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Extrasolar planets

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Title: Extrasolar planets


1
Extrasolar planets
2
In this lecture
  • Planets, Stars and Brown dwarves
  • Recap planetary formation stages
  • A missing population?
  • Planet detection methods
  • Radial velocity
  • Transits
  • Microlensing
  • Direct Imaging
  • Pulsar timing
  • Astrometry
  • Detection limits
  • weird systems detected
  • Giant branch stars
  • Hot Jupiters
  • Typical systems?
  • Prevalence of planets
  • Brown dwarf desert
  • Orbital behavior
  • The Future

www.exoplanet.eu
3
Planets and Brown Dwarves
  • Star
  • Interstellar cloud collapse
  • Burns hydrogen
  • Mass gt 75 MJ
  • Brown dwarf
  • Interstellar cloud collapse
  • Burns deuterium runs out fast
  • Mass gt 13 MJ
  • Jeans mass
  • Determines the mass of the smallest
  • object a collapsing cloud can form
  • At T10K
  • Densities not high enough to form

4
Planetary Formation Stages Revisited
  • Collapse of molecular cloud
  • In lt 106 year
  • Development of accretion disk
  • Create central gap at stars co-rotation distance
  • Form planetesimals
  • Bodies grow by pair-wise accretion
  • Self-gravity becomes important (r1km)
  • Oligarchic growth of largest objects
  • Gas Giant planets
  • Cores of 10 ME capture large gas envelopes
  • Opens gap in disk slowly migrates inward
  • Gaseous component dissipates lt 10 Myr

5
  • Disk
  • Gaseous component dissipates lt 10 Myr
  • Debris disks remain 200 Myr
  • Planets can migrate further by scattering small
    bodies
  • Large collisions still frequent

6
  • Inner planets are composed of rock and iron
  • Heated by radioactive decay

7
  • Gas giant planets Jupiter and Saturn
  • Similar rock/ice cores of about 10 earth masses
  • Large hydrogen envelopes molecular and metallic
  • Ice Giant Planets Uranus and Neptune
  • Rocky cores
  • Water and Ammonia interiors
  • Large hydrogen molecular envelopes

8
  • Another type of planet?
  • We have a gap in our solar system
  • An entire class of planet is unrepresented

?
  • More than 10 Earth Masses results in a gas giant
  • We know what planets in the 0-1 Earth Mass range
    look like
  • What about the 1-10 Earth Mass range -
    Super-Earths?

9
Planetary Detection Radial Velocity
  • Star and planet orbit systems center of mass
  • Stars motion small compared to planets as M gtgt
    MP
  • Star appears to approach and recede from us
    periodically
  • Causes Doppler blue- and red-shifting of spectral
    lines
  • Very precise spectral measurements needed
    iodine cell
  • Current technology 1-3 ms-1
  • Invert wavelength shift for velocity
  • e.g. max velocity of the sun due to Jupiter is
    12.5 ms-1
  • In reality fit signal for period, MP sin(i) and
    eccentricity
  • Cannot solve for inclination so mass is a lower
    limit
  • Star mass
  • Stars bigger (hotter) than the sun not enough
    absorption features
  • Stars smaller than the sun dont have a strong
    signal
  • Technique sensitive to big planets with small
    periods

10
Planetary Detection Transits
  • Planet passes in front of the star as seen from
    Earth
  • Inclination must be close to 90º
  • cos(i) lt (RRP)/a
  • If a1AU, R1 solar radius then probability
    0.4
  • If a0.05AU, R1 solar radius then probability
    8
  • Limits on transit technique
  • Brightness measurements precise to 0.1
  • (RP/R)2 gt 10-3 or Rp gt 0.032 R
  • e.g. for our solar system RPgt 22,000 km
  • Gas/ice giants, not terrestrial planets
  • Benefits of the transit technique
  • Gives you a size
  • All discoveries are good radial velocity
    candidates
  • Gets you a mass (and mean density)
  • Inclination is constrained

11
Planetary Detection Direct Imaging
  • 1AU separation at 1 parsec distance is 1
    arc-second
  • Definition of a par-sec (3.086x1016 m)
  • Angular separation is easy in ground-based
    telescopes
  • Problem is the glare from the main star
  • Use coronagraph
  • Speckle imagery
  • Longer wavelengths are better for contrast
  • But worse for resolution

12
  • Other methods
  • Microlensing
  • Pulsar timing
  • Supernova remnant
  • Very precise but rarely used
  • Astrometry

