Diversity in the outcome of dust radial drift in protoplanetary discs
Key Words.:
circumstellar matter; protoplanetary discs ; stars: formation; radiative transfer; methods: analytical, numericalThe growth of dust particles into planet embryos needs to circumvent the “radialdrift barrier”, i.e. the accretion of dust particles onto the central star by radial migration. The outcome of the dust radial migration is governed by simple criteria between the dusttogas ratio and the exponents and of the surface density and temperature power laws. The transfer of radiation provides an additional constraint between these quantities because the disc thermal structure is fixed by the dust spatial distribution. To assess which discs are primarily affected by the radialdrift barrier, we used the radiative transfer code MCFOST to compute the temperature structure of a wide range of disc models, stressing the particular effects of grain size distributions and vertical settling.
We find that the outcome of the dust migration process is very sensitive to the physical conditions within the disc. For high dusttogas ratios () and/or flattened disc structures (), growing dust grains can efficiently decouple from the gas, leading to a high concentration of grains at a critical radius of a few AU. Decoupling of grains from gas can occur at a large fraction () of the initial radius of the particle, for a dusttogas ratio greater than 0.05. Dust grains that experience migration without significant growth (millimetre and centimetresized) are efficiently accreted for discs with flat surface density profiles () while they always remain in the disc if the surface density is steep enough (). Between (), both behaviours may occur depending on the exact density and temperature structures of the disc. Both the presence of large grains and vertical settling tend to favour the accretion of nongrowing dust grains onto the central object, but it slows down the migration of growing dust grains. If the disc has evolved into a selfshadowed structure, the required dusttogas ratio for dust grains to stop their migration at large radius become much smaller, of the order of 0.01. All the disc configurations are found to have favourable temperature profiles over most of the disc to retain their planetesimals.
1 Introduction
The evolution of dust particles embedded in circumstellar discs constitutes the first step towards planet formation (bw08; Chiang2010). Micrometresized dust grains collide and grow by coagulation, forming larger pebbles (millimetre and centimetresized, Beckwith00; Dominik06PPV and references therein) that may ultimately give birth to kilometresized planetesimals. Dust grains also settle towards the disc midplane and migrate inwards as a result of the conjugate actions of stellar gravity, gas drag, and radial pressure gradient (e.g. Weidendust1977; Nakagawa86; Fromang06; Laibe2012, herafter Laibe2012). This results in a stratified disc structure with a population of small (micrometresized) grains remaining close to the surface and larger grains located deeper in the disc (e.g. Dullemond04; Duchene04; DAlessio06; Pinte07; Pinte08b). However, the interplay between these two mechanisms remains unclear. For instance, how dust grains overcome the “radialdrift barrier” — i.e. the accretion of dust grains onto the central star on timescales shorter than the disc’s lifetime. Several mechanisms have been invoked to overcome this barrier, such as grain growth (e.g. Laibe08, hereafter Laibe08, Brauer08; Okuzumi2009; Birnstiel09; Zsom2010; Windmark2012; Garaud2013) or trapping in pressure maxima (e.g. Pinilla2012; Gibbons2012).
Another mechanism has been studied by Stepinski97; Youdin2002 and Youdin2004 and revived by Laibe2012, Laibe2014a, and Laibe2014b for growing dust grains. As the grains move inward, their radial motion is affected by the increasing drag force, the increasing pressure gradient, and eventually a larger size due to grain growth. The combination of these effects can lead to a variety of outcomes. In particular, for specific values of the exponents of the gas surface density () and midplane temperature (), the time required for grains to reach smaller and smaller radii increases drastically^{1}^{1}1in the case where the gas accretion velocity is neglected. This causes dust grains to decouple from the gas phase and “pileup” in the dense, inner regions of the disc: the migration timescale becomes so long that dust particles are virtually stopped and never end up accreted onto the central object.
Growing grains may also break through the drift barrier because of the transition from Epstein to Stokes drag at high gas densities (Birnstiel10, see their Fig. 11).
Although the kinematics of the radial motion of the grains depends on the grain size, the outcome of the radial drift motion essentially depends on the values of and . Laibe2012 and Laibe2014b derived three analytic criteria that predict whether dust grains are ultimately accreted onto the central star or not. In order for dust to pile up, the criteria are
(i) and for growing grains, where
(1) 
measures the relative efficiency between growth and migration, and is the disc’s initial dusttogas ratio.
