Issue 
A&A
Volume 531, July 2011



Article Number  A166  
Number of page(s)  14  
Section  Planets and planetary systems  
DOI  https://doi.org/10.1051/00046361/201116901  
Published online  07 July 2011 
The fourpopulation model: a new classification scheme for preplanetesimal collisions
^{1}
Institut für Astronomie und Astrophysik, Abteilung Computational Physics, Eberhard Karls Universität Tübingen, Auf der Morgenstelle 10, 72076 Tübingen, Germany
email: ralf.j.geretshauser@unituebingen.de
^{2}
Physikalisches Institut, Eberhard Karls Universität Tübingen, Auf der Morgenstelle 14, 72076 Tübingen, Germany
Received: 16 March 2011
Accepted: 1 May 2011
Context. Within the collision growth scenario for planetesimal formation, the growth step from centimetresized preplanetesimals to kilometresized planetesimals remains unclear. The formation of larger objects from the highly porous preplanetesimals may be halted by a combination of fragmentation in disruptive collisions and mutual rebound with compaction. However, the right amount of fragmentation is necessary to explain the observed dust features in late T Tauri discs. Therefore, detailed data on the outcome of preplanetesimal collisions is required and has to be presented in a suitable and precise format.
Aims. We wish to develop a new classification scheme broad enough to encompass all events with sticking, bouncing, and fragmentation contributions, accurate enough to capture the important collision outcome nuances, and at the same time simple enough to be implementable in global dust coagulation simulations. We furthermore wish to demonstrate the reliability of our numerical smoothed particle hydrodynamics (SPH) model and the applicability of our new collision outcome classification to previous results as well as our simulation results.
Methods. We propose and apply a scheme based on the quantitative aspects of four fragment populations: the largest and second largest fragment, a powerlaw population, and a subresolution population. For the simulations of preplanetesimal collisions, we adopt the SPH numerical scheme with extensions for the simulation of porous solid bodies. On the basis of laboratory benchmark experiments, this model was previously calibrated and tested for the correct simulation of the compaction, bouncing, and fragmentation behaviour of macroscopic highly porous SiO_{2} dust aggregates.
Results. We demonstrate that previous attempts to map collision data were much too oriented on qualitatively categorising into sticking, bouncing, and fragmentation events. Intermediate categories are found in our simulations that are difficult to map to existing qualitative categorisations. We show that the fourpopulation model encompasses all previous categorisations and in addition allows for transitions. This is because it is based on quantitative characteristic attributes of each population such as the mass, kinetic energy, and filling factor. In addition, the numerical porosity model successfully passes another benchmark test: the correct simulation of the entire list of collision outcome types yielded by laboratory experiments. As a demonstration of the applicability and the power of the fourpopulation model, we utilise it to present the results of a study on the influence of collision velocity in headon collisions of intermediate porosity aggregates.
Key words: hydrodynamics / methods: data analysis / methods: numerical / planets and satellites: formation / protoplanetary disks / accretion, accretion disks
© ESO, 2011
1. Introduction
The primary way in which rocky planets are thought to form is by core accretion in protoplanetary discs consisting of gas and dust. Interaction between these components induces relative velocities and consequential mutual collisions among the initially micronsized dust grains (e.g. Weidenschilling 1977b; Weidenschilling & Cuzzi 1993). In this way, millimetre to centimetresized fluffy dust aggregates grow by a simple hitandstick mechanism (e.g. Blum & Wurm 2008). The growth mechanism in the preplanetesimal regime (centimetre to kilometre) is unclear and is addressed in this paper. Once a sufficient population of kilometresized objects has formed, gravitationassisted accretion ensures the final assembly of fullsized planets (e.g. Goldreich et al. 2004). The planetary building blocks in this gravitydominated regime are referred to as planetesimals.
The growth step from preplanetesimals to planetesimals is not wellconstrained and the subject of extensive numerical and experimental effort. The difficulties to be overcome in this step can be characterised with three types of barriers: fragmentation, drift, and bouncing barrier (e.g. Zsom et al. 2010). The most serious barrier is the fragmentation barrier: with increasing size, the relative velocities between preplanetesimals increase and potentially lead to catastrophic disruption in mutual collisions. Often a velocity threshold of 1 ms^{1} for disruptive events is assumed (Blum & Münch 1993). The threshold is mostly assumed to be independent of other parameters such as porosity, mass ratio, and impact parameter (e.g. Güttler et al. 2010). With the assumption of this fragmentation threshold and powerlaw distributed fragments, Brauer et al. (2008) find that dust coagulation is halted at centimetre or even millimetre sizes. Teiser & Wurm (2009) proposed a growth model that is based mainly on the accretion of fragments <1 mm by larger objects and therefore requires some amount of disruptive collisions.
The second obstacle to planetesimal formation is the radial drift of larger preplanetesimals (Weidenschilling 1977a). Owing to its pressure support, the gas in the disc rotates at a subKeplerian velocity, whereas the solid material lacks this pressure support and tends to rotate at a Keplerian velocity. As a consequence, the solid objects feel a headwind that causes an inward drift. For the minimummass solar nebula, it takes roughly a century for metresized objects to drift from 1 AU into the star. In contrast, for centimetre and kilometresized objects it takes ~10^{5} yr. This is because small objects are strongly coupled to the motion of the gas, whereas large objects are almost decoupled. As a consequence, in the intermediate regime, metresized objects are quickly lost by accretion onto the host star or by photoevaporation in the hot zones close to it. Collective effects in the midplane of the protoplanetary disc might diminish the problem (e.g. Cuzzi et al. 1993; Dominik et al. 2007; Weidenschilling 2010).
On the basis of empirical data showing the existence of rebound in dust collisions (Blum & Münch 1993; Heißelmann et al. 2007; Langkowski et al. 2008; Weidling et al. 2009; Güttler et al. 2010), Zsom et al. (2010) introduced a possible new obstacle to growth: the bouncing barrier, where collision growth is halted at centimetresized pebbles. In the collisions, aggregates only become compacted in mutual collisions but do not grow any further. However, recent studies (Geretshauser et al., in prep.; Wada et al., in prep.) indicate that the collision parameter space governed by bouncing may have been estimated to be too large by Güttler et al. (2010) and that rebound is not as frequent as they inferred.
However, fragmentation is also necessary in discs. Observations (e.g. Natta et al. 2007) suggest that submillimetre sized dust and millimetre to centimetresized pebbles are present for as long as about 10^{6} yr in T Tauri discs. However, Dullemond & Dominik (2005) find that without fragmentation the disc is depleted of small grains within 10^{3} yr. This is commonly referred to as the grain retention problem. With coagulation simulations, Birnstiel et al. (2009, 2010) tried to match the fragment distribution of disruptive events with the observational data.
To summarise, the formation of planetesimals requires the right amount of sticking, bouncing, and fragmentation to be consistent with observations. Therefore, collisions of preplanetesimals have to be investigated as thoroughly as possible and their outcome has to be mapped as precisely as possible taking into account all the relevant parameters such as initial porosity, collision partner size, impact velocity, mass ratio, and rotation. To classify collision outcomes, Güttler et al. (2010) compiled 19 experiments and mapped them to four types of sticking, two types of bouncing, and three types of fragmentation. However, owing to experimental restrictions they covered only small parts of the relevant parameter space. Many of their findings were not deduced from collisions between porous dust aggregates, but from dust collisions with a solid object. Collisions between aggregates larger than the decimetre size were not possible because of the limitations of their experimental apparatus. In addition, not all experiments could be carried out in protoplanetary disc conditions, i.e., in a vacuum and under microgravity.
