabling a two-phase equilibrium between cold and warm H i (CNM/WNM multiphase). As we describe in Section 2.2.9, this then drives αG to a narrow range, of order unity, intermediate between the weak- and strong-field limits, and only weakly dependent on the metallicity.
Finally, in Section 2.3 we extend our analysis to slabs exposed to isotropic radiation fields. An angular integration over all photodissociating ray directions is then also required in the computation of the H i column densities. Our resulting analytic expressions for the atomic columns and associated H i-dust opacities are similar to those for beamed fields, with similar behavior in the weak- and strong-field limits. Our analytic results for slabs irradiated by isotropic fields enable a direct comparison to the KMT/MK10 results for spheres, as we discuss in depth in Section 4. In Section 3 we verify our analytic results with detailed numerical model computations.
2.1. Radiation Fields and H2 Photodissociation Rate
We will consider static, optically thick plane-parallel clouds (slabs) exposed to either isotropic or corresponding beamed LW-band radiation fields. We define the spectral range of the LW band as 912–1108 Å (11.3–13.6 eV) as appropriate for line absorptions occurring out of low-lying rotational levels in the ground vibrational state.
Let Fν ≡ 4πIν, where Iν is the specific photon intensity (cm−2 s−1 Hz−1 sr−1) of an isotropic optically thin "free-space" LW radiation field. If an optically thick gas slab (or semi-infinite slab) is inserted, the flux density of the isotropic field at a cloud surface is equal to πIν = Fν/4. The corresponding unidirectional beamed field is defined such the LW photons are normally incident on the cloud surface with flux density 2πIν = Fν/2. The surface flux of the isotropic field is half that of the corresponding beamed field, but the energy densities are equal. The energy densities at the cloud surfaces are half that in the (full 4π) free-space radiation field.
In this paper we adopt the standard Draine (1978, 2011) expression
for the specific intensity of the isotropic free-space FUV (5–13.6 eV FUV) radiation field in the Galactic ISM. In Equation (2), λ is the photon wavelength in Angstroms. For this spectrum, the specific intensity varies by a factor of eight across the LW band. At 1000 Å, photons s−1 cm−2 Hz−1 sr−1, and the energy density erg cm−3 (where ν is the photon frequency in Hz). The total photon density in the 912–1108 Å LW band is 6.9 × 10−4 cm−3.
To consider radiation fields with greater or lesser intensities, we multiply by an overall field-strength scaling factor IUV, such that IUV = 1 corresponds to the unit free-space Draine field given by Equation (2). In this paper we do not consider radiation fields with alternate spectral shapes. For completeness we recall that the Draine energy density is 1.7 times larger than the Habing (1968) estimate for the LW energy density at 1000 Å.4
For the free-space fields, we define the LW-band photon flux integral
where ν1 to ν2 is the frequency range of the LW band and . For the Draine spectrum, Fν = 3.4 × 10−8IUV photons s−1 cm−2 Hz−1 at 1000 Å, and
At the cloud surfaces, the 1000 Å flux densities are then Fν/4 = 8.6 × 10−9IUV and Fν/2 = 1.7 × 10−8IUV photons s−1 cm−2 Hz−1 for the isotropic and corresponding beamed fields. The total LW-band surface fluxes are F0/4 = 5.18 × 106IUV and F0/2 = 1.03 × 107IUV photons cm−2 s−1. For a given IUV, the energy densities of the isotropic and corresponding beamed fields are equal at the cloud surfaces.
The photodissociation of H2 occurs via line absorption of LW photons in allowed transitions from the ground electronic state to the excited B1Σu or C1Πu states. These are followed by rapid decays to either bound ro-vibrational levels or to the continuum of the ground X state. Decays to the continuum lead to dissociation (P. M. Solomon, private communication in Field et al. 1966; Stecher & Williams 1967; Stephens & Dalgarno 1972; Abgrall et al. 1992). The B–X and C–X bound–bound transitions are mainly to excited vibrational levels followed by a near-infrared quadrupole radiative cascade (Gould & Harwit 1963; Black & Dalgarno 1976; Shull 1978; Black & van Dishoeck 1987; S88; Sternberg & Dalgarno 1989; Draine & Bertoldi 1996; Neufeld & Spaans 1996). Thus, all of the LW-band photons absorbed by the H2 are removed, but only a fraction of these absorptions (∼10%) lead to photodissociation.
The H2 photodissociation rate in the ISM is a fundamental quantity, and we recompute it in Section 3 by assuming the Draine spectrum for a range of assumed gas temperatures, densities, and field intensities. We find that for dissociation out of the 912–1108 Å LW band, the optically thin (full 4π) free-space photodissociation rate is
At a cloud surface the dissociation rate, D(0) ≡ D0/2, is half the free-space rate and
Because the dissociation rate is proportional to the radiation energy density, the dissociation rates for isotropic and corresponding beamed fields are identical at a cloud surface.
The photodissociation rate diminishes with cloud depth due to the combination of H2-line and dust absorptions. The attenuation of the LW radiation field is crucial in determining the depth dependence of the atomic and molecular densities, the shapes of the H i-to-H2 transition profiles, and the resulting atomic hydrogen column densities. The depth-dependent attenuation depends on the assumed field geometry, and we analyze the behavior for both beamed and isotropic fields, starting with beamed fields which are simpler.
2.2. Beamed Fields
We consider the H i-to-H2 transition and total column density of atomic hydrogen on one side of an optically thick plane-parallel slab of gas (or semi-infinite slab) that is exposed to a steady flux of LW-band photons normally incident on the cloud surface as unidirectional beamed radiation.
2.2.1. Dissociation Bandwidth and Self-shielding Function
Let N2 be the H2 column density (cm−2) at some depth normal to the cloud surface. Then, neglecting dust absorption of the LW photons, and for beamed radiation, the photodissociation rate (s−1) for a single LW absorption line ℓ may be written as
where
In these expressions, is the incident beamed flux density (photons cm−2 s−1 Hz−1) at the cloud surface, σν, d is the cross section (cm2) for absorptions that lead to molecular dissociation,5 and σν is the cross section for all photon absorptions (not just those that are followed by dissociation). The dissociation probabilities, fdiss ≡ σν, d/σν, range from ∼0 to more than 0.5 for individual LW transitions depending on the rotational quantum number in the excited B or C states. The mean (typical) dissociation probability averaged over all lines is 〈fdiss〉 = 0.12. For a single absorption line,
for a typical LW-band oscillator strength of fosc ≈ 0.01 and dissociation probability of fdiss ≈ 0.1 (and where e and me are the electron charge and mass, and c is the speed of light).
In Equation (7), we pull Fν out of the integral because we assume that the flux density varies very slowly over the narrow line profile (as represented by σν). In Equation (8), Wℓ, d(N2) is defined as the "equivalent bandwidth" (Hz) of radiation absorbed in H2 dissociations via absorption line ℓ, up to molecular column N2. The dissociation rate Dℓ(N2) decreases with the molecular column N2 as the absorption line become optically thick, and the ratio
is the individual H2-line "self-shielding" function. It quantifies the reduction of the line dissociation rate, where Dℓ(0) is the line dissociation rate at the cloud surface. By definition, the self-shielding function is proportional to the derivative of the dissociation bandwidth Wℓ, d (Federman et al. 1979; van Dishoeck & Black 1986; S88; Draine & Bertoldi 1996).
For the full multiline LW-band system, the dissociation rate (again neglecting dust absorption) may be written compactly as
where Wd(N2) is the equivalent dissociation bandwidth summed over all of the (possibly overlapping) absorption lines, and is a mean flux density. A plot of Wd versus N2 is the effective "curve of growth" for the dissociating LW radiation bandwidth in a dust-free cloud. We present computations for Wd(N2) in Section 3 (the blue curve in Figure 3).
The mean flux density in Equation (11) is given by
Here xi are the fractional populations of H2 molecules in ro-vibrational levels i of the ground electronic X state, is the (full 4π) free-space specific intensity at frequencies νij of LW-band transitions between level i and levels j in the excited B or C states, and are the absorption line dissociation cross sections (cm2 Hz). The mean flux density is weighted by the relative strengths of the dissociation transitions. For the Draine spectrum, photons cm−2 s−1 Hz−1.
The denominator in expression (12) is the total (frequency integrated) H2 dissociation cross section (cm2 Hz) summed over all absorption lines,
Most of the H2-line absorptions occur out of the lowest few rotational levels, and the total effective dissociation cross section is insensitive to the fractional populations xi. We find that
The ratio is then the approximate number of strong LW absorption lines involved in the multiline H2 photodissociation process (see also Figure 2 in Section 3).
With these definitions, the free-space photodissociation rate may be expressed as
At a cloud surface the photodissociation rate is . The ratio
is then the complete multiline H2 "self-shielding" function. It quantifies the reduction of the total dissociation rate due opacity in all of the absorption lines.
For a single line the self-shielding function varies as for large N2 because absorptions can always occur far out on the Lorentzian damping wings.6 Therefore, for a single absorption line, Wℓ, d as given by Equation (8) diverges as . For strong lines (with fosc ∼ 0.01), this "square root" part of the curve of growth begins when N2 ≳ 1017 cm−2. For the realistic multiline system, the absorption lines will overlap for sufficiently large (≳ 5 × 1020 cm−2) molecular columns, and Wd does not diverge as does Wℓ, d. For the multiline system, the total dissociation bandwidth
is limited to a finite maximal value (even in the absence of dust). We find that for the Draine spectrum Wd, tot = 9.1 × 1013 Hz (as computed in Section 3.1.2). In Section 3.1.3 we present our computations for the multiline self-shielding function (Figure 5). At the cloud surface, fshield = 1. As the Doppler cores become optically thick at N2 ≳ 1014 cm−2, fshield becomes small and the molecules are then said to self-shield against the dissociating radiation. The decline is more gradual at intermediate columns, 1017 to 1022 cm−2, for which most of the absorption is out of the line wings. Finally, as line overlap occurs and the dissociating radiation is fully absorbed, fshield becomes vanishingly small.
In the limit of complete line overlap, every photon in the (912–1108 Å) LW band is absorbed in H2-lines. The product is then the LW "dissociation flux" (photons cm−2 s−1) at the cloud surface. In the absence of dust absorption, this flux is equal to the H2 dissociation rate per unit area. For complete absorption of the LW-band radiation, the mean dissociation probability is
where F0/2 is the total incident LW-band flux. For the radiative transfer computations we present in Section 3, we find that and is essentially equal to the simple average over the individual line dissociation probabilities for the matrix of X–B and X–C transitions. Our result for is consistent with many previous calculations (e.g., Black & van Dishoeck 1987; Draine & Bertoldi 1996; Browning et al. 2003).
2.2.2. Dust and Metallicity
In addition to the H2-line absorptions, the LW-band photons are also absorbed by dust grains, further reducing the photodissociation rate. We assume that the dust is mixed uniformly with the gas with a dust-to-gas mass ratio that depends linearly on the metallicity of the cloud. For the grain–photon interaction, we assume pure absorption and no scattering (or equivalently only forward scattering). With the inclusion of dust, the local dissociation rate, D, at any cloud depth is then
where D0 is the free-space dissociation rate (Equation (5)). In this expression, τg ≡ σgN is the dust continuum optical depth, where N ≡ N1 + 2N2 is the column density of hydrogen nuclei, in molecules plus atoms. Here σg is the dust grain LW-photon absorption cross section (cm2) per hydrogen nucleon. With the inclusion of dust attenuation, the dissociation rate given by Equation (19) depends on both N2 and the column density of atomic hydrogen N1.
For simplicity we also assume that σg is independent of photon frequency over the narrow LW band. For a standard interstellar extinction curve, with a total-to-selective extinction ratio of RV ≡ AV/E(B − V) = 3.1, a 1000 Å grain albedo ≈ 0.3, and a scattering asymmetry factor 〈cos θ〉 ≈ 0.6, the effective absorption cross section per hydrogen nucleus σg = 1.9 × 10−21 cm2 (Draine 2003); RV = 3.1 is for diffuse gas (with densities n ∼ 102 cm−3). For RV = 3.1, AV/N = 5.35 × 10−22 mag cm2. In dense regions (n ≳ 103 cm−3), RV can be larger (up to ∼5.8) but with an extinction curve that is less steep toward the ultraviolet, with σg ≈ 8 × 10−22 cm−2 (Cardelli et al. 1989; Fitzpatrick 1999; Draine & Bertoldi 1996; Draine 2011). With the assumption that the dust-to-gas mass ratio is linearly proportional to the metallicity Z' of the gas, we therefore set
where Z' = 1 corresponds to the solar photospheric abundances of the heavy elements ("solar metallicity") and where ϕg of order unity depends on the grain composition and size distribution.
Dust grains are also essential for H2 formation (Hollenbach et al. 1971; Jura 1974; Barlow & Silk 1976; Leitch-Devlin & Williams 1985; Pirronello et al. 1997; Takahashi et al. 1999; Cazaux & Tielens 2002; Habart et al. 2004). We assume that per hydrogen nucleon the rate coefficient for H2 formation on grains is given by
where T is the gas temperature in °K. Our standard value is then R = 3 × 10−17 cm3 s−1 for T = 100 K and Z' = 1.
2.2.3. H i/H2 Formation–Destruction Equation
For a steady state in which molecular photodissociation is balanced everywhere by grain surface H2 formation, the H i/H2 formation–destruction equation may be written as
In this equation, n1 and n2 are the local volume densities (cm−3) of the H i atoms and H2 molecules, and
is the total volume density of hydrogen nuclei. The right-hand side of Equation (22) is the H2 photodissociation rate per unit volume (s−1 cm−3) at some cloud depth where the rate is reduced by the combined effects of self-shielding and dust attenuation. The left-hand side is the rate per unit volume of H2 formation on dust grains. We ignore all other formation or destruction processes (such as formation in the gas phase or destruction by X-ray or cosmic-ray ionization).
Given the free parameters n, D0 (or equivalently IUV), R, and σg (or given Z', which determines R and σg), Equation (22) together with particle conservation Equation (23) can be solved for the local atomic and molecular densities n1 and n2 and for the integrated atomic and molecular columns N1 and N2. If it is assumed that the incident LW radiation is fully absorbed, then (as we show below) Equation (22) gives our fundamental formula for the total atomic column that is maintained in the cloud.