(ii) for nongrowing grains in the Epstein drag regime (which corresponds to dust grains of size smaller than 10 cm for density conditions encountered in protoplanetary discs), and
(iii) for planetesimals ( m) in the Stokes drag regime.
In the following, we use the terms “growing grains”, “nongrowing
grains”, and “planetesimals” to refer to these three cases.
In these former studies, and were considered to be independent parameters that could take any value. However, the radial temperature profile of the disc is set by the transfer of radiation, which depends on both the dust properties and the disc geometry. The parameter therefore depends on the dust surface density profile and can only take a limited range of values. Furthermore, the grain size distribution (which affects the wavelength dependence of the opacity) and vertical settling (which lowers the surface, changing the amount of stellar light intercepted by the disc as a function of the radius) are expected to affect the value of and, in turn, the outcome of the radial migration.
In this paper, we present the first results of the effect of radiative transfer on the radialdrift barrier in both the Epstein and Stokes regimes. Specifically, we determine i) which parts of the (, ) diagram are populated with physical models, ii) whether these discs are strongly affected by the radialdrift barrier process, and iii) the key parameters that affect the stability of the dust particles with respect to radial migration.
Parameter  Range of values explored  Step 

0 – 1.5  0.25  
(gas) [AU] at 50 AU  5 – 15  5 
(gas)  1.0 – 1.35  0.05 
[m]  1 – 10 000  factor 10 
– + (no settling)  factor 10 
2 Methodology
In the following, we discuss the outcome of grains that are large enough (i.e. m) to be significantly affected by radial migration. These grains first settle toward the disc midplane before they migrate inward. Laibe2012’s criteria were originally derived for the migration of dust grains in the disc midplane but still remain valid if the grains are located close to the midplane, i.e. at lower altitudes than the local scale height (see App. A).
The criteria defined in Laibe2012 and Laibe2014b apply for and corresponding to the gas phase. Here we only consider young gasrich and radially optically thick discs (corresponding to the classical T Tauri stage). We assume that the density in the disc midplane is high enough to ensure thermal equilibrium between gas and dust and we take both T = T and , and only use the notation in the following. Disc temperature structures are computed for given density structures, i.e. for given values of . We assume that in the initial state of the discs, gas and dust grains are radially well mixed, implying . We discuss deviations from this case in section 3.5.
2.1 Model description
We assume an axisymmetric flared density structure with a Gaussian vertical profile where is the distance from the star in the disc midplane and the altitude above the midplane. We use powerlaw distributions for the dust surface density and the scale height where is the scale height at radius AU and the disc flaring exponent^{2}^{2}2 and as observed in discs strongly differ from the socalled minimal mass solar nebula disc models (e.g. Weidendust1977; Hayashi1981) used in most of theoretical studies.. We fix the density structure rather than assume hydrostatic equilibrium in order to assess the effect of each model parameter individually. In particular, the flaring parameter and scale height are free parameters that are not selfconsistently derived from the temperature calculation. The disc extends from an inner cylindrical radius AU to an outer limit AU. Since we are only interested in the disc’s temperature gradient and not its absolute value, we use a fixed central object (TK, RR) and a fixed dust disc mass of MM. The disc mass directly influences the local stopping time (or equivalently, the Stokes number) and thus the grains’ kinematics. However, the Stokes number is only a scaling factor in the equations of motion of the grains, and its value does not affect whether the grains will pile up or decouple at a finite radius. The key parameters are the dependencies of the Stokes number and the Stokes number’s rate with respect to both the grain size and distance to the central star, which are independent of the disc mass/density (Laibe2012; Laibe2014b). In particular, the decoupling radius for growing dust grains is independent of the disc mass.
Dust grains are modelled as homogeneous and spherical particles with sizes distributed according to the power law between (fixed to m) and . Absorption and scattering opacities, scattering phase functions, and Mueller matrices are calculated using the Mie theory.
The thickness of the dust layer results from the competition between gravity and turbulent stirring and depends on both the grain size and the turbulent viscosity coefficient (ShakuraSunyaev1973). Dust settling is implemented using a diffusionadvection equation with a variable diffusion coefficient, which has been found this to be a reasonable approximation to global MHD simulations of stratified and turbulent discs (Fromang09, Eq. 26). The degree of dust settling is changed by varying . For comparison, models without any settling are also included.