13
Whats Detectable?
  • Closer objects are easier
  • Radial velocity
  • Transits
  • Pulsar timing
  • Further objects are easier
  • Astrometry
  • Direct imaging
  • Microlensing not affected by distance
  • Heavy planets are always easier
  • Greater tug on star
  • Bigger signal easier to detect
  • Current sensitivity limits up to gt MSATURN
  • At reasonable distances from the star
  • Current observational record of 10-15 years is a
    big limitation
  • gt97 of these planets are within Jupiters
    distance

14
  • Relative performance of various methods

www.exoplanet.eu
15
  • Were on the verge of an explosion in exoplanet
    discovery rate

16
Prevalence of Planets
  • Population
  • Total of 450 extrasolar planets
  • Discovery rate 2 week-1
  • Radial velocity searches show planets around 10
    of stars
  • Stars are generally solar type
  • Selection effect best signal / spectral feature
    trade off
  • Planets are generally close in
  • Selection effect most easily detected, short
    observational record
  • Most planets orbit metal rich(er) stars
  • Metals for astronomers means Z gt 2
  • The sun is also metal rich

17
Geoff Marcys internet page.
Detection of weird systems
  • Planets around supergiants
  • Outward migration due to stellar mass loss
  • Some planets do survive
  • Many hot Jupiters
  • Massive planets found close to star
  • Pile up at periods of 4 days (0.05 AU)
  • Can only be the result of orbital migration
  • Large cores and gas envelopes require cool Ts

www.exoplanet.eu
18
  • What about these super-Earths
  • Only two to talk about so far but there will soon
    be many more

Uranus
Earth
www.exoplanet.eu
19
Properties of Super-Earths
  • Size vs Mass
  • Size from transits
  • Mass from radial velocities
  • Equation of state needed to get size/mass
    relation
  • Usually a non-unique solution
  • This is a very simplistic approach
  • With some knowledge of planetary science we can
    eliminate a few possibilities

Swift et al., AstroPH, 2010
20
  • Super-Earths have a minimum radii
  • Collision stripping can build super-Mercurys
  • But material cant escape easily from such a
    large planet
  • Theres no process that actually get you to a
    pure iron planet
  • i.e. super-Earths are not like asteroids

Green 1/10 projectile/target Red1/4
projectile/target Blue 1/1 projectile/target
Earth
Pure iron
Marcus et al., ApJ 2010
21
Properties of Super-Earths
  • Plate tectonics?
  • Earth yes
  • Venus No
  • What about bigger planets?
  • Competing factors
  • Higher gravity compresses and strengthens the
    lithosphere
  • More vigorous convection more shear stress to
    move and deform plates
  • Also, Faster convection means plates are younger
    at subduction zones
  • Cooled enough (dense enough) to subduct?

22
  • Valencia et al. 2010
  • Argues lithosphere will be thinner on larger
    planets
  • Counters the strengthening due to gravity
  • Super-Earths have plate tectonics
  • Earth is borderline for plate tectonics in this
    model
  • Requires wet conditions

Increasing shear stress
Dry
Wet
Fault strength vs planetary mass
23
  • Alternate viewpoint
  • ONeill and Lenardic 2007

24
  • Two case examples
  • CaRoT 7b
  • GJ 1214b
  • Both masses and sizes known
  • A few other super-Earth planets where we only
    have the mass are known

25
  • GJ1214b
  • Mass 6.6 Earth Masses
  • Radius 2.7 Earth Radii
  • Density 1900 kg/m3
  • Composition mostly water
  • H/He envelope probably required
  • Temperatures 450K
  • Probably a very deep ocean

26
  • CaRoT7b
  • Mass 4.8 Earth Masses
  • Radius 1.7 Earth Radii
  • Density Earth
  • Composition is rocky
  • Temperatures 2000K
  • Plate tectonics here?

27
The Story
4.5 Billion years
  • Weve seen 400 years worth of this story 1st
    hand
  • One ten millionth of solar system history
  • Equivalent to watching 1 milli-second of a three
    hour movie
  • Which we use to figure out the plot, the actors,
    and what plays out at each location

28
Dramaticus Personae
Volcanoes
Tectonics
Impact cratering
Eolian
Fluvial
Glacial
29
On location
Mercury
Enceladus
Titan
Mars
30
The Story
4.5 Billion years
  • Weve seen 400 years worth of this story 1st
    hand
  • One ten millionth of solar system history
  • Equivalent to watching 1 milli-second of a three
    hour movie
  • Which we use to figure out the plot, the actors,
    and what plays out at each location