The density ratio n1/n2 = dN1/dN2, and Equation (22) may be written as the separable differential equation (S88; see also Jura 1974; Hill & Hollenbach 1978):
In writing the formation–destruction equation this way, a key insight is that the dust opacities associated with the atomic and molecular columns can be considered separately. We will refer to "H2-dust" or "H i-dust" as the dust opacities associated with either just the H2 or the H i gas, respectively, whether or not the H i gas is mixed with the H2.
Integrating this expression and assuming that R and n are constants (i.e., do not vary with cloud depth) gives
which is a functional relationship, N1(N2), between the atomic and molecular column densities. We note that the independent variable parameterizing the cloud depth is here chosen to be N2 rather than the total gas column density N. Choosing N2 as the independent variable is essential for our analysis, even though it is N that is proportional to the visual extinction AV, or to the length scale z ≡ N/n.
2.2.4. H2-dust-limited Dissociation Bandwidth
Most importantly, for a given value of σg, the integral on the right-hand side of Equation (25),
is a function of the molecular column N2 only. This is because the exponential cutoff factor in the integrand is due to H2-dust opacity only—it excludes H i-dust—and because Wd itself depends only on N2. Furthermore, Wg(N2) is only very weakly dependent on n, R, or D0 and is essentially independent of these parameters (see Section 3). So, for a given σg, the effective equivalent width Wg(N2) is a quantity that can be calculated in advance as a "universal dust-limited curve of growth" for the H2-line absorption of LW radiation, independent of the other parameters, n, R, and D0, that together with σg determine the depth-dependent H i/H2 density ratios and the H i-to-H2 transition profiles.
Thus, Wg(N2) (as opposed to Wd[N2]) is the effective bandwidth of dissociating LW radiation in a dusty H2 cloud, where now this bandwidth is limited by H2-dust absorption of LW photons that would otherwise be available for H2 photodissociation in a dust-free cloud. H2-dust opacity is important if it becomes large before the H2 absorption lines can fully overlap. For sufficiently small σg, the lines do overlap completely, and then Wg(N2) = Wd(N2). For sufficiently large σg, the H2-dust provides a cutoff, and then Wg(N2) < Wd(N2) at large N2.
It is a remarkable physical coincidence that the H2 column density at which the H2-lines begin to overlap—a column that depends on the internal molecular oscillator strengths and energy level spacings—is comparable to the H2 column at which the H2-dust opacity 2N2σg ≳ 1 for standard interstellar dust absorption cross sections. Thus, both regimes of "small σg" and "large σg" for the dissociation bandwidth Wg(N2) are relevant for the range of interstellar dust properties and metallicities in galaxies. In Section 3.1.2, we present computations of Wg(N2) for a wide range of σg encompassing these regimes.
As N2 → ∞, the equivalent width Wg(N2) converges to a finite limit
either because the exponential H2-dust attenuation factor cuts off the integrand (for large σg) or because dWd/dN2 itself vanishes as the lines overlap (for small σg). Thus, Wg, tot(σg) is the total H2-dust-limited effective dissociation bandwidth. For large σg, Wg, tot < Wd, tot, and for small σg, Wg, tot = Wd, tot. For large σg, the absorption lines remain separated but are nevertheless highly damped for most of the integration range up to the H2-dust cutoff.
For a single absorption line, in the damped regime, and it follows from Equation (27) that Wg, tot(σg) scales as . Our numerical computations (Section 3.1.2) show that for large σg this scaling behavior is maintained in the full multiline problem to a good approximation. In Section 3, we find that the simple formula
is an excellent fit to our numerical radiative transfer results. The normalized H2-dust-limited dissociation bandwidth
where in the last equality we have assumed σg = 1.9 × 10−21ϕgZ' (Equation (20)). In these expressions, Wg, tot → Wd, tot and w → 1 for small σg (low metallicity) and decrease as for large σg (high metallicity). The normalized bandwidth w decreases from 0.9 to 0.2 for σg ranging from 1 × 10−23 cm−2 (small) to ∼6 × 10−21 cm−2 (large) or for Z' ranging from ∼0.01 to 3 (assuming σg∝Z'), which is the relevant range for galaxies.
2.2.5. Effective Dissociation Flux and Dissociation Probability
Given Equation (18), we may now write
and define the effective dissociation probability
The product is the "effective dissociation flux" for dusty clouds in which H2-dust may absorb some of the incident LW radiation. The effective dissociation flux depends on the competition between H2-line absorption and H2-dust absorption as given by the dependence of Wg, tot on σg. The effective dissociation flux is the H2 photodissociation rate per unit surface area for a dusty and optically thick molecular slab in which H i-dust opacity is negligible.
When H2-dust is negligible, w = 1 and . When H2-dust opacity is significant, w < 1 and . The effective dissociation probability is the fraction of the total 912–1108 Å LW-band flux that is absorbed in H2 photodissociation events in a dusty, optically thick, predominantly molecular slab (with vanishing H i-dust opacity). For low Z', is a constant. For high Z', decreases as Z'−1/2.
2.2.6. Formula for the H i Column Density
Returning now to Equation (25), it follows that
or
Following S88, we now define the dimensionless parameter
where D0 is the free-space dissociation rate,7 and we define the dimensionless "G integral"
We can then write
where
Given the "universal" dust-limited curve of growth Wg(N2), which can be computed "in advance" for any σg, the atomic column is then given by Equation (36) (or Equation (33)) for any surface dissociation rate D0 (or IUV), rate coefficient R, and density n.
We refer to Equation (36) as the "semi-analytic integral H i-to-H2 profile." It shows that the H i column at any depth depends on only two quantities—σg and αG(N2). In dimensionless form
where τ2 ≡ 2σgN2 is the dust optical depth associated with the molecular column, and τ1(τ2) ≡ σgN1 is the H i-dust optical depth at τ2.
As N2 → ∞, Wg(N2) → Wg, tot. The total atomic column density is therefore finite and is given by
or
Here the dimensionless parameter
is the limit of G(N2) as N2 → ∞, so that
We discuss these and additional expressions for αG in Section 2.2.6 below.
Equation (40) for the total H i column on one side of an optically thick cloud was first derived by S88 (see Equation (9) of that paper), and it is the fundamental relation in our analysis.8 The basic assumption is that all of the dissociating LW-band radiation is absorbed, as in a classical "ionization-bounded" H ii region or layer (Strömgren 1939). However, because of the three-way competition between H i-dust, H2-dust, and H2-lines, the behavior for H i is more complicated than for H ii. For a steady (dust-free) photoionized planar Strömgren layer, the H ii column equals the ratio of the Lyman continuum flux to the recombination rate, independent of the photoionization cross section. Similarly, in our Equation (39) or Equation (40), the H2-line absorption cross section does not appear explicitly (although it is implicit in our definition of the effective dissociation flux). The H i column depends on the ratio of the effective dissociation flux to the H2 formation rate, but this ratio is multiplied by the dust absorption cross section and appears inside a logarithm. We discuss this behavior, and the connection to Strömgren relations, in our description of the weak- and strong-field limits in Section 2.2.8.
In dimensionless form, the total H i-dust optical depth associated with the total atomic column is
The total H i-dust optical depth depends on the single dimensionless parameter αG constructed from the cloud variables D0 (or F0 or IUV), n, R, and σg (or Z', which determines R and σg).
The total gas column N ≡ N1(N2) + 2N2. It therefore follows from Equation (36) that the atomic column as a function of the total (atomic plus molecular) column, N1(N), also depends on just σg and αG. Similarly, for τg ≡ σgN, the H i-dust optical depth τ1(τg) depends on the single dimensionless parameter αG. Then, since n1/n2 ≡ dN1/dN2 it follows that the shapes of the H i-to-H2 transition profiles are invariant for identical αG. That is, the density fractions n1/n and 2n2/n expressed as functions of the dust optical depth τg (or visual extinction AV) depend on just the single dimensionless parameter αG.
In Section 3.1.4 we present detailed numerical computations for the H i-to-H2 transition profiles. We show that the transitions are "gradual" when αG ≪ 1 and are "sharp" when αG ≫ 1. An essential feature of our derivation and analytic expression for the total H i column is that no assumptions need to be made on the shape of the H i-to-H2 transition profile. Our Equation (39) or Equation (40) are universally valid for all profile shapes, gradual or sharp.
2.2.7. αG
It is useful to consider the physical meaning of the dimensionless parameters α and G and their product αG.
First, α is the ratio of the unattenuated free-space H2 photodissociation rate to the H2 formation rate and can be expressed as
Thus, α is just the free-space atomic-to-molecular density ratio n1/n2, and α/2 is the density ratio at the surface of an optically thick slab. For a characteristic interstellar cloud gas density n ∼ 102 cm−3, and with D0 = 5.8 × 10−11IUV s−1, the atomic-to-molecular density ratio is n1/n2 ≫ 1 at the cloud edge in the absence of shielding, unless IUV is unrealistically small. Conversion to the molecular phase in the ISM generally requires significant attenuation of the ambient and destructive radiation fields.
Now consider the parameter G. Defining the H2-dust opacity τ2 ≡ 2σgN2 (see Equation (35)),
Thus, G is the average H2 self-shielding factor. The average is over an H2 column for which the H2-dust opacity τ2 ≈ 1. Thus, (1/2)D0G is the characteristic photodissociation rate for self-shielded H2 in a fully molecular cloud, prior to the onset of any H2-dust attenuation. Because fshield is already ≪1 for τ2 ≪ 1, the H2 molecules are very self-shielded for an H2-dust opacity τ2 ∼ 1, and G is generally very small.
The product αG/2 = (1/2)D0G/Rn is then the atomic-to-molecular density ratio n1/n2 for the average shielded H2 dissociation rate. This is our first interpretation for αG (and as adopted in S88). If n1 > 2n2 for the shielded dissociation rate, then H i-dust must also contribute to the attenuation of the LW radiation since then τ1 > τ2 within the H2-dust attenuation column. If n1 ≪ 2n2, then H i-dust attenuation is negligible.
Alternatively, (Equation (41)) is the ratio of the UV continuum dust absorption cross section (cm2) to the total H2-line dissociation cross section (cm2 Hz) averaged over the effective dissociation bandwidth (Hz). Again, G is generally very small because H2-line absorption is so much more efficient than dust absorption. Given σg = 1.9 × 10−21ϕgZ' cm2 (Equation (20)) and our expression (28) for Wg, tot, and with cm2 Hz, we have
For example, for standard values Z' = 1 and ϕg = 1, Equation (46) gives G = 3.0 × 10−5 and the shielded H2 dissociation rate (1/2)D0G = 8.7 × 10−16IUV s−1. For low metallicity, small σg, it follows that G∝Z' (or G∝σg). For high metallicity, large σg, G∝Z'1/2 (or ).
Since α is the free-space atomic-to-molecular density ratio, we have
where in the second and third equalities we have used the relations and . This gives our second interpretation for αG. It is the free-space ratio of the H i-dust to H2-line absorption rates of LW photons in the H2-dust-limited dissociation band.
Third, since (and ), we have
Thus, αG is the free-space ratio of the dust absorption rate of the effective dissociation flux—per hydrogen atom—to the molecular formation rate per atom.
When αG ≪ 1, H i-dust plays no role anywhere in the cloud, since it is negligible even for the free-space field where the atomic density is largest. However, when αG ≫ 1, H i-dust becomes important and absorbs an increasing fraction of the LW photons that are otherwise available for H2 photodissociation.
Thus, with Equations (44) and (46),
or with Equation (48),
With Equation (4) or Equation (5) for F0 or D0, and Equations (20) and (21) for σg and R, we then have
For σg and R varying the same way with Z' there is a cancellation, but a metallicity dependence still remains via the dissociation bandwidth w (Equation (29)) and its dependence on the competition between H2-dust absorption and H2-line absorption. For low Z' (complete line overlap limit, w = 1), αG is independent of the metallicity, but for high Z', and αG ∼ Z'−1/2.
2.2.8. Weak- and Strong-field Limits
Expression (51) also shows that the regimes of large and small αG are both relevant for the widely varying conditions in localized environments of the ISM in galaxies. For example, IUV can range from ∼1 at "average" locations to ≳ 105 near hot stars, whereas n can range from ∼10 cm−3 in diffuse gas to ≳ 106 cm−3 in dense molecular clouds. On global scales in star-forming galaxy disks, IUV and n may be correlated (see Section 2.2.9). But on small scales, enhanced radiation fields will not necessarily be offset by higher gas densities, and IUV/n may span a wide range from "large" to "small."
For αG/2 ≪ 1 the absorption of the LW radiation is dominated by the combination of H2-line absorption and H2-dust absorption, and H i-dust is negligible.9 For αG/2 ≫ 1 H i-dust absorption dominates the attenuation of the radiation field. We refer to αG/2 ≪ 1 as the "weak-field limit" and to αG/2 ≫ 1 as the "strong-field limit."
We now consider the behavior of N1, tot in these two limits.
It follows from Equations (40) and (39) that for αG/2 ≪ 1,
So for weak fields, the total H i column density is equal to the ratio of the effective LW dissociation flux to the H2 formation rate (which is the removal rate of for the H i). The atomic column is proportional to the surface dissociation rate D0 (or to the field strength IUV) and inversely proportional to the cloud gas density n.
In the weak-field limit, the H i-dust opacity associated with the total atomic column τ1, tot ≡ σgN1, tot ≪ 1. We again see that H i-dust plays no role in attenuating the LW radiation field in this limit. For weak fields, the total H i column depends on σg only via Wg, tot, through the possible competition between H2-line absorption and H2-dust absorption. For small σg where H2-dust is negligible, dust absorption plays no role whatsoever, and N1, tot is completely independent of σg. In the small-σg limit, G∝σg, and the dust absorption cross section cancels out completely. For R∝Z', we then have N1, tot∝1/Z', and the metallicity dependence enters entirely via the H2 formation rate coefficient. For large σg, H2-dust absorption is non-negligible, and (and ), thus N1, tot scales as . Then with σg∝Z' and R∝Z', we have N1, tot∝Z'−3/2.
Expression (52) can be written as the simple "Strömgren relation"10
The effective dissociation flux on the right-hand side is the rate per unit area at which dissociating photons (those absorbed in H2-lines but not by H2-dust) penetrate the cloud surface. By definition these photons are fully absorbed by the H2 when H i-dust is negligible, so this is also the photodissociation rate per unit surface area. In steady state this must equal the total H2 formation rate per unit area, which is the left-hand side.