2.2 Computing the stability criteria
To ascertain the importance of radiative transfer on the outcome of the radial migration of dust grains, we computed a grid of disc models with the MCFOST radiative transfer code (Pinte06; Pinte09) varying both the dust optical properties and the disc density distribution and geometry (Table 1). This includes the exponent, which is treated here as an input parameter and is not evolved with time.
MCFOST solves the continuum transfer with a Monte Carlo method. In short, the code stochastically propagates photon packets in 3D through the disc: the transport of packets is governed by successive scattering, absorption, and reemission events, which are determined by the local dust properties. The temperature structure is calculated using the immediate reemission algorithm of Bjorkman01 combined with a continuous deposit of energy to estimate the mean intensity (Lucy99). The resulting midplane temperature profiles in the outer parts of the discs ( AU) are fitted by a power law . Radiative transfer calculations have shown that this is a good approximation of the temperature profile in the outer disc (see for instance the radial temperature profiles presented in DAlessio98; Dullemond02; Pascucci04; Pinte09). We additionally compute the local slope of the midplane temperature as in order to determine in which regions of the discs the temperature profile can be approximated by a power law and the simple analytical criteria can be applied, and to assess how the migration will be affected when the temperature profiles deviate strongly from the power law.
2.3 Model limitations
This work is based on analytical calculations of the dust evolution in discs, which necessarily implies some simplifying assumptions:

The equations are mathematically valid only when the temperature profile is a power law. We found that this is the case for AU in most of the disc configurations. When the temperature profile differs from a power law, the general trend remains, but the predictions become more qualitative.

The dusttogas ratio is assumed to be constant when integrating the analytical expressions. But because dust grains migrate, this is not the case in discs.

The underlying growth model remains simple and does not consider more complex effects that have been shown to affect the evolution of the dust population in young discs (see Dullemond13, for a recent review): for instance, bouncing or fragmentation barrier, charging barrier or porosity evolution (Okuzumi12).

The radial gas flow, which may be important in the very central parts of the disc was not considered here. It may also act to remove the dust particles from the disc, preventing them from being accreted onto planetesimals, as it may transport particles that are coupled to the gas inwards, even when they are not drifting.
Additionally, we do not consider the case of large dust grains that are observed at large distances from the star (see for instance Hughes08; Andrews09; Andrews10b; Isella09, who measured critical radii^{3}^{3}3The critical radius is defined as , approximately 2/3 of the mass lies within the critical radius ranging from 15 to 200 AU). The presence of millimetre sized grains at distance much greater than a few 10 AU requires additional mechanisms, such as local pressure maxima to trap the dust grains (e.g. Pinilla12).
3 Results and discussion
The values of obtained from radiative transfer modelling for the various disc models are presented in Fig. 1.
3.1 Stability of growing dust grains relative to radial migration
Initially small, interstellarlike dust grains (m) experience simultaneous migration and growth in the outer disc, until they reach a size of at least a few millimetres, when the sticking probabilities during collisions are strongly reduced (“bouncing barrier”, see section 3.2). For these growing dust grains, the criterion is satisfied for every disc’s configuration (see Fig. 1). If this first requirement were not fulfilled, growing grains would not pile up in discs. Figure 2 shows the values of for an initial gasdustratio of . The pileup of growing grains mainly depends on the value of : higher values of favour the pileup, which becomes systematic for ; i.e., is always larger than . The case results in values of close to 0, i.e. at the limit of stability. In that case, the stability of growing dust grains depends mainly on the local scale height (as previously discussed by Brauer08, see their Eq. 43): smaller scale heights tend to favour dust pileup. For instance, scale heights smaller than 10 AU at a reference radius of 100 AU result in a pileup for grains starting at 100 AU. increases as decreases and the conditions for pileup become less stringent as smaller radii, see for instance the righthand panel of Fig. 2 at AU, where most of the disc configurations will be favourable for dust grain pileup.
