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Planet Formation – an unresolved puzzle Michael Wilkinson (Open University) Bernhard Mehlig (Gothenburg University)

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Presentation on theme: "Planet Formation – an unresolved puzzle Michael Wilkinson (Open University) Bernhard Mehlig (Gothenburg University)"— Presentation transcript:

1 Planet Formation – an unresolved puzzle Michael Wilkinson (Open University) Bernhard Mehlig (Gothenburg University)

2 Overview Lecture 1: Particles suspended in a turbulent fluid flow can cluster together. This surprising observation has been most comprehensively explained using models based upon diffusion processes. Lecture 2: Planet formation is thought to involve the aggregation of dust particles in turbulent gas around a young star. Can the clustering of particles facilitate this process? The final lecture will discuss the problems of planet formation, and consider whether aggregation of particles is relevant. Clustering does not help to explain planet formation, but planet formation does introduce new applications of diffusion processes. However, no version of the dust aggregation model appears to be satisfactory. An alternative hypothesis is introduced.

3 The solar system : Eight planets, numerous smaller bodies, orbiting a typical star, mass The structure has some striking features: The orbits are nearly circular, and nearly coplanar with equator of sun. The planets rotate about axes close to the rotation axis of the sun. Several planets have moons, again with circular, coplanar orbits. These features suggest origin in a disc. M,V,E,M are rocky planets J,S are gas giants U,N are ice giants

4 Formation of stars by gravitational collapse : The interstellar medium includes large molecular clouds: mainly molecular hydrogen, some helium. There are also heavier materials which were made inside stars, and which where blown away from the surface, or dispersed by a supernova explosion. This includes water, small organic molecules, dust. The density and temperature are very low: The cloud collapses due to gravitational self-attraction. The collapse is limited by build up of pressure (which can be relieved as the collapsing gas cools) and by the conservation of angular momentum.The cores of the collapsed regions become dense and hot enough to start nuclear reactions (hydrogen to helium..). They become stars. Artist’s impression of a nascent star (a ‘protostar’)

5 Circumstellar discs : Some material has too much angular momentum to fall in to the stars, remaining behind as circumstellar nebula. It forms a structure with as little internal motion and potential energy as possible for the amount of angular momentum: a circumstellar disc. astro.berkeley.edu /~kalas/disksite/pages/bpic.html Artist’s impression Beta Pictoris at 0.5 micron

6 Accretion in circumstellar discs : Material in the circumstellar disc rotates with a speed close to the Kepler velocity: Because the Kepler rotation rate decreases with radius, there is a velocity gradient. If there are viscous forces acting, they cause a torque which speeds up material at higher radius, and slows material at smaller radius. Angular momentum is transferred from the centre to the outside of the disc. As the material at small radius slows, gravity draws it inwards. Viscous torque causes material to accrete onto the star by transferring angular momentum outwards. Viscosity causes the circumstellar disc to disappear. But molecular viscosity is much too slow. Surveys of stars indicate that the disc lifetime is order one million years. It is surmised that turbulence causes an effective viscosity which is much larger than the molecular viscosity.

7 The standard model for planet formation : Model Dust particles in the accretion disc collide and stick together, making larger and larger clusters. Eventually the clusters become large enough that their mutual gravitational interaction is significant. These planetessimals continue to collide with each other until they form planets. Supporting evidence Because the planets form within a disc, the model explains why the planets in our solar system have nearly circular and nearly coplanar orbits. Theoretical Questions We need to understand the rate of collision of particles in a turbulent environment, which is determined by their relative velocities. We need to estimate the intensity of turbulence in the circumstellar disc.

8 Turbulence Fluid motion is determined by the Navier-Stokes equation. When the effects of viscosity are weak, the fluid flow is very complex: Statistical ideas must be used to describe turbulence. Turbulence is a multi-scale flow: large-scale eddies interact to make smaller scale eddies. Energy is dissipated by viscosity on the smallest scale of the cascade. Image from M.A.Green et al, J. Fluid. Mech. 572, 111 (2007).