For the strong-field limit αG/2 ≫ 1, it follows from Equation (40) that
For strong fields, τ1, tot = σgN1, tot ≳ 1, and the H i-dust opacity associated with the total atomic column contributes significantly to the attenuation of the incident LW flux. This leads to a saturation and logarithmic dependence of the atomic column on the cloud parameters. For example, increasing the atomic column by increasing the LW-band flux also leads to more effective absorption of the LW photons by the larger H i-dust column. A decreasing fraction of the LW photons is then absorbed by the H2, and the growth of the atomic column is limited. Similarly, increasing the H2 formation rate reduces the atomic column, but the H i-dust opacity is then also reduced, which increases the LW fraction available for photodissociation, thereby moderating the reduction of the H i column.
If we neglect the logarithmic factor, then up to a factor of order unity, we have
for intense fields. Indeed, if the attenuation is dominated by H i-dust, the atomic column must approach a value such that τ1, tot ≡ σgN1, tot ≳ 1. Then, if σg∝Z' the H i column N1, tot∝1/Z' (neglecting the logarithmic factor). In the strong-field limit, the metallicity dependence enters via the grain absorption cross section.
Finally, Equation (54) for the strong-field limit may also be expressed as the Strömgren relation11
Here
is a reduction factor that accounts for H i-dust attenuation of the effective dissociation flux. The right-hand side of Equation (56), including the factor u, is the H2 photodissociation rate per unit surface area, and this equals the total H2 formation rate per unit area, which is the left-hand side.
2.2.9. (αG)CNM for Two-phase Equilibria
Galaxy disks may be self-regulated such that the thermal pressures in the H i gas enable a cold/warm (CNM/WNM) two-phased mixture, with cold neutral Hi (CNM) accumulating in the UV illuminated PDRs of the star-forming molecular clouds (Ostriker et al. 2010; Faucher-Giguère et al. 2013; Kim et al. 2013). As invoked by KMT/MK10, the ratio IUV/n may then be restricted to a narrow range. This then gives rise to a characteristic αG for self-regulated disks, as follows.
For a given heating rate, two-phased equilibrium occurs for a narrow range of thermal pressures and associated CNM and WNM densities, nCNM and nWNM, as controlled by the combined action of Lyα and C ii fine-structure emission line cooling, with a metallicity dependence via the abundance of the gas-phase carbon ions (Field et al. 1969; Wolfire et al. 2003). Given the FUV heating rates and the metallicity-dependent emission line cooling rates, the characteristic CNM density for two-phase equilibrium will be close to the minimum gas density for which CNM is possible. Wolfire et al. (2003) developed the analytic formula
for the characteristic CNM density, assuming that FUV grain photoelectric emission is the dominant heating mechanism for the gas. In this expression, IUV is again the FUV intensity (normalized to the Draine field), Z' is the metallicity, and ϕCNM is a factor of order unity. Following KMT/MK10 we set ϕCNM = 3. This gives nCNM = 23 cm−3 for IUV = 1, at Z' = 1.
Most importantly, nCNM is proportional to IUV. If the gas density n in the FUV illuminated gas is set equal to nCNM, the ratio IUV/n then depends on the metallicity only, as given by Equation (58). With Equation (51) we then have
for self-regulated systems. In Figure 1 the solid curve is (αG)CNM versus Z' as given by Equation (59) (assuming ϕg = 1). The dashed curve excludes the (2.64ϕgZ')1/2 term that accounts for H2-dust reduction of the effective dissociation bandwidth (not considered by KMT/MK10 as discussed in Section 4). Remarkably, the enhanced nCNM associated with reduced cooling efficiency at low metallicity (Equation (58) is offset by the increased dissociation bandwidth at low Z'. Thus, so long as grain photoelectric heating dominates, we have
for self-regulated systems, independent of Z'. The expected H i columns are then midway between the weak- and strong-field limits.
Figure 1. Metallicity dependence of (αG)CNM for two-phase equilibrium as given by Equation (59), with and without (solid and dashed curves) H2-dust reduction of the effective dissociation bandwidth.
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Standard image High-resolution image2.3. Isotropic Fields
We now consider clouds illuminated by isotropic radiation fields.
Let Iν be the specific LW photon intensity of an isotropic field, and let μ ≡ cos θ, where θ is the angle of an incident ray relative to the cloud normal. Again, we are assuming plane-parallel clouds. In the absence of dust, the photodissociation rate at a molecular column N2 normal to the cloud surface may be written as
where fshield(N2) is the unidirectional self-shielding function defined by Equation (16), and Wd(N2) is the same effective "multiline" curve of growth for the (dust-free) dissociating bandwidth that appears in Equation (11) for beamed fields. In Equation (61), the contribution to the angular-integrated dissociation rate is reduced by the self-shielding factor fshield(N2/μ) along each ray. Here is the free-space specific intensity averaged over the dissociating transitions, as given by Equation (12).
With the inclusion of dust absorption along each ray, the H i/H2 formation–destruction equation at a molecular column N2 is
Like Equation (24) for beamed fields, this is a differential equation for N1(N2). However, because of the angular integration, the exponential term exp(− σgN1/μ) for the H i-dust attenuation along a ray cannot be moved to the left-hand side as was done in Equation (24). To enable a separation of variables nevertheless, we replace the variable μ with some constant average 〈μ〉 in the H i-dust term, and we then move this term to the left-hand side. For H2-dust attenuation on the right-hand side, we keep μ as a variable in the exponential term.
Making this approximation and integrating over the atomic and molecular columns gives
where
For Wg, tot as defined by Equation (64), the integration variable is N2/μ, and the integration is from 0 to ∞. Thus, the Wg, tot that appears here is the same effective total H2-dust-limited dissociation bandwidth that we defined for beamed radiation in Equation (27) (and represented analytically by Equation (28)). The effective bandwidths are identical for isotropic and beamed fields because the relative fractions of LW photons absorbed by H2-lines versus H2-dust along a ray do not depend on the ray's orientation. The product is then the effective dissociating flux for the isotropic field.
It follows from Equation (63) that the total H i column is given by
or
where again α ≡ D0/Rn, and . The total H i-dust optical depth in the normal direction is then
Equations (65), (66), and (67) for isotropic fields are very similar to Equations (39), (40), and (43) for beamed fields. The values of α are equal for corresponding beamed and isotropic fields (i.e., fields with the same IUV). Furthermore, G is independent of the field geometry. A geometrical factor of 1/4 appears for slabs irradiated by isotropic fields (as opposed to 1/2 for beamed fields).
The average angle 〈μ〉 appears in Equations (65), (66), and (67) because the radiation fraction absorbed by H i-dust does depend on the field geometry and is larger for isotropic fields for which the relative H i-dust attenuation is increased along inclined rays. In Section 3.1.5 we calculate 〈μ〉 by fitting these analytic expressions to the results of our numerical computations for the atomic columns for isotropic fields. We find that universally and to an excellent approximation 〈μ〉 = 0.8, independent of αG or Z', i.e., independent of the cloud parameters n, R, D0, or σg.
We again consider the weak- and strong-field limits.
For weak fields (αG/4 ≪ 1),
and the H i-dust opacity ∼σgN1, tot/〈μ〉 is negligible and plays no role in attenuating the LW flux. The total atomic column depends on σg only via the dissociation bandwidth Wg, tot, i.e., via the competition between H2-line absorption and H2-dust absorption. As for beamed radiation, Equation (68) is a simple Strömgren relation, and N1, tot is equal to the ratio of the effective dissociation flux (or dissociation rate per unit surface area) to the H2 formation rate. In the weak-field limit, and for a given αG and σg, i.e., for a given D0 (or F0 or IUV), n, R, and σg (or Z'), the atomic column for isotropic radiation is equal to half that produced by a corresponding beamed field. This is simply due to the factor-of-two difference in the LW photon fluxes for corresponding isotropic versus beamed fields for a given field strength IUV.
In the strong-field limit, αG/4 ≫ 1,
For strong fields, σgN1, tot ≳ 1 and the H i-dust opacity is significant and dominates the attenuation of the radiation. As for beamed fields, the total atomic column saturates, and N1, tot is insensitive to the cloud parameters except for σg. Up to the logarithmic factor of order unity, we then have
Because 〈μ〉 = 0.8, the saturation columns are only slightly smaller for isotropic versus beamed fields for large αG, and they are not very different.
3. NUMERICAL MODEL COMPUTATIONS
With our analytic results (Section 2) in mind, we now present detailed numerical calculations for the H i-to-H2 transition profiles and the associated buildup of the atomic hydrogen columns for planar clouds illuminated by either beamed or isotropic FUV LW-band radiation fields. For this purpose we use the Meudon PDR code12 (Le Petit et al. 2006) for the computation of the UV radiative transfer and depth-dependent photodissociation rates and for the steady state atomic and molecular hydrogen gas densities. The code implements the "extended spherical harmonics" method (Flannery et al. 1980; Goicoechea & Le Bourlot 2007) for an exact numerical solution of the coupled H2-line and dust scattering and absorption radiative transfer. An adaptive frequency grid is employed with sufficient resolution (Δν/ν ∼ 10−5) to capture the contributions of the narrow H2-line Doppler cores and broad wings to the total ultraviolet opacities. The competition between dust absorption and scattering and H2-line absorptions, and the important effects of H2-line overlap, are included in the calculation of the local radiation field intensities and H2 photodissociation rates.
A principal feature of the Meudon PDR code is that the radiative transfer can be calculated for either beamed or isotropic fields. We assume the Draine spectrum (Equation (2)), and we calculate models for beamed and isotropic configurations. As defined in Section 2.2, for corresponding beamed and isotropic fields the radiation energy densities at the cloud surfaces are identical (Section 2.1). We compare our numerical results with the analytic formulae discussed above.
One of our main goals is the accurate computation of the effective H2-dust-limited dissociation bandwidth Wg, tot(σg) (Equation (27)) summed over all of the LW-band absorption lines, for a wide range of FUV dust absorption cross sections σg (as set by the metallicity Z'). We also calculate H i-to-H2 transition profiles and the resulting atomic hydrogen columns from the weak- to strong-field limits (small to large αG), for both beamed and isotropic fields and for a wide range of metallicities.
For computational efficiency in our large parameter space and for direct comparisons with our analytic formulae, we have made several simplifying assumptions and modifications to the standard Meudon PDR code. First, instead of considering a full range of grain sizes and wavelength-dependent absorption and scattering properties, we assume a single representative σg for each metallicity (as given by Equation (20)), independent of photon frequency within the narrow LW band. We assume pure forward scattering by the grains and neglect the (small) effects of back-scattering discussed by Goicoechea & Le Bourlot (2007). Thus, our σg enters as a simple effective absorption cross section. We have verified by spot checks within our parameter space that our assumption of a constant σg alters the results for the computed H i columns by no more than 10% for any metallicity compared with computations incorporating a standard grain-size distribution.
Second, we decouple the H i/H2 formation–destruction equation from the complex gas and grain networks that govern the heavy element chemistry. We assume that the H2 is formed on grain surfaces only with a rate coefficient R as given by Equation (21) and is destroyed only by (depth-dependent) LW photodissociation. We exclude gas-phase formation, e.g., via the sequence H + e → H− + ν, H− + H → H2 + e,13 or destruction by cosmic-ray or X-ray secondary ionization (and we set the ionization rate ζ equal to zero). Thus, at depths where the LW radiation field is fully absorbed, the atomic density vanishes, and the entire H i column is maintained by photodissociation.
Third, we consider isothermal clouds rather than solving a heating–cooling equation for the gas temperature T. Our standard is T = 100 K, for which the H2 formation rate coefficient R = 3 × 10−17 cm3 s−1 for Z' = 1. And fourth, we assume that the total hydrogen nucleon density, n = n1 + 2n2, is a constant independent of cloud depth, so that the local H2 formation rate Rn (s−1) is also constant for any given model.
Fifth, we ignore absorption by neutral atomic carbon (C i) in the H2 photodissociation layers. The carbon (continuum) photoionization band 1100–912 Å coincides almost exactly with the LW band for H2 photodissociation, and C i, H2, and dust compete for the same photons. The carbon photoionization cross section is 1.6 × 10−17 cm−2 (van Dishoeck et al. 2006), so that the C i opacity τCI = 1.6 × 10−17AZ'NxCI ≈ 1.6 × 10−21Z'NxCI, where N is the hydrogen gas column, A ≈ 10−4 is the gas-phase carbon abundance for solar (Z' = 1) metallicity, and xCI is the fraction of carbon present in atomic form. For xCI ≈ 1, τCI is competitive with the dust opacity τg = σgN ≈ 1.9 × 10−21N. However, the carbon is primarily C+ and xCI is generally very small in the dust-limited or H2-line-limited absorption layers in which the H i columns are built up, as follows. In the absence of dust or H2 absorption, and assuming that C i absorbs the entire LW flux in maintaining an outer and optically thick C+ zone, then , where F0 = 2 × 107IUV is the ionizing photon flux (Equation (3)), α ≈ 2 × 10−11 cm3 s−1 is the electron–carbon recombination rate coefficient (Wolfire et al. 2008), is the volume density of C+ ions, ℓ is the length scale of the optically thick C+ Strömgren layer, and N is the hydrogen gas column associated with the C+ layer. We are assuming that the carbon ions are neutralized by recombination with free electrons and that . However, if the dust opacity associated with this gas column is large, i.e., if σgN ≳ 1, then the C+ layer is limited by dust and C i absorption may be ignored. The condition σgN ≳ 1 may be expressed as σgF0/[(AZ')2αn] ≳ 1, or IUV/n ≳ 5 × 10−6Z' cm3, or αG ≳ 10−3Z'. Thus, unless αG is unusually small, C i absorption is negligible. Using our PDR code, and turning on the effects of additional C+ neutralization processes such as dust-assisted recombination and chemical removal processes, we find that even for Z' = 1 the C i absorption is less than a 10% effect for αG = 0.01 and is negligible for larger αG.