The previously described criteria only tell us whether pileup will occur. For this pileup to help the formation of planetary cores, it has to occur at a distance that is sufficiently far from the star that the dust grains do not reach the very central regions where dust sublimation or the gas accretion flow will remove the dust particles before they can be incorporated in planetesimals. The pileup of growing dust grains, when it happens, is extremely efficient (the migration time goes as an exponential of a power law with respect to the grain’s position), and the grains literally stop their migration. The stopping radius of the grains depends on the relative efficiency of the growth and migrations processes and the value of . Figure 3 shows the decoupling radius as a fraction of the initial radius and as a function of the parameter for the various values of and obtained in our grid of radiative transfer models. We estimated numerically, by solving simultaneously the equations for grains migration and growth using the (YL; Vnew) model of Laibe2014b. We calculated as the grain’s radius in the asymptotic limit. We used years here and checked that the asymptotic limit was reached. The decoupling radius is essentially not sensitive to the value of the surface density exponent . However, a noticeable dispersion is obtained when varying the temperature exponent . The decoupling of the grains is more efficient for discs with smooth thermal profiles. For , the decoupling radius can be located at up to 6 % of the initial distance to the central star for low values of (0.15). For larger , the corresponding decoupling radius decreases and reach values lower than 1 % for . For , the decoupling occurs at values ranging between 18 and 30 % of the initial radius. This process was also observed in numerical simulations as presented in Laibe08, explaining why dust grains can be found to overcome the radialdrift barrier, depending on the physical conditions in the disc.
Figure 4 presents the dusttogas ratios that are required for the dust grains to decouple at a final radius equal to 1 % (left) and 10 % (right) of their initial radius. Dust grains starting a few hundred AU will stop their migration at a distance greater than a few AU as long as the dusttogas ratio is higher than the generally assumed interstellar value . A slight enhancement compared to this value, for instance , is enough to obtain a decoupling in almost all the disc configurations we have explored. For a higher dusttogas ratio, the decoupling will occur at even greater distances. With between and , most of the disc configurations will show dust grains decoupling at a radius larger than 10 % of their initial radius. The required for dust grains to pile up at a given radius is smaller for discs with flatter surface density profiles and shallower midplane temperature gradients. For a given surface density, there are large variations in the required depending on the temperature structure of the disc. For instance, for , the required values for to obtain dust pileup range from to 0.032 for a relative decoupling radius of 0.01 and from 0.043 to 0.085 for a relative decoupling radius of 0.1. Taking the details of the temperature structure and radiative transfer effects into account is therefore critical in dust evolution simulations to accurately predict the outcome of the dust migration processes.
3.2 Stability of nongrowing dust grains and planetesimals relative to radial migration
When dust grains reach centimetric size, they start bouncing instead of sticking during collisions. This reduces the growth efficiency dramatically (Guttler2010; Zsom2010; Windmark2012), though stochastic processes may assist the formation of larger bodies (Okuzumi11; Windmark2012b, but see also their Corrigendum Windmark2012c, and Garaud2013). When the growth becomes negligible, the migration outcome is given by the criterion derived in Laibe2012: (displayed in Fig. 1). We note that all discs with shallow initial profiles () will lose a large fraction of their grains by accretion onto the central star. In the absence of additional mechanisms to slow down the migration, and if these grains do not cross regions where the conditions allow them to grow again, these discs will be efficiently depleted in millimetresize grains. For profiles with , grains pile up and the discs efficiently retain their grain population in the inner disc. For intermediate surface density profiles (), either dust migration or dust pileup can happen, depending on the details of the disc structure and grain properties. Interestingly, this includes the standard case , which is the limiting profile of a viscous evolution after several viscous timescales (for a constant ). This range of values for is close to the observed surface density in the millimetre regime. For instance, Andrews2010 found a narrow distribution of surface density gradients for a sample of discs in Ophiuchus: , which does not seem to depend on the millimetre flux (in their Table 4, only one disc in 12 is found to have ), suggesting that most of the discs are located at the interface between the stable and unstable regimes with respect to the migration of their millimetre/centimetre grains.
The highest value of we obtain remains less than the critical value of predicted for planetesimals to be efficiently accreted onto the central star. The thermal profile of the outer disc is therefore favourable to retaining potential planetesimals, regardless of the grain distribution.
For nongrowing grains or planetesimals, the pileup process is smoother than for the growing grain case. There is no actual stopping point since the pileup occurs progressively, slowing down the particles more and more as they reach the disc’s inner region. (The migration time goes as a power law with respect to the grain’s position.) Quantitatively, particles reduce their migration efficiency compared to the case without pileup when they reach a radius that is roughly 10 of their initial distance to the central star (Fig. 3 of Laibe2012). Then, it takes an order of magnitude more time for the grain to decrease its radial position by another factor 10.
