Brownian motion growth: self-similar

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Dullemond & Dominik 2005 Brownian motion growth: self- similar

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Brownian motion growth: self-similar. Dullemond & Dominik 2005. Sedimentation-driven growth („rainshower“). One-particle model. Equator. Sedimentation-driven growth („rainshower“). One-particle model. Equator. Sedimentation-driven growth („rainshower“). One-particle model. Equator. - PowerPoint PPT Presentation

Transcript of Brownian motion growth: self-similar

Page 1: Brownian motion growth: self-similar

Dullemond & Dominik 2005

Brownian motion growth: self-similar

Page 2: Brownian motion growth: self-similar

One-particle model

Equator

Sedimentation-driven growth („rainshower“)

Page 3: Brownian motion growth: self-similar

One-particle model

Equator

Sedimentation-driven growth („rainshower“)

Page 4: Brownian motion growth: self-similar

One-particle model

Equator

Sedimentation-driven growth („rainshower“)

Page 5: Brownian motion growth: self-similar

One-particle model

Equator

Sedimentation-driven growth („rainshower“)

Warning: Not to scale! ;-)

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Sedimentation-driven growth („rainshower“)Equation of settling of the big dust grain:

Equation of growth by sweep-up as the big grain falls:

Relation between m(t) and a(t):

Distribution of the small dust:

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Sedimentation-driven growth („rainshower“)

Dullemond & Dominik (2005)

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“Rainshower” in a disk

Dullemond & Dominik (2005)

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Rain falling from a cumulus congestus cloud

Parallel with meteorology

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Now with convection

Dullemond & Dominik (2005)

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Cumulonimbus cloud, most probably with severe hail

Parallel with meteorology

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Layered structure of giant hail stone

Parallel with meteorology

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Main problem: high velocities

Particle size [meter]

30 m/s =100 km/h !!

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Dust coagulation+fragmentation model

Birnstiel, Dullemond & Ormel 2010

Grain size [cm]10-4 10-2 100

10-8

10-6

10-4

10-2Σ d

ust [

g/cm

2 ]

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Dust coagulation+fragmentation model

10-8

10-6

10-4

10-2Σ d

ust [

g/cm

2 ]

Grain size [cm]10-4 10-2 100

Birnstiel, Dullemond & Ormel 2010

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Meter-size barrier

1m 1mm 1m 1km

Growth from ‘dust’ to planetary building blocks

Brownianmotion

Differentialsettling Turbulence

Aggregation

Meter-size barrier

Sweep-up growthFragmentation

Rapid radial drift

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More barriers...

1m 1mm 1m 1km

Growth from ‘dust’ to planetary building blocks

Brownianmotion

Differentialsettling Turbulence

Meter-size barrier

Sweep-up growthFragmentation

Rapid radial drift

Aggregation

Bouncing barrier

Zsom et al. 2010, Güttler et al. 2010

Charge barrier

Okuzumi 2009

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The “Lucky One” idea

1m 1mm 1m 1km

Growth from ‘dust’ to planetary building blocks

Brownianmotion

Differentialsettling Turbulence

Meter-size barrier

Sweep-up growthFragmentation

Rapid radial drift

Aggregation

Let’s focus on the fragmentation barrier

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Windmark et al. 2012

How to create these seeds? Perhaps velocity distributions:Garaud et al. 2013; Windmark et al. 2012

Low sticking efficiency

Par

ticle

abu

ndan

ceThe “Lucky One” idea

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All the different collision outcomes...

Güttler et al. 2010

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Fluffy grains, compaction, bouncing...

Zsom et al. 2010