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Synthesized grain size distribution in the interstellar medium
Earth, Planets and Space volume 65, Article number: 7 (2013)
We examine a synthetic way of constructing the grain size distribution in the interstellar medium (ISM). First, we formulate a synthetic grain size distribution composed of three grain size distributions processed with the following mechanisms that govern the grain size distribution in the Milky Way: (i) grain growth by accretion and coagulation in dense clouds, (ii) supernova shock destruction by sputtering in diffuse ISM, and (iii) shattering driven by turbulence in diffuse ISM. Then, we examine if the observational grain size distribution in the Milky Way (called MRN) is successfully synthesized or not. We find that the three components actually synthesize the MRN grain size distribution in the sense that the deficiency of small grains by (i) and (ii) is compensated by the production of small grains by (iii). The fraction of each contribution to the total grain processing of (i), (ii), and (iii) (i.e., the relative importance of the three contributions to all grain processing mechanisms) is 30–50%, 20–40%, and 10–40%, respectively. We also show that the Milky Way extinction curve is reproduced with the synthetic grain size distributions.
Dust grains are important in some physical processes in the interstellar medium (ISM). For example, they dominate the absorption and scattering of the stellar light, affecting the radiative transfer in the ISM. The extinction (absorption + scattering) by dust in the ISM as a function of wavelength is called the extinction curve (Wickramasinghe, 1967; Hoyle and Wickramasinghe, 1991; Draine, 2003 for review). Extinction curves are important not only in basic radiative processes in the ISM, but also in interpreting observational data: part of stellar light in a galaxy is scattered, or absorbed, by dust grains within the galaxy in a wavelength-dependent way according to the extinction curve. Therefore, to derive the intrinsic stellar spectral energy distribution of a galaxy, we always have to correct for dust extinction by considering the extinction curve (Calzetti, 2001).
Extinction curves generally reflect the grain composition and the grain size distribution. Mathis et al. (1977, hereafter MRN) show that a mixture of silicate and graphite dust, as originally proposed by Hoyle and Wickramasinghe (1969), with a grain size distribution (number of grains per grain radius) proportional to a−3 5, where a is the grain radius (a ~ 0.001–0.25 μm), reproduces the Milky Way extinction curve. Pei (1992) shows that the extinction curves in the Magellanic Clouds are also explained by the same power-law grain size distribution (i.e., ∝ a−3 5) with different abundance ratios between the silicate and graphite. Kim et al. (1994) and Weingartner and Draine (2001) have applied a more detailed fit to the Milky Way extinction curve in order to obtain the grain size distribution. Although their grain size distributions deviate from the MRN size distribution, the overall trend from small to large grain sizes roughly follows a power law with an index near to -3.5. Therefore, the MRN grain size distribution is still valid as a first approximation of the interstellar grain size distribution in the Milky Way.
What regulates or determines the grain size distribution? There are some possible processes that actively and rapidly modify the grain size distribution. Hellyer (1970) shows that the collisional fragmentation of dust grains finally leads to a power law grain size distribution similar to the MRN size distribution (see also Bishop and Searle, 1983). In fact, Hirashita and Yan (2009) show that such a fragmentation and disruption process (or shattering) can be driven efficiently by turbulence in the diffuse ISM. However, they also show that grain velocities are strongly dependent on grain size; as a result, the grain size distribution does not converge to a simple power-law after shattering. Moreover, dust grains are also processed by other mechanisms. Various authors show that the increase of dust mass in the Milky Way ISM is mainly governed by grain growth through the accretion of gas phase metals onto the grains (elements comprised of dust grains are referred to as “metals”) (Dwek, 1998; Inoue, 2003; Zhukovska et al., 2008; Draine, 2009; Inoue, 2011; Asano et al., 2013). In the dense ISM, coagulation also occurs, making the grain sizes larger (e.g., Hirashita and Yan, 2009). In the diffuse ISM phase, interstellar shocks associated with supernova (SN) remnants (simply called SN shocks in this paper) destroy dust grains, especially small ones, by sputtering (e.g., McKee, 1989). Shattering also occurs in SN shocks (Jones et al., 1996).