For instance, in a disc with and (no pileup) and a disc mass of 0.1 M and gastodust ratio of 100, it takes years for a mm grain initially located at AU to reach AU, a mere additional years to reach AU and an even fewer additional years to reach AU (i.e. years in total). For comparison, in the same disc but with and (pileup), it takes years for a mm grain initially located at AU to reach AU (i.e. roughly the same time as without the pileup) but more additional years to reach AU and an even more additional years to reach AU (i.e. years in total). Figures 6 to 10 of Laibe2012 shows a parameter study for the time required for a grain to reach the inner regions of typical classical TTauri discs. The global behaviour is not modified if the disc mass is changed and only the respective times are scaled. For a lower disc mass, the corresponding times are reduced in the case of pileup, while they are increased when there is no pileup.
3.3 Effect of grain size distribution & vertical settling
In the case of optically thin dust with an opacity law that can be described by a power law , the temperature is determined by
(2) 
resulting in a temperature profile . As the effective grain size grows, varies from 2 for small ISMlike grains to 0 for millimetre or larger grains, the resulting values range from to . Taking the details of radiative transfer into account, e.g. high optical depth and shadowing effects, we obtain values of ranging from 0.10 to almost 0.65 with the same trend of higher values for larger grains, on average. (Fig. 1 illustrates this effect with 2 subsets of the disc models: m and and m.) As a consequence, discs where dust grain have grown will have a steeper temperature profile and will be more prone to losing their grain population by accretion onto the central object. In contrast, a possible regeneration of micrometresized grains (Brauer2008; Guttler2010; Zsom2010) will make the temperature profile shallow and stabilise the outcome of the millimetre grains.
The temperature gradient becomes steeper (larger ) as the degree of dust settling increases (smaller , Fig. 5). Dust settling lowers the altitude of the surface, thus reducing the amount of light intercepted at large radii and steepening the radial temperature profile. This is critical for discs with a surface density slope close to 1.0, since dust settling may in that case be enough for to become positive resulting in a strongly increased migration rate for mm/cm sized grains.
For growing dust grains, two opposite effects have to be considered. Grain growth and/or dust settling will steepen the temperature profile, but they will also reduce the midplane temperature in the outer disc. As illustrated in Fig. 6 (where results are presented using the local hydrostatic scale height), the latter effect dominates: increases in the presence of already grown dust grains and/or settling. Both the presence of grain growth and vertical settling tend to favour pileup of the grains. In particular, if m and (blue models in the right panel of Fig. 6), pileup of dust grains will almost always occur, even with . (87 % of this subset of models have .)
If the dust opacities are significantly lowered in the outer disc due to grain growth or dust settling, the outer disc structured can be strongly modified, changing from a flared geometry to selfshadowed one (e.g. Dullemond04). Because the outer parts of the disc do not intercept much stellar light directly, the temperature drops significantly, resulting in reduced local sound speed and scale height. Around a T Tauri star, for instance, the midplane temperature can drop from 40 K down to 10 K at 10 AU and from 20 K down to 5 K at at 100 AU when changing the geometry from a flared to a selfshadowed geometry. This translates into a factor 2 on the gas scale height and the resulting dusttogas ratio required for dust grains to pile up is also reduced by 4. In a selfshadowed disc with a dusttogas ratio of 0.01, growing dust grains will thus stop their migration at a radius larger than 10 % of their initial radius. Such discs represent excellent sites for forming giant planet cores even in the absence of dust trapping mechanisms. We note, however, that discs are immersed in molecular clouds, whose temperatures range from 7 K to 15 K (e.g. Schnee05). This is likely to set a lower limit to the temperature reached in the coldest parts of the disc’s midplane and somehow counterbalance the effects of selfshadowing at very large distances from the star.
3.4 The radialdrift barrier in the central few astronomical units
The midplane temperature can only be approximated by a power law in the outer regions (where the heating is due to the reprocessing of the stellar light by the disc’s surface). However, a local temperature slope can be computed at any point to derive a local stability criteria, describing the proneness of grains to be accreted across a specific region of the disc. The stability criteria were only formally established for a power law temperature distribution, but their evolution as a function of radius, when the temperature structure differs from a power law, can be used to estimate if the radial drift will be enhanced or slowed down.
