formation of planetary systems protoplanetary disks contain dust

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ASTR 3730: Fall 2003 Formation of planetary systems Protoplanetary disks contain dust - micron sized solid particles formed for example in the stellar winds of some stars. Initially the dust is uniformly mixed with the gas in the disk, but over time it will settle under gravity toward the midplane of the gas disk. Collisions between particles lead to growth: Initially because particles are `sticky’ - dissipate energy of relative velocity on impact Eventually because bodies become large enough that their own gravity attracts other bodies Dust Pebbles / rocks Planetesimals Planets microns cm - m km 10 3 km

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Page 1: Formation of planetary systems Protoplanetary disks contain dust

ASTR 3730: Fall 2003

Formation of planetary systemsProtoplanetary disks contain dust - micron sized solid particlesformed for example in the stellar winds of some stars.Initially the dust is uniformly mixed with the gas in the disk, butover time it will settle under gravity toward the midplane of the gas disk.Collisions between particles lead to growth:

• Initially because particles are `sticky’ - dissipate energy ofrelative velocity on impact

• Eventually because bodies become large enough that their own gravity attracts other bodies

Dust Pebbles / rocks Planetesimals Planetsmicrons cm - m km 103 km

Page 2: Formation of planetary systems Protoplanetary disks contain dust

ASTR 3730: Fall 2003

The architecture of the Solar System

Terrestrial planets: rocky, small gas fraction, close to Sun Giant planets: primarily gaseous, further from SunAll major bodies have close to circular orbits

Page 3: Formation of planetary systems Protoplanetary disks contain dust

ASTR 3730: Fall 2003

Traditionally, understood this as resulting from a temperaturegradient in the protoplanetary disk:

High temperature Low temperature

Rocky planetesimals Rocky and icy planetesimals

Snow lineat r ~ 3 au

• Surface density of planetesimals is larger beyond thesnow line, in parts of the disk cool enough for iceto be present

• Higher surface density -> more rapid formation of planets• In the outer Solar System, planets grew to ~20 MEarth while

gas was still present, captured gas to form gas giants• In inner Solar System, no gas was captured• All circular orbits as formed from a circular disk

Page 4: Formation of planetary systems Protoplanetary disks contain dust

ASTR 3730: Fall 2003

Extrasolar planetsAll but one known extrasolar planet around an ordinary starhave been found by monitoring the stellar radial velocity

First planet found:around the star 51 Peg by Mayorand Queloz (1995) Sinusoidal curve:circular orbitPeriod: 4.2 days

A `hot Jupiter’

Page 5: Formation of planetary systems Protoplanetary disks contain dust

ASTR 3730: Fall 2003

Orbital period ~ 1 yearNot circular: e = 0.32

Eccentricity e > 0.9

No examples of comparable planets in the Solar System

Page 6: Formation of planetary systems Protoplanetary disks contain dust

ASTR 3730: Fall 2003

`Typical’ planetmay be at sameorbital radius asJupiterHigh valuesof the orbitaleccentricity arecommonHot Jupitershave circularorbits

Page 7: Formation of planetary systems Protoplanetary disks contain dust

ASTR 3730: Fall 2003

Sensitivity:

Mmin µ a

Mostly moremassive thanJupiter

Page 8: Formation of planetary systems Protoplanetary disks contain dust

ASTR 3730: Fall 2003

Metallicity distributionof host stars

Consistent with theoretical ideas about massive planet formation:

• Higher fraction of heavy elements in the disk• More planetesimals• Faster planet formation / more likely to have planets

Page 9: Formation of planetary systems Protoplanetary disks contain dust

ASTR 3730: Fall 2003

Probability of transits:

P ªR*

7 ¥1010 cm6 ¥1011 cm

~ 10%

a = 0.04 au for a hot Jupiter

10 - 20 such planets known - approximately one likely to haveorbital inclination favorable for detecting a transit…

Observation from theground

Page 10: Formation of planetary systems Protoplanetary disks contain dust

ASTR 3730: Fall 2003

HST light curve

Determines:• Planetary radius• Constrains presence of moons / dense rings• Atmospheric composition (level of clouds)