Modeling the evolution of the grain size distribution in the ISM is a challenging problem because a variety of processes are concerned as mentioned above. Those processes are also related to the multi-phase nature of the ISM. Liffman and Clayton (1989) calculate the evolution of grain size distributions by taking into account grain growth and shock destruction. However, their method could not treat disruptive and coagulative processes (i.e., shattering and coagulation). O’Donnell and Mathis (1997) also model the evolution of grain size distribution in a multi-phase ISM, taking into account shattering and coagulation, in addition to the processes considered in Liffman and Clayton (1989). They use the extinction curve and the depletion of gas-phase metals as quantities to be compared with observations. Although their models are broadly successful, the fit to the ultraviolet extinction curve is poor, which they attribute to the errors caused by their adopted optical constants. They also show that inclusion of molecular clouds in addition to diffuse ISM phases improves the fit to the observed depletion, but they did not explicitly show the effects of molecular clouds on the extinction curve. Yamasawa et al. (2011) have recently calculated the evolution of the grain size distribution in the early stage of galaxy evolution by considering the ejection of dust from SNe and subsequent destruction in SN shocks. Since they focus on the early stage, they did not include other processes such as grain growth and disruption (shattering), which are important in solar-metallicity environments such as in the Milky Way (Hirashita and Yan, 2009).
Comparing theoretical grain size distributions with observations is not a trivial procedure. In a line of sight, we always observe a mixture of grains processed in various ISM phases. Therefore, a “synthetic” grain size distribution, which is made by summing typical grain size distributions in individual ISM phases with certain weights, is to be compared with observations. In this paper, we first formulate a synthetic way of reproducing the grain size distribution. Then, we carry out a fitting of synthetic grain size distributions to the observational grain size distribution, in order to obtain the relative importance of individual grain processing mechanisms. We do not model the multi-phase ISM in detail, but our fitting contains the information on the weights (i.e., relative importance) of different grain processing mechanisms, which depend on the ISM phase.
This paper is organized as follows. In Section 2, we explain our synthetic method to reconstruct the grain size distribution in the ISM. In Section 3, we fit our synthetic models to the observational grain size distribution in the Milky Way, and examine if the fitting is successful or not. In Section 4, after we discuss our results, we calculate the extinction curves to examine if our synthesized grain size distributions are consistent with the observed extinction or not. In Section 5, we give our conclusions.
2. Synthetic Grain Size Distribution
As explained in Introduction, we “synthesize” the observational grain size distribution (here, the MRN size distribution) by summing some representative grain size distributions in various ISM phases. These representative grain size distributions are explained in Subsection 2.1.
First, the ISM is divided into two parts: one is the part where the grain processing is occurring (called the “grain-processing region”), and the other is the area where the grains already processed in the various grain-processing regions are well mixed (called the “mixing region”). The mass fractions of the former and the latter regions are, respectively, fproc and 1 − fproc. It is reasonable to assume that the grain size distribution in the mixing region should be the mean grain size distribution in the ISM (Subsection 2.2).
We assume that all grains are spherical with material density s; thus, the grain mass m is expressed as . Although coagulation may produce porous grains (e.g., Ormel et al., 2009), we neglect the effects of porosity and assume all grains to be compact. Two grain species are treated in this paper; silicate and graphite. To avoid complexity arising from compound species, we treat these two species separately. This separate treatment is also practical in this paper as we (and other authors usually) assume that the observed extinction curve can be fitted with the two species (Subsection 4.4). Before being processed, the grain size distribution is assumed to be MRN: a power-law function with power index −r (r = 3.5), and upper and lower bounds for the grain radii (whose values are determined below) amin and amax, respectively:
for amin ≤ a ≤ amax. If a < amin or a > amax, nMRN(a) = 0. The grain size distribution is defined so that nMRN(a) da is the number of grains whose sizes are between a and a + da per hydrogen nucleus. The dust mass density, ρd, is related to the metallicity Z (the mass fraction of elements heavier than helium in the ISM) and the hydrogen number density nH as (Hirashita and Kuo, 2011)
where mX is the atomic mass of the key element X (X = Si for silicate and C for graphite), fX is the mass fraction of X in the dust, ξ is the fraction of element X in the gas phase (i.e., the fraction 1 − ξ is in the dust phase), and (X/H)⊙ is the solar abundance relative to hydrogen in the number density. The metallicity is assumed to be solar (Z = Z⊙).