Figure 7 shows the stability criteria for discs of different surface density slopes. In the outer regions, remains almost constant (since the temperature structure is similar to a power law), but with a shallow increase with decreasing radius. As a consequence, the conditions for dust stability relative to migration remain mostly unchanged over a wide range of radii (– a few 100 AU). The case is of particular interest since can become positive at a relatively large radius (AU). Inside this radius, migration of mm/cm sized grains becomes more efficient, and the disc may display a lack of continuum emission at millimetre wavelengths in the central regions. In contrast, the pileup of still growing dust grains becomes more efficient at smaller radius, and the stability criteria starts to be validated for radii smaller than 15 to 30 AU depending on the surface density profile.
The temperature profiles in the very inner disc become extremely steep () due to direct heating from the stellar photosphere. As a consequence, all dust grains in the Epstein regime, growing or nongrowing, as well as planetesimals in the Stokes regime, will experience very efficient migration, independently of the value of . Accretion heating (not included in our modelling) can affect the midplane temperature but only within a few AU of the star (e.g. DAlessio98) where it can result in an enhanced migration rate for the dust grains and planetesimals.
3.5 Long term evolution of the migration process
As the dust migrates inward the dust surface density starts to depart from the initial gas distribution. Neglecting grain growth, Youdin2002 show that the drift velocity of grains in the Epstein regime is given by . This differential drift velocity results in dust concentration in the central regions, and steeper dust surface density profiles if (and flatter profiles if ). More complex profiles are obtained if grain growth is taken into account (e.g. Laibe08).
The stability criteria for nongrowing grains and planetesimals are only marginally affected though, because (i) the temperature gradient on large scales depends moderately on (all other parameters being fixed, see Fig. 7 right panel for instance) and (ii) this gradient is mainly set by the distribution of small grains (m), which intercept most of the stellar radiation in the disc surface and which remain coupled to the gas distribution. We assume here that the small dust population is mostly uninfluenced by the growth process. In the outer disc, where the “plateau of fast migration” occurs, the maximum expected grain size is roughly equal to the optimal size of migration
(3) 
where and are the gas density and sound speed, the intrinsic dust density and the Keplerian frequency. The parameter scales like the disc’s surface density; i.e., . We computed a second version of the grid presented in Table 1 where the maximum grain size at each radius is set , whereas the mass and density slope for each grain size bin is kept unchanged. As expected and as shown in Fig. 8,the resulting temperature distribution is indeed hardly modified.
Assuming that the gas surface density remains more or less constant (the viscous timescale of the disc being much longer than the migration timescale), the ability of nongrowing dust grains and planetesimals to overcome the radialdrift barrier will thus also only slightly evolve with time.
In the case of growing dust grains, if the condition for pileup are met, the pile up efficiency will increase with time as migrating dust grains will enter regions where previous dust grains have already piledup and where the local dusttogas ratio is higher (Laibe2014b). Interestingly, Laibe08 found that dust grains break through the migration barrier at a few 10 AU with , , and . These simulations were performed with , meaning that dust grains should pile up at large distances for . (This number is derived from the right panel of Fig. 4, scaled by 1/4 to account for the different .) A proper treatment of hydrodynamics effects results in a pileup with a smaller dusttogas ratio illustrating that the criteria we describe are strict conditions but that pileup can occur for less stringent conditions. Dust grains that pile up in the inner disc regions increase the local dusttogas ratio and trigger the pileup of the dust arising from the outer disc (see Laibe2014b). Moreover, migration becomes less efficient as the dusttogas ratios reaches values close to unity (Nakagawa86). These two effects favour the pileup of the grains and were not accounted for in the Laibe2014b model. Conversely, pileup will always occur if the criteria (and the assumptions they are based on) are met.
4 Conclusions
Based on analytical calculations of the dust evolution in discs (we highlight the limitations in section 2.3), we have investigated the effects of a complete treatment of radiative transfer on the stability of dust grains and planetesimals relative to radial migration within protoplanetary discs. We find that for a significant fraction of the discs we considered, the dust particles pile up in the disc, potentially providing material for the formation of planetary cores.