An alternative to experiments is to study preplanetesimal collisions numerically. To explore the region where experimental data is lacking, we perform simulations of preplanetesimal collisions with our solidbody smoothed particle hydrodynamics (SPH) code, which was previously used by Schäfer et al. (2007) to emphasise the importance of precise material parameters and a thorough calibration of the implemented porosity model. Geretshauser et al. (2010) expanded the porosity model and both calibrated and tested it extensively to simulate preplanetary dust material based on laboratory benchmark experiments (Güttler et al. 2009). The code and calibration procedure is briefly described in Sect. 2. In Sect. 3, we show that the code can furthermore reproduce all sticking, bouncing, and fragmentation types proposed by Güttler et al. (2010). However, we find that their categorisation can also introduce unnecessary complexity and on some occasions may lack the required accuracy. It is possible that in a collision more than one process of sticking, bouncing, and fragmentation can take place and qualitative models do not make it clear whether the overall growth is positive, negative, or neutral. Therefore, we propose a new, simpler but at the same time more quantitative model for mapping collision data that is presented in Sect. 4. To show the applicability of this model, we present the first results of simulations of collisions between macroscopic objects consisting of realistic preplanetesimal material in Sect. 5. We finally summarise our findings and discuss future work in Sect. 6.
2. Code and calibration
For the simulations presented in this paper, we utilise the parallel SPH code parasph (Hipp & Rosenstiel 2004; Schäfer 2005; Schäfer et al. 2007), which was calibrated to simulate porous dust material (Geretshauser et al. 2010). This section briefly summarises the numerical model and calibration procedure.
2.1. SPH and porosity model
For collision simulations, SPH as a meshless Lagrangian particle method is superior to gridbased methods. This is because the continuous fluid or solid is divided into interacting mass packages, which serve as numerical sampling points and form a natural frame of reference for deformation and fragmentation (see reviews, e.g. by Monaghan 2005; and Rosswog 2009). Originally developed for astrophysical fluid flows, SPH has also been extended to model solid material (e.g. Libersky & Petschek 1991; Benz & Asphaug 1994; Randles & Libersky 1996; Libersky et al. 1997).
Within the SPH scheme, the equations of continuum mechanics are solved in their Lagrangian form. In this framework, the continuity and momentum equations are given by where the Greek indices indicate the spatial components and the Einstein sum convention is applied. The quantities ρ and v are the density and velocity, respectively, and σ_{αβ} is the stress tensor which is defined as (3)where p is the pressure, which accounts for pure hydrostatic compression or tension, and S_{αβ} is the deviatoric stress tensor, which represents pure shear. For the time evolution of the deviatoric stress tensor in the elastic regime, we adopt the approach of Benz & Asphaug (1994), which uses the Jaumann rate form and follows Hooke’s law. The elastic hydrostatic pressure is modelled as part of the porous equation of state (Eq. (8)).
SiO_{2} dust material parameters used in the porosity model.
To model subresolution porosity, we relate the filling factor φ to the continuous quantities according to (4)where ρ_{s} = 2000 kg m^{3} is the density of the matrix material of SiO_{2} (e.g. Blum & Schräpler 2004). Table 1 shows the material parameters of the calibrated porosity model determined by Geretshauser et al. (2010). To model the plastic behaviour, we modified the approach by Sirono (2004), who models plasticity with fillingfactordependent strength quantities. The compressive strength Σ(φ), the tensile strength T(φ), and shear strength Y(φ) represent transition thresholds between the elastic and plastic regime. In particular, we adopt the relations (see Güttler et al. 2009; and Geretshauser et al. 2010) (5)for φ_{min} + ε < φ < φ_{max} and ε = 0.005. The quantities φ_{min} = 0.12 and φ_{max} = 0.58 denote the minimum and maximum filling factors, respectively, in the compressive strength relation. However, the material can exceed both of these values. The power of the compressive strength relation is ln(10) times the parameter Δ with Δ = 0.58 (see Geretshauser et al. 2010, for a study of this parameter), which can be found together with the other material parameters in Table 1. For φ ≤ φ_{min} + ε, the compressive strength relation is continuously extended by the constant function Σ(φ) = Σ(φ_{min} + ε) and for φ_{max} ≤ φ we set Σ(φ) = ∞. The tensile strength is given by (6)and the shear strength is the geometric mean of the compressive and tensile strength (7)Hence, the full equation of state for the hydrostatic pressure reads (8)where , and and are critical filling factors. The value of marks the transition between elastic and plastic compression and defines the transition between elastic and plastic tension. The filling factors inbetween the critical values represent the elastic regime. The quantity is the reference density at vanishing external pressure and K(φ) is the fillingfactordependent bulk modulus given by (9)where γ = 4, K_{0} is the bulk modulus of an uncompressed random ballistic deposition (RBD) dust sample with φ_{RBD} = 0.15 (e.g. Blum & Schräpler 2004) such that K_{0} = K(φ_{RBD}) = 4.5 kPa, and the shear modulus is given by μ(φ) = 0.5K(φ).
Plasticity is modelled such that once the filling factor exceeds the critical values or , the hydrostatic pressure, which is computed according to the elastic equation of state (second line in Eq. (8)), is reduced to Σ(φ) or T(φ), respectively. For the reduction in pure shear, the deviatoric stress tensor S_{αβ} is limited according to the van Mises plasticity given by (e.g. Benz & Asphaug 1994) (10)where , J_{2} = S_{αβ}S_{αβ} is the second irreducible invariant of the deviatoric stress tensor, and Y = Y(φ) is the shear strength.
2.2. Calibration procedure
The above porosity model was carefully calibrated and tested in Geretshauser et al. (2010) with the aid of three benchmark experiments (Güttler et al. 2009): (1) the compaction of dust by a glass sphere; (2) the rebound of a dust aggregate from a solid surface; and (3) the fragmentation of a dust aggregate colliding with a solid surface. This is the most elaborate material calibration which is available for astrophysically relevant macroscopic dust aggregates. All benchmark experiments were carried out in the laboratory as well as in simulations.
Because compaction of porous material is a very efficient energy dissipation mechanism that allows dust aggregates to stick rather than break apart, in our first experiment we tested the compression properties of the model, ensuring that both the dynamic compressive strength and the shear strength relations were calibrated.
Since rebound is discussed as an obstacle to planetesimal formation, the second benchmark experiment tested the bouncing properties of a dust aggregate. With the aid of this benchmark setup, we calibrated the bulk modulus as a characteristic quantity of the elastic properties. We also confirmed the relation of the compressive strength which is a characteristic quantity for the energy dissipation during compaction.
For preplanetesimal collisions that end in fragmentation, the largest fragment and the mass distribution of the fragments is highly important for subsequent collisions. For this reason, our last calibration experiment tested the correct reproduction of the fragmentation properties of the porosity model. The bulk modulus, which is the quantity that has the strongest influence on the fragment mass distribution, was also confirmed.
After the successful calibration procedure, we are able to correctly reproduce the compaction, bouncing, and fragmentation behaviour of porous SiO_{2} dust aggregates quantitatively with one consistent set of material parameters as shown in Table 1. These material parameters are used for all simulations discussed in the following.
3. Reproducing sticking, bouncing, and fragmentation collision types
Fig. 1 The outcome of our simulations of preplanetesimal collisions encompasses all sticking (S), bouncing (B), and fragmentation (F) types proposed by Güttler et al. (2010). The initial configuration for each simulation is a sphere with radius r_{t} = 10 cm as resting target and a sphere with r_{p} = 6 cm as projectile except for S3 and F2, where r_{p} = 2 cm. The colour code indicates the filling factor φ. Both objects are initially set up with φ = 0.35 except for the F2 case, where φ = 0.55. The simulations are carried out with different impact velocities and the snap shots are taken at different times. The details are given in the text. 