We fix the maximum grain radius as amax = 0.25 μm (MRN). Although the lower bound of the grain size is poorly determined from the extinction curve (Weingartner and Draine, 2001), we assume that amin = 0.3 nm, since a large number of very small grains are indeed necessary to explain the mid-infrared excess of the dust emission in the Milky Way (Draine and Li, 2001). For the other parameters, we follow Hirashita (2012). We assume that 0.75 of Si is condensed into silicate (i.e., ξ = 0.25) while 0.85 (i.e., ξ = 0.15) of C is included into graphite. Those values are roughly consistent with the observed depletion (e.g., Savage and Sembach, 1996), and reproduce the Milky Way extinction curve (Subsection 4.4). We adopt the following abundances for Si and C: (Si/H)⊙ = 3.55 × 10−5 and (C/H)⊙ = 3.63 × 10−4. We assume that Si occupies a mass fraction of 0.166 (fX = 0.166) in silicate, while C is the only element composing graphite (fX = 1). We adopt s = 3.3 and 2.26 g cm−3 for silicate and graphite, respectively.
By using the MRN size distribution as the initial condition, we calculate the evolution of grain size distribution by the various processes treated in Subsection 2.1. In the numerical calculation, the grains outside the radius range between amin and amax are removed from the calculation (the removed mass fraction is < 1%). The processes considered are (i) “grain growth”—grain growth by accretion and coagulation in a dense medium, (ii) “shock destruction”—destruction by sputtering in SN shocks, and (iii) “grain disruption”—grain disruption by shattering in interstellar turbulence. Shattering in SN shocks (Jones et al., 1996) could be included as a separate component, but in our framework, it is not possible to separately constrain the contributions from the two shattering mechanisms because both shattering mechanisms (turbulence and SN shocks) selectively destroy grains with a ≳ 0.03 μm and increase smaller grains, predicting similar grain size distributions. Thus, we simply assume that the size distribution of shattered grains, whatever the shattering mechanism may be, is represented by the one adopted in Subsection 2.1.3.
Although our fitting procedures are based on grain size distributions, we should keep in mind that observational constraints on the grain size distribution are mainly obtained by extinction curves. Weingartner and Draine (2001) performed a detailed fit to the Milky Way extinction curve. However, the grain size distributions derived by them broadly follow an MRN-like power law, although there are bumps and dips at some sizes. We will examine the consistency with the extinction curve later in Subsection 4.4.
2.1 Processes considered
2.1.1 Grain growth
Grain growth occurs in the dense ISM, especially in molecular clouds, through the accretion of metals (called accretion) and the sticking of grains (called coagulation). The change of grain size distribution by grain growth has been considered in our previous paper (Hirashita, 2012). The grain size distribution after grain growth is denoted as ngrow(a, tgrow), where tgrow is the duration of grain growth. We adopt tgrow = 10 and 30 Myr based on a typical lifetime of molecular clouds (e.g., Lada et al., 2010). The metallicity in the Milky Way is high enough to allow the complete depletion of grain-composing materials into dust grains in ~10 Myr. Thus, the total masses of silicate and graphite become 1.33 (= 1/0.75) and 1.18 (= 1/0.85) times as large as the initial values, respectively (recall that the dust mass becomes 1/(1 − ξ) times as much if all the dust grains accrete all the gas-phase metals). The difference in the grain size distribution between tgrow = 10 and 30 Myr is predominantly caused by coagulation rather than accretion.
2.1.2 Shock destruction
We calculate the change of grain size distribution by SN shock destruction in a medium swept by an SN shock, following Nozawa et al. (2006). All SN explosions are represented by an explosion of a star which has a mass of 20 M⊙ at the zero-age main sequence, and the SN explosion energy is assumed to be 1051 erg. For the ISM, we adopt a hydrogen number density of 0.3 cm−3 (since the destruction is predominant in the diffuse ISM; McKee, 1989), and solar metallicity. The calculation of grain destruction is performed until the shock velocity is decelerated down to 100 km s−1 (8 × 104 yr after the explosion). We apply the material properties of Mg2SiO4 and carbonaceous dust in Nozawa et al. (2006) for silicate and graphite, respectively. We denote the grain size distribution after shock destruction by nshock(a). The destroyed mass fractions of silicate and graphite are 0.38 and 0.27, respectively.