Excluding the first few central tenths of AU, all the disc configurations we explored lead to favourable temperature profiles () for the discs to retain their planetesimals.
The necessary criterion for discs to retain their growing grains is also always fulfilled. In most of the disc configurations, the conditions are met for dust grains to decouple at a radius larger than 1 % if the initial dusttogas ratio is higher than 0.03. In the case of a flat surface density, lower initial dusttogas ratios, around 0.01, are enough. In those cases, dust grains starting at a few hundred AU will pile up and stop migrating in the regions where telluric planets are formed. If the initial dusttogas ratio is higher, between 0.05 and 0.1, dust grains pile up at a radius larger than 10 % of their initial radius and could provide the material for forming the cores of massive planets.
Three classes of discs can be distinguished with respect to the outcome of the radial motion of nongrowing grains. Discs with steep density profiles () will retain their grains, whereas dust migration will be very efficient for flat surface densities (). For intermediate cases (), significant migration of dust grains can occur, but its outcome needs to be studied via casebycase detailed simulations coupling hydrodynamics and radiative transfer. Interestingly, this includes the case , which corresponds to the peak of the distribution of the observed disc profiles.
The presence of large grains and vertical settling steepens the temperature profile and tends to enhance the radial migration of the nongrowing grains, favouring accretion onto the central object. For growing dust grains, however, the reduced temperature in presence of large grains and/or settling will slow down the migration and result in pileup for almost all the disc configurations.
If the settling and/or grain growth increases, the disc structure can become selfshadowed, resulting in much lower gas temperature and sound speed. In this case, the conditions become much more favorable for dust grains piling up and dusttogas ratios over around 0.01 are enough to stop the migration of the grains coming from 100 AU at distances over a few AU.
In the central regions of the disc where the stellar radiation can penetrate directly or accretion heating can contribute, the temperature profile is so steep () that both the dust grains, whether they are still growing or not, and planetesimals are rapidly accreted in all cases. This will also be the case if accretion heating becomes significant and results in a steep temperature profile in these central regions.
Understanding the detailed outcome of the radial migration in protoplanetary discs requires numerical simulations to catch the complexity of all the processes at play ([e.g.][]Laibe08, Birnstiel09; Birnstiel10).
Ideally, these simulations should be coupling radiative transfer and dynamics, since the conditions for the migration or pileup of the dust grains are strongly affected by the thermal structure of the disc. In this simple study, we performed an exhaustive exploration of the parameter space and, based on analytical criteria, we give the main results of the migration outcome. These results can provide valuable help in tailoring the input parameters of the dust evolution codes used to understand the now growing evidence of dust radial segregation in discs.
Acknowledgements.
We thank F. Ménard, C. Dougados, J.C. Augereau, J.F. Gonzalez, S.T. Maddison, D.J. Price and J.B. Kajtar for useful discussions. C. Pinte acknowledges funding from the European Commission’s FP7 (contract PERG06GA2009256513) and the Agence Nationale pour la Recherche of France (contract ANR2010JCJC050401). G. Laibe is grateful to the Australian Research Council for funding (contract DP1094585) and acknowledges funding from the European Research Council for the FP7 ERC advanced grant project ECOGAL. Computations were performed at the Service Commun de Calcul Intensif de l’Observatoire de Grenoble (SCCI).References
Appendix A Validity of the criteria outside the disc midplane
In protoplanetary discs, grains migrate because the local azimuthal velocity of the gas is slightly slower than the Keplerian velocity (i.e. subKeplerian rotation). Eq. B.21 of Laibe2012 gives the analytic expression for with respect to the radial and vertical coordinates :
(4) 
where is the gas pressure in the disc midplane, is the sound speed and is a function defined by
(5) 
The first term of the righthand side of Eq. 4 is the Keplerian contribution. The second term is the pressure gradient term, which depends only on . Laibe2012’s criteria originate from this contribution. The third term is the baroclinic term. It contributes to the deviation to the Keplerian velocity only if . However, the ratio between the baroclinic term and the pressure gradient term is of order . This implies that for particles slightly outside the disc midplane, the baroclinic term has a negligible contribution and all the criteria used above apply.
Appendix B Models including simple dust migration
The results of the grid of models where we assume that is a function of the radius and is set to be equal to the optimum size of migration :
(6) 
are presented in Fig. 8.