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Güttler et al. (2010) compiled a large number of experiments with dust aggregates and suggested categorising them into four types of sticking, two types of bouncing, and three types of fragmentation. The sticking events were subdivided according to sticking mechanisms (hitandstick for micron sized monomers, surface effects, or deep penetration) and a quantitative criterion (mass transfer). Growth neutral bouncing with compaction and bouncing with mass transfer were distinguished in terms of rebound. Fragmentation was classified according to its degree (complete fragmentation or erosion) and whether some sticking was involved (fragmentation with mass transfer).
In this section we show that our code and its underlying calibrated porosity model can reproduce these empirical outcome types in numerical simulations. Images of the final result of each example simulation are presented in Fig. 1 according to this categorisation. The end times of the simulations are chosen by visual control of the fragment evolution and particle velocities close to the thermal equilibrium for each fragment. For each category, an exterior view (left) and a cut through the centre of the resulting aggregate(s) (right) is shown (except for type F1). The target is always a dust aggregate with radius r_{t} = 10 cm modelled using 238 238 SPH particles. The projectiles are modelled using 1905 and 51 477 SPH particles for projectile radii r_{p} = 2 cm and r_{p} = 6 cm, respectively, and placed on a cubic lattice with edge length 2.6 mm. The collision partners are aligned head on with a shift of half a lattice constant into each direction perpendicular to the collision axis to avoid particle interpenetration. In all simulations (except F2), both objects are set up with φ = 0.35 and the masses of the target, and the 6 cm, and 2 cmprojectiles are 2.93 kg, 0.63 kg, and 0.023 kg, respectively. An overview of the initial conditions of the simulations is given in Table 2. The colour in Fig. 1 indicates the filling factor φ. We now discuss the simulation outcomes in detail. We adopt the notation by Güttler et al. (2010).
S1 (hit & stick) is not represented in Fig. 1 as it is not applicable within the continuous SPH scheme. This category describes the outcome of collisions in which microscopic fractal dust aggregates are involved. In this regime, the continuum limit, which is a fundamental assumption of our model, is invalid. We focus on collisions of macroscopic dust since for the fractal regime the numerical and empirical basis is profound.
S2 (sticking through surface effects) The example shows the result of the impact of an aggregate with radius r_{p} = 6 cm and collision velocity v_{0} = 2.0 ms^{1}. The image shows the situation 250 ms after the impact. The filling factor of the outer shell of the aggregates remains nearly unchanged as indicated by the exterior view. In contrast, large parts of the interior are compressed to φ ~ 0.45. The target and the projectile merge to form one object. The initial setup matches that used for the B2 case but has a higher impact velocity. As a consequence, the contact area is larger and compressed to higher filling factors. This leads to a higher tensile strength in this region, which prevents the objects from rebounding from each other. This situation is referred to as sticking through surface effects. A single aggregate remains and no fragments are ejected.
S3 (sticking by deep penetration) is found in our simulations if the projectile is sufficiently smaller than the target. In the example case, the projectile has a radius of r_{p} = 2 cm and hits the target with v_{0} = 10.0 ms^{1}. The image is taken 388 ms after the impact. A small crater is formed on the target and a small number of single SPH particles are ejected. This characterises deep penetration. The crater is visible in the crosssection. Material is compressed to a maximum of φ ~ 0.52 down to a depth of about one target radius.
S4 (mass transfer) occurs if the projectile is large and moves fast enough to stick but still slow enough to not fully disrupt the target. As an example, we choose an impact of a 6 cm aggregate onto a target with the same filling factor. The impact velocity is v_{0} = 10.0 ms^{1} and the image shows the result after 50 ms. During the collision, the target is highly deformed and compressed to filling factors of φ ~ 0.45 to 0.52. Single SPH particles are ejected. Most of the projectile merges, which accounts for the mass transfer. The final mass of the largest fragment is 3.56 kg.
B1 (bouncing with compaction) is only seen in the case of objects of medium and low porosity at low collision speeds. Highly porous objects have an extremely low compressive strength. As a consequence, low pressures suffice to plastically deform the target and the highly porous aggregates do not gain enough elastic loading for bouncing. In our example, the projectile is 6 cm in radius. It impacts at v_{0} = 1.0 ms^{1}. In Fig. 1, the final state at 500 ms is shown. In the collision, both objects are flattened at the impact site and the elastic loading is sufficient to make them rebound after the impact. Part of the interior of the target and projectile is compressed to φ ~ 0.45. We note that this is exactly the same setup as in the S2 case but with a lower impact velocity. The bouncing event is a result of a smaller contact area and a lower tensile strength in this region, which is indicated by the lower filling factor. As a consequence, the two objects rebound. A close investigation reveals that in nearly every simulation with bouncing, a small amount of material is transferred between the projectile and target. Thus, it is very unlikely that pure growth neutral bouncing without any mass transfer exists. In this particular simulation, material of ~0.54 g is transferred from the projectile to the target. Hence, the result could also be classified into the next category.
B2 (bouncing with mass transfer) occurs in simulations where the compressive strength is sufficiently large to allow for elastic loading and consequential bouncing, and where the tensile strength is small enough for the impactor to rip out a small fraction of mass from the target. This happens at very low impact speeds. The final state at 1.7 s after the collision is the result of a collision with v_{0} = 0.2 ms^{1}. The projectile has r_{p} = 6 cm. During the impact, a small region of target and projectile is compressed to φ ~ 0.45. In the consequential rebound, this region sticks to the projectile and is ripped out of the target. The remaining crater on the target can be seen in the crosssection. In this collision, 29.5 g are transferred from the target to the projectile.
F1 (fragmentation) is generally the outcome of collisions with high impact velocities. Highly porous objects effectively dissipate energy by deformation because of their low compressive strength but they are also easy to disrupt because of their low tensile strength. In contrast, objects of low porosity have high tensile strengths, but lack the ability to dissipate large amounts of kinetic energy. The degree of fragmentation is therefore strongly porosity dependent. Our example shows the result of a collision between objects, where the projectile features r_{p} = 6 cm. The impact speed is v_{0} = 17.5 ms^{1}. During the collision, both the target and the projectile completely shatter and the result of this collision (shown only in exterior view 800 ms after the impact) is a continuous fragment distribution, whose masses range from 285 g down to single SPH particles of 12 mg. The fragments consist of target and projectile material that are indistinguishably combined together. The filling factors of the fragment distribution are φ ~ 0.54, which is close to the maximum filling factor of 0.58 (see Table 1).
F2 (erosion) is observed particularly for high filling factors and small projectile radii. The initial setup for the example case involves two objects with φ = 0.55. The target and projectile masses were 4.60 kg and 0.037 kg, respectively. The projectile radius is r_{p} = 2 cm and the impact velocity v_{0} = 20.0 ms^{1}. During the intrusion of the projectile, fragments consisting of a small number of SPH particles are ejected opposite the impact site. The figure shows the situation 438 ms after the collision, where small fragments and SPH particles are ejected from the crater. In this collision, 63.2 g of material are eroded from the target. The projectile intrudes to the centre of the target and the intrusion channel is clearly visible in the crosssection. Because of the high compressive strength elastic deformation also takes place on the target. The figure shows a snap shot of a decompression wave of lower filling factor, which appears as a vertical ring on the target.
The category F3 (fragmentation with mass transfer) contains conceptual difficulties. The first reason is that in the simulation outcomes of the F1 and F2 categories, some mass is always transferred to the target. Secondly, the demarcation between sticking with mass transfer (S4) and F3 is unclear and a continuous transition between these categories is expected. This problem can be solved by our new model proposed below. Our simulations incorporate category F3 by reproducing the S4 and F1 types.
In conclusion, our code is not only capable of quantitatively reproducing sticking, bouncing, and fragmentation in general (Geretshauser et al. 2010) but also of correctly simulating the subtypes for each macroscopic collision outcome. However, we also experienced difficulties in classifying the results of our simulations according to the model of Güttler et al. (2010). This motivates our wish to find a new approach.
4. A new model for mapping collision outcomes
We introduce a new model to classify the outcome of preplanetesimal collisions. We first describe its structure. We then show that all sticking, bouncing, and fragmentation events of the previous section can be incorporated into the new model.
4.1. The motivation behind a new classification scheme
The model of Güttler et al. (2010) was developed based on particular laboratory setups. In several of these, one of the collision partners was not a dust aggregate but a solid surface or a glass bead, which itself cannot fragment. Therefore, applying this categorisation to preplanetesimal dust collisions, which here are solely carried out as simulations between dust aggregates, leads to some difficulties.
In our simulations, the collisions of S3 (sticking by penetration) always produce ejected dust. Therefore, it is unclear whether they should be classified as S3 or rather S4 (mass transfer). On the other hand, S2 (sticking through surface effects) involves also a mass transfer but without the production of fragments. It can also be expected that there is a continuous transition from S2 to S3 with increasing impact velocity. The demarcation between the sticking types is also conceptually difficult to make. The types S1 to S3 are distinguished on the basis of the sticking mechanism, whereas for S4 the criterion is an increase in target mass and the generation of some fragments. In the context of preplanetesimal growth, the exact sticking mechanism is of minor importance. The distinction between growing and disruptive events is simply given by comparing the largest fragment before and after the collision.
Applying the bouncing categories to collision data also causes some difficulties. Pure bouncing with compaction (B1) events are never seen in our simulations. Analysing the final mass of both collision partners after the impact reveals that some mass is always transferred either from the projectile to the target or vice versa. In the first case, growth occurs and the result should be categorised under S4 with a growing target, but with one remaining fragment instead of a fragment distribution. If mass is transferred to the projectile, then the event belongs to B2 (bouncing with mass transfer). However, since the largest object is losing mass, B2 is also a type of erosion (F2), where instead of a fragment distribution only one large fragment (the enlarged projectile) is present. Since bouncing may be an obstacle to planetesimal growth (Zsom et al. 2010), the effect of bouncing has to be included in any collision map. However, instead of distinguishing between two types of bouncing, we find that it is sufficient to distinguish between the mass of the largest and the second largest fragment.
Analysing the numerical results for disruptive events, it is also hard to distinguish between types F1 (fragmentation) and F3 (fragmentation with mass transfer). As already mentioned above, in any fragmenting collision, mass is transferred from the projectile to the target and the fragments consist of both projectile and target material. In eroding events (F2), mass is also transferred to the target and a fragment distribution is produced. Once again the continuous transition between the three fragmentation types and between sticking and fragmentation events cannot adequately be described by the given model. In our view, it is sufficient to characterise the outcome of disruptive events in terms of the size of the largest fragment (which for F2 is much larger than the other fragments) and a powerlaw distribution of the remaining fragments. Thus, for correct mapping of any combination of sticking, bouncing, and fragmentation, the following objects have to be considered: both a largest and a second largest fragment as well as a powerlaw fragment distribution.
This discussion shows that the classification of different sticking, bouncing, and fragmentation events is not sufficient. This is because many intermediate events exist. For example, a bouncing event can involve some sticking and fragmentation, whereas a sticking event can also involve some fragmentation. The model by Güttler et al. (2010) tries to capture these intermediate events. However, it is based on physical mechanisms rather than collision outcome. Owing to its discrete approach, the model generates some unnecessary complexity and cannot easily describe transitions between categories. To improve on this, we propose a model that is based solely on quantitative aspects. It distinguishes between four types of fragment populations characterised by continuous quantities such as their mass, filling factors, velocities, and size. In this way, we are able to map all types of sticking, bouncing, and fragmentation events but also model continuous transitions between these types.
4.2. Fragment populations
Fig. 2 Illustration of the fourpopulation model. The left side displays the situation before the collision: two preplanetesimals collide with impact velocity v_{0} and impact parameter b. The target and projectile are characterised by their defining quantities, e.g., mass m, filling factor φ, and rotational energy E_{rot}. Depending on these parameters, an outcome population is generated in the collision (middle). The fourpopulation model distinguishes the fragments according to their mass. The population classes are: a) the largest fragment; b) the second largest fragment; c) the powerlaw population; and d) the subresolution population. This categorisation is sufficient to describe the outcome types of Fig. 1 as well as intermediate outcomes. 