Sixth, we ignore H i Lyman-series line absorption of the LW-band photons. These atomic lines (beginning with Lyβ at 1026 Å) do appear within the molecular LW absorption band (e.g., Draine & Bertoldi 1996), and the Meudon PDR code includes them. However, very large atomic columns are required for the atomic line equivalent widths to contribute significantly to the absorption. We find that an H i column of ∼1024 cm−2 is required for the summed equivalent widths of the Ly-series lines to equal half the LW bandwidth (most of this absorption is due to just Lyβ). Such large H i columns are produced only for very small values of σg and Z', even in the strong-field large αG limit. For example, for αG ∼ 100 it follows from Equation (40) that N1, tot ≳ 1024 cm−2 requires σg ≲ 3.9 × 10−24 cm2, or Z' ≲ 2 × 10−3. Thus, for the relevant range of metallicities, the atomic line absorptions can be ignored, and we exclude them in the radiative transfer.
With the above assumptions, the basic inputs to the code are the intensity, IUV, and spectral shape of the radiation field (we assume the Draine representation, Equation (2)), in either a beamed or isotropic configuration, the total gas density n, the associated H2 formation rate Rn (temperature and metallicity dependent), and the dust grain absorption cross section σg (metallicity dependent). The dimensionless parameter αG is formed from these cloud variables as described in Sections 2.2.5 and 2.2.6.
For any set of parameters the critical numerical computation is for the depth-dependent line-plus-continuum absorptions and the attenuation of the H2 photodissociation rate. For the H2, our code includes all 302 ro-vibrational vj levels in the ground electronic state and the entire matrix of Lyman and Werner transitions to discrete v'j' levels in the excited B1Σu and C1Πu states. We exclude transitions with energies greater than the hydrogen ionization energy of 13.59 eV. (As is standard, we assume that any ionizing photons are always absorbed in adjacent H ii regions outside of the PDRs.) Our code includes transitions out of excited v levels of the X state. However, for almost all conditions of interest and throughout most of the H i-to-H2 transition zones, the dominating line absorptions are from the lowest few rotational levels (j = 0 to 5) levels of the v = 0 level.14 Thus, the relevant UV transitions lie between 1108 and 912 Å, and this is the wavelength range of our "standard LW band."
The fractional populations, xvj, of the vj levels in the X state are computed assuming population and depopulation by the upward and downward X–B and X–C transitions, quadrupole radiative (cascade) transitions between the X-state vj levels, and excitations and deexcitations in collisions with He, H+, H, and other H2 molecules. We use the Abgrall et al. (1993a) and Abgrall et al. (1993b) LW-band oscillator strengths and transition wave-numbers and the Abgrall et al. (2000) probabilities for spontaneous radiative dissociations from the individual ro-vibrational levels in the excited B and C states. For the radiative quadrupole transitions, we use the Einstein-A values computed by Wolniewicz et al. (1998). For the collisional processes we use the ro-vibrational state-to-state rate coefficients reported in Le Bourlot et al. (1999) and Wrathmall et al. (2007) in their study of H2 excitation in astrophysical media.
As an example of our radiative transfer computations, we show in Figure 2 the energy density (erg cm−3 Å−1) at a cloud column depth of N = 3.74 × 1020 cm−2, or τg = 0.7 (AV = 0.2), for σg = 1.9 × 10−21 cm2 (Z' = 1) for a model computation with IUV = 35.5 (isotropic) and n = 1000 cm−3, or αG/2 = 1. At this depth the cores of the individual absorption line are very optically thick, but the continuum between the lines has not yet been significantly attenuated by overlapping line wings. Around 80 strong lines are visible in Figure 2, consistent with our analytic estimate for the number of lines involved in the photodissociation process, as discussed in Section 2.2.1.
Figure 2. Absorbed far-UV spectrum showing partially overlapping Lyman–Werner band absorption lines, for beamed radiation into a cloud, at a total hydrogen gas column density of 3.74 × 1020 cm−2, for a free-space radiation intensity IUV = 35.5, gas density n = 103 cm−3, and metallicity Z' = 1 (αG/2 = 1).
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Standard image High-resolution image3.1. Results
We now present our numerical code results for (1) the unattenuated free-space H2 photodissociation rate; (2) the curves of growth for the H2-dust-limited dissociation bandwidth Wg(N2); (3) the total dissociation bandwidth Wg, tot(σg); (4) the self-shielding function fshield(N2); and (5) the mean self-shielding factor G(Z'). We then present H i-to-H2 transition profiles and total integrated H i columns for beamed and isotropic fields and for a range of αG and metallicities Z'.
3.1.1. Free-space H2 Photodissociation Rate
The optically thin (full 4π) free-space (optically thin) H2 photodissociation rate, D0, is a fundamental parameter for ISM and galaxy evolution studies, and we have recalculated it here for the Draine FUV spectrum (Equation (2)). In Table 1, and for IUV = 1, we list the free-space UV excitation rates, Pvj (s−1) out of the 14 lowest-lying H2 (v, j) ro-vibrational levels. Each rate is summed over all upward LW transitions. We also list the mean dissociation probabilities 〈fdiss〉vj, averaged over all of the transitions, and the resulting dissociation rates, Dvj (s−1) out of each (v, j) level. Our numbers are consistent with Draine & Bertoldi (1996) (see their Table 2), who used our basic input molecular data sets.
Table 1. The H2 Excitation Rates, Pvj, Mean Dissociation Fractions, 〈fdiss〉vj, and Dissociation Rates, Dvj; for the Free-space (Optically Thin) Draine Radiation Field, Out of the Lowest 14 Ro-vibrational H2 (v, j) Levels in Order of Energy, Ei (in cm−1), Relative to the Ground (0,0) Level
(v, j) | Ei | Pvj | 〈fdiss〉vj | Dvj |
---|---|---|---|---|
(cm−1) | (s−1) | (s−1) | ||
(0,0) | 0.000 | 4.71(−10) | 0.117 | 5.51(−11) |
(0,1) | 118.505 | 4.75(−10) | 0.119 | 5.65(−11) |
(0,2) | 354.363 | 4.83(−10) | 0.123 | 5.94(−11) |
(0,3) | 705.567 | 4.95(−10) | 0.130 | 6.44(−11) |
(0,4) | 1168.825 | 5.11(−10) | 0.145 | 7.41(−11) |
(0,5) | 1740.277 | 5.30(−10) | 0.141 | 7.47(−11) |
(0,6) | 2414.852 | 5.57(−10) | 0.160 | 8.91(−11) |
(0,7) | 3187.691 | 5.86(−10) | 0.160 | 9.38(−11) |
(0,8) | 4051.884 | 6.19(−10) | 0.175 | 1.08(−10) |
(1,0) | 4161.259 | 7.14(−10) | 0.051 | 3.64(−11) |
(1,1) | 4273.913 | 7.21(−10) | 0.055 | 3.97(−11) |
(1,2) | 4497.992 | 7.31(−10) | 0.057 | 4.17(−11) |
(1,3) | 4831.595 | 7.43(−10) | 0.057 | 4.24(−11) |
(0,9) | 5002.162 | 6.58(−10) | 0.197 | 1.30(−10) |
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The total dissociation rate is weighted by the population fractions xvj but is insensitive to the gas temperature or density when the excitation is mainly out of the lowest few j levels. For T between 10 to 103 K, and for n ranging from 10 to 106 cm−3, we find that to within at most a 2% variation, D0 = 5.8 × 10−11 s−1 for IUV = 1. The dissociation rate is essentially proportional to the field intensity. For very intense fields, the rate is increased by enhanced excitation of the rotational states and photodissociation out of these states by photons longward of 1108 Å, outside our nominal LW band. For T = 100 K, and n = 100 cm−3, we find that for IUV from 1 to 103, D0 = 5.8 × 10−11ϕexIUV s−1, where the "rotational excitation factor" ϕex increases from 1 to 1.5 for this range of field intensities. We have also computed the mean flux density in the free-space radiation field, as defined by Equation (12). For the Draine spectrum, we find that photons cm−2 s−1 Hz−1 for the same range of T, n, and IUV. For the analysis we present in Section 2, we assume ϕex = 1.
3.1.2. Wg(N2) and Wg, tot(σg)
As discussed in Section 2.2.4, the "H2-dust-limited dissociation bandwidth" Wg(N2) (Equation (26)) is a fundamental quantity for the H i-to-H2 transitions and the buildup of the H i column densities.
In Figure 3 we plot our curve-of-growth computations for Wg(N2) integrated over all of the LW-band absorption lines, for σg ranging from 1.9 × 10−20 to 1.9 × 10−23 cm2, corresponding to metallicities Z' from 0.01 to 10. We set the Doppler-b parameters for all of the lines equal to a typical ISM cloud value of 2 km s−1. Our results are insensitive to the precise choice for b because the dominant absorption lines are very highly damped. We extract the Wg(N2) curves from our numerical radiative transfer computations for the radiation flux absorbed in the lines, self-consistently accounting for the flux reduction due to the presence of H2-dust. For any σg, the curve of growth Wg(N2) depends primarily on the internal molecular oscillator strengths, line profile cross sections, and dissociation probabilities for the excited states. We have verified by explicit computations that Wg(N2) is indeed very insensitive to external cloud parameters such as the field intensity IUV and/or gas density n, or temperature T. The curves of growth are also insensitive to the rotational-level distributions and ortho-to-para H2 ratio. The specific curves displayed in Figure 3 were extracted from model runs with IUV = 4, n = 105 cm−3, and T = 100 K, and for a constant ortho-to-para ratio set equal to 3 (with H+–H2 proton exchange reactions turned off).
Figure 3. Curves of growth, Wg(N2), for the dust-limited dissociation bandwidth. The far-UV dust absorption cross sections σg range from 1.9 × 10−20 to 1.9 × 10−23 cm−2. For σg = 1.9 × 10−23 cm−2 (blue curve), the H2-lines fully overlap, and Wg(N2) = Wd(N2) (see text).
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Standard image High-resolution imageFor N2 ≲ 1014 cm−2, all of the lines are optically thin, and Wg increases linearly with N2. Between 1015 and 1017 cm−2, the growth is logarithmic as the Doppler cores become optically thick. At larger columns, Wg increases more rapidly again as absorptions start occurring out of the line wings. For N2 between 1018 and 1020 cm−2, we find that Wg grows as , a bit more slowly than for a single damped line (for which it would be ).
The Wg saturates at sufficiently large H2 columns. When H2-dust is negligible, the entire LW band is absorbed in fully overlapping lines, and Wg reaches a maximal value of 9 × 1013 Hz, for N2 ≳ 1022 cm−2. In Figure 3 the absorption is essentially dust-free for σg = 1.9 × 10−23 cm2, since the lines overlap before the H2-dust opacity becomes significant, and for the (blue) curve Wg(N2) = Wd(N2) (see Sections 2.2.1 and 2.2.4). For larger σg, and for N2 ≳ 1/(2σg), the asymptotic Wg is limited by H2-dust opacity.
Figure 4 shows our results for the "total dust-limited bandwidth" Wg, tot(σg) (Equation (27)) for σg from 10−24 to 10−20 cm2. The points are our numerical results, and the solid curve is our analytic representationg
as already introduced in Section 2. This expression is accurate to within 4% compared with the numerical results. The transition from the line overlap to H2-dust-limited regimes (small to large σg) occurs at σg ∼ 7.2 × 10−22 cm2. Line overlap is just starting to become important for solar (Z' ∼ 1) metallicities. For a fully molecular slab, most of the LW-band radiation is absorbed by H2-dust for Z' ≳ 0.5. For Z' ≲ 0.5, most of the radiation is absorbed in H2-lines. Our results show that the regimes of small and large σg are both relevant for the realistic range of metallicities in galaxies.
Figure 4. Total dust-limited dissociation bandwidth Wg, tot(σg). The points are the results of our radiative transfer computations. The solid curve is our fitting formula Equation (28).
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Standard image High-resolution imageTo a good approximation for large σg as indicated by our numerical results and Equation (28). This is the expected scaling for a single (effective) damped absorption line in competition with H2-dust (see Section 2.2.4). We adopt for large σg for our analytic scaling relations in Section 2, although Wg(N2) grows somewhat more slowly with N2 than for a single line.
3.1.3. Self-shielding Function and G(Z')
By definition, the H2 "self-shielding function" , where Wd(N2) is the dissociation bandwidth for vanishing σg (see Equation (16)).
In Figure 5 we plot (solid curve) our numerically computed derivative fshield(N2). We also plot (dashed) the Draine & Bertoldi (1996) fit (their Equation (37)) for the shielding function, given by
where x = N2/5 × 1014cm−2 and b5 = b/105 cm s−1 (we assume b5 = 2). It is evident that our computed shielding function is in excellent agreement with this formula.
Figure 5. Our computed H2 self-shielding function (solid curve) and the Draine & Bertoldi (1996) fitting formula (dashed curve) as given by Equation (72) for a Doppler parameter b = 2 km s−1.
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Standard image High-resolution imageAt low N2, the lines are optically thin and fshield = 1. As the line cores become optically thick for N2 ≳ 1014 cm−2, the molecules "self-shield" and fshield decreases. By 1018 cm−2, fshield = 5 × 10−4. Between 1018 and 1020 cm−2, the shielding function declines as , as expected given the (integral) behavior of Wd(N2) in this range. Finally, at larger columns fshield drops sharply as the lines fully overlap. As found by Draine & Bertoldi (1996), the reduction due to line overlap sets in at a column of 3 × 1020 cm−2. We again see that attenuation due to line overlap becomes important for Z' ≲ 1. For such metallicities, H2-dust opacity becomes significant only at columns 1/(2σg) ≳ 3 × 1020 cm−2, at which point the lines have already overlapped and the LW photons fully absorbed.
In Figure 6 we plot the "average self-shielding factor," (Equation (41) or Equation (45)), as a function of the metallicity, assuming σg = 1.9 × 10−21Z' cm−2 (ϕg = 1). The points are our numerical results, and the curve is our analytic fitting formula Equation (46). As expected, for low metallicity (full overlap) G∝Z', but for high metallicity G∝Z'1/2 because of the H2-dust cutoff. For Z' = 10, 1, 0.1, and 0.01, we find that G equals 1.3 × 10−4, 2.8 × 10−5, 5.4 × 10−6, and 7.1 × 10−7. For these metallicities, the average self-shielded dissociation rates are D0G/2 = 3.8 × 10−15, 8.1 × 10−16, 1.6 × 10−16, and 2.1 × 10−17 s−1. As discussed in Section 2.2.6 the average is over an H2-dust optical depth τ2 ∼ 1. For low metallicities, D0G/2 becomes very small because the LW radiation is fully absorbed in lines at very low H2-dust optical depths.