Grain motions driven by interstellar turbulence lead to grain disruption (shattering) in the diffuse ISM (Yan et al, 2004; Hirashita and Yan, 2009). Among the various ISM phases, dust grains can acquire the largest velocity dispersion in a warm ionized medium (WIM). We recalculated the results of earlier workers based on our assumed initial conditions. We adopt the same grain velocity dispersions and hydrogen number density (nH = 0.1 cm−3) in the WIM as adopted in Hirashita and Yan (2009). The fragments are assumed to follow a power-law size distribution with a power index of −3.3 (Jones et al., 1996; Hirashita and Yan, 2009). We denote the grain size distribution after disruption as ndisr(a, tdisr), where tdisr is the duration of shattering in the WIM. The lifetime of WIM is estimated to be a few Myr from the recombination timescale and the lifetime of ionizing stars (Hirashita and Yan, 2009). Thus, we adopt tdisr = 3 and 10 Myr for our calculation in causing moderate and significant disruption.
2.2 Synthesizing the grain size distribution
At the beginning of this section, we introduced the mass fraction (fproc) of ISM hosting grains which are now being processed (“grain-processing region”). The mean grain size distribution over all the grain-processing region, nsynt(a), can be synthesized with the processed grain size distributions, ngrow(a, tgrow) (grain size distribution after grain growth with a growth duration of tgrow), nshock(a) (grain size distribution after shock destruction), and ndisr( a, tdisr) (grain size distribution after disruption with a shattering duration of tdisr):
where fgrow, fdisr and fshock are the mass fractions of medium hosting, respectively, grain growth, disruption, and grain destruction in the grain-processing region. We call nsynt(a) the “synthetic grain size distribution”. If both species are spatially well mixed, they would have common values for fgrow, fshock, and fdisr.
The mean grain size distribution in the ISM is denoted as nmean(a) and expressed as
since it is assumed that the grain size distribution in the mixing region has already become the mean grain size distribution. By assumption, the mean size distribution is MRN: nmean(a) = nmrn(a). This condition is equivalent to
In the Milky Way ISM, since the grain mass is roughly in equilibrium between the growth in clouds and the destruction by SN shocks (Inoue, 2011), we apply fgrowR1 = fshockR2, where R1 is the fraction of dust mass growth in clouds (0.33 and 0.18 for silicate and graphite, respectively; Subsection 2.1.1), and R2 is the destroyed fraction of dust in a SN blast (0.38 and 0.27 for silicate and graphite, respectively; Subsection 2.1.2). Thus, we put a constraint,
We approximately adopt R1/R2 = 0.8 as a mean value between silicate and graphite. As mentioned above, if the two species (silicate and graphite) are spatially well-mixed, both species would have common values for fgrow, fshock, and fdisr. Thus, we adopt a single value for R1/R2.
Using the above constraints, Eq. (3) is reduced to
where ng,s(a) ≡ ngrow(a, tgrow) + (R1 / R2)nshock(a). Thus, we treat fgrow and fdisr as free parameters. We define the sum of all the fractions as
If the grain size distribution is predominantly modified by the three processes considered in this paper, we expect that ftot = 1. The deviation of ftot from 1 is an indicator of goodness of our assumption that the grain size distribution is modified by the three processes.
2.3 Best fitting parameters
We search for a set of parameters, (fgrow, fdisr), which minimizes the square of the difference:
where a i is the grain size sampled by logarithmic bins (i.e., log ai+1 — log a i is the same for any i), and N is the number of the sampled grain radii (N = 512 in our model, but the results are insensitive to N).
The individual components of the processed grain size distributions [ ngrow (a, tgrow ), nshock (a ), and ndisr (a, tdisr)] as well as ng,s(a) for silicate and graphite are shown in Fig. 1. The MRN size distribution, which should be fitted, is also presented. Our fitting procedure is first applied separately for silicate and graphite, although we discuss a possibility that both species have common values for (fgrow, fdisr) later in Section 4.