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The fundamental idea of the new classification is that any outcome of a collision can adequately be modelled by distinguishing four kinds of fragment “populations”. This is illustrated in Fig. 2. Example input parameters for the collision include the masses of the target (label “t”) m_{t} and projectile (label “p”) m_{p}, their filling factors φ_{t} and φ_{p}, their rotational energies E_{rot, t} and E_{rot, p}, their impact parameter b and, most importantly, their collision velocity v_{0} (see Fig. 2, left). Depending on these parameters, the collision between two bodies produces a welldefined outcome of populations. To be able to map sticking, bouncing, and fragmentation events, it is suitable to sort this distribution according to the mass of the fragments in the respective population. For these, output parameters such as mass, filling factor, rotational energy, and velocity are determined as exact or averaged values, or as distributions depending on the population. Specifically, the new scheme consists of the following four types: (1) largest fragment; (2) second largest fragment; (3) powerlaw population; and (4) subresolution population:

(a)
Largest fragment: comparing the mass of the largest fragmentbefore and after a collision distinguishes between positive andnegative growth. The characteristic output quantities aresupplied;

(b)
Second largest fragment: this enables bouncing events to be mapped. In pure bouncing events, the largest and the second largest fragment will be the only members of the fragment population. The quantities describing this fragment are supplied. The second largest fragment only exists if it consists of more than a single SPH particle;

(c)
Powerlaw population: in disruptive collision events in particular, the mass distribution of the fragments can be modelled by a powerlaw to describe the fragment distribution. Instead of describing each fragment of the powerlaw population with quantities as done previously for the largest and second largest fragment, the number of parameters is reduced significantly by utilising distribution functions;