Figure 6. Average self-shielding factor G as a function of metallicity Z' or dust absorption cross section σg. The points are our numerical results, and the curve is our analytic expression Equation (46).
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Standard image High-resolution image3.1.4. H i-to-H2 Transition Profiles
We now present illustrative computations for the H i-to-H2 transition profiles for a range of αG spanning the weak- to strong-field limits, and for metallicities Z' from high to low, for beamed and isotropic fields.
As discussed in Section 2.2.5, the profile shapes, i.e., the density ratios n1/n and 2n2/n as functions of the dust optical depth τg ≡ σgN (where N ≡ N1 + 2N2), depend on just the single dimensionless parameter αG ≡ D0G/Rn. This includes the locations of the H i-to-H2 transition points expressed in terms of τg. We define the transition point as the cloud depth where n1/n = 2n2/n = 0.5. For both beamed and isotropic fields we compute five transition profiles for αG/2 = 0.01, 0.1, 1, 10, and 102, for Z' = 1 and σg = 1.9 × 10−21 cm−2 (ϕg = 1). These sequences illustrate the change in profile shapes, from "gradual" to "sharp," from the weak-field (H i-dust negligible) to strong-field limits (H i-dust dominant). In these computations G = 2.8 × 10−5 as appropriate for Z' = 1, and we set D0 = 2 × 10−9 s−1 (IUV ≈ 35) and R = 3 × 10−17 cm3 s−1 (T = 100 K). To alter α and αG, we vary n from 10 to 105 cm−3.
For each αG/2 we plot the atomic and molecular fractions, n1/n and 2n2/n, as functions of the total (atomic plus molecular) column density, N. For fully atomic gas n1/n = 1, and for fully molecular gas 2n2/n = 1. For each model we also plot the normalized atomic column, , also as a function of N. Thus, at sufficiently large cloud depths where the LW radiation is fully absorbed. The curves for show how and where the atomic column is built up relative to the atomic-to-molecular transition points.
Figure 7, left panels, display the H i-to-H2 transition profiles for the five beamed-field models with varying αG.
Figure 7. H i/H2 transitions for beamed (left panels) and isotropic (right panels) radiation fields, for αG/2 ranging from 0.01 (top panels) to 100 (bottom panels). The solid curves show the atomic and molecular gas fractions, n1/n and 2n2/n, as functions of the total gas column density N into the cloud. The (blue) dashed curves are the normalized atomic columns, , as functions of cloud depth.
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Standard image High-resolution imageSeveral important features can be seen in these plots. First, the atomic-to-molecular transition points move deeper into the cloud with increasing αG. For αG/2 = 0.01, 0.1, 1, 10, and 102, the total gas columns N1 → 2 at the transition points equal 5.6 × 1017, 1.4 × 1019, 3.0 × 1020, 1.2 × 1021, and 2.4 × 1021 cm−2. For the assumed σg = 1.9 × 10−21 cm−2, these columns correspond to total dust optical depths τg = 1.05 × 10−3, 2.6 × 10−2, 0.58, 2.3, and 4.5. The H i-dust optical depths at the transition points are 9.0 × 10−4, 2.0 × 10−2, 0.45, 2.1, and 4.2. In the weak-field limit, the transition depths increase rapidly with αG. In the strong-field limit, the UV penetration is moderated by H i-dust absorption, and the transition depths increase slowly.
Second, the profile shapes vary with αG. In the weak-field limit, the atomic-to-molecular conversion is controlled by H2-line self-shielding, but significant H i exists beyond the transition point up to the H2-dust cutoff. In the weak-field limit, most of the H i column is built up past the transition point where the gas is predominantly molecular. In the strong-field limit, the transition point is controlled by (exponential) H i-dust absorption, and most of the H i is built up in an outer full atomic layer. Thus, in the weak-field limit the transitions are gradual, and in the strong-field limit the transitions are sharp. For example, at the H i-to-H2 transition points, the normalized atomic column , 0.19, 0.63, 0.85, and 0.92, from small to large αG. For αG/2 = 0.01, 92% of the total atomic column is built up past the transition point inside the molecular zone. For αG/2 = 100, only 8% of the atomic column is produced past the transition point.
Figure 7, right panels, show the transition profiles for isotropic fields for αG/2 ranging from 0.01 to 100, for Z' = 1 and σg = 1.9 × 10−21 cm2. As for the beamed-field models, the shapes of the profiles vary from gradual to sharp from the weak- to strong-field limits. The transition gas columns are N1 → 2 = 3.7 × 1017, 8.4 × 1018, 1.6 × 1020, 7.0 × 1020, and 1.6 × 1021 cm−2, or τg = 5.8 × 10−4, 1.6 × 10−2, 0.30, 1.4, and 3.0. The normalized atomic columns at the transition points are , 0.23, 0.59, 0.82, and 0.90. The H i-dust opacities are 5.8 × 10−4, 1.3 × 10−2, 0.24, 1.2, and 2.8.
For fixed αG but varying Z' and σg, we expect the profile shapes to be invariant as functions of the dust optical depth τg, and we expect the UV penetration scale lengths and transition gas columns, N1 → 2, to vary simply as 1/Z' or 1/σg. This behavior is illustrated in the upper panel of Figure 8 showing four transition profiles for Z' = 10, 1, 0.1, and 0.01 (again for beamed fields). For clarity we only plot the atomic n1/n curves. For these models we set αG/2 = (αG)CNM(Z')/2 = 1.11, 1.30, 1.28, and 1.12, as given by Equation (59) for self-regulated multiphased gas. Because αG is about the same for these models, the profile shapes are indeed very similar, and the transition columns grow inversely with Z'. For these four models, N1 → 2 = 3.0 × 1019, 3.7 × 1020, 4.0 × 1021, and 4.2 × 1022 cm−2, corresponding to dust opacities τg = 0.57, 0.70, 0.76, and 0.78. The H i-dust opacities at the transition points are 0.46, 0.56, 0.63, and 0.70. This behavior is in excellent agreement with the analytic theory presented in Section 2. For two-phased equilibrium, αG/2 ∼ 1 for all metallicities and is intermediate between the weak- and strong-field limits for which H i-dust opacity is just becoming significant.
Figure 8. H i gas fractions, n1/n, for beamed (upper panel) and isotropic (lower panel) radiation, for αG = (αG)CNM for metallicities Z' from 0.01 to 10 times solar.
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Standard image High-resolution imageFigure 8, lower panel, shows the n1/n curves for Z' = 10, 1, 0.1, and 1 for the isotropic-field models, with αG/2 = (αG)CNM(Z')/2 as for the beamed-field models. Again, because αG is about the same for all four models, the profile shapes are very similar. The transition point columns are N1 → 2 = 1.6 × 1019, 1.9 × 1020, 2.1 × 1020, and 2.2 × 1022 cm−2, or τg = 0.31, 0.36, 0.40, and 0.42. The H i-dust optical depths at the transition points are 0.25, 0.29, 0.33, and 0.37.
The transition columns and optical depths for all of the isotropic-field models are smaller than for the beamed-field models because of the factor-of-two reductions in the incident fluxes for corresponding isotropic fields with the same αG.
3.1.5. Total H i Columns
A key goal is the computation of the total atomic column densities, N1, tot, for beamed and isotropic fields for a comparison with our analytic formulae.
In Figure 9, upper panel, we display N1, tot for beamed fields, as a function of αG/2 spanning the range from 0.01 to 100, for Z' = 10, 1, 0.1, and 0.01.
Figure 9. Total H i column as a function of αG/2 for beamed (upper panel) and isotropic (lower panel) radiation, for metallicities Z' from 0.01 to 10 times solar. The square points are the numerical results, and the solid (black) curves are as given by our analytic formulae (Equations (40) and (65)). The red curves show (αG)CNM as functions of Z' for self-regulated two-phased equilibrium.
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Standard image High-resolution imageFor our numerical models, we again set D0 = 2 × 10−9 s−1 and R = 3 × 10−17Z' cm3 s−1 and vary the gas density n (to select α ≡ D0/Rn), and we set σg = 1.9 × 10−21Z' cm2. For the given input parameters D0, R, n, and σg, we compute the total integrated atomic column density and also calculate Wg, tot and the associated average self-shielding factor . For each model we compute N1, tot for the corresponding αG and σg. The points in Figure 9 are our model results for selected αG and Z'. Again, for the four metallicities, G = 1.3 × 10−4, 2.8 × 10−5, 5.4 × 10−6, and 7.1 × 10−7. The curves in Figure 9 are as given by our fundamental analytic formula for beamed fields
where 1/σg = 5.3 × 1020/Z' cm−2 as for the numerical models.
Our analytic and numerical results are in excellent agreement from the weak- to strong-field regimes. For weak fields (high gas densities), (Equation (52)). In this regime the total atomic column is proportional to the field intensity (dissociation flux) and varies inversely with the gas density. For strong fields (low densities), the dependence is logarithmic and N1, tot = (1/σg)ln(αG) (Equation (54)). In this regime the atomic column is weakly dependent on IUV/n, and it is limited to values close to 1/σg because of the dominating H i-dust absorption. For example, for Z' = 1 and αG/2 = 0.01, 0.1, 1, 10, and 100, our model computations give N1, tot = 5.6 × 1018, 5.3 × 1019, 3.8 × 1020, 1.2 × 1021, and 2.4 × 1021 cm−2, as also given by our analytic formula.
Expressed as a function of αG, N1, tot∝1/Z'. However, we recall that for large σg (Z' ≳ 1), αG is itself metallicity dependent and αG∝Z'1/2 (see Equation (51)). Thus, for high metallicities in the weak-field limit, N1, tot∝Z'−3/2. In this regime the column decreases by one power of Z' because of enhanced H2 formation efficiency and decreases by an additional factor of Z1/2 because of the reduction of the effective dissociation flux by the H2-dust. For low metallicities in the weak-field limit, the dissociation flux is maximal, and N1, tot∝Z'−1. In the strong-field limit, the atomic column is only weakly (logarithmically) dependent on αG, and the metallicity dependence is mainly via the H i-dust opacity, and N1, tot∝Z'−1 for all metallicities. These metallicity scalings, discussed in Section 2.2.8, are validated by our numerical model results for the atomic column.
In Figure 9 we also plot a (red) curve for (αG)CNM(Z') as given by Equation (59) for self-regulated multiphased H i. As is again illustrated in Figure 9, (αG)CNM(Z')/2 ∼ 1. Given the assumptions underlying Equation (59), the H i columns for self-regulated multiphased gas are intermediate between the linear (weak-field) and logarithmic (strong-field) regimes for all metallicities.
Our computational results show that our analytic expression for N1, tot is valid for all transition profile shapes, whether gradual (weak fields) or sharp (strong fields), regardless of where the atomic column is built up (whether in the molecular zone or in the outer fully atomic layer). Indeed, in our analytic derivation we did not make any assumptions on the profile shape. Our expression is universal and valid for all regimes (weak and strong fields, high and low metallicities) and for all transition profile shapes (gradual or sharp). We emphasize this point again in our alternate derivation via the KMT/MK10 "transfer-dissociation equation" (Section 4.1.1).
In Figure 9, lower panel, we plot the total atomic columns for our isotropic-field models. For these models we select D0 and R, and vary n to set α, and we compute the total H i column. As discussed in Section 3.2, the total dust-limited dissociation bandwidth, Wtot, and the average self-shielding factor, G, are identical for beamed and isotropic fields. In Figure 12 we plot N1, tot as a function of αG, where for each Z' we use the G(Z') computed using beamed fields. Again, αG ranges from 0.01 to 100, and we present results for Z' from 10 to 0.01. The (αG)CNM(Z') curve is also displayed. In Figure 9, the points are our numerical results, and the curves are as given by our fundamental analytic formula for isotropic fields (Section 2.3),
where again 1/σg = 5.3 × 1020/Z' cm−2. To obtain the match between the numerical results and analytic formula shown in Figure 9, we have fit for the average angle factor 〈μ〉. We find that
provides an excellent fit for all αG and for all σg∝Z'.
For isotropic fields in the weak-field limit, (Equation (68)). As discussed in Section 2.3, this is half the column for the corresponding beamed field because of the factor-of-two difference in the incident dissociation fluxes. For weak fields, N1, tot is independent of 〈μ〉. In the strong-field limit, N1, tot = (〈μ〉/σg)ln(αG/4〈μ〉) (Equation (69)), and the column is reduced by the factor 〈μ〉 = 0.8 compared with beamed-field models (neglecting the small difference in the logarithms). For example, for Z' = 1 and αG/2 = 0.01 0.1, 1, 10, and 100, our model results for the total atomic column are 3.1 × 1018, 2.9 × 1019, 2.1 × 1020, 7.7 × 1020, and 1.6 × 1021 cm−2, smaller in the expected way compared with beamed-field models. The linear and logarithmic behaviors for small and large αG∝IUV/n and the scaling with Z' are identical for isotropic and beamed fields.
Our expression for the total column for isotropic fields is also valid for all profile shapes, from gradual to sharp.
4. COMPARISON WITH KMT/MK10
In a series of papers, Krumholz et al. (2008, 2009) and McKee & Krumholz (2010; hereafter KMT/MK10) considered the interstellar atomic-to-molecular transition in the context of galaxy-wide conditions for star formation. For this purpose, KMT/MK10 developed analytic models for the H i-to-H2 transitions in spherical clouds irradiated by isotropic radiation fields. They also considered planar models. KMT/MK10 were particularly interested in exploring the role of metallicity in setting star-formation thresholds, and in MK10 they applied their spherical models to compute metallicity-dependent H2 mass fractions in star-forming clouds as functions of the gas mass surface densities in galaxy disks. The integral H2 mass fraction, , may be a critical parameter in galaxy-wide Kennicutt–Schmidt (KS) relations, especially if conversion to H2 is required for star formation.15 For spheres, , where and Mgas are the molecular and total gas masses within the volumes. For slabs , where and Σgas are the molecular and total gas mass surface densities in the normal directions.