In Table 1, we show the best-fitting values of fgrow and fdisr. We examine tgrow = 30 and 10 Myr, and tdisr = 3 and 10 Myr as mentioned in Subsection 2.1. We observe that fgrow = 0.16–0.55 and fdisr = 0.06–0.57 fit the MRN grain size distribution. The sum of all the fractions, ftot (Eq. (8)) is unity with the maximum difference of 15% (see the column of ftot in Table 1).
In order to show how the synthetic grain size distributions reproduce the MRN size distribution, we present Fig. 2, where we only show Models A and D for the smallest and the largest residuals δ2. We observe that the best-fitting results are fairly consistent with the MRN size distribution. In particular, the enhanced and depleted abundances of small grains at a ≲ 0.001 μm in ndisr and ng,s, respectively, cancel out very well, especially in Model A. In Model D, the synthesized size distribution slightly fails to fit the MRN around a ~ 0.001–0.002 μm because both ng,s and ndisr (which are used for the fitting) show an excess around this grain radius range; thus, the excess around these sizes in the synthesized grain size distribution inevitably remains in Model D. However, the Milky Way extinction curve is reproduced even by Model D within a difference of ~10% (see Subsection 4.4).
In order to see the details of the fitting, we show the ratio between the synthesized grain size distribution and the MRN distribution in Fig. 3. There is a general trend of excess around a ~ 0.001–0.003 μm, which is due to grain growth (see Fig. 1). The excess is stronger in Models B and D than in Models A and C, which is why the fit is worse in Models B and D than Models A and C (Table 1). Since the bump comes from grain growth, the fit tends to suppress fgrow in the presence of a strong bump. As a result, ftot is smaller in Models B and D than Models A and C (Table 1). We also observe in Fig. 3 that the bump appears at different grain radii between Models A/C and B/D because of the difference in the duration of grain growth. This bump may disappear if coagulation is more efficient than assumed here: more efficient coagulation may be realized if tgrow ≫ 30 Myr and/or coagulation also occurs in denser regions (Subsection 4.2).
Figure 3 also indicates that the synthetic grain size distributions tend to be deficient at the largest grain sizes (a ≳ 0.1 μm). This is because shattering tends to process large grains into small sizes (see Fig. 1). The deficiency of large grains may be overcome if we include the supply of large grains by stellar sources of efficient coagulation as discussed in Subsection 4.2. Because of significant grain growth in Models A and C, the deficiency of large grains is recovered by grain growth at a ~ 0.01–0.03 μm for silicate. In Models A and C of graphite, shattering causes a dip feature around a ~ 0.03 μm as seen in Fig. 1, which also appears in Fig. 3. In the WIM, where shattering is assumed to occur in this paper, grains with a ≳ a few × 10−2μm are accelerated up to velocities larger than the shattering threshold by turbulence. Shattering efficiently destroys small grains because of their large surface-to-volume ratios. Thus, the shattering efficiency is the largest for the smallest grains that attain a velocity above the shattering threshold. This is the reason why the grains around a ~ 0.03 μm are particularly destroyed by shattering. This dip feature would be smoothed out in reality since the grain velocity driven by turbulence has a dependence on grain charge, gas density, magnetic field, etc., all of which have a wide range within a galaxy.
4.1 Derived parameters
The obtained values of the parameters fgrow and fdisr reflect the fraction of individual grain processing mechanisms. In other words, these two quantities show the relative importance of grain growth and disruption. Note that the efficiency of shock destruction is automatically constrained by the balance with the mass growth by grain growth (Eq. (6)). Table 1 shows that the best-fitting parameters are not very sensitive to tgrow (duration of grain growth) but that they are sensitive to tdisr. For larger tdisr, only a smaller fdisr is necessary because the grain size distribution is more modified. As expected, fdisrtdisr is less sensitive to tdisr; note that fdisrtdisr is the mean duration of disruption per processed grain.