(d)
Subresolution population: this population is introduced for numerical reasons. Fragments of the subresolution population consist only of a single SPH particle. The existence of this population represents the resolution limit of the simulations and therefore represents only an upper limit to the smallest dust fragments, which are produced in a collision. This population is also convenient to control sufficient resolution. The SPH numerical scheme is capable of simulating objects of metre size and more. However, because of limited computational resources, single SPH particles then represent objects of centimetre size and larger. The subresolution population keeps track of these objects. It is convenient to describe this population with averaged characteristic quantities. We note that also in laboratory experiments a subresolution population exists, for which the fragment distribution is determined by high speed cameras.
With this approach, we considerably reduce the complexity of the sticking, bouncing, and fragmentation classification from nine types of collision outcomes to four fragment populations. Moreover, our model is based solely on continuous quantities characterising the collision outcome and not on physical mechanisms. This allows us to model any mixed types of collisions and transitions between growth and disruption with the necessary accuracy.
Compared to fragmentation data that are mapped to a powerlaw distribution alone (e.g. Mathis et al. 1977; Davis & Ryan 1990; Blum & Münch 1993; Güttler et al. 2010), the new model is also more accurate. In some of our simulations, a fragment distribution contains one large fragment and many small ones. The small ones can be accurately modelled with a powerlaw mass distribution. However, the mass of the largest fragment often does not match the power law. This is particularly true for grazing collisions between highly porous aggregates, where the filling factor of the largest remnant differs significantly from those of the other fragments. Since this has a major impact on subsequent collisions, we treat the largest fragment and its filling factor separately. Furthermore, powerlaw distributions cannot map bouncing collisions. For these reasons, we distinguish the largest and second largest fragment from the rest of the fragment distribution.
With the four given fragment populations and their defining properties, we present a closed model that is capable of modelling any collision outcome of preplanetesimals with minimum complexity but with the accuracy necessary to model the dust aggregation in global coagulation models. In the next section, we show how the model by Güttler et al. (2010) can be represented in our new model.
4.3. Mapping sticking, bouncing, and fragmentation to the new model
Mapping sticking, bouncing, and fragmentation.
The key idea behind mapping the sticking, bouncing, and fragmentation subtypes to the fourpopulation model is to describe the collision outcome by the characteristic quantities of each of the four populations. If one of the populations does not exist, its characteristic quantity is simply set to zero. In principle, a number of quantities can be used to determine the population. To illustrate the use of this model, we select the characteristic quantities mass m and filling factor φ as examples. Table 3 demonstrates the successful mapping of the Güttler et al. (2010) types into our quantitative fourpopulation model. The indices “t”, “p”, “1”, “2”, “pw”, and “sr” denote target, projectile, largest, second largest, powerlaw, and subresolution quantities, respectively. For the illustration, we assume that the mass of the target m_{t} is greater than or equal to the projectile mass m_{p}, i.e. m_{t} ≥ m_{p}. We find a filling factor increase in all collisions if the initial filling factor is smaller than the maximum compaction at φ_{max} = 0.58 (see Fig. 7 for the largest fragment).
For pure sticking (S1 to S3 types) only one fragment in the final population exists, which is identified as the largest fragment. Consequently, this fragment contains the mass of the total system, i.e. m_{1} = m_{t} + m_{p}. Within the fourpopulation approach, the S1 to S3 subtypes can be combined in terms of the mass and filling factor. In general, the filling factor of the target φ_{t} is increased during the impact such that the filling factor of the largest fragment φ_{1} > φ_{t}. For sticking with mass transfer (S4), a range of fragments exists. Since sticking is identified with growth of the largest fragment, it is m_{1} > m_{t}. If there are only fragments below the resolution limit, then the mass of the second largest fragment m_{2} and the mass of the powerlaw population m_{pw} vanish. Otherwise there are a range of fragments with nonzero masses.
Bouncing is characterised by two fragments in the final fragment distribution. For bouncing with compaction (B1), the masses are unaltered, i.e., m_{1} = m_{t} and m_{2} = m_{p}, but the filling factors are increased such that φ_{1} > φ_{t} and φ_{2} > φ_{p}. For the case of bouncing with mass transfer (B2), the filling factors are also increased but the masses are altered such that m_{1} + m_{2} = m_{t} + m_{p} and m_{1} ≠ m_{t} as well as m_{2} ≠ m_{p}. By definition, no fragments are produced in the bouncing events such that m_{pw} = m_{sr} = 0. For B2, the filling factors are also increased, i.e., φ_{1} > φ_{t} and φ_{2} > φ_{p}.
The fragmentation events (F1 to F2 types) are characterised by the mass of the largest fragment being lower than the highest mass before the collision, i.e. m_{1} < m_{t}. The distinction between F1 and F2 in terms of the collision outcome is unclear. In both cases, a powerlaw as well as a subresolution population is generated, i.e. m_{pw} > 0 and m_{sr} > 0. It seems that for F2, the mass of the target is only reduced by a small amount such that m_{1} ≲ m_{t} (Güttler et al. 2010). In this reference, F3 is also characterised by the target (solid plate) gaining mass, i.e. m_{1} > m_{t}. This is inconsistent with the idea that fragmentation is equivalent to m_{1} < m_{t}. The mass of the second largest fragment has some value m_{2} > 0 and total masses of the powerlaw and subresolution populations are m_{pw} > 0 and m_{sr} > 0.
The transition between sticking and fragmentation can consequently be characterised by the transition m_{1} > m_{t} → m_{1} < m_{t}, since for the S4 type powerlaw and subresolution population are already present. In contrast, the transition from bouncing (which also includes the change of target and projectile masses by mass transfer in B2) can be defined by the appearance of a powerlaw and subresolution population, i.e. m_{pw} = 0 → m_{pw} > 0 and m_{sr} = 0 → m_{sr} > 0, together with a nongrowing target m_{1} ≤ m_{t}.
In this section, we have shown that the fourpopulation model for collision outcomes is capable of encompassing all the sticking, bouncing, and fragmentation subtypes. Furthermore, we have demonstrated that the transition between these types can be modelled continuously by utilising the masses of each of the four populations.
5. Applying the new model to simulation data
We apply the fourpopulation model to a study of collisions of medium porosity preplanetesimals with different velocities to demonstrate that the outcomes of preplanetesimal collisions can be described quantitatively using the model. We carry out 24 simulations of headon collisions involving spherical dust aggregates with target and projectile radii of r_{t} = 10 cm and r_{p} = 6 cm modelled using 238 238 and 51 477 SPH particles, respectively. We choose the initial filling factor of the aggregates to be φ = 0.35 resulting in target and projectile masses of 2.93 and 0.63 kg, respectively. We vary the collision velocity between 0.1 and 27.5 ms^{1}. Table 4 summarises the simulations carried out. We broadly categorise the simulations by eye into bouncing, sticking, or fragmentation so that a comparison can be made between the results of our model and the categorisations used previously. We note that these broad categorisations are only employed to show where the boundaries between these regimes lie and are not used for the quantitative approach of our model.
As discussed in Sect. 4.2, the outcome of preplanetesimal collisions can be quantitatively described by a number of parameters such as the final mass, size, energy, velocity, porosity, and rotation and each of these parameters can be used to describe the four populations. In this preliminary, study we focus on the final mass, porosity, and energy of the different populations in our model.
Collision velocities used in the simulations.
Figure 3 shows how the mass distribution amongst the four populations varies with collision velocity. At low collision velocities, the contact energy and thus the tensile strength is too low to hold the objects together. This results in bouncing causing the overall mass distribution being similar to the initial distribution. The collision with 0.2 ms^{1} shows evidence of mass transfer resulting in the largest fragment being smaller than the target. As the collision velocity increases, the energy is dissipated by plastic deformation resulting in sticking such that all the mass is stored in a single object. At even higher collision velocities in which fragmentation is seen, the mass stored in the largest fragment is reduced but is increasingly present in the powerlaw population. Figure 3 also shows how the mass of the largest fragment varies with collision velocity. It can be seen that three distinct regions exist, which justify the broad classification of Table 4. However, there do not appear to be any distinctions within these regions which justify an additional division into sticking, bouncing, and fragmentation subtypes. A sharp transition between the bouncing and sticking regions exists at ~1 ms^{1}. Above 10.5 ms^{1}, pure sticking no longer occurs and the mass of the largest fragment begins to decrease as the transition between sticking and fragmentation takes place. As a result of very high collision velocities, the mass contribution of the subresolution population dominates over the largest and second largest fragment which is an indicative of violent disruption. We note that the simulation with collision velocity 11.5 ms^{1} still results in collision growth but above this velocity the mass gain of the largest fragment is negative.
Fig. 3 Cumulative plot of the contributions to the total mass in the system by the largest (grey slashed), second largest (solid grey), powerlaw (black slashed), and subresolution (solid black) populations after the aggregate collisions at various velocities. At low velocities, where bouncing occurs, the mass is wholly within the first and second largest fragments, while at intermediate velocities, where sticking occurs, the contribution to the mass is in the largest fragments. At high velocities, the mass contribution from the powerlaw population becomes significant. 