31
Masses and the Brown Dwarf Desert
  • Binary stars are common 50
  • Initially controversial as to whether these
    orbiting bodies were
  • Low mass binary companions (brown dwarves)
  • Planets formed from an accretion disk
  • Mass distribution is heavily skewed to lower
    masses
  • Not (for once) a selection effect
  • Low mass bodies are harder to detect yet we still
    find more of them
  • Follows a power law
  • Indicates large population of smaller objects
  • The brown dwarf desert
  • Few bodies between 10 and 80 MJ
  • This low-mass population probably had a separate
    formation mechanism

32
Orbital Behavior
  • 26 multiple planet systems
  • E.g. Upsilon Andromedea
  • Some with mean motion-resonances
  • Hot-Jupiters/Neptunes
  • Pile up at 4 day periods
  • Eccentricities very small
  • Tidal damping has been very effective
  • Other systems
  • Unusually high eccentricities
  • Unexplained passing stars, disk interactions
  • Eccentric gas giants are a problem for
    terrestrial planets

33
Physical Properties
  • Not much to go on
  • Future missions will provide spectra
  • Planets that both transit and have radial
    velocity measurements indicate gas giant
    densities
  • Hot Neptunes now also known
  • Overall understanding hasnt improved much in the
    past 10 years
  • Modeling of expected atmospheric behavior yields
    some exotic results

Gillon et al., 2007
34
Future Missions
  • Terrestrial Planet Finder (TPF)
  • Direct imaging and spectra
  • 1. Coronagraph
  • 2. Interferometer
  • KEPLER
  • Transit observatory 1m mirror
  • Launch 2009
  • Monitor 105 stars for 4 years
  • Space Interferometry Mission (SIM)
  • Astrometric observatory
  • 4 µ arcsec
  • Will discover a lot of Jupiters
  • Probably not terrestrial planets
  • DARWIN
  • ESA mission
  • Direct imaging and spectra

35
  • Hopes for TPF and DARWIN
  • Non-equilibrium component in atmospheres may be
    signs of life

36
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37
Planetary Detection Microlensing
  • Planet and star pass in front of a background
    star
  • Masses act as gravitational lenses
  • Background star amplified
  • Spread into Einstein ring (unresolved)
  • Limitations
  • Once off observation
  • Lensing from planets lasts less than a day
  • Retrieves mass, but not period
  • Need dense background of stars
  • E.g. galactic bulge
  • Low mass planet detected
  • 5.5 Earth mass around a cool red dwarf (a
    super-Pluto)

Beaulieu et al., 2006
38
Planetary Detection Pulsar Timing
  • Neutron star with magnetic and rotational axes
    unaligned
  • Rotation causes energetic beams to sweep through
    space
  • We measure very regular radio pulses
  • Pulsars are thought to be the best time-keepers
    in the universe, but
  • some have pulses speeding up and slowing down
  • Pulses take longer to travel here when the star
    is further away
  • Rotation around a center of mass causes distance
    changes
  • Pulse frequency oscillates with orbit
  • Analogous to Doppler effect
  • Technique also applied to pulsating white dwarves
  • Very precise technique
  • Can detect planets down to below 0.1 Earth Masses
  • Smallest planet to date PSR 125712 b (2 Earth
    Mass)
  • Drawbacks
  • Pulsars are relatively rare
  • Planets probably affected by supernovae blast
    wave

39
Planetary Detection Astrometry
  • Look directly for positional shifting
  • Remove effects of proper motion
  • Angular motion given by
  • E.g. Jupiter around the sun at 10pc 0.5
    milli-arcsec
  • Doable with interferometers
  • Most sensitive to large orbits
  • but you have to wait a long time
  • Good mass estimates but poor eccentricity
    control
  • Still no planet detected this way
  • but it can pin down inclinations of known planets

Benedict et al., 2002
40
  • Type I migration spiral density waves (fast)
  • Torque exerted at Lindblad resonances
  • Torque on outer disk is stronger than inner disk
  • So planet migrates inwards on timescale
  • Not very long!
  • Type II migration gap opens (slower)
  • Planet moves inward with the viscous gas
    timescales of 106 years
  • Independent of planet mass
  • Disk is truncated at the inner edge.
  • Planets can stall there

Phil Armitages internet page.
  • Close proximity high mass
  • Ideal candidates for radial velocity and transit
    obs
  • Transit gives sin(i) and size
  • Radial velocity gives mass, eccentricity and
    period
  • \We can get density values
  • Objects are definitely gas giants
  • Hot Neptunes now also discovered
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