Seeing all the models, we find fgrow ~ 0.2–0.6 and fdisr ~ 0.06–0.6 (or fdisrtdisr ~ 0.6–1.7 Myr). As mentioned in Subsection 2.2, if silicate and graphite are well mixed in the ISM, they are expected to have the common values for fgrow, fshock, and fdisr. In this sense, Models C and D work better than Models A and B. In summary, 20–60% of processing occurs in dense clouds (i.e., grain growth), while a processed dust grain experiences disruption for ~1 Myr on average (or disruption accounts for 6–60% of processing). From the equilibrium constraint of the total dust mass (Eq. (6)), the fraction of shock destruction to all the processing is fshock = 0.8 fgrow ~ 0.1–0.4.
The sum of all the fractions, ftot (Eq. (8)), is unity, with a maximum deviation of 15%. In other words, we cannot reject other processing mechanisms, which could contribute to the grain processing with ≲ 15%.
We have shown that the grain size distributions after (i) grain growth, (ii) shock destruction, and (iii) grain disruption can synthesize the MRN size distribution. It is also likely that we can state the opposite; that is, to realize the MRN size distribution, those three processes are crucial. Without (i), the grain mass just decreases; without (ii), the grain mass just increases; without (iii), there is no mechanism that produces the large abundance of small grains.
4.2 Stellar sources?
In this paper, we have not considered dust supply from stars, because the dust mass in the Milky Way is governed by the equilibrium between grain growth in molecular clouds and grain destruction by SN shocks (e.g. Inoue, 2011). Dust grains supplied from stars may be biased to large sizes. Production of large grains from asymptotic giant branch (AGB) stars is indicated observationally (Groenewegen, 1997; Gauger et al., 1998; Hofner, 2008; Mattsson and Hofner, 2011). The dust ejected from SNe is also biased to large grain sizes, because small grains are selectively destroyed by the shocked region within the SNe (Bianchi and Schneider, 2007; Nozawa et al., 2007). Coagulation associated with star formation is also a source of large grains, if coagulated grains in circumstellar environments are somehow ejected into the ISM. For this possibility, Hirashita and Omukai (2009) have shown that dust grains can grow up to micron sizes by coagulation in star formation (see also Ormel et al., 2009). As mentioned in Section 3, efficient coagulation may also solve the bump problem around a ~ 0.001–0.003 μm. These possible sources of large grains may be worth including in dust evolution models in the future.
4.3 Fitting under other constraints
In Subsection 2.2, we adopted the balance between the dust mass growth by accretion and the dust mass loss by shock destruction (Eq. (6)) as a constraint. Although this constraint is reasonable for the dust content in the Milky Way (e.g., Inoue, 2011), it may be useful to apply other constraints without using Eq. (6), to see how the best-fitting parameters have been controlled by Eq. (6).
First we try to fit the MRN size distribution with the three components under the condition that the sum of all the fractions is unity: fgrow +fshock+ fdisr = 1. The results with this fitting are shown in Table 2. The best-fitting values of fdisr vary from those in Table 1 within a difference of 10% except for Model B of silicate (25% less). However, the best-fitting values of fgrow is broadly 1/2-2/3 of those in Table 1. As a result, Eq. (6) is not satisfied, and the total dust mass decreases.
Next, we perform fitting to the MRN size distribution with the parameters fgrow, fshock, and fdisr free. The results are shown in Table 3. Again, the values of fdisr differ by only ≲10% except for Model B of silicate (18% less). However, fgrow is only ~ 1/3–2/3 of the values in Table 1, and fshock is made large to compensate for the decreased fgrow. This means that the fitting is practically dominated by the balance between the decreased small grains in shock destruction and the increased small grains in disruption (shattering). Because of the dominance of fshock, Eq. (6) is not satisfied, and the total dust mass decreases.
4.4 Extinction curve
The MRN grain size distribution is originally derived from the Milky Way extinction curve. Therefore, in order to check if our fitting by synthetic grain size distributions is successful or not, it is useful to calculate extinction curves.
Extinction curves are calculated by using the same optical properties of silicate and graphite as those in Hirashita and Yan (2009). The grain extinction cross-section as a function of wavelength and grain size is derived from the Mie theory, and is weighted for the grain size distribution per hydrogen nucleus to obtain the extinction curve per unit hydrogen nucleus (denoted as Aλ/NH). The abundances of silicate and graphite relative to hydrogen nuclei are already inherent in the models through the abundances of Si and C and ξ (Section 2).