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Fig. 4 Outcome of the dust collision simulation with 11.5 ms^{1} (top) and 12.5 ms^{1} (bottom) at a time, t = 0.8 s. The collision with 11.5 ms^{1} results in the growth of the target but also a large chunk does break off such that pure sticking does not occur. The situation is adequately mapped with the appearance of a second largest fragment. For 12.5 ms^{1} the target breaks apart and the powerlaw population becomes as significant as the largest fragment. The transition from sticking to fragmentation occurs in between the presented collision velocities. 

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Figure 3 clearly shows that at velocities ≳ 11.5 ms^{1}, pure sticking no longer occurs and a transition into the fragmentation regime begins. For the simulation with a collision velocity of 11.5 ms^{1} (see Fig. 4, top, for an illustration of the resulting fragments), the mass of the largest fragment clearly increases but according to the model by Güttler et al. (2010), it is unclear whether this simulation would be classed as sticking with mass transfer (S4) or fragmentation with mass transfer (F3). Using our model, such an intermediate region can be described quantitatively. At ~12.5 ms^{1} (see Fig. 4, bottom, for an illustration), the mass contribution from the powerlaw population becomes as significant as the contribution from the largest fragment. In this region, the target fragments into a small number of large pieces. We expect that the transition from the sticking to fragmentation regime, described in Sect. 4.3, occurs between 11.5 and 12.5 ms^{1}.
Using the model, it is clear that the mass of the largest fragment decreases sharply for collision velocities ≳ 11.5 ms^{1}, thus this is the region where fragmentation takes place. We expect that this fragmentation boundary will change depending on a number of other parameters such as impact parameter and mass ratio (Blum & Münch 1993), porosity, and the rotation of the dust aggregates. Further investigation into the factors that determine the fragmentation boundary is crucial to ultimately understand under what conditions fragments may grow to planetesimal sizes. It is important to note that to decrease the computational expense, the SPH particles that move out of a radius of 20 m are removed from the simulation. Therefore, the total mass at the end of the higher velocity simulations is smaller than the initial mass. However, the total mass removed from the simulation is ~2% in the highest velocity simulation.
Fig. 5 Mass of the second largest fragments. The broad categorisation into bouncing (open triangles), sticking (closed triangles), and fragmentation (open squares) can be identified by masses of the second largest fragments being approximately the projectile mass (dashed line), nearly vanishing, and smaller than the projectile mass, respectively. For the fragmenting collisions, the mass of the second largest fragment initially increases with collision velocity. However, at higher collision velocities, the fragment mass decreases because of the collision nature of the simulations. 

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Figure 5 shows how the mass of the second largest fragment varies. For low collision velocities, it is evident that bouncing occurs and the projectile, whose mass is indicated by the dashed line in Fig. 5, appears as the second largest fragment with unaltered or slightly increased mass in the final distribution. For higher collision velocities, the projectile sticks to the target and no second largest fragment results, which is indicated by vanishing masses in this regime. As the velocity further increases, the resulting mass of the second largest fragment increases again but is smaller than the projectile mass, which indicates fragmentation. The increase is followed by a sharp decrease in the mass of the largest fragment. These simulations, which are reasonably close to the stickingfragmentation boundary not only cause the two aggregates to fragment, but also cause mass to be transferred between the target and projectile. At higher velocities still, the impact is sufficiently violent for the second largest fragment to also decrease sufficiently.
Figure 3 shows that as the collision velocity increases, the contribution to the mass from the powerlaw population also increases. As an outcome of preplanetesimal collisions, the cumulative mass distribution of the fragments is often described by a powerlaw (11)where n(m) dm is the number of fragments within the mass range [m,m + dm ] , m_{f} is the fragment mass, and μ_{pw} is the most massive member of the powerlaw population. The quantities m, m_{f}, and μ_{pw} are normalised by the total mass of the powerlaw population m_{pw} and κ is the powerlaw index.
Figure 6 shows the cumulative mass distribution m_{cum}(m_{f}) against the fragment mass normalised by m_{pw}. For higher fragment masses m_{f}, a powerlaw fit can be obtained that describes the mass distribution of the powerlaw population. As the velocity increases, the slope of the powerlaw decreases. This is because at higher collision velocities, the destruction of the dust aggregates is more violent and a larger number of smaller fragments results. At low fragment masses, it is currently unclear whether the deviation from the powerlaw distribution is physical, or whether it is a result of a low number of SPH particles (≲ 100) per fragment. We note that this deviation is also seen in the experimental results of Güttler et al. (2010).
Fig. 6 Cumulative mass distribution (given by Eq. (11)) against fragment mass of the powerlaw populations resulting from the simulations with 17.5 (open triangles), 25.0 (closed triangles), and 27.5 ms^{1} (open squares). Both axes are normalised by m_{pw}. For high fragment masses, the gradient of the slope decreases with increasing velocity. For low masses, it remains unclear whether the deviation from the powerlaw is a physical or numerical artefact. 

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Fig. 7 Final average filling factor of the largest fragment in each of the simulations. The simulations have been broadly categorised into bouncing (open triangles), sticking (solid triangles) and fragmentation (open squares). The filling factor varies smoothly as the collision velocity is increased. 

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Fig. 8 Final average filling factor (black line) of the powerlaw populations in each of the simulations. We also plot the maximum (upper grey line) and minimum (lower grey line) filling factors for each simulation, as well as the initial filling factor (dashed line). As the collision velocity increases, the range of filling factors for any one simulation increases. 

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We now consider how much compaction takes place in each of the simulations by considering the resulting filling factors of the various populations. Figure 7 shows the average filling factor of the largest fragment, φ_{1}, compared to the initial filling factor. As the velocity increases, the compaction also increases, causing the filling factor to increase with velocity. This forms a smooth curve between the initial filling factor of 0.35 and the maximum filling factor of ~0.58 for SiO_{2}. The curve resembles the FermiDirac shape of the compressive strength relation (Eq. (5)), which directly links the dynamic pressure to the obtained filling factor. We note that the appearance of fragmenting events coincides with the largest fragment reaching a filling factor close to the maximum filling factor. This suggests that fragmentation sets in when the material is maximally compressed. Furthermore, we stress that the transition of the filling factor is smooth right from the low velocity (bouncing) collisions, through to the medium velocity (sticking) collisions to the high velocity (fragmentation) collisions. For simulations with higher initial filling factors, we expect there to be a direct transition between the bouncing and fragmentation regimes, as discussed in Sect. 4.3.
The transition is particularly important because for planet formation, we are primarily concerned with the evolution of the largest fragment. This demonstrates that our model can quantitatively capture the results of the collisions over a wide region of velocity parameter space. Our preliminary results for the second largest fragment suggest that only a small amount of compaction takes place for the second largest fragment in low velocity bouncing simulations such that the final filling factor is very close to the initial filling factor, while for high velocity fragmentation simulations, a large amount of compaction takes place resulting in filling factors close to the maximum value of 0.58. Additional investigations will be carried out in a future study.
Fig. 9 Filling factor distribution for the simulations with 17.5 (solid line), 25.0 (short dashed line) and 27.5 ms^{1} (long dashed line). The size of a filling factor bin is 0.01. As the collision velocity increases, the number of fragments increases. For higher collision velocities, the majority of fragments have lower filling factors than the original value (dotted line). 