9 Kolmogorov theory of turbulence All modern theories of turbulence are based upon work by Kolmogorov (1941). He argued that the on shorter length scales the turbulence ‘forgets’ how it was generated. The only variables that enter are the energy dissipation per unit mass and the kinematic viscosity (which is a diffusion constant for the transfer of momentum). The kinematic viscosity can only influence properties of the smallest eddies, where energy is dissipated. Dissipation of energy occurs at the Kolmogorov lengthscale and timescale. These are deduced by dimensional analysis: Many properties of motion one scales larger than the dissipation scale can be deduced from dimensional analysis alone:

10 Motion of dust particles Model the dust grains as spheres of radius moving in a gas with a turbulent velocity field. The equation of motion is Damping rate for a spherical particle of radius in a conventional fluid was given by Stokes In gases with very low density (mean free path large compared to the particle), the same equation of motion hold. The damping rate was obtained by Epstein (1923):

11 Collision rates For spherical particles the collision rate of a particle in a dilute gas is: It is important to estimate the relative velocity of the dust particles. When the dust grain clusters become sufficiently large, their inertia becomes important, and their velocity becomes different from that of the surrounding gas. We model the evolution of the relative positions and velocities of particles by a diffusion process.

12 Diffusive model for relative velocities Equation of motion for separation of dust grains: Langevin model: Corresponding Fokker-Planck equation:

13 Predictions for relative velocities An approximate solution of the Fokker-Planck equation yields the following approximate distribution for relative velocities: From this we obtain an estimate for the variance: Here is dimensionless. This can also be surmised from the Kolmogorov theory of turbulence. We expect that the motion of weakly-damped particles depends only upon the rate of dissipation, and not on the kinematic viscosity. The result then follows from dimensional analysis alone.

14 Modelling circumstellar gas discs : We will find that the properties of accretion discs are (with some simplifying assumptions) determined by the accretion rate. Surveys indicate disc lifetimes of roughly a million years, and it is estimated that the disc initially contains about 10 percent of the mass of the star. We therefore use Other parameters for model:

15 Accretion discs – conservation principles : The structure is determined by the conservation equations for mass, angular momentum and energy, combined with equations for hydrostatic equllibrium, and an estimate of turbulent viscosity. Viscous drag leads to a torque Conservation of mass: Transport of angular momentum: Steady state solution, valid at large radius: Viscous drag causes dissipation, at a rate per unit area Find:

16 Accretion disc structure - equations : Mass, angular momentum and energy balance give: We make an ansatz for the effective kinematic viscosity due to turbulent motion: Equations are closed by relating disc height to temperature and speed of sound: These yield an estimate: These equations describe a thin, optically thick accretion disc which is heated by viscous dissipation. The solution is specified by a single parameter, the accretion rate.

17 Some properties of circumstellar discs : Our steady-state model predicts that quantities have a power-law scaling: Values at radius of based upon

18 Collision velocity as a function of size

19 The Stokes trap The relative velocity of clusters with Stokes number larger than unity is sufficiently large that the clusters will usually fragment upon impact: for solar- type stars we estimate (at radius): When dust clusters become large enough that their Stokes number is order unity, they start to fragment upon collision. This is the Stokes trap. It occurs for particles of approximate size: It is not clear how to escape this ‘Stokes trap’ and proceed to larger clusters.

20 Extra-solar planets : detection : About 300 extra-solar planets have been detected, orbiting other stars. Several methods have been used: 1.The ‘wobble’ in motion of a star due to an orbiting planet can be detected by the Doppler effect. Velocity of star Apparent amplitude Limit of sensitivity: Signal due to Jupiter: 2.The transit of a planet across a star can be detected as a slight reduction in luminosity of the star. 3.Gravitational lensing effects from planets have been observed. With these techniques it is easier to detect large planets with small rotational periods.