The assumption of spherical versus plane-parallel geometry complicates the analysis and computation of the H i-to-H2 transition because for spheres oblique rays cross through the clouds even when optically thick H2 cores are present. Optically thick slabs are simpler because all rays are absorbed. To proceed, KMT/MK10 made the simplifying assumption that the H i-to-H2 transitions are always sharp, such that any atomic layer has a well-defined length scale. For the spheres, fully atomic and dusty H i shells are then assumed to surround fully molecular H2 cores. Rays that cross through the H i shells are either unattenuated or are absorbed by dust, or by H2-lines under the assumption that the molecular fractions in the shells are small. Rays that impinge on the H2 cores are fully attenuated. MK10 employ a "variable Eddington factor" formalism to close the angular moments of the radiative transfer equation for the radiation fields in the H i shells. For a given total cloud mass and radiation field intensity, a complicated iterative procedure then yields the spherical and nested H i/H2 structures, and associated H2 mass fractions.
KMT/MK10 implicitly assumed that the H2-lines are always in the fully overlapping regime, independent of Z' and σg, and they did not consider the possible reduction of the effective dissociation bandwidth by H2-dust. KMT/MK10 did not make the distinction between H i-dust and H2-dust that we have been emphasizing.
According to KMT/MK10, the spherical H i/H2 "shell–core" structures depend on two dimensionless parameters, "χ" and "τr." In their definition, "χ/f1 is the ratio of the number of LW photons absorbed by dust to the number absorbed by H2," where f1 is the fraction of gas in atomic form. As we clarify below, χ is actually identical to our αG in the low-Z', small-σg, (w = 1) limit where H2-dust absorption is negligible. The second parameter, τr ≡ nσgr, is the "dust optical depth associated with the cloud radius r," where n is the hydrogen nucleon density at the cloud surface. For a slab (of finite width) the corresponding second parameter is the total dust optical depth τz ≡ σgnz through the slab, where z is the linear extent. The parameters τr and τz will enter into our discussion of the H2 mass fractions for spheres and slabs (Section 4.2).
We wish to compare our analytic theory for the H i column densities for planar clouds with the KMT/MK10 formulae for spheres. This will enable us to also compare results for the H2 mass fractions. We will show that any differences between corresponding (i.e., properly normalized) slabs and spheres are very small and that it is therefore advantageous to use our much simpler and fully analytic plane-parallel formalism.
We start (in Section 4.1) by clarifying the relationship between the KMT/MK10 χ and our αG. To do this we reanalyze the "transfer-dissociation equation" presented by Krumholz et al. (2008). This also enables a comparison of our formulae for the H i columns with KMT/MK10's similar, though not identical, expressions for the atomic columns for planar geometry. In Section 4.2.1 we develop a simple expression for for optically thick slabs for two-sided irradiation using our analytic expressions for the total H i-dust optical depths for one-sided irradiation of semi-infinite clouds, for isotropic or beamed fields. In Section 4.2.2 we re-express the MK10 formulae for uniform density (isochoric) spheres and (isobaric) "atomic–molecular complexes" for (1) the critical H i-dust optical depths required for the formation of H2 cores and (2) the H2 mass fractions as functions of the total cloud optical depths (or gas masses). This will enable a clear comparison with our expressions for slabs.
We find that for corresponding spheres and slabs embedded in isotropic fields, the predicted H i columns are very similar. The differences are no greater than 20% for αG ranging from 0.01 to 100. For two-phased H i equilibria for which αG/2 ∼ 1, the differences between spheres and slabs are negligible, and the H i columns for spheres and slabs are essentially identical. In fact, we show that switching from a beamed to an isotropic field for a slab is much more significant than switching from a slab to a sphere for a fixed isotropic field. We then show that for proper normalization of the three configurations—uniform sphere, complex, or slab—the predicted H2 mass fractions as functions of total cloud masses or columns are also very similar.
4.1. χ and αG
To clarify the relationship between the KMT/MK10 χ and our αG, it is useful to consider the "transfer-dissociation equation" developed by Krumholz et al. (2008), here for beamed radiation into a slab. This discussion will also provide an alternate derivation of our fundamental formula (Equation (40)) for the total H i column density.
4.1.1. Transfer-dissociation Equation
Let Fν(z) be the flux density (photons cm−2 s−1 Hz−1) at frequency ν of beamed LW radiation at linear depth z into a slab. The radiation flux (cm−2 s−1) between frequencies ν1 and ν2 is then
At the cloud surface F(0) = F0/2, where F0 is the flux integral (our Equation (3)) for the free-space radiation field.
The transfer equation for F(z) is
Here n ≡ n1 + 2n2 is the total (atomic plus molecular) hydrogen gas volume density, and σν is the ("complicated") cross section for the multiline H2 absorption process.16 The first term on the right-hand side of Equation (77) is the dust absorption rate of the local radiative flux. The second term is the H2-line absorption rate.
The steady state H2 formation–destruction equation is
where in this expression, (as defined in Section 2) is the mean fraction of all H2-line absorptions that lead to photodissociation. Following Krumholz et al. (2008) and our discussion in Section 2, we assume that is independent of cloud depth.
The "complicated" integral in Equation (77) may be eliminated to give the transfer-dissociation equation (Krumholz et al. 2008)
In dimensionless form
where is the normalized depth-dependent flux, τ ≡ nσgz is the dust optical depth, and f1(τ) ≡ n1/n is the depth-dependent fraction of gas in atomic form.
In Equation (80)
This is the KMT/MK10 χ, here introduced for one-sided irradiation of a slab by a beamed field with incident LW flux F(0) ≡ F0/2.17 Compared with our Equation (48) it is already clear that χ = αG for w = 1.
Because the product σgnF0 is the dust absorption rate per unit volume of the surface LW radiation flux, and because is the H2-line absorption rate per unit volume, KMT/MK10 interpret χ/f1 as the ratio of the number of LW photons absorbed by dust to the number absorbed by H2-lines at the optically thin cloud surface (with one factor of n canceling when doing the division). In this interpretation, the dust absorption being referred to in the numerator is independent of whether the gas is atomic or molecular.
However, as we now show, if the dust absorption term in the transfer-dissociation equation is redefined to refer to H i-dust absorption only, we will recover our fundamental formula for the H i column density, including a method for "renormalizing" the dissociation flux to account for H2-dust absorption. We demonstrate this by analyzing the transfer-dissociation equation in the following three steps.
4.1.2. Step 1: Transition Assumed Sharp
First, we assume—as done by KMT/MK10—that the atomic-to-molecular transition is always sharp. We impose this assumption even though we know that it is good only if our αG ≫ 1, i.e., only if F0/n and χ are sufficiently large. Nevertheless, in seeking a solution for Equation (80), we assume that for any χ the atomic fraction f1 = 1 everywhere is non-zero, up to the (unknown) transition point where vanishes. At that point the gas switches suddenly from H i to H2.
Setting f1 = 1, the solution to Equation (80) is
It is evident that the flux vanishes for τ = τ1, tot, where
and this is then the solution for the transition point (Krumholz et al. 2008). The total atomic column density up to the transition point is
because by assumption there is no H2 in the photodissociated layer and τ1 is the optical depth due to H i-dust only.
We immediately recognize Equations (83) and (84). They are identical to our expressions (40) and (43) for the total H i-dust optical depth and H i column density, except that here the argument is χ, as given by Equation (81), rather than our αG as defined by the similar but not quite identical Equation (48). Indeed, it is apparent that αG = wχ, where w is the normalized effective dissociation bandwidth as defined by Equation (31). (This identity is clarified in Step 3.)
For χ ≫ 1, the attenuation of the LW flux is dominated by dust absorption, and . An exponentially attenuating flux is precisely what produces a sharp transition profile. Therefore, for χ ≫ 1 the assumption that the transition is sharp is consistent. Furthermore, the exponential attenuation is due specifically to H i-dust absorption. Sharp profiles occur when H i-dust dominates the attenuation.
For χ ≪ 1, dust absorption is negligible compared with H2-lines, τ ≪ 1 throughout the atomic layer, and to first-order in τ. For small χ, Equation (83) gives τ1, tot = χ/2, so that
in this limit. However, when H2-lines dominate the attenuation the transition is not sharp, and the assumption that f1 = 1 is inconsistent.
Nevertheless, as we now show in Step 2, the above expressions for , τ1, and for large and small χ are valid for any varying f1, whether or not the H i/H2 transition is sharp, provided that H2-dust is always negligible compared with H i-dust or H2-lines, so that τ in Equation (80) can be redefined as the optical depth associated with H i-dust absorption only.18
4.1.3. Step 2: H2-dust Negligible, and τ Redefined
With the neglect of H2-dust absorption, Equation (79) is
where now n has been replaced by n1 in the first term on the right-hand side, or
where χ is again given by Equation (81) but where now
is defined in advance as the optical depth associated with H i-dust only.
In Equations (86) and (87), a factor f1 ≡ n1/n does not appear. The solutions are still given by Equations (84) and (85) for large and small χ but now with no assumptions on the shapes of the transition profiles.
For large χ the transition is sharp because the radiation flux is attenuated exponentially by the H i-dust, as shown in Step 1. However, for low χ, for which τ1, tot is small, the transition need not be sharp. In this limit we again have,
But this is just a Strömgren relation (as also noted by MK10). Therefore, it must hold independent of the shape of the H i/H2 profile, provided only that the entire incident dissociation flux, , is fully absorbed by H2-lines, which it indeed will be for small τ1, tot. Again, RnN1, tot is the integrated H2 formation rate per unit area, and in steady state this equals the fully absorbed dissociation flux impinging on the surface, independent of profile shape. In fact, we know that for low χ (i.e., for small F0/n and αG) the transition profile is gradual, with most of the H i column built up in the molecular zone, as we have shown and discussed in Section 3.
Although Krumholz et al. (2008) derived their expression (83) for the dust optical depth assuming a sharp transition, it is actually valid for all χ, large and small, for sharp and gradual atomic hydrogen profiles, provided that H2-dust absorption is negligible compared with H i-dust and H2-lines.
4.1.4. Step 3: H2-dust and Renormalization of the Dissociation Flux
We now include H2-dust. In Equations (79) and (80), the original dust absorption term, nσgF, is not necessarily negligible—even when χ ≪ 1—if the atomic fraction f1 is sufficiently small. This is the regime where H2-dust absorption may be significant, even if H i-dust is negligible.
Because of H2-dust absorption of radiation "between the lines," not all of the photons in the LW band are absorbed by the H2, even for a fully molecular slab. The effective dissociation flux is then smaller than . The Strömgren relation then implies that for χ ≪ 1 the total H i-dust optical depth τ1, tot must be smaller than χ/2, rather than equal to χ/2 as given by Equation (89).
If τ is redefined to refer to H i-dust only as in Step 2, the effect of H2-dust absorption can be included in the transfer-dissociation equation by a simple "renormalization" of the effective dissociation flux. We replace F0/2 with a suitably reduced wF0/2 equal to the flux of LW photons absorbed in H2-lines in a dusty molecular slab, excluding in advance photons that are inevitably absorbed by H2-dust. The renormalization factor can be computed in advance for any given σg, and we immediately recognize w as the (normalized) effective dissociation bandwidth that we defined and computed in Sections 2 and 3.
The transfer-dissociation equation for the renormalized LW flux is
where again the dust term on the right-hand side refers to H i-dust absorption only. Photons absorbed by H2-dust anywhere in the slab are excluded from consideration "in advance."
In dimensionless form
where , dτ ≡ n1σgz, and
We see that χ' is just our αG (Equation (48)). Thus,
as already indicated in Step 1.
Most importantly, in Equations (90) and (91) a factor "f1" does not appear at all. The solution is
where τ is the H i-dust optical depth, and there are no assumptions on the shape of the H i-to-H2 transition profile. The flux vanishes for τ = τ1, where
and the expression for the total atomic column is then
We have thus recovered our original expressions (39) and (40) for the total atomic column and H i-dust opacity for beamed radiation into a slab. It is again clear that these expressions are general. They are valid for large or small αG (strong or weak fields) for the regimes of significant H i-dust and/or H2-dust absorption and are independent of the profile shapes (gradual or sharp). We also have in Equation (94) a closed-form expression for the depth-dependent LW-band flux as a function of the H i-dust optical depth.
We again see that αG is the fundamental dimensionless parameter. Physically, αG is the ratio of the H i-dust to H2-line absorption rates of the effective dissociation flux, excluding any LW photons that are absorbed by H2-dust. The relationship between χ and our αG is now clear. Specifically, wχ ≡ αG, where crucially our factor w accounts for H2-dust absorption and the resulting reduction of the effective dissociation flux. In the low-Z', small-σg limit, H2-dust is negligible, w = 1, and χ = αG. For high Z' and large σg, w < 1 (decreasing as or as Z'−1/2), and then αG < χ. KMT/MK10 did not make the distinction between H i-dust and H2-dust and ignored the effects of H2-dust entirely in their definition of χ. As we have discussed in Sections 2 and 3, H2-dust can reduce the effective dissociation bandwidth by a factor ∼4 for the (realistic) range of metallicities in galaxies.
In Figure 10 we again schematically summarize the four regimes that are incorporated by our formula for the total H i column density. In each quadrant, large or small αG for large or small Z', we indicate the shape of the H i-to-H2 transition (sharp or gradual), the dominant source of opacity (H i-dust, H2-lines, or H2-lines plus H2-dust), and the expression for the H i-dust opacity in terms of the parameters σg, F0, Rn, and w.
Figure 10. Dominant sources of far-UV absorption (H i-dust, H2-lines, and H2-dust), H i-to-H2 transition profile shapes (gradual or sharp), and total H i-dust opacities (large or small), in the vs. Z' plane.
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Standard image High-resolution image4.2. Critical H i-dust Opacities and H2 Mass Fractions: Slabs versus Spheres
4.2.1. Slabs
Given our expressions (Equation (40) or Equation (65)) for the total H i-dust optical depths in semi-infinite slabs, we can write down a simple formula for the integrated H2 mass fraction, , for planar geometry for a comparison with the KMT/MK10 results for spheres. Our main focus is a comparison of slabs and spheres irradiated by isotropic fields, but we also consider beamed radiation for slabs.
For an isotropic field with a given IUV, a uniformly illuminated sphere corresponds to two-sided irradiation of a slab of finite width, with properly normalized total optical depths for the sphere and slab. For a slab with total dust thickness τz ≡ σgnz = σgN (where N is the total gas column density in the normal direction), the H2 mass fraction is simply
where y ≡ τz/τ1, and τ1 is the H i-dust depth summed over both sides of the slab (the superscript "p" indicates plane-parallel slab). By definition, y ⩾ 1. We plot versus y in Figure 11.
Figure 11. H2 mass fractions as given by Equations (97), (100), and (102), for plane-parallel slabs ("p"), uniform-density spheres ("s"), and complexes ("c"), as functions of the normalized H i-dust optical depth y.