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Figure 8 shows the average, maximum, and minimum filling factors of the powerlaw population. At higher velocities when more violent fragmentation occurs, the spread in the filling factor is greater than at lower velocities. This suggests that at lower velocities, fragments may be chipped off without too much change to their compaction, whereas in the more violent cases with higher collision velocities, the fragments may become compacted before being chipped off or rupture because the plastic flow occurs where parts of the dust are stretched before being ripped off. Figure 9 shows the filling factor distribution of the powerlaw populations resulting from the simulations with 17.5, 25.0, and 27.5 ms^{1}. As the collision velocity increases, the number of fragments increases. In particular, most of the particles have filling factors smaller than the initial value of 0.35. This suggests that during the collision, fragments are ripped off instead of being compressed before breaking apart.
Finally, we explore the contributions to the total energy (normalised by the initial energies) from the different populations. The total energy is the sum of the energy stored in translation, rotation, and vibration. Figure 10 shows that at low velocities the major energy contribution comes from the largest fragment, while at higher velocities the contribution from the powerlaw population becomes somewhat equally significant (at ~12.5 ms^{1}) and even more so at even higher velocities. At low velocities, the energy is stored in elastic deformation and released into kinetic energy again so that a smaller fraction of the initial energy is dissipated. As the velocity increases plastic deformation occurs causing energy dissipation. At even higher velocities, though energy is still dissipated (since bonds are broken in the fragmentation process), the dissipated energy as a fraction of the initial energy due to bonds being broken is not as large as the energy dissipation due to plastic deformation. For very high impact velocities, a considerable amount of energy is stored in the subresolution population. Figure 11 shows the absolute energy dissipated at each collision velocity as well as the initial energy. The total amount of energy dissipated increases smoothly with increasing velocity, irrespective of the bouncing, sticking, or fragmentation regime. We note that in these examples, the final rotational energies are not very significant because the collisions are headon. The difference between the rotational and translational energies will become more important in simulations with nonzero impact parameters.
Fig. 10 Cumulative plot of the contributions to the total energy in the system by the largest (grey slashed), second largest (solid grey), powerlaw (black slashed), and subresolution (solid black) populations after the aggregate collisions at various velocities. At low velocities, the energy is primarily from the largest fragment, whereas at higher collision velocities, where more fragments form, the contribution from the powerlaw population becomes more significant. 

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Fig. 11 Initial (dotted line) and dissipated (solid line) energies against the collision velocity. The amount of energy dissipated changes smoothly with collision velocity, regardless of whether the simulations involves bouncing (open triangles), sticking (closed triangles), or fragmentation (open triangles). 

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We have presented here the results of a small number of simulations, which show that transitions between the bouncing, sticking, and fragmentation regions occur and that the results of preplanetesimal collisions can be described quantitatively. Our study could be extended to explore a vast parameter space of inputs. Our model has been shown not only to encompass previous qualitative models (Sect. 4) but also provide an alternative model that focuses on the quantitative outcome of preplanetesimal collisions. Furthermore, the model can provide an accurate input into global models, which may then carry out detailed calculations of preplanetesimal collisions. In addition, this model provides a powerful aid to determine the region of parameter space that allows growth of preplanetesimals to occur.
6. Discussion and outlook
We have demonstrated that our SPH code, extended and calibrated for the simulation of porous SiO_{2} dust, is capable of reproducing all sticking, bouncing, and fragmentation types that appear in collision experiments with macroscopic porous dust aggregates. In addition to the quantitatively correct simulation of laboratory benchmark experiments (Güttler et al. 2009; Geretshauser et al. 2010), this consolidates the validity of the applied porosity model and shows its readiness for the application in the field of investigating preplanetesimal collisions. Since the continuum approach of the SPH method does not place an upper bound on the aggregate size, collision data of a parameter space that have been inaccessible so far in laboratory experiments can now be provided for further use in global coagulation models.
For this transfer, a suitable mapping of collision data has to be chosen, which is accurate enough to quantitatively capture the most important features of any combination of sticking, bouncing, and fragmentation and simple enough to be implementable in global coagulation models. We have attempted to map our simulation data to the categorisation by Güttler et al. (2010), which was the most elaborate collision model previously available. On the one hand, the distinction between four sticking, two bouncing, and three fragmentation types introduces a considerable amount of complexity caused by distinguishing between a mixture of qualitative and quantitative attributes and by adhering to a distinct classification of these events. On the other hand, we have found a collision outcome that could not clearly be attributed to one of the proposed categories.
Because of this ambiguity, we have proposed a new model, which is based on quantitative aspects. For this purpose, we have divided the set of fragments of a collision into four populations: the largest and second largest fragment are described by distinct values for the characteristic quantities of mass, filling factor, and kinetic energy to name only a few. The powerlaw population is described by distributions and the subresolution population by average values of the characteristic quantities. The largest fragment indicates growth or erosion, the second largest fragment accounts for bouncing, the powerlaw population quantitatively describes the amount of fragmentation, and the subresolution population gives an upper limit for smaller fragments, which are not captured because of insufficient resolution. Since the SPH code is not restricted to small aggregate sizes, the importance of the subresolution population becomes significant for aggregate collisions between objects of approximately metre size and more. For growth models that rely on the sweeping up of small particles (Teiser & Wurm 2009), the subresolution population also plays an important role. We have demonstrated that this model in general encompasses the model proposed by Güttler et al. (2010) but is also capable of capturing intermediate events.
Finally we have applied the new model to map data for headon collisions of aggregates with intermediate (φ = 0.35) porosity and varying impact velocity. We have shown that the broad sticking, bouncing, and fragmentation categorisation can still be found in the fourpopulation model. But in addition, we have also shown that continuous transitions in the variation in the mass of the largest fragment, the filling factor, and the final kinetic energy of the fragments with collision velocity exhibit a more quantitative description. The ability to capture these transitions justifies the design of the fourpopulation model and demonstrates its descriptive power.
Despite its narrow parameter range, we can draw the following conclusions from the velocity study of Sect. 5. For the transition between bouncing and sticking, we find a threshold velocity of ~1 ms^{1} and that the transition from sticking to fragmentation lies between 11.5 and 12.5 ms^{1}. Since our initial filling factor φ = 0.35 is close to the critical filling factor 0.4, which separates porous from compact aggregates in Güttler et al. (2010), our findings cannot be directly compared to their results. For collisions between equally sized highly porous and very compact aggregates, they found a direct transition from bouncing to fragmentation at ~1 ms^{1}. However, for collisions between a compact target and a porous projectile of equal size they find a bouncingsticking transition at 1 ms^{1} and a transition from sticking to no mass gain at 9.4 ms^{1}. These thresholds resemble our findings for intermediate porosity very well. Our results for fragmenting collisions indicate that the powerlaw index of the fragment mass distribution is velocity dependent. This is supported by the collection of laboratory fragmentation data (Mathis et al. 1977; Davis & Ryan 1990; Blum & Münch 1993; Güttler et al. 2010). Furthermore, it is physically reasonable that in more violent collisions the fraction of smaller fragments increases. This suggests a velocitydependent powerlaw index.
We note that the results presented in Sect. 5 are valid for collisions between homogeneous aggregates of intermediate porosity. Increasing inhomogeneity might affect the presented threshold velocities. Furthermore, rotation of the largest and second largest fragments might cause them to fall apart beyond the simulated time, an outcome that eventually affects their final size. The results presented here, in particular for fragmenting collisions, are based on one simulation for each collision velocity. Although we do not expect a large variation in outcome because of the symmetry given by a headon collision of two spheres, a profound statistical investigation has to be carried out. It remains to be investigated whether the deviation of the powerlaw mass distribution from a powerlaw for low fragment masses is a numerical or physical effect. Despite these drawbacks, we have been able to demonstrate the applicability and functionality of the fourpopulation model by means of our simulation results.
Despite increased experimental efforts, only small spots of the required parameter space of preplanetesimal collisions are actually covered by empirical data. Vast regions of these maps remain terra incognita and collision data for preplanetesimal sizes larger than centimetre are missing.
With both a code calibrated for the simulation of preplanetesimals (Geretshauser et al. 2010) and the fourpopulation model as an adequate mapping model, we have established a basis for profoundly investigating all aspects of preplanetesimal collisions and transferring acquired data to global dust coagulation models. In future studies, these tools can be utilised to generate a catalogue of preplanetesimal collisions. The fourpopulation model will be applied to investigate how the collision behaviour depends on important parameters such as aggregate porosity and inhomogeneity, mass ratio of the collision partners, impact velocity, impact parameter, and rotation. Furthermore, we will assess the statistics of our fragmentation results.
Appendix A: List of symbols
List of symbols.
Acknowledgments
R.J.G. and R.S. wish to thank C. Güttler, M. Krause, and J. Blum for the intensive and fruitful collaboration and W. Benz and his group for many illuminating discussions. We thank our anonymous referee for the thorough revision and constructive comments, which helped to improve this paper. The SPH simulations were performed on the university cluster of the computing centre of Tübingen, the bwGriD clusters in Karlsruhe, Stuttgart, and Tübingen. Computing time was also provided by the High Performance Computing Centre Stuttgart (HLRS) on the national supercomputer NEC Nehalem Cluster under project grant SPHPPC/12848. This project was funded by the Deutsche Forschungsgemeinschaft within the Forschergruppe “The Formation of Planets: The Critical First Growth Phase” under grant Kl 650/81.
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All Tables
All Figures
Fig. 1 The outcome of our simulations of preplanetesimal collisions encompasses all sticking (S), bouncing (B), and fragmentation (F) types proposed by Güttler et al. (2010). The initial configuration for each simulation is a sphere with radius r_{t} = 10 cm as resting target and a sphere with r_{p} = 6 cm as projectile except for S3 and F2, where r_{p} = 2 cm. The colour code indicates the filling factor φ. Both objects are initially set up with φ = 0.35 except for the F2 case, where φ = 0.55. The simulations are carried out with different impact velocities and the snap shots are taken at different times. The details are given in the text. 