21 Extra-solar planets : observations : The extra-solar planets turned out to have some surprising features. Some observations: 1.There are many planets with large eccentricity. 2.There are numerous examples of ‘hot Jupiters’, that is gas-giant planets which orbit very close to their star. 3. There are many examples with more than one planet. Resonances between periods are common in these cases:

22 Data on exo-solar planets : eccentricity :

23 Data on exo-solar planets : masses :

24 Concurrent collapse We propose that planets are formed by gravitational condensation of a cloud of interstellar gas, at the same time as their star is being formed by the same process. This mechanism does not rely upon colliding particles adhering to each other. The objects which are produced by gravitational collapse will be termed juvenile planets. They must initially have a composition which is similar to that of the interstellar medium. They would have to undergo a radical transformation to become rocky or icy planets. We propose that such transformations can occur due to interaction with the residual gas in the protostellar nebula, or by collisions.

25 Gravitational collapse Simulations of gravitational collapse by Matthew Bate,

26 Interaction of juvenile planet with gas disc Juvenile planet may pass through the gas disc at a high velocity, of order. Material can be removed from its outer layers, reducing the fraction of lighter elements (because heavier elements may sink to its core). Also, momentum is transferred, and the motion of the juvenile planet might become entrained to the disc (reaching a nearly circular, nearly in-plane orbit). Can this happen? The planet becomes entrained to the disc if the mass of gas displaced is comparable to the mass of the juvenile planet. Estimate the number of orbits for this to be achieved: The numbers in this estimate are uncertain by orders of magnitude. This implies that in some cases juvenile planets would be entrained to circular orbits, in other cases the orbits remain elliptical. Planet mass, density, size Gas disc density, orbit radius Mass of gas displaced per orbit planet entrained in

27 Collisions between juvenile planets Let us estimate the probability for collision of two juvenile planets, in eccentric orbits of approximate radius : Approximate area swept out by orbit of one planet: Approximate cross sectional area of a planet: Probability of collision per orbit: We conclude that collisions between juvenile planets in elliptical orbits are possible. Depending upon parameters, they may be unlikely or almost inevitable. What are the consequences? Large amounts of debris would be produced. If two Jupiter size planets collide, large amounts of debris will be scattered into orbits which will reach the star. The first fragments will reach the star in a fraction of the orbital period (perhaps 1-10 years), and material will continue to reach the star at a significant rate for several multiples of the orbital period (perhaps years). The total amount of material is solar masses, which gives a rate of accretion three orders of magnitude higher than the typical rate. Collisions can explain the magnitude and timescale of outbursts.

28 FU Orionis outbursts FU Orionis is a star which started to increase in luminosity in Over a few years the luminosity increased by three orders of magnitude, before starting to decrease. The star appears to be surrounded by a dusty cloud, consistent with it being a young star. Since them many other outburst events have been observed in other young stars. The events are very diverse. Common features are: quick rise time (1-10 years), relatively slow decay ( years), increase in magnitude is very large (2-6 orders). There is no apparent change preceding the outburst. Surveys suggest that most young stars experience a few outbursts. Most published explanations assume an instability of the accretion disc. These instabilities require the gas to become opaque due to ionisation of hydrogen. This requires very high temperatures.

29 Summary on concurrent collapse 1.The juvenile planets are formed in eccentric orbits. The existence of circular orbits can be explained by entrainment to the gas disc. 2.Collisions between juvenile planets could explain ‘outbursts’. 3. The model is consistent with planetary systems being highly variable in structure. The concurrent collapse hypothesis avoids the problems of having to build planets by aggregation of dust in a turbulent environment. It suggests simple models or explanations for some observations: The juvenile planets are created with a composition reflecting that of the interstellar medium. Rocky or icy planets can be formed if heavier elements sink to the core of the juvenile planet, and if motion through the gas in the circumstellar disc strips away the outer layers.


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