First, we show the extinction curves of the individual components, which are used to fit the MRN size distribution, in Fig. 4. Grain growth does not make the extinction curve flatter in spite of the increase of the mean grain size. The reason is already explained in Hirashita (2012): accretion predominantly occurs at the smallest sizes. Since the extinction at short wavelengths is more sensitive to the increase of the mass of small grains than that at long wavelengths, the extinction curve becomes rather steeper. Although coagulation flattens the extinction curve, the flattening due to coagulation does not overwhelm the steepening due to the above effect of accretion.
Shock destruction makes the extinction curve flatter because small grains are more easily destroyed than large grains. Grain disruption steepens the extinction curve because of the production of a large number of small grains. The 0.22 μm bump created by small graphite grains in this model becomes also prominent by grain disruption. We also show the extinction curve for the grain size distribution ng,s(a) (The component ng,s has a total dust mass 1.8 times as large as the initial value. To see the difference in the extinction curve, it would be helpful to make a comparison under the same dust mass, so ngs/1.8 is compared with the MRN in Fig. 4.)
In Fig. 5, we show the extinction curves calculated for Models A–D. First of all, we confirm that the MRN size distribution reproduces the observed extinction curve (some small deviations can be fitted further if we adopt a more detailed functional form of the grain size distribution, which is beyond the scope of this paper; see Weingartner and Draine, 2001, for a detailed fitting). Comparing the extinction curve for the MRN size distribution and those for Models A–D, we observe that the extinction curve is reproduced within a difference of ~10%. Models A and C are successful, while Models B and D systematically underproduce the MRN extinction curve (although the difference is small). The under-prediction by ~ 10% in Models B and D occurs because ftot is ~0.9.
In the above, we adopted different values for fgrow and fdisr between silicate and graphite. As mentioned in Subsection 2.2, if both species are well mixed in the ISM, they would have common values of these parameters. In Fig. 6, we show the extinction curve by taking the average of the values for silicate and graphite (for example, fgrow = 0.35 and fdisr = 0.35 for Model A). We find that the difference between Figs. 5 and 6 is small. Therefore, the mean values work to reproduce the Milky Way extinction curves. The mean values are in the range of fgrow = 0.3–0.5 and fdisr = 0.1–0.4. We conclude that the synthetic grain size distributions with these parameter ranges reproduce the Milky Way extinction curve.
In our previous papers (Nozawa et al., 2006; Hirashita and Yan, 2009; Hirashita, 2012), we showed that dust grains are quickly processed by shock destruction, disruption, and grain growth. In this paper, we have examined if the MRN grain size distribution, which is believed to represent the grain size distribution in the Milky Way, can be reproduced by the processed grain size distributions. We “synthesized” the grain size distribution by summing the processed grain size distributions under the condition that the decrease of dust mass by shock destruction is compensated by grain growth. We have found that the synthetic grain size distribution can reproduce the MRN grain size distribution in the sense that the deficiency of small grains by grain growth and shock destruction can be compensated by the production of small grains by disruption. The values of the fitting parameters indicate that, among the processed grains, 30–50% are growing in a dense medium, 20–40% are being destroyed by shocks in a diffuse medium, and 10–40% are being shattered in a diffuse medium (the percentage shows the relative importance of each process). The extinction curves calculated by the synthesized grain size distributions reproduce the observed Milky Way extinction curve within a difference of ~10%. This means that our approach of synthesizing the grain size distribution based on major processing mechanisms (i.e., grain growth, shock destruction, and disruption) is promising as a general method to “reconstruct” the extinction curve.
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We are grateful to C. Wickramasinghe and an anonymous reviewer for helpful comments in their review of this paper. HH has been supported through NSC grant 99-2112-M-001-006-MY3. TN has been supported by a World Premier International Research Center Initiative (WPI Initiative), MEXT, Japan, and by the Grant-in-Aid for Scientific Research of the Japan Society for the Promotion of Science (20340038, 22684004, 23224004).
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Hirashita, H., Nozawa, T. Synthesized grain size distribution in the interstellar medium. Earth Planet Sp 65, 7 (2013). https://doi.org/10.5047/eps.2012.03.003
- Cosmic dust
- interstellar medium
- grain size distribution
- extinction, Milky Way