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In the text 
Fig. 2 Illustration of the fourpopulation model. The left side displays the situation before the collision: two preplanetesimals collide with impact velocity v_{0} and impact parameter b. The target and projectile are characterised by their defining quantities, e.g., mass m, filling factor φ, and rotational energy E_{rot}. Depending on these parameters, an outcome population is generated in the collision (middle). The fourpopulation model distinguishes the fragments according to their mass. The population classes are: a) the largest fragment; b) the second largest fragment; c) the powerlaw population; and d) the subresolution population. This categorisation is sufficient to describe the outcome types of Fig. 1 as well as intermediate outcomes. 

Open with DEXTER  
In the text 
Fig. 3 Cumulative plot of the contributions to the total mass in the system by the largest (grey slashed), second largest (solid grey), powerlaw (black slashed), and subresolution (solid black) populations after the aggregate collisions at various velocities. At low velocities, where bouncing occurs, the mass is wholly within the first and second largest fragments, while at intermediate velocities, where sticking occurs, the contribution to the mass is in the largest fragments. At high velocities, the mass contribution from the powerlaw population becomes significant. 

Open with DEXTER  
In the text 
Fig. 4 Outcome of the dust collision simulation with 11.5 ms^{1} (top) and 12.5 ms^{1} (bottom) at a time, t = 0.8 s. The collision with 11.5 ms^{1} results in the growth of the target but also a large chunk does break off such that pure sticking does not occur. The situation is adequately mapped with the appearance of a second largest fragment. For 12.5 ms^{1} the target breaks apart and the powerlaw population becomes as significant as the largest fragment. The transition from sticking to fragmentation occurs in between the presented collision velocities. 

Open with DEXTER  
In the text 
Fig. 5 Mass of the second largest fragments. The broad categorisation into bouncing (open triangles), sticking (closed triangles), and fragmentation (open squares) can be identified by masses of the second largest fragments being approximately the projectile mass (dashed line), nearly vanishing, and smaller than the projectile mass, respectively. For the fragmenting collisions, the mass of the second largest fragment initially increases with collision velocity. However, at higher collision velocities, the fragment mass decreases because of the collision nature of the simulations. 

Open with DEXTER  
In the text 
Fig. 6 Cumulative mass distribution (given by Eq. (11)) against fragment mass of the powerlaw populations resulting from the simulations with 17.5 (open triangles), 25.0 (closed triangles), and 27.5 ms^{1} (open squares). Both axes are normalised by m_{pw}. For high fragment masses, the gradient of the slope decreases with increasing velocity. For low masses, it remains unclear whether the deviation from the powerlaw is a physical or numerical artefact. 

Open with DEXTER  
In the text 
Fig. 7 Final average filling factor of the largest fragment in each of the simulations. The simulations have been broadly categorised into bouncing (open triangles), sticking (solid triangles) and fragmentation (open squares). The filling factor varies smoothly as the collision velocity is increased. 

Open with DEXTER  
In the text 
Fig. 8 Final average filling factor (black line) of the powerlaw populations in each of the simulations. We also plot the maximum (upper grey line) and minimum (lower grey line) filling factors for each simulation, as well as the initial filling factor (dashed line). As the collision velocity increases, the range of filling factors for any one simulation increases. 

Open with DEXTER  
In the text 
Fig. 9 Filling factor distribution for the simulations with 17.5 (solid line), 25.0 (short dashed line) and 27.5 ms^{1} (long dashed line). The size of a filling factor bin is 0.01. As the collision velocity increases, the number of fragments increases. For higher collision velocities, the majority of fragments have lower filling factors than the original value (dotted line). 

Open with DEXTER  
In the text 
Fig. 10 Cumulative plot of the contributions to the total energy in the system by the largest (grey slashed), second largest (solid grey), powerlaw (black slashed), and subresolution (solid black) populations after the aggregate collisions at various velocities. At low velocities, the energy is primarily from the largest fragment, whereas at higher collision velocities, where more fragments form, the contribution from the powerlaw population becomes more significant. 

Open with DEXTER  
In the text 
Fig. 11 Initial (dotted line) and dissipated (solid line) energies against the collision velocity. The amount of energy dissipated changes smoothly with collision velocity, regardless of whether the simulations involves bouncing (open triangles), sticking (closed triangles), or fragmentation (open triangles). 

Open with DEXTER  
In the text 
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