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Standard image High-resolution imageFor optically thick slabs in which the radiation incident on both sides is fully absorbed, and for illumination by isotropic fields, , where
This is twice the optical depth given by our Equation (66) for one-sided illumination of a semi-infinite slab. (We have set 〈μ〉 = 0.8, as found in Section 3.) For beamed radiation , where
given our Equation (39) for one-sided illumination (the superscript "b" is for beamed radiation). We plot and versus αG in Figure 12.
Figure 12. Critical (total) H i-dust optical depths; for beamed fields into a slab (dot-dashed), for isotropic fields into a slab (dotted), and 〈τ1〉 for critical spheres in isotropic fields (dotted), as functions of αG/2, as given by Equations (99), (98), and (101).
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Standard image High-resolution imageFor two-sided illumination of optically thick slabs, Equation (97) for together with Equation (98) or Equation (99) for the total H i-dust optical depths may be used to compute the integral H2 mass fractions whether the H i-to-H2 transitions are gradual or sharp. For αG ≫ 1, an optically thick slab consists of a simple H i-H2-H i sandwich structure, with two fully atomic layers outside an inner H2 zone, with sharp transitions between the atomic and molecular layers. For sharp transitions a "critical" optically thick slab occurs for y = 1 for which an H2 layer just appears at the midplane, and or are then the critical H i-dust optical depths. The planar sandwich for sharp transitions corresponds to the spherical core–shell structures considered by KMT/MK10, as illustrated in Figure 13.
Figure 13. Corresponding shell–core structures for spheres and sandwich structure for slabs, for sharp H i-to-H2 transitions and illumination by isotropic radiation.
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Standard image High-resolution image4.2.2. Spheres
MK10 carried out their iterative radiative transfer procedure to compute spherical H i shell and H2 core structures for two types of systems. First, they considered "uniform density" spheres for which the density of hydrogen nuclei, n = n1 + 2n2, is constant through the spheres as in our slabs. Second, they considered "atomic–molecular complexes" in which the H2 gas density, n2, is 10 times the atomic density, n1, for approximate pressure equilibrium between the shells and the cores. MK10 then presented fitting formulae (their Equations (82) and (93)) for in uniform density spheres and complexes, as functions of their cloud parameters χ and τr.
We can re-express the MK10 formulae for as simple functions of y, similar to our Equation (97) for slabs. For spheres y ≡ 〈τ〉/〈τ1〉, where 〈τ〉 ≡ σg〈N〉 is the area-averaged total dust column density of the sphere and where 〈N〉 ≡ Mgas/mπr2 is the average gas column density, r is the cloud radius, and m is the mean particle mass per hydrogen nucleon. For a uniform density sphere, the total optical depth 〈τ〉 = 〈τr〉 ≡ (4/3)σgnr. For a complex, 〈τ〉 ⩾ (4/3)σgn1r ≡ 〈τr〉, where n1 is the gas density in the atomic shell. The parameter y is defined such that the total optical depth 〈τ〉 is normalized relative to the critical (area-averaged) dust depth 〈τ1〉 required for the appearance of an H2 core at r = 0. The critical depths 〈τ1〉 are auxiliary quantities also computed by MK10 for the uniform density spheres and complexes, assuming irradiation by isotropic radiation fields. The 〈τ1〉 for spheres correspond to our for two-sided illumination of slabs by isotropic fields. In our terminology, these are the (total) H i-dust optical depths in spheres and slabs. For sharp transitions these are critical optical depths.
The MK10 fitting formula (their Equation (82)) for the H2 mass fraction in uniform density spheres may be rewritten as19
(where the superscript "s" is for spheres). Their critical H i-dust optical depth is
Again, in Equation (100) y ≡ 〈τ〉/〈τ1〉. In Figures 11 and 12 we plot versus y and 〈τ1〉 versus αG for comparisons with our expressions for slabs.
For complexes, the MK10 fit formula for the H2 mass fraction (their Equation (93)) may be rewritten as20
(The superscript "c" is for complexes.) Fully atomic complexes and uniform density spheres are identical, so the critical H i-dust depth 〈τ1〉 for complexes is also given by Equation (101). Because of the compression of the molecular gas, the functional form for is altered compared with uniform density spheres, and the y−1.8 factor in the denominator of Equation (100) is replaced by unity in Equation (102). We also plot for the complexes in Figure 11.
Figure 12 shows the similarity in the critical H i-dust optical depths for slabs and spheres. For isotropic fields, and for αG ranging from 0.01 to 102, the differences are no greater than 20%. Furthermore, Figure 12 shows that switching from isotropic to corresponding beamed radiation for a slab is in fact much more significant than switching from a slab to a sphere for an isotropic field. For isotropic fields, the H i-dust optical depths for slabs and complexes are equal for αG ≈ 1.5, so for two-phased H i equilibrium ([αG]CNM/2 ∼ 1) the differences between the H i-dust optical depths for spheres and slabs are negligible. Thus, for αG ∼ 1 any differences between spheres and slabs arise only because of any remaining differences in the functional forms for .
Figure 11 shows the similarity and small differences in for slabs, uniform-density spheres, and complexes, as given by Equations (97), (100), and (102). For slabs, our formula (97) for is unaltered if the molecular gas is assumed to be denser than the atomic gas, and there is no distinction between uniform-density and isobaric conditions. The differences are all small. For example, for a spherical complex compared with a slab, the percentage difference in is at most 40% at y = 3.
4.2.3. H2 Mass Fractions and Star-formation Thresholds in Self-regulated Gas
If H2 is a requirement for star formation, we may define the cloud gas column at which as the "star-formation threshold." This is a plausible definition for sharp H i-to-H2 transitions for which a "sterile" atomic layer is well defined. As given by Equations (97), (100), and (102), for y = 2, 2.93, and 2.5, for slabs, uniform density spheres, and complexes. We define Σgas, * as the threshold gas mass surface density for which .
For estimates of metallicity-dependent H2 mass fractions and star-formation thresholds in Kennicutt–Schmidt relations for galaxy disks, we adopt the KMT/MK10 "self-regulation" ansatz that the H i in star-forming clouds is typically driven to the CNM densities/pressures required for two-phase equilibria as set by the stellar FUV radiation fields. Thus, for any Z' we assume that αG = (αG)CNM(Z') (Equation (59)). Because (αG)CNM ∼ 1 to 2 for all Z', the H i-to-H2 transitions are sharp to a good approximation (as argued by KMT/MK10). For our slabs we therefore assume H i-H2-H i sandwich structures, for which critical optically thick slabs occur at y = 1 (as discussed in Section 4.2.1).
We present four sets of computations to compare results for spheres versus slabs.
First, in Figure 14, panel (a), we use Equations (102) and (101) to reproduce the MK10 results for for spherical atomic–molecular complexes (Figure 5 in MK10). Here Σgas ≡ (m/σg)〈τ〉 is the area-averaged gas mass surface density, where m is the mean particle mass per hydrogen nucleus and 〈τ〉 is the area-averaged dust opacity. Thus, in Equation (102) y = Σgas/Σ1, where Σ1 ≡ (m/σg)〈τ1〉, and where 〈τ1〉 is given by Equation (101) for each (αG)CNM(Z'). We set m = 2.34 × 10−24 g as appropriate for a cosmic hydrogen–helium mixture. KMT/MK10 assume that the dust cross section scales with metallicity as σg = 1.0 × 10−21Z' cm2, so we set our ϕg = 1/1.9 (see Equation (20)). MK10 also implicitly assume that H2-dust absorption is negligible for all Z', so we exclude our H2-dust term, (2.64ϕgZ')1/2, in the denominator of Equation (59). The resulting curves for as functions of Σgas (M☉ pc−2) are displayed in Figure 14 for Z' ranging from 0.01 to 10. They are a precise reproduction of the MK10 results (their Figure 5). For example, with the above assumptions, Z' = 1 gives (αG)CNM = 3.6 so that 〈τ1〉 = 1.3, and a molecular core appears (y = 1) for Σgas = 14.6 M☉ pc−2. The star-formation threshold (y = 2.5) is then Σgas, * = 36.5 M☉ pc−2. For smaller (larger) Z', the curves shift to the right (left) exactly as in Figure 5 of MK10.
Figure 14. H2 mass fractions as functions of total gas mass surface density for metallicities Z' from 0.01 to 10 times solar. (a) Spherical complex, with σg = 1.0 × 10−21Z' cm2 and excluding H2-dust absorption in setting (αG)CNM, as assumed by MK10. (b) Spherical complex with σg = 1.0 × 10−21Z' cm2 but including H2-dust. (c) Plane-parallel slab, with the MK10 relation σg = 1.0 × 10−21Z' cm2 and excluding H2-dust. (d) Slab with σg = 1.9 × 10−21Z' cm2 and including H2-dust.
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Standard image High-resolution imageSecond, in Figure 14, panel (b), we show results for spherical complexes, again with ϕg = 1/1.9 but now with the H2-dust term included in the estimate for (αG)CNM(Z'). As expected, for very low Z' the curves and the corresponding star-formation thresholds are unaltered, since this is the complete line overlap regime for which H2-dust is negligible. However, for Z' ≳ 0.3 the curves start to shift to the left and the thresholds are reduced to smaller gas mass surface densities. These shifts are due to the reductions of the effective dissociation fluxes by the non-negligible H2-dust opacities. For example, when H2-dust is included for Z' = 1 we have (αG)CNM = 1.6 (for ϕg = 1/1.9) so that 〈τ1〉 = 0.77, and the H2 core appears at Σgas ≃ 8.6 M☉ pc−2 and Σgas, * = 21.5 M☉ pc−2. The inclusion of H2-dust in the estimate for (αG)CNM modifies the MK10 results for solar and super-solar metallicities.
Third, in Figure 14, panel (c), we again adopt the MK10 assumptions, ϕg = 1/1.9 and negligible H2-dust for any Z' but for slabs instead of spheres, and we use Equation (97) to compute . Here Σgas = (m/σg)τz, where τz is the total dust depth of the slab, so that y = Σgas/Σ1 where , and the critical H i-dust optical depth is given by Equation (98) for each (αG)CNM(Z'). We have already seen that the functional forms for the mass fractions are very similar for complexes and slabs (with at most a 40% difference at y = 3) and that the critical H i-dust columns are essentially equal for αG ∼ 1 (as for self-regulated gas). It is therefore not surprising that the curves for slabs are almost identical to the MK10 results in Figure 14. For Z' = 1, we again have (αG)CNM = 3.6 so that and H2 appears for Σgas ≃ 13.4 M☉ pc−2 and the star-formation threshold (y = 2) is at Σgas, * = 26.8 M☉ pc−2. For metallicities Z' ≳ 0.3, the neglect of H2-dust in setting (αG)CNM is more significant than switching from spherical to plane-parallel cloud geometry.
In Figure 14, panel (d), we again present results for slabs but now with our preferred and somewhat larger σg = 1.9 × 10−21Z' cm2 (ϕg = 1) and with the inclusion of H2-dust absorption in setting (αG)CNM(Z'). The curves and thresholds are shifted to lower gas mass surface densities compared to Figure 14. For Z' = 1, we now have (αG)CNM = 2.6, given that , so that H2 appears at Σgas = 5.6M☉ pc−2 and the star-formation threshold surface gas mass density is Σgas, * = 11 M☉ pc−2.
Finally, in Figure 15 we plot Σgas, *(Z') for the above four model sets. At any Z' the star-formation thresholds vary by factors of 2–3 for the four model assumptions, for Z' between 0.01 and ∼2. Again, we are assuming that αG = (αG)CNM(Z') for which the critical H i-dust optical depths are all of order unity. The threshold gas mass surface densities therefore scale as ∼2m/σg, and we have
For Z' ∼ 1, the star-formation thresholds are of order 10 M☉ pc−2.
Figure 15. Star-formation threshold gas mass surface density Σgas, * at which the H2 mass fraction for the four models, (a), (b), (c), and (d), in Figure 14 (see text).
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Standard image High-resolution imageThe predicted H i columns and star-formation thresholds appear consistent with observations, at least for ∼solar metallicity systems. For example, in a recent GALFA-H i study of the H i-to-H2 transition on sub-parsec scales in the Perseus giant molecular cloud, Lee et al. (2012) find an almost constant H i surface density of M☉ pc−2 in each of the mapped sub-regions. For Z' = 1, this is consistent with the H i columns expected for αG of order unity, including conditions appropriate for two-phased equilibrium. Thus, Perseus is in the H i-dust-limited and strong-field regime. On larger scales, Leroy et al. (2008) find a mean total gas column of 14 M☉ pc−2 at the H i-to-H2 transition radii (see their Table 5) in their analysis of the H i and CO distributions in the THINGS and HERACLES galaxy surveys. The observed threshold column density of 14 M☉ pc−2 is in harmony with our 1D predictions or the spherical KMT/MK10 models (see Figure 15). However, in this interpretation there must be typically one primary UV absorbing cloud (GMC) per line of sight in the galaxy surveys, with negligible additional diffuse H i, since our predicted thresholds are for single cold clouds.
5. RECAP AND SUMMARY
In this paper we have presented analytic theory and numerical computations for the atomic-to-molecular (H i-to-H2) transitions, and the buildup of atomic hydrogen (H i) gas columns, in the PDRs of optically thick interstellar clouds illuminated by photodissociating FUV LW radiation fields. We have focused on simple idealized uniform density (1D) planar slabs that fully absorb the incident radiation. This enables a Strömgren type analysis (Sternberg 1988, "S88") for the total steady state column density of H i that is maintained by the incident photodissociating flux. The behavior is more complicated than for classical (dust-free) photoionized H ii regions, (1) because H2 photodissociation is a (multi-)line absorption process and (2) because of the generally inevitable competition between H2-line absorption, H2-dust absorption, and H i-dust absorption of the LW photons.
As discussed in Section 1, the H i-to-H2 transition in interstellar gas has been investigated by numerous authors over many years, with varying levels of analytic and numerical sophistication. In this paper we extend the analytic theory developed in S88 and consider 1D slabs irradiated by either beamed or isotropic fields. The beamed configuration is appropriate for clouds near a localized radiation source. Isotropic irradiation may be more appropriate for ambient or "global" conditions in galaxies. In our theoretical development we make the important distinction between H i-dust and H2-dust absorption, which is not previously discussed in the literature. The three-way competition between H i-dust absorption, H2-dust absorption, and H2-line absorption determines the behavior and dependence of the atomic column density on the environmental parameters.
Our analytic formulae and results are developed in Section 2 and verified in Section 3 with detailed numerical radiative transfer computations, including for the H2-dust-limited dissociation bandwidth. In Section 4 we compare our results to models that assume spherical symmetry.
To conclude this paper, we recap our basic results as follows.
The fundamental dimensionless parameter in the problem is
(See also expressions (49) and (50).) Here IUV is the free-space FUV intensity (relative to the Draine field), D0 is the free-space (optically thin) H2 photodissociation rate (s−1), n is the total hydrogen gas volume density (cm−3), R is the H2 formation rate coefficient (cm3 s−1), G (dimensionless) is the mean self-shielding factor, σg is the FUV continuum dust absorption cross section (cm2), is the mean photon flux density (cm−2 s−1 Hz−1) in the (912–1108 Å) LW band, F0 is the total LW photon flux (cm−2 s−1), is the mean dissociation probability, Z' is the metallicity relative to solar, Wg, tot is the total H2-dust-limited dissociation bandwidth (Hz), w (dimensionless) is the normalized bandwidth, and ϕg is a factor of order unity depending on the dust grain absorption properties. The final dependence of αG on Z' is via the metallicity-dependent dissociation bandwidth w (see Equation (29)).
For two-sided illumination of an optically thick slab by beamed radiation, our analytic expression for the total atomic (H i) column density is (see Equation (40))
or as a gas mass surface density (including a factor of 1.4 for helium)
For two-sided irradiation by an isotropic field (see Equation (66)),
(where 〈μ〉 = 0.8), or
These expressions are generally valid for all regimes, from the weak- to strong-field limits (small and large αG), for all H i-to-H2 transition profile shapes (gradual or sharp), and for arbitrary metallicity Z' (small or large).
For an optically thick cloud with total gas mass surface density Σgas, the integral molecular (H2) gas fraction is
with as given above for either beamed or isotropic fields. In Figure 14 (panel (a) versus (c)) we compare our results for 1D slabs with the H2 mass fractions for spheres. The differences are very small.
Our formulae for the H i columns and H2 mass fractions may be incorporated easily into hydrodynamics simulations for galaxy evolution.
For αG/2 ≲ 1 the H i-to-H2 transitions are gradual, and the atomic columns are built up in the predominantly molecular portions of the cloud. For αG/2 ≳ 1 the transitions are sharp, and the H i is built up in outer fully atomic layers. For sharp transitions, the H i-H2-H i sandwich structure for slabs corresponds to H i shell and H2 core structures for spheres. If star-formation requires the conversion to H2, then a threshold surface density, Σgas, *, may be defined at which the molecular fraction . For αG/2 ≳ 1 and sharp transitions we then have .
For self-regulated galaxy disks (ala KMT/MK10) in which the H i is driven to two-phased thermal equilibrium (and heated by FUV photoelectric emission from dust grains), the dimensionless parameter αG is restricted to a narrow range close to (αG)CNM, where
independent of the metallicity Z'. For such self-regulated systems, our theory then predicts a metallicity-dependent H i-to-H2 star-formation threshold for individual clouds
This appears consistent with Galactic and extragalactic observations, at least for solar metallicity systems.
We thank Chris McKee for many discussions and for detailed comments on our manuscript, including assistance with Equation (100). We thank Alex Dalgarno, Reinhard Genzel, Avi Loeb, David Neufeld, Tsevi Mazeh, Ewine van Dishoeck, and the referee for helpful comments and conversations about this work. A.S. is supported by the DFG via German-Israeli Project Cooperation grant STE1869/1-1/GE625/15-1 and by a PBC Israel Science Foundation I-CORE Program grant 1829/12. This work was supported in part by grant SYMPAYTICO (ANR-11-BS56-0023) from the French Agence Nationale de la Recherche and by the French CNRS national program PCMI. The early stages of our project was funded by the France-Israel High Council for Science and Technology.
APPENDIX: GLOSSARY OF SYMBOLS
Table 2 is a glossary of symbols we have used in this paper. In this listing we also refer to the equations in which the various symbols appear and/or are defined.
Table 2. Glossary of Symbols
Symbol | Definition | Units |
---|---|---|
Far-UV specific photon intensity. | photons cm−2 s−1 Hz−1 sr−1 | |
Free-space far-UV specific intensity (Equation (2)). | photons cm−2 s−1 Hz−1 sr−1 | |
IUV | Intensity scaling factor relative to the unit free-space Draine field. | ⋅⋅⋅ |
Fν | Flux density, . | photons cm−2 s−1 Hz−1 |
Mean flux density in LW band (Equation (12)). | photons cm−2 s−1 Hz−1 | |
F0 | Free-space LW band photon flux integral (Equations (3) and (4)). | photons cm−2 s−1 |
Fν(z) | Beamed photon flux density at linear depth z in a slab. | photons cm−2 s−1 Hz−1 |
F(z) | Beamed photon flux at linear depth z in a slab (Equation (76)). | photons cm−2 s−1 |
σν, d | H2 photodissociation cross section at frequency ν (Equations (7) and (77)). | cm2 |
σd | Individual H2-line photodissociation cross section (Equation (9)). | cm2 Hz |
H2 photodissociation cross section summed over all lines (Equation (13)). | cm2 Hz | |
D | Depth-dependent H2 photodissociation rate. | s−1 |
D0 | Free-space H2 photodissociation rate (Equation (5) and (15)). | s−1 |
D(0) | H2 photodissociation rate at the surface of a optically thick slab (Equation (6)). | s−1 |
Pvj | LW photon H2 pumping rate out of ro-vibrational level vj (Table 1). | s−1 |
〈fdiss〉vj | Mean dissociation probability out of level vj (Table 1). | ⋅⋅⋅ |
Mean dissociation fraction per absorbed LW photon (Equation (18)). | ⋅⋅⋅ | |
σg | Far-UV grain absorption cross section per hydrogen nucleon (Equation (20)). | cm2 |
ϕg | Order unity grain composition factor. | ⋅⋅⋅ |
Z' | Metallicity relative to solar abundances. | ⋅⋅⋅ |
R | Grain surface H2 formation rate coefficient (Equation (21)). | cm3 s−1 |
T | Gas temperature. | K |
n1 | Atomic hydrogen (H i) volume density. | cm−3 |
n2 | Molecular hydrogen (H2) volume density. | cm−3 |
n | Total hydrogen gas volume density, ≡ n1 + 2n2. | cm−3 |
N1 | H i column density. | cm−2 |
N2 | H2 column density. | cm−2 |
N | Hydrogen gas column density, N ≡ N1 + 2N2. | cm−2 |
τg ≡ σgN | Dust opacity in normal direction. | ⋅⋅⋅ |
N1, tot | Total H i column density on one side of an optically thick slab. | cm−2 |
τ1, tot ≡ σg | H i-dust opacity in normal direction. | ⋅⋅⋅ |
Wd(N2) | H2-line overlap limited dissociation bandwidth. | Hz |
Wg(N2) | H2-dust-limited dissociation bandwidth. | Hz |
Wd, tot | Total H2-dust-limited dissociation bandwidth. | Hz |
w | Normalized H2-dust-limited dissociation bandwidth (Equation (29)). | ⋅⋅⋅ |
fshield(N2) | H2 self-shielding function (Equations (16) and (72)). | ⋅⋅⋅ |
〈μ〉 | Mean ray-angle factor for H i-dust opacity (Equations (63) and (75)). | ⋅⋅⋅ |
α ≡ D0/(Rn) | Free-space atomic-to-molecular density ratio (Equations (34) and (44)). | ⋅⋅⋅ |
G(σg) | Mean self-shielding factor (Equations (41), (45)–(48)). | ⋅⋅⋅ |
αG | Fundamental dimensionless parameter for the HI-to-H2 transition (Equations (49)– (51)). | ⋅⋅⋅ |
nCNM | CNM gas density for multiphased H i equilibrium (Equation (58)). | cm−3 |
(αG)CNM | αG for two-phase H i equilibrium (Equation (59)). | ⋅⋅⋅ |
H2 mass surface density in plane-parallel slab. | M☉ pc−2 | |
Σgas | Total gas mass surface density in plane-parallel slab. | M☉ pc−2 |
H2 gas mass within sphere. | M☉ | |
Mgas | Total gas mass within sphere. | M☉ |
τz ≡ nσgz | Total dust optical depth through slab of finite linear width z. | ⋅⋅⋅ |
τr ≡ nσgr | Dust optical depth along radius r of a sphere. | ⋅⋅⋅ |
y | Total dust optical depth normalized to the H i-dust optical depth (Equation (97)). | ⋅⋅⋅ |
H i-dust optical depth, finite slab, two-sided irradiation, isotropic (Equation (98)). | ⋅⋅⋅ | |
H i-dust optical depth, finite slab, two-sided radiation, beamed (Equation (99)). | ⋅⋅⋅ | |
〈τ1〉 | Mean H i-dust optical depth, sphere, isotropic irradiation (Equation (101)). | ⋅⋅⋅ |
H2 mass fraction for slab (Equation (97)). | ⋅⋅⋅ | |
H2 mass fraction for uniform density sphere (Equation (100)). | ⋅⋅⋅ | |
H2 mass fraction for spherical atomic-molecular complex (Equation (102)). | ⋅⋅⋅ | |
Σgas, * | Star-formation threshold gas surface density at which . | M☉ pc−2 |
Footnotes
- 4
We note that in the classical "PDR literature," the FUV field strength is designated variously as G0, IUV, or χ (e.g., Hollenbach et al. 1971; van Dishoeck & Black 1986; Sternberg & Dalgarno 1989; Draine & Bertoldi 1996). In this paper we adopt IUV for the field strength to avoid confusion with the "αG factor" defined in Section 2.2.5 or with the KMT/MK10 "χ," which as we discuss in Section 4 is equivalent to our αG in the low-metallicity limit. The adopted normalizations can be confusing. For example, in the classic Tielens & Hollenbach (1985) paper, G0 = 1 refers to an FUV field for which the energy density at the surface of an optically thick cloud is equal to the energy density in the free-space (all 4π) Habing (1968) field. That is, G0 = 0.5 for an optically thick slab embedded in a unit (isotropic) Habing field. With our definitions, IUV = 1 (not 0.5) for a cloud inserted into a unit isotropic Draine field with or for a cloud illuminated by a corresponding beamed field with surface flux density . For IUV = 1, the H2 photodissociation rates at the cloud surfaces are equal to half the full 4π "free-space" rate in a unit Draine field (see also Equation (5)).
- 5
In our notation, the subscript "d" refers to H2 photodissociation. Thus, σν, d is the cross section for line absorption followed by dissociation. The subscript "g" refers to dust grains. Thus, σg is the FUV dust grain absorption cross section (Section 2.2.2).
- 6
This can be seen directly from Equation (7). For damped lines, σν and σν, d are proportional to ν−2, and the integral over frequency is then proportional to .
- 7
- 8
The main goal and result of S88 was an analytic formula for the intensity of UV excited (fluorescent) IR H2 emission lines from PDRs. Because the FUV-pumped H2 vibrational excitation rate is proportional to the dissociation rate, the IR intensity is proportional to the H i column density, as expressed in Equation (10) of that paper.
- 9
This limit is often referred to in the literature as the "self-shielding" limit. However, this is potentially confusing if self-shielding is properly understood to be associated with just H2-line absorption. As we have been emphasizing, H2-dust also absorbs and cannot be ignored for small αG, unless the metallicity is very low. So the weak-field limit may be referred to as the "H2-line plus H2-dust" shielding limit.
- 10
This is analogous to the Strömgren expression, , for the column density, , of ionized hydrogen in a slab that fully absorbs a flux, FLyc, of Lyman continuum photons. Here ne is the electron density, and αB is the electron–proton recombination coefficient.
- 11
To see this, note that when αG ≫ 1.
- 12
Publically available at http://pdr.obspm.fr.
- 13
With our assumption that the grain surface H2 formation rate coefficient R is linearly proportional to the metallicity, the gas-phase formation routes become important for Z' ≲ 5 × 10−3, depending on the temperature and fractional ionization, xe, of the gas. For an estimate of the effective rate coefficient, R−, for H2 formation via the negative-ion H− intermediary, see, e.g., Equation (A7) of MK10, cm3 s−1.
- 14
Photodissociation out of excited vibrational levels becomes significant when IUV ≳ 105 and the UV excitation rates become comparable to the quadrupole vibrational decay rates (Shull 1978). However, even for such intense fields, the excitation rates become small as the lines rapidly become optically thick, and for most of the H i layer absorption out of excited vibrational states is negligible (S88).
- 15
For example, in the expression , the molecular fraction enters as a threshold, and the star-formation rate is quenched as becomes small. In this form of the KS relation, is the star-formation rate per unit mass surface density, Σgas is the total gas mass surface density, τdyn is the dynamical time, and
is the star-formation efficiency per dynamical time.
- 16
- 17
When Krumholz et al. (2008) defined their χ via the transfer-dissociation equation, they wrote the surface flux F(0) in the numerator, rather than the full 4π free-space F0. However, when discussing spherical models, KMT/MK10 redefine their χ and replace F(0) with F0 in the numerator. In this paper we use the free-space F0 throughout, including here in our discussion of the transfer-dissociation equation. With this adjustment a factor of two appears in the second term on the right-hand side of Equation (80), which is not there in Krumholz et al. (2008).
- 18
- 19
This follows from MK10 Equation (82) for , where is the scaled radius of the H2 core in a uniform density cloud. For a critical cloud , and this occurs when their ξd = 1.944, where ξd ≡ 2.22ln[1 + 0.6χ + 0.01χ2]/〈τr〉. This gives our expression (101) for the critical depth 〈τ1〉, where we have replaced χ with our αG. Our expression (100) is then MK10 Equation (82), where y = 2/ξd.
- 20
For MK10 Equation (93) for the complexes their just vanishes for the critical value s = 2, where s ≡ 2.22ln[1 + 0.6χ + 0.01χ2]/〈τc〉, and 〈τc〉 is the total area-averaged dust optical depth of the complex (MK10, Equation (91)). This again gives our expression (101) for the critical depth . Our expression (102) is then MK10 Equation (93), where their s ≡ 2/y.